Inferring LGM sedimentary and climatic changes in the southern Eastern Alps foreland through the analysis of a 14C ages database (Brenta megafan, Italy)
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文摘

14C ages database analysis examining LGM glaciofluvial system evolutions.

The Brenta megafan aggraded with three different trends during LGM.

Local climatic forcing controlled glaciers fluctuations in southern Eastern Alps.

Peat production increases during climate wet events.

Peat layer production correlates with climatic proxies across the N hemisphere.

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