Articles | Volume 6, issue 1
Clim. Past, 6, 63–76, 2010
https://doi.org/10.5194/cp-6-63-2010
Clim. Past, 6, 63–76, 2010
https://doi.org/10.5194/cp-6-63-2010

  29 Jan 2010

29 Jan 2010

High Arabian Sea productivity conditions during MIS 13 – odd monsoon event or intensified overturning circulation at the end of the Mid-Pleistocene transition?

M. Ziegler et al.

Related subject area

Subject: Ocean Dynamics | Archive: Marine Archives | Timescale: Pleistocene
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Cited articles

Adler, M., Hensen, C., Wenzhoefer, F., Pfeifer, K., and Schulz, H. D.: Modeling of calcite dissolution by oxic respiration in supralysoclinal deep-sea sediments, Mar. Geol., 177(1–2), 167–189, 2001.
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. Micropalontol., 40(3), 295–319, 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(6868), 159–162, 2002.
Anderson, D. M., Overpeck, J. T., and Gupta, A. K.: Increase in the Asian Southwest Monsoon During the Past Four Centuries, Science, 297(5581), 596–599, 2002.
Barker, S., Archer, D., Booth, L., Elderfield, H., Henderiks, J., and Rickaby, R. E. M.: Globally increased pelagic carbonate production during the Mid-Brunhes dissolution interval and the CO2 paradox of MIS 11, Quaternary Sci. Rev., 25, 3278–3293, 2006.
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