TY - JOUR
T1 - Bovidae (Mammalia, artiodactyla) from the neogene Irrawaddy beds, Myanmar
AU - Nishioka, Yuichiro
AU - Takai, Masanaru
AU - Tsubamoto, Takehisa
AU - Egi, Naoko
AU - Nishimura, Takeshi
AU - Kono, Reiko
AU - Ogino, Shinkai
AU - Thaung-Htike,
AU - Zin-Maung-Maung-thein,
AU - Vidthayanon, Chavalit
N1 - Funding Information:
We thank to personnel from the Ministry of Religious Affairs and Cultural, Myanmar for providing the permission for field research and assistance. We thank specially to P. Jintasakul (Nakhon Ratchasima Rajabhat University, Nakhon Ratchasi-ma, Thailand), S. Juan-Ngam (Sukhothai Museum of Natural History, Sukhothai, Thailand), and P. Vachajitpan (Bangkok, Thailand) for their kindness of providing the ONG and PRY collections for our study. Comparative material referred in this study was observed in American Museum of Natural History (New York, USA), Smithsonian Institute National Museum of Natural History (Washington, D.C., USA), The Natural History Museum (London, UK), Indian Museum, Geological Survey of India (Kolkata, India), Panjab University (Chandigarh, India), and Museum Geologi Bandung (Java, Indonesia). We appreciate the great help of all members of the Myanmar-Japan Palaeontological Expedition Team, who helped us to arrange the field research and collect fossil specimens. The present study was financially supported in part by Japan Society for the Promotion of Science KAKEN-HI, Grant-in-Aid for Scientific Research to MT [20405015, 26304019], NE [15K05330], and YN [16K17828].
Funding Information:
We thank to personnel from the Ministry of Religious Affairs and Cultural, Myanmar for providing the permission for field research and assistance. We thank specially to P. Jintasakul (Nakhon Ratchasima Rajabhat University, Nakhon Ratchasima, Thailand), S. Juan-Ngam (Sukhothai Museum of Natural History, Sukhothai, Thailand), and P. Vachajitpan (Bang-kok, Thailand) for their kindness of providing the ONG and PRY collections for our study. Comparative material referred in this study was observed in American Museum of Natural History (New York, USA), Smithsonian Institute National Museum of Natural History (Washington, D.C., USA), The Natural History Museum (London, UK), Indian Museum, Geological Survey of India (Kolkata, India), Panjab University (Chandigarh, India), and Museum Geologi Bandung (Java, Indonesia). We appreciate the great help of all members of the Myanmar-Japan Palaeontological Expedition Team, who helped us to arrange the field research and collect fossil specimens. The present study was financially supported in part by Japan Society for the Promotion of Science KAKEN-HI, Grant-in-Aid for Scientific Research to MT [20405015, 26304019], NE [15K05330], and YN [16K17828].
Publisher Copyright:
© 2019 E. Schweizerbart’sche Verlagsbuchhandlung, Stuttgart, Germany.
PY - 2019/5
Y1 - 2019/5
N2 - The evolution of the Neogene bovids (Mammalia, Artiodactyla, Ruminantia) in central Myanmar was examined, with descriptions of new specimens of caprine and bovine bovids from the upper Miocene to Pliocene part of the Irrawaddy beds. In the early late Miocene of central Myanmar, bovids had a relatively low diversity and were represented by Helicoportax sp. and Selenoportax vexillarius. Thereafter, they rapidly diversified until the latest Miocene (c. 6 Ma), including a caprine species (Caprinae gen. et sp. indet.) with spiral horn cores and seven bovines – Sivaportax dolabella, Tragoportax sp., Selenoportax vexillarius, Selenoportax falconeri, Pachyportax latidens, Pachyportax giganteus, and Proleptobos birmanicus. The latest Miocene/early Pliocene bovids are characterised by the coexistence of the Irrawaddy-endemic species (Sivaportax dolabella and Proleptobos birmanicus) and the other genera/species shared with the Nagri/Dhok Pathan faunas of the Siwaliks of Indo-Pakistan (Tra-goportax, Selenoportax vexillarius, Selenoportax falconeri, Pachyportax latidens, and Pachyportax giganteus). Among them, only the endemic species had survived throughout the Pliocene. The occurrence of Duboisia (Pleistocene bovids in Java, Indonesia) from the upper part (upper Pliocene) of the Irrawaddy beds also supports the dominance of endemic species in Southeast Asia. Through the late Neogene, no typical faunal turnovers were demonstrated in the Irrawaddy bovids with respect to those in the Siwalik bovids. This relatively low turnover rate was possibly affected by the progress in the faunal isolation of central Myanmar from the fauna of Indo-Pakistan during the late Pliocene owing to the formation of biogeographical barriers between central Myanmar and South Asia.
AB - The evolution of the Neogene bovids (Mammalia, Artiodactyla, Ruminantia) in central Myanmar was examined, with descriptions of new specimens of caprine and bovine bovids from the upper Miocene to Pliocene part of the Irrawaddy beds. In the early late Miocene of central Myanmar, bovids had a relatively low diversity and were represented by Helicoportax sp. and Selenoportax vexillarius. Thereafter, they rapidly diversified until the latest Miocene (c. 6 Ma), including a caprine species (Caprinae gen. et sp. indet.) with spiral horn cores and seven bovines – Sivaportax dolabella, Tragoportax sp., Selenoportax vexillarius, Selenoportax falconeri, Pachyportax latidens, Pachyportax giganteus, and Proleptobos birmanicus. The latest Miocene/early Pliocene bovids are characterised by the coexistence of the Irrawaddy-endemic species (Sivaportax dolabella and Proleptobos birmanicus) and the other genera/species shared with the Nagri/Dhok Pathan faunas of the Siwaliks of Indo-Pakistan (Tra-goportax, Selenoportax vexillarius, Selenoportax falconeri, Pachyportax latidens, and Pachyportax giganteus). Among them, only the endemic species had survived throughout the Pliocene. The occurrence of Duboisia (Pleistocene bovids in Java, Indonesia) from the upper part (upper Pliocene) of the Irrawaddy beds also supports the dominance of endemic species in Southeast Asia. Through the late Neogene, no typical faunal turnovers were demonstrated in the Irrawaddy bovids with respect to those in the Siwalik bovids. This relatively low turnover rate was possibly affected by the progress in the faunal isolation of central Myanmar from the fauna of Indo-Pakistan during the late Pliocene owing to the formation of biogeographical barriers between central Myanmar and South Asia.
KW - Artiodactyla
KW - Mammalia
KW - Miocene
KW - Pliocene
KW - Southeast Asia
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U2 - 10.1127/pala/2019/0088
DO - 10.1127/pala/2019/0088
M3 - Article
AN - SCOPUS:85071003818
SN - 0375-0442
VL - 314
SP - 11
EP - 68
JO - Palaeontographica, Abteilung A: Palaozoologie - Stratigraphie
JF - Palaeontographica, Abteilung A: Palaozoologie - Stratigraphie
IS - 1-3
ER -