Literature DB >> 24352284

Earth science: Erosion by cooling.

David Lundbek Egholm1.   

Abstract

Year:  2013        PMID： 24352284     DOI： 10.1038/504380a

Source DB:  PubMed          Journal:  Nature        ISSN： 0028-0836            Impact factor:   49.962


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  4 in total

1.  Increased sedimentation rates and grain sizes 2-4 Myr ago due to the influence of climate change on erosion rates.

Authors:  Z Peizhen; P Molnar; W R Downs
Journal:  Nature       Date:  2001-04-19       Impact factor: 49.962

Review 2.  Trends, rhythms, and aberrations in global climate 65 Ma to present.

Authors:  J Zachos; M Pagani; L Sloan; E Thomas; K Billups
Journal:  Science       Date:  2001-04-27       Impact factor: 47.728

3.  Long-term stability of global erosion rates and weathering during late-Cenozoic cooling.

Authors:  Jane K Willenbring; Friedhelm von Blanckenburg
Journal:  Nature       Date:  2010-05-13       Impact factor: 49.962

4.  Worldwide acceleration of mountain erosion under a cooling climate.

Authors:  Frédéric Herman; Diane Seward; Pierre G Valla; Andrew Carter; Barry Kohn; Sean D Willett; Todd A Ehlers
Journal:  Nature       Date:  2013-12-19       Impact factor: 49.962
  4 in total

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