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Ursula Quillmann

Biographic Data

ID6372789
NAMEUrsula Quillmann
GIVEN NAMESUrsula
FAMILY NAMEQuillmann
SIGNATUREQUILLMANN U
AFFILIATIONSUniversity of Colorado System
VERIFIEDNo
TOTAL WORKS2
TOTAL CITATIONS0
WORKS AS AUTHOR2
WORKS AS EDITOR0
FIRST PUBLICATION YEAR2012
LATEST PUBLICATION YEAR2013
H-INDEX0
  • Holocene changes in marine productivity and terrestrial organic carbon inputs into an Icelandic fjord

    Open Access•Heiko Moossen, Richard Abell et al.•ARTICLE•The Holocene•2013•References: 13

    This study examines the dynamics of organic carbon contributions from different sources to the sediments of a ~39 m core from Ísafjarðardjúp Fjord, Northwest Iceland, throughout the Holocene. Furthermore, it shows that the variability of terrestrial organic carbon (OC terr ) and marine organic carbon (OC mar ) is linked to palaeoclimatic change throughout the Holocene. glycerol-dialkyl-glycerol-tetraether (GDGT), alkenone, n-alkane, total OC and …

  • Cooling and freshening at 8.2 ka on the NW Iceland Shelf recorded in paired δ 18 O and Mg/Ca measurements of the benthic foraminifer Cibicides lobatulus

    Open Access•Ursula Quillmann, Thomas M Marchitto et al.•ARTICLE•Quaternary Research•2012

    A shallow marine sediment core from NW Iceland provides evidence for a brief cooling and freshening at ~ 8200 cal yr BP, consistent with the hypothesis that the catastrophic outburst flood of the proglacial lakes Oijbway and Agassiz caused the 8.2 ka event. This is the first high-resolution record reconstructing near-surface temperatures and δ 18 O sw by paired measurements of Mg/Ca and δ 18 O calcite of a benthic foraminifer. We developed a new …

No prominent works on this page.

  • Cooling and freshening at 8.2 ka on the NW Iceland Shelf recorded in paired δ 18 O and Mg/Ca measurements of the benthic foraminifer Cibicides lobatulus

    Open Access•Ursula Quillmann, Thomas M Marchitto et al.•ARTICLE•Quaternary Research•2012

    A shallow marine sediment core from NW Iceland provides evidence for a brief cooling and freshening at ~ 8200 cal yr BP, consistent with the hypothesis that the catastrophic outburst flood of the proglacial lakes Oijbway and Agassiz caused the 8.2 ka event. This is the first high-resolution record reconstructing near-surface temperatures and δ 18 O sw by paired measurements of Mg/Ca and δ 18 O calcite of a benthic foraminifer. We developed a new …

  • Holocene changes in marine productivity and terrestrial organic carbon inputs into an Icelandic fjord

    Open Access•Heiko Moossen, Richard Abell et al.•ARTICLE•The Holocene•2013•References: 13

    This study examines the dynamics of organic carbon contributions from different sources to the sediments of a ~39 m core from Ísafjarðardjúp Fjord, Northwest Iceland, throughout the Holocene. Furthermore, it shows that the variability of terrestrial organic carbon (OC terr ) and marine organic carbon (OC mar ) is linked to palaeoclimatic change throughout the Holocene. glycerol-dialkyl-glycerol-tetraether (GDGT), alkenone, n-alkane, total OC and …

Geology and Paleoclimatology Research (2 works) · Isotope Analysis in Ecology (2 works) · Alkenone (1 work) · Arctic (1 work) · Benthic zone (1 work) · Calcite (1 work) · Climate change (1 work) · Ecology (1 work) · Environmental change (1 work) · Environmental Science (1 work)

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