Use of proxies in paleoceanography examples from the South Atlantic Libro electrónico

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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Main Authors: Fischer, Gerhard editor, Wefer, Gerold editor/a
Format: Texto biblioteca
Language:eng
Published: New York, New York, United States Springer c199
Subjects:Paleoceanography,
Online Access:http://link.springer.com/openurl?genre=book&isbn=978-3-642-63681-3
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id KOHA-OAI-ECOSUR:55926
record_format koha
institution ECOSUR
collection Koha
country México
countrycode MX
component Bibliográfico
access En linea
En linea
databasecode cat-ecosur
tag biblioteca
region America del Norte
libraryname Sistema de Información Bibliotecario de ECOSUR (SIBE)
language eng
topic Paleoceanography
Paleoceanography
spellingShingle Paleoceanography
Paleoceanography
Fischer, Gerhard editor
Wefer, Gerold editor/a
Use of proxies in paleoceanography examples from the South Atlantic Libro electrónico
description 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.
format Texto
topic_facet Paleoceanography
author Fischer, Gerhard editor
Wefer, Gerold editor/a
author_facet Fischer, Gerhard editor
Wefer, Gerold editor/a
author_sort Fischer, Gerhard editor
title Use of proxies in paleoceanography examples from the South Atlantic Libro electrónico
title_short Use of proxies in paleoceanography examples from the South Atlantic Libro electrónico
title_full Use of proxies in paleoceanography examples from the South Atlantic Libro electrónico
title_fullStr Use of proxies in paleoceanography examples from the South Atlantic Libro electrónico
title_full_unstemmed Use of proxies in paleoceanography examples from the South Atlantic Libro electrónico
title_sort use of proxies in paleoceanography examples from the south atlantic libro electrónico
publisher New York, New York, United States Springer
publishDate c199
url http://link.springer.com/openurl?genre=book&isbn=978-3-642-63681-3
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spelling KOHA-OAI-ECOSUR:559262021-01-11T22:00:26ZUse of proxies in paleoceanography examples from the South Atlantic Libro electrónico Fischer, Gerhard editor Wefer, Gerold editor/a textNew York, New York, United States Springerc1999engPaleoceanographic 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.Incluye bibliografía e índice: páginas 729-735Chapter 1. Introduction.. Chapter 2. Surface water circulation.. Chapter 3. Bottom- and deep water circulation.. Chapter 4. Paleoproductivity and nutrients.. Chapter 5. Co2 in oceans and atmosphere.. Chapter 6. Atmospherical circulation.. Chapter 7. Environmental magnetism.. Chapter 8. Modelling.. Chapter 9. Data management.. Subject IndexPaleoceanographic 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.Disponible en formato PDFSubscripción a ELSEVIERPaleoceanographyDisponible en líneahttp://link.springer.com/openurl?genre=book&isbn=978-3-642-63681-3URN:ISBN:3540663401URN:ISBN:9783642636813 (Print)URN:ISBN:9783642586460 (Online)Disponible para usuarios de ECOSUR con su clave de acceso