2019 en paleontología

Overview of the events of 2019 in paleontology
Lista de años en paleontología( mesa )
En paleontología de artrópodos
2016
2017
2018
2019
2020
2021
2022
En paleoentomología
2016
2017
2018
2019
2020
2021
2022
En paleomalacología
2016
2017
2018
2019
2020
2021
2022
En paleoictiología
2016
2017
2018
2019
2020
2021
2022
En paleontología de reptiles
2016
2017
2018
2019
2020
2021
2022
En la paleontología de los arcosaurios
2016
2017
2018
2019
2020
2021
2022
En paleontología de mamíferos
2016
2017
2018
2019
2020
2021
2022

La paleontología o paleontología es el estudio de las formas de vida prehistóricas en la Tierra a través del examen de fósiles de plantas y animales . [1] Esto incluye el estudio de fósiles corporales, huellas ( icnitas ), madrigueras , partes desechadas, heces fosilizadas ( coprolitos ), palinomorfos y residuos químicos . Debido a que los humanos han encontrado fósiles durante milenios, la paleontología tiene una larga historia tanto antes como después de formalizarse como ciencia . Este artículo registra descubrimientos y eventos significativos relacionados con la paleontología que ocurrieron o fueron publicados en el año 2019.

Flora

Plantas

Hongos

NombreNovedadEstadoAutoresEdadLocalidad tipoPaísNotasImágenes

Chaetosphaeria elsikii [2]

noviembre esp.

Válido

Libra y otros.

mioceno

Formación Brassington

 Reino Unido

Un hongo , una especie de Chaetosphaeria .

Meliolinites neogenicus [3]

noviembre esp.

Válido

Khan, Bera y Bera

Plioceno tardío a Pleistoceno temprano

Formación Kimin

 India

Un hongo perteneciente a la familia Meliolaceae .

Meliolinites pliocenicus [4]

noviembre esp.

Válido

Bera, Khan y Bera

Plioceno

Formación Subansiri

 India

Un hongo perteneciente a la familia Meliolaceae .

Ophiocordyceps dominicanus [5]

noviembre esp.

Válido

Poinar y Vega

Burdigaliano

Ámbar dominicano

 República Dominicana

Hongo, especie de Ophiocordyceps . Anunciado en 2019; la versión final del artículo que lo nombra se publicó en 2020.

Ourasphaira [6]

Gen. y sp. nov.

Válido

Loron y otros.

Transición MesoproterozoicoNeoproterozoico

Formación Bahía Grassy

 Canadá

Un microorganismo eucariota multicelular portador de procesos . Loron et al. (2019) sostienen que es un hongo primitivo. [7] El género incluye la nueva especie O. giraldae .

Paleoglomus strotheri [8]

noviembre esp.

Válido

Retallack

Ordovícico ( Darriwiliano )

Formación Lenoir

 Estados Unidos
( Tennessee ) 

Phomites neogenicus [9]

noviembre esp.

Válido

Vishnu, Khan y Bera en Vishnu et al.

Neógeno

 India

Un hongo similar a los miembros del género Phoma .

Phomites siwalicus [9]

noviembre esp.

Válido

Vishnu, Khan y Bera en Vishnu et al.

Neógeno

 India

Un hongo similar a los miembros del género Phoma .

Policefalomices báltica [5]

noviembre esp.

Válido

Poinar y Vega

Priaboniano

Ámbar báltico

 Rusia
( Óblast de Kaliningrado ) 

Hongo perteneciente a la familia Ophiocordycipitaceae . Anunciado en 2019; la versión final del artículo que lo nombra se publicó en 2020.

Priscadvena [10]

Gen. y sp. nov.

Válido

Poinar y Vega

Cretácico tardío ( Cenomaniano )

Ámbar birmano

 Birmania

Tricomiceto kickxellomycotine del nuevo orden Priscadvenales. Especie tipo P. corymbosa .

Prototaxites honeggeri [8]

noviembre esp.

Válido

Retallack

Ordovícico (Darriwiliano)

Formación Lenoir

 Estados Unidos
( Tennessee ) 

Rhexoampullifera stogieana [2]

noviembre esp.

Válido

Libra y otros.

mioceno

Formación Brassington

 Reino Unido

Un hongo perteneciente al grupo Ascomycota .

Rhexoampullifera sufflata [2]

noviembre esp.

Válido

Libra y otros.

mioceno

Formación Brassington

 Reino Unido

Un hongo perteneciente al grupo Ascomycota .

Investigación paleomicológica

Esponjas

Investigación

Nuevos taxones

NombreNovedadEstadoAutoresEdadLocalidad tipoPaísNotasImágenes

Acanthochaetetes huauclillensis [17]

noviembre esp.

Válido

Sánchez-Beristain, García-Barrera & Moreno-Bedmar

Cretácico temprano (finales del Hauteriviano a principios del Barremiano )

 México

Una esponja quetétida .

Allosacus pedunculatus [18]

noviembre esp.

Válido

Carrera y Sumrall

Ordovícico

Caliza Lenoir

 Estados Unidos
( Tennessee ) 

Un miembro de la familia Streptosolenidae.

Auraeopirania [19]

Gen. y comb. y 3 sp. nov.

Válido

Botting y otros.

Ordovícico

Formación Fezouata
Formación Llanfallteg
Formación Ningkuo

 China Marruecos Reino Unido
 
 

Miembro de Protomonaxonida perteneciente a la familia Piraniidae. La especie tipo es " Pirania " auraeum Botting (2007); El género también incluye nuevas especies A. pinwyddeni , A. pykitia y A. sciurucauda .

Cannapirania [19]

Gen. y 2 sp. y comb. nov.

Válido

Botting y otros.

Ordovícico

Formación Llanfawr Mudstones
Formación Wenchang

 China Reino Unido
 

Miembro de Protomonaxonida perteneciente a la familia Piraniidae. La especie tipo es C. canna ; El género también incluye nuevas especies C. vermiformis' , así como "Pirania" llanfawrensis Botting (2004).

Carduspongia [20]

Gen. y sp. nov.

Válido

Nadhira y otros.

Silúrico ( Wenlock )

Formación Coalbrookdale

 Reino Unido

Esponja , posiblemente calcárea . La especie tipo es C. pedicula .

Centrosia clavata [21]

noviembre esp.

Válido

Świerczewska-Gładysz, Jurkowska y Niedźwiedzki

Cretácico tardío ( Turoniense tardío )

Cuenca de Opole

 Polonia

Una esponja hexactinelida perteneciente a la familia Callodictyonidae.

Crateromorpha opolensis [21]

noviembre esp.

Válido

Świerczewska-Gładysz, Jurkowska y Niedźwiedzki

Cretácico tardío ( Turoniense tardío y Coniaciense temprano )

Cuenca de Opole

 Polonia

Una esponja hexactinelida perteneciente a la familia Rossellidae .

Primordios de cistostroma [22]

noviembre esp.

Válido

Jeon y otros.

Ordovícico ( Floiano a Darriwiliano )

Formación Duwibong
Formación Hunghuayuan

 China Corea del Sur
 

Un miembro de Stromatoporoidea .

Eoghanospongia [23]

Gen. y sp. nov.

Válido

Botting y otros.

Silúrico ( Telychian )

 Reino Unido

Esponja hexactinellida . El género incluye la nueva especie E. carlinslowpensis . Anunciada en 2019 ; la versión final del artículo que la nombra se publicó en 2020.

Hamptonia jianhensis [24]

noviembre esp.

Válido

Wang y otros.

Estadio cámbrico 4

 Porcelana

Una esponja .

Jianhella [25]

Gen. y sp. nov.

Válido

Wang y otros.

Estadio cámbrico 4

Formación Balang

 Porcelana

Una esponja leptomítida. El género incluye la nueva especie J. obconica .

Monoplectroninia malonei [26]

noviembre esp.

Válido

McSweeney, Buckeridge y Kelly

Mioceno temprano

Caliza de Batesford

 Australia

Una esponja calcárea perteneciente a la familia Minchinellidae .

Pachastrella rara [21]

noviembre esp.

Válido

Świerczewska-Gładysz, Jurkowska y Niedźwiedzki

Cretácico tardío ( Turoniense tardío )

Cuenca de Opole

 Polonia

Una demosponja perteneciente a la familia Pachastrellidae .

Paleorosella [27]

Gen. y sp. nov.

Válido

Li y otros.

Ordovícico más reciente

 Porcelana

Una esponja hexactinellida rossélida . El género incluye la nueva especie P. sinensis .

Pellipirania [19]

Gen. y sp. nov.

Válido

Botting y otros.

Ordovícico ( Tremadociano )

Formación Fezouata

 Marruecos

Miembro de Protomonaxonida perteneciente a la familia Piraniidae. La especie tipo es P. gloria .

Pirania?ericia [19]

noviembre esp.

Válido

Botting y otros.

Ordovícico ( Tremadociano )

Formación Dol-Cyn-Afon

 Reino Unido

Un miembro de Protomonaxonida perteneciente a la familia Piraniidae.

Pirania peregrinata [19]

noviembre esp.

Válido

Botting y otros.

Ordovícico ( Floiano )

Formación Ningkuo

 Porcelana

Un miembro de Protomonaxonida perteneciente a la familia Piraniidae.

Pseudoleptomito [28]

Gen. y sp. nov.

Válido

Botting y otros.

Triásico temprano

 Estados Unidos

Esponja perteneciente al grupo Protomonaxonida y a la familia Leptomitidae. El género incluye la nueva especie P. advenus .

Rugocoelia loudonensis [18]

noviembre esp.

Válido

Carrera y Sumrall

Ordovícico

Caliza Lenoir

 Estados Unidos
( Tennessee ) 

Un miembro de la familia Anthaspidellidae .

Subesferospongia [29]

Gen. y comb. nov.

Válido

Bizzarini

Triásico tardío

 Italia

Una esponja ; un nuevo género para "Stellispongia" subsphaerica Dieci, Antonacci & Zardini (1970).

Teganiella finksi [30]

noviembre esp.

Válido

Mouro y otros.

Carbonífero ( Pensilvaniano )

Esquisto de la cantera de la Meca

 Estados Unidos

Vasospongia [31]

Gen. y sp. nov.

Válido

Tang y Xiao en Tang et al.

Etapa 2 del Cámbrico

Formación Hetang

 Porcelana

Esponja de ubicación filogenética incierta. La especie tipo es V. sinensis .

Vauxia leioia [32]

noviembre esp.

Válido

Luo, Zhao y Zeng

Etapa 3 del Cámbrico

 Porcelana

Una esponja vauxídica .

Cnidarios

Investigación

  • Sun, Elias y Lee (2019) publican un estudio sobre las características de crecimiento de tres especies de corales del Ordovícico pertenecientes al género Agetolites de la Formación Xiazhen ( China ), y sobre sus implicaciones para inferir las relaciones filogenéticas de este género. [33]
  • Harris et al. (2019) publican un estudio sobre un gran coral rugoso colonial de la Formación Kope del Ordovícico ( Kentucky , Estados Unidos ). [34]
  • Liang, Elias y Lee (2019) publicaron un estudio sobre la morfología , las características de crecimiento y las relaciones filogenéticas del coral tabulado silúrico Halysites catenularius . [35]
  • Landmeyer et al. (2019) informaron de fósiles de corales tabulados sin septos en Carolina del Sur , lo que representa la primera evidencia de que areniscas paleozoicas no metamorfoseadas y ligeramente endurecidas afloran entre los depósitos de la provincia de la llanura costera atlántica de los Estados Unidos . [36] Este hallazgo es muy discutido porque todas las demás rocas de la era paleozoica en el área de estudio están muy metamorfoseadas, las rocas donde se encontraron los fósiles se mapean tradicionalmente como la Formación Middendorf del Cretácico y se sugiere que los fósiles en cuestión son la corteza de coníferas cretácicas en arenisca cretácica, en lugar de corales paleozoicos en arenisca paleozoica. [37]
  • Weiss y Martindale (2019) publicaron un estudio cuyo objetivo era determinar si la selección ecológica basada en la fisiología, el comportamiento, el hábitat, etc., jugó un papel en la supervivencia a largo plazo de los corales durante el Paleoceno tardío y el Eoceno temprano . [38]
  • Precht et al. (2019) informan sobre fósiles de Acropora prolifera que datan del Pleistoceno . [39]
  • Jones et al. (2019) publican un estudio sobre la distribución de los corales de arrecife durante el último interglacial y también evalúan la utilidad de los datos de corales de arrecife fósiles para predecir el impacto de los cambios climáticos futuros en los corales de arrecife. [40]
  • Un estudio sobre un espécimen fósil problemático de la Formación Devónica Ponta Grossa ( Brasil ), asignado por diferentes autores a la especie Serpulites sica o Euzebiola clarkei , es publicado por Van Iten et al. (2019), quienes interpretan este fósil como un medusozoo capaz de gemación clonal , y lo transfieren al género Sphenothallus . [41]
  • Zapalski y Berkowski han descrito los ecosistemas de coral mesofóticos más antiguos, que datan del Silúrico medio, de los lechos inferiores de Visby en Gotland. [42] Estas comunidades, dominadas por corales laminares, también brindan pistas sobre el inicio de la simbiosis coral-alga.
  • Mihaljević (2019) describe nuevas colecciones de corales fósiles del Oligoceno y Mioceno de Sarawak ( Malasia ), la isla de Negros y Cebú ( Filipinas ). [43]
  • Senowbari-Daryan & Link (2019) publican un estudio sobre la anatomía, ontogenia y taxonomía del hidrozoo noriano Heterastridium , basado en datos de especímenes fósiles del centro de Irán y el sur de Turquía . [44]

Nuevos taxones

NombreNovedadEstadoAutoresEdadLocalidad tipoPaísNotasImágenes

Amygdalophylloides omarai [45]

noviembre esp.

Válido

Kora, Herbig y El Desouky

Carbonífero ( Moscoviense )

Formación Rod El Hamal

 Egipto

Un coral rugoso .

Antilia coatesi [46]

noviembre esp.

Válido

Budd y Klaus en Budd et al.

Mioceno tardío – Plioceno tardío

Formación Bowden Formación
Gurabo Formación
Mao
Formación Old Bank

 República Dominicana Jamaica Panamá
 
 

Un coral perteneciente a la subfamilia Mussinae .

Aulopora chiharai [47]

noviembre esp.

Válido

Niko, Ibaraki y Tazawa

devoniano

 Japón

Bothrophyllum cylindricum [45]

noviembre esp.

Válido

Kora, Herbig y El Desouky

Carbonífero ( Moscoviense )

Formación Rod El Hamal

 Egipto

Un coral rugoso .

Bothrophyllum suezensis [45]

noviembre esp.

Válido

Kora, Herbig y El Desouky

Carbonífero ( Moscoviense )

Formación Rod El Hamal

 Egipto

Un coral rugoso .

Ceratophyllum simplex [48]

noviembre esp.

Válido

Liao y Liang

Devónico ( Givetian )

Formación Wenglai

 Porcelana

Un coral rugoso.

Conopora alloporoides [49]

noviembre esp.

Válido

Cairns

Mioceno ( Meseniense )

 España

Un miembro de la familia Stylasteridae .

Conopora forticula [49]

noviembre esp.

Válido

Cairns

Mioceno ( Meseniense )

 España

Un miembro de la familia Stylasteridae .

Crypthelia ingens [49]

noviembre esp.

Válido

Cairns

Mioceno ( Meseniense )

 España

Un miembro de la familia Stylasteridae .

Crypthelia zibrowii [49]

noviembre esp.

Válido

Cairns

Mioceno ( Meseniense )

 España

Un miembro de la familia Stylasteridae .

Cyathophyllum wenglaiense [48]

noviembre esp.

Válido

Liao y Liang

Devónico (Givetiano)

Formación Wenglai

 Porcelana

Un coral rugoso.

Cystiphylloides marennense [50]

noviembre esp.

Válido

Coen-Aubert

Devónico ( Givetian )

Formación Mont d'Haurs

 Bélgica

Un coral rugoso perteneciente a la familia Cystiphyllidae. Originalmente descrito como una especie de Cystiphylloides , pero posteriormente se convirtió en la especie tipo del género independiente Marennophyllum . [51]

Devonodisco [52]

Gen. y 2 sp. y comb. nov.

Válido

Pedrero

devoniano

 Canadá Colombia Rusia Australia ? China ? Estados Unidos ? Vietnam ?
 
 
 
 
 
 

Un coral. La especie tipo es D. latisubex ; el género también incluye nuevas especies: D. pedderi , [53] "Combophyllum" multiradiatum Meek (1868), " Glossophyllum " discoideum Soshkina (1936) y posiblemente también "Hadrophyllum" wellingtonense Packham (1954) y "Glossophyllum" clebroseptatum Kravtsov (1975).

Dirimía [54]

Gen. y 6 sp. nov.

Válido

Fedorowski y Ohar

Carbonífero ( Bashkirio )

 Ucrania

Coral rugoso perteneciente a la familia Kumpanophyllidae. La especie tipo es D. multiplexa ; el género también incluye D. similis , D. recessia , D. composita , D. extrema y D. nana .

Distichopora patula [49]

noviembre esp.

Válido

Cairns

Mioceno ( Meseniense )

 España

Un miembro de la familia Stylasteridae .

Gyanyimaphyllum [55]

Gen. y sp. nov.

Válido

Wang y otros.

Pérmico ( Changhsingiano )

 Porcelana

Un coral rugoso . El género incluye la nueva especie G. crassiseptatum .

Heritschioides simplex [56]

noviembre esp.

Válido

Fedorowski, Bamber y Richards

Carbonífero ( Bashkirio )

Formación Mattson

 Canadá
( Territorios del Noroeste ) 

Coral rugoso perteneciente al grupo Stauriida y a la familia Aulophyllidae.

Hispaniastraea ousriorum [57]

noviembre esp.

Válido

Boivin, Vasseur y Lathuilière en Boivin et al.

Jurásico temprano ( Pliensbachiano )

 Marruecos

Un antozoo , posiblemente miembro de Hexanthiniaria.

Ipciphyllum floricolumellum [55]

noviembre esp.

Válido

Wang y otros.

Pérmico ( Changhsingiano )

 Porcelana

Un coral rugoso .

Ipciphyllum naoticum [55]

noviembre esp.

Válido

Wang y otros.

Pérmico ( Changhsingiano )

 Porcelana

Un coral rugoso .

Ipciphyllum zandaense [55]

noviembre esp.

