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  • 1
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    In:  EPIC3Geophysical Research Abstracts 13, EGU2011-10226, EGU General Assembly 2011.
    Publikationsdatum: 2019-07-16
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Conference , notRev
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
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    AGU (American Geophysical Union)
    In:  Paleoceanography, 17 (2). p. 1025.
    Publikationsdatum: 2017-05-10
    Beschreibung: Ice sheets in the North American Arctic and, to a lesser extent, those in northern Eurasia calved large quantities of icebergs that drifted through Fram Strait into the Greenland Sea several times during the late Pleistocene. These icebergs deposited Fe oxide grains (45–250 mm) and coarse lithic clasts 〉250 mm matched to specific circum-Arctic sources. Four massive Arctic iceberg export events are identified from the Laurentide and the Innuitian ice sheets, between 14 and 34 ka (calendar years) in a sediment core from Fram Strait. These relatively short duration (〈1–4 kyr) events contain 3–5 times the background levels of Fe oxide grains. They began suddenly, as indicated by a steep rise in the number of grains matched to an ice sheet source, suggesting rapid purges of ice through Fram Strait, due perhaps to collapse of ice sheets. The larger events from the northwestern Laurentide ice sheet are preceded by events from the Innuitian ice sheet. Despite the chronological uncertainties, the Arctic export events appear to occur prior to Heinrich events.
    Materialart: Article , PeerReviewed
    Format: text
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    Publikationsdatum: 2015-03-14
    Beschreibung: A bstract :  An accurate method of determining source locations for detrital sediment is presented using the chemical composition of Fe-oxide minerals like a fingerprint. This method is an improvement in the use of Fe-oxide minerals for provenance determinations because it requires less time and fewer source samples. A rigorous test of the method uses a database of more than 38,000 grains from known locations. The average error of matching grains back to 45 source locations designated for this database is less than 2%. The method allows for proportional matching of a grain to multiple sources if other grains in the source database meet the compositional match criteria, which helps reduce the error of incorrect matches. Most provenance studies do not involve source basins as large as the entire Arctic Ocean, where sediment can be ice-rafted several thousand kilometers. For most studies, only a few samples (~ 100 grain analyses/sample) would be required to characterize a source if strategically placed, such as near a river mouth. Deposits more than 40 million years old can be traced to specific sources using this method because Fe-oxide grains are relatively stable in most deposits.
    Print ISSN: 1527-1404
    Thema: Geologie und Paläontologie
    Standort Signatur Einschränkungen Verfügbarkeit
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