Early Holocene deglaciation of Drangajökull, Vestfirðir, Iceland
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文摘

Threshold lake sediment constrain the early Holocene deglaciation of NW Iceland.

Warm early Holocene summers are supported by high lacustrine algal productivity.

Local warmth and aridity likely drove the ice cap's rapid recession.

It is very unlikely that the ice cap persisted through the Holocene.

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