Cenozoic evolution of the Indonesian Throughflow and the origins of Indo-Pacific marine biodiversity: Mapping the biotic response to environmental change.
The research aim of THROUGHFLOW is to establish a greater understanding of key processes in the biotic response of coral reefs to long-term environmental changes resulting from closure of the Indonesian Throughflow during the Oligocene-Miocene transition (~25 Million years ago). This will establish important baseline data on which researchers can model the impact of predicted environmental change on present reef ecosystems.
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The mollusc Architectonica songoensis (Martin 1914) The coral Odontocyathus radiatus Gert, 1923 The benthic foraminifera Pseudotaberina
Kali Songo,Java, on ofour fieldwork areas East Kalimantan, our other fieldwork area malabarica from our research area in Java
