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Deep ocean carbonate ion increase during mid Miocene CO2 decline

Kender, S.; Yu, Jimin; Peck, V.L.


Characterised by long term cooling and abrupt ice sheet expansion on Antarctica ~14 Ma ago, the mid Miocene marked the beginning of the modern ice-house world, yet there is still little consensus on its causes, in part because carbon cycle dynamics are not well constrained. In particular, changes in carbonate ion concentration ([CO3(2-)]) in the ocean, the largest carbon reservoir of the ocean-land-atmosphere system, are poorly resolved. We use benthic foraminiferal B/Ca ratios to reconstruct...[Show more]

CollectionsANU Research Publications
Date published: 2014
Type: Journal article
Source: Scientific Reports
DOI: 10.1038/srep04187
Access Rights: Open Access


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