The Drangajökull ice cap, northwest Iceland, persisted into the early-mid Holocene
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We obtained sediment cores from threshold lakes around the Drangajökull ice cap, NW Iceland.

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Most cores show a transition from minerogenic to organic sediments reflecting a termination of glacial meltwater inflow.

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We identified key tephra layers in the lake sediment cores.

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The SE part of the early Holocene Drangajökull was larger than at present and persisted until 7.2-7.8 cal. kyr BP.

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We speculate that Drangajökull survived Holocene warm periods due to increased winter precipitation during such periods.

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