2023
DOI: 10.31223/x5r054
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Validation of glacial-interglacial rainfall variations in southwest Sulawesi using Mg/Ca and δ18O in speleothems

Abstract: Speleothem δ18O is widely used as a proxy for rainfall amount in the tropics on glacial-interglacial to interannual scales. However, uncertainties in the interpretation of this renowned proxy pose a vexing problem in tropical paleoclimatology. Here, we present paired measurements of Mg/Ca and δ18O for multiple stalagmites from southwest Sulawesi, Indonesia, that that confirm changes in rainfall amount across ice age terminations. Collectively, the stalagmites span two glacial-interglacial transitions from 380 … Show more

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Cited by 2 publications
(2 citation statements)
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“…The adjusted d 18 O record is interpreted in terms of relative changes in monsoon rainfall on the premise that the d 18 O of tropical rainfall is inversely proportional to rainfall amount. Measurements of Mg/Ca in stalagmites from the Maros karst have validated the large change in d 18 O between drier glacials and wetter interglacials in southwest Sulawesi (Kimbrough, 2016).…”
Section: Methodsmentioning
confidence: 75%
“…The adjusted d 18 O record is interpreted in terms of relative changes in monsoon rainfall on the premise that the d 18 O of tropical rainfall is inversely proportional to rainfall amount. Measurements of Mg/Ca in stalagmites from the Maros karst have validated the large change in d 18 O between drier glacials and wetter interglacials in southwest Sulawesi (Kimbrough, 2016).…”
Section: Methodsmentioning
confidence: 75%
“…The adjusted δ 18 O record is interpreted in terms of relative changes in monsoon rainfall on the premise that the δ 18 O of tropical rainfall is inversely proportional to rainfall amount. Measurements of Mg/Ca in stalagmites from the Maros karst have validated the large change in δ 18 O between drier glacials and wetter interglacials in southwest Sulawesi 62 .…”
Section: Methodsmentioning
confidence: 75%