Titlebook: Reconstructing Ocean History; A Window into the Fu Fatima Abrantes,Alan C. Mix Book 1999 Springer Science+Business Media New York 1999 Atla

GLUT

An Introduction to “Biotic Responses to Major Paleoceanographic Changes”npronounceable names of microfossils showing which ones survived being hit by an asteroid”. This response would be very wide of the mark. The “biotic response” session reflected a recent trend in paleoceanographic research that in my personal opinion is particularly fruitful: the integration of rese

Precursor

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nauseate

Antagonist

commonsense

Polar Stratospheric Cloud Forcing in a Greenhouse Worldin regions of very low temperature and as a result the clouds only exist in winter stratospheric polar regions. The formation of Type II PSCs may be linked to tropospheric methane concentrations because oxidation of tropospheric methane is a significant source of stratospheric water vapor. It has be

Fecundity

Variability of Extreme Cretaceous-Paleogene Climatese present evidence from ODP Leg 171 drilling at Blake Nose for climate variability during the Late Paleocene Thermal Maximum (LPTM) and late Albian-early Cenomanian time periods. Borehole logs and continuous core measurements, such as magnetic susceptibility and color variations, reveal that most of

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Innovations in Monitoring Ocean History. Research presented at ICP6 and in this volume demonstrate that development of new tracers and refinement of existing ones are both highly active research areas. Available proxies fall into three broad categories: biotic, chemical, and sedimentological. The chemical proxies are the largest group an

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Deconvolving Glacial Ocean Carbonate Chemistry from the Planktonic Foraminifera Carbon Isotope RecorLast Glacial Maximum (LGM). One of the more widely accepted clues for this mechanism is the observation that the carbon isotopic composition (δ.C) of glacial planktic and benthic foraminifera was more negative relative to the Holocene (Curry and Crowley, 1987; Shackleton, 1977; Shackleton .., 1992).

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