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  Could changing ocean circulation have destabilized methane hydrate at the Paleocene/Eocene boundary?

Bice, K., & Marotzke, J. (2002). Could changing ocean circulation have destabilized methane hydrate at the Paleocene/Eocene boundary? Paleoceanography, 17(2): 1018. doi:10.1029/2001PA000678.

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Paleocean-17-2002-8-1.pdf (Verlagsversion), 2MB
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 Urheber:
Bice, K.L.1, Autor
Marotzke, Jochem1, Autor           
Affiliations:
1external, ou_persistent22              

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Schlagwörter: ABRUPT CLIMATE-CHANGE; THERMAL MAXIMUM; THERMOHALINE CIRCULATION; EOCENE BOUNDARY; ISOTOPE EXCURSION; ATMOSPHERE MODEL; BIGHORN BASIN; FRESH-WATER; SIMULATION; PALEOGENEGeology; Oceanography; Paleontology; paleoceanography; modeling; Paleocene; Eocene; methane; hydrology;
 Zusammenfassung: [1] During the Paleocene-Eocene Thermal Maximum (PETM, similar to55 Ma), marine and terrestrial carbon isotope values exhibit a negative shift of at least 2.5parts per thousand, indicative of massive destabilization of marine methane hydrates, releasing similar to2000 gigatons of methane carbon. The cause of the hydrate destabilization is unknown but has been speculated to be warming due to a change from high-latitude to low-latitude deepwater formation. Here we present results from a numerical ocean model indicating that a sudden switch of deepwater formation from southern to northern high latitudes caused middepth and deep-ocean warming of 3degrees-5degreesC. The switch is caused by a slow increase in the intensity of the atmospheric hydrologic cycle, as expected under increasing temperatures and consistent with PETM sedimentary evidence. Deepened subtropical subduction prior to the thermohaline circulation switch causes warming of 1degrees-4degreesC in limited areas at thermocline through upper intermediate depths, which could destabilize methane hydrates gradually and at progressively greater depths. Warming accompanying a south-to-north switch in deepwater formation would produce sufficient warming to destabilize seafloor gas hydrates over most of the world ocean to a water depth of at least 1900 m.

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Sprache(n): eng - English
 Datum: 20022002
 Publikationsstatus: Erschienen
 Seiten: 16
 Ort, Verlag, Ausgabe: -
 Inhaltsverzeichnis: -
 Art der Begutachtung: Expertenbegutachtung
 Identifikatoren: ISI: 000178940200010
DOI: 10.1029/2001PA000678
Anderer: A [35]
 Art des Abschluß: -

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Titel: Paleoceanography
Genre der Quelle: Zeitschrift
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Ort, Verlag, Ausgabe: Washington, DC : American Geophysical Union
Seiten: - Band / Heft: 17 (2) Artikelnummer: 1018 Start- / Endseite: - Identifikator: ISSN: 0883-8305
CoNE: https://pure.mpg.de/cone/journals/resource/954925549330