2018 in paleomammalogy: Difference between revisions

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* Microscopic glass shards characteristic of the Youngest Toba Tuff (ashfall from the Toba eruption), dated as approximately 74,000 years old, are described from two archaeological sites on the south coast of [[South Africa]] by Smith ''et al.'' (2018), who interpret their findings as indicating that humans in this region thrived through the Toba event and the ensuing full glacial conditions.<ref>{{Cite journal|author1=Eugene I. Smith |author2=Zenobia Jacobs |author3=Racheal Johnsen |author4=Minghua Ren |author5=Erich C. Fisher |author6=Simen Oestmo |author7=Jayne Wilkins |author8=Jacob A. Harris |author9=Panagiotis Karkanas |author10=Shelby Fitch |author11=Amber Ciravolo |author12=Deborah Keenan |author13=Naomi Cleghorn |author14=Christine S. Lane |author15=Thalassa Matthews |author16=Curtis W. Marean |year=2018 |title=Humans thrived in South Africa through the Toba eruption about 74,000 years ago |journal=Nature |volume=555 |issue=7697 |pages=511–515 |doi=10.1038/nature25967 |pmid=29531318 }}</ref>
* Microscopic glass shards characteristic of the Youngest Toba Tuff (ashfall from the Toba eruption), dated as approximately 74,000 years old, are described from two archaeological sites on the south coast of [[South Africa]] by Smith ''et al.'' (2018), who interpret their findings as indicating that humans in this region thrived through the Toba event and the ensuing full glacial conditions.<ref>{{Cite journal|author1=Eugene I. Smith |author2=Zenobia Jacobs |author3=Racheal Johnsen |author4=Minghua Ren |author5=Erich C. Fisher |author6=Simen Oestmo |author7=Jayne Wilkins |author8=Jacob A. Harris |author9=Panagiotis Karkanas |author10=Shelby Fitch |author11=Amber Ciravolo |author12=Deborah Keenan |author13=Naomi Cleghorn |author14=Christine S. Lane |author15=Thalassa Matthews |author16=Curtis W. Marean |year=2018 |title=Humans thrived in South Africa through the Toba eruption about 74,000 years ago |journal=Nature |volume=555 |issue=7697 |pages=511–515 |doi=10.1038/nature25967 |pmid=29531318 }}</ref>
* Evidence of human activity dating back to 78,000 years ago is reported from the Panga ya Saidi cave ([[Kenya]]) by Shipton ''et al.'' (2018), who describe a rich technological sequence that includes lithic forms elsewhere associated with the [[Middle Stone Age]] and the [[Later Stone Age]].<ref>{{cite journal |author1=Ceri Shipton |author2=Patrick Roberts |author3=Will Archer |author4=Simon J. Armitage |author5=Caesar Bita |author6=James Blinkhorn |author7=Colin Courtney-Mustaphi |author8=Alison Crowther |author9=Richard Curtis |author10=Francesco d’ Errico |author11=Katerina Douka |author12=Patrick Faulkner |author13=Huw S. Groucutt |author14=Richard Helm |author15=Andy I. R Herries |author16=Severinus Jembe |author17=Nikos Kourampas |author18=Julia Lee-Thorp |author19=Rob Marchant |author20=Julio Mercader |author21=Africa Pitarch Marti |author22=Mary E. Prendergast |author23=Ben Rowson |author24=Amini Tengeza |author25=Ruth Tibesasa |author26=Tom S. White |author27=Michael D. Petraglia |author28=Nicole Boivin |year=2018 |title=78,000-year-old record of Middle and Later stone age innovation in an East African tropical forest |journal=Nature Communications |volume=9 |pages=Article number 1832 |doi=10.1038/s41467-018-04057-3 |pmid=29743572 |pmc=5943315 }}</ref>
* Evidence of human activity dating back to 78,000 years ago is reported from the Panga ya Saidi cave ([[Kenya]]) by Shipton ''et al.'' (2018), who describe a rich technological sequence that includes lithic forms elsewhere associated with the [[Middle Stone Age]] and the [[Later Stone Age]].<ref>{{cite journal |author1=Ceri Shipton |author2=Patrick Roberts |author3=Will Archer |author4=Simon J. Armitage |author5=Caesar Bita |author6=James Blinkhorn |author7=Colin Courtney-Mustaphi |author8=Alison Crowther |author9=Richard Curtis |author10=Francesco d’ Errico |author11=Katerina Douka |author12=Patrick Faulkner |author13=Huw S. Groucutt |author14=Richard Helm |author15=Andy I. R Herries |author16=Severinus Jembe |author17=Nikos Kourampas |author18=Julia Lee-Thorp |author19=Rob Marchant |author20=Julio Mercader |author21=Africa Pitarch Marti |author22=Mary E. Prendergast |author23=Ben Rowson |author24=Amini Tengeza |author25=Ruth Tibesasa |author26=Tom S. White |author27=Michael D. Petraglia |author28=Nicole Boivin |year=2018 |title=78,000-year-old record of Middle and Later stone age innovation in an East African tropical forest |journal=Nature Communications |volume=9 |pages=Article number 1832 |doi=10.1038/s41467-018-04057-3 |pmid=29743572 |pmc=5943315 }}</ref>
* A cross-hatched pattern drawn with an ochre crayon is reported from approximately 73,000-year-old [[Middle Stone Age]] levels at [[Blombos Cave]] ([[South Africa]]) by Henshilwood ''et al.'' (2018), pre-dating previously known abstract and figurative drawings by at least 30,000 years.<ref>{{cite journal |author1=Christopher S. Henshilwood |author2=Francesco d’Errico |author3=Karen L. van Niekerk |author4=Laure Dayet |author5=Alain Queffelec |author6=Luca Pollarolo |year=2018 |title=An abstract drawing from the 73,000-year-old levels at Blombos Cave, South Africa |journal=Nature |volume=in press |issue= |pages= |doi=10.1038/s41586-018-0514-3 }}</ref>
* A study on the age of the cave art from the [[Kapova Cave]] ([[Russia]]) is published by Dublyansky ''et al.'' (2018).<ref>{{cite journal |author1=Yuri Dublyansky |author2=Gina E. Moseley |author3=Yuri Lyakhnitsky |author4=Hai Cheng |author5=Lawrence R. Edwards |author6=Denis Scholz |author7=Gabriella Koltai |author8=Christoph Spötl |year=2018 |title=Late Palaeolithic cave art and permafrost in the Southern Ural |journal=Scientific Reports |volume=8 |pages=Article number 12080 |doi=10.1038/s41598-018-30049-w |pmid=30104606 |pmc=6089975 }}</ref>
* A study on the age of the cave art from the [[Kapova Cave]] ([[Russia]]) is published by Dublyansky ''et al.'' (2018).<ref>{{cite journal |author1=Yuri Dublyansky |author2=Gina E. Moseley |author3=Yuri Lyakhnitsky |author4=Hai Cheng |author5=Lawrence R. Edwards |author6=Denis Scholz |author7=Gabriella Koltai |author8=Christoph Spötl |year=2018 |title=Late Palaeolithic cave art and permafrost in the Southern Ural |journal=Scientific Reports |volume=8 |pages=Article number 12080 |doi=10.1038/s41598-018-30049-w |pmid=30104606 |pmc=6089975 }}</ref>
* A reassessment of the Late [[Pleistocene]] human occupation site at Leang Burung 2 ([[Sulawesi]], [[Indonesia]]), presenting new stratigraphic information and dating evidence from the site, is published by Brumm ''et al.'' (2018).<ref>{{Cite journal|author1=Adam Brumm |author2=Budianto Hakim |author3=Muhammad Ramli |author4=Maxime Aubert |author5=Gerrit D. van den Bergh |author6=Bo Li |author7=Basran Burhan |author8=Andi Muhammad Saiful |author9=Linda Siagian |author10=Ratno Sardi |author11=Andi Jusdi |author12=Abdullah |author13=Andi Pampang Mubarak |author14=Mark W. Moore |author15=Richard G. Roberts |author16=Jian-xin Zhao |author17=David McGahan |author18=Brian G. Jones |author19=Yinika Perston |author20=Katherine Szabó |author21=M. Irfan Mahmud |author22=Kira Westaway |author23=Jatmiko |author24=E. Wahyu Saptomo |author25=Sander van der Kaars |author26=Rainer Grün |author27=Rachel Wood |author28=John Dodson |author29=Michael J. Morwood |year=2018 |title=A reassessment of the early archaeological record at Leang Burung 2, a Late Pleistocene rock-shelter site on the Indonesian island of Sulawesi |journal=PLoS ONE |volume=13 |issue=4 |pages=e0193025 |doi=10.1371/journal.pone.0193025 |pmid=29641524 |pmc=5894965 }}</ref>
* A reassessment of the Late [[Pleistocene]] human occupation site at Leang Burung 2 ([[Sulawesi]], [[Indonesia]]), presenting new stratigraphic information and dating evidence from the site, is published by Brumm ''et al.'' (2018).<ref>{{Cite journal|author1=Adam Brumm |author2=Budianto Hakim |author3=Muhammad Ramli |author4=Maxime Aubert |author5=Gerrit D. van den Bergh |author6=Bo Li |author7=Basran Burhan |author8=Andi Muhammad Saiful |author9=Linda Siagian |author10=Ratno Sardi |author11=Andi Jusdi |author12=Abdullah |author13=Andi Pampang Mubarak |author14=Mark W. Moore |author15=Richard G. Roberts |author16=Jian-xin Zhao |author17=David McGahan |author18=Brian G. Jones |author19=Yinika Perston |author20=Katherine Szabó |author21=M. Irfan Mahmud |author22=Kira Westaway |author23=Jatmiko |author24=E. Wahyu Saptomo |author25=Sander van der Kaars |author26=Rainer Grün |author27=Rachel Wood |author28=John Dodson |author29=Michael J. Morwood |year=2018 |title=A reassessment of the early archaeological record at Leang Burung 2, a Late Pleistocene rock-shelter site on the Indonesian island of Sulawesi |journal=PLoS ONE |volume=13 |issue=4 |pages=e0193025 |doi=10.1371/journal.pone.0193025 |pmid=29641524 |pmc=5894965 }}</ref>

Revision as of 17:05, 12 September 2018

List of years in paleontology (table)
In science
2015
2016
2017
2018
2019
2020
2021
+...

This article records new taxa of fossil mammals of every kind are scheduled to be described during the year 2018, as well as other significant discoveries and events related to paleontology of mammals that are scheduled to occur in the year 2018.

Mammals in general

  • A study on the structure and origin of the braincase sidewalls of monotremes, multituberculates and therians, based on data from extant and fossil mammals and non-mammalian cynodonts, is published by Crompton et al. (2018).[1]
  • A study on changes in mammalian faunal composition and structure during the earliest Paleogene biotic recovery, based on data from four localities in the Hell Creek Formation and Tullock Member of the Fort Union Formation (Montana, United States), will be published by Smith et al. (2018).[2]
  • A study on the mammalian extinction selectivity, continental body size distributions, and taxonomic diversity over five time periods spanning the past 125,000 years is published by Smith et al. (2018), who report evidence indicating that larger species of mammals were at greater risk of extinction following the global expansion of hominins over the late Quaternary, and that the degree of size-selectivity of mammalian extinctions in this period was unprecedented in the past 65 million years of mammalian evolution.[3]
  • A study on the relationship between extinctions of insular endemic mammal species in the Late Pleistocene and Holocene and their body mass, the size of the island and the first human arrival to the archipelago is published by Kouvari & van der Geer (2018).[4]
  • A study on the relationship between diversification rates and climatic niche evolution in mammals is published by Castro-Insua et al. (2018).[5]
  • A study on the dietary isotopic signatures recorded in tissues of herbivorous mammals, focusing on extant and fossil sloths, and evaluating the hypothesis that a single isotope enrichment pattern holds for all herbivorous mammals, is published by Tejada-Lara et al. (2018).[6]

Metatherians

  • A study on the changes of the global diversity of metatherians through time based on a new dataset of metatherian fossil occurrences is published by Bennett et al. (2018).[7]
  • A study on the morphological diversity of sparassodonts and its implications for the structure of the terrestrial carnivore guild from the middle Cenozoic of South America is published by Croft et al. (2018).[8]
  • Description of a partial skull of Allqokirus australis from the Paleocene Santa Lucía Formation (Bolivia) and a study on the phylogenetic relationships of this species is published by de Muizon et al. (2018), who name a new metatherian superorder Pucadelphyda.[9]
  • A study on the age of thylacine and Tasmanian devil fossils from the mainland Australia and their implications for estimating the time of extinction in mainland Australia for both species is published by White et al. (2018).[10]
  • A study on the phylogeography and demographic history of the thylacine during the late Pleistocene and Holocene is published by White, Mitchell & Austin (2018).[11]
  • A study on the phylogeography and demographic history of the Tasmanian devil across southern Australia over the last ~30,000 years, based on genomes from 202 devils representing the extinct mainland and the extant Tasmanian populations, is published by Brüniche–Olsen et al. (2018).[12]
  • A study on the phylogenetic relationships of Palaeopotorous priscus is published by den Boer & Kear (2018), who interpret this taxon as a probable non-macropodoid macropodiform marsupial.[13]
  • Revision of the taxonomic status of fossil kangaroo relatives attributed to the genera Ganawamaya and Nambaroo is published by Butler et al. (2018), who also describe new fossil material of Ganawamaya couperi (formerly assigned to the genus Nambaroo), Ganawamaya acris and G. aediculis.[14]
Name Novelty Status Authors Age Unit Location Notes Images

Australogale[15]

Gen. et sp. nov

In press

Engelman, Anaya & Croft

Miocene (Serravallian)

Honda Group

 Bolivia

A member of Sparassodonta. Genus includes new species A. leptognathus.

