Temporal Trends of Dissolved Trace Metals in Jamaica Bay,NY: Importance of Wastewater Input and Submarine Groundwater Discharge in an Urban Estuary |
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| Authors: | Aaron J Beck J Kirk Cochran Sergio A Sañudo-Wilhelmy |
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| Institution: | (1) Marine Sciences Research Center, Stony Brook University, Stony Brook, NY 11794-5000, USA;(2) Department of Biological Sciences and Department of Earth Sciences, University of Southern California, Los Angeles, CA 90089-0371, USA;(3) Present address: Max Planck Institute for Marine Microbiology, Celsiusstrasse 1, 28359 Bremen, Germany |
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| Abstract: | Jamaica Bay, NY, is a highly urbanized estuary within the boroughs of New York City conspicuously lacking published information
on dissolved trace metal concentrations. The current study examines the distribution and cycling of trace metals in that embayment
with data gathered during cruises in November 2004, April 2005, and June 2006. Most of the metal distributions (Fe, Zn, Co,
Ag, Cu, Pb, Ni) in the water column are explained by the input of substantial volumes of treated wastewater effluent. However,
several lines of evidence suggest that submarine groundwater discharge (SGD) is also an important source of dissolved Fe,
Zn, Co, Ni, and isotopically distinct stable Pb ratios (206Pb, 207Pb, 208Pb) in the Bay. Conversely, the recirculated seawater component of SGD is an apparent sink for dissolved Mo. This study provides
the first measurements of dissolved trace metals in the Jamaica Bay water column and subterranean estuary and provides evidence
for trace metal input due to SGD. |
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