Overview
Estuarine and Coastal
Processes
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Estuarine and Coastal Processes
1998-2000 Projects
Dynamics of the Toxic Dinoflagellate, Alexandrium,
in the Gulf of Maine: Source Populations and Downstream Impacts
Donald M. Anderson, Woods Hole Oceanographic Institution, and
Jefferson T. Turner, University of Massachusetts at Dartmouth
Toxic algal blooms or "red tides" can cause serious health
and economic problems, including Paralytic Shellfish Poisoning (PSP),
which occurs when shellfish, zooplankton, and other marine animals
accumulate toxins while feeding on dinoflagellates of the genus
Alexandrium. For humans, impacts of Alexandrium blooms range from
the quarantine of shellfish beds to sickness or even death if the
contaminated shellfish are eaten. For marine ecosystems, the impacts
can be equally devastating, with mortalities or incapacitation occurring
at multiple levels of the food web as toxins are passed from consumer
to consumer. With evidence that toxic Alexandrium cells may be transported
into Massachusetts coastal waters from the southwestern Gulf of
Maine, researchers are investigating bloom dynamics before and after
a sewage outfall pipe begins to re-route waste from Boston Harbor
to a site nine miles offshore into Massachusetts Bay. During the
first year of the multi-year project, investigators conducted three
cruises in Massachusetts Bay and found Alexandrium to be present
only in very low levels, similar to observations from the previous
three years. Shellfish toxicity was detected in Casco Bay, Maine,
in 1997, and intensive field efforts will be conducted there in
1998. In 1999 sampling efforts will again be focused on Massachusetts
Bay, just months after the outfall will have begun discharging primary
treated effluent into the bay. This research will undoubtedly assist
in future management decisions relating to the controversial outfall
project. (R/B-140)
Impacts of Accelerated Sea Level Rise in
Storm-Induced Sedimentation on Southern New England Coastal Wetlands
Thompson Webb III and Jeffrey P. Donnelly, Brown University
To manage and restore coastal wetlands effectively, the processes
that induce changes in the species distribution in salt marsh communities
must be understood. Many global warming scenarios are predicting
further increases in the rate of sea level rise as well as increases
in the frequency of intense storms in the coming decades. Therefore,
it is important to understand the effects of these factors on the
structure and function of coastal wetland communities. This project
will explore the regional consequences of accelerated sea level
rise and the frequency of storm-induced sedimentation on the community
structure of existing and prehistoric coastal wetlands. Field sampling
and laboratory analysis will be used to test four hypotheses:
- (1) the coastal wetlands of Cape Cod, which are experiencing
the greatest subsidence in the region, have been the first to
be impacted by accelerations in the rate of sea level rise;
- (2) the response of both modern and ancient coastal wetlands
to relative sea level rise rates greater than approximately 2.5
mm/year is a landward shift in community structure favoring stunted
Spartina alterniflora and Salicornia-dominated communities;
- (3) the impacts of accelerated sea level rise have been diminished
in portions of coastal wetlands subject to periodic storm-induced
sedimentation; and
- (4) the timing of recent changes in wetland structure associated
with an acceleration in the rate of sea level rise is coincident
with increased emission of "greenhouse" gases associated
with the onset of the industrial revolution. (R/G-25)
Multiple Tidal Inlet Stability
David G. Aubrey, Woods Hole Oceanographic Institution
A significant portion of the coastlines worldwide are comprised
of estuaries or lagoonal systems, which often serve as habitat for
diverse species and are increasingly used for human settlement.
Many of these systems are connected to the open ocean by one or
more inlets, through which most of the water circulation occurs
due to buoyancy-driven, tidal, and wind-driven motions. A precise
understanding of tidal inlet stability is fundamental for issues
such as water quality, navigability, and beach and barrier stability.
For long embayments, the existence and stability of multiple inlets
can be important for a more efficient water exchange between the
embayment and the ocean. The understanding of inlet interaction
is important since changes in the physical characteristics of one
inlet may affect the stability of adjacent inlets. This project
will develop a model to identify the processes important for stability
in multiple tidal inlet systems and will conduct a field experiment
to test the model. (R/G-27)
Assessing the Potential for Increased Paralytic
Shellfish Poisoning in Massachusetts and Cape Cod Bays due to the
Outfall Effluents
Donald M. Anderson and Andrew R. Solow, Woods Hole Oceanographic
Institution
Harmful algal blooms (HABs) are a serious economic and public health
threat throughout the world. Toxins from dinoflagellates can lead
to Paralytic Shellfish Poisoning (PSP), known to cause shellfish
quarantines, mortality of birds, larval and adult fish, and marine
mammals, and illness or even death in humans. In the Northeastern
U.S. and Canada, organisms responsible for PSP are two dinoflagellates
in the genus Alexandrium. This project is designed to enhance ongoing
research efforts examining the occurrence of toxic Alexandrium blooms
in the Massachusetts and Cape Cod Bays. A new sewage outfall that
will discharge primary treated effluent into Massachusetts Bay is
set to go on-line late in 1998. Opponents to the project believe
that there could be an increase of harmful or toxic algal species
due to nutrients from the outfall effluent. Before this can be proven
or disproven, the variability of Alexandrium population abundance
within the bays must be established, along with thresholds that
are indicative of significant change. Investigators will compile
25 years of state-gathered shellfish toxicity data for the bays
and nearby locations. From the data, they will develop a statistical
model of pre-outfall variability in shellfish toxicity. Once that
is complete, investigators hope to propose "caution" and
"warning" levels that are indicative of significant change
from historical means. And, once the outfall begins operation, the
researchers will test the utility of these criteria using actual
PSP data. (R/B-149)
Controls on Nitrogen Fluxes from Estuarine
Sediments: The Importance of Salinity
Anne E. Giblin and Charles S. Hopkinson, The Ecosystems Center,
Marine Biological Laboratory, and Gary T. Banta, Roskilde University
(Denmark)
It is widely known and accepted that coastal ecosystems can be altered
by nutrient inputs and that there is a direct relationship between
human population in a watershed and the amount of nitrate-nitrogen
that comes out of the watershed and into coastal waters. While many
studies have looked at the relationship between nitrogen loading,
nutrient recycling in the benthos, and the role of nitrogen in primary
productivity, fewer have considered the effect of human-induced
freshwater runoff (deforestation, agriculture, urbanization, river
channeling, and damming, for example) on estuarine systems. Freshwater
input strongly influences estuarine circulation, salinity distribution,
primary production, plant and animal distributions, and nutrient
dynamics. This project will focus on the interaction between freshwater
flow and nutrient dynamics by:
- (a) determining the effect of salinity on nitrogen storage
and release from sediments;
- (b) determining the effect of porewater (the water that is present
in bottom sediment) salinity on rates of sediment nitrification
and denitrification; and
- (c) modeling the implications of salinity control of benthic
nutrient dynamics on temporal and spatial patterns of estuarine
metabolism.
Results from this study will be used to improve
the understanding of the controls on estuarine primary and secondary
productivity, and to refine an existing model of estuarine primary
productivity. This model, which includes a hydrologic component,
could be adapted for any estuary and could be used to assess the
impact of water withdrawal (in drought conditions) or addition (floods
or storms) to a watershed. It could also be used as a management
tool for estuaries where there is some control over the freshwater
inputs on a seasonal basis, to minimize eutrophication problems.
(R/M-41)
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