Austropediomys[16]

Gen. et sp. nov

Valid

Carneiro, Oliveira & Goin

Itaboraian

Itaboraí Formation

 Brazil

A member of Marsupialiformes belonging to the order Archimetatheria and the superfamily Pediomyiodea. The type species is A. marshalli.

Coloradolops[17]

Gen. et sp. nov

Valid

Chornogubsky et al.

Middle Eocene

Quebrada de Los Colorados Formation

 Argentina

A member of Bonapartherioidea belonging to the family Prepidolopidae. Genus includes new species C. cardonensis.

Fumodelphodon[18]

Gen. et sp. nov

Valid

Cohen

Late Cretaceous (Turonian)

Straight Cliffs Formation

 United States
( Utah)

A member of Stagodontidae. Genus includes new species F. pulveris.

Herpetotherium tabrumi[19]

Sp. nov

Valid

Korth

Late Paleogene (Chadronian)

 United States
( Montana
 Nebraska
 North Dakota)

Hoodootherium[18]

Gen. et sp. nov

Valid

Cohen

Late Cretaceous (Turonian)

Straight Cliffs Formation

 United States
( Utah)

A member of Stagodontidae. Genus includes new species H. praeceps.

Miminipossum[20]

Gen. et sp. nov

Valid

Archer et al.

Miocene

Riversleigh World Heritage Area
Wipajiri Formation

 Australia

A member of Phalangerida belonging to the new family Miminipossumidae. The type species is M. notioplanetes.

Perameles papillon[21]

Sp. nov

Valid

Travouillon & Phillips

Holocene

Nullarbor Plain

 Australia

A long-nosed bandicoot.

Rhizophascolonus ngangaba[22]

Sp. nov

Valid

Brewer et al.

Miocene

Riversleigh site

 Australia

A wombat.

Varalphadon janetae[23]

Sp. nov

Valid

Carneiro

Late Cretaceous (late Cenomanian to early Coniacian)

Naturita Formation
Straight Cliffs Formation

 United States
( Utah)

Possibly a member of Sparassodonta.

Eutherians

  • A study on the causes of the increase of body size in aquatic mammals, based on data on the body masses of living and fossil mammals, is published by Gearty, McClain & Payne (2018).[24]
  • A study on large mammal burrows from the Upper Miocene Cerro Azul Formation (Argentina), aiming to infer their likely producers and to interpret the taphonomic processes involved in the preservation of the burrow casts, is published by Cardonatto & Melchor (2018).[25]
  • A study on the evolution and interconnectedness of the mammal faunas living in the Old World savannas in the Neogene is published by Kaya et al. (2018).[26]
  • A study on the changes of the species richness of mammals from the Iberian Peninsula between 15 and 2 million years ago, and on the modulating role of different factors influencing that species richness, is published by Cantalapiedra, Domingo & Domingo (2018).[27]
  • A study on changes in local climate and habitat conditions in central Spain in a period from 9.1 to 6.3 million years ago, and on the diet and ecology of large mammals from this area in this time period as indicated by tooth wear patterns, is published by De Miguel, Azanza & Morales (2018).[28]
  • Faith (2018) evaluates the aridity index, a widely used technique for reconstructing local paleoclimate and water deficits from oxygen isotope composition of fossil mammal teeth, arguing that in some taxa altered drinking behavior (influencing oxygen isotope composition of teeth) might have been caused by dietary change rather than water deficits.[29][30][31]
  • A revision of the mammal fauna from the Miocene site of Bukwa (Uganda) and a study on the age of this fauna is published by Cote et al. (2018), who interpret their finding as indicating that a significant faunal turnover may have occurred in East Africa between 20 and 19 million years ago.[32]
  • A study on changes of the species- and genus-level diversity of large mammals in the Omo-Turkana Basin (eastern Africa) in the Pliocene and Pleistocene will be published by Du & Alemseged (2018).[33]
  • The primary description and analysis of the so called GD A faunal assemblage from the Gondolin Cave (South Africa) is published by Adams (2018).[34]
  • A study on the diet of large mammals from the Pleistocene sediments at Olduvai Gorge (Tanzania), as indicated by tooth wear and stable isotope data from fossil teeth, is published by Uno et al. (2018).[35]
  • A study on the diet of the most abundant ungulate taxa from the Oldowan site HWK EE (Olduvai Gorge, Tanzania), as indicated by tooth wear and stable isotope analyses, is published by Rivals et al. (2018).[36]
  • Description of new mammal and fish remains from the Olduvai Gorge site, comparing the mammal assemblage from this site to the present mammal community of Serengeti, and a study on their implications for reconstructing the paleoecology of this site at ∼1.7–1.4 million years ago, is published by Bibi et al. (2018).[37]
  • A study on the distance of seed dispersal by extant and extinct mammalian frugivores and on the impact of the extinction of Pleistocene megafauna on seed dispersal is published by Pires et al. (2018).[38]
  • A study on the diet and habitat of ungulates from the Middle Pleistocene site of Fontana Ranuccio (Italy) as indicated by their tooth wear is published by Strani et al. (2018).[39]
  • A study on the response of large ungulates to the palaeoenvironmental changes that occurred at the passage between the Gelasian and Calabrian in the Italian Peninsula, based on the dental wear patterns and hypsodonty of the ungulates from the fossil assemblage of Olivola (Aulla, Italy), is published by Strani et al. (2018).[40]
  • A study on the ungulate and carnivoran carrying capacity of the late Early and early Middle Pleistocene ecosystems of Europe is published by Rodríguez & Mateos (2018).[41]
  • A study on the changes of vegetation in the temperate zone of Asia during an interval containing the Mid-Pleistocene Transition, ~1.2–0.7 million years ago, as indicated by pollen data from a drilling core from the North China Plain, as well as on their effect on the large mammal fauna is published by Xinying et al. (2018).[42]
  • A study evaluating how the mammoth steppe ecosystem with its expected low vegetation productivity managed to support a high diversity and density of large mammalian herbivores during the Last Glacial Maximum is published by Zhu et al. (2018).[43]
  • A study modeling spatial and temporal patterns of habitat suitability for 24 megafauna species and Homo sapiens in the Late Pleistocene in Eurasia is published by Carotenuto et al. (2018), who state that extinct herbivorous megafauna species were consistently rare within habitat patches optimal for humans.[44]
  • A study on the morphology of the skulls of extant and extinct elephants and hippos, evaluating the hypothesis that the skulls of extinct island dwarf members of these groups were pedomorphic, is published by van der Geer et al. (2018).[45]
  • The first evidence of bears scavenging on horses in the South American fossil record is reported from the Pleistocene deposits of the Gruta do Urso cave (Brazil) by Avilla et al. (2018).[46]

Xenarthrans

  • A study on the species distribution of 15 fossil xenarthrans from the late Pleistocene of South America will be published by Varela et al. (2018).[47]
  • A study on the relationship between humerus shape and the modes of exploring substrate among extant and fossil members of Pilosa will be published by de Oliveira & Santos (2018).[48]
  • A study on the microwear patterns in the teeth of the Oligocene sloths Orophodon hapaloides and Octodontotherium grande, as well its implications for inferring the diet of these taxa, will be published by Kalthoff & Green (2018).[49]
  • A study on the anatomy of the ear region in Glossotherium robustum and on the evolution of the inner ear anatomy in the xenarthrans is published by Boscaini et al. (2018).[50]
  • A study on the internal morphology of the skull of Glossotherium robustum will be published by Boscaini et al. (2018).[51]
  • A skull of a megatheriid sloth belonging to a member or a relative of the genus Proeremotherium is described from the Pliocene San Gregorio Formation (Venezuela) by Carlini et al. (2018).[52]
  • A study on the feet anatomy of the fossil sloths Megatherium and Eremotherium, as well as its implications for inferring the degree to which their feet were habitually inverted, will be published by Toledo et al. (2018).[53]
  • New remains (skull and humeri) of Megathericulus patagonicus are described from the middle Miocene fossiliferous locality of Quebrada Honda (Bolivia) by Brandoni et al. (2018).[54]
  • A study on the bone structure of the skull of Thalassocnus and on the evolution of bone mass increase in extinct aquatic sloths is published by Amson, Billet & de Muizon (2018).[55]
  • A study on the phylogenetic relationships of Mylodon darwinii, based on mitogenomic and nuclear data, is published by Delsuc et al. (2018).[56]
  • A study on the impact of climate changes on the distribution of armadillos as indicated by fossil record will be published by Soibelzon (2018).[57]
  • A study on the morphology and histology of glyptodont osteoderms from the Gruta do Urso cave (Brazil), representing the first juvenile specimen of Glyptotherium described from the Late Pleistocene of South America, is published by Luna et al. (2018).[58]
  • Taxonomic revision of glyptodonts from Uruguay belonging to the tribe Plohophorini is published by Toriño & Perea (2018).[59]
  • A study comparing the morphology of South American species of Glyptodon and Glyptotherium, in order to identify diagnostic differences and potential synapomorphies, is published by Zurita et al. (2018).[60]
  • A study on the anatomy of the hyoid apparatus of two glyptodontid specimens from Lujanian sediments of the Pampean Region (Argentina), assigned to the genus Panochthus, is published by Zamorano et al. (2018).[61]
Name Novelty Status Authors Age Unit Location Notes Images

Neoglyptatelus uruguayensis[62]

Sp. nov

Valid

Fernicola et al.

Late Miocene

Camacho Formation

 Uruguay

A member of Cingulata.

Pattersonocnus[63]

Gen. et sp. nov

Valid

Rincón et al.

Late Miocene

Urumaco Formation

 Venezuela

A sloth belonging to the family Megalonychidae. The type species is P. diazgameroi.

Urumacocnus[63]

Gen. et sp. nov

Valid

Rincón et al.

Late Miocene

Urumaco Formation

 Venezuela

A sloth belonging to the family Megalonychidae. The type species is U. urbanii.

Xibalbaonyx microcaninus[64]

Sp. nov

Valid

Stinnesbeck, Frey & Stinnesbeck

Late Pleistocene

 Mexico

A ground sloth belonging to the family Megalonychidae.

Afrotherians

  • A study on the anatomy and phylogenetic relationships of the elephant shrew Chambius kasserinensis based on known and newly described fossil remains from the Eocene of Tunisia is published by Tabuce (2018).[65]
  • Description of the anatomy of middle and inner ears of the golden mole Namachloris arenatans from the Palaeogene of Namibia is published by Mason, Bennett & Pickford (2018).[66]
  • A method to estimate the body mass of extinct proboscideans on the basis of skull remains is presented by Jukar, Lyons & Uhen (2018).[67]
  • A study on the evolution of the cheek teeth displacement mechanism in elephantiform proboscideans is published by Sanders (2018).[68]
  • Phytoliths preserved in the dental calculus of specimens of Gomphotherium connexum and Gomphotherium steinheimense from the Miocene Halamagai Formation (northern Junggar Basin, China) are described by Wu et al. (2018), who interpret their findings as indicating that G. connexum was an obligate browser or a mixed feeder, while G.steinheimense may have had a more grass-dominated feeding preference, and was the earliest-known proboscidean with a predominantly grazing habit.[69]
  • Mothé, Ferretti & Avilla (2018) support the validity of Notiomastodon as a genus separate from Stegomastodon, arguing that members of the genus Stegomastodon were absent from South America.[70]
  • A study on the diet and habitat of Notiomastodon platensis from Central Chile is published by González-Guarda et al. (2018).[71]
  • A study on the diet of the Columbian mammoths, pygmy mammoths and American mastodons as indicated by tooth wear is published by Smith & Desantis (2018).[72]
  • A study on permafrost‐preserved Siberian woolly mammoths, aiming to measure testosterone in the hair samples of the studied specimens, will be published by Koren et al. (2018).[73]
  • A study on the evolutionary history of the family Elephantidae based on 14 genomes from extant and fossil elephantids and from the American mastodon is published by Palkopoulou et al. (2018).[74]
Name Novelty Status Authors Age Unit Location Notes Images

Promicrogale[75]

Gen. et sp. nov

Valid

Pickford

Early Miocene

Elisabeth Bay Formation

 Namibia

A tenrec. The type species is P. namibiensis.