Válido

Wang y otros.

Pérmico ( Changhsingiano )

 Porcelana

Un coral rugoso .

Isophyllia jacksoni [46]

noviembre esp.

Válido

Budd y Klaus en Budd et al.

Mioceno tardío – Pleistoceno temprano

Formación Cercado Formación
Gurabo Formación
Los Haitises Formación
Mao
Formación Seroe Domi

 Curazao República Dominicana
 

Una especie de Isophyllia .

Isophyllia maoensis [46]

noviembre esp.

Válido

Budd y Klaus en Budd et al.

Mioceno tardío – Pleistoceno temprano

Formación Cercado Formación
Gurabo Formación
Isla Colón Formación
Mao

 República Dominicana Panamá
 

Una especie de Isophyllia .

Kumpanophyllum columellatum [58]

noviembre esp.

Válido

Fedorowski

Carbonífero ( Bashkirio )

 Ucrania

Coral rugoso perteneciente a la familia Kumpanophyllidae .

Kumpanophyllum decessum [58]

noviembre esp.

Válido

Fedorowski

Carbonífero ( Bashkirio )

 Ucrania

Coral rugoso perteneciente a la familia Kumpanophyllidae .

Kumpanophyllum levis [58]

noviembre esp.

Válido

Fedorowski

Carbonífero ( Bashkirio )

 Ucrania

Coral rugoso perteneciente a la familia Kumpanophyllidae .

Kumpanophyllum praecox [58]

noviembre esp.

Válido

Fedorowski

Carbonífero ( Bashkirio )

 Ucrania

Coral rugoso perteneciente a la familia Kumpanophyllidae .

Lepidopora fistulosa [49]

noviembre esp.

Válido

Cairns

Mioceno ( Meseniense )

 España

Un miembro de la familia Stylasteridae .

Nemistium liardense [56]

noviembre esp.

Válido

Fedorowski, Bamber y Richards

Carbonífero ( Bashkirio )

Formación Mattson

 Canadá
( Territorios del Noroeste ) 

Un coral rugoso perteneciente al grupo Stauriida y a la familia Lithostrotionidae.

Neorylstonia [59]

Nombre. noviembre

Válido

Vasseur y otros.

Jurásico temprano ( Sinemuriano a Pliensbachiano )

 Marruecos

Un coral pétreo perteneciente al grupo Caryophylliina y a la superfamilia Volzeioidea; un nombre de reemplazo para Mesophyllum Beauvais (1986).

Octapirgitas [60]

Gen. y sp. nov.

Válido

Guo y otros.

Etapa 2 del Cámbrico

Formación Yanjiahe

 Porcelana

Un medusozoo olivoide . El género incluye la nueva especie O. elongatus .

Paraconularia kikapu [61]

noviembre esp.

Válido

Quiroz-Barroso, Sour-Tovar y Quiroz-Barragán

Pérmico

Formación Las Delicias

 México

Un miembro de Conulariida .

Paraconularia kingii [61]

noviembre esp.

Válido

Quiroz-Barroso, Sour-Tovar y Quiroz-Barragán

Pérmico

Formación Las Delicias

 México

Un miembro de Conulariida .

Pliobothrus nielseni [49]

noviembre esp.

Válido

Cairns

Mioceno ( Meseniense )

 España

Un miembro de la familia Stylasteridae .

Pliobothrus striatus [49]

noviembre esp.

Válido

Cairns

Mioceno ( Meseniense )

 España

Un miembro de la familia Stylasteridae .

Procterias (Granulidictyum) alechinskyi [53]

noviembre esp.

En prensa

Másquellec

Devónico ( Emsiano )

Formación Floresta

 Colombia

Un coral tabulado perteneciente al grupo Favositida y a la familia Micheliniidae.

Scolymia meederi [46]

noviembre esp.

Válido

Budd y Klaus en Budd et al.

Plioceno tardío

Formación Tamiami

 Estados Unidos

Una especie de Scolymia .

Scolymia tamiamiensis [46]

noviembre esp.

Válido

Budd y Klaus en Budd et al.

Plioceno tardío

Formación Tamiami

 Estados Unidos

Una especie de Scolymia .

Septuconularios [62]

Gen. y sp. nov.

Válido

Guo y otros.

Etapa 2 del Cámbrico

Formación Yanjiahe

 Porcelana

Un hexangulaconulariido. El género incluye la nueva especie S. yanjiaheensis .

Sinkiangopora kawanoi [63]

noviembre esp.

Válido

Niko y Fujikawa

Pérmico

Caliza Zomeki

 Japón

Un coral tabulado.

Stephanocoonia annae [64]

noviembre esp.

Válido

Perdedor

Cretácico temprano ( Albiano )

 México Estados Unidos
 

Un coral pétreo perteneciente al grupo Astrocoeniina.

Estilaster digitiforme [49]

noviembre esp.

Válido

Cairns

Mioceno ( Meseniense )

 España

Una especie de Stylaster .

Stylaster multicavus [49]

noviembre esp.

Válido

Cairns

Mioceno ( Meseniense )

 España

Una especie de Stylaster .

Stylaster tuberosus [49]

noviembre esp.

Válido

Cairns

Mioceno ( Meseniense )

 España

Una especie de Stylaster .

Thamnophyllum godefroidi [50]

noviembre esp.

Válido

Coen-Aubert

Devónico ( Givetian )

Formación Mont d'Haurs

 Bélgica

Un coral rugoso perteneciente a la familia Phillipsastreidae.

Thamnopora sumitaensis [65]

noviembre esp.

Válido

Nico

Devónico medio

Formación Kamiarisu

 Japón

Un coral tabulado perteneciente al orden Favositida y a la familia Pachyporidae.

Trachyphyllia mcneilli [46]

noviembre esp.

Válido

Budd y Klaus en Budd et al.

Mioceno tardío – Plioceno tardío

Formación Cercado Formación
Gurabo Formación
Mao Formación
Old Bank Formación
Seroe Domi

 Curazao República Dominicana Panamá
 
 

Un pariente del coral cerebro abierto .

Waagenophyllum clisicolumellum [55]

noviembre esp.

Válido

Wang y otros.

Pérmico ( Changhsingiano )

 Porcelana

Un coral rugoso .

Waagenophyllum gyanyimaense [55]

noviembre esp.

Válido

Wang y otros.

Pérmico ( Changhsingiano )

 Porcelana

Un coral rugoso .

Waagenophyllum intermedio [55]

noviembre esp.

Válido

Wang y otros.

Pérmico ( Changhsingiano )

 Porcelana

Un coral rugoso .

Artrópodos

Briozoos

NombreNovedadEstadoAutoresEdadLocalidad tipoPaísNotasImágenes

Adeonellopsis keralaensis [66]

noviembre esp.

Válido

Sonar y Badve

Mioceno ( Burdigaliense )

Camas Quilon

 India

Un briozoo queilostoma .

Aluis [67]

Gen. y sp. nov.

Válido

López-Gappa & Pérez

Mioceno ( Burdigaliense )

Formación Chenque Formación
Monte León
Formación Puesto del Museo

 Argentina

Briozoo queilostomado perteneciente a la familia Chaperiidae . El género incluye la nueva especie A. spinettai .

Atlantisina mylaensis [68]

noviembre esp.

Válido

Rojo y ciruelo

Pleistoceno temprano ( Gelasiano )

 Italia

Ceriocava escuelas [69]

noviembre esp.

Válido

Martha y otros.

Cretácico tardío ( Santoniano )

 Alemania

Un supuesto ciclóstoma cerioporino .

Characodoma multiavicularia [70]

noviembre esp.

Válido

Di Martino y Taylor en Di Martino et al.

mioceno

 Indonesia

Una especie de Characodoma .

Charixa bispinata [71]

noviembre esp.

Válido

Martha, Taylor y Rader

Cretácico temprano ( Albiano )

 Estados Unidos

Un miembro de Cheilostomata .

Charixa emanuelae [71]

noviembre esp.

Válido

Martha, Taylor y Rader

Cretácico temprano ( Albiano )

 Estados Unidos

Un miembro de Cheilostomata.

Charixa sexspinata [71]

noviembre esp.

Válido

Martha, Taylor y Rader

Cretácico temprano ( Albiano )

 Estados Unidos

Un miembro de Cheilostomata.

Devona Victoria [72]

Nombre. noviembre

Válido

Hernández

devoniano

 Rusia

Un briozoo rabdomésido; un nombre de reemplazo para Salairella Mesentseva (2015).

Evactinopora mangeri [73]

noviembre esp.

Válido

Yancey y otros.

Carbonífero ( Misisipiense )

América del norte

Un miembro de Cystoporata .

Gigantopora vartonensis [74]

noviembre esp.

Válido

Pedramara y otros.

mioceno

Formación Qom

 Irán

Homotrypa niagarensis [75]

noviembre esp.

Válido

Ernst, Brett y Wilson

Silúrico ( Aeroniano )

Formación Reynales

 Estados Unidos

Un briozoo trepostoma .

Hyporosopora keera [76]

noviembre esp.

Válido

Martha, Taylor y Rader

Cretácico temprano ( Albiano )

 Estados Unidos

Un miembro de Cyclostomatida .

Iyarispora [71]

Gen. y 2 sp. nov.

Válido

Martha, Taylor y Rader

Cretácico temprano ( Albiano )

 Estados Unidos

Miembro de Cheilostomata. El género incluye las nuevas especies I. ikaanakiteeh e I. chiass .

Lacrimula patriciae [70]

noviembre esp.

Válido

Di Martino y Taylor en Di Martino et al.

mioceno

 Indonesia

Un queilostoma de grado ascóforo .

Leioclema adsuetum [75]

noviembre esp.

Válido

Ernst, Brett y Wilson

Silúrico ( Aeroniano )

Formación Reynales

 Estados Unidos

Un briozoo trepostoma .

Leptotrypa lipovkiensis [77]

noviembre esp.

Válido

Tolokonnikova y Pakhnevich

Devónico ( Fameniano )

Formación Zadonsk

 Rusia

Un briozoo trepostoma .

Mesonopora bernardwalteri [76]

noviembre esp.

Válido

Martha, Taylor y Rader

Cretácico temprano ( Albiano )

 Estados Unidos

Un miembro de Cyclostomatida.

Micropora stellata [78]

noviembre esp.

Válido

Di Martino, Taylor & Portell

Plioceno ( Piacenziano )

Formación Tamiami

 Estados Unidos

Una especie de Micropora .

Microporella sarasotaensis [78]

noviembre esp.

Válido

Di Martino, Taylor & Portell

Plioceno ( Piacenziano )

Formación Tamiami

 Estados Unidos

Un miembro de Ascophora perteneciente a la familia Microporellidae .

Microporella tamiamiensis [78]

noviembre esp.

Válido

Di Martino, Taylor & Portell

Plioceno ( Piacenziano )

Formación Tamiami

 Estados Unidos

Un miembro de Ascophora perteneciente a la familia Microporellidae .

Moyerella parva [75]

noviembre esp.

Válido

Ernst, Brett y Wilson

Silúrico ( Aeroniano )

Formación Reynales

 Estados Unidos

Un briozoo criptóstomo rabdomesino .

Oncousoecia khirar [76]

noviembre esp.

Válido

Martha, Taylor y Rader

Cretácico temprano ( Albiano )

 Estados Unidos

Un miembro de Cyclostomatida.

Pinegopora chilensis [79]

noviembre esp.

Válido

Carrera y col.

Pérmico

Formación Cerro El Árbol

 Chile

Miembro de Cryptostomata perteneciente al grupo Rhabdomesina y a la familia Nikiforovellidae.

Pourtalesella chiarae [78]

noviembre esp.

Válido

Di Martino, Taylor & Portell

Plioceno ( Piacenziano )

Formación Tamiami

 Estados Unidos

Un miembro de Ascophora perteneciente a la familia Celleporidae .

Pseudidmonea debodeae [80]

noviembre esp.

Válido

Di Martino y Taylor

Mioceno temprano

Caliza de Forest Hill

 Nueva Zelanda

Un ciclóstomo pseudomonéido .

Pseudomonas oretiensis [80]

noviembre esp.

Válido

Di Martino y Taylor

Mioceno temprano

Caliza de Forest Hill

 Nueva Zelanda

Un ciclóstomo pseudomonéido .

Pseudobathystomella mira [81]

noviembre esp.

Válido

Koromyslova, Martha y Pakhnevich

Cretácico tardío ( Maastrichtiano tardío )

 Turkmenistán

Un briozoo queilostoma perteneciente a la superfamilia Lepralielloidea.

Ptilotrypa bajpaii [82]

noviembre esp.

Válido

Swami y otros.

Ordovícico ( Katian )

Caliza Yong

 India

Un miembro de Cryptostomata .

Reptomultisparsa mclemoreae [76]

noviembre esp.

Válido

Martha, Taylor y Rader

Cretácico temprano ( Albiano )

 Estados Unidos

Un miembro de Cyclostomatida.

Rhammatopora glenrosa [71]

noviembre esp.

Válido

Martha, Taylor y Rader

Cretácico temprano ( Albiano )

 Estados Unidos

Un miembro de Cheilostomata.

Simplicidium jontoddi [71]

noviembre esp.

Válido

Martha, Taylor y Rader

Cretácico temprano ( Albiano )

 Estados Unidos

Un miembro de Ctenostomatida .

Skylonia malabarica [66]

noviembre esp.

Válido

Sonar y Badve

Mioceno ( Burdigaliense )

Camas Quilon

 India

Un briozoo queilostoma .

Laurel de Spiniflabellum [78]

noviembre esp.

Válido

Di Martino, Taylor & Portell

Plioceno ( Piacenziano )

Formación Tamiami

 Estados Unidos

Un miembro de Ascophora perteneciente a la familia Cribrilinidae .

Stenosipora? cribrata [70]

noviembre esp.

Válido

Di Martino y Taylor en Di Martino et al.

mioceno

 Indonesia

Un queilostoma de grado ascóforo .

Stylopoma warkhalensis [66]

noviembre esp.

Válido

Sonar y Badve

Mioceno ( Burdigaliense )

Camas Quilon

 India

Un briozoo queilostoma .

Tobolocel [83]

Gen. y sp. nov.

Válido

Koromyslova, Pakhnevich y Fedorov

Cretácico tardío ( Maastrichtiano )

 Kazajstán

Briozoo queilostomado . El género incluye la nueva especie T. levinae .

Trypostega composita [78]

noviembre esp.

Válido

Di Martino, Taylor & Portell

Plioceno ( Piacenziano )

Formación Tamiami

 Estados Unidos

Un miembro de Ascophora perteneciente a la familia Trypostegidae .

Uzbekipora [81]

Gen. y comb. nov.

Válido

Koromyslova, Martha y Pakhnevich

Cretácico tardío ( Campaniano tardío )

 Uzbekistán

Briozoo queilostomado perteneciente a la superfamilia Lepralielloidea. La especie tipo es " Porina " anplievae Favorskaya (1992).

Vincularia taylori [66]

noviembre esp.

Válido

Sonar y Badve

Mioceno ( Burdigaliense )

Camas Quilon

 India

Un briozoo queilostoma .

Braquiópodos

Moluscos

Equinodermos

Investigación

  • Topper et al. (2019) publican un estudio sobre la morfología y las relaciones filogenéticas del supuesto equinodermo del tallo Yanjiahella biscarpa ; [84] el estudio es posteriormente criticado por Zamora et al. (2020). [85] [86]
  • Lefebvre et al. (2019) describen rastros de tejido blando encontrados junto con moldes esqueléticos en estilóforos , quienes interpretan sus hallazgos como un respaldo a las afinidades de los estilóforos con los equinodermos y no con los hemicordados . [87]
  • Nohejlová et al. (2019) publican un estudio sobre la morfología y las relaciones filogenéticas del equinodermo lepidocistoideo Vyscystis . [88]
  • Sheffield y Sumrall (2019) publican un estudio sobre las relaciones filogenéticas de los blastozoos diploporitanos . [89]
  • Sheffield y Sumrall (2019) publican un estudio sobre la morfología del sistema ambulacral de alimentación en el diploporita del Ordovícico Eumorphocystis , tal como lo indican los datos de especímenes bien conservados de la Formación Bromide ( Oklahoma , Estados Unidos ), quienes interpretan sus hallazgos como una indicación de que Eumorphocystis estaba estrechamente relacionado con los crinoideos y que los crinoideos están anidados dentro de los blastozoos; [90] sus conclusiones sobre la relación entre Eumorphocystis y los crinoideos son posteriormente refutadas por Guensburg et al. (2020). [91]
  • Bauer, Waters y Sumrall (2019) publican un estudio sobre la morfología y las relaciones filogenéticas de Macurdablastus uniplicatus . [92]
  • Un estudio sobre la morfología y las relaciones filogenéticas de Hexedriocystis es publicado en línea por Zamora & Sumrall (2019), quienes consideran a este taxón como un blastozoo. [93]
  • Shroat-Lewis, Greenwood y Sumrall (2019) publican un estudio sobre la paleoecología de los especímenes del edrioasteroide Neoisorophusella lanei conservados en losas de piedra caliza de la Formación Kinkaid del Carbonífero ( Chesteriano ) ( Illinois , Estados Unidos ). [94]
  • Peter (2019) publicó un estudio sobre la morfología de Cupulocrinus y sus implicaciones para inferir el origen de los crinoideos flexibles . [95]
  • Cole (2019) publicó un estudio sobre las relaciones filogenéticas de los crinoideos diplobatrídeos . [96]
  • Cole (2019) publicó en línea un estudio sobre los controles biológicos y ecológicos de la duración de los géneros de crinoideos diplobatrídeos. [97]
  • Brom (2019) publicó un estudio sobre los patrones macroevolutivos de las tendencias del tamaño corporal de los crinoideos citocrinidos . [98]
  • Cole, Wright y Ausich (2019) publican un estudio sobre los patrones de estructura de la paleocomunidad y la partición del nicho en crinoideos del Ordovícico ( Katian ) Brechin Lagerstätte ( Ontario , Canadá ). [99]
  • Saulsbury & Zamora (2019) publica en línea un estudio sobre la anatomía de los sistemas nervioso y circulatorio del crinoideo del Cretácico Decameros ricordeanus y sobre las relaciones filogenéticas de esta especie. [100]
  • Thompson y Bottjer (2019) publicarán un estudio sobre la preferencia de sustrato en los erizos de mar del grupo de tallos durante el período Carbonífero . [101]
  • Pietsch et al. (2019) publican un estudio sobre la recuperación de los erizos de mar en el Triásico temprano después de la extinción masiva del Pérmico-Triásico [102] .
  • Una estrella frágil fósil perteneciente al género Ophiopetra , que representa el primer registro de estrella frágil articulada del Mesozoico de América del Sur reportado hasta el momento, es descrita del Miembro Agua de la Mula del Cretácico Inferior de la Formación Agrio ( Argentina ) por Fernández et al. (2019), quienes transfieren el género Ophiopetra a la familia Ophionereididae dentro del orden Amphilepidida . [103]

Nuevos taxones

NombreNovedadEstadoAutoresEdadLocalidad tipoPaísNotasImágenes

Acanthocrinus carsli [104]

noviembre esp.

