ABSTRACT. Photosynthetic pico-and nanoplankton dominate phytoplankton biomass and primary production in the oligotrophic open ocean. Species composition, community structure, and dynamics of the eukaryotic components of these size classes are poorly known primarily because of the difficulties associated with their preservation and identification. Molecular techniques utilizing 18S rRNA sequences offer a number of new and rapid means of identifying the picoplankton. From the available 18S rRNA sequence data for the algae, we designed new group-specific oligonucleotide probes for the division Chlorophyta, the division Haptophyta, and the class Pelagophyceae (division Heterokonta). Dot blot hybridization with polymerase chain reaction amplified target rDNA and whole-cell hybridization assays with fluorescence microscopy and flow cytometry were used to demonstrate probe specificity. Hybridization results with representatives from seven algal classes supported the phylogenetic affinities of the cells. Such group-or taxon-specific probes will be useful in examining community structure, for identifying new algal isolates, and for in situ detection of these three groups, which are thought to be the dominant algal taxa in the oligotrophic regions of the ocean.
The dispersal and history of species affects their genetic population structure at both small and large geographical scales. The common whelk, Buccinum undatum, is a widespread subtidal gastropod in the North Atlantic that has no planktonic larvae and has thus limited dispersal capacity. The snail, which has been harvested by humans for centuries, is highly variable in morphology. To evaluate the population structure in the rich fishing grounds in western Iceland and its divergence from samples across the Atlantic, genetic patterns based on sequence variation in two mitochondrial (mt)DNA genes (COI and 16S) and five microsatellites were studied and compared with variation in populations from both sides of the Atlantic. Significant differences in allele and haplotype frequencies were found among samples separated by short distances along the coast of Iceland. Partition of the variation showed larger variance among samples obtained from distant regions than from neighbouring sites and genetic distances were correlated with geographical distance among populations in Europe. Phylogeographic patterns in mtDNA reveal different monophyletic lineages on both sides of the Atlantic, which predate the onset of the Ice Age and which may constitute cryptic species. Similar micro-and macrogeographical patterns were observed for the mtDNA and microsatellite markers, despite high frequencies of null alleles. Bayesian skyline reconstructions of the demographic history and mismatch distributions suggest that, although sizes of some populations were unaffected by Ice Age glaciations, others show signs of expansion after the Last Glacial Maximum. These phylogeographical patterns are consistent with patterns expected for low dispersal species that have survived in allopatric glacial refugial populations on both sides of the Atlantic and in deep-sea refugia within each continent. The observed genetic structure has implications for conservation and sustainable management of the harvested populations.
Benthic Cladocera were monitored at five sites in Lake Myvatn, Iceland, over a decade (1990)(1991)(1992)(1993)(1994)(1995)(1996)(1997)(1998)(1999), as part of a programme documenting the population fluctuations of animals at different trophic levels in the lake. The species composition remained relatively stable over the first seven years, but in 1997 the population of Eurycercus lamellatus was greatly reduced at all sites. The following year saw a mass occurrence of Alona rectangula and Alonella nana that were previously abundant only locally and rare at most sites. Alona affinis, A. quadrangularis, Acroperus harpae and Chydorus sphaericus were not affected. In 1999 the Cladocera assemblages returned to the pre-1997 situation. The shift was from large-bodied epibenthic and planktonic species (Eurycercus, Daphnia) to small infaunal (Alona rectangula) and ubiquitous (Alonella nana) species. Medium sized (Alona, Acroperus) and some small cladocerans (Chydorus) were not affected. The course of events was reminiscent of a trophic cascade caused by a change in size-selective predation pressure. If so, the impact of a predatory fish population (three-spined stickleback, Gasterosteus aculeatus) depended on whether cyclic chironomid populations were in a high or a low phase. The change in the Cladocera coincided with profound changes in the sediment characteristics associated with low chironomid abundance. We suggest that the relative competitive ability of the Cladocera species is reversed when the sediment has become homogeneous and nutrient-poor after overexploitation by the dominant, tube building and detritivorous chironomid Tanytarsus gracilentus.
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