Laurentide Ice Sheet extent over the last 130 thousand years traced by the Pb isotope signature of weathering inputs to the Labrador Sea

Medientyp: E-Artikel

Titel: Laurentide Ice Sheet extent over the last 130 thousand years traced by the Pb isotope signature of weathering inputs to the Labrador Sea

Beteiligte: Parker, Rebecca L. [Verfasser:in]; Foster, Gavin L. [Verfasser:in]; Gutjahr, Marcus [Verfasser:in]; Wilson, Paul A. [Verfasser:in]; Littler, Kate L. [Verfasser:in]; Cooper, Matthew J. [Verfasser:in]; Michalik, Agnes [Verfasser:in]; Milton, James A. [Verfasser:in]; Crocket, Kirsty C. [Verfasser:in]; Bailey, Ian [Verfasser:in]

Erschienen: Elsevier, 2022-07-01

Sprache: Englisch

DOI: https://doi.org/10.1016/j.quascirev.2022.107564

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Beschreibung: Highlights • We present LGC record of the Pb isotope composition Labrador Sea seawater. • These data can be used to track Laurentide Ice Sheet extent over Hudson Bay. • LIS retreat during the PGM was relatively fast compared to the LGM • The LIS first advanced significantly over Hudson Bay during MIS 4. • Our record does not support significant LIS retreat during MIS 3. Understanding the history of continental ice-sheet growth on North America, and in particular that of the Laurentide Ice Sheet (LIS), is important for palaeoclimate and sea-level reconstructions. Information on ice-sheet extent pre-dating the Last Glacial Maximum (LGM) is heavily reliant, though, on the outputs of numerical models underpinned by scant geological data. Important aspects of LIS history that remain unresolved include the timing of its collapse during Termination 2, the first time that it expanded significantly during the Last Glacial Cycle, and whether its volume was significantly reduced during marine isotope stage (MIS) 3. To address these issues and more, we present authigenic iron-manganese (Fe–Mn) oxyhydroxide-derived high-resolution records of Pb isotope data and associated rare earth element profiles for samples spanning the past ∼130 kyr from northwest North Atlantic Labrador Sea, IODP Site U1302/3. We use these new data to track chemical weathering intensity and solute flux to the Labrador Sea associated with LIS extent on the adjacent highly radiogenic (high Pb isotope composition) North American Superior Province (SP) craton since the Penultimate Glacial Maximum (PGM). Our new records show that relatively high (radiogenic) values characterise warm marine isotope stages (MIS) 5, 3 and 1 and the lowest (most unradiogenic) values occurred during cold stages MIS 6, 4 and 2. The radiogenic Pb isotope excursion associated with Termination 2 is short-lived relative to the one documented for Termination 1, suggesting that LIS retreat during the PGM was relatively fast compared to the LGM and that its collapse during the last ...

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