Stéphane Ducrocq

ORCID: 0000-0002-3552-6657
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About
Contact & Profiles
Research Areas
  • Evolution and Paleontology Studies
  • Bat Biology and Ecology Studies
  • Primate Behavior and Ecology
  • Paleontology and Evolutionary Biology
  • Pleistocene-Era Hominins and Archaeology
  • Geology and Paleoclimatology Research
  • Animal Ecology and Behavior Studies
  • Morphological variations and asymmetry
  • Marine animal studies overview
  • Comparative Animal Anatomy Studies
  • Ichthyology and Marine Biology
  • Wildlife Ecology and Conservation
  • Amphibian and Reptile Biology
  • Forensic Anthropology and Bioarchaeology Studies
  • Genetic diversity and population structure
  • Plant Diversity and Evolution
  • Geological and Geophysical Studies
  • Animal Vocal Communication and Behavior
  • Ecology and biodiversity studies
  • Yersinia bacterium, plague, ectoparasites research
  • International Labor and Employment Law
  • Geological formations and processes
  • Legal and Labor Studies
  • Healthcare Systems and Practices
  • Social Sciences and Governance

Université de Poitiers
2015-2025

Institute of Paleoprimatology Human Paleontology Evolution and Paleoenvironments
2015-2025

Centre National de la Recherche Scientifique
2007-2021

Institut des Sciences de l'Evolution de Montpellier
1996-2007

Institut de Paléontologie Humaine
2006-2007

Université de Montpellier
1995-2005

University of Yangon
2000-2003

Universidad Nacional Autónoma de México
2002

Staatliches Museum für Naturkunde Stuttgart
1995

A new genus and species of anthropoid primate, Bahinia pondaungensis gen. et sp. nov., is described from the Yashe Kyitchaung locality in Late Middle Eocene Pondaung Formation (Myanmar). It related to Eosimias , but it represented by more complete remains, including upper dentition with associated lower jaw fragment. interpreted as a representative family Eosimiidae, which corresponds sister group Amphipithecidae all other anthropoids. Eosimiidae are now recorded three distinct localities...

10.1126/science.286.5439.528 article EN Science 1999-10-15

In the absence of a comprehensive fossil record, origin and early evolution Malagasy lemurs have been subject to much uncertainty. We report here discovery strepsirrhine with strong cheirogaleid lemur affinities, Bugtilemur mathesoni gen. et sp. nov., from Oligocene deposits Bugti Hills (Balochistan, Pakistan). represents earliest record Lemuriformes, which hence appear already diversified outside Madagascar at least 30 million years ago. This clearly enhances critical role Indian...

10.1126/science.1065257 article EN Science 2001-10-19

The earliest known hippopotamids, attributed to the subfamily Kenyapotaminae, are essentially from dental remains of two species. first was found in middle Miocene Kenya, second at beginning upper eastern and northern Africa. exact affinities Kenyapotaminae critical for resolving long debated origin Hippopotamidae, as part wider question cetacean within artiodactyls. We performed detailed comparative description, character by character, kenyapotamines, using following putatively related...

10.1111/j.1096-3642.2009.00548.x article EN Zoological Journal of the Linnean Society 2010-01-25

Orliac, M. J., Antoine, P. ‐O., Ducrocq, S. (2010). Phylogenetic relationships of the Suidae (Mammalia, Cetartiodactyla): new insights on within Suoidea. — Zoologica Scripta , 39 315–330. In most analyses, both molecular and morphological phylogenies Cetartiodactyla support monophyly However, evolutionary history this superfamily remains poorly known primarily due to long‐lasting debates about taxonomic content suoid families subfamilies. Despite their crucial position in reconstruction...

10.1111/j.1463-6409.2010.00431.x article EN Zoologica Scripta 2010-05-07

According to molecular data, hippopotamuses and cetaceans form a clade excluding other extant cetartiodactyls. Despite wealth of spectacular specimens documenting cetacean evolution, this relationship remains poorly substantiated by the fossil record. Indeed, evolutionary path leading from hippo-cetacean ancestor Hippopotamidae is plagued missing data phylogenetic uncertainties. Only an origination within extinct anthracotheres compatible with results, substantial filling phyletic gaps...

