Cause of the chalcophile trace element enrichments marking the Holocene to Anthropocene transition in northern Chesapeake Bay sediments

Author:

Dolor Marvourneen K.,Helz George R.,McDonough William F.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference62 articles.

1. Reconstructing the rise of recent coastal anoxia; molybdenum in Chesapeake Bay sediments;Adelson;Geochim. Cosmochim. Acta,2001

2. Baker J., Mason R., Cornwell J., Ashley J., Halka J. and Hill J. (1997) Spatial mapping of sedimentary contaminants in the Baltimore Harbor/Patapsco River/Back River system. UMCES[CBL] Report 97-142, University of Maryland, Solomons, MD, 102 pp.

3. The trace metal content of recent organic carbon-rich sediments: implications for Cretaceous black shale formation;Brumsack;Palaeogeog. Palaeoclim. Palaeoecol.,2006

4. Calvert S. E. and Pedersen T. F. (2007) Elemental proxies for palaeoclimatic and palaeoceanographic variability in marine sediments; interpretation and application. Chap. 14 in Developments in Marine Geology, vol. 1, Elsevier, pp. 567–644.

5. Elemental analysis of estuarine sediments by lithium metaborate fusion and direct current plasma emission spectrometry;Cantillo;Anal. Chem.,1984

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