Válido

Ausich y Zamora

Devónico ( Emsiano )

Formación Mariposas

 España

Un crinoideo camerado .

Aplinocrino estriado [105]

noviembre esp.

Válido

Vendaval

Cretácico tardío

 Francia Reino Unido
 

Un crinoideo perteneciente al grupo Roveacrinida y a la familia Saccocomidae.

Arqueocidaris ivanovi [106]

noviembre esp.

Válido

Thompson y Mirantsev en Thompson et al.

Carbonífero

 Rusia

Un erizo de mar .

Astrosombra [107]

Gen. y sp. nov.

Válido

Thuy, Gale y Numberger-Thuy

Cretácico tardío ( Maastrichtiano )

 Alemania

Estrella frágil perteneciente a la familia Amphilimnidae . La especie tipo es A. rammsteinensis .

Atenacrino [108]

Gen. y sp. nov.

Válido

Guensburg y otros.

Ordovícico

Formación Fillmore

 Estados Unidos
( Utah ) 

Crinoideo perteneciente al grupo Disparida . La especie tipo es A. broweri .

Becsciecrinus groulxi [109]

noviembre esp.

Válido

Ausich y Cournoyer

Límite Ordovícico - Silúrico

 Canadá

Un crinoideo .

Binocalix [110]

Gen. y sp. nov.

Válido

McDermott y Paul

Ordovícico tardío

 Reino Unido

Un diploporito aristocistídeo . El género incluye la nueva especie B. dichotomus .

Bucucrinus isotaloi [109]

noviembre esp.

Válido

Ausich y Cournoyer

Límite Ordovícico - Silúrico

 Canadá

Un crinoideo .

Carstenicrino [111]

Gen. y comb. nov.

Válido

Roux, Eléaume y Améziane

Cretácico superior ( Campaniano y Maastrichtiano ) y Paleoceno ( Daniano )

 Dinamarca Alemania Turkmenistán
 
 

Un crinoideo . La especie tipo es "Apiocrinus" constrictus von Hagenow en Quenstedt (1876); El género también incluye "Bourgueticrinus" baculatus Klikushin (1982) y "Bourgueticrinus" danicus Brünnich Nielsen (1913).

Caveacrino [105]

Gen. y 2 sp. nov.

Válido

Vendaval

Cretácico tardío ( Turoniense )

 Francia Reino Unido
 

Crinoideo perteneciente al grupo Roveacrinida y a la familia Roveacrinidae. La especie tipo es C. asynchronousus ; el género también incluye a C. serratus .

Coláster blanco [112]

noviembre esp.

Válido

Blake y Nestell

Carbonífero ( Chesteriano )

Caliza de Bangor

 Estados Unidos

Una estrella frágil .

Conocrinus cahuzaci [111]

noviembre esp.

Válido

Roux, Eléaume y Améziane

Eoceno ( Bartoniano )

 Francia

Un crinoideo .

Costatocrinus elegans [105]

noviembre esp.

Válido

Vendaval

Cretácico tardío

 Francia Reino Unido
 

Un crinoideo perteneciente al grupo Roveacrinida y a la familia Saccocomidae.

Costatocrinus erismus [105]

noviembre esp.

Válido

Vendaval

Cretácico tardío

 Francia Reino Unido
 

Un crinoideo perteneciente al grupo Roveacrinida y a la familia Saccocomidae.

Costatocrinus rostratus [105]

noviembre esp.

Válido

Vendaval

Cretácico tardío ( Santoniano )

 Francia Reino Unido
 

Un crinoideo perteneciente al grupo Roveacrinida y a la familia Saccocomidae.

Crassicoma cretacea [105]

noviembre esp.

Válido

Vendaval

Cretácico tardío ( Turoniense )

 Francia Reino Unido
 

Un crinoideo perteneciente al grupo Roveacrinida y a la familia Saccocomidae.

Crassicoma veulesensis [105]

noviembre esp.

Válido

Vendaval

Cretácico tardío ( Santoniano )

 Francia

Un crinoideo perteneciente al grupo Roveacrinida y a la familia Saccocomidae.

Culicocrinus breimeri [104]

noviembre esp.

Válido

Ausich y Zamora

Devónico ( Emsiano )

Formación Mariposas

 España

Un crinoideo camerado .

Dendrocrinus simcoensis [113]

noviembre esp.

Válido

Wright, Cole y Ausich

Ordovícico ( Katian )

Establos de Brechin

 Canadá
( Ontario ) 

Un crinoideo perteneciente al grupo Cladida .

Dentatocrino [105]

Gen. y 4 sp. nov.

Válido

Vendaval

Cretácico tardío ( Turoniense )

 Francia Reino Unido
 

Crinoideo perteneciente al grupo Roveacrinida y a la familia Roveacrinidae. La especie tipo es D. dentatus ; el género también incluye a D. minutus , D. compactus y D. hoyezi .

Drepanocrinus marocensis [105]

noviembre esp.

Válido

Vendaval

Cretácico tardío ( Turoniense )

 Francia Marruecos Reino Unido
 
 

Un crinoideo perteneciente al grupo Roveacrinida y a la familia Roveacrinidae.

Drepanocrinus striatulus [105]

noviembre esp.

Válido

Vendaval

Cretácico tardío ( Turoniense )

 Francia Reino Unido
 

Un crinoideo perteneciente al grupo Roveacrinida y a la familia Roveacrinidae.

Echinolampas veracruzensis [114]

noviembre esp.

Válido

Buitrón-Sánchez et al.

Oligoceno

Formación Coatzintla

 México

Un erizo de mar perteneciente a la familia Echinolampadidae .

Echinosphaerites dianae [115]

noviembre esp.

En prensa

Zamora y col.

Ordovícico tardío

 Marruecos

Un blastozoo rombifero . Anunciado en 2019; la versión final del artículo que lo nombra aún no se ha publicado.

Eotiaris teseroensis [116]

noviembre esp.

Válido

Thompson y otros.

Límite Pérmico - Triásico ( Changhsingiano tardío - Induiano temprano )

Formación Werfen

 Italia

Un erizo de mar perteneciente al grupo Cidaroida y a la familia Miocidaridae.

Euglifocrino [105]

Gen. y comb. nov.

Válido

Vendaval

Cretácico ( Albiano y Cenomaniano )

 Marruecos Estados Unidos ( Texas )
 
 

Crinoideo perteneciente al grupo Roveacrinida y a la familia Roveacrinidae. La especie tipo es "Roveacrinus" euglypheus Peck (1943); el género también incluye "R." Pyramidalis Peck (1943).

Euspirocrinus hintsae [117]

noviembre esp.

Válido

Ausich, Wilson y Toom

Silúrico ( Rhuddaniano )

 Estonia

Un crinoideo eucladido .

Falloaster [118]

Gen. y sp. nov.

Válido

Blake, Gahn y Guensburg

Ordovícico ( Floiano )

Formación de la ciudad jardín

 Estados Unidos
( Idaho ) 

Miembro de Asterozoa de ubicación filogenética incierta. El género incluye la nueva especie F. anquiroisitus .

Gamiroastre [119]

Gen. y sp. nov.

Válido

Reid y otros.

Devónico temprano

Formación Voorstehoek

 Sudáfrica

Estrella frágil perteneciente a la familia Protasteridae. La especie tipo es G. tempestatis .

Heloambocolumno [120]

Gen. y sp. nov.

Válido

Donovan y Doyle

Carbonífero ( Bashkirio )

Formación de esquisto Clare

 Irlanda

Un crinoideo . El género incluye la nueva especie Heloambocolumnus (col.) harperi .

Hessicrinus primus [105]

noviembre esp.

Válido

Vendaval

Cretácico tardío ( Turoniense )

 Francia Reino Unido
 

Un crinoideo perteneciente al grupo Roveacrinida y a la familia Roveacrinidae.

Hessicrinus robustus [105]

noviembre esp.

Válido

Vendaval

Cretácico tardío (Coniacan)

 Francia Reino Unido
 

Un crinoideo perteneciente al grupo Roveacrinida y a la familia Roveacrinidae.

Hessicrinus thoracifer [105]

noviembre esp.

Válido

Vendaval

Cretácico tardío ( Turoniense y Coniacano)

 Francia Reino Unido
 

Un crinoideo perteneciente al grupo Roveacrinida y a la familia Roveacrinidae.

Homocystites adidiensis [115]

noviembre esp.

En prensa

Zamora y col.

Ordovícico tardío

 Marruecos

Blastozoo rombifero. Anunciado en 2019; la versión final del artículo que lo nombra aún no se ha publicado.

Hyattechinus anglicus [121]

noviembre esp.

Válido

Thompson y Ewin

Devónico ( Fameniano )

Formación de lodolita Pilton

 Reino Unido

Un erizo de mar .

Jovacrinus clarki [109]

noviembre esp.

Válido

Ausich y Cournoyer

Límite Ordovícico - Silúrico

 Canadá

Un crinoideo .

Kalanacrino [122]

Gen. y sp. nov.

Válido

Ausich, Wilson y Tinn

Silúrico ( Aeroniano )

 Estonia

Crinoideo camerado . El género incluye la nueva especie K. mastikae .

Konieckicrino [113]

Gen. y 2 sp. nov.

Válido

Wright, Cole y Ausich

Ordovícico ( Katian )

Establos de Brechin

 Canadá
( Ontario ) 

Crinoideo perteneciente al grupo Cladida . El género incluye las nuevas especies K. brechinensis y K. josephi .

Lateranicrino [109]

Gen. y sp. nov.

Válido

Ausich y Cournoyer

Límite Ordovícico - Silúrico

 Canadá

Un crinoideo . El género incluye la nueva especie L. saintlaurenti .

Lebenharticrinus [123]

Gen. y 3 sp. nov.

Válido

Žítt y otros.

Cretácico tardío ( Cenomaniano a Santoniano ) [105]

Cuenca cretácica de Bohemia y Sajonia

 República Checa Francia [124] Alemania Marruecos [124] Túnez [124] Reino Unido [124]
 
 
 
 
 

Crinoideo perteneciente al grupo Roveacrinida. El género incluye las nuevas especies L. canaliculatus , L. incisurus y L. ultimus . [105]

Lucernacrinus oculus [105]

noviembre esp.

Válido

Vendaval

Cretácico tardío ( Santoniano )

 Francia Reino Unido
 

Un crinoideo perteneciente al grupo Roveacrinida y a la familia Roveacrinidae.

Magnofossacrinus [125]

Gen. y sp. nov.

Válido

Mirantsev

Carbonífero ( Moscoviense )

 Rusia

Crinoideo perteneciente a la familia Poteriocrinidae. El género incluye la nueva especie M. domodedovoensis .

Monostychia glenelgensis [126]

noviembre esp.

Válido

Sadler, Holmes y Gallagher

mioceno

 Australia

Un dólar de arena .

Monostychia merrimanensis [126]

noviembre esp.

Válido

Sadler, Holmes y Gallagher

mioceno

 Australia

Un dólar de arena .

Multisievertsia [127]

Gen. y sp. nov.

Válido

Müller & Hahn

Devónico temprano

 Alemania

Miembro de Echinozoa perteneciente al grupo Cyclocystoidea. La especie tipo es M. eichelei .

Oepikicrinus [117]

Gen. y sp. nov.

Válido

Ausich, Wilson y Toom

Silúrico ( Aeroniano )

 Estonia

Un crinoideo camerado . El género incluye nuevas especies O. perensae .

Orthogonocrinus cantabrigensis [105]

noviembre esp.

Válido

Vendaval

Cretácico tardío ( Cenomaniano )

 Alemania Marruecos Reino Unido
 
 

Un crinoideo perteneciente al grupo Roveacrinida y a la familia Roveacrinidae.

Paraconocrino [111]

Gen. y comb. y sp. nov.

Válido

Roux, Eléaume y Améziane

Eoceno

 Italia Francia España
 
 

Un crinoideo . La especie tipo es "Eugeniacrinus" pyriformis Münster en Goldfuss (1826); El género también incluye " Conocrinus " cazioti Valette (1924), "Conocrinus" handiaensis Roux (1978) y "Conocrinus" romanensis Roux & Plaziat (1978), así como una nueva especie P. pellati .

Perforocicloides [128]

Gen. y sp. nov.

Válido

Ewin y otros.

Silúrico ( Telychian )

Formación de Júpiter

 Canadá
( Quebec ) 

Miembro de Echinozoa perteneciente al grupo Cyclocystoidea. La especie tipo es P. nathalieae .

Platyhexacrinus santacruzensis [104]

noviembre esp.

Válido

Ausich y Zamora

Devónico ( Emsiano )

Formación Mariposas

 España

Un crinoideo camerado .

Plicodendrocrinus martini [109]

noviembre esp.

Válido

Ausich y Cournoyer

Límite Ordovícico - Silúrico

 Canadá

Un crinoideo .

Plicodendrocrinus petryki [109]

noviembre esp.

Válido

Ausich y Cournoyer

Límite Ordovícico - Silúrico

 Canadá

Un crinoideo .

Pliotoxaster buitronae [129]

noviembre esp.

Válido

Forner

Cretácico temprano ( Aptiano )

Formación Margas del Forcall

 España

Un erizo de mar perteneciente a la familia Toxasteridae .

Pseudoconocrino [111]

Gen. y comb. nov.

Válido

Roux, Eléaume y Améziane

Paleoceno y Eoceno

Península de Crimea Dinamarca Francia
 
 

Un crinoideo . La especie tipo es " Conocrinus " doncieuxi Roux (1978); El género también incluye "Democrinus" maximus Brünnich Nielsen (1915) y "Conocrinus" tauricus Klikushin (1982).

Rhenopyrgus viviani [130]

noviembre esp.

Válido

Ewin y otros.

Silúrico ( Telychian )

Formación de Júpiter

 Canadá
( Quebec ) 

Un miembro de Edrioasteroidea .

Roveacrinus bifidus [105]

noviembre esp.

Válido

Vendaval

Cretácico tardío ( Cenomaniano )

 Reino Unido

Un crinoideo perteneciente al grupo Roveacrinida y a la familia Roveacrinidae.

Roveacrinus falcifer [105]

noviembre esp.

Válido

Vendaval

Cretácico tardío ( Turoniense )

 Francia Reino Unido
 

Un crinoideo perteneciente al grupo Roveacrinida y a la familia Roveacrinidae.

Roveacrinus ferrei [105]

noviembre esp.

Válido

Vendaval

Cretácico tardío ( Turoniense )

 Francia Reino Unido
 

Un crinoideo perteneciente al grupo Roveacrinida y a la familia Roveacrinidae.

Roveacrinus laberinto [105]

noviembre esp.

Válido

Vendaval

Cretácico tardío ( Turoniense )

 Francia Reino Unido
 

Un crinoideo perteneciente al grupo Roveacrinida y a la familia Roveacrinidae.

Rozhnovicrino [117]

Gen. y sp. nov.

Válido

Ausich, Wilson y Toom

Silúrico ( Aeroniano )

 Estonia

Crinoideo eucladiforme . El género incluye la nueva especie R. isakarae .

Sagittacrinus transiens [105]

noviembre esp.

Válido

Vendaval

Cretácico tardío

 Francia Reino Unido
 

Un crinoideo perteneciente al grupo Roveacrinida y a la familia Saccocomidae.

Sagittacrinus tricostatus [105]

noviembre esp.

Válido

Vendaval

Cretácico tardío ( Santoniano )

 Francia Reino Unido
 

Un crinoideo perteneciente al grupo Roveacrinida y a la familia Saccocomidae.

Shoshonura [131]

Gen. y sp. nov.

Válido

Thuy y otros.

Triásico temprano

 Estados Unidos

Estrella frágil . El género incluye la nueva especie S. brayardi .

Simcoecrino [113]

Gen. y sp. nov.

Válido

Wright, Cole y Ausich

Ordovícico ( Katian )

Establos de Brechin

 Canadá
( Ontario ) 

Crinoideo perteneciente al grupo Cladida . El género incluye la nueva especie S. mahalaki .

Sollasina cthulhu [132]

noviembre esp.

Válido

Rahman y otros.

Silúrico ( Wenlock )

Formación Coalbrookdale

 Reino Unido

Miembro de Ophiocistioidea perteneciente a la familia Sollasinidae.

Stellacrinus angelicus [105]

noviembre esp.

Válido

Vendaval

Cretácico tardío ( Santoniano )

 Reino Unido

Un crinoideo perteneciente al grupo Roveacrinida y a la familia Roveacrinidae.

Stellacrinus delicatus [105]

noviembre esp.

Válido

Vendaval

Cretácico tardío ( Santoniano )

 Francia Reino Unido
 

Un crinoideo perteneciente al grupo Roveacrinida y a la familia Roveacrinidae.

Estribo de Stellacrinus [105]

noviembre esp.

Válido

Vendaval

Cretácico tardío ( Coniaciense )

 Francia Reino Unido
 

Un crinoideo perteneciente al grupo Roveacrinida y a la familia Roveacrinidae.

Tartucrino [122]

Gen. y sp. nov.

Válido

Ausich, Wilson y Tinn

Silúrico ( Aeroniano )

 Estonia

Crinoideo dispárido . El género incluye la nueva especie T. kalanaensis .

Thalamocrinus daoustae [109]

noviembre esp.

Válido

Ausich y Cournoyer

Límite Ordovícico - Silúrico

 Canadá

Un crinoideo .

Totiglobus spencensis [133]

noviembre esp.

Válido

Wen y otros.

Cámbrico ( Wuliuan )

Esquisto Spence

 Estados Unidos

Un miembro de Edrioasteroidea perteneciente a la familia Totiglobidae.

