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The Timing of the Postglacial Marine Invasion of Kau Bay, Halmahera, Indonesia

Bibliographic Data

ID9245295
AuthorsD M Barmawidjaja, A F M De Jong, Klaas Van Der Borg (0000-0002-5999-2804), W A van der Kaars, W J M van der Linden, W J Zachariasse
Year1989
Volume31
Issue03
Pages948-956
Publication date1989-01-01
Open AccessNo
TypeARTICLE
VenueRadiocarbon (JOURNAL)
Journal identifiersISSN: 0033-8222 • E-ISSN: 1945-5755
PublisherCambridge University Press (CUP) (PUBLISHER)
DOI10.1017/s0033822200012571
OpenAlexW2506040471
LanguageEN

Kau Bay Halmahera, Indonesia is a small marine basin that is separated from the adjacent SW Pacific Ocean by a shallow sill, 40m deep. Radiocarbon dating on piston cores in combination with a study on microfossils demonstrate that Kau Bay was a freshwater lake in Weichselian times. At 10,000 BP, the Bay became reconnected with the open ocean. It sill depth did not change in the intervening years, sea level at 10,000 BP stood 40m below the present level

Bay · Geochemistry · Radiocarbon dating · Sill · Structural basin · Volcano · Geological and Geophysical Studies · Geology · Oceanography · Paleontology

Highly citedNo

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