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Long-Term Trends in Submersed Aquatic Vegetation (SAV) in Chesapeake Bay, USA, Related to Water Quality
Authors:Robert J Orth  Michael R Williams  Scott R Marion  David J Wilcox  Tim J B Carruthers  Kenneth A Moore  W Michael Kemp  William C Dennison  Nancy Rybicki  Peter Bergstrom  Richard A Batiuk
Institution:1. Virginia Institute of Marine Science, Rt. 1208, Greate Road, Gloucester Point, VA, 23062, USA
2. Center for Environmental Sciences, Integration Application Network, University of Maryland, 111 Cathedral Street, Annapolis, MD, 21401, USA
3. Center for Environmental Sciences, Horn Point Laboratory, University of Maryland, 2020 Horns Point Road, Cambridge, MD, 21613, USA
4. US Geological Survey, 12201 Sunrise Valley Drive, Reston, VA, 20192, USA
5. National Oceanic and Atmospheric Administration, 410 Severn Avenue, Annapolis, MD, 21403, USA
6. US Environmental Protection Agency, Chesapeake Bay Program, Severn Ave., Annapolis, MD, 21403, USA
Abstract:Chesapeake Bay supports a diverse assemblage of marine and freshwater species of submersed aquatic vegetation (SAV) whose broad distributions are generally constrained by salinity. An annual aerial SAV monitoring program and a bi-monthly to monthly water quality monitoring program have been conducted throughout Chesapeake Bay since 1984. We performed an analysis of SAV abundance and up to 22 environmental variables potentially influencing SAV growth and abundance (1984–2006). Historically, SAV abundance has changed dramatically in Chesapeake Bay, and since 1984, when SAV abundance was at historic low levels, SAV has exhibited complex changes including long-term (decadal) increases and decreases, as well as some large, single-year changes. Chesapeake Bay SAV was grouped into three broad-scale community-types based on salinity regime, each with their own distinct group of species, and detailed analyses were conducted on these three community-types as well as on seven distinct case-study areas spanning the three salinity regimes. Different trends in SAV abundance were evident in the different salinity regimes. SAV abundance has (a) continually increased in the low-salinity region; (b) increased initially in the medium-salinity region, followed by fluctuating abundances; and (c) increased initially in the high-salinity region, followed by a subsequent decline. In all areas, consistent negative correlations between measures of SAV abundance and nitrogen loads or concentrations suggest that meadows are responsive to changes in inputs of nitrogen. For smaller case-study areas, different trends in SAV abundance were also noted including correlations to water clarity in high-salinity case-study areas, but nitrogen was highly correlated in all areas. Current maximum SAV coverage for almost all areas remain below restoration targets, indicating that SAV abundance and associated ecosystem services are currently limited by continued poor water quality, and specifically high nutrient concentrations, within Chesapeake Bay. The nutrient reductions noted in some tributaries, which were highly correlated to increases in SAV abundance, suggest management activities have already contributed to SAV increases in some areas, but the strong negative correlation throughout the Chesapeake Bay between nitrogen and SAV abundance also suggests that further nutrient reductions will be necessary for SAV to attain or exceed restoration targets throughout the bay.
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