Joint discussion of sedimentary geochemistry data management systems that cross the waterline
Identifieur interne : 001168 ( Main/Exploration ); précédent : 001167; suivant : 001169Joint discussion of sedimentary geochemistry data management systems that cross the waterline
Auteurs : Cinzia Cervato ; Steven L. Goldstein [États-Unis] ; Ethan L. Grossman ; Kerstin Lehnert [États-Unis] ; John M. Mcarthur [Royaume-Uni]Source :
- Eos, Transactions American Geophysical Union [ 0096-3941 ] ; 2004-11-02.
Abstract
Earth's evolution, its climate history, and the history of life are archived in the chemical and isotopic compositions of marine and terrestrial sediments and fossils found within them. This information provides evidence for crustmantle recycling, bolide impacts, mass extinction events, gas hydrate expulsion, climate cycles, and much more. Much of this geochemical evidence, such as the discoveries of oxygen isotope cycles in Quaternary sediments, enhanced iridium at the Cretaceous/Paleocene boundary and relationships between near‐trench sediments and associated arc volcanics, have overturned paradigms, opened new avenues of inquiry, and helped launch international research programs (e.g., the Deep Sea Drilling Project [DSDP]). In addition to revealing much about important Earth events and processes, geochemical records preserved in marine and terrestrial sediments are increasingly important for the correlation of global records; indeed, for Precambrian and anoxic sediments, chemical and isotopic methods are indispensable and provide the main basis for correlation.
Url:
DOI: 10.1029/2004EO440004
Affiliations:
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This information provides evidence for crustmantle recycling, bolide impacts, mass extinction events, gas hydrate expulsion, climate cycles, and much more. Much of this geochemical evidence, such as the discoveries of oxygen isotope cycles in Quaternary sediments, enhanced iridium at the Cretaceous/Paleocene boundary and relationships between near‐trench sediments and associated arc volcanics, have overturned paradigms, opened new avenues of inquiry, and helped launch international research programs (e.g., the Deep Sea Drilling Project [DSDP]). In addition to revealing much about important Earth events and processes, geochemical records preserved in marine and terrestrial sediments are increasingly important for the correlation of global records; indeed, for Precambrian and anoxic sediments, chemical and isotopic methods are indispensable and provide the main basis for correlation.</div></front></TEI><affiliations><list><country><li>Royaume-Uni</li><li>États-Unis</li></country><region><li>Angleterre</li><li>Grand Londres</li><li>État de New York</li></region><settlement><li>Londres</li></settlement></list><tree><noCountry><name sortKey="Cervato, Cinzia" sort="Cervato, Cinzia" uniqKey="Cervato C" first="Cinzia" last="Cervato">Cinzia Cervato</name><name sortKey="Grossman, Ethan L" sort="Grossman, Ethan L" uniqKey="Grossman E" first="Ethan L." last="Grossman">Ethan L. 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