Khoratpithecus piriyai, a late Miocene Hominoid of Thailand
Autor: | Paul Tafforeau, Kitti Khaowiset, Chotima Yamee, Christian Nemoz, Bernard Marandat, Yaowalak Chaimanee, Jean-Jacques Jaeger, Pannipa Tian |
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Přispěvatelé: | Department of Mineral Resources [Bangkok] (DMR), Institut des Sciences de l'Evolution de Montpellier (UMR ISEM), École pratique des hautes études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Montpellier (UM)-Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-Centre National de la Recherche Scientifique (CNRS)-Institut de recherche pour le développement [IRD] : UR226, European Synchrotron Radiation Facility (ESRF), Laboratoire de géobiologie, biochronologie et paléontologie humaine (LGBPH), Université de Poitiers-Centre National de la Recherche Scientifique (CNRS) |
Jazyk: | angličtina |
Rok vydání: | 2006 |
Předmět: |
0106 biological sciences
010506 paleontology Ankarapithecus Mandible Environment Late Miocene Southeast asian 010603 evolutionary biology 01 natural sciences Anthropology Physical Paleontology stomatognathic system biology.animal Image Processing Computer-Assisted Animals Sivapithecus Khoratpithecus ComputingMilieux_MISCELLANEOUS 0105 earth and related environmental sciences Lufengpithecus biology Fossils Vertebrate Hominidae 15. Life on land Thailand biology.organism_classification Biological Evolution Dentition Permanent Radiography Anthropology Mammal Anatomy [SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontology Tooth |
Zdroj: | American Journal of Physical Anthropology American Journal of Physical Anthropology, Wiley, 2006, 131, pp.311-323. ⟨10.1002/ajpa.20437⟩ |
ISSN: | 0002-9483 1096-8644 |
DOI: | 10.1002/ajpa.20437⟩ |
Popis: | A Khoratpithecus piriyai lower jaw corresponds to a well-preserved Late Miocene hominoid fossil from northeastern Thailand. Its morphology and internal structure, using a microcomputed tomography scan, are described and compared to those of other known Miocene hominoids. It originated from fluviatile sand and gravel deposits of a large river, and was associated with many fossil tree trunks, wood fragments, and large vertebrate remains. A biochronological analysis by using associated mammal fauna gives an estimated geological age between 9-6 Ma. The flora indicates the occurrence of a riverine tropical forest and wide areas of grassland. K. piriyai displays many original characters, such as the great breadth of its anterior dentition, suggesting large incisors, large lower M3, a canine with a flat lingual wall, and symphysis structure. Several of its morphological derived characters are shared with the orangutan, indicating sister-group relationship with that extant ape. This relationship is additionally strongly supported by the absence of anterior digastric muscle scars. These shared derived characters are not present in Sivapithecus, Ankarapithecus, and Lufengpithecus, which are therefore considered more distant relatives to the orangutan than Khoratpithecus. The Middle Miocene K. chiangmuanensis is older, displays more primitive dental characters, and shares several dental characters with the Late Miocene form. It is therefore interpreted as its probable ancestor. But its less enlarged M3 and more wrinkled enamel may suggest an even closer phylogenetic position to orangutan ancestors, which cannot yet be supported because of the incomplete fossil record. Thus Khoratpithecus represents a new lineage of Southeast Asian hominoids, closely related to extant great ape ancestors. |
Databáze: | OpenAIRE |
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