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Use of Proxies in Paleoceanography - Examples from the South Atlantic (Paperback, Softcover reprint of the original 1st ed. 1999)
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Use of Proxies in Paleoceanography - Examples from the South Atlantic (Paperback, Softcover reprint of the original 1st ed. 1999)
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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.
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