全新世中期8.2 ka事件及其他冷气候振荡——来自波兰东北部Suchar Wielki湖的证据

M. Fiłoc
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引用次数: 0

摘要

全新世中期最著名的气候变化是大约8200 cal. ybp的突然降温(例如O 'Brien et al., 1995;Bond et al., 1997)。这种振荡被称为8.2 ka事件,在过去所有最重要的气候记录中都得到了确认,即格陵兰冰芯(GRIP和GRIP2)和北大西洋深海冰芯(O 'Brien et al., 1995;Bond et al., 1997),然后在世界上的许多记录中得到了证明
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8.2 ka event and others cold climate oscillations in middle Holocene – evidence from Suchar Wielki Lake, NE Poland
The best-known climate change in the middle part of the Holocene is an abrupt cooling around 8200 cal. yrs BP (e.g. O’Brien et al., 1995; Bond et al., 1997). This oscillation, known as the 8.2 ka event, was recognised in all most important past climate records, i.e. in the Greenland ice cores (GRIP and GRIP2) and in North Atlantic deep sea cores (O’Brien et al., 1995; Bond et al., 1997), and then it was demonstrated in many records in the world
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