Detrital zircons reveal sea-level and hydroclimate controls on Amazon River to deep-sea fan sediment transfer

Author:

Mason Cody C.1,Romans Brian W.2,Stockli Daniel F.3,Mapes Russel W.4,Fildani Andrea5

Affiliation:

1. Department of Geosciences, University of West Georgia, Callaway Building, 1601 Maple St., Carrollton, Georgia 30118, USA

2. Department of Geosciences, Virginia Tech, 4044 Derring Hall, 926 W. Campus Dr., Blacksburg, Virginia 24061, USA

3. Department of Geological Sciences, The University of Texas at Austin, 1 University Station C1100, Austin, Texas 78712, USA

4. ExxonMobil, 22777 Springwoods Village Pkwy, Spring, Texas 77389, USA

5. Equinor Research Center, Austin, Texas 78730, USA

Publisher

Geological Society of America

Subject

Geology

Reference41 articles.

1. Climate forcing of the Pb isotope record of terrigenous input into the equatorial Atlantic;Abouchami;Earth and Planetary Science Letters,2003

2. Construction of detrital mineral populations: Insights from mixing of U-Pb zircon ages in Himalayan rivers;Amidon;Basin Research,2005

3. Nature and causes of Quaternary climate variation of tropical South America;Baker;Quaternary Science Reviews,2015

4. Climate change, sea-level change, and fluvial sediment supply to deepwater depositional systems;Blum,2009

5. Fluvial responses to climate and sea-level change: A review and look forward;Blum;Sedimentology,2000

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