Steve W. Ross, North Carolina National Estuarine Research Reserve The U.S. East Coast continental slope, from Norfolk Canyon (off Virginia) south to Cape Lookout, NC, is an area of dramatic transition between the Middle Atlantic Bight province, with its major submarine canyons, and the South Atlantic Bight province of the Blake Plateau. The central part of this region, just north of Cape Hatteras, is unique hydrographically, (1) as the zone where the northward-flowing Gulf Stream meets the southward-flowing Virginia current, which together turni seaward, and (2) as the zone where the Gulf Stream crosses the underlying southward- flowing Western Boundary Undercurrent, resulting in an upper middle slope zone of little net motion. These characteristics produce highly productive conditions in the area. The Hatteras slope around The Point harbors a unique, productive, and potentially fragile biological community as well as extremely important commercial and recreational fisheries. The area has the highest densities of benthic infauna anywhere along the U.S. East Coast continental slope, much higher organic carbon deposition rates than adjacent regions, an unusual concentration of benthic fishes and megafaunal invertebrates, and high levels of unusually rich suspended matter. The high productivity translates into an unusual concentration of large pelagic sportfishes, seabirds, and whales at or near the surface in the same area. The mission objectives for this segment of the Islands in the Stream/South Atlantic Bight Expedition are to (1) document fish communities and habitats throughout the water column, and (2) define trophic/energetic pathways over the whole water column (surface to around 1,000 m). We hypothesize that the unique surface and bottom faunas of The Point are interdependent (ecologically linked). If so, human perturbations of the bottom and midwater faunas may have significant impacts on pelagic fishes, seabirds, and marine mammals of economic and aesthetic importance. However, such an ecological coupling, which would be expressed by food-web interconnections among the nekton (fishes and large mobile invertebrates), has not yet been established. Nevertheless, dense concentrations of midwater fishes and squids observed near the bottom at depths of 400-800 m suggest upward cycling of organic matter as living prey for pelagic fishes. We hope to define these nekton faunal trophic linkages at The Point. Habitats to be examined include:
Key Species (S=surface, M=midwater, B=bottom)
Protected Areas
(top) |