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MSI Technical Seminars
Monday, May 7, 2007, 12:30 p.m.
Robinson W. "Wally" Fulweiler, Ph.D.
Graduate
School of Oceanography
University of Rhode Island
"Climate Change Impacts on Benthic-Pelagic Coupling
and the Biogeochemistry of Narragansett Bay, R.I."
Climate change has altered the phenology or
seasonal sequencing of events in many ecosystems, including Narragansett Bay, RI
(USA). The timing and magnitude of the winter-spring bloom has changed
dramatically over the last three decades resulting in a 60% decline in water
column chlorophyll a concentrations in mid-Narragansett Bay. This large
decline has been linked to a long-term warming trend. We hypothesized that the
decline in chlorophyll led to a decrease in the quantity and/or quality of
organic matter deposition to the benthos and fundamental changes in sediment
biogeochemical cycling and benthic-pelagic coupling. We observed significant
decreases in sediment respiration and dissolved inorganic nitrogen fluxes in mid
and upper Narragansett Bay compared to rates measured in the 1970s/80s. Net
sediment denitrification in mid-Narragansett Bay also decreased significantly.
In the summer of 2006, high rates of net
sediment nitrogen fixation (-5 to –650 mmol N2-N m-2 h-1)
were measured at four sites. This is particularly unusual since nitrogen
fixation in marine sediments has traditionally been considered inconsequential.
In an effort to understand why this dramatic shift in N2 fluxes
occurred, a series of experiments were conducted using sediment cores and large
marine mesocosms. The experiments were designed to study the effects of
enriching the overlying water with nitrate, ammonium, or phosphate on the net N2
fluxes across the sediment water-interface. In addition to inorganic nutrient
enrichment of the water we also carried out separate experiments in which
organic matter was added to the sediment surface. While inorganic enrichment of
the overlying water caused no change in the net sediment N2 flux,
organic matter enrichment ultimately switched the sediments from net N-fixation
to net denitrification. |