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Physical variables, carbon cycling and primary producer couplings
in a shallow tropical lagoon (Barra Lagoon, Brazil)
Jean-Pierre Carmouzea,
Patricia Domingosb
aDepartamento
de Geoquimica, UFF, Morro do Valonguinho, 24021-007 Niteroi,
RJ, Brazil.
Present address: IRD BP. 165, 97 323 Cayenne Cedex, French
Guiana.
bNPPN, UFRJ, C.C.S. Bloco H, Ilha do Fundão, 21941-590
Rio de Janeiro, RJ, Brazil
carmouze@cayenne.cayenne.ird.fr.
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Abstract
The Barra Lagoon (28°S and 43°W, 7 km²,
mean depth, 1m, salinities from 3 to 12) was investigated
between October 1990 and August 1993. We report here a first synthesis
of organic carbon metabolism, the phytoplankton community and their
mutual interactions. Barra Lagoon exhibited a hypereutrophic state
(high values of phytoplanktonic biomasses, diurnal metabolic rates,
particulate and dissolved organic carbon concentrations). As with
most shallow lagoons, Barra Lagoon was very sensitive to short-term
meteorological changes which induced high day to day changes in
organic carbon metabolism and severely dampened seasonal trends.
But surprisingly, when consistent structural changes occurred, its
total organic carbon metabolism was rapidly dampened by shifts from
pelagic to benthic carbon metabolism and vice-versa. Seasonal auto/heterotrophic
shifts of the ecosystem (generally autotrophy in summer and heterotrophy
in winter) were not always verified. They were more strongly linked
to growing and degeneration phases of pelagic and benthic algae.
Biological activity was mainly controlled by the rate of nutrient
in situ regeneration (low nutrient concentrations in water). In
these conditions, small-size phytoplankton species predominated,
as they are more efficient than large forms in sharing nutritive
resources. Cyanophyceae were ecologically favoured by low transparency,
nitrogen limitation and high nutrients regenerated in the water
column, while small species of Dinophyceae and Chrysophyceae were
promoted by a higher photic layer, nitrogen content and benthic
nutrient regeneration. Extra input of nutrients (proceeding from
fish-kill in February1991, from decomposition of macro-algae after
a temporary phase of colonization in August-September 1992, and
from abundant rainfalls) induced an ephemeral growth of larger species
at the expense of Cyanophyceae. Cyanophyceae lost their dominance
also when temperature fell to 20° C.
Keywords: Eutrophication, pelagic metabolism, metabolism
nutrient dynamic, nitrogen deficiency,
phytoplankton size, macro-algae colonization
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