Sobrarbesiren[76]

Gen. et sp. nov

Valid

Díaz-Berenguer et al.

Eocene (Lutetian)

Sobrarbe Formation

 Spain

A sirenian of uncertain phylogenetic placement. The type species is S. cardieli.

Stylolophus[77]

Gen. et sp. nov

Valid

Gheerbrant, Schmitt & Kocsis

Eocene (Ypresian)

Ouled Abdoun Basin

 Morocco

An early member of Embrithopoda. The type species is S. minor.

Bats

  • A review of the distribution of sesamoids in extant bats, as well as in Eocene bats Onychonycteris finneyi and Icaronycteris index, is published by Amador et al. (2018).[78]
  • A study on the phylogeny of extant and fossil short-faced bats (leaf-nosed bats belonging to the subfamily Stenodermatinae and the subtribe Stenodermatina) and on the ancestral distributions of the group, evaluating whether this group was more likely to originate on Antilles or on the American mainland, is published by Tavares et al. (2018).[79]
Name Novelty Status Authors Age Unit Location Notes Images

Anatolianycteris[80]

Gen. et sp. nov

Valid

Jones et al.

Eocene (late Lutetian)

Uzunçarşidere Formation

 Turkey

A member of the family Palaeochiropterygidae. The type species is A. insularis.

Mops kerio[81]

Sp. nov

In press

Gunnell & Manthi

Pliocene

Kanapoi site

 Kenya

A species of Mops.

Mops turkwellensis[81]

Sp. nov

In press

Gunnell & Manthi

Pliocene

Kanapoi site

 Kenya

A species of Mops.

Pteronotus trevorjacksoni[82]

Sp. nov

Valid

Van Den Hoek Ostende, Van Oijen & Donovan

Late Pleistocene

 Jamaica

A species of Pteronotus.

Rousettus pattersoni[81]

Sp. nov

In press

Gunnell & Manthi

Pliocene

Kanapoi site

 Kenya

A species of Rousettus.

Saccolaimus kenyensis[81]

Sp. nov

In press

Gunnell & Manthi

Pliocene

Kanapoi site

 Kenya

A species of Saccolaimus.

Turkanycteris[81]

Gen. et sp. nov

In press

Gunnell & Manthi

Pliocene

Kanapoi site

 Kenya

A very large fruit bat, larger than all extant fruit bats other than some species of Pteropus and Hypsignathus. Genus includes new species T. harrisi.

Vulcanops[83]

Gen. et sp. nov

Valid

Hand et al.

Early Miocene

Bannockburn Formation

 New Zealand

A New Zealand short-tailed bat. The type species is V. jennyworthyae.

Odd-toed ungulates

  • Tooth anomalies in two juvenile specimens of the Miocene rhinoceros Prosantorhinus germanicus are described by Böhmer & Rössner (2018), who discuss probable causes of these anomalies.[84]
  • A jaw of Stephanorhinus kirchbergensis is described from the Mus Khaya locality on the Yana River in the Sakha Republic (Russia) by Shpansky & Boeskorov (2018), representing the northernmost occurrence of this species; the authors also interpret Coelodonta jacuticus as the junior synonym of the woolly rhinoceros (Coelodonta antiquitatis).[85]
  • A study on the morphology of the postcranial skeleton of Teleolophus, based on new remains from the Eocene of China, is published by Bai, Wang & Meng (2018).[86]
  • A study on the digit reduction in the evolution of horses is published by Solounias et al. (2018).[87]
  • A study testing for the presence of broad-scale habitat partitioning in fossil horses of North America is published by Parker, McHorse & Pierce (2018).[88]
  • A revised diagnosis and a description of the anatomy of the Miocene hipparionine species Sivalhippus ptychodus and S. platyodus from China is published by Sun et al. (2018).[89]
  • A study on the ontogeny (mineralization, eruption, and replacement patterns) of postcanine teeth of members of the genus Hipparion from Cerro de los Batallones (Spain) is published by Domingo et al. (2018).[90]
  • Review of fossils of members of the family Equidae from the Pleistocene site of lac Karâr (Algeria) is published by Sam (2018).[91]
  • A study on the diet and habitat of Pleistocene members of the genera Equus and Hippidion from southern United States, Mexico and South America, as indicated by carbon and oxygen isotopic data, will be published by Pérez-Crespo et al. (2018).[92]
  • A study evaluating how the geographic distribution of horses changed through time in the Late Pleistocene and Holocene, based on paleontological and archeological horse finds across the whole of Eurasia evaluated in association with paleoclimatic and paleoenvironmental reconstructions for the Late Quaternary, is published by Leonardi et al. (2018).[93]
Name Novelty Status Authors Age Unit Location Notes Images

Ardynia ordosensis[94]

Sp. nov

Valid

Bai, Wang & Zhang

Late Eocene

 China

A member of the family Hyracodontidae.

Chilotherium licenti[95]

Sp. nov

Valid

Sun, Li & Deng

Late Miocene

 China

Danjiangia lambdodon[96]

Sp. nov

Bai, Wang & Meng

Earliest Eocene

Hengyang Basin

 China

A member of the family Brontotheriidae.

Epimanteoceras mae[97]

Sp. nov

Valid

Li

Eocene (Irdinmanhan)

Üqbulak Formation

 China

A member of the family Brontotheriidae.

Erihippus[96]

Gen. et sp. nov

Bai, Wang & Meng

Earliest Eocene

Lingcha Formation

 China

A member of the family Equidae. The type species is E. tingae.

Forstercooperia ulanshirehensis[98]

Sp. nov

Valid

Wang et al.

Eocene

Irdin Manha Formation
Ulan Shireh Formation

 China

Hispanotherium wushanense[99]

Sp. nov

Valid

Sun et al.

Miocene

Wushan Subbasin

 China

Maobrontops[100]

Gen. et sp. nov

Valid

Averianov et al.

Late Eocene

Youganwo Formation

 China

A member of the family Brontotheriidae. The type species is M. paganus.

Sellamynodon[101]

Gen. et comb. nov

Valid

Tissier et al.

Late Eocene or Early Oligocene

 Romania

A member of the family Amynodontidae. The type species is "Cadurcodon" zimborensis Codrea & Şuraru (1989).

Shanxihippus[102]

Gen. et comb. nov

Valid

Bernor et al.

Late Miocene

 China

A member of the family Equidae belonging to the tribe Hipparionini. The type species is "Hipparion" dermatorhinum Sefve (1927).

Even-toed ungulates

  • A study evaluating whether tooth measurements of the kind typically used in the systematics of Merycoidodontoidea can diagnose between related, similarly-sized even-toed ungulates is published by Emery-Wetherell & Davis (2018).[103]
  • Description of the fossil material of the camel species Camelus thomasi from the Pleistocene locality of Tighennif (Algeria) and a study on the phylogenetic relationships of this species is published by Martini & Geraads (2018).[104]
  • New specimen of the fossil peccary Parachoerus carlesi will be described from the Upper Pleistocene of the Chaco Province of Argentina by Gasparini et al. (2018), representing the most complete fossil material of a member this species reported so far, and providing new information on the morphology of the species and the environment it lived in.[105]
  • A study on the diet of extinct peccaries in Florida from the late Miocene throughout the Pleistocene, as indicated by tooth microwear and stable carbon isotopes, is published by Bradham et al. (2018).[106]
  • A description of the skull anatomy of the fossil suid Nyanzachoerus jaegeri based on new fossil material and a study on the phylogenetic relationships of the species will be published by Reda, Lazagabaster & Haile-Selassie (2018).[107]
  • New fossil suid specimens, providing new information on the classification and relationships of the Miocene Suinae from China, will be described from the latest Miocene site of Shuitangba (Zhaotong Basin, China) by Hou et al. (2018).[108]
  • Partial skull of a suid assigned to the genus Metridiochoerus is described from the Malapa Fossil Site (South Africa) by Lazagabaster et al. (2018).[109]
  • A study on the evolution of hypsodonty in ruminants as indicated by phylogeny of ruminants, estimated ancestral ruminant diets and habitats, and fossil record of grasslands is published by Toljagić et al. (2018).[110]
  • A study comparing the exclusivity and magnitude of changes in diversification rates during the evolution of ruminants and other lineages of placental mammals is published by Rossi, Mello & Schrago (2018).[111]
  • Fossils of the chevrotain Dorcatherium crassum, including a skull and teeth remains, are described from the Miocene (Langhian) of the Faluns Auger quarry (Contres, France) by Mennecart et al. (2018).[112]
  • Croitor, Sanz & Daura (2018) report the findings from a morphological and demographic analysis of remains of the endemic deer Haploidoceros mediterraneus from the Late Pleistocene of the Cova del Rinoceront (Spain).[113]
  • A study on the feeding habits of Morenelaphus as indicated by tooth enamel microwear is published by Rotti et al. (2018).[114]
  • A study on the dietary plasticity of specimens of Eucladoceros ctenoides from eight middle and late Villafranchian localities in Europe, as indicated by tooth microwear, is published by Berlioz et al. (2018).[115]
  • Antler remains of the wapiti (Cervus canadensis) are described from the Late Paleolithic site of Climăuți II (Moldova) by Croitor & Obada (2018), confirming the presence of wapiti in the Late Pleistocene of western Eurasia.[116]
  • Pfeiffer-Deml (2018) raises fossil fallow deer Dama dama geiselana to the rank of a separate species Dama geiselana, and compares its antler and skeletal characteristics with other fossil and recent fallow deers.[117]
  • Description of new specimens of Sardomeryx oschiriensis from the Miocene (Burdigalian) of Sardinia (Italy) and a study on the phylogenetic relationships of this species will be published by Mennecart et al. (2018).[118]
  • Description of new fossils of Propalaeoryx stromeri from the Miocene of Namibia, redescription of the skull anatomy of Propalaeoryx and a study on the phylogenetic relationships of this taxon is published by Sánchez et al. (2018).[119]
  • A study on the dietary preferences of extant and fossil members of the family Giraffidae as indicated by teeth microwear is published by Merceron, Colyn & Geraads (2018).[120]
  • Giraffe tracks are described from the Pleistocene Waenhuiskrans Formation (Bredasdorp Group, South Africa) by Helm et al. (2018), increasing known historical range of giraffes.[121]
  • A study on the diet and habitat of Leptomeryx from the Eocene (Uintan) Yolomécatl Formation (Mexico) as indicated by tooth enamel carbon and oxygen isotopic relationships will be published by Ferrusquía-Villafranca et al. (2018).[122]
  • A study on the dietary preferences of members of the tribe Tragelaphini from the Plio-Pleistocene Shungura Formation (Lower Omo Valley, Ethiopia) as indicated by their tooth wear is published by Blondel et al. (2018).[123]
  • Description of the late Miocene gazelle fossils from the Qingyang area (Gansu, China), and a review of the taxonomy of gazelle species known from this area, is published by Li et al. (2018).[124]
  • A study on the impact of climate changes on the evolution of body size of members of the genus Bison based on the data from extant and fossil bisons is published by Martin, Mead & Barboza (2018).[125]
  • A study on the dietary preference and habitat use of three Mexican samples of Bison antiquus, as indicated by tooth wear, will be published by Díaz-Sibaja et al. (2018).[126]
  • A study evaluating when the island of Sulawesi (Indonesia) gained its modern shape and size, and determining the timings of diversification of the three largest endemic mammals on the island (the babirusa, the Celebes warty pig and the anoa) is published by Frantz et al. (2018).[127]
  • Putative helohyids Pakkokuhyus and Progenitohyus are transferred to the family Dichobunidae by Ducrocq (2018).[128]
Name Novelty Status Authors Age Unit Location Notes Images

Bachitherium thraciensis[129]

Sp. nov

Valid

Mennecart et al.

Eocene (latest Bartonian or early Priabonian)

 Bulgaria

An early ruminant belonging to the group Tragulina and the family Bachitheriidae.

Candiacervus devosi[130]

Sp. nov

Valid

Van der Geer

Late Pleistocene

 Greece

An Old World deer.

