Publications
Scientific literature and information products produced by Woods Hole Coastal and Marine Science Center staff.
Filter Total Items: 1749
Responses of infaunal populations to benthoscape structure and the potential importance of transition zones Responses of infaunal populations to benthoscape structure and the potential importance of transition zones
Relationships between population abundance and seafloor landscape, or benthoscape, structure were examined for 16 infaunal taxa in eastern Long Island Sound. Based on analyses of a side-scan sonar mosaic, the 19.4-km2 study area was comprised of six distinct large-scale (> km2) benthoscape elements, with varying levels of mesoscale (km2-m2) and small-scale ( m2) physical and biological...
Authors
R.N. Zajac, R. S. Lewis, L. J. Poppe, D.C. Twichell, J. Vozarik, M. L. DiGiacomo-Cohen
Variation in habitat use by juvenile Acadian redfish, Sebastes fasciatus Variation in habitat use by juvenile Acadian redfish, Sebastes fasciatus
A basic paradigm in behavioral ecology is that organisms expand their distribution as preferred sites become saturated with individuals that reduce the availability of resources (e.g., shelter, prey) on a per capita basis. Previous fish community studies at Stellwagen Bank National Marine Sanctuary have shown that juvenile Acadian redfish Sebastes fasciatus (
Authors
P.J. Auster, J. Lindholm, P. C. Valentine
Birth of the modern Chesapeake Bay estuary between 7.4 and 8.2 ka and implications for global sea-level rise Birth of the modern Chesapeake Bay estuary between 7.4 and 8.2 ka and implications for global sea-level rise
Two major pulses of sea-level rise are thought to have taken place since the last glacial maximum — meltwater pulses (mwp) 1A (12 cal ka) and 1B (9.5 cal ka). Between mwp 1B and about 6 cal ka, many of the complex coastal ecosystems which ring the world’s oceans began to form. Here we report data for rhenium, carbon isotopes, total organic carbon, and fossil oysters from Chesapeake Bay...
Authors
John F. Bratton, Steven M. Colman, E. Robert Thieler, Robert R. Seal
Anthropogenically induced changes in sediment and biogenic silica fluxes in Chesapeake Bay Anthropogenically induced changes in sediment and biogenic silica fluxes in Chesapeake Bay
Sediment cores as long as 20 m, dated by 14C, 210Pb, and 137Cs methods and pollen stratigraphy, provide a history of diatom productivity and sediment-accumulation rates in Chesapeake Bay. We calculated the flux of biogenic silica and total sediment for the past 1500 yr for two high-sedimentation-rate sites in the mesohaline section of the bay. The data show that biogenic silica flux to...
Authors
Steven M. Colman, J.F. Bratton
Stratigraphic framework of sediment-starved sand ridges on a mixed siliciclastic/carbonate inner shelf; west-central Florida Stratigraphic framework of sediment-starved sand ridges on a mixed siliciclastic/carbonate inner shelf; west-central Florida
Seismic reflection profiles and vibracores have revealed that an inner shelf, sand-ridge field has developed over the past few thousand years situated on an elevated, broad bedrock terrace. This terrace extends seaward of a major headland associated with the modern barrier-island coastline of west-central Florida. The overall geologic setting is a low-energy, sediment-starved, mixed...
Authors
J.H. Edwards, S. E. Harrison, S. D. Locker, A. C. Hine, D.C. Twichell
Real-time seismic data from the coastal ocean Real-time seismic data from the coastal ocean
A moored-buoy system for collecting real-time seismic data from the coastal ocean has been developed and will be deployed for its initial field trial in the fall of 2003. The key component in this moored system is an ultra-stretchy mooring hose that provides compliance for waves and currents and protects the electrical conductors connecting an Ocean Bottom Seismometer (OBS) to a surface...
Authors
D. Frye, Uri S. ten Brink, W. Paul, K. Peal, K. Von Der Heydt
Sand ridges off Sarasota, Florida: A complex facies boundary on a low-energy inner shelf environment Sand ridges off Sarasota, Florida: A complex facies boundary on a low-energy inner shelf environment
The innermost shelf off Sarasota, Florida was mapped using sidescan-sonar imagery, seismic-reflection profiles, surface sediment samples, and short cores to define the transition between an onshore siliciclastic sand province and an offshore carbonate province and to identify the processes controlling the distribution of these distinctive facies. The transition between these facies is...
Authors
D. Twichell, Gillian L. Brooks, G. Gelfenbaum, V. Paskevich, Brian Donahue
Mobile fishing gear reduces benthic megafaunal production on Georges Bank Mobile fishing gear reduces benthic megafaunal production on Georges Bank
This study addresses the effect of mobile fishing gear disturbance on benthic megafaunal production on the gravel pavement of northern Georges Bank. From 1994 to 2000, we sampled benthic megafauna with a 1 m Naturalists' dredge at shallow (47 to 62 m) and deep (80 to 90 m) sites. The cessation of fishing in large areas of Georges Bank in January 1995 allowed us to monitor changes in...
Authors
J.M. Hermsen, J.S. Collie, P. C. Valentine
Sediment-starved sand ridges on a mixed carbonate/siliciclastic inner shelf off west-central Florida Sediment-starved sand ridges on a mixed carbonate/siliciclastic inner shelf off west-central Florida
High-resolution side-scan mosaics, sediment analyses, and physical process data have revealed that the mixed carbonate/siliciclastic, inner shelf of west-central Florida supports a highly complex field of active sand ridges mantled by a hierarchy of bedforms. The sand ridges, mostly oriented obliquely to the shoreline trend, extend from 2 km to over 25 km offshore. They show many...
Authors
S. E. Harrison, S. D. Locker, A. C. Hine, J.H. Edwards, D. F. Naar, D.C. Twichell, D. J. Mallinson
Use of sand wave habitats by silver hake Use of sand wave habitats by silver hake
Silver hake Merluccius bilinearis are common members of fish communities in sand wave habitats on Georges Bank and on Stellwagen Bank in the Gulf of Maine. Observations of fish size v. sand wave period showed that silver hake are not randomly distributed within sand wave landscapes. Regression analyses showed a significant positive relationship between sand wave period and fish length...
Authors
P.J. Auster, J. Lindholm, S. Schaub, G. Funnell, L.S. Kaufman, P. C. Valentine
Tidal truncation and barotropic convergence in a channel network tidally driven from opposing entrances Tidal truncation and barotropic convergence in a channel network tidally driven from opposing entrances
Residual circulation patterns in a channel network that is tidally driven from entrances on opposite sides are controlled by the temporal phasing and spatial asymmetry of the two forcing tides. The Napa/Sonoma Marsh Complex in San Francisco Bay, CA, is such a system. A sill on the west entrance to the system prevents a complete tidal range at spring tides that results in tidal truncation...
Authors
J.C. Warner, D. Schoellhamer, G. Schladow
Winter-time circulation and sediment transport in the Hudson Shelf Valley Winter-time circulation and sediment transport in the Hudson Shelf Valley
The Hudson Shelf Valley is a bathymetric low that extends across the continental shelf offshore of New York and New Jersey. From December 1999 to April 2000 a field experiment was carried out to investigate the transport of sediment in the shelf and valley system. Near-bed tripods and water-column moorings were deployed at water depths from 38 to 75 m in the axis of the shelf valley and...
Authors
C. K. Harris, B. Butman, P. Traykovski