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Stable isotope (δ13C and δ15N) based interpretation of organic matter source and paleoenvironmental conditions in Al-Azraq basin, Jordan

  • Published:2017-03 Issue: Volume:78 Page:49-60
  • ISSN:0883-2927
  • Container-title:Applied Geochemistry
  • language:en
  • Short-container-title:Applied Geochemistry

Author:

Ahmad Khaldoun,Davies Caroline

Funder

American Center of Oriental Research

University of Missouri Research Board

Natural Resources Authority

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Pollution,Environmental Chemistry

Reference81 articles.

1. The paleoclimate of the eastern desert of Jordan during marine isotope stage 9;Abed;Quat. Res.,2008

2. Organic Geochemistry of Al-azraq Basin, Jordan, an Interpretation of Paleoenvironment and Paleoclimate Using Bulk OM;Ahmad,2010

3. Compositional variations in sedimentary lacustrine OM and their implications for high Alpine Holocene environmental changes: lake St. Moritz, Switzerland;Ariztegui;Org. Geochem.,1996

4. Geology of Jordan;Bender,1974

5. Dissecting palimpsests in a late lower and middle paleolithic flint acquisition site on the Madaba plateau, Jordan;Bisson;Quat. Int.,2014
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