
NSF Org: |
DEB Division Of Environmental Biology |
Recipient: |
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Initial Amendment Date: | June 30, 2023 |
Latest Amendment Date: | June 30, 2023 |
Award Number: | 2329941 |
Award Instrument: | Standard Grant |
Program Manager: |
Jason West
jwest@nsf.gov (703)292-7410 DEB Division Of Environmental Biology BIO Directorate for Biological Sciences |
Start Date: | January 1, 2023 |
End Date: | June 30, 2024 (Estimated) |
Total Intended Award Amount: | $87,731.00 |
Total Awarded Amount to Date: | $44,826.00 |
Funds Obligated to Date: |
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History of Investigator: |
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Recipient Sponsored Research Office: |
2801 W BANCROFT ST TOLEDO OH US 43606-3328 (419)530-2844 |
Sponsor Congressional District: |
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Primary Place of Performance: |
2801 W BANCROFT ST TOLEDO OH US 43606-3390 |
Primary Place of
Performance Congressional District: |
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Unique Entity Identifier (UEI): |
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Parent UEI: |
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NSF Program(s): | Ecosystem Science |
Primary Program Source: |
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Program Reference Code(s): | |
Program Element Code(s): |
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Award Agency Code: | 4900 |
Fund Agency Code: | 4900 |
Assistance Listing Number(s): | 47.074 |
ABSTRACT
The goal of this award is to determine the origin and fate of mercury in a salt marsh ecosystem in the Plum Island Sound of Massachusetts and potential export to near shore coastal oceans. Mercury is a potent neurotoxin and leading cause for fish consumption advisories in the U.S and across the world. Along the U.S. East Coast, salt marsh sparrows have shown harmful exposures to mercury with elevated blood levels posing risks for reproductive outputs. The origin of mercury in these salt marshes is largely unknown. Possible reasons for high mercury exposure are contributions from runoff from adjacent watersheds or atmospheric inputs from legacy industrial impacts. This award will study the role of direct plant uptake of atmospheric mercury by salt marsh plants as the mercury source for these salt marsh ecosystems. In this tidal system, an additional focus lies on the transfer of mercury to soils by the plants and with death of the plants its export to the coastal ocean. The award will train and involve graduate and undergraduate students in the research.
This award aims to quantify mercury sinks and sources and their relationships to plant primary productivity, tissue turnover rates, and soil dynamics, in a salt marsh ecosystem where some of the highest biological mercury exposures have been reported. The first hypothesis is that that plant mercury assimilation is the dominant source of mercury in this estuary where salt marshes dominate in areal extent (50 to 90% of surface area). The second hypothesis is that vegetation assimilation of mercury is incorporated into soils upon plant senesce leading to high mercury accumulation in soils, which ultimately is mobilized to tidal water leading to net export of mercury from salt marshes to tidal water. This is analogue to the ?outwelling? hypothesis for carbon that proposes that salt marshes produce an excess of autochthonous carbon over what is degraded and stored resulting in net export to the coastal ocean where it stimulates ocean net primary production. Proposed measurements include quantification of atmospheric mercury deposition inputs via deployment of a micrometeorological flux-gradient system that allows to measure ecosystem-level gaseous atmospheric mercury fluxes including plant mercury assimilation, along with detailed vegetation mercury dynamics and other deposition processes. Spatial transect sampling of tidal water from the ocean through the tidal water up to the freshwater headwater will be conducted and analyzed for mercury species (dissolved, particulate, methyl-mercury and mercury bound contained in wrack detritus) in order to assess lateral exchanges between salt marsh and tidal water. Finally, distribution patterns of total mercury and methylated mercury in salt marsh soils will be characterized to constrain processes ? both natural and anthropogenic ? that lead to mercury accumulation in these 2,500-to-3,500 year old soils.
This award reflects NSF's statutory mission and has been deemed worthy of support through evaluation using the Foundation's intellectual merit and broader impacts review criteria.
PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH
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PROJECT OUTCOMES REPORT
Disclaimer
This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.
Estuaries are conduits of the mobilization of mercury (Hg), a neurotoxic environmental pollutant, between watersheds and the coastal ocean. In New England, salt marsh ecosystems compose many estuaries, with some showing evidence of enhanced levels of Hg exposure. Here, we investigated Hg dynamics in vegetation and soils in the Plum Island Sound estuary in Massachusetts, USA, the largest salt marsh estuary in New England. Our methods included sampling of salt marsh vegetation, soils, air, and tidal water, along with stable Hg isotope characterization and Hg air-surface exchange.
A detailed assessment of Hg allowed us to constrain mass balance fluxes in this estuary. We estimate the current origins of Hg in salt marsh vegetation to originate from about equal contributions from precipitation uptake, uptake of gaseous atmospheric Hg, and, surprisingly, root (i.e., soil) uptake. The latter normally plays a minor role as a source of Hg in vegetation, and we attribute the relatively high root uptake to high Hg pools found in the carbon-rich salt marsh soils (>25 mg m-2 in the top 40 cm). The reasons for high soil Hg at this site are unknown, but it could possibly originate from past industrial legacy pollution imported via ocean sediments from nearby rivers.
A strong effort in this study included measuring gaseous Hg exchanges using tower-based methods above the salt marsh. Gaseous Hg fluxes were highly variable, lacked clear seasonal patterns and no significant growing season vegetation GEM uptake, and amounted to a minor annual emission of 6.7 µg m-2 yr-1. This finding is consistent with previous observations of reported GEM evasion from aquatic ecosystems, but contrasts observations of significant GEM deposition in most terrestrial ecosystems, including in two nearby forest ecosystems (deposition of 13.4 µg m-2 yr-1 and 25.1 µg m-2 yr-1, respectively). The reason for the high flux variability and small deposition flux likely includes high surface heterogeneity with high and submerged marsh, as well as tidal and water surface fluctuations, channels, etc.).
This study produced and contributed to 8 peer-reviewed scientific publications which have generated over 175 citations in other published articles. We presented 19 presentations about this study at national and international conferences and seminars. This study provided novel scientific information about the cycling of Hg in this New England salt marsh ecosystem, the role of vegetation and soils, and the connectivity of Hg flows across the estuaries and between the adjacent terrestrial and marine ecosystems. The findings of this study are being integrated to assess local and regional Hg exposures and used to explain enhanced blood Hg levels that are observed in salt marsh sparrows at this study site. In addition, the study is informing models of global and regional mercury cycling and expected to help assess the Minamata Convention, an international agreement intended to curb anthropogenic mercury emissions and reduce mercury risks to humans and the environment.
Last Modified: 11/27/2024
Modified by: Inke Forbrich
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