Dynamic hydrologic and biogeochemical processes drive microbially enhanced iron and sulfur cycling within the intertidal mixing zone of a beach aquifer-Reference-Cited by-同舟云学术

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Dynamic hydrologic and biogeochemical processes drive microbially enhanced iron and sulfur cycling within the intertidal mixing zone of a beach aquifer

Published:2015-01 Issue:1 Volume:60 Page:329-345
ISSN:0024-3590
Container-title:Limnology and Oceanography
language:en
Short-container-title:Limnol. Oceanogr.

Author:

McAllister Sean M.¹,Barnett Joshua M.²,Heiss James W.³,Findlay Alyssa J.¹,MacDonald Daniel J.⁴,Dow Charles L.⁵,Luther George W.¹⁴,Michael Holly A.³⁶,Chan Clara S.¹³

Affiliation:

1. School of Marine Science and Policy; University of Delaware; Newark and Lewes Delaware

2. Department of Biological Sciences; University of Delaware; Newark Delaware

3. Department of Geological Sciences; University of Delaware; Newark Delaware

4. Department of Chemistry and Biochemistry; University of Delaware; Newark Delaware

5. Stroud Water Research Center; Avondale Pennsylvania

6. Department of Civil and Environmental Engineering; University of Delaware; Newark Delaware

Funder

National Science Foundation

Earth Sciences

National Aeronautics and Space Administration

Publisher

Wiley

Subject

Aquatic Science,Oceanography

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/lno.10029/fullpdf

Reference61 articles.

1. The distribution and speciation of dissolved trace metals in a shallow subterranean estuary;Beck;Mar. Chem.,2010

2. Groundwater discharge: Potential association with fecal indicator bacteria in the surf zone;Boehm;Environ. Sci. Technol.,2004

3. QIIME allows analysis of high-throughput community sequencing data;Caporaso;Nat. Methods,2010

4. Oxidative precipitation of groundwater-derived ferrous iron in the subterranean estuary of a coastal bay;Charette;Geophys. Res. Lett.,2002

5. Trace element cycling in a subterranean estuary: Part 1;Charette;Geochemistry of the permeable sediments. Geochim. Cosmochim. Acta,2005

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