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Respuesta fluvial al abrupto calentamiento global en el límite Paleoceno/Eoceno

Brady Z Foreman1, Paul L Heller, Mark T Clementz

  • 1University of Wyoming, Department of Geology and Geophysics, 1000 East University Avenue, Laramie, Wyoming 82071, USA. bforema1@uwyo.edu

Nature
|November 7, 2012
PubMed
Resumen

El Máximo Térmico Paleoceno-Eoceno (PETM) causó cambios significativos en los ríos en el oeste de Colorado, lo que llevó a depósitos gruesos de arenisca. Estas respuestas fluviales persistieron mucho después del evento de calentamiento, destacando el clima climático.

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