Use of Proxies in Paleoceanography. Examples from the South Atlantic.

Fischer, Gerhard and Wefer, Gerold (eds.).

ISBN 10: 3540663401 / ISBN 13: 9783540663409

Published by Berlin / Heidelberg, Springer, 1999

About this Item

X, 735 pp. -TEXT IN ENGLISH- Sprache: Englisch Gewicht in Gramm: 1700 4to. Hardcover, no dust jacket, binding slightly rubbed, paper a bit browned, all in all very fine.

Seller Inventory # 322495

Bibliographic Details

• Title: Use of Proxies in Paleoceanography. Examples from the South Atlantic.
• Publisher: Berlin / Heidelberg, Springer
• Publication Date: 1999
• Language: English
• ISBN 10: 3540663401
• ISBN 13: 9783540663409
• Binding: Hardcover
• Weight: 1700 grams
• Seller catalogs:
  • Geologie

About this title

Synopsis

Paleoceanographic proxies provide infonnation for reconstructions of the past, including climate changes, global and regional oceanography, and the cycles of biochemical components in the ocean. These prox­ ies are measurable descriptors for desired but unobservable environmental variables such as tempera­ ture, salinity, primary productivity, nutrient content, or surface-water carbon dioxide concentrations. The proxies are employed in a manner analogous to oceanographic methods. The water masses are first characterized according to their specific physical and chemical properties, and then related to particular assemblages of certain organisms or to particular element or isotope distributions. We have a long-standing series of proven proxies available. Marine microfossil assemblages, for instance, are employed to reconstruct surface-water temperatures. The calcareous shells of planktonic and benthic microorgan­ isms contain a wealth of paleoceanographic information in their isotopic and elemental compositions. Stable oxygen isotope measurements are used to detennine ice volume, and MglCa ratios are related to water temperatures, to cite a few examples. Organic material may also provide valuable infonnation, e. g. , about past productivity conditions. Studying the stable carbon isotope composition of bulk organic matter or individual marine organic components may provide a measure of past surface-water CO 2 conditions within the bounds of certain assumptions. Within the scope of paleoceanographic investigations, the existing proxies are continuously evolving and improving, while new proxies are being studied and developed. The methodology is improved by analysis of samples from the water column and surface sediments, and through laboratory experiments.