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Open access Sep 2026

Paleogeographic controls on Phanerozoic weathering rates and implications for climate regulation

Earth’s climate has remained habitable for billions of years, a stability usually attributed to a negative feedback from silicate weathering – the chemical breakdown of silicate rocks on land, which consumes atmospheric carbon dioxide faster as climate warms. However, whether temperature or hydrology primarily drives t...

R. J. Graham, B. Cael, M. Fu et al. · 0 citations
Sep 2026

Comparing the Simulated Surface Mass Balance of the Laurentide Ice Sheet During the Last Deglaciation With a Geophysical Reconstruction

Despite decades of research, our understanding of the role of climate feedbacks in shaping Pleistocene glacial cycles remains incomplete. Here, we investigate the decay of the Laurentide Ice Sheet (LIS) by calculating its surface mass balance (SMB) during the last deglaciation using the isotope‐enabled transient climat...

Kirstin Koepnick, M. Fu, Eli Tziperman · 0 citations

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