Conodontos

Investigación

  • Balter et al. (2019) publican un estudio sobre los hábitos alimentarios de los conodontos, según lo indican los datos de los isótopos estables de calcio. [134]
  • Medici et al. (2019) publican en línea un estudio sobre la variación de la estructura cristalina del elemento conodonte a lo largo de su historia evolutiva. [135]
  • Ginot y Goudemand (2019) publican un estudio sobre la evolución de elementos P 1 similares a plataformas en conodontos, evaluando su posible vínculo con la ecología de los conodontos. [136]
  • Barnes (2019) publicó en línea un estudio sobre el impacto de los cambios ambientales del Paleozoico temprano en la evolución y la paleoecología de los conodontos de la parte canadiense de Laurentia . [137]
  • Mestre & Heredia (2019) publica en línea un estudio sobre la morfología, las ocurrencias y el valor bioestratigráfico de Paroistodus horridus . [138]
  • Yang et al. (2019) publican una revisión de la taxonomía y las relaciones evolutivas de los géneros del Ordovícico tardío Tasmanognathus y Yaoxianognathus . [139]
  • Dhanda et al. (2019) publicaron un estudio sobre la composición y arquitectura del aparato de Erismodus quadridactylus . [140]
  • Corriga y Corradini (2019) publican un estudio sobre la ontogenia de la especie de conodonte de Lochkov, Ancyrodelloides carlsi . [141]
  • Świś (2019) publica un estudio sobre fósiles de miembros del género Alternognathus del Devónico superior de la cantera de Kowala ( Polonia central ), que intenta calibrar el curso de su ontogenia en días y documentar eventos cíclicos de mortalidad. [142]
  • El aparato de Vogelgnathus simplicatus es reconstruido a partir de elementos discretos de una muestra de diversidad limitada de los estratos Carboníferos de Irlanda por Sanz-López, Blanco-Ferrera y Miller (2019). [143]
  • Souquet y Goudemand (2019) informan sobre elementos de conodontos neospatódidos con un cuerpo basal parcialmente preservado (una de las dos partes principales de los elementos de conodontos, además de la corona) del Triásico Inferior de Omán , e interpretan su hallazgo como una indicación de que la ausencia de cuerpos basales en conodontos post- Devónicos se debió únicamente a un sesgo de preservación. [144]
  • Takahashi, Yamakita y Suzuki (2019) describen conjuntos naturales de conodontos que conservan posibles impresiones de "ojos" a partir de arcillas negras pelágicas del Triásico Inferior del Cinturón de Kitakami del Norte ( Japón ). [145]
  • Huang et al. (2019) publican un estudio sobre la composición del aparato de Nicoraella , basado en datos de cúmulos de la Biota Luoping del Triásico Medio ( Yunnan , China ). [146]
  • Huang et al. (2019) reconstruyeron la arquitectura del aparato de Nicoraella kockeli y también evaluaron las interpretaciones funcionales propuestas del aparato de alimentación del conodonto. [147]
  • Chen et al. (2019) publican un estudio sobre conjuntos de conodontes del Triásico Medio de la sección Jenzig de la Formación Jena y la sección Troistedt de la Formación Meissner ( Alemania ), quienes también estudian la morfología de los aparatos de Neogondolella haslachensis y Nicoraella germanica , y revisan y corrigen la especie Neogondolella mombergensis . [148]
  • Guenser et al. (2019) publican un estudio que evalúa la variación morfológica cuantitativa de los elementos de conodontes P 1 dentro y entre siete morfoespecies de conodontes de la sección Pizzo Mondello ( Sicilia , Italia ) y su evolución dentro de 7 millones de años alrededor del límite Carniano / Noriano . [149]
  • Suttner y Kido (2019) publicaron en línea un estudio sobre la tafonomía del tejido basal de elementos conodontes. [150]

Nuevos taxones

NombreNovedadEstadoAutoresEdadLocalidad tipoPaísNotasImágenes

Gnathodus lanei [151]

noviembre esp.

Válido

Lane y otros.

Carbonífero

Formación de aves en primavera

 Estados Unidos

Icriodella iberiensis [152]

noviembre esp.

Válido

Voldman y Toyos

Ordovícico ( Katian )

Formación Casaio

 España

Palmatolepis chaemensis [153]

noviembre esp.

Válido

Salvaje

Devónico tardío

 Tailandia

Palmatolepis thamensis [153]

noviembre esp.

Válido

Salvaje

Devónico tardío

 Tailandia

¿Parapetela? guanyinensis [154]

noviembre esp.

Válido

Jiang y otros.

Triásico Tardío ( Carniano )

 Porcelana

Polygnathus serriformis [155]

noviembre esp.

Válido

Plotitsyn y Gatovsky

Devónico ( Fameniano )

 Rusia

Polygnathus sharyuensis [156]

Nombre. noviembre

Válido

Ovnatanova y otros.

Devónico ( Fameniano )

Formación Sortomael

 Australia Rusia
 

Un nombre de reemplazo Polygnathus mawsonae Ovnatanova et al. (2017).

Polygnathus tenellus surinensis [153]

Subsp. nov

Válido

Salvaje

Devónico tardío

 Tailandia

Polygnathus tsygankoi [155]

noviembre esp.

Válido

Plotitsyn y Gatovsky

Devónico ( Fameniano )

 Rusia

Protofragmodo [157]

Gen. y comb. nov.

Válido

Zhen

Ordovícico ( Darriwiliense y Sandbiano )


Camas Glenwood de Canning Basin

 Australia Estados Unidos
 

Un nuevo género para "Phragmodus" polystrophos Watson, "Phragmodus" spicatus Watson y "Phragmodus" cognitus Stauffer.

Zieglerodina schoenlaubi [158]

noviembre esp.

Válido

Corradini y otros.

Devónico ( Lochkoviano )

 Italia

Peces

Anfibios

Reptiles

Sinápsidos

Sinápsidos no mamíferos

Investigación

Nuevos taxones

NombreNovedadEstadoAutoresEdadLocalidad tipoPaísNotasImágenes

Arisierpetón [203]

Gen. y sp. nov.

Válido

Viaje

Pérmico ( Artinskiano )

 Estados Unidos

Miembro de la familia Caseidae . La especie tipo es A. simplex .

Bohemiclavulo [204]

Gen. y comb. nov.

Válido

Husillo, Voigt & Fischer

Carbonífero ( Gzheliano )

Formación Slaný

 República Checa

Miembro de la familia Edaphosauridae ; un nuevo género para " Naosaurus " mirabilis Fritsch (1895). Anunciado en 2019; la versión final del artículo que lo nombra se publicó en 2020.

Cabarcia [205]

Gen. y sp. nov.

Válido

Spindler, Werneburg y Schneider

Pérmico ( Asseliano o Sakmariano )

Formación Goldlauter

 Alemania

Miembro de Varanopidae perteneciente a la subfamilia Mesenosaurinae . La especie tipo es C. trostheidei .

Concilios [206]

Gen. y sp. nov.

Válido

Olivier y otros.

Lo más probable es que sea del Triásico Temprano

Cuenca de Luang Prabang
(formación de arcilla violeta)

 Laos

Un dicinodonte de grado Dicynodon . El género incluye la nueva especie C. superoculis .

Dendromaia [207]

Gen. y sp. nov.

En prensa

Maddin, Mann y Hebert

Carbonífero

 Canadá
( Nueva Escocia ) 

Miembro de Varanopidae . El género incluye la nueva especie D. unamakiensis . Anunciado en 2019; la versión final del artículo que lo nombra está prevista para 2020.

Dicynodon angielczyki [208]

noviembre esp.

Válido

Cámara

Pérmico tardío

Formación Usili

 Tanzania

Gorynychus sundyrensis [209]

noviembre esp.

Válido

Suchkova y Golubev

Pérmico medio

 Rusia

Un terocéfalo perteneciente a la familia Lycosuchidae .

G. sundyrensis (abajo)

Hipselohaptodus [210]

Gen. y comb. nov.

Válido

Husillo

Pérmico ( Cisuraliano )

 Reino Unido

Un miembro temprano de Sphenacodontia ; un nuevo género para " Haptodus " grandis . Anunciado en 2019; la versión final del artículo que lo nombra se publicó en 2020.

Jiufengia [211]

Gen. y sp. nov.

Válido

Liu y Abdala

Pérmico tardío

Formación Naobaogou

 Porcelana

Un terocéfalo perteneciente a la familia Akidnognathidae . La especie tipo es J. jiai .

Julognato [212]

Gen. y sp. nov.

Válido

Suchkova y Golubev

Pérmico medio

 Rusia

Un terocéfalo perteneciente a la familia Scylacosauridae . El género incluye la nueva especie J. crudelis .

Kembawacela [213]

Gen. y sp. nov.

Válido

Angielczyk, Benoit y Rubidge

Pérmico tardío

Formación de lutitas Madumabisa

 Zambia

Dicinodonte perteneciente a la familia Cistecephalidae . El género incluye la nueva especie K. kitchingi .

Lisowicia [214]

Gen. y sp. nov.

Sulej y Niedźwiedzki

Triásico tardío ( Noriano tardío - Rético temprano )

 Polonia

Un dicinodonte gigantesco que alcanza una masa corporal estimada de 9 toneladas. La especie tipo es L. bojani . Anunciado en 2018; la versión final del artículo que lo nombra se publicó en 2019.

Mesenosaurus efremovi [215]

noviembre esp.

Válido

Maho, Gee y Reisz

Pérmico temprano

 Estados Unidos
( Oklahoma ) 

Un miembro de Varanopidae .

Pseudoterio [216]

Gen. y sp. nov.

Válido

Wallace, Martínez y Rowe

Triásico Tardío ( Carniano )

Formación Ischigualasto

 Argentina

Un cinodonte probainognato estrechamente relacionado con los tritilodóntidos . La especie tipo es P. argentinus .

Remigiomontano [204]

Gen. y sp. nov.

Válido

Husillo, Voigt & Fischer

Transición Carbonífero - Pérmico

Cuenca del Sarre-Nahe

 Alemania

Miembro de la familia Edaphosauridae . El género incluye la nueva especie R. robustus . Anunciado en 2019; la versión final del artículo que lo nombra se publicó en 2020.

Repelinosaurio [206]

Gen. y sp. nov.

Válido

Olivier y otros.

Lo más probable es que sea del Triásico Temprano

Cuenca de Luang Prabang
(formación de arcilla violeta)

 Laos

Un dicinodonte kannemeyeriiforme . El género incluye la nueva especie R. robustus .

Thliptosaurus [217]

Gen. y sp. nov.

Válido

Cámara

Pérmico tardío ( Changhsingiano )

Zona de ensamblaje de Daptocephalus

 Sudáfrica

Un dicinodonte pequeño de la familia Kingoriidae que sobrevivió en etapas tardías . El género incluye la nueva especie T. imperforatus .

Ufudociclops [218]

Gen. y sp. nov.

Válido

Kammerer y otros.

Probablemente Triásico Medio

Formación Burgersdorp

 Sudáfrica

Un dicinodonte estahleckeriido . El género incluye la nueva especie U. mukanelai .

Vetusodon [219]

Gen. y sp. nov.

Válido

Abdala y col.

Pérmico ( Lopingiano )

Supergrupo Karoo ( zona de ensamblaje de Daptocephalus )

 Sudáfrica

Un cinodonte estrechamente relacionado con el grupo Eucynodontia . El género incluye la nueva especie V. elikhulu .

Mamíferos

Otros animales

Nuevos taxones

NombreNovedadEstadoAutoresEdadLocalidad tipoPaísNotasImágenes

Adeloceta [220]

Gen. y sp. nov.

Han, Conway Morris y Shu en Han et al.

Etapa 3 del Cámbrico

Formación Chiungchussu

 Porcelana

Un poliqueto . La especie tipo es A. sinensis .

Alfaítas [221]

Gen. y sp. nov.

Válido

Valent, Fatka y Marek

Cámbrico ( Drumiano )

Formación Buchava

 República Checa

Miembro de Hyolitha . La especie tipo es A. romeo .

Alulagrafto [222]

Gen. y comb. nov.

Válido

Chen y otros.

Ordovícico tardío

 Porcelana

Un graptolito . El género incluye A. ensiformis (Mu & Zhang en Mu et al. , 1963).

Anomalocaris magnabasis [223]

noviembre esp.

Válido

Pates y otros.

Estadio cámbrico 4

Formación Carrara
Formación Pioche

 Estados Unidos

Miembro de Radiodonta. Originalmente descrito como una especie de Anomalocaris , pero transferido al género Houcaris en 2021. [224]

Archiasterella auriculata [225]

noviembre esp.

Válido

Moore en Moore et al.

cambriano

 Estados Unidos
( Nevada ) 

Una esclerita cancillerida .

Archiasterella cometensis [225]

noviembre esp.

Válido

Moore en Moore et al.

cambriano

 Estados Unidos
( Nevada ) 

Una esclerita cancelórida.

Archiasterella uncinata [225]

noviembre esp.

Válido

Moore en Moore et al.

cambriano

 Estados Unidos
( Nevada ) 

Una esclerita cancelórida.

Bauruascaris [226]

Gen. y 2 sp. nov.

Válido

Cardia y col.

Cretácico tardío ( Campaniano / Maastrichtiano )

Formación Adamantina

 Brasil

Nematodo ascaridoide descrito a partir de huevos fósiles preservados en coprolitos crocodiliformes . El género incluye nuevas especies: B. cretacicus y B. adamantinensis .

Bicingulites nanningensis [227]

noviembre esp.

Válido

Wei, Zong y Gong

Devónico temprano

Formación Nagaoling

 Porcelana

Un miembro de Tentaculitida.

Cambrachelous [228]

Gen. y sp. nov.

Válido

Geyer, Valent y Meier

cambriano

Formación Tannenknock

 Alemania

Miembro de Hyolitha . El género incluye la nueva especie C. diploprosopus .

Cambróster [229]

Gen. y sp. nov.

Válido

Moysiuk y Caron

cambriano

Esquisto de Burgess

 Canadá China [230] [231]
 

Radiodonte perteneciente a la familia Hurdiidae . El género incluye la nueva especie C. falcatus .

Cefalónega [232]

Nombre. noviembre

Válido

Ivantsov y otros.

Ediacárico

 Rusia

Miembro de Proarticulata ; un nombre de reemplazo para Onega Fedonkin (1976).

Cancillería australiana [233]

noviembre esp.

Válido

Yun y otros.

Estadio cámbrico 4

Esquisto de la bahía de Emu

 Australia

Cancillería impar [225]

noviembre esp.

Válido

Moore en Moore et al.

cambriano

 Estados Unidos
( Nevada ) 

Una esclerita cancelórida.

Cancillería lilioides [225]

noviembre esp.

Válido

Moore en Moore et al.

cambriano

 Estados Unidos
( Nevada ) 

Una esclerita cancelórida.

Cornulites sokiranae [234]

noviembre esp.

Válido

Vinn , Musabelliu y Zatoń

Devónico tardío

Campo Devónico Central

 Rusia

Un miembro de Cornulitida .

Costatubo [235]

Gen. y sp. nov.

Válido

Selly y otros.

Ediacárico

 Estados Unidos

Un nubínido . El género incluye la nueva especie C. bibendi .

Costulatoteca [236]

Gen. y sp. nov.

Válido

oreja

Devónico temprano

 Australia

Miembro de Hyolitha . El género incluye la nueva especie C. schleigeri .

Cupitheca decollata [237]

noviembre esp.

Válido

Sol y otros.

Cámbrico temprano

Formación Yu'anshan

 Porcelana

Un miembro de Hyolitha .

Dahescolex [238]

Gen. y sp. nov.

Válido

Shao y otros.

Cámbrico ( Fortuniense )

Formación Kuanchuanpu

 Porcelana

Un animal que podría ser un derivado de linaje madre de Scalidophora . El género incluye la nueva especie D. kuanchuanpuensis . Anunciado en 2019; la versión final del artículo que lo nombra se publicó en 2020.

Daihua [239]

Gen. y sp. nov.

Válido

Zhao y otros.

Etapa 3 del Cámbrico

Formación Chiungchussu

 Porcelana

Miembro del grupo total de Ctenophora . La especie tipo es D. sanqiong .

Dailyatia decobruta [240]

noviembre esp.

Válido

Betts en Betts et al.

Cámbrico temprano

 Australia

Un tommotido perteneciente a la familia Kennardiidae.

Equinoclepto [241]

Gen. y sp. nov.

Válido

Muir y otros.

Ordovícico ( Tremadociano )

 Reino Unido

Tubos aglutinados, probablemente producidos por un poliqueto . El género incluye la nueva especie E. anileis .

Gothograptus auriculatus [242]

noviembre esp.

Válido

Kozłowska y otros.

siluriano

 Alemania Lituania Polonia Suecia
 
 
 

Un graptolito .

Gothograptus diminutus [242]

noviembre esp.

Válido

Kozłowska y otros.

siluriano

 Polonia

Un graptolito .

Gothograptus domeyki [242]

noviembre esp.

Válido

Kozłowska y otros.

siluriano

 Lituania

Un graptolito .

Gothograftus velo [242]

noviembre esp.

Válido

Kozłowska y otros.

siluriano

 Polonia

Un graptolito .

Graniteca? clan [228]

noviembre esp.

Válido

Geyer, Valent y Meier

cambriano

Formación Tannenknock

 Alemania

Un miembro de Hyolitha .

Harrisgraptus [243]

Gen. y comb. nov.

Válido

Vandenberg

Ordovícico ( Floiano )

 Australia

Graptolito perteneciente al grupo Dichograptina y a la familia Pterograptidae . La especie tipo es " Didymograptus " eocaduceus Harris ( 1933).

Hexitheca washingtonensis [244]

noviembre esp.

Válido

Malinky y Geyer

Cámbrico temprano ( Dyerano )

 Estados Unidos

Un miembro de Hyolitha .

Heydenius simulphilus [245]

noviembre esp.

Válido

Poinar y Currie

Eoceno

Ámbar báltico

Europa ( región del mar Báltico )

Nematodo perteneciente a la familia Mermithidae . Anunciado en 2019; la versión final del nombre del artículo se publicó en 2020.

Hipólito [220]

Gen. y sp. nov.

Han, Conway Morris y Shu en Han et al.

Etapa 3 del Cámbrico

Formación Chiungchussu

 Porcelana

Un poliqueto . La especie tipo es I. avitus .

Lonchidium cylicus [227]

noviembre esp.

Válido

Wei, Zong y Gong

Devónico temprano

Formación Nagaoling

 Porcelana

Un miembro de Tentaculitida.

