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The prokaryotic picoplankton (PPP) composition was studied in the tropical high-altitude saline Lake Alchichica, Mexico, using fluorescence in situ hybridization. Thetemporal dynamics of the PPP followed the annual hydrodynamics of this warm-monomictic lake. The abundance of both the autotrophic (APP) and heterotrophic(HPP) functional groups of PPP increased during the mixing period to reachmaximum values at the beginning of the stratification period, when the highesthybridization percentages for the domain Bacteria were also registered. The increasein PPP was most likely related to the availability of nutrients soon after the start ofthe mixing period. Throughout the rest of the stratification, APP and HPP decreasedsignificantly together with the hybridization percentages, mostly related to theexhaustion of nutrients in the mixing zone. In spite of being oligosaline, the prokar-yotic composition of Lake Alchichica was more typical of fresh than of saltier waterbodies. During the mixing period, the Pcy and Planctomycetes (PLA) formed the mainbacterioplankton fraction. Meanwhile throughout the stratification period PLA,Betaproteobacteria (BET) and Gammaproteobacteria (GAM) were the most abun-dant groups in the epilimnion and metalimnion. The domain Archaea (ARCH), BET,GAM, Paracoccus the principal denitrifier of the Alphaproteobacteria and sulphate-reducing bacteria were dominant in the oxycline and hypolimnion in associationwith dissolved oxygen depletion and the nutrient enrichment of the deeper strata.KEYWORDS: prokaryoplankton; warm-monomictic; oligosaline; tropical high-altitude

Ciliate picoplanktivory was studied in two different freshwater systems with abundant auto- trophic picoplankton (APP): the eutrophic Rimov Reservoir (South Bohemia) during the late summer of 1993 and the oligo- to mesotrophic lake Piburger See (Tyrol) during May 1994. Picoplankton were sized by an image-analysis system and species-specific grazing rates of ciliates on bacteria and APP were determined using fluorescently labelled prey. According to the grazing data (as the mean uptake rate of picoplankton ind.~' h1), ciliates were split into three ecological groups in order of their decreas- ing picoplanktivory and increasing significance of nanophytoplankton in their diet, (i) Highly efficient fine suspension feeders consisting of vorticellids (4200 bacteria, 560 APP), four oligotrichs and Cyclidium sp. (380-1580 bacteria, 57-210 APP), with 2 u.m. (ii) Less efficient fine suspension feeders, coarse filter feeders and detritophages consisting of Cinetochilum margaritaceum, Pelagostrombidium fallax, Cyrtolophosis mucicola and Coleps spp. (60-173 bacteria, 2-27 APP), with 7-32% of individuals ingesting algae >2 n.m. (iii) Raptorial feeders consisting of four prostomatids belonging to the genera Urotricha and Balanion, with a negligible importance of picoplanktivory (8-61 bacteria, 0.2-14 APP). With the exception of one prostomatid. >58% of individuals ingested algae >2 (j.m. Grazing data for the six species from the first group were converted into organic carbon. Assuming a 35 % gross growth efficiency, the calculated potential doub- ling times were between 29 (Hatteria grandinella) and 43 h (an unidentified oligotrich), except for the mixotrophic Pelagohalteria viridis (118 h). The doubling times estimated from changes in ciliate abun- dance for four out of the six species were very close to the calculated values, indicating that this group of heterotrophic ciliates can meet all of its carbon requirements by feeding exclusively on picoplankton.