Mediterranean climate variability during the Holocene.
Mediterranean climate variability during the Holocene.
复制标题
全新世期间地中海气候变化。
DOI:
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发表时间:
2001
期刊:
影响因子:
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通讯作者:
V. Lykousis
中科院分区:
文献类型:
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作者:
J. Casford;R. H. Abu;E. Rohling;S. Cooke;K. Boessenkool;H. Brinkhuis;C. D. Vries;G. Wefer;M. Geraga;G. Papatheodorou;I. Croudace;J. Thomson;V. Lykousis
We present a study on four high sedimentation-rate marine cores with suppressed bioturbation effects, recovered along the northern margin of the eastern Mediterranean. We demonstrate that this region, central to the development of modern civilisation, was substantially affected throughout the Holocene by a distinct cycle of cooling events on the order of 2o C. In the best-preserved cases the onset of these events appears particularly abrupt, within less than a century. The cooling events typically lasted several centuries, and there are compelling indications that they were associated with increased aridity in the Levantine/NE African sector (Rossignol-Strick, 1995; 1998; Alley et al., 1997; Hassan, 1986; 1996; 1997a,b; McKim Malville et al., 1998). Several of these episodes appear coincident with cultural reorganisations, with indigenous developments (eg. cattle domestication, new technologies) and population migrations and fusion of peoples and ideas (Hassan, 1986; 1996; 1997a,b; McKim Malville, 1998). We infer that climatic events of a likely high-latitude origin (O’Brien et al., 1995; Bond et al., 1997; Mayewski et al., 1997; Alley et al., 1997) caused cooling and aridity in and around the eastern Mediterranean via a direct atmospheric link, and therefore played an important role in the development of modern civilisation.