Nectocotis [246]

Gen. y sp. nov.

Válido

Herrero

Ordovícico ( Katian )

Formación del golfo de Whetstone

 Estados Unidos
( Nueva York ) 

Un pariente de Nectocaris ; un animal de ubicación filogenética incierta, posiblemente un cefalópodo primitivo . La especie tipo es N. rusmithi .

Normalograptus baridaensis [247]

noviembre esp.

Válido

Štorch, Roqué Bernal & Gutiérrez-Marco

Ordovícico ( Hirnantian )

 España

Un graptolito .

Normalograptus ednae [247]

noviembre esp.

Válido

Štorch, Roqué Bernal & Gutiérrez-Marco

Silúrico ( Rhuddaniano )

 España

Un graptolito .

Odesitas aurisitas [227]

noviembre esp.

Válido

Wei, Zong y Gong

Devónico temprano

Formación Nagaoling

 Porcelana

Un miembro de Tentaculitida.

Odessites nahongensis [227]

noviembre esp.

Válido

Wei, Zong y Gong

Devónico temprano

Formación Nagaoling

 Porcelana

Un miembro de Tentaculitida.

Paratriplicatella [248]

Gen. y sp. nov.

Válido

Pan y otros.

Cámbrico temprano

 Porcelana

Miembro de Hyolitha . El género incluye la nueva especie P. shangwanensis .

Protomicrocornus [248]

Gen. y sp. nov.

Válido

Pan y otros.

Cámbrico temprano

 Porcelana

Miembro de Hyolitha . El género incluye la nueva especie P. triplicensis .

Saarina hagadorni [235]

noviembre esp.

Válido

Selly y otros.

Ediacárico

 Estados Unidos

Shenzianyuloma [249]

Gen. y sp. nov.

Válido

McMenamin

cambriano

Esquistos de Maotianshan

 Porcelana

Miembro de Vetulicolia . La especie tipo es S. yunnanense .

Sialomorfos [250]

Gen. y sp. nov.

Válido

Poinar y Nelson

Eoceno o Mioceno

Ámbar dominicano

 República Dominicana

Pequeño invertebrado de ubicación filogenética incierta, que comparte caracteres con los tardígrados y los ácaros , pero no pertenece a ninguno de los dos grupos. La especie tipo es S. dominicana .

Tentaculites brevitenui [227]

noviembre esp.

Válido

Wei, Zong y Gong

Devónico temprano

Formación Nagaoling

 Porcelana

Un miembro de Tentaculitida.

Triplicación de la xinjia [248]

noviembre esp.

Válido

Pan y otros.

Cámbrico temprano

 Porcelana

Un miembro de Hyolitha .

Ursulinacaris [251]

Gen. y sp. nov.

Patés, Daley y Butterfield

cambriano

Formación Monte Cap
Formación Carrara ?

 Canadá Estados Unidos ?
 

Radiodonte perteneciente a la familia Hurdiidae . La especie tipo es U. grallae .

Volynites nagaolingensis [227]

noviembre esp.

Válido

Wei, Zong y Gong

Devónico temprano

Formación Nagaoling

 Porcelana

Un miembro de Tentaculitida.

Yilingia [252]

Gen. y sp. nov.

Válido

Chen y otros.

Ediacárico tardío

 Porcelana

Un bilateriano temprano , posiblemente relacionado con los panartrópodos o los anélidos . El género incluye la nueva especie Y. spiciformis .

Investigación

  • Ivantsov, Zakrevskaya y Nagovitsyn (2019) publican un estudio sobre los moldes de animales pertenecientes al grupo Proarticulata del área sudoriental del Mar Blanco ( Rusia ) y sobre sus implicaciones para el conocimiento de la morfología de los tegumentos de los miembros de Proarticulata. [253]
  • Gibson et al. (2019) publican un estudio sobre las acumulaciones de Ernietta en la subcuenca de Witputs ( Namibia ) y sus implicaciones para el conocimiento de la ecología de estos organismos. [254]
  • Cai et al. (2019) describen un conjunto diverso de fósiles tubulares, dominado por organismos típicos del Ediacárico, como Cloudina y Sinotubulites , pero que también conserva fósiles que muestran similitudes con fósiles con conchas del Cámbrico temprano , de la Formación Dengying del Ediacárico ( China ) . [255]
  • Letsch et al. (2019) informan sobre fósiles discoidales de tipo Ediacara del Ediacárico tardío y microfósiles del Ediacárico tardío al Cámbrico temprano de los miembros Tabia y Tifnout de la Formación Adoudou ( Marruecos ), que constituyen la evidencia directa más antigua conocida de presumiblemente vida animal del noroeste de África. [256]
  • Min et al. (2019) publicaron un estudio que describe los diferentes tipos de reproducción asexual de Cloudina y Multiconotubus . [257]
  • Dunn et al. (2019) publican un estudio sobre la anatomía de Charnia masoni . [258]
  • Evans, Gehling y Droser (2019) publicaron un estudio que evalúa si Dickinsonia era capaz de moverse. [259]
  • Evans et al. (2019) publicaron un estudio que compara las respuestas biomecánicas de los tejidos de Dickinsonia a diversas fuerzas con las típicas de los organismos modernos. [260]
  • Dunn, Liu y Gehling (2019) publicaron un estudio sobre la anatomía, el crecimiento y las relaciones filogenéticas de Arborea arborea . [261]
  • Xiao et al. (2019) describen un nuevo fósil traza de la Formación Dengying ediacárica (China), interpretado como producido por un animal bilateral que exploró un oasis de oxígeno en tapetes microbianos , y nombran un nuevo icnotaxón Yichnus levis . [262]
  • MacGabhann et al. ( 2019) publican un estudio sobre moldes y vaciados fósiles del Ordovícico de Marruecos y del Devónico de Nueva York , así como sobre moldes y vaciados fósiles del Ediacárico de Australia del Sur , la región del Mar Blanco de Rusia , Namibia y Terranova , y evalúan con qué fidelidad los fósiles representan a los organismos originales, y si los primeros animales que evolucionaron en la Tierra podrían haberse fosilizado de forma similar a los eldónidos de Tafilalt Lagerstätte de Marruecos. [263]
  • Pruss et al. (2019) informan sobre arqueociatos fosfatados excepcionalmente conservados y pequeños fósiles de conchas de la Formación Salaagol del Cámbrico Inferior del suroeste de Mongolia . [264]
  • Cordie et al. (2019) publican un estudio sobre el momento del desarrollo de la biodiversidad de los arrecifes , basado en datos de arrecifes microbianos y arqueociatos de la Formación Salaagol en Mongolia y otros arrecifes del Paleozoico temprano. [265]
  • Cordie y Dornbos (2019) publicaron un estudio sobre la diversidad morfológica de los arqueociatos. [266]
  • Pratt y Kimmig (2019) presentan evidencia de excavaciones extensas en arcilla laminada del Lagerstätte del río Ravens Throat del Cámbrico ( Drumiano ) en la Formación Rockslide ( Canadá ). [267]
  • Parry et al. (2019) publican una descripción del aparato mandibular de Plumulites bengtsoni de la Formación Fezouata de Marruecos , evaluando sus implicaciones para el conocimiento de las relaciones filogenéticas de los machaeridios . [268]
  • Parry y Caron (2019) publican una descripción de las características anatómicas internas de Canadia spinosa identificadas como restos del sistema nervioso . [269]
  • Georgieva et al. (2019 ) publican un estudio sobre la composición química, la morfología y la filogenia de los tubos de anélidos fósiles ( Cenozoicos , Mesozoicos y Paleozoicos ) y de los tubos que antes se creía que habían sido hechos por anélidos, recuperados de ambientes de respiraderos hidrotermales y filtraciones frías . [270]
  • A massive deposit composed of fossil serpulid worm tubes dating to the late Pleistocene is reported from the Santa Monica Basin off the coast of southern California by Georgieva et al. (2019).[271]
  • A study on the microstructure of hyolith conchs and opercula from the lower Cambrian Xinji Formation of North China, and on its implications for inferring the phylogenetic relationships of Hyolitha, is published by Li et al. (2019).[272]
  • Description of soft parts associated with the feeding apparatus of the hyolith Triplicatella opimus from the Chengjiang biota of South China, and a study on the implications of this finding for the knowledge of the phylogenetic affinities of hyoliths, is published online by Liu et al. (2019).[273]
  • A study on changes of conch size in tentaculitoids from the Silurian and Devonian strata is published by Wei (2019).[274]
  • A study on the anatomy of Amiskwia sagittiformis is published by Vinther & Parry (2019), who interpret two reflective patches present in fossils of this species, previously interpreted as paired cerebral ganglia, as a pair of pharyngeal jaws similar to those of gnathiferans.[275]
  • A study on the anatomy and phylogenetic affinities of Amiskwia sagittiformis is published by Caron & Cheung (2019).[276]
  • The oldest record of acanthocephalan parasite eggs described so far is reported from probable crocodyliform coprolites from the Upper Cretaceous Adamantina Formation (Brazil) by Cardia et al. (2019).[277]
  • Exceptionally preserved trace and body fossils are described from the Cambrian File Haidar Formation (Sweden) by Kesidis et al. (2019), who interpret these fossils as made by priapulid-like scalidophorans.[278]
  • Description of exuviae of microscopic scalidophoran worms from the lowermost Cambrian Kuanchuanpu Formation (China) is published by Wang et al. (2019), who interpret this finding as the oldest record of moulting in ecdysozoans reported so far.[279]
  • A reassessment of radiodontan fossils known from the Cambrian Kinzers Formation (Pennsylvania, United States) is published by Pates & Daley (2019), who argue that at least four radiodontan taxa are known from this formation, and confirm that Anomalocaris pennsylvanica is a distinct species from A. canadensis.[280]
  • A study on the moulting behaviour of the chengjiangocaridid fuxianhuiid Alacaris mirabilis is published by Yang et al. (2019).[281]
  • A study on the anatomy and phylogenetic relationships of a stem-arthropod Guangweicaris spinatus is published by Wu & Liu (2019).[282]
  • A fossil interpreted as a partial mold of a specimen of Paropsonema cryptophya is described from the Middle-Upper Devonian of New York by Hagadorn & Allmon (2019), representing the most recent occurrence of the paropsonemids reported so far.[283]
  • A study evaluating the utility of eye melanosomes for determination of the phylogenetic affinities of Tullimonstrum is published by Rogers et al. (2019).[284]

Foraminifera

Research

New taxa

NameNoveltyStatusAuthorsAgeType localityCountryNotesImages

Acervoschwagerina gongendaniensis[287]

Sp. nov

Valid

Kobayashi in Kobayashi & Furutani

Permian (late Cisuralian)

 Japan

A member of Fusulinida.

Ammodiscus jordanensis[288]

Sp. nov

Valid

Gennari and Rettori in Powell et al.

Early and Middle Triassic

Ma'in Formation

 China
 Hungary
 Jordan
 Poland
 Romania

A species of Ammodiscus.

Bispiraloconulus[289]

Gen. et sp. nov

Valid

Schlagintweit, Bucur & Sudar

Early Cretaceous (Berriasian)

 Serbia

Genus includes new species B. serbiacus.

Canalispina[290]

Gen. et sp. nov

Valid

Robles-Salcedo et al.

Late Cretaceous (Maastrichtian)

 Italy

A member of the family Siderolitidae. Genus includes new species C. iapygia.

Chusenella tsochenensis[291]

Sp. nov

Valid

Zhang et al.

Middle Permian

Xiala Formation

 China

A member of the family Schwagerinidae.

Cuniculinella omiensis[287]

Sp. nov

Valid

Kobayashi in Kobayashi & Furutani

Permian (late Cisuralian)

 Japan

A member of Fusulinida.

Cyclopsinella roselli[292]

Sp. nov

Valid

Villalonga et al.

Late Cretaceous (Campanian)

Terradets Limestone

 Spain

Globigaetania[293]

Gen. et sp. nov

Valid

Gennari & Rettori

Permian (Wordian to Capitanian)

Gnishik Formation

 Iran
 Japan

A member of the family Globivalvulinidae. Genus includes new species G. angulata.

Pachycolumella[294]

Gen. et 2 sp. nov

Valid

Septfontaine, Schlagintweit & Rashidi

Late Cretaceous (Maastrichtian) and Paleocene (Danian)

Tarbur Formation

 India
 Iran
 Oman
 Pakistan
 Turkey

The type species is P. elongata; genus also includes P. acuta.

Pseudochablaisia[295]

Gen. et sp. nov

Valid

Schlagintweit, Septfontaine & Rashidi

Late Cretaceous (Maastrichtian)

Tarbur Formation

 Iran

A member of the family Pfenderinidae. Genus includes new species P. subglobosa.

Serrakielina[296]

Gen. et sp. nov

Valid

Schlagintweit & Rashidi

Paleocene

 Iran

Genus includes new species S. chahtorshiana.

Simobaculites saundersi[297]

Sp. nov

Valid

Wilson & Kaminski in Wilson et al.

Cenozoic

Nariva Formation

 Trinidad and Tobago

Socotraella? yazdiana[296]

Sp. nov

Valid

Schlagintweit & Rashidi

Paleocene

 Iran

Tambareauella[298]

Gen. et comb. et sp. nov

Valid

Boukhary & El Naby

Eocene

 Egypt
 France

A member of the family Nummulitidae. The type species is "Operculina (Nummulitoides)" azilensis Tambareau (1966); genus also includes new species T. russeiesensis.

Other organisms

New taxa

NameNoveltyStatusAuthorsAgeType localityCountryNotesImages

Aguirrea[299]

Gen. et sp. nov

Valid

Teichert, Woelkerling & Munnecke

Silurian (Wenlock)

Högklint Formation

 Sweden

A coralline alga. Genus includes new species A. fluegelii.

Amsassia yushanensis[300]

Sp. nov

Valid

Lee et al.

Late Ordovician

Xiazhen Formation

 China

A coral-like organism.

Anechosoma[301]

Gen. et sp. nov

Valid

Krings & Kerp

Early Devonian

 United Kingdom

A unicellular organism with possible affinities to the Glaucophyta or Chlorophyta. Genus includes new species A. oblongum.

Appendisphaera clustera[302]

Sp. nov

Valid

Liu & Moczydłowska

Ediacaran

Doushantuo Formation

 China

A microfossil.

Appendisphaera lemniscata[302]

Sp. nov

Valid

Liu & Moczydłowska

Ediacaran

Doushantuo Formation

 China

A microfossil.

Asterocapsoides fluctuensis[302]

Sp. nov

Valid

Liu & Moczydłowska

Ediacaran

Doushantuo Formation

 China

A microfossil.

Bacatisphaera sparga[302]

Sp. nov

Valid

Liu & Moczydłowska

Ediacaran

Doushantuo Formation

 China

A microfossil.

Baculiphyca brevistipitata[303]

Sp. nov

Valid

Ye et al.

Ediacaran

 China

A macroalga.

Briareus robustus[302]

Sp. nov

Valid

Liu & Moczydłowska

Ediacaran

Doushantuo Formation

 China

A microfossil.

Briareus vasformis[302]

Sp. nov

Valid

Liu & Moczydłowska

Ediacaran

Doushantuo Formation

 China

A microfossil.

Cambrowania[304]

Gen. et sp. nov

Disputed

Tang & Xiao in Tang et al.

Early Cambrian

Hetang Formation

 China

An organism of uncertain phylogenetic placement. Originally classified as an animal of uncertain phylogenetic placement, possibly a sponge or a bivalved arthropod; Slater & Budd (2019) contested its animal affinity, and considered its fossil material to be more likely collapsed hollow organic spheroidal acritarchs belonging to the genus Leiosphaeridia.[305][306] Genus includes new species C. ovata.

Casterlorum[8]

Gen. et sp. nov

Valid

Retallack

Ordovician (Darriwilian)

Lenoir Formation

 United States
( Tennessee)

An organism of uncertain affinities, originally described as a hornwort. Genus includes new species C. crispum.

Cavaspina conica[302]

Sp. nov

Valid

Liu & Moczydłowska

Ediacaran

Doushantuo Formation

 China

A microfossil.

Chiastozygus fahudensis[307]

Sp. nov

Valid

Al Rawahi & Dunkley Jones

Late Cretaceous (late Coniacian to late Campanian)

Fiqa Formation

 Oman

A heterococcolith.

Circumpodium[308]

Gen. et sp. nov

Valid

Wisshak & Hüne

Middle Jurassic (Callovian)

Marnes de Dives Formation

 France

A microfossil of uncertain phylogenetic placement. Genus includes new species C. enigmaticum.

Cyathinema[309]

Gen. et sp. nov

Valid

Agić et al.

Early Ediacaran

Nyborg Formation

 Norway

A eukaryote of uncertain phylogenetic placement. The type species is C. digermulense.

Cymatiosphaeroides forabilatus[302]

Sp. nov

Valid

Liu & Moczydłowska

Ediacaran

Doushantuo Formation

 China

A microfossil.

Daedalosphaera[6]

Gen. et sp. nov

Valid

Loron et al.

MesoproterozoicNeoproterozoic transition

Grassy Bay Formation

 Canada

A spheroidal acritarch with inner wall sculpture. Genus includes new species D. digitisigna.

Dicrospinasphaera improcera[302]

Sp. nov

Valid

Liu & Moczydłowska

Ediacaran

Doushantuo Formation

 China

A microfossil.

Distosphaera? corniculata[302]

Sp. nov

Valid

Liu & Moczydłowska

Ediacaran

Doushantuo Formation

 China

A microfossil.

Dollyphyton[8]

Gen. et sp. nov

Valid

Retallack

Ordovician (Darriwilian)

Lenoir Formation

 United States
( Tennessee)

An organism of uncertain affinities, originally described as a moss belonging to the group Sphagnales. Genus includes new species D. boucotii.

Doushantuophyton? laticladus[303]

Sp. nov

Valid

Ye et al.

Ediacaran

 China

A macroalga.

Edwardsiphyton[8]

Gen. et sp. nov

Valid

Retallack

Ordovician (Darriwilian)

Lenoir Formation

 United States
( Tennessee)

An organism of uncertain affinities, originally described as a moss belonging to the group Pottiales. Genus includes new species E. ovatum.

Enteromorphites magnus[303]

Sp. nov

Valid

Ye et al.

Ediacaran

 China

A macroalga.

Eotylotopalla quadrata[302]

Sp. nov

Valid

Liu & Moczydłowska

Ediacaran

Doushantuo Formation

 China

A microfossil.

