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.
Published in: | Earth and Planetary Science Letters |
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Main Authors: | , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Elsevier
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Subjects: | |
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 |
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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