A first chironomid-based summer temperature reconstruction (13-5 ka BP) around 49°N in inland Europe compared with local lake development
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文摘

Mean July temperature was reconstructed based on chironomids in East–Central Europe.

Younger Dryas fluctuations coincided with changes in water level.

All proxies mirrored rapid climate change at the Pleistocene-Holocene transition.

Distinct thermal maximum started 11,400 cal BP ago, followed by cooling since 8700 BP

Algal, pollen and chemical proxies supported the chironomid-based climate reconstruction.

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