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Data Description |
| Citation: | Jansen, E; Veum, T (1990): Stable isotope analysis of foraminifera from sediment core V23-81 (Table 2). doi:10.1594/PANGAEA.106768,
Supplement to: Jansen, Eystein; Veum, T (1990): Evidence for two-step deglaciation and its impact on North Atlantic deep water circluation. Nature, 343(6259), 612-616, doi:10.1038/343612a0 | ||||||||||||||||||||||||||||||||||||||||||
| Abstract: | Oxygen and carbon isotope records from benthic and planktonic foraminifera are presented for the past 35,000 years in the northeastern Atlantic. The results support the idea that the last deglaci-ation took place in two major steps (Duplessy et al., 1981 doi:10.1016/0031-0182(81)90096-1; Mix and Ruddiman, 1985 doi:10.1016/0277-3791(85)90015-0; Ruddiman, 1987; Fairbanks, 1989 doi:10.1038/342637a0), and conflict with theories calling for a strong reduction in North Atlantic deep-water formation to explain the abrupt cooling of the Younger Dryas cold period (Broecker et al., 1985 doi:10.1038/315021a0; Rind et al., 1986 doi:10.1007/BF01277044; Broecker et al., 1988 doi:10.1029/PA003i001p00001).
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| Coverage: | West: -16.8300 * East: -16.8300 * South: 54.2500 * North: 54.2500
Minimum DEPTH, sediment: 0.0 m * Maximum DEPTH, sediment: 5.0 m
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| Comment: | For age model see Broecker et al. (1988) dataset: doi:10.1594/PANGAEA.726285
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| Parameter(s): |
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| Size: | 156 data points
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