1.2. Impact of Nutrients
on Reefs in the Florida Keys
Key
Investigators
Peter K Swart and
Kathryn Lamb
Project Duration
December 15, 1999 – December 14, 2003
OBJECTIVE(S)
The objectives of this
research are to i) document temporal and spatial patterns of variations
in the stable N isotopic composition of organisms in the Florida Keys,
ii) document the variations in the sources of inorganic and organic
nitrogen which are inputted into the Florida Keys form anthropogenic and
natural sources, and iii) construct a model for the cycling of nitrogen
in the Florida Keys
SUMMARY
Dissolved Inorganic Nitrogen Species
(DIN) A new bacterial method (Sigman et al 2001 and Casciotti
et al.2002) is being employed for the analysis of the nitrogen
isotopic concentration of nitrate in waters found in the Florida Keys,
which typically have concentrations less than 1M. Water for isotopic
analysis has been collected from stations with varying depths from
cruises off the Florida reef tract made during June, August, October,
December 2000, February, June, August, November 2001, and February,
April, June, August, October, and December 2002. These samples have
been analyzed for their nitrate concentration and samples collected
during 2002 will be processed according to the new bacterial method
Particulate Organic Material (POM):
The nitrogen and carbon isotopic composition of the particulate organic
matter has also been analyzed from samples collected on the
above-mentioned cruises. The POM data show highly varied patterns
of
Δ15N
and there is seemingly no correlation between
Δ15N
values and any sort of cyclic seasonal patterns of
Δ15N composition. It
is possible that a portion of the signal may be due in part to upwelling
of deep nutrient rich waters off the coast, but this hypothesis is still
being explored.
Algal and Sea Grass Material:
Over 100 samples of macro and turf algae, as well as sea grasses have
been collected from the Pennekamp State Park, Florida Keys National
Marine Sanctuary and analyzed for the carbon and nitrogen isotopic
composition. Preliminary results show that the inshore reefs had
an elevated
Δ15N signal, as compared to the offshore reefs,
which is often cited as an indicator of anthropogenic waste. However,
when looking at a single transect line from inshore to offshore, the 15N
values show no definitive trend which may indicate a mixing of different
nutrient sources.
Herbivorous Fish: The carbon and
nitrogen isotopic composition has been measured on approximately 75
herbivorous fish muscle tissue from the FKNMS. Tissue sampled in the
show a similar trend of heavy
Δ15N values on more inshore
reefs and lighter values on the more offshore reefs. At this point in
time, however, we are working towards expanding the breadth of focus to
include piscivores fish as an additional point of comparison. Further
assessments are currently being investigated and will be reported in the
near future.
Corals: Stable N isotopic
analysis of coral tissues and zoozanthellae revealed them to have a
normal range of values.
PUBLICATION(S)
Lamb, K.A., Swart, P.K.,
and Ellis, G.S. (2002) Insights into Nitrogen Isotope Fractionation in
Coral Reefs, Eos. Trans. AGU, vol.83, no.47, Fall Meeting Suppl.,
Abstract B71A-0718
Lamb, K.A., Swart, P.K.,
and Ellis, G.S. (2002) A detailed study of the nitrogen isotopic
composition of organic and inorganic nitrogen in a coral reef
environment, Proceedings from 2002 Ocean Sciences Meeting, American
Geophysical Union, vol.83, no.4.
Ellis, G., Moses, C.,
Swart, P.K., and Milne, P. (2000) Contributions of natural and
anthropogenic nitrogen in the Florida Keys reef tract using stable
isotope composition and natural sterol concentration, GSA Abstracts with
Programs, p. 102.
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