Ericiasphaera fibrilla[302]

Sp. nov

Valid

Liu & Moczydłowska

Ediacaran

Doushantuo Formation

 China

A microfossil.

Estrella[302]

Gen. et 2 sp. nov

Valid

Liu & Moczydłowska

Ediacaran

Doushantuo Formation

 China

A microfossil. Genus includes new species E. greyae and E. recta.

Germinosphaera alveolata[310]

Sp. nov

Valid

Miao et al.

Late Paleoproterozoic

Chuanlinggou Formation

 China

An organic-walled microfossil interpreted as a unicellular eukaryote.

Hercochitina violana[311]

Sp. nov

Valid

Nõlvak & Liang in Liang et al.

Ordovician (Katian)

Viola Springs Formation

 United States

A chitinozoan.

Herisphaera[6]

Gen. et 2 sp. nov

Valid

Loron et al.

MesoproterozoicNeoproterozoic transition

Grassy Bay Formation
Nelson Head Formation

 Canada

A spiny acritarch with regularly distributed processes. Genus includes new species H. arbovela and H. triangula.

Janegraya[8]

Gen. et sp. nov

Valid

Retallack

Ordovician (Darriwilian)

Lenoir Formation

 United States
( Tennessee)

An organism of uncertain affinities, originally described as a liverwort belonging to the group Sphaerocarpales. Genus includes new species J. sibylla.

Knollisphaeridium coniformum[302]

Sp. nov

Valid

Liu & Moczydłowska

Ediacaran

Doushantuo Formation

 China

A microfossil.

Knollisphaeridium heliacum[302]

Sp. nov

Valid

Liu & Moczydłowska

Ediacaran

Doushantuo Formation

 China

A microfossil.

Konglingiphyton? laterale[303]

Sp. nov

Valid

Ye et al.

Ediacaran

 China

A macroalga.

Laminasphaera[302]

Gen. et sp. nov

Valid

Liu & Moczydłowska

Ediacaran

Doushantuo Formation

 China

A microfossil. Genus includes new species L. capillata.

Laufeldochitina toilaensis[312]

Sp. nov

Valid

Nõlvak, Liang & Hints

Ordovician (Dapingian)

 Estonia

A chitinozoan.

Maxiphyton[303]

Gen. et sp. nov

Valid

Ye et al.

Ediacaran

 China

A macroalga. Genus includes new species M. stipitatum.

Membranosphaera[302]

Gen. et sp. nov

Junior homonym

Liu & Moczydłowska

Ediacaran

Doushantuo Formation

 China

A microfossil. Genus includes new species M. formosa. The generic name is preoccupied by Membranosphaera Samoilovitch in Samoilovitch and Mtchedlishvili (1961); Shang & Liu (2024) coined a replacement name Membranospinosphaera.[313]

Mengeosphaera flammelata[302]

Sp. nov

Valid

Liu & Moczydłowska

Ediacaran

Doushantuo Formation

 China

A microfossil.

Mengeosphaera lunula[302]

Sp. nov

Valid

Liu & Moczydłowska

Ediacaran

Doushantuo Formation

 China

A microfossil.

Mengeosphaera membranifera[314]

Sp. nov

Valid

Shang, Liu & Moczydłowska

Ediacaran

Doushantuo Formation

 China

An acritarch.

Moorodinium crispa[315]

Sp. nov

Valid

Wainman et al.

Late Jurassic (late Kimmeridgian–early Tithonian)

Surat Basin

 Australia

A dinoflagellate.

Nimbosphaera[316]

Gen. et sp. nov

Valid

Harper & Krings

Early Devonian

Windyfield chert

 United Kingdom

A microfossil resembling the sheathed zoosporangia of extant chytrids. Genus includes new species N. rothwellii.

Nunatsiaquus[6]

Gen. et sp. nov

Valid

Loron et al.

MesoproterozoicNeoproterozoic transition

Grassy Bay Formation

 Canada

A spheroidal acritarch with inner wall sculpture. Genus includes new species N. cryptotorus.

Obelix[317]

Gen. et comb. nov

Valid

Morais et al.

Neoproterozoic

Callison Lake Formation
Chuar Group
(Kwagunt Formation)

 Canada United States

A vase-shaped microfossil representing tests of protists. The type species is "Cycliocyrillium" rootsi Cohen, Irvine & Strauss (2017); Morais et al. (2019) corrected the suffix for the specific epithet to rootsii.

Palaeoleptochlamys[318]

Gen. et sp. nov

Valid

Strullu-Derrien et al.

Early Devonian

Rhynie chert

 United Kingdom

A member of Amoebozoa belonging to the group Arcellinida. Genus includes new species P. hassii.

Palaeolyngbya kerpii[319]

Sp. nov

Valid

Krings

Early Devonian

Rhynie chert

 United Kingdom

A cyanobacterium with affinities to Oscillatoriaceae.

Paleoplastes[320]

Gen. et sp. nov

In press

Poinar & Vega

Late Cretaceous (Cenomanian)

Burmese amber

 Myanmar

A possible dictyostelid. Genus includes new species P. burmanica. Announced in 2019; the final version of the article naming it was published in 2021.

Perexiflasca ventricosa[321]

Sp. nov

Valid

Krings & Harper

Early Devonian

Windyfield chert

 United Kingdom

A small, chytrid-like organism.

Rhyniotaxillus[322]

Gen. et sp. nov

Valid

Krings & Sergeev

Early Devonian

Rhynie chert

 United Kingdom

A minute coccoid cyanobacterium. Genus includes new species R. devonicus.

Rhyniovexator[301]

Gen. et sp. nov

Valid

Krings & Kerp

Early Devonian

 United Kingdom

Possibly a chytrid or a member of Aphelida. Genus includes new species R. penetrans.

Sinocylindra linearis[303]

Sp. nov

Valid

Ye et al.

Ediacaran

 China

An organism of uncertain phylogenetic placement, possibly an alga or an exceptionally large prokaryote.

Skuadinium fusum[315]

Sp. nov

Valid

Wainman et al.

Late Jurassic (late Kimmeridgian–early Tithonian)

Surat Basin

 Australia

A dinoflagellate.

Sporosphaera[323]

Gen. et sp. nov

Valid

Landon et al.

Ediacaran

 China

A eukaryote reminiscent of acritarchs. Genus includes new species S. guizhouensis.

Staurolithites ormae[307]

Sp. nov

Valid

Al Rawahi & Dunkley Jones

Late Cretaceous (late Santonian to late Campanian)

Fiqa Formation

 Oman

A heterococcolith.

Tanarium capitatum[302]

Sp. nov

Valid

Liu & Moczydłowska

Ediacaran

Doushantuo Formation

 China

A microfossil.

Tanarium uniformum[302]

Sp. nov

Valid

Liu & Moczydłowska

Ediacaran

Doushantuo Formation

 China

A microfossil.

Tetraphycus laminiformis[310]

Sp. nov

Valid

Miao et al.

Late Paleoproterozoic

Chuanlinggou Formation

 China

An organic-walled microfossil, a colonial organism of uncertain phylogenetic placement, possibly a cyanobacteria.

Variomargosphaeridium varietatum[302]

Sp. nov

Valid

Liu & Moczydłowska

Ediacaran

Doushantuo Formation

 China

A microfossil.

Verrucosphaera[302]

Gen. et sp. nov

Junior homonym

Liu & Moczydłowska

Ediacaran

Doushantuo Formation

 China

A microfossil. Genus includes new species V. minima. The generic name is preoccupied by Verrucosphaera Górka (1970); Shang & Liu (2024) coined a replacement name Spinomargosphaera.[313]

Research

  • Putative traces of life older than 3.95 Ga, reported from northern Labrador (Canada) by Tashiro et al. (2017)[324] are reevaluated by Whitehouse et al. (2019).[325]
  • Description of cellularly preserved microfossils from ~3.4 Ga-old deposits of the Kromberg Formation (South Africa), providing information on reproduction patterns of these organisms, is published by Kaźmierczak & Kremer (2019).[326]
  • El Albani et al. (2019) describe 2.1 billion-year-old fossils belonging to the Francevillian biota of Gabon, including pyritized string-shaped structures interpreted as produced by a multicellular or syncytial organism able to migrate laterally and vertically to reach food resources.[327]
  • A study on ca. 1.9 Ga hairpin-shaped trace fossils and discoid fossils from the Stirling Range Formation (Western Australia) is published by Retallack & Mao (2019), who interpret these fossils as evidence of early life on land.[328]
  • A study on organic-walled microfossils from the Cailleach Head Formation (Torridon Group, Scotland) is published by Wacey et al. (2019), who report exceptional preservation of sub-cellular detail in selected cells.[329]
  • Phosphatized three-dimensional fossil of a putative calcimicrobe Epiphyton are reported from the Neoproterozoic Dengying Formation (China) by Min et al. (2019).[330]
  • A study on the affinities of tubular microfossils from the Ediacaran Doushantuo Formation (China), i.e. Crassitubus, Quadratitubus, Ramitubus and Sinocyclocyclicus, is published by Sun et al. (2019), who reject the interpretation of these taxa as early animals.[331]
  • Lehn, Horodyski & Paim (2019) report the first known occurrence of Ediacaran organic-walled microfossils preserved in fine-grained siliciclastic strata of the Camaquã Basin (southernmost Brazil).[332]
  • A study on the structure, developmental biology and affinities of Caveasphaera costata from the Ediacaran Doushantuo Formation (China) is published by Yin et al. (2019).[333]
  • A study on possible cells and their appendages in fossils of Epiphyton from the Wuliuan of the North China Platform, and on their implications for the classification of this taxon, is published by Zhang et al. (2019).[334]
  • A study on the morphology and colony organization of Rhyniococcus uniformis (a Devonian organism resembling extant cyanobacteria in the genus Merismopedia), based on data from new specimens, is published by Krings & Harper (2019).[335]
  • A new method of assessing the morphology of fossil radiolarian specimens is presented by Kachovich, Sheng & Aitchison (2019), who apply their method to six specimens from the Cambrian Inca Formation (Australia) and Ordovician Piccadilly Formation (Canada) and evaluate the implications of their method for the studies of radiolarian evolution.[336]

Trace fossils

History of life in general

Research related to paleontology that concerns multiple groups of the organisms listed above.

