Integrated Management of a Coastal Lagoon in the Ebro Delta
Integrated Management of a Coastal Lagoon in the Ebro DeltaF.A. Comin1, M. Martin1, M. Menendez1, J.A. Romero1,
J.A. HerreraSilveira2
1 Department of Ecology, University of Barcelona, Barcelona,
Spain
2 CINVESTAVIPN, Cordemex, Merida, Yucatan, Mexico
Abstract
Tancada is a shallow (average depth 37 cm) and small
(1.8 km2) coastal lagoon in the Delta of the Ebro River
(NE Spain) which has been submitted to different management
practices since 1990 as a consequence of agricultural
regulatory developments. The objective of this paper
is to describe the consequences of these management
of these practices in the water quality and the biological
community of the lagoon and to present management practices
which could be put in operation at low cost to achieve
an improvement in the ecological characteristics of
the lagoon.
Based on its geomorphology and hydrography, two
basins (West and East basins) connected by a narrow
strait can be distinguished in the lagoon. The longest
axis of the lagoon is parallel to the sea coast with
water exchanges take place in both basins through several
channels in each basin. Fresh water inflows through
drainage channels from rice fields take place only
in the West basin.
Differences observed in hydrological (freshwater
inputs and water turnover), chemical (dissolved inorganic
nutrients in the water) and biological (phytoplankton,
macroalgae and submerged rooted macrophytes) variables
studied in 199091 and 199293 indicate that high freshwater
inputs decrease the conductivity of the water in the
lagoon from 30 mS cm1 to 15 mS cm1 in one month and
at the same time increased dissolved inorganic nitrogen
(DIN) and phosphorous (SRP) concentrations in the water,
reaching maxima of 50 micrometer and 9 micrometer,
respectively, at the peaks of the fresh water discharges.
During the periods of high freshwater discharge, phytoplankton
increased its populations (maximum of 50 mg chlorophyll
a m3) and experiment pulses related to external nutrient
inputs.
In contrast during periods of no freshwater inputs
and very low water exchange with the sea, conductivity
increases over the sea water (60 mS cm1) nutrient concentrations
in the water of the lagoon are much lower (maxima of
5 micro M DIN and 1.5 micro M SRP). Phytoplankton is
much lower (10 mg chlorophyll a m3) and huge amounts
of macroalgae develop during summer depleting submerged
rooted populations of macrophytes and phytoplankton.
Macroalgae (including Chaetomorpha, Cladophora, and
Ulva species) occupy large areas of the lagoon during
these periods and reach in some places higher biomasses
than macrophytes (Ruppia). These differences
between the two basins of the lagoon during two years
with different water regime suggest that an intermediate
water (with low nutrient concentrations) between no
freshwater inflows and heavy freshwater discharges
would improve the characteristics of the water in the
lagoon, allowing submerged rooted macrophytes, which
are the basis for a well structured trophic web, to
develop extensive and permanent populations. The objective
of decreasing the nutrient concentrations in the freshwater
discharged in the lagoon can be achieved using small
areas of marshes dominated by emergent macrophytes
as filters of nutrients in the surroundings of the
lagoon. Experiments performed "in situ" (in
5000 m2 experimental marshes demonstrated that between
79 and 98% of the nitrogen and 300 and 90% of the phosphorous
in the water from rice fields can be retained in marshes
before the water reaches the lagoon.
The combination of using marshes to filter nutrients
in the freshwater discharged into the lagoon and an
adequate water regime avoiding huge discharges in a
short period of time would improve water characteristics
in the lagoon and would permit the development of a
biological community based on submerged rooted macrophytes
which will give support to fish and aquatic bird populations.