10.1038/ncomms7264 article EN cc-by Nature Communications 2015-02-24

Pondaungia cotteri is the largest primate known from Late Middle Eocene Pondaung Formation, Myanmar. Its taxonomic status has been subject of much debate because fragmentary nature its remains. Initially described as an anthropoid, some authors recently have associated it with adapid primates. These debates fueled not only by incompleteness fossils attributed to but also reticence many regard Asia important evolutionary theater for anthropoids. During November 1998 Myanmar-French Expedition,...

10.1073/pnas.97.8.4102 article EN Proceedings of the National Academy of Sciences 2000-04-11

A new tragulid, Archaeotragulus krabiensis , gen. n. et sp. n., is described from the late Eocene Krabi Basin (south Thailand). It represents oldest occurrence of family which was previously unknown prior to Miocene. displays a mixture primitive and derived characters, together with M structure on trigonid, appears be main dental autapomorphy family. We also report at Lophiomerycid, Krabimeryx primitivus affinities Chinese representatives family, particularly Lophiomeryx . The familial...

10.1046/j.0300-3256.2001.00071.x article EN Zoologica Scripta 2001-10-01

Primate dental and postcranial remains from the Eocene Pondaung Formation (Myanmar) have been subject of considerable confusion since their initial discoveries, anthropoid status has widely debated. We report here a well preserved primate talus discovered in Segyauk locality near Mogaung that displays derived anatomical features typical haplorhines, notably anthropoids, lacks strepsirhine synapomorphies. Linear discriminant parsimony analyses indicate Myanmar is more similar structurally to...

10.1073/pnas.2332542100 article EN Proceedings of the National Academy of Sciences 2003-10-31

In contrast to the Neogene fossil assemblages, Late Paleogene mammal localities are rare in Africa. The most famous ones situated Fayum depression Egypt, from which several rich fossi...

10.1080/02724630903413065 article EN Journal of Vertebrate Paleontology 2010-01-29

10.1127/pala/252/1999/93 article EN Palaeontographica Abteilung A 1999-05-18

ABSTRACT Except for the few specimens previously reported from late middle Eocene of North Africa (Algeria) and more recently South Asia (Myanmar), fossil record anomaluroid rodents is relatively scarce Paleogene Period. In this paper, we describe new material, notably a skull, taxon Pondaungimys anomaluropsis Dawson et al., 2003, described latest Pondaung Formation in Central Myanmar (South Asia). shows dental pattern very similar to that Nementchamys, an rodent roughly coeval deposits...

10.1671/0272-4634(2005)025[0214:nropar]2.0.co;2 article EN Journal of Vertebrate Paleontology 2005-03-11

Previous studies showed that in modern humans the basicranium is formed of two modules: midline cranial base and lateral which are integrated with face very different ways. The study relationship between these structures prime interest context hominids craniofacial evolutionary history. In this study, we aim to test if on one hand other qualitatively quantitatively chimpanzees: phylogenetically close but morphologically hominids. This work performed using three‐dimensional (3D) landmarks...

10.1002/ar.22654 article EN The Anatomical Record 2013-02-05

Research Article| February 01, 2001 Eocene Krabi basin (southern Thailand): Paleontology and magnetostratigraphy Mouloud Benammi; Benammi 1Laboratoire de Geophysique et Tectonique, Cc 60 Université Montpellier II, Place Eugène Bataillon, F-34095 cedex 5, France Search for other works by this author on: GSW Google Scholar Yaowalak Chaimanee; Chaimanee 2Geological Survey Division, Department of Mineral Resources, Rama VI Road, Bangkok 10400, Thailand Jean-Jacques Jaeger; Jaeger 3Laboratoire...

10.1130/0016-7606(2001)113<0265:ekbstp>2.0.co;2 article EN Geological Society of America Bulletin 2001-02-01
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