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Lower export production during glacial periods in the equatorial Pacific derived from (Pa-231/Th-230)(xs,0) measurements in deep-sea sediments ArchiMer
Pichat, S; Sims, Kww; Francois, R; Mcmanus, Jf; Leger, Sb; Albarede, F.
The (Pa-231/Th-230)(xs,0) records obtained from two cores from the western (MD97-2138; 1degrees25'S, 146degrees24'E, 1900 m) and eastern (Ocean Drilling Program Leg 138 Site 849, 0degrees11.59'N, 110degrees31.18'W, 3851 m) equatorial Pacific display similar variability over the last 85,000 years, i.e., from isotopic stages 1 to 5a, with systematically higher values during the Holocene, isotopic stage 3, and isotopic stage 5a, and lower values, approaching the production rate ratio of the two isotopes (0.093), during the colder periods corresponding to isotopic stages 2 and 4. We have also measured the Th-230-normalized biogenic preserved and terrigenous fluxes, as well as major and trace elements concentrations, in both cores. The (Pa-231/Th-230)(xs,0)...
Tipo: Text Palavras-chave: (Pa-231/Th-230)(xs; 0) export productivity Pacific.
Ano: 2004 URL: https://archimer.ifremer.fr/doc/00228/33933/32240.pdf
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Ocean climate variability in the eastern North Atlantic during interglacial marine isotope stage 11: A partial analogue to the Holocene? ArchiMer
De Abreu, C; Abrantes, Ff; Shackleton, Nj; Tzedakis, Pc; Mcmanus, Jf; Oppo, Dw; Hall, Ma.
Similar orbital geometry and greenhouse gas concentrations during marine isotope stage 11 ( MIS 11) and the Holocene make stage 11 perhaps the best geological analogue period for the natural development of the present interglacial climate. Results of a detailed study of core MD01-2443 from the Iberian margin suggest that sea surface conditions during stage 11 were not significantly different from those observed during the elapsed portion of the Holocene. Peak interglacial conditions during stage 11 lasted nearly 18 kyr, indicating a Holocene unperturbed by human activity might last an additional 6-7 kyr. A comparison of sea surface temperatures ( SST) derived from planktonic foraminifera for all interglacial intervals of the last million years reveals that...
Tipo: Text Palavras-chave: Stage 11; Interglacials; Planktonic foraminifera; Stable isotopes; Western Iberian margin; Eastern North Atlantic.
Ano: 2005 URL: https://archimer.ifremer.fr/doc/00233/34407/32828.pdf
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