Candiacervus listeri[130]

Sp. nov

Valid

Van der Geer

Late Pleistocene

 Greece

An Old World deer.

Candiacervus reumeri[130]

Sp. nov

Valid

Van der Geer

Late Pleistocene

 Greece

An Old World deer.

"Dorcatherium" namaquensis[131]

Sp. nov

Valid

Sánchez et al.

Middle Miocene

 Namibia

A chevrotain.

Kubanochoerus parvus[132]

Sp. nov

In press

Hou & Deng

Latest Middle or earliest Late Miocene

 China

A member of the family Suidae belonging to the subfamily Listriodontinae.

Megaloceros matritensis[133]

Sp. nov

In press

Van der Made

Middle Pleistocene

 Spain

Paenanthracotherium[134]

Gen. et sp. et comb. nov

Valid

Scherler, Lihoreau & Becker

Oligocene

 France
 Germany
 Pakistan
 Romania
  Switzerland

An anthracotheriine hippopotamoid. The type species is P. bergeri; genus also includes "Anthracotherium" hippoideum Rütimeyer (1857) and "Brachyodus" strategus Forster-Cooper (1913).

Parmularius maasaicus[37]

Sp. nov

Valid

Bibi et al.

Pleistocene

Olduvai Gorge site

 Tanzania

A member of the family Bovidae belonging to the tribe Alcelaphini.

Stryfnotherium[135]

Gen. et sp. nov

Valid

Kostopoulos & Soubise

Late Miocene

 Greece

A member of the family Bovidae. Genus includes new species S. exophthalmon.

Cetaceans

  • A study assessing the lumbar mobility in archaeocetes is published by Bebej & Smith (2018).[136]
  • A study on the anatomy of the auditory region of the skull of protocetids as indicated by fossils from the Eocene of Togo is published by Mourlam & Orliac (2018).[137]
  • A study on the teeth complexity across fossil and living cetaceans, attempting to identify a trend toward dental simplicity through the Neogene, is published by Peredo, Peredo & Pyenson (2018).[138]
  • A quantitative analysis and a study on the evolution of cranial telescoping (sliding of facial bones over each other, in much the same way as long sections of telescope slide over shorter sections) in toothed whales is published by Churchill et al. (2018).[139]
  • A study on the morphology of the bony labyrinth in extant and fossil toothed whales is published by Costeur et al. (2018), who interpret their findings as indicating that the bony labyrinth provides key information both about phylogeny and habitat preferences of members of this group of cetaceans.[140]
  • Isolated teeth resembling tooth taxon Phococetus vasconum are described from the Pungo River Formation (North Carolina, United States) by Boessenecker (2018), who also notes their similarities to the teeth of Inticetus vertizi, and suggests that Phococetus may be an Inticetus-like, large heterodont toothed whale.[141]
  • A study on the anatomy and phylogenetic relationships of Phoberodon arctirostris will be published by Viglino et al. (2018).[142]
  • A study on the life history and ecology of Neogene members of Physeteroidea known from the Lee Creek Mine (North Carolina, United States) based on the examination of their teeth is published by Gilbert, Ivany & Uhen (2018).[143]
  • Description of postcranial remains of the stem-beaked whale Messapicetus gregarius from the Miocene (Tortonian) of Peru is published by Ramassamy et al. (2018), who also propose a reconstruction of the musculature of the neck and forelimb of the species.[144]
  • An almost complete skull of Llanocetus denticrenatus is described from the Eocene La Meseta Formation (Antarctica) by Fordyce & Marx (2018), who also study the phylogenetic relationships and likely feeding strategy of this species, as well as its implications for inferring the origin of baleen and gigantism in baleen whales.[145]
  • Partial periotic bone of a member of the genus Caperea is described from the latest Miocene of southern Australia by Marx et al. (2018), representing the oldest record of this genus reported so far.[146]
  • A study on the anatomy of cochleae of extant and extinct cetaceans, the relationships of cochlear shape and the frequency ranges heard by cetaceans, and their implications for determining the occurrence of very low frequency and infrasonic hearing in fossil baleen whales is published by Ritsche et al. (2018).[147]
  • Oxygen-isotope analysis of a whale barnacle specimen collected from early Pleistocene deposits of Apulia (Italy) is published by Collareta et al. (2018), who interpret their findings as indicating that the barnacle lived on a cetacean that seasonally migrated towards high-latitude areas outside the Mediterranean.[148]
Name Novelty Status Authors Age Unit Location Notes Images

Aondelphis[149]

Gen. et sp. nov

Valid

Viglino et al.

Early Miocene

Gaimán Formation

 Argentina

A member of Platanistoidea. The type species is A. talen.

Eschrichtius akishimaensis[150]

Sp. nov

Valid

Kimura, Hasegawa & Kohno

Early Pleistocene

 Japan

A relative of the gray whale.

Khoikhoicetus kergueleni[151]

Sp. nov

Valid

Lambert et al.

Uncertain, possibly Miocene

Seafloor 370 km SWW to Kerguelen Islands

A beaked whale belonging to the subfamily Hyperoodontinae.

Kwanzacetus[152]

Gen. et sp. nov

Valid

Lambert et al.

Late Miocene

 Angola

A member of the family Iniidae. The type species is K. khoisani.

Macrosqualodelphis[153]

Gen. et sp. nov

Valid

Bianucci et al.

Miocene (Burdigalian)

Chilcatay Formation

 Peru

A member of the family Squalodelphinidae. The type species is M. ukupachai.

Salishicetus[154]

Gen. et sp. nov

Valid

Peredo & Pyenson

Late Oligocene

Lincoln Creek Formation

 United States
( Washington)

A member of the family Aetiocetidae. The type species is S. meadi.

Taikicetus[155]

Gen. et sp. nov

Valid

Tanaka, Ando & Sawamura

Middle Miocene

Hikatagawa Formation

 Japan

A cetotheriid-like baleen whale. The type species is T. inouei.

Tlaxcallicetus[156]

Gen. et sp. nov

Valid

Hernández Cisneros

Late Oligocene

El Cien Formation

 Mexico

A member of Chaeomysticeti of uncertain phylogenetic placement. The type species is T. guaycurae.

Toipahautea[157]

Gen. et sp. nov

Valid

Tsai & Fordyce

Oligocene (Chattian)

Kokoamu Greensand

 New Zealand

An archaic baleen whale. The type species is T. waitaki.

Wimahl[158]

Gen. et sp. nov

Valid

Peredo, Uhen & Nelson

Early Miocene

Astoria Formation

 United States
( Washington)

A member of the family Kentriodontidae. Genus includes new species W. chinookensis.

Carnivorans

  • A systematic examination of members of the family Canidae from the Hemphillian Mehrten Formation (California, United States) is published by Balisi et al. (2018).[159]
  • A study evaluating whether body size and the occurrence of skull and teeth traits related to the dietary specialization were correlated with species duration and locality coverage in North American canids over 40 million years of their evolution is published by Balisi, Casey & Van Valkenburgh (2018).[160]
  • A study on the teeth microwear in extant gray wolves and coyotes, and its implications for dietary studies of extant and fossil canids, is published by Tanis, DeSantis & Terry (2018).[161]
  • Description of a sample of coprolites from the Upper Miocene Mehrten Formation (California, United States), likely produced by Borophagus parvus, and a study on their implications for inferring the diet of this species, is published by Wang et al. (2018).[162]
  • Revision of the taxonomy and relative age of the Javanese canid fossils will be published by van der Geer, Lyras & Volmer (2018).[163]
  • A study on the phylogenetic relationships of extant and fossil members of the subfamily Caninae is published by Zrzavý et al. (2018).[164]
  • Revision of fossils attributed to the species Canis variabilis and a study on the morphotype variability of the Pleistocene members of the genus Canis is published by Jiangzuo et al. (2018), who considered C. variabilis to be a subspecies of Canis mosbachensis.[165]
  • A study on the morphological diversity of the limb bones of fossil and modern North American gray wolves is published by Tomiya & Meachen (2018).[166]
  • A study on the morphological and morphometric variability of late Pleistocene gray wolves from Avetrana (Italy) in comparison to other populations from northern and southern Italy, as well as from other localities in Europe, is published by Mecozzi & Bartolini Lucenti (2018).[167]
  • A study on the evolutionary history of the domestic dogs living in the Americas before the arrival of European colonists, based on data from sequenced mitochondrial and nuclear genomes from ancient North American and Siberian dogs from time frames spanning ~9000 years, is published by Ní Leathlobhair et al. (2018).[168]
  • A study on the age of dingo bones from Madura Cave on the Nullarbor Plain (Australia), and its implications for inferring the likely rate of dingo spread throughout Australia from their point of arrival, is published by Balme, O’Connor & Fallon (2018).[169]
  • A study on the diet of Agriotherium africanum from the South African fossil site of Langebaanweg, as indicated by tooth microwear, will be published by Stynder et al. (2018).[170]
  • The complete mitochondrial genome of a ∼22,000-year-old giant panda specimen from the Cizhutuo Cave (Leye County, Guangxi, China) is sequenced by Ko et al. (2018).[171]
  • A study on the age of the fossil remains of short-faced bears (Arctodus simus) and brown bears (Ursus arctos) from Pellucidar Cave (Vancouver Island, Canada) is published by Steffen & Fulton (2018).[172]
  • A study on the living conditions of Pleistocene bears (belonging to the species Ursus ingressus) from Jaskinia Niedźwiedzia (Bear Cave) in Kletno (Poland) as indicated by the frequency of Harris lines in their bones is published by Nowakowski (2018).[173]
  • A study on the diet of the cave bears from four MIS 3 sites in the Carpathian Mountains, based on isotopic data, is published by Robu et al. (2018).[174]
  • A study on the feedings preferences and timing of extinction of cave bears in Mediterranean Europe based on data from two Paleolithic cave bear sites in northeastern Italy (Paina Cave and Trene Cave) will be published by Terlato et al. (2018).[175]
  • Multifold coverage genomic data from four Late Pleistocene cave bears is presented by Barlow et al. (2018), who report that cave bears hybridized with brown bears during the Pleistocene, and that segments of cave bear DNA still persist in the genomes of living brown bears.[176]
  • A study on the dynamics of lineage diversification and diversity of body mass and length in the evolution of musteloid carnivorans based on data from extant and fossil taxa is published by Law, Slater & Mehta (2018).[177]
  • A study estimating the body mass of the fossil procyonids Cyonasua, Parahyaenodon and Tetraprothomo is published by Tarquini et al. (2018).[178]
  • Fossils of members of the genera Nasua and Procyon are described from the Marplatan stage of the El Breal of Orocual locality (Venezuela) by Ruiz-Ramoni, Rincón & Montellano-Ballesteros (2018), representing the oldest record of these procyonids in South America reported so far.[179]
  • The first well-preserved skull of the fossil mustelid Leptarctus oregonensis is described from the Miocene Mascall Formation (Oregon, United States) by Calede, Kehl & Davis (2018).[180]
  • Femur of a member of the genus Enhydra (a relative of the sea otter) is described from the middle Pleistocene Merced Formation (California, United States) by Boessenecker (2018), representing the oldest record of Enhydra in the Pacific with robust geochronologic age control reported so far.[181]
  • New specimens of members of the genus Enaliarctos are described from the Miocene Skooner Gulch Formation (California, United States), Oligocene Yaquina Formation (Oregon, United States) and Miocene Astoria Formation (Oregon, United States) by Poust & Boessenecker (2018), extending the geographic and temporal range of the genus.[182]
  • A study on the morphology of the forelimbs of Enaliarctos mealsi and extant phocine earless seals, on the use of forelimbs to secure and tear prey by extant phocine seals, and on its implications for inferring the feeding behaviour of early pinnipeds, is published by Hocking et al. (2018).[183]
  • A study on the bone histology of Nanophoca vitulinoides will be published by Dewaele et al. (2018).[184]
  • New specimen of Ontocetus emmonsi is described from the Austin Sand Pit (Ridgeville, South Carolina, United States) by Boessenecker, Boessenecker & Geisler (2018), representing the youngest record of O. emmonsi from the Atlantic coastal plain reported so far.[185]
  • A study evaluating the ability of the extinct giant fossa to hunt large lemurs will be published by Meador et al. (2018).[186]
  • Evidence of Pleistocene hyenas preying upon small rodents is reported from the Bois Roche cave site (France) by Williams et al. (2018).[187]
  • Cougar skull is described from the Pleistocene (Ensenadan) of Argentina by Chimento & Dondas (2018), representing the first unequivocal record of the cougar prior to late Pleistocene times in South America.[188]
  • A study on the shape and the dimensions of the bony vestibular system in the inner ear of the cheetah, comparing it with the vestibular system in other extant felids and in the extinct giant cheetah (Acinonyx pardinensis) and Proailurus lemanensis, and on the evolution of the vestibular system of the cheetah is published by Grohé, Lee & Flynn (2018).[189]
  • Description of a partial skull of a large felid from the late Villafranchian site of Monte Argentario (Italy), formerly assigned to the species Panthera gombaszoegensis, is published by Cherin et al. (2018), who refer this specimen (and some other Italian materials previously referred to P. gombaszoegensis) to the species Acinonyx pardinensis.[190]
  • Description of fossils of at least four adult cave lions (Panthera spelaea) from Medvedia Cave in the Západné Tatra Mountains (Slovakia) and a study on the range and social behavior of members of this taxon is published by Sabol, Gullár & Horvát (2018).[191]
  • An exceptionally large skull of a lion, comparable to large specimens of the American lion in terms of skull length and substantially larger than known skulls of extant lions, is described from the Pleistocene of Kenya by Manthi et al. (2018).[192]
  • The northernmost fossil record of the jaguar from Argentina is reported from the late Pleistocene-early Holocene Río Bermejo Formation (Formosa Province) by Rodriguez et al. (2018).[193]
  • A study on the evolution of the morphological diversity of the mandibles of saber-toothed cats, as well as on the speciation and extinction rates in the evolution of saber-toothed cats, is published by Piras et al. (2018).[194]
  • A study on the evolution of upper canine length in the felid lineages leading to the fossil saber-toothed cats and extant clouded leopard is published by Harano & Kutsukake (2018).[195]
  • An almost complete skull of Smilodon fatalis will be described from the Pleistocene Sopas Formation (Uruguay) by Manzuetti et al. (2018), representing the first known record of the species from the eastern part of South America.[196]
  • Large carnivore footprints, probably produced by Smilodon populator, will be described from a new ichnological site from the Late Pleistocene of Buenos Aires Province (Argentina) by Agnolin et al. (2018), who name a new ichnotaxon Felipeda miramarensis.[197]
Name Novelty Status Authors Age Unit Location Notes Images