  • Experiments indicating that abiotic chemical gardening can mimic structures interpreted as the oldest known fossil microorganisms in both morphology and composition are conducted by McMahon (2019).[337]
  • A study on biomarkers recovered from cap dolomites of the Araras Group (Brazil), interpreted as evidence of the transition from a bacterial to eukaryotic dominated ecosystem after the Marinoan deglaciation, likely caused by massive bacterivorous grazing by ciliates, is published by van Maldegem et al. (2019).[338]
  • Biomarkers thought to be diagnostic for demosponges and cited as evidence of rise of animals to ecological importance prior to the Cambrian radiation are reported to be also synthesized by rhizarians by Nettersheim et al. (2019), who place the oldest unambiguous evidence for animals closer to the Cambrian Explosion.[339][340][341]
  • A study on crucial conditions affecting the evolution of a proto-metabolism in early life is published by Goldford et al. (2019).[342]
  • A study on the age of the Ediacaran fossils from the Podolya Basin (southwestern Ukraine) is published by Soldatenko et al. (2019).[343]
  • A study on occurrences of body and trace fossils in Ediacaran and lower Cambrian (Fortunian) rocks around the world is published by Muscente et al. (2019), who report evidence indicative of existence of a global, cosmopolitan assemblage unique to terminal Ediacaran strata, living between two episodes of biotic turnover which might be the earliest mass extinctions of complex life.[344]
  • A study on the diversification of animals and their behaviour in the Ediacaran–Cambrian interval, as indicated by fossil and environmental proxy records, is published by Wood et al. (2019), who interpret the fossil record as indicating that the rise of early animals was more likely a series of successive, transitional radiation events which extended from the Ediacaran to the early Paleozoic, rather than competitive or biotic replacement of the latest Ediacaran biotas by markedly distinct Cambrian ones.[345]
  • A study comparing the variability of Ediacaran faunal assemblages to that of more recent fossil and modern benthic assemblages is published by Finnegan, Gehling & Droser (2019).[346]
  • A study on the intensity of animal bioturbation and ecosystem engineering in trace fossil assemblages throughout the latest Ediacaran Nama Group (Namibia), evaluating the implications of this data for the knowledge of the causes of the disappearance of the Ediacaran biota, is published by Cribb et al. (2019).[347]
  • A study on mechanisms of skeletal biomineralization in early animals (focusing on Cloudina and Cambrian hyoliths and halkieriids) is published by Gilbert et al. (2019).[348]
  • A study on the relationship between atmospheric oxygen oscillations, the extent of shallow-ocean oxygenation and the animal biodiversity in the Cambrian period is published by He et al. (2019).[349]
  • A study on the course of the transition from microbial-dominated reef environments to animal-based reefs in the early Cambrian, as indicated by data from strata in the western Basin and Range of California and Nevada, is published by Cordie, Dornbos & Marenco (2019).[350]
  • An assemblage of early Cambrian small carbonaceous fossils and acritarchs, including possible oldest known annelid remains, is described from the siltstones of the Lappajärvi impact structure (Finland) by Slater & Willman (2019).[351]
  • A study aiming to explain the occurrence of the variety of trace fossils associated with Tuzoia carapaces from the Cambrian Burgess Shale (British Columbia, Canada) is published by Mángano, Hawkes & Caron (2019).[352]
  • Cambrian Lagerstätte from the Qingjiang biota (Shuijingtou Formation; Hubei, China), preserving fossils of diverse, ~518 million years old biota, is reported by Fu et al. (2019).[353][354]
  • A study aiming to infer whether a marked drop in known diversity of marine life during the period between the Cambrian explosion and the Great Ordovician Biodiversification Event (the Furongian Gap) is apparent, due to sampling failure or lack of rock, or real, is published by Harper et al. (2019).[355]
  • A study on the marine biodiversity changes throughout the first 120 million years of the Phanerozoic is published by Rasmussen et al. (2019).[356]
  • A study aiming to determine factors influencing early Palaeozoic marine biodiversity is published by Penny & Kröger (2019).[357]
  • A study on rates of origination and extinction at the genus level throughout early Paleozoic is published by Kröger, Franeck & Rasmussen (2019), who also present estimates of longevity, taxon age and taxon life expectancy of early Paleozoic marine genera.[358]
  • A review of biodiversity curves of marine organisms throughout early Paleozoic, indicating the occurrence of a large-scale, long-term radiation of life that started during late Precambrian time and was only finally interrupted in the Devonian Period, is published online by Harper, Cascales-Miñana & Servais (2019).[359]
  • A study on processes causing fluctuations of biodiversity of marine invertebrates throughout the Phanerozoic is published by Rominger, Fuentes & Marquet (2019).[360]
  • A study on the impact of environmental changes on the biodiversity of North American marine organisms throughout the Phanerozoic is published by Roberts & Mannion (2019).[361]
  • A study testing the hypothesis that the influence of ocean chemistry and climate on the ecological success of marine calcifiers decreased throughout the Phanerozoic is published by Eichenseer et al. (2019).[362]
  • A study on genus origination and extinction rates in the Ordovician on a global scale, for the paleocontinents Baltica and Laurentia, and for onshore and offshore areas, is published by Franeck & Liow (2019).[363]
  • First Middle Ordovician (DapingianDarriwilian) soft-bodied fossils from northern Gondwana (fossils of medusozoan possibly belonging to the genus Patanacta, possible members of the family Wiwaxiidae and an arthropod possibly belonging to the family Pseudoarctolepidae) are described from the Valongo Formation (Portugal) by Kimmig et al. (2019).[364]
  • New Konservat-Lagerstätte containing exceptionally preserved soft-bodied organisms, including the earliest record of Acoelomorpha, Turbellaria, Nemertea and Nematoda reported so far, is described from the Ordovician (Katian) Vauréal Formation (Canada) by Knaust & Desrochers (2019).[365]
  • A review of occurrence data of latest Ordovician benthic marine organisms is published by Wang, Zhan & Percival (2019), who evaluate the implications of the studied data for the knowledge of the course of the end-Ordovician mass extinction.[366]
  • A revision of Silurian fauna from the Pentland Hills (Scotland) described by Archibald Lamont in 1978 is published by Candela & Crighton (2019).[367]
  • A study on the course of graptolite extinctions during the middle Homerian biotic crisis and on the impact of this crisis on other marine invertebrates, as indicated by data from the Kosov Quarry section of the Prague Synform (Czech Republic), is published by Manda et al. (2019).[368]
  • Well-preserved fossil cryptic biota is reported from the submarine cavities of the Devonian (Emsian to Givetian) mud mounds in the Hamar Laghdad area (Morocco) by Berkowski et al. (2019).[369]
  • A study aiming to test and quantify the classification of Devonian biogeographic areas, based on distributional data of Devonian trilobite, brachiopod and fish taxa, is published by Dowding & Ebach (2019).[370]
  • A study on patterns of local richness of terrestrial tetrapods throughout the Phanerozoic is published by Close et al. (2019).[371]
  • Description of tetrapod and fish fossils from the coastal locality of Burnmouth, Scotland (Ballagan Formation), associated plant material and sedimentological context of these fossils is published by Clack et al. (2019), who interpret these fossils as evidence of the potential richness of the Tournaisian fauna, running counter to the assumption of a depauperate nonmarine fauna following the end-Devonian Hangenberg event.[372]
  • A study on the impact of climate changes during the Carboniferous–Permian transition on the evolution of land-living vertebrates is published by Pardo et al. (2019).[373]
  • A study aiming to test one of the scenarios proposed by Robert L. Carroll in 1970 to explain the origin of the amniotic egg, based on data from Permo-Carboniferous tetrapods, is published by Didier, Chabrol & Laurin (2019).[374]
  • An overview of the studies researching biodiversity changes in the Permian and their links to volcanism is published by Chen & Xu (2019).[375]
  • Haridy et al. (2019) report the occurrence of overgrowth of palatal dentition of Cacops and Captorhinus by a new layer of bone to which the newest teeth are then attached (the overgrowth pattern also documented in early fishes), and evaluate the implications of this finding for the knowledge of the origin of teeth.[376]
  • A study on the severity of the end-Guadalupian extinction event is published online by Rampino & Shen (2019).[377]
  • A study on the ecology of Permian tetrapods from the Abrahamskraal Formation (South Africa), as indicated by stable oxygen isotope compositions of phosphate from teeth and bones used as a proxy for water dependence, is published online by Rey et al. (2019).[378]
  • Two Permian tetrapod assemblages, recovered from the northernmost point at which the lowest Beaufort Group has been targeted for collecting fossils, are reported from the southern Free State (South Africa) by Groenewald, Day & Rubidge (2019), who evaluate the implications of these fossils for the knowledge of faunal provincialism within the Middle to Late Permian Karoo Basin.[379]
  • A study aiming to determine which Permian tetrapod assemblage zones are present in the vicinity of Victoria West (Northern Cape, South Africa), and to reassess the biostratigraphic provenance of specimens collected historically in this area (including the holotype of Lycaenops ornatus), is published by Day & Rubidge (2019).[380]
  • A study on the course of the turnover from the Daptocephalus to Lystrosaurus Assemblage Zones of the Karoo Basin is published by Gastaldo et al. (2019).[381]
  • A study on the timing of the extinction of latest Permian vertebrates in the Karoo Basin of South Africa is published online by Rampino et al. (2019).[382]
  • A study on the identification and position of the terrestrial end-Permian mass extinction in southern African sediments, based on data from a new site in the South African Karoo Basin, is published online by Botha et al. (2019).[383]
  • A study on the functional diversity of middle Permian and Early Triassic marine paleocommunities in the area of present-day western United States, and on its implications for the knowledge of functional re-organization of these communities in the aftermath of the Permian–Triassic extinction event, is published by Dineen, Roopnarine & Fraiser (2019).[384]
  • A study aiming to explain high biodiversity preserved in the Triassic Cassian Formation (Italy) is published online by Roden et al. (2019).[385]
  • A study on shark, sizable carnivorous archosaur, big herbivorous tetrapod and probable turtle bromalites (coprolites and possibly some cololites) from a turtle-dominated fossil assemblage from the Upper Triassic Poręba site (Poland) is published by Bajdek et al. (2019), who evaluate the implications of their findings for inferring the diet of the Triassic turtle Proterochersis porebensis.[386]
  • A study on seawater oxygenation during the Early Jurassic and its impact on the recovery of marine benthos after the Triassic–Jurassic extinction event, as indicated by data from Blue Lias Formation (United Kingdom), is published by Atkinson & Wignall (2019).[387]
  • A study on the patterns and processes of recovery of marine fauna after the Toarcian oceanic anoxic event, as indicated by data from the Cleveland Basin (Yorkshire, United Kingdom), is published by Caswell & Dawn (2019).[388]
  • A study on changes of land vegetation resulting from the Toarcian oceanic anoxic event is published by Slater et al. (2019).[389]
  • Skeletal elements of Oxfordian ichthyosaurs and plesiosaurs are reported from the Kingofjeld mountain (north-east Greenland) by Delsett & Alsen (2019).[390]
  • New marine reptile-bearing localities documenting the TithonianBerriasian transition at the High Andes (Mendoza Province, Argentina) are reported by Fernández et al. (2019).[391]
  • A study on microvertebrate fossils from the Upper Jurassic or Lower Cretaceous of Ksar Metlili (Anoual Syncline, Morocco), evaluating their palaeobiogeographical implications, and on the age of this fauna, is published online by Lasseron et al. (2019).[392]
  • Description of mid-Cretaceous invertebrate fauna from Batavia Knoll (eastern Indian Ocean), and a study on its similarities to other Cretaceous faunas from around the Indian Ocean, is published by Wild & Stilwell (2019).[393]
  • A study on the age of the vertebrate fauna from the Cretaceous Cerro Barcino Formation (Argentina) is published online by Krause et al. (2019).[394]
  • Possible amphibian, gastropod and insect egg masses are described from the Cretaceous amber from Myanmar by Xing et al. (2019).[395]
  • A study on coprolites from the Upper Cretaceous deposits in the Münster Basin (northwestern Germany), evaluating their implications for the knowledge of Cretaceous trophic structures and predator–prey interactions, is published by Qvarnström et al. (2019).[396]
  • New vertebrate assemblage from the upper Turonian Schönleiten Formation of Gams bei Hieflau (Austria) is described by Ősi et al. (2019).[397]
  • Turonian marine vertebrate fossils from the Huehuetla quarry (Puebla, Mexico) are described by Alvarado-Ortega et al. (2019).[398]
  • A study on the biogeography of Cretaceous terrestrial tetrapods is published by Kubo (2019).[399]
  • A study on the structure and contents of a large piece of amber attached to a jaw of a specimen of Prosaurolophus maximus from the Cretaceous Dinosaur Park Formation (Alberta, Canada), evaluating the implications of this finding for the knowledge of the habitat and taphonomy of the dinosaur, is published by McKellar et al. (2019).[400]
  • An accumulation of fossil eggshells of bird, crocodylomorph and gekkotan eggs is reported from the Late Cretaceous Oarda de Jos locality in the vicinity of the city of Sebeș (Romania) by Fernández et al. (2019).[401]
  • A review of the fossil record of Late Cretaceous and Paleogene vertebrates from the Seymour Island (Antarctica) is published by Reguero (2019).[402]
  • A study on the evolutionary history of the family Pospiviroidae, aiming to assess possible impact of the Cretaceous–Paleogene extinction event on the divergence rates in this family, is published by Bajdek (2019).[403]
  • A study on calcareous nanoplankton and planktic foraminiferal assemblages in a Cretaceous-Paleogene section from the peak ring of the Chicxulub crater, and on their implications for the knowledge of recovery of plankton after the Cretaceous–Paleogene extinction event, is published by Jones, Lowery & Bralower (2019).[404]
  • A study on the course of recovery of the nanoplankton communities after the Cretaceous–Paleogene extinction event is published by Alvarez et al. (2019), who report evidence indicative of 1.8 million years of exceptional volatility of post-extinction communities and indicating that the emergence of a more stable equilibrium-state community coincided with indicators of carbon cycle restoration and a fully functioning biological pump.[405]
  • A study on the timing and nature of recovery of benthic marine ecosystems of Antarctica after the Cretaceous–Paleogene mass extinction, as indicated by data from fossils of benthic molluscs, is published by Whittle et al. (2019).[406]
  • A study on the drivers and tempo of biotic recovery after Cretaceous–Paleogene mass extinction, as indicated by data from the Corral Bluffs section of the Denver Basin (Colorado, United States), is published by Lyson et al. (2019).[407]
  • Description of the vertebrate assemblage from the Oligocene Shine Us locality in the Khaliun Basin (Mongolia) is published by Daxner-Höck et al. (2019).[408]
  • Description of reptile and amphibian fossils from the early Miocene localities of the Kilçak section (Turkey) is published by Syromyatnikova et al. (2019).[409]
  • Description of fossil fish, amphibian and reptilian fauna from the middle Miocene locality Gračanica (Bosnia and Herzegovina) is published online by Vasilyan (2019).[410]
  • A study on the vertebrate fossils from the early Clarendonian localities within the Goliad Formation in Bee and Live Oak Counties in Texas (comprising the Lapara Creek Fauna), and on the stratigraphic context of these localities, is published by May (2019).[411]
  • New late Miocene vertebrate assemblage, including turtle, rodent and xenarthran fossils (among which is the oldest record of an armadillo belonging to the genus Dasypus reported so far), is described from the Los Alisos locality (Guanaco Formation, Argentina) by Ercoli et al. (2019).[412]
  • Description of a diverse late Miocene marine fauna from the Bloomfield Quarry (Wilson Grove Formation; California, United States), including the most diverse assemblage of fossil walruses yet reported worldwide from a single locality, is published by Powell et al. (2019).[413]
  • Fish, turtle and mammals fossils are described from a locality near Whitehorse (Yukon, Canada), probably of Miocene age, by Eberle et al. (2019).[414]
  • A study on microscopic traces of hominin and animal activities in the Denisova Cave (Russia), providing the information on the use of this cave over the last 300,000 years, is published by Morley et al. (2019).[415]
  • A study on the age of the Pleistocene vertebrate assemblage from the Khok Sung locality (Thailand) is published by Duval et al. (2019).[416]
  • Revision of reptile and amphibian fossils from the late Pleistocene collection of the "Caverne Marie-Jeanne" (Hastière-Lavaux, Namur Province, Belgium) is published by Blain et al. (2019).[417]
  • New late Pleistocene site Tsaramody (Sambaina basin, Madagascar), preserving diverse subfossil remains of vertebrates, is reported by Samonds et al. (2019).[418]
  • A study on the paleoecology and diet of late Pleistocene terrestrial vertebrates known from an asphalt deposit (Project 23, Deposit 1) at Rancho La Brea (California, United States) is published online by Fuller et al. (2019).[419]
  • A study on changes of vegetation in southern Borneo over the past 40,000  calibrated years BP, as indicated by data from Saleh Cave (South Kalimantan, Indonesia), is published by Wurster et al. (2019).[420]
  • Late Quaternary fossils of vertebrates are described from caves in the Manning Karst Region of eastern New South Wales (Australia) by Price et al. (2019).[421]
  • A study aiming to determine the relationships between extinctions of megafauna, climatic changes and patterns of human appearance in south-eastern Australia over the last 120,000 years is published by Saltré et al. (2019).[422]
  • A study on the causes of Holocene extinction of megafauna of Madagascar is published by Godfrey et al. (2019).[423]
  • A review discussing possible links between the fossil record of marine biodiversity, nutrient availability and primary productivity is published online by Martin & Servais (2019).[424]
  • A study on factors which determined the relative intensity of marine extinctions during greenhouse–icehouse transitions in the Late Ordovician and the Cenozoic is published online by Saupe et al. (2019).[425]
  • A study on the possible relationship between speciation and extinction rates of different groups of organisms and the ages of these groups, as indicated by data from extant and fossil species, is published by Henao Diaz et al. (2019).[426][427][428]
  • A study on the evolution of bite force of amniotes, as indicated by data from extant and fossil taxa, is published by Sakamoto, Ruta & Venditti (2019).[429]
  • A study on the phylogenetic distribution, morphological variation and functions of apicobasal ridges (elevated ridges of tooth enamel) in aquatic reptiles and mammals, as indicated by data from extant and fossil taxa, is published by McCurry et al. (2019).[430]
  • A study on the impact of uncertainty of stratigraphic age of fossils on studies estimating species divergence times which incorporate fossil taxa, based on data from the fossil record of North American mammals and from the dataset of extant and fossil cetaceans, is published by Barido-Sottani et al. (2019).[431]
  • A study evaluating the impact of information about stratigraphic ranges of fossil taxa on the analyses of timing of evolutionary divergence is published online by Püschel et al. (2019).[432]
  • A study on anatomical distribution, abundance, geometry, melanin chemistry and elemental inventory of melanosomes in tissues of extant vertebrates, evaluating their implications for reconstructions of internal soft-tissue anatomy in fossil vertebrates, is published by Rossi et al. (2019).[433]
  • A study on the chronostratigraphy and biostratigraphy of Cenozoic vertebrate (mostly mammal) fossils from the South Carolina Coastal Plain is published by Albright et al. (2019).[434]

Other research

Other research related to paleontology, including research related to geology, palaeogeography, paleoceanography and paleoclimatology.

