The shelf edge exchange processes experiment, SEEP-II: an introduction to hypotheses, results and conclusions

Abstract The SEEP (Shelf Edge Exchange Processes)-II experiment was the second of two that took place in the Middle Atlantic Bight (MAB) of the eastern U.S. continental shelf and slope. The experiment included an array of 10 multi-instrumented moorings deployed for 15 months and 10 oceanographic cruises, all designed to address the problem of the fate of continental shelf particulate matter in general, and organic carbon in particular. This paper provides the setting and background for the SEEP Program, the SEEP-II experiment and an introduction to the 18 papers constituting the subject of this special volume. Because those papers lack one of a general nature on the physical oceanographic setting of the experiment, that aspect is treated in somewhat more detail here. The results of the experiment overwhelmingly show that the working hypothesis on which the SEEP Program was undertaken and sponsored by the Department of Energy is not valid. That is, there is not an export to the adjacent slope and open ocean of a large proportion of the particulate matter introduced to and biologically generated in the waters of the continental shelf; most of the biogenic particulate matter is recycled by consumption (bacterial and otherwise) and oxidation on the shelf, and only a small proportion (of order ⪡5%) is exported to the adjacent slope. The small amount that is exported appears to be deposited preferentially in the sediments of an area of the slope centered at about 1000 m, and the export and sedimentation to that depocenter appears to increase from the northern to the southern MAB.

[1]  B. Butman Downslope Eulerian mean flow associated with high-frequency current fluctuations observed on the outer continental shelf and upper slope along the northeastern United States continental margin: implications for sediment transport , 1988 .

[2]  R. Anderson,et al.  Carbon budget for the mid-slope depocenter of the Middle Atlantic Bight , 1994 .

[3]  J. Walsh Particle export at Cape Hatteras , 1994 .

[4]  Graham P. Harris,et al.  Temporal and Spatial Scales in Phytoplankton Ecology. Mechanisms, Methods, Models, and Management , 1980 .

[5]  M. Bothner,et al.  210Pb balance and implications for particle transport on the continental shelf, U.S. Middle Atlantic Bight , 1994 .

[6]  J. Walsh,et al.  The 1983-1984 Shelf Edge Exchange Processes (SEEP)--I experiment: hypotheses and highlights , 1988 .

[7]  L. Pietrafesa,et al.  Water mass linkages between the Middle and South Atlantic bights , 1994 .

[8]  Pierre E. Biscaye,et al.  Fluxes of particles and constituents to the eastern United States continental slope and rise: SEEP—I , 1988 .

[9]  Charles N. Flagg,et al.  Sediment resuspension over the continental shelf east of the Delmarva Peninsula , 1994 .

[10]  L. Pietrafesa,et al.  Summertime thermocline salinity maximum intrusions in the Mid-Atlantic Bight , 1994 .

[11]  J. Ryther Photosynthesis and fish production in the sea. , 1969, Science.

[12]  C. Wirick Exchange of phytoplankton across the continental shelf-slope boundary of the Middle Atlantic Bight during spring 1988 , 1994 .

[13]  P. Falkowski,et al.  Summer nutrient dynamics in the Middle Atlantic Bight: primary production and utilization of phytoplankton carbon , 1983 .

[14]  M. Caruso,et al.  Large‐scale penetration of Gulf Stream water onto the Continental Shelf north of Cape Hatteras , 1992 .

[15]  John J. Walsh,et al.  A simulation analysis of the fate of phytoplankton within the Mid-Atlantic Bight , 1988 .

[16]  John J. Walsh,et al.  Herbivory as a factor in patterns of nutrient utilization in the sea1 , 1976 .

[17]  Karen L. Tracey,et al.  On Gulf Stream Meander Characteristics Near Cape Hatteras , 1986 .

[18]  Sharon L. Smith,et al.  The interaction of phytoplankton, zooplankton and currents from 15 months of continuous data in the Mid-Atlantic Bight , 1994 .

