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USGS Studies in Long Island Sound:
Geology, Contaminants, and Environmental Issues

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Introduction
Long Island Sound is a major coastal estuary near the New York-Connecticut metropolitan area. More than eight million people live in its watershed. Due to the enormous population, the Sound is used heavily and its sea floor has been impacted by human activities. There are many benthic habitats in the Sound that support large commercial and recreational fisheries. Sediments of the Sound are a sink for wastes and contaminants from various sources such as wastewater treatment plants, urban and agricultural runoff, and waste disposal.

USGS Studies in Long Island Sound

Figure 1. Deployment of a grab sampler, equipped with still and video cameras, in Long Island Sound.

USGS Research

The U.S. Geological Survey's Coastal and Marine Geology Program began studying the Long Island Sound region in the 1980s. The Long Island Sound Environmental Studies program, initiated in 1995, was designed to understand three main points: 1) the modern sedimentary processes that control the transport of bottom processes and the formation of related habitats, 2) to identify and define benthic habitats throughout the region for future studies and management decisions, and 3) to understand the distribution, transport, and fate of contaminants in sediments of the Sound.

Other USGS studies have focused on the behavior of water and contaminants in the watersheds that discharge into the Sound, and on coastal wildlife. Additional studies have been undertaken in collaboration with the States of Connecticut and New York, the Environmental Protection Agency, NOAA, the Corps of Engineers, and academic institutions in the region. Descriptions of USGS research on geologic, chemical, oceanographic, and biological aspects of the Long Island Sound are accessible in the menu to the left. Research highlights are shown below.

  Research Highlights

Distribution of Surficial Sediment in Long Island Sound
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Figure 2. The distribution of surficial sediments in Long Island Sound and adjacent waters. Triangular and block diagrams explain the map units.

Surficial Sediment Distribution

The regional surficial sediment distribution is extremely patchy, but exhibits textural trends which are related to sea-floor geology, bathymetry, and the effects of currents. In general, gravelly sediments are dominant in easternmost Long Island Sound, where tidal currents are strong, and in areas characterized by glacial tills. Sand occurs across the east-central Sound and along most of the nearshore margins. Silty sand and sand-silt-clay mark transitions within the Sound from higher to lower energy environments, such as on the flanks of bathymetric highs. Clayey silt and silty clay are predominant in low-energy environments, such as on the floors of the central and western basins.

Sedimentary Environments
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Figure 5. Shows the regional distribution of the four categories of sea-floor sedimentary environments identified in the Long Island Sound study area.

Sedimentary Environments

The circulation in Long Island Sound, which is controlled by an east-to-west weakening of tidal-current speeds coupled with the westward-directed estuarine bottom drift, has produced a succession of sedimentary environments. The succession begins with erosion or nondeposition at the narrow eastern entrance to the Sound, changes to an extensive area of coarse-grained bedload transport in the east-central Sound, passes into a contiguous band of sediment sorting (where the estuary noticeably widens), and ends with broad areas of fine-grained deposition on the flat basin floor in the central and western Sound. The distribution of these environments provides insight into the long-term fate of contaminants, and is a guide to the future utilization of the sea floor. This information also helps to define the general locations and variability of benthic biological habitats, and gives a long-term perspective of sea-floor conditions in the Sound. Click here to view a USGS fact sheet on this topic.

Copper concentrations
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Figure 3. Copper (Cu) concentrations in the surface sediments (0-2 cm) of Long Island Sound.

Contaminant Distribution and Accumulation in Sediments

Trace metal contamination of sediments from land-based activities is found throughout Long Island Sound and its watershed. In 1996, the USGS collected samples of surface sediments in the Sound to measure amounts and locations of metal contaminants and to establish a baseline for identifying changing conditions. Average concentrations of silver and copper in the Sound were 4-5 times greater than naturally-occurring background values. Zinc, lead, and manganese concentrations were enriched 1.5-2 times greater than natural background levels. The concentration distributions of these elements correlates with the sedimentary environment, the sediment texture, the organic carbon content, and the abundance of Clostridium perfringens, a bacterium used as a sewage tracer. Strong water currents remove fine-grained sediments, and the contaminants that are associated with them from sandy, reworked environments and concentrate them in the depositional basins. Thus, the greatest enrichment of metals is found in the depositional environments and muddy sediments of the central and western basins, due to both proximity to pollutant sources and the natural movement of sediments and contaminants within the Sound. Click here to view a USGS fact sheet on this topic.

Concentration Profiles
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Figure 4. Concentration profiles of Clostridium perfringens,
mercury, and zinc for a sediment core in western Long Island Sound shown with the regional population increase.

Historical Record of Pollution and Environmental Changes

Sediment cores provide a record of past conditions in Long Island Sound because recently deposited sediments at the top overlie older sediments below. Measurements of mercury and of Clostridium perfringens, a bacterial tracer of sewage, in cores show the onset of anthropogenic contamination two centuries ago and the effects of the increase in a regional human population since then. Concentrations of metal contaminants have decreased in recent decades, but Clostridium perfringens has not. Some areas of the Sound have much faster accumulation of sediment and contaminants than others, but regions of the Sound which now have high contaminant enrichments have also had them in the past. Sediments record changes in pollution and other environmental conditions which may be linked to fluctuations over the same time periods in the populations of small organisms (benthic foraminifera) that live on the sea floor.

Environmental Change
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Figure 6. A simulation of bottom bedload transport by currents. Arrows are not scaled; color legend shows magnitude of transport.

Sediment Transport

Three-dimensional, numerical modeling provides a general description of the regional distribution and causes of bottom currents in Long Island Sound in relation to sedimentary environments. Near-bottom current simulations show that the tidal currents, locally enhanced by estuarine circulation and wind events, control transport in the deeper parts of the Sound and promote net westward sediment transport. Our simulations also show that wind- and wave-driven bottom currents control transport along the shallow margins and cause the relatively coarse-grained sediments that occur in these regions, but that the effect of these currents drops off dramatically with increasing water depth.

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Scientists

USGS Coastal & Marine Geology Program

Lawrence J. Poppe; lpoppe@usgs.gov (Geology, Seafloor Mapping)
Richard Signell; rsignell@usgs.gov (Sediment Transport, Bathymetry, Oceanography)
Harley Knebel; retired (Sedimentary Environments/Sea-Floor Mapping)
S. Jeffress Williams; jwilliams@usgs.gov (Aggregate Resources)
Valerie Paskevich; vpaskevich@usgs.gov (GIS and Imagery)

 

Collaborators

NOAA
Marc Moser
Shep Smith
State of Connecticut
Beth Doran
University of Connecticut
Ralph S. Lewis
Peter Auster
University of New Haven
Roman Zajak
U.S. Army Corps of Engineers
Thomas Fredette
U.S. Environmental Protection Agency
Mark Tedesco
Wesleyan Univeristy
Johan C. Varekamp
Ellen Thomas

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This page last modified on Monday, 14-Jan-2013 04:51:00 EST