| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 6446351 | Quaternary Science Reviews | 2014 | 18 Pages |
Abstract
The evolution of the Pb isotope compositions of past seawater was dominated by local signatures characterized by high 208, 207, 206Pb/204Pb values during the warm Early and Mid-Holocene periods related to enhanced chemical weathering on Svalbard and high glacial and riverine input derived from young granitic (more radiogenic) material to the West Spitsbergen margin. At 3 cal ka BP both detrital and seawater Pb isotope data changed towards more Kara Sea-like signatures.
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Authors
Kirstin Werner, Martin Frank, Claudia Teschner, Juliane Müller, Robert F. Spielhagen,