Allodesmus demerei[198]

Sp. nov

Valid

Boessenecker & Churchill

Miocene (Tortonian)

Montesano Formation

 United States
( Washington)

Allodesmus uraiporensis[199]

Sp. nov

Valid

Tonomori et al.

Middle Miocene

Okoppezawa Formation

 Japan

Auroraphoca[200]

Gen. et sp. nov

Valid

Dewaele et al.

Pliocene (Zanclean)

Yorktown Formation

 United States
( North Carolina)

An earless seal belonging to the subfamily Monachinae. The type species is A. atlantica.

Civettictis braini[201]

Sp. nov

Valid

Fourvel

Pliocene-Pleistocene transition

Kromdraai fossil site

 South Africa

A relative of the African civet.

Frisiphoca[202]

Gen. et comb. nov

Valid

Dewaele, Lambert & Louwye

Late Miocene

Probably Diest Formation

 Belgium

An earless seal belonging to the subfamily Phocinae. The type species is "Monotherium" aberratum Van Beneden (1876); genus also includes "Monotherium" affine Van Beneden (1876).

Gulo sudorus[203]

Sp. nov

Valid

Samuels, Bredehoeft & Wallace

Early Pliocene (earliest Blancan)

Gray Fossil Site

 United States
( Tennessee)

A relative of the wolverine.

Katifelis[204]

Gen. et sp. nov

Valid

Adrian, Werdelin & Grossman

Early Miocene

Lothidok Formation

 Kenya

A member of the family Felidae. The type species is K. nightingalei.

Kichechia savagei[204]

Sp. nov

Valid

Adrian, Werdelin & Grossman

Early Miocene

Lothidok Formation

 Kenya

A member of the family Viverridae belonging to the subfamily Paradoxurinae.

Leptofelis[205]

Gen. et comb. nov

In press

Salesa et al.

Late Miocene

 Spain

A member of the family Felidae belonging to the subfamily Felinae; a new genus for "Styriofelis" vallesiensis Salesa et al. (2012).

Martellictis[206]

Gen. et comb. nov

In press

Bartolini Lucenti

Pleistocene

 Austria
 France
 Italy
 Netherlands
 Slovakia

A member of the family Mustelidae. Genus includes "Mustela" ardea Gervais (1848–1852).

Meles magnus[207]

Sp. nov

Valid

Jiangzuo et al.

Early Pleistocene

 China

A badger, a species of Meles.

Nanodobenus[208]

Gen. et sp. nov

Valid

Velez-Juarbe & Salinas-Márquez

Miocene

Tortugas Formation

 Mexico

A relative of the walrus. The type species is N. arandai.

Nasua mastodonta[209]

Sp. nov

Valid

Emmert & Short

Blancan

 United States
( Florida)

A species of Nasua.

Noriphoca[202]

Gen. et comb. nov

Valid

Dewaele, Lambert & Louwye

Late Oligocene or early Miocene

Probably Bolognano Formation

 Italy

An earless seal belonging to the subfamily Monachinae. The type species is "Monotherium" gaudini (Guiscardi, 1870).

Procyon gipsoni[209]

Sp. nov

Valid

Emmert & Short

Blancan

 United States
( Florida)

A species of Procyon.

Procyon megalokolos[209]

Sp. nov

Valid

Emmert & Short

Blancan

 United States
( Florida)

A species of Procyon.

Tchadailurus[210]

Gen. et sp. nov

Valid

De Bonis et al.

Late Miocene

 Chad

A member of the family Felidae belonging to the subfamily Machairodontinae. The type species is T. adei.

Virginiaphoca[200]

Gen. et sp. nov

Valid

Dewaele et al.

Late Miocene or Pliocene (Zanclean)

Eastover Formation or Yorktown Formation

 United States
( Virginia)

An earless seal belonging to the subfamily Monachinae. The type species is V. magurai.

Rodents

Name Novelty Status Authors Age Unit Location Notes Images

Aepyocricetus[229]

Gen. et sp. nov

Valid

Li et al.

Pliocene

Zanda Basin

 China

A hamster. Genus includes new species A. liuae.

Bustrania[230]

Gen. et sp. nov

Valid

De Bruijn et al.

Eocene

 Serbia

A member of Muroidea belonging to the subfamily Pappocricetodontinae. The type species is B. dissimile.

Cholamys[231]

Gen. et sp. nov

Valid

Pérez et al.

Deseadan

Salla beds

 Bolivia

A New World porcupine. Genus includes new species C. tetralophodonta.

Eoincamys parvus[232]

Sp. nov

In press

Boivin et al.

Early Oligocene

Pozo Formation

 Peru

Possibly a member of Chinchilloidea.

Eoincamys valverdei[232]

Sp. nov

In press

Boivin et al.

Early Oligocene

Pozo Formation

 Peru

Possibly a member of Chinchilloidea.

Eumyarion gordesensis[233]

Sp. nov

Valid

Pelaez-Campomanes et al.

Early Miocene

 Turkey

Euroxenomys nanus[234]

Sp. nov

Valid

Mörs & Tomida

Early Miocene

Nakamura Formation

 Japan

A member of the family Castoridae.

Gregorymys veloxikua[235]

Sp. nov

Valid

Jiménez-Hidalgo, Guerrero-Arenas & Smith

Eocene (Chadronian)

 Mexico

A member of Geomyidae.

Karydomys strati[236]

Sp. nov

Valid

López‐Antoñanzas et al.

Miocene

Keramia Formation

 Greece

A species of Karydomys.

Kichkasteiromys[232]

Gen. et sp. nov

In press

Boivin et al.

Early Oligocene

Pozo Formation

 Peru

A member of Erethizontoidea. The type species is K. raimondii.

Lapazomys[231]

Gen. et sp. nov

Valid

Pérez et al.

Deseadan

Salla beds

 Bolivia

A caviomorph rodent related to the group Octodontoidea. Genus includes new species L. hartenbergeri.

Mayomys[232]

Gen. et sp. nov

In press

Boivin et al.

Early Oligocene

Pozo Formation

 Peru

A member of Octodontoidea of uncertain phylogenetic placement. The type species is M. confluens.

Migraveramus lavocati[231]

Sp. nov

Valid

Pérez et al.

Deseadan

Salla beds

 Bolivia

A caviomorph rodent related to the group Octodontoidea.

Mogilia[237]

Gen. et 2 sp. nov

Valid

Wessels et al.

Eocene and early Oligocene

 Serbia

A member of the family Muridae belonging to the subfamily Melissiodontinae. The type species is M. miloshi; genus also includes M. lautus.

Namaparamys[238]

Gen. et sp. nov

Valid

Mein & Pickford

Eocene (Ypresian/Lutetian)

Black Crow Limestone

 Namibia

Possibly a relative of Reithroparamys. The type species is N. inexpectatus.

Nannocricetus qiui[229]

Sp. nov

Valid

Li et al.

Pliocene

Zanda Basin

 China

A hamster. Genus includes new species A. liuae.

Neocavia pampeana[239]

Sp. nov

Valid

Madozzo-Jaén et al.

Huayquerian

Cerro Azul Formation

 Argentina

A member of Caviinae.

Orcemys[240]

Gen. et sp. nov

Valid

Martin et al.

Early Pleistocene

 Spain

A member of Arvicolidae. Genus includes new species O. giberti.

Paracricetodon gracilis[241]

Sp. nov

Valid

Van de Weerd et al.

Early Oligocene

 Serbia

A member of the family Muridae belonging to the subfamily Paracricetodontinae.

Paracricetodon stojanovici[241]

Sp. nov

Valid

Van de Weerd et al.

Late Eocene and early Oligocene

 Serbia

A member of the family Muridae belonging to the subfamily Paracricetodontinae.

Phenacomys europaeus[242]

Sp. nov

Valid

Van Kolfschoten, Tesakov & Bell

Early Pleistocene (Gelasian)

 Netherlands

A heather vole, the first known European member of the genus Phenacomys.

Protosteiromys pattersoni[231]

Sp. nov

Valid

Pérez et al.

Deseadan

Salla beds

 Bolivia

A New World porcupine.

Sallamys woodi[231]

Sp. nov

Valid

Pérez et al.

Deseadan

Salla beds

 Bolivia

A caviomorph rodent related to the group Octodontoidea.

Selvamys[232]

Gen. et sp. nov

In press

Boivin et al.

Early Oligocene

Pozo Formation

 Peru

A member of Octodontoidea of uncertain phylogenetic placement. The type species is S. paulus.

Shapajamys[232]

Gen. et sp. nov

In press

Boivin et al.

Early Oligocene

Pozo Formation

 Peru

A member of Erethizontoidea. The type species is S. labocensis.

Tarapotomys[232]

Gen. et 2 sp. nov

In press

Boivin et al.

Early Oligocene

Pozo Formation

 Peru

A member of Caviomorpha of uncertain phylogenetic placement. The type species is T. subandinus; genus also includes T. mayoensis.

Tsaukhaebmys[243]

Gen. et sp. nov

Valid

Pickford

Eocene (Ypresian/Lutetian)

Black Crow Limestone

 Namibia

A member of the family Zegdoumyidae. The type species is T. calcareus.

Tufamys[244]

Gen. et sp. nov

Valid

Pickford

Eocene (Bartonian, possibly Priabonian)

Eocliff Limestone

 Namibia

A member of Hystricognathi belonging to the new family Tufamyidae. The type species is T. woodi.

Vasseuromys tectus[245]

Sp. nov

Valid

Sinitsa & Nesin

Late Miocene

 Ukraine

A dormouse belonging to the subfamily Leithiinae.

Witenia europea[230]

Sp. nov

Valid

De Bruijn et al.

Eocene

 Serbia

A member of Muroidea belonging to the subfamily Pappocricetodontinae.