[19]  G. Gawarkiewicz Linear Stability Models of Shelfbreak Fronts , 1991 .

[20]  J. Walsh On the Nature of Continental Shelves , 1988 .

[21]  K. Buesseler,et al.  Mixing of particles and organic constituents in sediments from the continental shelf and slope off Cape Cod: SEEP—I results , 1988 .

[22]  B. Butman,et al.  The Middle Atlantic Bight Cold Pool: Evolution of the Temperature Structure During Summer 1979 , 1982 .

[23]  L. Pietrafesa,et al.  Low-frequency oscillations on the outer shelf in the southern Mid-Atlantic Bight , 1994 .

[24]  P. Falkowski,et al.  Modeling vertical oxygen and carbon flux during stratified spring and summer conditions on the continental shelf, Middle Atlantic Bight, eastern U.S.A. , 1994 .

[25]  P. Kemp Microbial carbon utilization on the continental shelf and slope during the SEEP-II experiment , 1994 .

[26]  R. Beardsley Physical oceanography of the Middle Atlantic Bight , 1976 .

[27]  R. Fairbanks The origin of continental shelf and slope water in the New York Bight and Gulf of Maine: Evidence from H2 18O/H2 16O ratio measurements , 1982 .

[28]  E. Levine,et al.  Mixing of shelf, slope and Gulf Stream water over the continental slope of the Middle Atlantic Bight , 1993 .

[29]  P. Hamilton,et al.  Circulation of slopewater , 1988 .

[30]  G. Gawarkiewicz,et al.  A Gulf Stream-Derived Pycnocline Intrusion on the Middle Atlantic Bight Shelf , 1990 .

[31]  W. Esaias,et al.  COMPOSITION, ABUNDANCE, AND DISTRIBUTION OF ZOOPLANKTON IN THE NEW YORK BIGHT, SEPTEMBER 1974-SEPTEMBER 1975 , 1979 .

[32]  D. Wallace Anthropogenic chlorofluoromethanes and seasonal mixing rates in the Middle Atlantic Bight , 1994 .

[33]  L. Pietrafesa,et al.  Shelf-slope water frontal structure, motion and eddy heat flux in the southern Middle Atlantic Bight , 1994 .

[34]  J. Walsh,et al.  Biological export of shelf carbon is a sink of the global CO2 cycle , 1981, Nature.

[35]  R. Anderson,et al.  Fluxes of particulate matter on the slope of the southern Middle Atlantic Bight: SEEP-II , 1994 .

[36]  P. Kubik,et al.  Anomalous boundary scavenging in the Middle Atlantic Bight: evidence from 230Th, 231Pa, 10Be and 210Pb , 1994 .

[37]  R. Anderson,et al.  Deep-sea floor respiration as an indication of lateral input of biogenic detritus from continental margins , 1994 .

[38]  J. Steele The Structure of Marine Ecosystems , 1974 .

[39]  P. Falkowski,et al.  The fate of a spring phytoplankton bloom: export or oxidation? , 1988 .

[40]  D. Bumpus A description of the circulation on the continental shelf of the east coast of the United States , 1973 .

[41]  P. Falkowski,et al.  The lateral flux of biogenic particles from the eastern North American continental margin to the North Atlantic Ocean , 1994 .

[42]  Sharon L. Smith,et al.  Carbon flux and recycling associated with zooplanktonic fecal pellets on the shelf of the Middle Atlantic Bight , 1994 .

[43]  P. Cornillon,et al.  Gulf Stream water on the shelf and upper slope north of Cape Hatteras , 1991 .

[44]  K. Turekian,et al.  Lead-210 and polonium-210 in ocean water profiles of the continental shelf and slope south of New England , 1988 .

[45]  M. Dagg,et al.  The Impact of Copepod Grazing on the Phytoplankton of Georges Bank and the New York Bight , 1982 .