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Stable isotope ratios from sediment core MD76-131
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(Table S1) Age determination of sediment cores SK99_17 and MD76-131
Productivity in the Arabian Sea is one of the highest in the world. It is controlled by seasonally reversing monsoonal wind-driven upwelling of nutrient-rich deeper waters which... -
(Appendix 1) Stable carbon and oxygen isotope ratios of Cibicidoides spp. fro...
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(Appendix 1) Stable carbon and oxygen isotope ratios of Cibicidoides spp. fro...
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(Table 2) Stable carbon and oxygen isotope ratios of Globigerinoides ruber fr...
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Sedimentology on core MD76-135
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Stable carbon and oxygen isotope ratios of foraminifera from North Atlantic s...
Oxygen-18 records of benthic foraminifera from the Atlantic Ocean are significantly different from those of the Pacific and Indian Oceans indicating that the Glacial North... -
Composition of sediments from the Arabian Sea
Thirty seven deep-sea sediment cores from the Arabian Sea were studied geochemically (49 major and trace elements) for four time slices during the Holocene and the last glacial,... -
Stable isotope on G. ruber w of sediment core MD76-132
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Stable isotope on G. ruber w of sediment core MD76-135
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Stable isotope on G. ruber w of sediment core MD76-136
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Sedimentology on core MD76-123
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Sedimentology on core MD76-125
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Sedimentology on core MD76-132
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Sedimentology on core MD76-128
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Sedimentology on core MD76-136
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Sedimentology on core MD76-135
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Sedimentology on core MD76-127
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Last Glacial Maximum seawater temperature estimates based on planktonic foram...
Estimates of Last Glacial Maximum annual mean seawater temperatures at 50 m depth. The temperature estimates are derived using the Modern Analogue Technique using the ForCenS... -
Geochemistry of surface sediments from the Indian Ocean
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