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    Publication Date: 2024-02-07
    Description: During the last deglaciation substantial volumes of meltwater from the decaying Laurentide Ice Sheet were supplied to the Arctic, Gulf of Mexico and North Atlantic along different drainage routes, sometimes as catastrophic flood events. These events are suggested to have impacted global climate, for example initiating the Younger Dryas cold period. Here we analyze the authigenic Pb isotopic composition of sediments in front of the Arctic Mackenzie Delta, a sensitive tracer for elevated freshwater runoff of the retreating Laurentide Ice Sheet. Our data reveal continuous meltwater supply to the Arctic along the Mackenzie River since the onset of the Bølling–Allerød. The strongest Lake Agassiz outflow event is observed at the end of the Bølling–Allerød close to the onset of the Younger Dryas. In context of deglacial North American runoff records from the southern and eastern outlets, our findings provide a detailed reconstruction of the deglacial drainage chronology of the disintegrating Laurentide Ice Sheet.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
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    Format: text
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  • 3
    Publication Date: 2022-08-15
    Description: © The Author(s), 2022. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Sufke, F., Gutjahr, M., Keigwin, L. D., Reilly, B., Giosan, L., & Lippold, J. Arctic drainage of Laurentide Ice Sheet meltwater throughout the past 14,700 years. Communications Earth & Environment, 3(1), (2022): 98, https://doi.org/10.1038/s43247-022-00428-3.
    Description: During the last deglaciation substantial volumes of meltwater from the decaying Laurentide Ice Sheet were supplied to the Arctic, Gulf of Mexico and North Atlantic along different drainage routes, sometimes as catastrophic flood events. These events are suggested to have impacted global climate, for example initiating the Younger Dryas cold period. Here we analyze the authigenic Pb isotopic composition of sediments in front of the Arctic Mackenzie Delta, a sensitive tracer for elevated freshwater runoff of the retreating Laurentide Ice Sheet. Our data reveal continuous meltwater supply to the Arctic along the Mackenzie River since the onset of the Bølling–Allerød. The strongest Lake Agassiz outflow event is observed at the end of the Bølling–Allerød close to the onset of the Younger Dryas. In context of deglacial North American runoff records from the southern and eastern outlets, our findings provide a detailed reconstruction of the deglacial drainage chronology of the disintegrating Laurentide Ice Sheet.
    Description: Open Access funding enabled and organized by Projekt DEAL.
    Repository Name: Woods Hole Open Access Server
    Type: Article
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  • 4
    Publication Date: 2022-05-26
    Description: © The Author(s), 2019. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Zhao, N., Oppo, D. W., Huang, K., Howe, J. N. W., Blusztajn, J., & Keigwin, L. D. Glacial-interglacial Nd isotope variability of North Atlantic Deep Water modulated by North American ice sheet. Nature Communications, 10, (2019): 5773, doi: 10.1038/s41467-019-13707-z.
    Description: The Nd isotope composition of seawater has been used to reconstruct past changes in the contribution of different water masses to the deep ocean. In the absence of contrary information, the Nd isotope compositions of endmember water masses are usually assumed constant during the Quaternary. Here we show that the Nd isotope composition of North Atlantic Deep Water (NADW), a major component of the global overturning ocean circulation, was significantly more radiogenic than modern during the Last Glacial Maximum (LGM), and shifted towards modern values during the deglaciation. We propose that weathering contributions of unradiogenic Nd modulated by the North American Ice Sheet dominated the evolution of the NADW Nd isotope endmember. If water mass mixing dominated the distribution of deep glacial Atlantic Nd isotopes, our results would imply a larger fraction of NADW in the deep Atlantic during the LGM and deglaciation than reconstructed with a constant northern endmember.
    Description: This study was supported by National Science Foundation grants (OCE 1335191 and OCE 1811305) to D.W.O. We thank Kathryn Pietro and Mary Carman for help with lab work, Steve Galer and Jerry McManus for helpful discussions. L.D.K. acknowledges the Grayce B. Kerr Fund for supporting research cruise KNR198. N.Z. acknowledges supports by a graduate internship from National Ocean Sciences Accelerator Mass Spectrometry facility and a post-doctoral scholarship from Max Planck Institute for Chemistry. K.-F.H. acknowledges funding from Taiwan MOST (MOST 104-2628-M-001-007-MY3).
    Repository Name: Woods Hole Open Access Server
    Type: Article
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