Primates

  • A study on the anatomy and phylogenetic relationships of Propotto leakeyi is published by Gunnell et al. (2018), who support George Simpson's original interpretation of this species as a strepsirrhine primate, and consider both P. leakeyi and Plesiopithecus teras to be relatives of the aye-aye.[246]
  • A study on reconstructing the jaw muscles and bite force of subfossil lemurs from Madagascar, as well as on their implications for inferring the diet of these lemurs, is published by Perry (2018).[247]
  • A study on the early evolution of North American adapids and omomyids, comparing reconstructed dietary niches of these primates and other animals from their guild to establish the nature of the competitive environment surrounding primate origins in North America, is published by Stroik & Schwartz (2018).[248]
  • Description of isolated phalanges from four early Eocene localities in Wyoming (United States), indicative of presence of grooming claws in five genera of early haplorhine primates (including Teilhardina), is published by Boyer et al. (2018).[249]
  • A study on the evolutionary history of the New World monkeys (especially on the evolution of their body mass, changes of the mean latitude of their geographic range, and species diversification rates), based on data from extant and fossil species, will be published by Silvestro et al. (2018).[250]
  • A tibia of a large-bodied arboreally-adapted Old World monkey (a member or a relative of the genus Rhinocolobus) is described from the Australopithecus afarensis-bearing Upper Laetolil Beds (∼3.7 Ma) of Laetoli (Tanzania) by Laird et al. (2018), who also study the implications of the specimen for inferring the paleoenvironment of the Upper Laetolil Beds.[251]
  • A skull of a large papionin monkey is described from the Lower Pleistocene site of Dafnero-3 (Greece) by Kostopoulos et al. (2018), who interpret the anatomy of this skull as indicating that the specimen could equally be ascribed to either the Eurasian genus Paradolichopithecus or to the East Asian Procynocephalus, and argue in favor of the synonymy of these genera.[252]
  • A study on the phylogenetic relationships of living and fossil African papionins is published by Pugh & Gilbert (2018).[253]
  • A study on the fossil members of the genus Papio from across Africa, focusing on their distinguishing features and distribution, is published by Gilbert et al. (2018).[254]
  • A study evaluating whether climatic and environmental changes were the main cause of extinction of Oreopithecus bambolii is published by DeMiguel & Rook (2018).[255]
  • A study on the body mass sexual dimorphism in Nacholapithecus kerioi is published by Kikuchi et al. (2018).[256]
  • A review of the paleontological, archeological, genetic and behavioral evidence of the impact of at least 70,000 years of human influence on orangutan distribution, abundance and ecology is published by Spehar et al. (2018).[257]
  • Description of tooth decay affecting the type specimen of Dryopithecus carinthiacus, and a study on its implications for inferring the diet of this specimen, is published by Fuss, Uhlig & Böhme (2018).[258]
  • A study on the phylogenetic relationships of Graecopithecus published by Benoit & Thackeray (2017), aiming to refute the hypothesis that Graecopithecus is a member of the hominin clade,[259] is criticized by Fuss et al. (2018).[260]
  • A study evaluating whether machine learning methods can accurately classify extant apes based on dental data, and using this classification method to explore the affinities between dentitions of Miocene hominoid fossils and living apes, is published by Monson, Armitage & Hlusko (2018).[261]

