Hydrological and temperature change in Arctic Siberia during the intensification of Northern Hemisphere Glaciation
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文摘

Pliocene Arctic temperature and hydrology reconstructed using brGDGTs and δDwax.

Cooling and drying coincident with intensified northern hemisphere glaciation (iNHG).

Range of δDwax and MBT/CBT temperature increased following iNHG.

Proxy behavior linked to development of positive feedbacks in the Arctic.

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