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Contrasting effects of marine and terrestrially derived dissolved organic matter on mercury speciation and bioavailability in seawater Amina Traore Schartup, Udonna Chinedu Ndu, Prentiss H Balcom, Robert P. Mason, and Elsie M. Sunderland Environ. Sci. Technol., Just Accepted Manuscript • DOI: 10.1021/es506274x • Publication Date (Web): 16 Apr 2015 Downloaded from http://pubs.acs.org on April 20, 2015

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Environmental Science & Technology

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Contrasting effects of marine and terrestrially

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derived dissolved organic matter on mercury

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speciation and bioavailability in seawater

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Amina T. Schartup1*, Udonna C. Ndu2, Prentiss H. Balcom3,4, Robert P. Mason3 and Elsie M.

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Sunderland1,4

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United States

Department of Environmental Health, Harvard School of Public Health, Boston MA 02215,

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Brunswick NJ 08901, United States

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Department of Environmental Science, Rutgers University, 14 College Farm Road, New

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Department of Marine Sciences, 1080 Shennecossett Rd Groton CT 06340, United States

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4School

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*Corresponding author

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[email protected]

of Engineering and Applied Sciences, Harvard University, Cambridge MA, 02138

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TOC art

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Abstract

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Methylmercury (MeHg) is the only species of mercury (Hg) to biomagnify in aquatic

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food-webs to levels that are a widespread concern for human and ecological health. Here we

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investigate the association between dissolved organic matter (DOM) in seawater and Hg

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speciation and uptake using experimental data and field measurements from Long Island Sound

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(LIS) and the Northwestern Atlantic continental margin (NWA). We measured differences in

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DOM composition across sampling stations using excitation emission matrix (EEM)

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fluorescence spectroscopy and further separated DOM into terrestrial and marine components

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using Parallel Factor Analysis (PARAFAC). Highest MeHg concentrations were found in the

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estuarine stations (LIS) with highest DOM concentrations due to enhanced external inputs from

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the watershed and rivers. For stations on the shelf and slope, MeHg in plankton increased

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linearly with a decreasing fraction of fluorescence attributable to DOM components with a

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terrestrial rather than marine origin. These results are corroborated by experimental data showing

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higher MeHg uptake by cells in the presence of predominantly marine DOM compared to

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terrestrial DOM. Highest fractions of dissolved gaseous mercury were also found at stations with

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the highest marine DOM content, suggesting a greater reducible fraction of divalent inorganic

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Hg. These data suggest DOM composition is a critical driver of Hg reactivity and bioavailability

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in offshore marine waters.

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Introduction Mercury (Hg) is a naturally occurring heavy metal with a biogeochemical cycle that has

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been substantially perturbed by human activity.1,2 Methylmercury (MeHg) is the only Hg species

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to biomagnify in aquatic food-webs and accumulate at levels that are a widespread concern for

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human and ecological health.3,4 Dissolved organic matter (DOM) binds strongly with both Hg

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and MeHg in natural ecosystems and affects bioavailability.5 Freshwater systems exhibit much

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wider gradients in DOM concentrations (1700 µM)6 than marine systems (34-80 µM).7

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Molecular structure and primary sources marine DOM are much more diverse than in terrestrial

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systems.8–10 Here we investigate how differences in marine DOM composition affect Hg

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reactivity and biological uptake of MeHg in estuarine and continental shelf waters.

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In aquatic ecosystems, divalent inorganic mercury (HgII) can be converted to MeHg by a

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variety of microbial claves or reduced to elemental mercury (Hg0) through a combination of

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photolytic and biological reactions.11–14 Strong binding of HgII to DOM has been hypothesized to

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affect the reactive pool available for both net methylation and net reduction.8,9,15,16 DOM may

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also enhance the activity of methylating microbes in oligotrophic ecosystems by providing a

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substrate for bacterial activity, while under eutrophic conditions impacts on binding to HgII may

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be more important.17,18–20 Previous experimental and field studies report mixed effects of DOM

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on biological uptake of MeHg.21–24 We hypothesize here that variability in DOM composition

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helps to explain these results.

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Excitation emission matrix (EEM) fluorescence spectroscopy is widely used to

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characterize differences in the composition of DOM. These data can be used to identify DOM

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that originates from soils, rivers and marine productivity according to their characteristic

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fluorescence intensities and differences in the wavelength maxima.25 Parallel Factor Analysis

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(PARAFAC) has been widely used to further separate DOM into chemically distinct

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components, based on spectra of known compounds or organic matter structure, that are difficult

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to distinguish in the EEMs.26 Here we use such an analysis to distinguish broadly between

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sources with a terrestrial and marine origin in order to minimize over interpretation of the

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individual PARAFAC components.27–29

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The main objective of this work is to better understand how DOM composition affects

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Hg reactivity and MeHg bioavailability in marine ecosystems. To do this, we collected data on

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Hg and DOM concentrations and composition in filtered seawater from two estuarine stations in

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Long Island Sound (LIS), and along a gradient of terrestrial and marine influenced locations of

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the Northwest Atlantic continental margin (abbreviated as NWA from hereon). We compare

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identified components of DOM using EEM and PARAFAC analysis to Hg concentrations

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measured at each site and uptake of MeHg by plankton. We complement these data with

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laboratory experiments that further investigate how DOM composition affects Hg binding using

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a titration experiment and biological uptake using a bioreporter.

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Methods

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Field sampling

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Figure 1 shows seawater sampling locations for DOM and Hg species in LIS and the

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NWA, which includes the Gulf of Maine, shelf and slope. We collected Long Island Sound

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seawater using acid-washed, Teflon-lined General Oceanics GO-FLO sampling bottles and

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Teflon coated messengers deployed on a Kevlar line following trace-metal clean protocols.30

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LIS samples were obtained from two sites on three cruises: (1) 6-7 August 2009, (2) 09 November-14 December 2009, and (3) 24-27 May 2010 (see Supporting Information (SI) Table

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S1 for further details of sampling locations). Samples from the NWA were collected between

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17-26 August 2008 and 29 September-7 October 2009. Total Hg, MeHg and dissolved gaseous

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mercury (DGM) concentrations in seawater and MeHg in plankton were measured at stations

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shown in Figure 1. We use particulate MeHg measured in LIS as a proxy for concentrations in

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microseston (> 0.2 µm).31

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We measured dissolved organic carbon (DOC) concentrations and DOM composition for

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all LIS cruises and at stations shown in Figure 1 on the NWA cruise in 2008 (Table S2). We

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measured Hg species concentrations for LIS across seasons. For the NWA, we used 2008-2009

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data from Soerensen et al.8 on total Hg and DGM and 2008-2009 data from Hammerschmidt et

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al.31 on MeHg in seawater and MeHg in plankton.

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Total mercury and methylmercury analyses

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All LIS seawater for Hg species analysis was transferred into acid washed FEP bottles in

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the field prior to filtration, and stored double-bagged inside iced coolers. We filtered samples in

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a laminar flow hood

Contrasting effects of marine and terrestrially derived dissolved organic matter on mercury speciation and bioavailability in seawater.

Methylmercury (MeHg) is the only species of mercury (Hg) to biomagnify in aquatic food-webs to levels that are a widespread concern for human and ecol...
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