Deglaciation of the Greenland and Laurentide ice sheets interrupted by glacier advance during abrupt coolings

Young, Nicolás E.; Briner, Jason P.; Miller, Gifford H.; Lesnek, Alia J.; Crump, Sarah E.; Thomas, Elizabeth K.; Pendleton, Simon L.; Cuzzone, Joshua; Lamp, Jennifer; Zimmerman, Susan; Caffee, Marc; Schaefer, Joerg M.

doi:10.1016/j.quascirev.2019.106091

Deglaciation of the Greenland and Laurentide ice sheets interrupted by glacier advance during abrupt coolings

Journal Article · Mon Dec 16 00:00:00 EST 2019 · Quaternary Science Reviews

DOI:https://doi.org/10.1016/j.quascirev.2019.106091· OSTI ID:1905204

Young, Nicolás E. ^[1]; Briner, Jason P. ^[2]; Miller, Gifford H. ^[3]; Lesnek, Alia J. ^[2]; Crump, Sarah E. ^[3]; Thomas, Elizabeth K. ^[2]; Pendleton, Simon L. ^[3]; Cuzzone, Joshua ^[4]; Lamp, Jennifer ^[1]; Zimmerman, Susan ^[5]; Caffee, Marc ^[6]; Schaefer, Joerg M. ^[1]

Columbia Univ., New York, NY (United States). Lamont-Doherty Earth Observatory
Univ. at Buffalo, NY (United States)
Univ. of Colorado, Boulder, CO (United States)
Univ. of California, Irvine, CA (United States)
Lawrence Livermore National Lab. (LLNL), Livermore, CA (United States)
Purdue Univ., West Lafayette, IN (United States)

Understanding patterns of ice-sheet deglaciation is key for predicting the rate of future ice-sheet melt, yet the processes underlying deglaciation remain elusive. The early Holocene (11.7 ka to 8.2 ka; Greenlandian Stage) represents the most recent period when the Laurentide and Greenland ice sheets underwent large-scale recession. Moreover, this ice-sheet recession occurred under the backdrop of regional temperatures that were similar to or warmer than today, and comparable to those projected for the upcoming centuries. Reconstructing Laurentide and Greenland ice sheet behavior during the early Holocene, and elucidating the mechanisms dictating this behavior may serve as a partial analog for future Greenland ice-sheet change in a warming world. Here, we present 123 new ¹⁰Be surface exposure ages from two sites on Baffin Island and southwestern Greenland that constrain the behavior of the Laurentide and Greenland ice sheets, and an independent alpine glacier during the early Holocene. On Baffin Island, we focus on a unique area where moraines deposited by the Laurentide Ice Sheet rest directly adjacent to moraines deposited by an independent alpine glacier. Sixty-one ¹⁰Be ages reveal that advances and/or stillstands of the Laurentide Ice Sheet and an alpine glacier occurred in unison around 11.8 ka, 10.3 ka, and 9.2 ka. Sixty-two ¹⁰Be ages from southwestern Greenland indicate that the Greenland Ice Sheet margin experienced re-advances or stillstands around 11.6 ka, 10.4 ka, 9.1 ka, 8.1 ka, and 7.3 ka. Our results reveal that ice sheets respond to climate perturbations on the same centennial timescale as small alpine glaciers. Further, we hypothesize that during the warming climate of the early Holocene, freshening of the North Atlantic Ocean induced by ice-sheet melt resulted in regional cooling and brief periods of ice-sheet stabilization superimposed on net glacier recession. These observations point to a negative feedback mechanism inherent to melting ice sheets in the Baffin Bay region that slows ice-sheet recession during intervals of otherwise rapid deglaciation.

View Accepted Manuscript (DOE)

Research Organization:: Lawrence Livermore National Laboratory (LLNL), Livermore, CA (United States)

Sponsoring Organization:: National Science Foundation (NSF); USDOE National Nuclear Security Administration (NNSA)

Grant/Contract Number:: AC52-07NA27344

OSTI ID:: 1905204

Report Number(s):: LLNL-JRNL-798584; 1001326

Journal Information:: Quaternary Science Reviews, Journal Name: Quaternary Science Reviews Vol. 229; ISSN 0277-3791

Publisher:: ElsevierCopyright Statement

Country of Publication:: United States

Language:: English

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Journal Article · Fri May 31 20:00:00 EDT 2019 · Quaternary Science Reviews · OSTI ID:1872295

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Data for: Deglaciation of the Greenland and Laurentide ice sheets interrupted by glacier advance during abrupt coolings Young, Nicolas https://doi.org/10.17632/crds8jrgnt The current record is supplemented by this dataset	dataset	January 2019
Data for: Deglaciation of the Greenland and Laurentide ice sheets interrupted by glacier advance during abrupt coolings Young, Nicolas https://doi.org/10.17632/crds8jrgnt.1 The current record is supplemented by this dataset	dataset	January 2019

Deglaciation of the Greenland and Laurentide ice sheets interrupted by glacier advance during abrupt coolings

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