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dc.contributor.authorNaik, S.S.
dc.contributor.authorNaidu, P.D.
dc.date.accessioned2015-09-08T09:35:33Z
dc.date.available2015-09-08T09:35:33Z
dc.date.issued2015
dc.identifier.citationGeochemical Journal, vol.49(2 ); 2015; 229-231
dc.identifier.urihttp://drs.nio.org/drs/handle/2264/4785
dc.description.abstractWe assess the usefulness of the empirical boron partition coefficient, K<sub>D</sub> and B/Ca measured from planktonic foraminifera in estimation of pCO<sub>2</sub> using three different relationships between K<sub>D</sub> and temperature derived from various studies. Two sediment cores spanning the last 22 kyr were utilised, one from the intense CO<sub>2</sub> source region of the Western Arabian Sea (WAS) and another from the Eastern Arabian Sea (EAS). The sea-air difference in pCO<sub>2</sub> at these sites shows results contrary to the present day scenario. Moreover the reconstructions using the three K<sub>D</sub> relationships lead to assorted results which suggests that the K<sub>D</sub> approach may not be suitable in paleo-pCO<sub>2</sub> reconstructions
dc.language.isoen
dc.publisherGeochemical Society of Japan
dc.rightsCopyright [2015]. All efforts have been made to respect the copyright to the best of our knowledge. Inadvertent omissions, if brought to our notice, stand for correction and withdrawal of document from this repository
dc.subjectPALAEO-STUDIES
dc.subjectCHEMISTRY AND BIOGEOCHEMISTRY
dc.subjectPALAEO-STUDIES
dc.titleUse of the Boron partition coefficient ‘K<sub>D</sub>’ and B/Ca from planktonic foraminifera in the estimation of past seawater pCO<sub>2</sub>
dc.typeJournal Article


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