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An event stratigrap...
An event stratigraphy for the Last Termination in the North Atlantic region based on the Greenland Ice-core record: a proposal by the INTIMATE group.
- Article/chapterEnglish1998
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Numbers
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LIBRIS-ID:oai:DiVA.org:lnu-17013
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https://urn.kb.se/resolve?urn=urn:nbn:se:lnu:diva-17013URI
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https://doi.org/10.1002/(SICI)1099-1417(199807/08)13:4<283::AID-JQS386>3.0.CO;2-ADOI
Supplementary language notes
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Language:English
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Summary in:English
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Classification
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Subject category:ref swepub-contenttype
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Subject category:art swepub-publicationtype
Notes
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It is suggested that the GRIP Greenland ice-core should constitute the stratotype for the Last Termination. Based on the oxygen isotope signal in that core, a new event stratigraphy spanning the time interval from ca. 22.0 to 11.5 k GRIP yr BP (ca. 19.0-10.0 k C-14 yr BP) is proposed for the North Atlantic region. This covers the period from the Last Glacial Maximum, through Termination 1 of the deep-ocean record, to the Pleistocene-Holocene boundary, and encompasses the Last Glacial Late-glacial of the traditional northwest European stratigraphy. The isotopic record for this period is divided into two stadial episodes, Greenland Stadials 1 (GS-1) and 2 (GS-2), and two interstadial events, Greenland Interstadials 1 (GI-1) and 2 (GI-2). In addition, GI-1 and GS-2 are further subdivided into shorter episodes. The event stratigraphy is equally applicable to ice-core, marine and terrestrial records and is considered to be a more appropriate classificatory scheme than the terrestrially based radiocarbon-dated chronostratigraphy that has been used hitherto.
Subject headings and genre
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Paleoecology
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Paleoekologi
Added entries (persons, corporate bodies, meetings, titles ...)
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Walker, M.J.C.
(author)
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Cwynar, L.C.
(author)
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Johnsen, S.
(author)
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Knudsen, K.-L.
(author)
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Lowe, J.J.
(author)
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Wohlfarth, B.
(author)
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Högskolan i KalmarNaturvetenskapliga institutionen
(creator_code:org_t)
Related titles
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In:Journal of Quaternary Science13:4, s. 283-2920267-81791099-1417
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