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Climate of the Past An interactive open-access journal of the European Geosciences Union
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Volume 13, issue 5
Clim. Past, 13, 533–544, 2017
https://doi.org/10.5194/cp-13-533-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Clim. Past, 13, 533–544, 2017
https://doi.org/10.5194/cp-13-533-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 24 May 2017

Research article | 24 May 2017

A 21 000-year record of fluorescent organic matter markers in the WAIS Divide ice core

Juliana D'Andrilli et al.

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Cited articles

Acree, W. E., Tucker, S. A., and Fetzer, J. C.: Fluorescence Emission Properties of Polycyclic Aromatic Compounds in Review, Polycycl. Aromat. Comp., 2, 75–105, https://doi.org/10.1080/10406639108048933, 1991.
Albani, S., Mahowald, N. M., Murphy, L. N., Raiswell, R., Moore, J. K., Anderson, R. F., McGee, D., Bradtmiller, L. I., Delmonte, B., Hesse, P. P., and Mayewski, P. A.: Paleodust variability since the Last Glacial Maximum and implications for iron inputs to the ocean, Geophys. Res. Lett., 43, 3944–3954, https://doi.org/10.1002/2016GL067911, 2016.
Alley, R. B.: The Two-Mile Time Machine: Ice Cores, Abrupt Climate Change, and Our Future, Princeton University Press, Princeton, New Jersey, 2002.
Balcarczyk, K. L., Jones, J. B., Jaffe, R., and Maie, N.: Stream dissolved organic matter bioavailability and composition in watersheds underlain with discontinuous permafrost, Biogeochemistry, 94, 255–270, https://doi.org/10.1007/s10533-009-9324-x, 2009.
Banta, J. R., McConnell, J. R., Frey, M. M., Bales, R. C., and Taylor, K.: Spatial and temporal variability in snow accumulation at the West Antarctic Ice Sheet Divide over recent centuries, J. Geophys. Res.-Atmos., 113, 10.1029/2008jd010235, 2008.
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Climate-driven trends in fluorescent organic matter (OM) markers from Antarctic ice cores revealed fluctuations over 21.0 kyr, reflecting environmental shifts as a result of global ecosystem response in a warming climate. Precursors of lignin-like fluorescent chemical species were detected as OM markers from the Last Glacial Maximum to the mid-Holocene. Holocene ice contained the most complex lignin-like fluorescent OM markers. Thus, ice cores contain paleoecological OM markers of Earth’s past.
Climate-driven trends in fluorescent organic matter (OM) markers from Antarctic ice cores...
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