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Variability of the western Mediterranean Sea surface temperature during the last 25,000 years and its connection with the Northern Hemisphere climatic changes 5
Cacho, I; Grimalt, Jo; Canals, M; Sbaffi, L; Shackleton, Nj; Schonfeld, J; Zahn, R.
Sea surface temperature (SST) profiles over the last 25 kyr derived from alkenone measurements are studied in four cores from a W-E latitudinal transect encompassing the Gulf of Cadiz (Atlantic Ocean), the Alboran Sea, and the southern Tyrrhenian Sea (western Mediterranean). The results document the sensitivity of the Mediterranean region to the short climatic changes of the North Atlantic Ocean, particularly those involving the latitudinal position of the polar front. The amplitude of the SST oscillations increases toward the Tyrrhenian Sea, indicating an amplification effect of the Atlantic signal by the climatic regime of the Mediterranean region. All studied cores show a shelter cooling phase (700 years) for the Younger Dryas (YD) than that observed in...
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Ano: 2001 URL: https://archimer.ifremer.fr/doc/00220/33173/31682.pdf
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Rapid transient changes in northeast Atlantic deep water ventilation age across Termination I 5
Skinner, Lc; Shackleton, Nj.
A sequence of accelerator mass spectrometry (AMS) C-14 dates performed on benthic and planktonic foraminifera from a northeast Atlantic deep-sea core (MD99-2334K; 37degrees480N, 10degrees10'W; 3146 m) permit the reconstruction of deep water ,,C-14 ventilation ages'' across the last deglaciation. The records from MD99-2334K have been placed on the GISP2 timescale via the synchrony of temperature changes recorded in the Greenland ice cores and in North Atlantic planktonic delta(18)O(cc) (calcite delta(18)O). On the basis of a range of estimates for past source water Delta(14)C, this permits the estimation of C-14 projection ventilation ages for comparison with benthic-planktonic C-14 age differences. Although the accurate estimation of past ventilation ages...
Tipo: Text Palavras-chave: Termination I; Ventilation age; Thermohaline circulation.
Ano: 2004 URL: https://archimer.ifremer.fr/doc/00228/33971/32339.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? 5
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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Millennial-scale variability of deep-water temperature and delta O-18(dw) indicating deep-water source variations in the Northeast Atlantic, 0-34 cal. ka BP 5
Skinner, Lc; Shackleton, Nj; Elderfield, H.
Paired measurements of Mg/Ca and delta(18)O(cc) (calcite delta(18)O) in benthic foraminifera from a deep-sea core recovered on the Iberian Margin (MD99-2334K; 37degrees 48'N, 10degrees10'W; 3,146 m) have been performed in parallel with planktonic delta(18)O(cc) analyses and counts of ice-rafted debris (IRD). The synchrony of temperature changes recorded in the Greenland ice cores and in North Atlantic planktonic delta(18)O(cc) allows the proxy records from MD99-2334K to be placed confidently on the GISP2 time-scale. This correlation is further corroborated by AMS C-14-dates. Benthic Mg/Ca measurements in MD99-2334K permit the reconstruction of past deep-water temperature (T-dw) changes since -34 cal. ka BP (calendar kiloyears before present). Using these...
Tipo: Text Palavras-chave: Deep-water temperature; Mg/Ca; Termination I; Thermohaline circulation; Paleoceanographycal and chemical : trace elements; Oceanography : biological and chemical : trace elements; Oceanography : biological and chemical : stable isotopes.
Ano: 2003 URL: https://archimer.ifremer.fr/doc/00225/33654/32087.pdf
Registros recuperados: 4
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