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Biogenic and detrital-rich intervals in central Arctic Ocean cores identified using x-ray fluorescence scanning
Stockholm Univ, Dept Geol Sci, SE-10691 Stockholm, Sweden..
Natl Taiwan Univ, Dept Geosci, Taipei 106, Taiwan.;Alfred Wegener Inst Polar & Marine Res, Climate Sci Div, DE-27570 Bremerhaven, Germany..
Stockholm Univ, Dept Geol Sci, SE-10691 Stockholm, Sweden..
Responsible organisation
2013 (English)In: Polar Research, ISSN 0800-0395, E-ISSN 1751-8369, Vol. 32, 18386Article in journal (Refereed) Published
Abstract [en]

X-ray fluorescence (XRF) scanning of sediment cores from the Lomonosov Ridge and the Morris Jesup Rise reveals a distinct pattern of Ca intensity peaks through Marine Isotope Stages (MIS) 1 to 7. Downcore of MIS 7, the Ca signal is more irregular and near the detection limit. Virtually all major peaks in Ca coincide with a high abundance of calcareous microfossils; this is particularly conspicuous in the cores from the central Arctic Ocean. However, the recorded Ca signal is generally caused by a combination of biogenic and detrital carbonate, and in areas influenced by input from the Canadian Arctic, detrital carbonates may effectively mask the foraminiferal carbonates. Despite this, there is a strong correlation between XRF-detected Ca content and foraminiferal abundance. We propose that in the Arctic Ocean north of Greenland a common palaeoceanographic mechanism is controlling Ca-rich ice-rafted debris (IRD) and foraminiferal abundance. Previous studies have shown that glacial periods are characterized by foraminfer-barren sediments. This implies that the Ca-rich IRD intervals with abundant foraminifera were most likely deposited during interglacial periods when glaciers left in the Canadian Arctic Archipelago were still active and delivered a large amount of icebergs. At the same time, conditions were favourable for planktic foraminifera, resulting in a strong covariance between these proxies. Therefore, we suggest that the XRF scanner's capability to efficiently map Ca concentrations in sediment cores makes it possible to systematically examine large numbers of cores from different regions to investigate the palaeoceanographic reasons for the calcareous microfossils' spatial and temporal variability.

Place, publisher, year, edition, pages
2013. Vol. 32, 18386
Keyword [en]
Foraminifera, Arctic Ocean, IRD, calcareous microfossils, XRF scanning
National Category
Natural Sciences
Research subject
SWEDARCTIC 2007, LOMROG
Identifiers
URN: urn:nbn:se:polar:diva-2354DOI: 10.3402/polar.v32i0.18386ISI: 000314828200001OAI: oai:DiVA.org:polar-2354DiVA: diva2:858736
Available from: 2015-10-05 Created: 2015-10-05 Last updated: 2016-11-11

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CiteExportLink to record
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