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Settling the issue of “decoupling” between atmospheric carbon dioxide and global temperature: [CO2]atm reconstructions across the warming Paleogene-Neogene divide
Tekie Tesfamichael; Bonnie Jacobs; Neil Tabor; Lauren Michel; Ellen Currano; Mulugeta Feseha; Richard Barclay; John Kappelman; Mark Schmitz
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Cover Image
Cover Image
COVER: Glacial polish reflects sunlight at Pothole Dome, Yosemite National Park, California, USA. The granitic bedrock here was polished by glacier sliding during the Last Glacial Maximum. In “The coating layer of glacial polish” (p. 991–994), Siman-Tov et al. propose that rather than simply the result of material removal, glacial polish forms by the accretion of a thin coating layer on top of glacially abraded surfaces.
Photo by: Shalev Siman-Tov
Cover design by: Heather L. Sutphin
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