Change in the intensity of low-salinity water inflow from the Bay of Bengal into the Eastern Arabian Sea from the Last Glacial Maximum to the Holocene: Implications for monsoon variations

Palaeogeography, Palaeoclimatology, Palaeoecology

Volumn 397, Issue , 2014, Pages 31-37

  Mahesh, B S ^a,b   Banakar, V K ^a  

^a NATIONAL INSTITUTE OF OCEANOGRAPHY   (India)

^b NATIONAL CENTRE FOR ANTARCTIC AND OCEAN RESEARCH   (India)

Author keywords

Arabian Sea; Indian monsoon; Paleo salinity; Paleo Sea Surface Temperature; Planktonic foraminifera 18O and Mg Ca

Indexed keywords

EID: 84894277277     PISSN: 00310182     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.palaeo.2013.05.024     Document Type: Article

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