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Salinity changes in the Agulhas leakage area recorded by stable hydrogen isotopes of C-37 alkenones during Termination I and II ArchiMer
Kasper, Sebastian; Van Der Meer, M. T. J.; Mets, A.; Zahn, R.; Damste, J. S. Sinninghe; Schouten, S..
At the southern tip of Africa, the Agulhas Current reflects back into the Indian Ocean causing so-called "Agulhas rings" to spin off and release relatively warm and saline water into the South Atlantic Ocean. Previous reconstructions of the dynamics of the Agulhas Current, based on paleo-sea surface temperature and sea surface salinity proxies, inferred that Agulhas leakage from the Indian Ocean to the South Atlantic was reduced during glacial stages as a consequence of shifted wind fields and a northwards migration of the subtropical front. Subsequently, this might have led to a buildup of warm saline water in the southern Indian Ocean. To investigate this latter hypothesis, we reconstructed sea surface salinity changes using alkenone delta D, and...
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Ano: 2014 URL: https://archimer.ifremer.fr/doc/00274/38488/36959.pdf
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