General paleoanthropology

  • Estimations of body mass in Pliocene and Pleistocene hominins based on lower limb bones dimensions are presented by Ruff et al. (2018).[262]
  • A study on the evolution of the brain size in hominins is published by Du et al. (2018).[263]
  • A study on the evolution of the mandible shape in hominins, based on an analysis of the mandibular shape variation in a large sample of plesiadapiforms and primates, is published by Raia et al. (2018).[264]
  • A study on the cervical kinematics in early fossil hominins, based on an analysis of uncinate processes in the vertebrae of fossil hominins, Homo sapiens and extant nonhuman primates, is published by Meyer et al. (2018).[265]
  • A study on the intra-specific variation of patterns of metatarsal robusticity (a measure reflecting habitual stresses in long bones, and in particular, loads experienced over an animal's lifetime) in modern humans and extant African apes, and its implications for inferring whether the Olduvai Hominid 8 foot was biomechanically similar to the feet of modern humans, is published by Patel et al. (2018).[266]
  • A study on the bony shape variables in the metatarsals of extant anthropoid primates and fossil hominins, and on their importance to the evolution of terrestrial bipedalism in hominins, is published by Fernández et al. (2018).[267]
  • Domínguez-Rodrigo & Baquedano (2018) evaluate the ability of successful machine learning methods to compare and distinguish various types of bone surface modifications (trampling marks, crocodile bite marks and cut marks made with stone tools) in archaeofaunal assemblages.[268]
  • Taphonomic study on the ca. 1.84 million year old bovid fossils (preserving evidence of meat eating by early hominins) from Olduvai Gorge (Tanzania), evaluating whether hominins had early access to fleshed carcasses through hunting or active scavenging, or late access to largely defleshed carcasses through passive scavenging, is published by Parkinson (2018).[269]
  • The study published by Gierliński et al. (2017), reporting putative tetrapod footprints with hominin-like characteristics from the late Miocene of Crete (Greece),[270] is criticized by Meldrum & Sarmiento (2018).[271]
  • A study aiming to estimate body mass of Orrorin tugenensis and Ardipithecus ramidus is published by Grabowski, Hatala & Jungers (2018).[272]
  • A study on the hydrological changes in the Limpopo River catchment and in sea surface temperature in the southwestern Indian Ocean for the past 2.14 million years, and on their implications for inferring the palaeoclimatic changes in southeastern Africa in this time period and their possible impact on the evolution of early hominins, is published by Caley et al. (2018).[273]
  • A study on the behavioral features which might have contributed to the demographic success of early hominids such as Australopithecus, based on comparison with macaques, is published by Meindl, Chaney & Lovejoy (2018).[274]
  • A study on the diversity dynamics of early hominins, evaluating whether the observed patterns of early hominin diversity can be better explained by sampling biases or genuine evolutionary processes, is published by Maxwell et al. (2018).[275]
  • A study on the pelvic morphology in Ardipithecus and Australopithecus, evaluating the hypothesis that early hominins retained ischial proportions and orientation that favored greater force production during climbing but limited their ability to hyperextend the hip and walk as economically as modern humans, is published by Kozma et al. (2018).[276]
  • New fossils attributable to the species Australopithecus anamensis will be described from Kanapoi (Kenya) by Ward, Plavcan & Manthi (2018).[277]
  • Endocrania of two specimens of Australopithecus africanus from Sterkfontein Member 4 (South Africa) are virtually reconstructed by Beaudet et al. (2018).[278]
  • A study on the paleoenvironment and diet of Australopithecus africanus and Paranthropus robustus as indicated by tooth microwear is published by Peterson et al. (2018).[279]
  • A study on the relationship between root splay and overall morphology of first maxillary molars and jaw kinematics in South African Australopithecus africanus and Paranthropus robustus, and on its implications for inferring the dietary niches of these species, is published by Kupczik, Toro-Ibacache & Macho (2018).[280]
  • A study on the variation in trabecular bone structure of the femoral head in fossil hominins attributed to the species Australopithecus africanus, Paranthropus robustus and to the genus Homo, attempting to reconstruct hip joint loading conditions in these fossil hominins, is published by Ryan et al. (2018).[281]
  • The skull of ‘Mrs. Ples’ (Sts 5 specimen of Australopithecus africanus) is interpreted as a skull of a small male rather than a large female individual by Tawane & Thackeray (2018).[282]
  • A study on the variation in the structure of trabecular bone and joint loading in the humeral head of extant hominoids, spider monkeys and Australopithecus africanus will be published by Kivell et al. (2018), who interpret their findings as indicating that A. africanus may have still used its forelimbs for arboreal locomotion.[283]
  • Description of a nearly complete, 3.32-million-year-old foot of a juvenile Australopithecus afarensis from Dikika (Ethiopia) is published by DeSilva et al. (2018).[284]
  • A study on the possible date of the first appearance of Australopithecus sediba as indicated by the average hominin species’ temporal range is published by Robinson et al. (2018).[285]
  • A study on the linear marks observed on the hominin fossil Stw53 from the Sterkfontein cave site (South Africa), evaluating whether these marks were cutmarks inflicted by stone tools or non-anthropic modifications, is published by Hanon, Péan & Prat (2018).[286]
  • New artifacts are described from the Swartkrans cave (South Africa) by Kuman et al. (2018), who confirm the affinity of the Swartkrans artifacts with the Oldowan industrial complex.[287]
  • Pelvic remains of Homo naledi from the Dinaledi Chamber in the Rising Star Cave system (Cradle of Humankind, South Africa) will be described by VanSickle et al. (2018).[288]
  • A study on the minimum number of individuals and on a demographic profile of the assemblage of Homo naledi individuals in the Dinaledi Chamber (Rising Star Cave system, South Africa) is published by Bolter et al. (2018).[289]
  • A study on the diet of Homo naledi as indicated by teeth wear textures is published by Ungar & Berger (2018).[290]
  • A study comparing tooth shape and size in Homo naledi and other South African Plio-Pleistocene hominins, as well as a study on the possible diet of Homo naledi, is published by Berthaume, Delezene & Kupczik (2018).[291]
  • A study on the endocast morphology of Homo naledi, comparing it with other hominoids and fossil hominins, is published by Holloway et al. (2018).[292]
  • A study on the phenetic affinities and taxonomic validity of Homo naledi as indicated by teeth morphology will be published by Irish et al. (2018).[293]
  • Three incudes of Homo naledi recovered from the Dinaledi Chamber in the Rising Star cave system are described by Elliott et al. (2018).[294]
  • A study on evaluating whether deliberate disposal of corpses is the only likely explanation for large assemblages of fossil human bones from the Middle Pleistocene sites of Sima de los Huesos (Spain) and the Dinaledi Chamber (South Africa) is published by Egeland et al. (2018).[295]
  • A study on the phylogenetic relationships of the Pleistocene hominin specimen (a fragmented skullcap) from Kocabaş (Denizli Basin, Turkey) is published by Vialet et al. (2018).[296]
  • A study on the morphology and affinities of the hominin calvaria KNM-ER 42700 from Ileret, Kenya is published by Neubauer et al. (2018).[297]
  • A study on the frequency and location of hominin (likely Homo habilis) butchery marks and carnivore tooth marks on mammal bones from the HWK EE site (Olduvai Gorge, Tanzania), and on their implications for inferring carnivorous feeding behavior of the HWK EE hominins and the ecological interactions they had with carnivores, is published by Pante et al. (2018).[298]
  • A study estimating possible adult stature and body mass of the Homo erectus specimen KNM-WT 15000 ("Turkana Boy") is published by Cunningham et al. (2018).[299]
  • A study on the structure of the animal community known from the Okote Member of the Koobi Fora Formation at East Turkana (Kenya) as indicated by tracks and skeletal assemblages, and on the interactions of Homo erectus with environment and associated faunas from this site, is published by Roach et al. (2018).[300]
  • A study on 1.07–0.99 million-year-old pelvic remains from Buia (Eritrea) is published by Hammond et al. (2018), who interpret their findings as indicating that the postcranial morphology of Homo erectus sensu lato was variable and, in some cases, nearly indistinguishable from modern human morphology, and that the shared last common ancestor of Late Pleistocene Homo species was unlikely to have an australopith-like pelvis.[301]
  • A study on the humeral rigidity and strength in members of the species Homo erectus known from Zhoukoudian (China), comparing it with the humeral rigidity and strength in the African members of the species, is published by Xing et al. (2018).[302]
  • A study on the morphology of teeth of Homo erectus from Zhoukoudian is published by Xing, Martinón-Torres & Bermúdez de Castro (2018).[303]
  • A study on the age of the archaeological layers from the Zhoukoudian Upper Cave, and on its implications for understanding Late Quaternary human evolution in eastern Asia, is published by Li et al. (2018).[304]
  • New magnetostratigraphic dating results for the Bailong Cave (China) sedimentary sequence containing hominin teeth assigned to the species Homo erectus are presented by Kong et al. (2018).[305]
  • An Early Pleistocene artefact sequence, containing 17 artefact layers that extend from approximately 1.26 million years ago to about 2.12 million years ago, is described from the Shangchen locality (Loess Plateau, China) by Zhu et al. (2018), indicating that hominins left Africa earlier than indicated by the evidence from Dmanisi.[306]
  • A study on the morphology and affinities of the Middle Pleistocene hominin mandible recovered from La Niche cave site of the Montmaurin karst system (France) is published by Vialet et al. (2018).[307]
  • A series of excavated Middle Stone Age sites from the Olorgesailie Basin (Kenya), dated as ~320,000 years old, is presented by Brooks et al. (2018), who report evidence of hominins preparing cores and points, exploiting iron-rich rocks to obtain red pigment, and procuring stone tool materials from ≥25–50 km distance.[308]
  • A study on the environmental dynamics before and after the onset of the early Middle Stone Age in the Olorgesailie Basin (Kenya) is published by Potts et al. (2018).[309]
  • A study on the chronology of the Acheulean and early Middle Stone Age sedimentary deposits in the Olorgesailie Basin (Kenya) is published by Deino et al. (2018).[310]
  • A study on the stone tools from the Acheulean site of Saffaqah near Dawadmi (Saudi Arabia), and their implications for inferring how hominins adapted to this region, is published by Shipton et al. (2018).[311]
  • A study on the age of stone tools from the Attirampakkam site in India is published by Akhilesh et al. (2018), indicating the emergence of a Middle Paleolithic culture in India at 385 ± 64 thousand years ago.[312]
  • Stone tools associated with a skeleton of Rhinoceros philippinensis showing clear signs of butchery are described from a bone bed at Kalinga in the Cagayan Valley of northern Luzon (the Philippines), dated to between 777 and 631 thousand years ago, by Ingicco et al. (2018).[313]
  • The study on the Cerutti Mastodon site published by Holen et al. (2017), reporting possible evidence of an unidentified species of the genus Homo living in California 130,000 years ago,[314] is criticized by Ferraro et al. (2018).[315][316]
  • Bone retouchers dated as approximately 125–105,000 years old are described from the Lingjing site in Henan, China by Doyon et al. (2018), representing the first evidence from Eastern Asia for the use of bone as raw material to modify stone tools.[317]
  • A study on the antiquity of the remains of Homo antecessor, based on the first direct Electron Spin Resonance dating of a tooth from the TD6 unit of Atapuerca Gran Dolina site (Spain), is published by Duval et al. (2018).[318]
  • An assemblage of hominin tracks produced by adults and children potentially as young as 12 months, probably members of the species Homo heidelbergensis living 700,000 years ago, is described from the Upper Awash Valley (Ethiopia) by Altamura et al. (2018).[319]
  • A study on the morphology and function of the browridge of the Kabwe 1 archaic hominin specimen is published by Godinho, Spikins & O’Higgins (2018).[320]
  • A study intending to detect introgressed Denisovan genetic material in present-day human genomes is published by Browning et al. (2018), who report evidence of Denisovan ancestry in populations from East and South Asia and Papuans, and interpret their findings as indicating that at least two distinct instances of Denisovan admixture into modern humans occurred.[321]
  • Genome recovered from a bone fragment from the Denisova Cave (Russia) is presented by Slon et al. (2018), who interpret the studied individual as the offspring of a Neanderthal mother and a Denisovan father.[322]
  • A study on the morphology of hominin teeth from the Middle Pleistocene sites of Arago (southeast France) and Sima de los Huesos (northern Spain), as well as on their implications for inferring how the settlement of Europe by hominins in the Middle Pleistocene occurred, is published by Bermúdez de Castro et al. (2018).[323]
  • A study aiming to estimate total lung capacity of Neanderthals, as well as Early Pleistocene hominins from the Gran Dolina site ATD6 (Spain), is published by García-Martínez et al. (2018).[324]
  • A series of partially charred wooden tools is described from the late Middle Pleistocene site of Poggetti Vecchi (central Italy) by Aranguren et al. (2018), who interpret their findings as indicating that Neanderthals were able to choose the appropriate timber and to process it with fire to produce tools.[325]
  • A wooden tool (possibly a digging stick), likely produced by Neanderthals, is described from the early Late Pleistocene Aranbaltza III site (Basque Country, Spain) by Rios-Garaizar et al. (2018), representing the oldest wooden tool from southern Europe reported so far.[326]
  • Cave art in Cave of La Pasiega, Maltravieso cave and Ardales cave (Spain) is dated as older than 64,000 years (thus predating the arrival of modern humans in Europe) by Hoffmann et al. (2018), who interpret their findings as indicative of Neandertal authorship of the art;[327] the study is subsequently criticized by Pearce & Bonneau (2018)[328][329] and Aubert, Brumm & Huntley (2018).[330]
  • A study on the age of the flowstone capping the Cueva de los Aviones deposit in southeast Spain is published by Hoffmann et al. (2018), who report that Neanderthal-associated evidence of symbolic behavior found at the site is 115,000 to 120,000 years old and predates the earliest known comparable evidence associated with modern humans by 20,000 to 40,000 years.[331]
  • Genomes of five Neanderthals from Belgium (Spy Cave and Goyet Caves), France (Les Cottés cave), Croatia (Vindija Cave) and Russia (Mezmaiskaya cave), who lived around 39,000 to 47,000 years ago, are sequenced by Hajdinjak et al. (2018).[332]
  • A study evaluating three hypotheses forwarded to explain the distinctive Neanderthal face is published by Wroe et al. (2018).[333]
  • A study evaluating ecological niche similarity between the datasets of morphologically diagnostic Neanderthal remains and of archaeological sites with Middle Paleolithic artifacts (but no diagnostic hominin remains), as well as assessing its implications for inferring whether those archaeological sites represent Neanderthal occurrences, is published by Bible & Peterson (2018).[334]
  • Gaudzinski-Windheuser et al. (2018) report perforations observed on two fallow deer skeletons from the 120,000-year-old lake shore deposits from Neumark-Nord (Germany), interpreted as evidence of close-range use of thrusting spears by Neanderthals.[335]
  • A study on the timing and duration of periods of climate deterioration in the interior of the Iberian Peninsula in the late Pleistocene, evaluating the impact of climate on the abandonment of inner Iberian territories by Neanderthals 42,000 years ago, is published by Wolf et al. (2018).[336]
  • Evidence of bird and carnivore exploitation by Neanderthals (cut-marks in golden eagle, raven, wolf and lynx remains) is reported from the Axlor site (Spain) by Gómez-Olivencia et al. (2018).[337]
  • The first direct artefactual evidence for regular, systematic fire production by Neanderthals is reported from archaeological layers attributed to late Mousterian industries at multiple sites throughout France by Sorensen, Claud & Soressi (2018).[338]
  • A study aiming to determine whether metabolic differences between competing populations of Neanderthals and anatomically modern humans alone could have accounted for Neanderthal extinction, as well as investigating Neanderthal fire use, will be published by Goldfield, Booton & Marston (2018).[339]
  • A study on the climate changes in Europe during the Middle–Upper Paleolithic transition (based on speleothem records from the Ascunsă Cave and from the Tăușoare Cave, Romania), and on their implications for the replacement of Neanderthals by modern humans in Europe, is published by Fernández et al. (2018).[340]
  • A study aiming to reconstruct 3D brain shape of Neanderthals and early Homo sapiens is published by Kochiyama et al. (2018).[341]
  • A study on the use of plants by early modern humans during the Middle Stone Age as indicated by analyses of phytoliths from the Pinnacle Point locality (South Africa) is published by Esteban et al. (2018).[342]
  • A study on the climatic changes in the Lake Tana area in the last 150,000 years and their implications for early modern human dispersal out of Africa is published by Lamb et al. (2018).[343]
  • A review of fossil, archaeological, genetic, and paleoenvironmental data on the origin of Homo sapiens is published by Scerri et al. (2018), who argue that Homo sapiens evolved within a set of interlinked groups living across Africa, whose connectivity changed through time, rather than from a single region/population in Africa.[344]
  • A review of the archaeological and palaeoenvironmental datasets relating to the Middle–Late Pleistocene dispersal of Homo sapiens within and beyond Africa is published by Roberts & Stewart (2018), who argue that H. sapiens developed a new ecological niche.[345]
  • A study on the evolution of modern human brain shape based on endocasts of Homo sapiens fossils from different geologic time periods is published by Neubauer, Hublin & Gunz (2018).[346]
  • Late Pleistocene hominin tracks, probably produced by Homo sapiens, are described from the Waenhuiskrans Formation (South Africa) by Helm et al. (2018).[347]
  • A study on the age of a modern human mandible with teeth from the Misliya cave (Mount Carmel, Israel) is published by Hershkovitz et al. (2018), who date the fossil as at least 177,000 years old, representing the oldest reported fossil of a member of the Homo sapiens clade found outside Africa.[348]
  • A phalanx of a member of the species Homo sapiens is described from the ~95–86,000 years old Al Wusta site (An Nafud, Saudi Arabia) by Groucutt et al. (2018), representing the oldest directly dated fossil of Homo sapiens found outside Africa and the Levant.[349]
  • A study on the effects of the Toba supereruption in East Africa is published by Yost et al. (2018), who find no evidence of the eruption causing a volcanic winter in East Africa or a population bottleneck among African populations of anatomically modern humans.[350]
  • Microscopic glass shards characteristic of the Youngest Toba Tuff (ashfall from the Toba eruption), dated as approximately 74,000 years old, are described from two archaeological sites on the south coast of South Africa by Smith et al. (2018), who interpret their findings as indicating that humans in this region thrived through the Toba event and the ensuing full glacial conditions.[351]
  • Evidence of human activity dating back to 78,000 years ago is reported from the Panga ya Saidi cave (Kenya) by Shipton et al. (2018), who describe a rich technological sequence that includes lithic forms elsewhere associated with the Middle Stone Age and the Later Stone Age.[352]
  • A cross-hatched pattern drawn with an ochre crayon is reported from approximately 73,000-year-old Middle Stone Age levels at Blombos Cave (South Africa) by Henshilwood et al. (2018), pre-dating previously known abstract and figurative drawings by at least 30,000 years.[353]
  • A study on the age of the cave art from the Kapova Cave (Russia) is published by Dublyansky et al. (2018).[354]
  • A reassessment of the Late Pleistocene human occupation site at Leang Burung 2 (Sulawesi, Indonesia), presenting new stratigraphic information and dating evidence from the site, is published by Brumm et al. (2018).[355]
  • A study on the timing of arrival of anatomically modern humans to Southeast Asia and Sahul is published by O’Connell et al. (2018), who consider it unlikely that the artifacts from Madjedbebe (northern Australia) reported by Clarkson et al. (2017)[356] are more than 50,000 years old.[357]
  • Genomic data from seven 15,000-year-old modern humans from Morocco, attributed to the Iberomaurusian culture, is presented by van de Loosdrecht et al. (2018), who report evidence of a genetic affinity of the studied individuals with early Holocene Near Easterners.[358]
  • A study on charred food remains from Shubayqa 1, a Natufian hunter-gatherer site located in northeastern Jordan and dated to 14.6–11.6 ka cal BP, is published by Arranz-Otaegui et al. (2018), who interpret their findings as providing the earliest empirical evidence for the preparation of bread-like products by Natufian hunter-gatherers, predating the emergence of agriculture by at least 4,000 years.[359]
  • Description of the morphology of three partial human mandibles from the Niah Caves (Sarawak, Malaysia) and a study on the age of these bones is published by Curnoe et al. (2018).[360]
  • A review of the genetic, archeological and paleoecological data on the course of the settlement of the Americas is published by Potter et al. (2018), who argue that available evidence is consistent with an inland migration through an ice-free corridor or with a migration through Pacific coastal routes (or both), but neither can be rejected.[361]
  • A study on the timing of the latest Pleistocene glaciation in southeastern Alaska and its implication for inferring the route and timing of early human migration to the Americas is published by Lesnek et al. (2018).[362]
  • A study on the technological traits of fluted projectile points from northern Alaska and Yukon, in combination with artifacts from further south in Canada, the Great Plains, and eastern United States, evaluating the plausibility of historical relatedness and evolutionary patterns in the spread of fluted-point technology in North America in the latest Pleistocene and earliest Holocene, is published by Smith & Goebel (2018).[363]
  • Late Pleistocene human footprints left by a minimum of three people are described from the Calvert Island (British Columbia, Canada) by McLaren et al. (2018).[364]
  • Associated human and ground sloth tracks are described from the Rancholabrean deposits in the White Sands National Monument (New Mexico, United States) by Bustos et al. (2018), who interpret their finding as evidence of humans actively stalking, harassing and likely hunting ground sloths in the late Pleistocene.[365]
  • A study on the age of a series of sedimentary samples from the earliest cultural assemblage at the Gault Site (Texas, United States), including a previously unknown, early projectile point technology unrelated to Clovis, is published by Williams et al. (2018).[366]
  • A study on the age of the Anzick burial site (Montana, United States) is published by Becerra-Valdivia et al. (2018).[367]
  • The genome of two infants from the Upward Sun River site dated 11,500 years ago is sequenced, leading to the discovery of the Ancient Beringian ethnic group.[368][369]
  • Scheib et al. (2018) sequence 91 ancient human genomes from California and southwestern Ontario, demonstrating the existence of two distinct ancestries in North America, and finding contribution from both of these ancestral populations in all modern Central and South Americans.[370]
  • Evidence of plant domestication and food production from the early and middle Holocene site of Teotonio (southwestern Amazonia, Brazil) is presented by Watling et al. (2018).[371]
  • A study on the morphological affinity of the late Paleolithic human skull from the Zlatý kůň site in the Bohemian Karst (Czech Republic) is published by Rmoutilová et al. (2018), who also evaluate whether it is possible to determine the sex of the Zlatý kůň individual based on its skull morphology.[372]
  • A study on the Mesolithic site of Star Carr, indicating that there was intensive human activity at the site for several hundred years when the community was subject to multiple, severe, abrupt climate events that impacted air temperatures, the landscape and the ecosystem of the region, is published by Blockley et al. (2018).[373]
  • A study on the tools preserved with Ötzi, evaluating their implications for inferring Ötzi's individual history, the reconstruction of his last days and his cultural and social background, is published by Wierer et al. (2018).[374]
  • A study on the contents of Ötzi's stomach is published by Maixner et al. (2018).[375]
  • A study on the compositions of the faunal and stone artifact assemblages at Liang Bua (Flores, Indonesia), aiming to determine the last appearance dates of Stegodon, giant marabou stork, Old World vulture belonging to the genus Trigonoceps, and Komodo dragon at the Liang Bua site, and to determine what raw materials were preferred by hominins from this site ∼50,000–13,000 years ago and whether these preferences were similar to those seen in the stone artifact assemblages attributed to Homo floresiensis or to those attributed to modern humans, will be published by Sutikna et al. (2018).[376]
  • A study on genetic variation among a population of Rampasasa pygmies living close to the cave where remains of Homo floresiensis were discovered is published by Tucci et al. (2018), who find evidence of admixture with Denisovans and Neanderthals but no evidence for gene flow with other archaic hominins, and interpret their findings as indicating that at least two independent instances of hominin insular dwarfism occurred on Flores.[377]

New taxa

Name Novelty Status Authors Age Unit Location Notes Images

Asiadapis tapiensis[378]

Sp. nov

Valid

Rose et al.

