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High Arabian Sea productivity conditions during MIS 13-odd monsoon event or intensified overturning circulation at the end of the Mid-Pleistocene transition? ArchiMer
Ziegler, M.; Lourens, L. J.; Tuenter, E.; Reichart, G. -j..
Marine isotope stage (MIS) 13 (similar to 500 000 years ago) has been recognized as atypical in many paleoclimate records and, in particular, it has been connected to an exceptionally strong summer monsoon throughout the Northern Hemisphere. Here, we present a multi-proxy study of a sediment core taken from the Murray Ridge at an intermediate water depth in the northern Arabian Sea that covers the last 750 000 years. Our results indicate that primary productivity conditions were anomalously high during MIS 13 in the Arabian Sea and led to extreme carbonate dissolution and glauconitization in the deep-sea sediments. These observations could be explained by increased wind driven upwelling of nutrient-rich deep waters and, hence, by the occurrence of an...
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Ano: 2010 URL: https://archimer.ifremer.fr/doc/00218/32903/33069.pdf
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