Uranium, Thorium and Protactinium isotopes of ODP Site 172-1063, supplementary data to: Lippold, Jörg; Gruetzner, Jens; Winter, Diane M; Lahaye, Yann; Mangini, Augusto; Christl, Marcus (2009): Does sedimentary 231Pa/230Th from the Bermuda Rise monitor past Atlantic Meridional Overtuning Circulation?. Geophysical Research Letters, 36, L12601
Ocean circulation may have undergone reductions and reinvigorations in the past closely tied to regional climate changes. Measurements of 231Pa/230Th ratios in a sediment core from the Bermuda Rise have been interpreted as evidence that the Atlantic Meridional Overturning Circulation (AMOC) was weak...
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| Hauptverfasser: | , , |
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| Weitere Verfasser: | , , |
| Dokumenttyp: | Book/Monograph Forschungsdaten |
| Sprache: | Englisch |
| Veröffentlicht: |
Bremen/Bremerhaven
PANGAEA - Data Publisher for Earth & Environmental Science
2009-07-18
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| DOI: | 10.1594/PANGAEA.763199 |
| Schlagworte: | |
| Online-Zugang: | Resolving-System, Volltext: http://dx.doi.org/10.1594/PANGAEA.763199 Resolving-System, Volltext: http://nbn-resolving.de/urn:nbn:de:tib-10.1594/PANGAEA.7631990 |
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| 245 | 1 | 0 | |a Uranium, Thorium and Protactinium isotopes of ODP Site 172-1063, supplementary data to: Lippold, Jörg; Gruetzner, Jens; Winter, Diane M; Lahaye, Yann; Mangini, Augusto; Christl, Marcus (2009): Does sedimentary 231Pa/230Th from the Bermuda Rise monitor past Atlantic Meridional Overtuning Circulation?. Geophysical Research Letters, 36, L12601 |
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| 520 | |a Ocean circulation may have undergone reductions and reinvigorations in the past closely tied to regional climate changes. Measurements of 231Pa/230Th ratios in a sediment core from the Bermuda Rise have been interpreted as evidence that the Atlantic Meridional Overturning Circulation (AMOC) was weakened or completely eliminated during a period of catastrophic iceberg discharges (Heinrich-Event 1, H1). Here we present new data from the Bermuda Rise that show further 231Pa/230Th peaks during Heinrich-2 (H2) and Heinrich-3 (H3). Additionally, a tight correlation between diatom abundances (biogenic silica) and 231Pa/230Th is discovered in this core. Our results redirect the interpretation of 231Pa/230Th from the Bermuda Rise as a proxy for ocean circulation towards a proxy that reacts highly sensitive to changes of particle composition and water mass properties. | ||
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