The Late Quaternary evolution of water masses in the eastern Indian Ocean between Australia and Indonesia, based on benthic foraminifera faunal and carbon isotopes analyses

Benthic foraminifera and carbon isotopes from closely spaced samples taken from three deep-sea cores were analysed to reconstruct the palaeoceanographic evolution of the eastern Indian Ocean for the last 30 kyrs, with an extension back to 60 kyrs based

Bibliographic Details
Published in:Palaeogeography, Palaeoclimatology, Palaeoecology
Main Authors: Murgese, David, De Deckker, Patrick
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier
Subjects:
Keywords: accumulation rate
Antarctic Intermediate Water
benthic foraminifera
carbon isotope
dissolved oxygen
fauna
isotopic analysis
Last Glacial Maximum
oceanic circulation
oceanic current
organic matter
paleoceanography
paleoproductivity
Q factor
Q Antarctic Intermediate Water
Benthic foraminifer accumulation rate
Bulimina aculeata
Delta 13C
Indian Ocean water masses
Productivity
South Java Upwelling
Antarctic
Indian
Antarc*
Online Access:http://hdl.handle.net/1885/52360
https://doi.org/10.1016/j.palaeo.2006.11.002
https://openresearch-repository.anu.edu.au/bitstream/1885/52360/5/late_quaternary_evolution.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/52360/7/01_Murgese_The_Late_Quaternary_evolution_2007.pdf.jpg
Description
Summary:Benthic foraminifera and carbon isotopes from closely spaced samples taken from three deep-sea cores were analysed to reconstruct the palaeoceanographic evolution of the eastern Indian Ocean for the last 30 kyrs, with an extension back to 60 kyrs based

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