Equatorial Indian Ocean productivity during the last 33 kyr and possible linkage to Westerly Jet variability

Abstract

The top 1 m radiocarbon dated section of a 5.6 m long sediment core retrieved from the Equatorial Indian Ocean is studied for productivity changes in response to climate variability that have taken place during the last ~33 kyr. The robust indicators of marine productivity such as phytol and brassicasterol exhibit distinctly higher contents (av.5.8 ng/g and 4.8 ng/g respectively) during the LGM (25–17 ky BP) as compared to the succeeding period (16–5 ky BP: av.1.9 ng/g each) and preceding period (33–25 ky BP: av.1.8 and 0.8 ng/g respectively) which suggest increased productivity during the cold and dry climate of the LGM. The C_orgcontent is also relatively higher during this period than the warmer Holocene. However, marginally higher C/N ratios (~7.8) and enrichment of delta¹³ C_org(~-19.8‰) during the LGM than the Holocene (C/N ~6.4 and delta¹³ C_org~- 21.5‰), and also the higher carbon preference index (CPI) of n-alkanes and n-alkanols together suggest the presence of terrestrial organic matter in the sediment. The increased equatorial productivity and terrestrial organic matter input together during the LGM may indicate intensified inter-monsoon equatorial Westerly Jets resulting in elevated productivity