Continental weathering fluxes during the last glacial/interglacial cycle: insights from the marine sedimentary Pb isotope record at Orphan Knoll, NW Atlantic

Regional weathering intensity must have changed dramatically at high latitudes during the Quaternary as a consequence of repeated continental glaciation. Investigation of these glacial/interglacial changes at high temporal resolution is possible with the recent development of Pb isotopes in FeMn oxy...

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Bibliographic Details
Published in:Quaternary Science Reviews
Main Authors: Crocket, Kirsty C, Vance, D, Foster, GL, Richards, DA, Tranter, M
Format: Article in Journal/Newspaper
Language:English
Published: 2012
Subjects:
Online Access:https://hdl.handle.net/1983/d4321da2-aebe-410a-8ff2-b04687fa3437
https://research-information.bris.ac.uk/en/publications/d4321da2-aebe-410a-8ff2-b04687fa3437
https://doi.org/10.1016/j.quascirev.2012.02.004