2009 in paleontology

Paleontology or palaeontology is the study of prehistoric life forms on Earth through the examination of plant and animal fossils. This includes the study of body fossils, tracks (ichnites), burrows, cast-off parts, fossilised feces (coprolites), palynomorphs and chemical residues. Because humans have encountered fossils for millennia, paleontology has a long history both before and after becoming formalized as a science. This article records significant discoveries and events related to paleontology that occurred or were published in the year 2009.

Three new species of extinct Octopoda discovered in 2009. The species - Keuppia hyperbolaris, Keuppia levante, and Styletoctopus annae - lived about 95 million years ago, and bear a strong resemblance to modern octopuses, suggesting that the Octopoda order has remained relatively unchanged for tens of millions of years. The fossils included evidence of arms, muscles, rows of suckers, ink, and internal gills. The discovery was made by a team led by Dirk Fuchs of the Freie University, which is located at Berlin, Germany. The fossils were found at Hakel and Hadjoula, Lebanon. Various new ammonoid taxa were named, including Ivoites.

Keuppia

Gen et sp nov

Valid

Fuchs, Bracchi, & Weis

Upper Cenomanian

 Lebanon

Styletoctopus

gen et sp nov

Valid

Fuchs, Bracchi, & Weis

Upper Cenomanian

 Lebanon

Ivoites

gen nov

Valid

De Baets, Klug, & Korn

Lower Emsian

 Germany

Gansuselache

Gen. et sp. nov

Valid

Wang et al.

Late Permian

Fangshankou Formation

 China

A member of Hybodontoidea. Genus includes new species G. tungshengi.

Papilionichthys

Gen. et sp. nov

Valid

Carboniferous (Serpukhovian)

Bear Gulch Limestone

 United States

A member of Iniopterygidae. The type species is P. stahlae.

Rainerichthys

Gen. et sp. nov

Valid

Carboniferous (Serpukhovian)

Bear Gulch Limestone

 United States

A member of Iniopterygidae. The type species is R. zangerli.

Valid

Late Miocene

 Armenia

Valid

Oligocene

 Czech Republic
 Poland

Valid

Oligocene

 Russia

Valid

Eocene (late Ypresian)

Monte Bolca locality

 Italy

Valid

Late Devonian

Gogo Formation

 Australia

Valid

Famennian (Late Devonian)

Dura Den Formation

 Scotland

Valid

Eocene (late Ypresian)

Monte Bolca locality

 Italy

Valid

Famennian (Late Devonian)

Evieux Formation

 Belgium

Valid

Oligocene

Abkhazia
 Azerbaijan
 Czech Republic
 France
 Germany
 Hungary
 Poland
 Romania
 Russia
 Ukraine

Valid

Early Paleocene

 Angola

Valid

Oligocene

 Romania

Baphetes orientalis

Valid

Late Carboniferous

 Czech Republic

Cratia

Valid

Lower Cretaceous

Crato Formation

 Brazil

Possible stem neobatrachian

Eurycephalella

Valid

Lower Cretaceous

Crato Formation

 Brazil

A hyloid

Nannaroter

Valid

Early Permian

 USA

The smallest known ostodolepid microsaur

Nesovtriton

Valid

Turonian

Bissekty Formation

 Uzbekistan

A cryptobranchoid salamander

Regalerpeton

Valid

Early Cretaceous

Huajiying Formation

 China

A cryptobranchoid salamander

Spinarerpeton

Valid

Early Permian

Boskovice Furrow

 Czech Republic

A discosauriscid seymouriamorph

Australothyris

Valid

Middle Permian

Tapinocephalus Assemblage Zone

 South Africa

A basal parareptile

Procolina

Valid

early Late Olenekian

Czatkowice 1

 Poland

A procolophonine procolophonid

Angolachelys

Valid

Turonian (Late Cretaceous)

 Angola

Aurorachelys

Valid

Late Cretaceous

Strand Fiord Formation

 Canada

Basilochelys

Valid

Late Jurassic/Lower Cretaceous

Phu Kradung Formation

 Thailand

Cedrobaena

Valid

Paleocene

Fort Union Formation

 USA

New genus for "Plesiobaena" putorius Gaffney, 1972

Chelonoidis alburyorum

Valid

Holocene

 The Bahamas

A tortoise.

Chinlechelys

Valid

Late Triassic (Norian)

Bull Canyon Formation

 United States

A basal member of Testudinata. The type species is C. tenertesta. The genus Chinlechelys was considered to be a junior synonym of the genus Proganochelys by Joyce (2017), though the author maintained C. tenertesta as a distinct species within the latter genus.

Derrisemys

Junior synonym

Early Paleocene

 USA

Junior synonym of Hutchemys.

Eileanchelys

Valid

Middle Jurassic

Kilmaluag Formation

 Scotland

Hutchemys

Valid

Paleocene

Fort Union Formation Tullock Formation

 USA

A plastomenine softshell turtles

Kinkonychelys

Valid

Late Cretaceous

Maevarano Formation

 Madagascar

Palatobaena cohen

Valid

Maastrichtian

Hell Creek Formation

 USA

A baenid

Peckemys

Valid

Late Cretaceous

Hell Creek Formation

 USA

A baenid

Plastomenoides

Junior synonym

Early Paleocene

 USA

Junior synonym of Hutchemys.

Czatkowiella

Valid

earliest Late Olenekian

Czatkowice 1

 Poland

A long−necked archosauromorph

Pamelina

Valid

Early Olenekian

Czatkowice 1

 Poland

A basal kuehneosaurid

Sophineta

Valid

earliest Late Olenekian

Czatkowice 1

 Poland

A basal lepidosauromorph

Gallardosaurus

Valid

Late Jurassic (Oxfordian)

Jagua Formation

 Cuba

Nichollssaura

Valid

Early Cretaceous (Albian)

Clearwater Formation

 Canada

Replacement name for Nichollsia Druckenmiller & Russell, 2008, preoccupied by an isopod genus Nichollsia Chopra & Tiwari, 1950

Rarosaurus

Disputed

Late Cretaceous (Maastrichtian)

 Jordan

A member of Polycotylidae. The type species is R. singularis.

Carinodens minalmamar

Sp. nov

Valid

Schulp, Bardet & Bouya

Late Cretaceous (Maastrichtian)

 Morocco

A mosasaur.

Titanoboa

Gen. et sp. nov

Valid

Head et al.

Paleocene

 Colombia

In February, the fossils of 28 individual T. cerrejonensis (Titanoboas) were announced to have been found in the coal mines of Cerrejon, La Guajira, Colombia.

Protuberum

Valid

Middle Triassic (Ladinian)

Santa Maria Formation

 Brazil

Raranimus

Valid

Middle Permian (Roadian)

Xidagou Formation

 China

Yuanotherium

Valid

Late Jurassic (Oxfordian)

Shishugou Formation

 China

Eucalyptolaurus

gen et sp nov

Valid

Coiffard et al.

uppermost Albian-lowermost Cenomanian

Charente-Maritimes

 France

A study noting the effects of the KT mass extinction on Earth's modern biota is published.

As science becomes more collaborative, papers with large numbers of authors are becoming more common. To prevent the deformation of the tables, these footnotes list the contributors to papers that erect new genera and have many authors.