作者: J. C. Duplessy , L. Labeyrie , J. Moyes , J. L. Turon , J. Duprat
DOI: 10.1007/978-94-009-5494-6_6
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摘要: When the Earth’s climate changes from interglacial to glacial conditions, temperature and precipitation patterns over European continent are profoundly modified: at height of last ice age, surface water temperatures in neighbouring Atlantic Ocean were more than 10°C lower those present day. A cold dry had led development a polar desert northern Europe steppe conditions further south.