Carbon Cycling in the Glacial Ocean: Constraints on the - download pdf or read online

By Ingeborg Levin (auth.), Rainer Zahn, Thomas F. Pedersen, Michael A. Kaminski, Laurent Labeyrie (eds.)

ISBN-10: 3642787371

ISBN-13: 9783642787379

ISBN-10: 3642787398

ISBN-13: 9783642787393

A finished development document at the multi-disciplinary box of ocean and weather switch examine is given. It compiles introductory history papers and prime clinical effects at the ocean-atmosphere carbon cycle with emphasis at the ocean's carbon stock and some of the parts concerned. the connection among plankton productiveness, carbon fixation, oceanic PCO2 and weather swap is investigated from the perspective of long term climatic switch in the course of the overdue Quaternary cycles of ice a long time and hot a long time. some of the techniques diversity from micropaleontology over natural and hint aspect geochemistry to molecular isotope geochemistry.

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Read Online or Download Carbon Cycling in the Glacial Ocean: Constraints on the Ocean’s Role in Global Change: Quantitative Approaches in Paleoceanography PDF

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Extra info for Carbon Cycling in the Glacial Ocean: Constraints on the Ocean’s Role in Global Change: Quantitative Approaches in Paleoceanography

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Nature 308, 620-624. Sarnthein M, H Erlenkeuser, R von Grafenstein and C Schroder (1984) Stable-isotope stratigraphy for the last 750,000 years: "Meteor" core 13519 from the eastern Atlantic. , Reihe C, 38: 9-24. Siegenthaler U, and T Wenk (1984) Rapid atmospheric C02 variations and ocean circulation. Nature 308: 624-626. Stuiver M, and HD Polach (1977) Discussion reporting of 14C data. Radiocarbon 19: 355-363. Weiss RF (1974) Carbon dioxide in water and sea water: the solubility of a non-ideal gas, Mar.

Assuming that the basic gross world ocean circulation pattern was not too far away from the actual present ocean the approach may be justified. In the first experiment HO (Hydrography Only)the control run velocity field was used and all chemical constants (solubilities, solubility products, mass action constants, rain ratio) computed as if all ocean water temperatures were 2°C lower and salinities would be 1%0 higher than today. In this run nutrients and the carbon cycle tracers had the same initial inventories as in the control run.

ASME, Series D, 35-45. Keir, R (1988) On the late Pleistocene ocean geochemistry and circulation. Paleoceanography 3: 413-446. Knox F, and MB McElroy (\ 984) Changes in atmospheric C02: Influence of the marine biota at high latitude. 1. Geophys. Res. 89: 4629-4637. Kurz KD, and E Maier-Reimer (1992) Iron fertilization of the Austral Ocean -- the Hamburg Model assessment. Global Biogeochem. Cyc. 7: 229-244. Labeyrie LD, JC Duplessy, and PL Blanc (1987) VaIiations in mode of fOimation and temperature of oceanic deep waters over the past 125,000 years.

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Carbon Cycling in the Glacial Ocean: Constraints on the Ocean’s Role in Global Change: Quantitative Approaches in Paleoceanography by Ingeborg Levin (auth.), Rainer Zahn, Thomas F. Pedersen, Michael A. Kaminski, Laurent Labeyrie (eds.)


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