Eocene (early Ypresian)

Cambay Shale Formation

 India

Brontomomys[379]

Gen. et sp. nov

In press

Atwater & Kirk

Eocene (Uintan)

Friars Formation

 United States
( California)

A member of the family Omomyidae. Genus includes new species B. cerutti.

Ekwiiyemakius[379]

Gen. et sp. nov

In press

Atwater & Kirk

Eocene (Uintan)

Friars Formation

 United States
( California)

A member of the family Omomyidae. Genus includes new species E. walshi.

Gunnelltarsius[379]

Gen. et sp. nov

In press

Atwater & Kirk

Eocene (Uintan)

Friars Formation

 United States
( California)

A member of the family Omomyidae. Genus includes new species G. randalli.

Junzi[380]

Gen. et sp. nov

Valid

Turvey et al.

Holocene

 China

A gibbon. Genus includes new species J. imperialis.

Other eutherians

  • Putative Cretaceous metatherian Sinodelphys szalayi is reinterpreted as an early member of Eutheria by Bi et al. (2018).[381]
  • A study on the anatomy of the Early Cretaceous eutherian Endotherium niinomii is published by Wang et al. (2018), who consider this species to be a valid taxon.[382]
  • Napoli et al. (2018) digitally visualize and describe the endocast of a taeniodont Onychodectes tisonensis.[383]
  • A study evaluating when solenodons split from other eulipotyphlans, based on updated fossil calibrations, is published by Springer, Murphy & Roca (2018), who place the split between solenodons and other eulipotyphlans in the Late Cretaceous.[384]
  • A study comparing the size and morphology of the common shrew (Sorex araneus), Sorex runtonensis, the tundra shrew (S. tundrensis) and the Caucasian shrew (S. satununi) with the type material of the fossil shrew Sorex subaraneus (in order to either support or falsify the validity of S. subaraneus and the putative ancestry of the extant common shrew) is published by Rzebik-Kowalska & Pereswiet-Soltan (2018).[385]
  • A study on the phylogenetic relationships of the gymnure Deinogalerix within the tribe Galericini will be published by Borrani et al. (2018).[386][387]
  • A study on the systematic usefulness of the humerus in proterotheriid litopterns is published by Corona, Perea & Ubilla (2018), who consider the species Proterotherium berroi Kraglievich (1930) to be a probable synonym of Neolicaphrium recens.[388]
  • A study on the diversity of shapes of snout in notoungulates and on the evolution of the wide range of shapes of snout in this group of mammals is published by Gomes Rodrigues et al. (2018).[389]
  • A study on the variation of teeth shape and on the factors affecting changes in the shape of teeth of notopithecid notoungulates is published by Scarano & Vera (2018).[390]
  • A study on the variation of teeth shape in late Miocene members of the hegetotheriid notoungulate genus Paedotherium, as well as its implications for the systematics and phylogenetic relationships of the late Miocene species of Paedotherium, is published by Ercoli et al. (2018).[391]
  • A study on the variability of the diagnostic characters in the fossils of members of the hegetotheriid notoungulate genus Tremacyllus will be published by Sostillo, Cerdeño & Montalvo (2018), who consider the species T. incipiens to be a junior synonym of the species T. impressus.[392]
  • New fossil remains of pachyrukhine hegetotheriid notoungulates are described from the Huayquerías del Este (Mendoza, Argentina) by Vera & Ercoli (2018), who consider the species Tremacyllus subdiminutus to be a synonym of T. impressus.[393]
  • A study on the braincase anatomy in mesotheriid notoungulates will be published by Fernández-Monescillo et al. (2018).[394]
  • Fernández-Monescill et al. (2018) provide muscular reconstruction and infer functional properties of the forelimb of the mesotheriid notoungulate Plesiotypotherium achirense.[395]
  • A study on the tooth wear, tooth replacement and enamel microstructure in a perissodactyl-like ungulate Cambaytherium will be published by von Koenigswald et al. (2018).[396]
  • Anatomical redescription of the periptychid species Periptychus carinidens is published by Shelley, Williamson & Brusatte (2018).[397]
  • A study comparing the teeth of Prionogale to the teeth of subadult hyaenodonts and carnivorans, as well as evaluating the phylogenetic affinities of Prionogale and Namasector within Hyaenodonta, will be published by Borths & Stevens (2018), who reinterpret the type specimen of Prionogale breviceps and some of the paratype materials as preserving deciduous teeth which were previously interpreted as permanent dentition.[398]
Name Novelty Status Authors Age Unit Location Notes Images

Ambolestes[381]

Gen. et sp. nov

Valid

Bi et al.

Early Cretaceous

 China

An early eutherian. Genus includes new species A. zhoui.

Arcius hookeri[399]

Sp. nov

Valid

López-Torres & Silcox

Early Eocene

 United Kingdom

A member of Plesiadapiformes belonging to the family Paromomyidae.

Arcius ilerdensis[399]

Sp. nov

Valid

López-Torres & Silcox

Early Eocene

 Spain

A member of Plesiadapiformes belonging to the family Paromomyidae.

Chiromyoides mauberti[400]

Sp. nov

Valid

De Bast, Gagnaison & Smith

Late Paleocene

 France

A member of Plesiadapiformes belonging to the family Plesiadapidae.

Darbonetus sigei[401]

Sp. nov

Valid

Hooker

Eocene (Priabonian)

 France

A member of the family Nyctitheriidae.

Dissacus raslanloubatieri[402]

Sp. nov

Valid

Solé et al.

Eocene (Ypresian)

 France

A member of the family Mesonychidae.

Dissacus rougierae[402]

Sp. nov

Valid

Solé et al.

Eocene (Ypresian)

 France

A member of the family Mesonychidae.

Eomorphippus bondi[403]

Sp. nov

Valid

Wyss, Flynn & Croft

Early Oligocene

Abanico Formation

 Chile

A notohippid notoungulate.

Eomorphippus neilopdykei[403]

Sp. nov

Valid

Wyss, Flynn & Croft

Early Oligocene

Abanico Formation

 Chile

A notohippid notoungulate.

Falcontoxodon[404]

Gen. et sp. nov

Valid

Carrillo et al.

Early Pliocene–late Pliocene or early Pleistocene

Falcón Basin
(Codore Formation
San Gregorio Formation)

 Venezuela

A member of Toxodontidae. Genus includes new species F. aguilerai.

Ferrequitherium[405]

Gen. et sp. nov

Valid

Scott

Paleocene (early Tiffanian)

Paskapoo Formation

 Canada
( Alberta)

A relative of Horolodectes. Genus includes new species F. sweeti.

Hilarcotherium miyou[404]

Sp. nov

Valid

Carrillo et al.

Middle Miocene

Castilletes Formation

 Colombia

A member of Astrapotheriidae.

Hovurlestes[406]

Gen. et sp. nov

Valid

Lopatin & Averianov

Early Cretaceous (AptianAlbian)

Höovör locality

 Mongolia

A basal member of Eutheria. The type species is H. noyon.

Llullataruca[407]

Gen. et sp. nov

Valid

McGrath, Anaya & Croft

Laventan

 Bolivia

A member of Litopterna belonging the family Macraucheniidae. Genus includes new species L. shockeyi.

Platychoerops boyeri[400]

Sp. nov

Valid

De Bast, Gagnaison & Smith

Late Paleocene

 France

A member of Plesiadapiformes belonging to the family Plesiadapidae.

Plesiadapis berruensis[408]

Sp. nov

Valid

Jehle et al.

Late Paleocene

 France

A member of Plesiadapiformes.

Plesiadapis ploegi[400]

Sp. nov

Valid

De Bast, Gagnaison & Smith

Late Paleocene

 France

A member of Plesiadapiformes belonging to the family Plesiadapidae.

Propterodon panganensis[409]

Sp. nov

Valid

De Bonis et al.

Middle Eocene

Pondaung Formation

 Myanmar

A member of the family Hyaenodontidae.

Rosendo[403]

Gen. et comb. nov

Valid

Wyss, Flynn & Croft

Early Oligocene

Sarmiento Formation

 Argentina
 Chile

A notohippid notoungulate; a new genus for "Eomorphippus" pascuali Simpson (1967).

Rusconitherium[410]

Gen. et comb. nov

Valid

Cerdeño, Vera & Combina

Early Miocene

Mariño Formation

 Argentina

A mesotheriid notoungulate; a new genus for "Trachytherus" mendocensis Simpson & Minoprio (1949).

Sardolagus[411]

Gen. et sp. nov

Valid

Angelone et al.

Early Pleistocene

 Italy

A member of the family Leporidae. Genus includes new species S. obscurus.

Shargainosorex[412]

Gen. et sp. nov

Valid

Zazhigin & Voyta

Middle Miocene

Oshin Suite

 Mongolia

A shrew belonging to the subfamily Crocidosoricinae. The type species is S. angustirostris.

Termastherium[403]

Gen. et sp. nov

Valid

Wyss, Flynn & Croft

Early Oligocene

Abanico Formation

 Chile

A leontiniid notoungulate. Genus includes new species T. flacoensis.

‘Theosodon’ arozquetai[407]

Sp. nov

Valid

McGrath, Anaya & Croft

Laventan

 Bolivia

A member of Litopterna belonging the family Macraucheniidae, tentatively referred to the genus Theosodon.

Wyonycteris kingi[413]

Sp. nov

In press

Hooker

Paleogene

Woolwich Formation

 United Kingdom

A member of the family Nyctitheriidae.

Xotodon caravela[414]

Sp. nov

Valid

Armella, García-López & Dominguez

Late Miocene-early Pliocene

Aconquija Formation

 Argentina

Other mammals

Name Novelty Status Authors Age Unit Location Notes Images

Brasilestes[422]

Gen. et sp. nov

Castro et al.

Late Cretaceous

Adamantina Formation

 Brazil

An early member of Tribosphenida. The type species is B. stardusti.

Catopsalis kakwa[423]

Sp. nov

Valid

Scott, Weil & Theodor

Early Paleocene

 Canada
( Alberta)

A multituberculate belonging to the group Taeniolabidoidea.

Cifelliodon[424]

Gen. et sp. nov

Valid

Huttenlocker et al.

Early Cretaceous

Cedar Mountain Formation

 United States
( Utah)

A member of Haramiyida belonging to the family Hahnodontidae. The type species is C. wahkarmoosuch.

Khorotherium[425]

Gen. et sp. nov

Valid

Averianov et al.

Early Cretaceous (?Berriasian-Barremian)

Batylykh Formation

 Russia
( Sakha Republic)

A member of Docodonta belonging to the family Tegotheriidae. The type species is K. yakutensis.

Litovoi[426]

Gen. et sp. nov

Valid

Csiki-Sava et al.

Late Cretaceous (Maastrichtian)

 Romania

A multituberculate belonging to the family Kogaionidae. The type species is L. tholocephalos.

Sangarotherium[425]

Gen. et sp. nov

Valid

Averianov et al.

Early Cretaceous (?Berriasian-Barremian)

Batylykh Formation

 Russia
( Sakha Republic)

A member of Eutriconodonta of uncertain phylogenetic placement. The type species is S. aquilonium.

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