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Titel On the evolution of Mediterranean Sea Water during climate warm stages (MIS 1, 5, 7)
VerfasserIn Jean-Carlos Montero-Serrano, Norbert Frank, Christophe Colin
Konferenz EGU General Assembly 2011
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 13 (2011)
Datensatznummer 250054885
 
Zusammenfassung
The Nd isotopic composition of the aragonite skeleton of fossil reef framework forming cold-water corals provides a way to reconstruct the provenance of water masses bathing the reefs (e.g., Copard et al., 2010; van de Flierdt et al., 2010; Colin et al., 2010). Here, we have reconstructed the Nd-isotopic composition of corals on two sites along the eastern north Atlantic, the Gulf of Cadiz (off Morocco) to the south and the Porcupine Seabight (Belgica Mound Province) to the north. A stunting evolution of the northward propagation of Mediterranean Sea Water (MSW) came to light for the past three climate warm stages (Marine Isotope Stages –MIS– 1, 5, 7). In fact, water masses in the Gulf of Cadiz reveal rather constant Nd-isotopic composition (ɛNd ~ -9 to -11) during climate warm stages similar to present day MSW (ɛNd ~ -9.4 to -11). In contrast, corals from Porcupine Seabight reveal dramatic changes over the past three climatic warm stages. During stage MIS 7 the isotopic composition of water masses in Porcupine Seabight is identical to the one of the Gulf of Cadiz, most likely reflecting a strong northward export of MSW. In contrast, during MIS 5 and 1 a large contrast between southern (ɛNd ~ -9 to -11) and northern reefs is found (ΔɛND = -3 to -4) indicating largely reduced northward flow of MSW compared to MIS 7. This difference is likely related to a far stronger eastward export of intermediate water from the subpolar gyre during the past two climatic warm stages. References: Copard et al., 2010. Quaternary Science Reviews 29: 2499-2508. Colin et al., 2010. Quaternary Science Reviews 29: 2509-2517. van de Flierdt et al., 2010. Geochimica et Cosmochimica Acta 74: 6014-6032.