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MALALA, J.O.1,
M. TACKX2, F. FIERS3
& N. DARO2
1Kenya Marine
and Fisheries Research Institute, Lake Turkana Research Station,
P.O. Box 205, Lodwar, Kenya.
2Free University of Brussels (V.U.B),
Laboratory for Ecology and Systematics, Pleinlaan 2, B-1050, Brussels,
Belgium.
3Royal Belgian Institute for Natural
Sciences, Vautierstraat 29 B-1000 Brussels, Belgium.
The zooplankton community structure of Lake Turkana,
Kenya
Zooplankton distribution and abundance in Lake Turkana was studied
from subsurface samples during the flooding of the Omo River between
August and October 1999 at three sites in the western (Ferguson's
Gulf), central (near Central Island) and eastern (Allia Bay /Sibiloi
National Park) sectors of the lake. The aim was to provide information
on the community structure and diversity at the study sites along
an inshore-offshore direction. Standard environmental variables
such as temperature, Secchi depth, conductivity, pH and dissolved
oxygen were concurrently measured. Particulate Organic Carbon and
phytoplankton chlorophyll a were also determined for all stations.
When subjected to multivariate statistics, Canonical Correspondence
Analysis (CCA) clustered all stations into those located in the
Ferguson's Gulf and those in the rest of the study area. Results
for environmental variables show higher concentration of dissolved
oxygen, conductivity, chlorophyll a, and Particulate Organic Carbon
(POC) in areas located within Ferguson's Gulf, compared to the rest
of the study area. Zooplankton community analysis using TWINSPAN
also showed the inner Ferguson's Gulf as a distinct community separate
from the rest of the lake. The Cyclopoid copepodites and their nauplii,
with nauplii accounting for over 80% numerical abundance in most
gulf stations dominated zooplankton taxa. Calanoid copepod, Cladocera,
Rotifera, and Protozoa were ubiquitous. A Monte Carlo permutation
test (p < 0.05) showed the distribution of the taxa to be mainly
affected in a decreasing order by temperature, Secchi depth, conductivity,
and Particulate Organic Carbon. High carbon to chlorophyll a ratio
suggested that the source of particulate matter might be allochthonous,
mainly from the submerged decaying vegetation that once occupied
the dry Ferguson's Gulf and Allia Bay areas, before the recent flooding
caused by the El Nino rains. Diversity results show the Ferguson's
Gulf to be the least diverse community, while stations influenced
by the open lake waters but located in the Allia Bay/Sibiloi National
Park as the most diverse. Potential influence of temperature, Secchi
depth, conductivity, and Particulate Organic Carbon on the zooplankton
community in these two areas is discussed.
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