The Campo Felice late Pleistocene Glaciation (Apennines, central Italy)
The Campo Felice late Pleistocene Glaciation (Apennines, central Italy)
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坎波费利斯晚更新世冰川作用（亚平宁山脉，意大利中部）
DOI：
10.1002/jqs.1569
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发表时间：
2012
影响因子：
2.3
通讯作者：
C. Giraudi
中科院分区：
文献类型：
--
作者：
C. Giraudi
通过对Campo Felice（亚平宁山脉，意大利中部）冰川沉积物和湖泊沉积物的研究，可以更精确地确定最后40 ka的冰期，并证明最大冰川推进并不与最后一次全球冰川最大期和花粉所显示的最冷、最干旱期相对应，而是发生在大约33 - 27 ka之间，其特征是气候不那么极端。此外，在35 ka之前也发生了一次冰川扩张。与阿尔卑斯冰川变化的对比表明，亚平宁末次冰川高峰发生在阿尔卑斯南坡末次冰川高峰之前。版权所有©2012 John Wiley & Sons， Ltd。
Study of the glacial deposits and lacustrine sediments of Campo Felice (Apennines, central Italy) has enabled the glacial phases of the last 40 ka to be dated more precisely, and has demonstrated that the maximum glacial advance did not occur in correspondence with the last global glacial maximum and with the coldest and most arid phase suggested by the pollen, but in a period dated between about 33 and 27 ka, characterized by a less extreme climate. Furthermore, a glacial expansion took place also in the period prior to 35 ka. Correlation with the Alpine glacial variations has shown that the Apennine last glacial maximum occurred before that of the southern slope of the Alps. Copyright © 2012 John Wiley & Sons, Ltd.