Articles | Volume 13, issue 12
https://doi.org/10.5194/cp-13-1791-2017
https://doi.org/10.5194/cp-13-1791-2017
Research article
 | 
13 Dec 2017
Research article |  | 13 Dec 2017

A multi-proxy analysis of Late Quaternary ocean and climate variability for the Maldives, Inner Sea

Dorothea Bunzel, Gerhard Schmiedl, Sebastian Lindhorst, Andreas Mackensen, Jesús Reolid, Sarah Romahn, and Christian Betzler

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Cited articles

Allen, K., Roberts, S., and Murray, J. W.: Marginal marine agglutinated foraminifera: affinities for mineral phases, J. Micropaleontol., 35, 183–191, https://doi.org/10.1144/jm.18.2.183, 1999.
Almogi-Labin, A., Schmiedl, G., Hemleben, C., Siman-Tov, R., Segl, M., and Meischner, D.: The influence of the NE winter monsoon on productivity changes in the Gulf of Aden, NW Arabian Sea, during the last 530 ka as recorded by foraminifera, Mar. Micropaleontol., 40, 295–319, https://doi.org/10.1016/S0377-8398(00)00043-8, 2000.
Altabet, M. A., Higginson, M. J., and Murray, D. W.: The effect of millennial-scale changes in Arabian Sea denitrification on atmospheric CO2, Nature, 415, 159–162, https://doi.org/10.1038/415159a, 2002.
Alve, E.: Colonization of new habitats by benthic foraminifera: a review, Earth-Sci. Rev., 46, 167–185, https://doi.org/10.1016/S0012-8252(99)00016-1, 1999.
Anderson, R. F., Barker, S., Fleisher, M., Gersonde, R., Goldstein, S. L., Kuhn, G., Mortyn, P. G., Pahnke, K., and Sachs, J. P.: Biological response to millennial variability of dust and nutrient supply in the Subantarctic South Atlantic Ocean, Philos. T. R. Soc. A, 372, 1–17, https://doi.org/10.1098/rsta.2013.0054, 2014.
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Short summary
We investigated a sediment core from the Maldives to unravel the interaction between equatorial climate and ocean variability of the past 200 000 years. The sedimentological, geochemical and foraminiferal data records reveal enhanced dust, which was transported by intensified winter monsoon winds during glacial conditions. Precessional fluctuations of bottom water oxygen suggests an expansion of the Arabian Sea OMZ and a varying inflow of Antarctic Intermediate Water.
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