The role of the North Pacific Ocean in the deglacial CO₂ rise : insights from trace elements and boron isotopes in biogenic carbonates

The ∼90 ppmv increase in atmospheric CO₂ over the last deglaciation was most likely driven by changes in the way the high latitude oceans regulate the exchange of dissolved inorganic carbon (DIC) between the surface and interior ocean, however the mechanisms involved in this repartitioning remain un...

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Bibliographic Details
Main Author: Gray, W. R.
Published: University College London (University of London) 2015
Subjects:
550
Online Access:http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.639606