Younger Dryas-Holocene temperature and rainfall history of southern Indonesia from δ 18 O in speleothem calcite and fluid inclusions

We have applied a new technique to analyze the oxygen (δ18O) and hydrogen (δD) isotope ratios in speleothem fluid inclusions to reconstruct the temperature and rainfall history of southern Indonesia during the Younger Dryas (YD) event and the Holocene.

Bibliographic Details
Published in:Earth and Planetary Science Letters
Main Authors: Griffiths, Michael L, Drysdale, Russell N, Vonhof, Hubert B., Gagan, Michael, Zhao, Jian-xin, Ayliffe, Linda, Hantoro, Wahyoe, Hellstrom, John Charles, Cartwright, Ian, Frisia, Silvia, Suwargadi, Bambang W
Format: Article in Journal/Newspaper
Language:unknown
Published: Elsevier
Subjects:
Keywords: Air temperature
Deglacial
Eustatic sea-level rise
Fluid inclusion
High-elevation snow
Holocenes
In-phase
Indonesia
Intertropical convergence zone
Isotope ratio
Monsoon rainfall
Planktonic foraminifera
Rapid cooling
Sea surface temperatures
S Fluid inclusions
Monsoon
Speleothem
Stable isotopes
Younger Dryas
Online Access:http://hdl.handle.net/1885/38671
https://doi.org/10.1016/j.epsl.2010.03.018
https://openresearch-repository.anu.edu.au/bitstream/1885/38671/5/Griffiths_Gagan_Younger_Dryas_2010.pdf.jpg
https://openresearch-repository.anu.edu.au/bitstream/1885/38671/7/01_Griffiths_Younger_Dryas-Holocene_2010.pdf.jpg
Description
Summary:We have applied a new technique to analyze the oxygen (δ18O) and hydrogen (δD) isotope ratios in speleothem fluid inclusions to reconstruct the temperature and rainfall history of southern Indonesia during the Younger Dryas (YD) event and the Holocene.

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