2015 GSA Annual Meeting in Baltimore, Maryland, USA (1-4 November 2015)

Paper No. 67-9
Presentation Time: 3:45 PM

TROPICAL OSTRACOD DIVERSITY AND PALEOBIOGEOGRAPHY IN THE INDO-PACIFIC


SHIN, Caren, School of Biological Sciences, The University of Hong Kong, Kadoorie Biological Sciences Building, The University of Hong Kong, Pokfulam Road, Hong Kong, Hong Kong, IWATANI, Hokuto, School of Biological Sciences and the Swire Institute of Marine Science, The University of Hong Kong, Kadoorie Biological Sciences Building, The University of Hong Kong, Pokfulam Road, Hong Kong, Hong Kong, KASE, Tomoki, Department of Geology and Paleontology, National Museum of Nature and Science, Tokyo, Department of Geology and Paleontology, National Museum of Nature and Science, 4-1-1 Amakubo, Tsukuba, Ibaraki 305-0005, Tokyo, Japan and YASUHARA, Moriaki, School of Biological Sciences, Department of Earth Sciences, and Swire Institute of Marine Sciences, The University of Hong Kong, Kadoorie Biological Sciences Building, The University of Hong Kong, Pokfulam Road, Hong Kong, Hong Kong, h1180279@connect.hku.hk

The Southeast Asian shallow marine area situated between the Indian and Pacific Oceans currently exhibits incredible marine biodiversity, and is well known as the Coral Triangle or the Indo-Australian Archipelago (IAA) biodiversity hotspot. However, Cenozoic paleobiogeography of this region remains unclear except for larger benthic foraminifera, a relatively well-studied tropical taxon. We investigate Cenozoic history of the IAA hotspot using shallow marine Indonesian and Philippine ostracods (Crustacea) from the Mid-Miocene, Pliocene and Pleistocene. A diverse, extant class abundantly found and well-preserved in the fossil record, fossil ostracods may indicate community, habitat and environmental changes in the epochs examined. In Mid-Miocene outcrop samples, lower species diversity and fewer individuals were observed compared with those from the Plio-Pleistocene. Further work aims to determine potential factors or contributing mechanisms for this surge in diversity, and to investigate this increase at a finer time scale.
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