Manual Proxies in Late Cenozoic Paleoceanography

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Graham D. Strontium-calcium ratios in Cenozoic planktonic foraminifera. Geochimica et Cosmochimica Acta, Grossman E. Stable isotope in modern benthic foraminifera: A study of vital effect. Journal of Foraminiferal Research, 17 1 Guiot J. Transfer functions: methods for qualitative paleoceanography based on microfossils. In: C. De Vernal. Hampt G Delaney M. In: Shackleton N.

Proceedings of the Ocean Drilling, Scientific Results. Hall J.

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Traditional and emerging geochemical proxies in foraminifera.

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McArthur J. S, Chen M. Strontium isotope stratigraphy in the Late Cretaceous: numerical calibration of the Sr isotope curve and intercontinental correlation for the Campanian. Paleoceanography, Mitchell S. Carbon isotopes and sequence stratigraphy. In: Howell, J. High resolution sequence stratigraphy: innovations and applications.

Geological Society Special Publication, Stratigraphic revisions and correlations to an inferred galcioeustatic record. Paleoceanography, 9 3 Ravelo A. The use of oxygen and carbon isotopes of foraminifera in paleoceanography. In:Hillaire-Marcel, C. Proxies in late Cenozoic. Schackleton N. Learn how to enable JavaScript on your browser. NOOK Book. The present volume is the first in a series of two books dedicated to the paleoceanography of the Late Cenozoic ocean. The need for an updated synthesis on paleoceanographic science is urgent, owing to the huge and very diversified progress made in this domain during the last decade.

In addition, no comprehensive monography still exists in this domain. This is quite incomprehensible in view of the contribution of paleoceanographic research to our present understanding of the dynamics of the climate-ocean system. The focus on the Late Cenozoic ocean responds to two constraints. Firstly, most quantitative methods, notably those based on micropaleontological approaches, cannot be used back in time beyond a few million years at most. Secondly, the last few million years, with their strong climate oscillations, show specific high frequency changes of the ocean with a relatively reduced influcence of tectonics.

The first volume addresses quantitative methodologies to reconstruct the dynamics of the ocean andthe second, major aspects of the ocean system thermohaline circulation, carbon cycle, productivity, sea level etc. In this first volume, we have gathered up-to-date methodologies for the measurement and quantitative interpretation of tracers and proxies in deep sea sediments that allow reconstruction of a few key past-properties of the ocean temperature, salinity, sea-ice cover, seasonal gradients, pH, ventilation, oceanic currents, thermohaline circulation, and paleoproductivity.

Chapters encompass physical methods conventional grain-size studies, tomodensitometry, magnetic and mineralogical properties , most current biological proxies planktic and benthic foraminifers, deep sea corals, diatoms, coccoliths, dinocysts and biomarkers and key geochemical tracers trace elements, stable isotopes, radiogenic isotopes, and U-series.

Contributors to the book and members of the review panel are among the best scientists in their specialty.

They represent major European and North American laboratories and thus provide a priori guarantees to the quality and updat of the entire book. Scientists and graduate students in paleoclimatology, paleoceanography, climate modeling, and undergraduate and graduate students in marine geology represent the target audience. See All Customer Reviews. Shop Books.

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Proxies in Late Cenozoic Paleoceanography, Volume 1 - 1st Edition

Add to Wishlist. USD Sign in to Purchase Instantly. Explore Now. Buy As Gift. Overview The present volume is the first in a series of two books dedicated to the paleoceanography of the Late Cenozoic ocean. Presents updated techniques and methods in paleoceanography Reviews the state-of-the-art interpretation of proxies used for quantitative reconstruction of the climate-ocean system Acts as a supplement for undergraduate and graduate courses in paleoceanography and marine geology.

Product Details Table of Contents. Clay Minerals, Deep Circulation and Climate 5.

Chapter Eighteen The Use of Oxygen and Carbon Isotopes of Foraminifera in Paleoceanography

Diatoms: From Micropaleontology to Isotope Geochemistry 9. Biomarkers as Paleoceanographic Proxies Show More. Average Review. Write a Review.