Jr. Dolan, Tintinnid ciliate diversity in the Mediterranean Sea: longitudinal patterns related to water column structure in late spring-early summer, AQUAT MIC E, 22(1), 2000, pp. 69-78
Globally, north-south gradients in diversity are well known, and in the wor
ld ocean they have been related to north-south gradients in water column st
ructure. Here diversity in planktonic ciliates, both taxonomic and morpholo
gical, is explored in the Mediterranean Sea, which displays west-east gradi
ents in the water column characteristics of chlorophyll concentrations and
distributions. Tintinnids, which are loricate planktonic ciliates, were enu
merated and identified in samples from 23 stations between 2 and 32 degrees
E, obtained from the Catalan Sea in June 1993 and from a cross-Mediterrane
an transect in May-June 1996. From west to east, concentrations of tintinni
ds showed Little variability, while numbers of species and genera, as well
as diversity indices (H' values), increased. These parameters were positive
ly related to depths of the chlorophyll maximum layer and negatively correl
ated with chlorophyll concentrations. Corresponding to the west to east inc
reases in diversity were increases in community averages of lorica oral dia
meter and overall length, again positively correlated to deepening of chlor
ophyll maximum depths, and negatively related to average chlorophyll concen
trations. Morphological diversity was related to species diversity, not as
variability in lorica oral diameters, but as variability in average lorica
length. In the Mediterranean Sea, a gradient of taxonomic and morphological
diversity is relatable to a specific feature of the water column, the dept
h of the chlorophyll maximum layer. Trophic specialization as a dominant me
chanism underlying diversity was not supported by data on lorica oral diame
ters.