LohrenzSE, University of Southern Mississippi, Stennis Space Center, MS 39529, USA, Steven.Lohrenz@usm.edu
Redalje, D, G, University of Southern Mississippi, Stennis Space Center, MS 39529, USA, Donald.Redalje@usm.edu
Verity, P, G, Skidaway Institute of Oceanography, Savannah, GA 31411, USA, peter@skio.peachnet.edu
Flagg, C, , Brookhaven National Laboratory, Upton, NY 11973, USA, flagg@bnl.gov 
SEASONAL CONTRASTS IN BIOMASS AND PRIMARY PRODUCTION OVER THE CONTINENTAL SHELF OFF CAPE HATTERAS, NORTH CAROLINA
Coastal margins are frequently regions of high primary production and subject to variability from both natural and anthropogenic forcing. As part of DOE- and NSF-sponsored research, we conducted studies during March and July of 1996 of spatial and temporal patterns of chlorophyll and primary production in continental shelf waters off Cape Hatteras, North Carolina. Primary production was determined using a wavelength-resolved photosynthesis-irradiance model. Highest chlorophyll concentrations during March were located in a mid-shelf region corresponding to an area of intermediate salinities. Cross-shelf sections revealed high subsurface concentrations near the shelf break. In July, chlorophyll concentrations were generally lower. Highest water column integrated primary production during March (>2.5 gC/m2/d) was observed near the shelf break. In contrast, highest values in July (>3 gC/m/d) were associated with low salinity inner shelf water. The high spring productivity at the shelf break was dominated by larger (>8 micron) phytoplankton and nutrient data suggest this feature may be a consequence of upwelling at the shelf break. This productivity may be quantitatively important in the overall carbon/nitrogen budget of the southern Mid-Atlantic Bight shelf.
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RedaljeDG, The University of Southern Mississippi, Stennis Space Center, USA, Donald.Redalje@usm.edu
Lohrenz, S, E, The University of Southern Mississippi, Stennis Space Center, USA, Steven.Lohrenz@usm.edu
Verity, P, G, Skidaway Institute of Oceanography, Savannah, USA, peter@skio.peachnet.edu
Holtermann, K, , The University of Southern Mississippi, Stennis Space Center, USA, holterma@ssc.usm.edu
PHYTOPLANKTON COMMUNITY STRUCTURE WITHIN A DISCRETE WATER MASS IN THE COASTAL WATERS OFF CAPE HATTERAS, NORTH CAROLINA
As part of the Ocean Margins Program, we examined the biogeochemical cycling of carbon within discrete coastal water masses off Cape Hatteras, North Carolina. Drogues set at 10 meters were followed and water sampled daily from 3 depths, from the surface to the base of the euphotic zone, during Spring (March 1996) and Summer (July 1996). Pigments were analyzed using HPLC for the total water sample and for the < 8 micrometer size fraction. CHEMTAX (Mackey et al., 1996), a factor analysis computer program, was used to examine phytoplankton community structure using marker pigments to determine the relative importance of various taxa. In addition, we used stepwise multiple linear regression techniques relating chlorophyll a and marker xanthophyll pigments as a second approach. Initial applications indicate that both approaches yielded similar results. In March, whole water samples were dominated by diatoms, with consistent contributions from dinoflagellates and cryptophytes. The < 8 micrometer fraction was dominated by small diatoms, chrysophytes, cryptophytes and dinoflagellates. In Summer, diatoms were still present and important, but prymnesiophytes, cryptophytes and cyanobacteria contributed in both size classes.
 
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VerityPG, Skidaway Institute of Oceanography, 10 Ocean Science Circle, Savannah, GA 31411, USA, peter@skio.peachnet.edu
Redalje, D, G, Dept. of Marine Science, University of Southern Missippi, Stennis Space Center, MS 39529-0001, USA, donald.redalje@usm.edu
Lohrenz, S, E, Dept. of Marine Science, University of Southern Missippi, Stennis Space Center, MS 39529-0001, USA, steven.lohrenz@usm.edu
Paffenhofer, G, A, Skidaway Institute of Oceanography, 10 Ocean Science Circle, Savannah, GA 31411, USA, cmp@skio.peachnet.edu 
COUPLING BETWEEN PRIMARY PRODUCTION AND PELAGIC CONSUMPTION IN TEMPERATE OCEAN MARGIN PELAGIC ECOSYSTEMS
Three fates potentially consume primary production: portions can be oxidized within the water column, portions can sediment to shelf/slope depots, and portions can be exported to the interior ocean. Zooplankton mediate these events. During DOE- and NSF-sponsored studies on the Mid and South Atlantic Bight shelves, we determined the role of microzooplankton in these processes. Abundance, composition, and biomass were determined using an quasi-automated imaging cytometry system. Grazing and growth rates were measured during dilution incubation experiments using chlorophyll a as a proxy for phytoplankton biomass. Primary production (PP), measured as C-14 uptake, was generally 0.5-1.0 gC/m2/d in spring and 0.5-2.0 in summer. Typically, one-half or more of PP was contributed by <8um cells. Averaged over time and space, microzooplankton grazed 57% of chlorophyll a production. Chlorophyll production, the <8:total fraction of chlorophyll standing stock, and microzooplankton grazing impact all increased with increasing temperature. These data indicate that, contrary to traditional paradigms about shelf ecosystems, small autotrophs contributed the majority of production, and that this carbon was actively incorporated into the microbial food web.

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