  • A study on the biological oxygen production during the Mesoarchean, as indicated by data from Mesoarchean shales of the Mozaan Group (Pongola Supergroup, South Africa) preserving record of a shallow ocean "oxygen oasis", is published by Ossa Ossa et al. (2019).[435]
  • A study on the extent of the oxygenation of ocean waters over continental shelves before the Great Oxidation Event, as indicated by data from 2.5-billion-year-old Mount McRae Shale (Australia), is published by Ostrander et al. (2019).[436]
  • A study on the extent of the oxygenation of shallow oceans 2.45 billion years ago is published by Rasmussen et al. (2019), who interpret their findings as indicating that oxygen levels both the surface oceans and atmosphere were exceedingly low before the Great Oxidation Event, which the authors interpret as directly caused by evolution of oxygenic photosynthesis.[437]
  • A study aiming to determine whether the overall size of the biosphere decreased at the end of the Great Oxidation Event, based on data on isotope geochemistry of sulfate minerals from the Belcher Group (subarctic Canada), is published by Hodgskiss et al. (2019).[438]
  • Evidence of a burst of mantle activity at the end of the Archean (around 2.5 billion years ago) is presented by Marty et al. (2019), who interpret their findings as lending credence to models advocating a magmatic origin for environmental changes such as the Great Oxidation Event.[439]
  • A study aiming to determine the effects of competition of early anoxygenic phototrophs and primitive oxygenic phototrophs on the Earth system, especially on the large-scale oxygenation of Earth's atmosphere ~2.3 billion years ago, is published by Ozaki et al. (2019).[440]
  • A study on the geochemistry of mat-related structures and their host sediments from the Francevillian Formation (Gabon) is published by Aubineau et al. (2019), who evaluate the implications of their findings for the knowledge whether ancient microbes induced illitisation (conversion of smectite to illite–smectite mixed-layer minerals), and for the knowledge of Earth's climate and ocean chemistry in the Paleoproterozoic.[441]
  • A study on the organic geochemical (biomarker) signatures of the 1.38-billion-years-old black siltstones of the Velkerri Formation (Australia), and on their implications for inferring the microbial diversity and palaeoenvironment of the Proterozoic Roper Seaway, is published by Jarrett et al. (2019).[442]
  • A study on the origins of putative stromatolites and associated carbonate minerals from lacustrine sedimentary rocks of the 1.1-billion-years-old Stoer Group is published by Brasier et al. (2019).[443]
  • A study suggesting a link between early evolution and diversification of animals and high availability of copper in the late Neoproterozoic is published by Parnell & Boyce (2019).[444]
  • A study aiming to determine the cause of the uniquely high amplitudes of Neoproterozoic δ13C excursions is published by Shields et al. (2019).[445]
  • A study evaluating the possible relationship between the Cryogenian magmatic activity and the evolution of early life, based on data from the Cryogenian Yaolinghe Group (China), is published by Long, Zhang & Luo (2019).[446]
  • Evidence for oxygenated waters near ice sheet grounding lines during the Cryogenian is presented by Lechte et al. (2019).[447]
  • A study on ocean oxygen levels during the Ediacaran Shuram negative C-isotope Excursion and the middle Ediacaran, and on their implications for the evolution of the Ediacaran biota, is published by Zhang et al. (2019).[448]
  • A study on the causes of widespread preservation of soft-bodied organisms in sandstones of the Ediacara Member in South Australia is published by Liu et al. (2019).[449]
  • A study on the seafloor oxygen fugacity in the time of the emergence of the earliest known benthic animals, as inferred from data from the latest Ediacaran Dengying Formation (China), is published by Ding et al. (2019).[450]
  • A study on the process of fossilization of Ediacaran organisms, and on its impact on the preservation of the external shape of these organisms, is published by Bobrovskiy et al. (2019).[451]
  • A study on the global extent of the oxygenation of seafloor, surface oceans and atmosphere during early Cambrian is published by Dahl et al. (2019), who report evidence of two major oceanic anoxic events in the early Cambrian.[452]
  • A study on nitrogen isotope and organic carbon isotope data from the lower Cambrian Niutitang Formation (China) is published online by Xu et al. (2019), who link nitrogen cycle perturbations to animal diversification during the early Cambrian.[453]
  • A study on the paleoecological characteristics of Cambrian marine ecosystems of central Sonora (Mexico) is published by Romero et al. (2019).[454]
  • A study on seawater temperatures during the Cambrian, as indicated by data from oxygen isotope analyses of Cambrian brachiopod shells, is published by Wotte et al. (2019).[455]
  • A study on bottom-water redox conditions in the late Cambrian Alum Shale Sea, as indicated by sedimentary molybdenum contents of the Alum Shale, is published by Dahl et al. (2019), who interpret their findings as indicating that anoxic sulfidic bottom waters were an intermittent rather than persistent feature of Cambrian oceans, and that early animals invaded the seafloor during oxygenated periods.[456]
  • A study on the paleogeographic position of all major Phanerozoic arc-continent collisions, comparing it with the latitudinal distribution of ice-sheets throughout the Phanerozoic, is published by Macdonald et al. (2019).[457]
  • A study aiming to determine whether the Ordovician meteor event directly affected Earth's climate and biota is published by Schmitz et al. (2019).[458]
  • A review of the evidence of evolutionary radiation of animals throughout the Great Ordovician Biodiversification Event, and of environmental changes coincident with these biotic changes, is published by Stigall et al. (2019).[459]
  • A study on conodont oxygen isotope compositions in Ordovician samples from Argentine Precordillera and Laurentia, and on their implications for the knowledge of palaeothermometry and drift of the Precordillera in the early Paleozoic, is published online by Albanesi et al. (2019).[460]
  • A study on carbon isotope data from stratigraphic sections at Germany Valley (West Virginia) and Union Furnace (Pennsylvania) in the Central Appalachian Basin, evaluating its implications for the knowledge of change in atmospheric oxygen levels during the late Ordovician and its possible relationship with early diversification of land plants, is published by Adiatma et al. (2019).[461]
  • Signatures of Devonian (Famennian) forests and soils preserved in black shales in the southernmost Appalachian Basin (Chattanooga Shale; Alabama, United States) are presented by Lu et al. (2019).[462]
  • A study examining the intensity of explosive volcanism from 400 to 200 million years ago, and evaluating its impact on the late Paleozoic Ice Age, is published by Soreghan, Soreghan & Heavens (2019).[463]
  • Description of Cisuralian charcoal from the Barro Branco coal seam (Siderópolis Member of the Rio Bonito Formation, Brazil), and a study on its implications for reconstruction of palaeo-wildfire occurrences in peat-forming vegetation through the Late Palaeozoic in Gondwana, is published by Benicio et al. (2019).[464]
  • A study on the extent and causes of the end-Capitanian extinction event, based on data from the Middle to Late Permian section of the Sverdrup Basin (Ellesmere Island, Canada), is published online by Bond, Wignall & Grasby (2019).[465]
  • A study on the ocean chemistry during the Permian–Triassic extinction event, as indicated by data from a new stratigraphic section in Utah, and on its implications for the knowledge of the causes of this extinction, is published by Burger, Estrada & Gustin (2019).[466]
  • A study aiming to determine the stratigraphic position of the end-Permian biotic crisis in the Sydney Basin (Australia) is published by Fielding et al. (2019), who also attempt to determine the climate changes in this region concurrent with the end-Permian extinction.[467]
  • A study on shifts in volcanic activity across the Permian-Triassic boundary, as indicated by measurements of mercury in marine sections across the Northern Hemisphere, is published by Shen et al. (2019).[468]
  • A study on mercury enrichments in Permian-Triassic boundary sections from Lubei (South China craton) and Dalongkou (Junggar terrane), and on their implications for the knowledge of volcanic activity during the Permian-Triassic transition, is published by Shen et al. (2019).[469]
  • Evidence of the environmental transition from meandering to braided rivers and of the development of desert-like conditions in the earliest Triassic is reported from Permian-Triassic boundary sections in Shanxi (China) by Zhu et al. (2019).[470]
  • A study on the nitrogen isotope variations in oceanic waters in the aftermath of the end-Permian mass extinction is published by Sun et al. (2019), whose conceptual model indicates ammonium intoxication of the oceans during this time period.[471]
  • A study on microbially induced sedimentary structures from the Lower Triassic Blind Fiord Formation (Arctic Canada), evaluating their implications for the knowledge of the course of biotic recovery in the aftermath of the Permian–Triassic extinction event, is published online by Wignall et al. (2019).[472]
  • A study on the oxygen isotope compositions of discrete conodont elements from the Lower Triassic Mianwali Formation (Pakistan), and on their implications for inferring the timing of temperature changes and the interrelationship between climate and biodiversity patterns during the Smithian-Spathian biotic crisis, is published by Goudemand et al. (2019).[473]
  • A study on nutrient availability through the Early to Middle Triassic along the northern margin of Pangea is published online by Grasby et al. (2019).[474]
  • A study on the character and extent of the Triassic Boreal Ocean delta plain across the area of the present-day Barents Sea, interpreted as the largest delta plain reported so far, is published by Klausen, Nyberg & Helland-Hansen (2019).[475]
  • A study aiming to determine links between volcanic activity in the Central Atlantic magmatic province, elevated concentrations of mercury in marine and terrestrial sediments and abnormalities of fossil fern spores across the Triassic-Jurassic boundary in southern Scandinavia and northern Germany is published by Lindström et al. (2019).[476]
  • A study aiming to reconstruct the palaeoenvironmental changes of the late Pliensbachian outside of Western Tethys Ocean and to test their temporal relation to large igneous province volcanism is published by De Lena et al. (2019).[477]
  • Krencker, Lindström & Bodin (2019) present sedimentological, paleontological and geochemical evidence from the Central High Atlas Basin (Morocco) and Jameson Land (Greenland) indicative of the occurrence of a major sea-level drop prior to the onset of the Toarcian oceanic anoxic event.[478]
  • A study on the duration of the Toarcian oceanic anoxic event, as indicated by data from the Talghemt section in the High Atlas (Morocco), is published by Boulila et al. (2019).[479]
  • A study on the Middle Jurassic palaeoenvironment of La Voulte (France), as indicated by data from exceptionally preserved eyes of the polychelidan lobster Voulteryon parvulus and from epibiontic brachiopods associated with V. parvulus, is published by Audo et al. (2019).[480]
  • A study comparing the Jurassic floras of the Ayuquila Basin and the Otlaltepec Basin (Mexico) and evaluating their implications for the knowledge of the Jurassic environments of these basins is published by Velasco-de León et al. (2019).[481]
  • A study on Jurassic paleomagnetism, based on an updated set of Jurassic paleopoles from Adria (Italy), is published by Muttoni & Kent (2019).[482]
  • A study on the chronostratigraphy of the Upper Jurassic Morrison Formation is published by Maidment & Muxworthy (2019).[483]
  • Evidence of repeated significant oceanic and biotic turnovers in the area of the present-day Gulf of Mexico at the Jurassic-Cretaceous transition is presented by Zell et al. (2019).[484]
  • A study on the age of the dinosaur-bearing Upper Jurassic–Lower Cretaceous sediments of western Maestrazgo Basin and South-Iberian Basin (eastern Spain), aiming to also reconstruct the palaeoenvironments of this area on the basis of data from these sediments, is published by Campos-Soto et al. (2019).[485]
  • A review of data on the Jurassic and Cretaceous climates of Siberia is published by Rogov et al. (2019).[486]
  • A study on global climatic changes during the Early Cretaceous, focusing on the duration and magnitude of Early Cretaceous cold episodes, is published by Vickers et al. (2019).[487]
  • Evidence from the Lower Cretaceous strata around the southern margin of the Eromanga Basin (Australia) indicative of cold (limited glacial and/or seasonal freezing) conditions persisting in Southern Australia through the Hauterivian and the Aptian is presented by Alley, Hore & Frakes (2019).[488]
  • A study on phototropism in extant trees from Beijing and Jilin Provinces and fossil tree trunks from the Jurassic Tiaojishan and Tuchengzi formations in Liaoning and Beijing regions (China), and on its implications for inferring the history of the rotation of the North China Block, is published by Jiang et al. (2019).[489]
  • A study on the age of the Cretaceous Cloverly Formation is published by D'Emic et al. (2019).[490]
  • Evidence from the chronostratigraphy, fossil content, bracketing facies and ages of the Cretaceous Wayan Formation of Idaho and Vaughn Member of the Blackleaf Formation of Montana, indicating that they represent the same depositional system prior to disruption by subsequent tectonic and volcanic events, is presented by Krumenacker (2019).[491]
  • A study on Cenomanian plants from the Redmond no.1 mine near Schefferville (Redmond Formation; Labrador Peninsula, Canada) and on their implications for the knowledge of paleoclimate of this site is published by Demers-Potvin & Larsson (2019).[492]
  • The first high-resolution record of CenomanianTuronian paleotemperatures from the Southern Hemisphere, as indicated by data from the Ocean Drilling Program Site 1138 on the Kerguelen Plateau, is presented by Robinson et al. (2019).[493]
  • A study on the impact of marine biogeochemical processes on the Cretaceous Thermal Maximum is published by Wallmann et al. (2019).[494]
  • A study on the age of the Upper Cretaceous Wadi Milk Formation (Sudan) is published by Owusu Agyemang et al. (2019).[495]
  • A study on Cenomanian to Coniacian polar environmental conditions at eight locations in northeast Russia and northern Alaska is published online by Spicer et al. (2019).[496]
  • A study on variability of carbon, oxygen and nitrogen isotopes in multiple tissues from a wide array of extant vertebrate taxa from the Atchafalaya River Basin in Louisiana (inferred to be an environmental analogue to the Late Cretaceous coastal floodplains of North America), and on its implications for formulating and testing predictions about ancient ecological communities based on stable isotope data from fossil specimens, is published by Cullen et al. (2019).[497]
  • A study on the general distribution and stratigraphy of the lower shale member of the Campanian Aguja Formation (Texas, United States), and a revision of all significant larger vertebrate fossil specimens from these strata, is published by Lehman et al. (2019).[498]
  • High-precision dating for the Battle Formation (Alberta, Canada) is presented by Eberth & Kamo (2019).[499]
  • High-precision dating and the first calibrated chronostratigraphy for the Horseshoe Canyon Formation (Alberta, Canada) is presented by Eberth & Kamo (2019).[500]
  • A study on the Maastrichtian climate of Arctic Alaska, based on data from the Prince Creek Formation, is published by Salazar-Jaramillo et al. (2019).[501]
  • Studies on the timing of the Deccan Traps volcanism close to the Cretaceous-Paleogene boundary are published by Schoene et al. (2019), who interpret their findings as indicative of four high-volume eruptive periods close to the Cretaceous-Paleogene boundary, the first of which occurred tens of thousands of years prior to both the Chicxulub bolide impact and Cretaceous–Paleogene extinction event[502] and by Sprain et al. (2019), who interpret their findings as indicating that a steady eruption of the flood basalts mostly occurred in the earliest Paleogene.[503]
  • A study on the environmental variability before and across the Cretaceous-Paleogene mass extinction, as inferred from data on the calcium isotope ratios of aragonitic mollusc shells from the Lopez de Bertodano Formation (Antarctica), is published online by Linzmeier et al. (2019).[504]
  • A turbulently deposited sediment package directly overlain by the Cretaceous–Paleogene boundary tonstein is reported from the Tanis site (Hell Creek Formation, North Dakota, United States) by DePalma et al. (2019), who interpret their findings as indicating that deposition occurred shortly after a major bolide impact, and might have been caused by the Chicxulub impact.[505]
  • A study on the immediate aftermath of the Chicxulub impact at the Cretaceous–Paleogene boundary, based on data from the Chicxulub crater, is published by Gulick et al. (2019).[506]
  • Evidence of rapid ocean acidification in the aftermath of the Chicxulub impact and of the protracted Earth system recovery after the Cretaceous–Paleogene extinction event is presented by Henehan et al. (2019).[507]
  • The longest, highest resolution, stratigraphically continuous, single-species benthic foraminiferal carbon and oxygen isotope records for the Late Maastrichtian to Early Eocene from a single site in the South Atlantic Ocean, providing information on the evolution of climate and carbon-cycling during this time period, are presented by Barnet et al. (2019).[508]
  • O'Leary et al. (2019) publish a monograph on the sedimentology and sequence stratigraphy of the part of Mali which was covered by an ancient epeiric sea known as the Trans-Saharan Seaway during the Late Cretaceous and early Paleogene, provide the first formal description of and nomenclature for the Upper Cretaceous and lower Paleogene geological formations of this region, and revise fossil flora and fauna of this region.[509]
  • Zeebe & Lourens (2019) provide a new absolute astrochronology up to 58 Ma and a new Paleocene–Eocene boundary age.[510]
  • A study on stomata of fossil specimens of members of the family Lauraceae from the Eocene of Australia and New Zealand, evaluating their implications for reconstructions of Eocene pCO2 levels, is published by Steinthorsdottir et al. (2019).[511]
  • Climate simulations capturing major climatic features of the Early Eocene and the Paleocene–Eocene Thermal Maximum in a state-of-the-art Earth system model are presented by Zhu, Poulsen & Tierney (2019).[512]
  • A study evaluating the utility of membrane lipids of members of Thaumarchaeota (now Nitrososphaerota) as proxies for the carbon isotope excursion and surface ocean warming, and assessing their implications for the knowledge of the source and size of carbon emissions during the Paleocene–Eocene Thermal Maximum, is published by Elling et al. (2019).[513]
  • A study on abundant black charcoal shards from Paleogene sites of Wilson Lake B (New Jersey) and Randall's Farm (Maryland) is published by Fung et al. (2019), who interpret these shards as most likely to be evidence of widespread wildfires at the Paleocene-Eocene boundary caused by extraterrestrial impact.[514]
  • A study on the impact of carbon-based greenhouse gas fluxes associated with the North Atlantic Igneous Province on the onset of the Paleocene–Eocene Thermal Maximum is published by Jones et al. (2019).[515]
  • Evidence from the Deep Ivorian Basin offshore West Africa (equatorial Atlantic Ocean), indicating that peak warming during the Middle Eocene Climatic Optimum was associated with upper-ocean stratification, decreased export production, and possibly harmful algal blooms, is presented by Cramwinckel et al. (2019).[516]
  • New stable isotopes record of the Middle Eocene Climatic Optimum event is reported from eastern Turkey by Giorgioni et al. (2019).[517]
  • A study on variations of ocean circulation and marine bioproductivity related to the beginnings of the formation of the Antarctic Circumpolar Current, based on data from Eocene and Oligocene sedimentary drift deposits east of New Zealand, is published by Sarkar et al. (2019).[518]
  • A study on changes in surface water temperature in the eastern North Sea Basin during the late Priabonian to earliest Rupelian is published by Śliwińska et al. (2019).[519]
  • A study linking the onset or strengthening of an Atlantic meridional overturning circulation to the closure of the Arctic–Atlantic gateway at the Eocene–Oligocene transition is published by Hutchinson et al. (2019).[520]
  • A study on the timing of the uplift of the Tibetan Plateau, as indicated by the discovery of the Oligocene palm fossils in the Lunpola Basin in Tibet, is published by Su et al. (2019).[521]
  • A review of vertebrate fossils from the Tibetan Plateau, evaluating their implications for inferring the course of the uplift of the Tibetan Plateau, is published by Deng et al. (2019).[522]
  • A study on the impact of changing Eocene paleogeography and climate on the utility of stable isotope paleoaltimetry methods in the studies aiming to reconstruct the elevation history of the Tibetan Plateau is published by Botsyun et al. (2019).[523][524][525]
  • A study on the causes of the long-term climate cooling during the Neogene is published by Rugenstein, Ibarra & von Blanckenburg (2019).[526]
  • A study on the climatic and environmental conditions in the Loperot site (Kenya) in the early Miocene is published by Liutkus-Pierce et al. (2019).[527]
  • A study on the timing and course of the separation of the Indian Ocean and the Mediterranean Sea in the Miocene is published by Bialik et al. (2019).[528]
  • A study comparing changes of the export of intermediate-depth Pacific waters to the western North Atlantic prior to the closure of the Central American Seaway with records of strength of the Atlantic meridional overturning circulation, evaluating the implications of this data for the knowledge of the timing of closure of the Central American Seaway, is published by Kirillova et al. (2019).[529]
  • A study on climatic and environmental changes in central Andes during the late Miocene is published by Carrapa, Clementz & Feng (2019).[530]
  • A study on the exact age of the marine fauna from the Miocene Chilcatay and Pisco formations (Peru), and on its implications for reconstructions of local paleoenvironment, is published online by Bosio et al. (2019).[531]
  • A study on the origin of the African C4 savannah grasslands is published by Polissar et al. (2019).[532]
  • A study on the anatomical traits of teeth and inferred diet of bovids, suids and rhinocerotids from Kanapoi, and on their implications for reconstructing the environments of this site, is published online by Dumouchel & Bobe (2019).[533]
  • New spatial data on the Plio-Pleistocene Bolt's Farm pits from the Cradle of Humankind site (South Africa) is presented by Edwards et al. (2019), who also attempt to provide key biochronological ages for the Bolt's Farm deposits.[534]
  • A study on the global mean sea level during the Pliocene mid-Piacenzian Warm Period is published by Dumitru et al. (2019).[535]
  • A study on the amplitude of sea-level variations during the Pliocene is published by Grant et al. (2019).[536]
  • Simulations of coevolution of climate, ice sheets and carbon cycle over the past 3 million years are presented by Willeit et al. (2019).[537]
  • A study on the age of the Sahara, as indicated by data from Pliocene and Pleistocene paleosols from the Canary Islands, is published by Muhs et al. (2019).[538]
  • A study on the latest Villafranchian climate and environment of the area of southern Italy, as indicated by amphibian and reptile fossil record from the Pirro Nord karstic complex, is published by Blain et al. (2019).[539]
  • A study on atmospheric gas levels before and after the shift from glacial cycles of 100 thousand years to 40-thousand-year cycles around one million years ago, as inferred from data from ice core samples from the Allan Hills Blue Ice Area (East Antarctica), is published by Yan et al. (2019).[540]
  • A study on pCO2 levels from 2.6 to 0.8 Ma is published by Da et al. (2019), who find no evidence indicating that the Mid-Pleistocene Transition was caused by the decline of pCO2.[541]
  • A study on changes in winter rainfall in the Mediterranean over the past 1.36 million years is published by Wagner et al. (2019).[542]
  • Results of stable carbon and oxygen isotope analyses of tooth enamel samples from Pleistocene mammals from the Yugong Cave and Baxian Cave (China) are presented by Sun et al. (2019), who evaluate the implications of their findings for the knowledge of Pleistocene climatic and environmental changes in South China.[543]
  • A study on Pleistocene mammal fossils from the Yai Ruak Cave (Krabi Province, Thailand), including the southernmost known record of Crocuta crocuta ultima, is published by Suraprasit et al. (2019), who evaluate the implications of these fossils for reconstructions of the environment in the area of the Malay Peninsula in the Pleistocene.[544]
  • A study on Acheulean and Middle Stone Age sites from the Eastern Desert (Sudan), preserving stone artifacts, is published by Masojć et al. (2019), who interpret these sites as evidence of green corridor or corridors across Sahara which made early hominin dispersal possible.[545]
  • Evidence from oxygen isotope data from Soreq Cave speleothems (Israel), indicative of the occurrence of summer monsoon rainfall in the Middle East during recurrent intervals of the last interglacial period (overlapping with archeological indicators of human migration), is presented by Orland et al. (2019).[546]
  • A study on the spatial and temporal distribution of ancient peatlands in the past 130,000 years is published by Treat et al. (2019).[547]
  • A study on the size of fossil rabbits from 14 late Pleistocene and Holocene archaeological sites in Portugal, and on its implications for the knowledge of temperatures and environment in the area of Portugal during the last glaciation, is published by Davis (2019).[548]
  • A study on Pleistocene small mammal remains from Stratigraphic Unit V from El Salt site (Alcoy, Spain), evaluating their implications for the knowledge of climatic conditions in the eastern Iberian Peninsula at the time of the disappearance of local Neanderthal populations during Marine Isotope Stage 3, is published by Fagoaga et al. (2019).[549]
  • A study on the sedimentary sequence from the Pilauco site in Chile, evaluating whether evidence from this site is consistent with the Younger Dryas impact hypothesis, is published by Pino et al. (2019).[550]
  • A study on variations of size of fossil murine rodents from Liang Bua (Flores, Indonesia) through time, and on their implications for reconstructions of paleoclimate and paleoenvironment of Flores, is published by Veatch et al. (2019).[551]
  • A study on human land use worldwide from 10,000 years before the present to 1850 CE, indicating that Earth was to a large extent transformed by human activity by 3000 years ago, is published by Stephens et al. (2019).[552]
  • Evidence for synchronous cyclical changes in monsoon climate, human activity and prehistoric cultural development in the area of northeast China throughout the Holocene is presented by Xu et al. (2019).[553]
  • A study on Andean plate tectonics since the late Mesozoic is published by Chen, Wu & Suppe (2019).[554]
  • A study on the course of the collision of India and Asia, as indicated by palaeomagnetic data from the Burma Terrane, is published by Westerweel et al. (2019).[555]
  • A scenario for the genesis of tropical cyclones throughout the Cenozoic is presented by Yan et al. (2019).[556]
  • A study on the extent of ice sheets in the Northern Hemisphere throughout the Quaternary is published by Batchelor et al. (2019).[557]
  • A new method of concentration of proteins from fossil specimens with high humic content and of removal of humic substances is presented by Schroeter et al. (2019).[558]

References

  • Media related to 2019 in paleontology at Wikimedia Commons
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