Melissa R. McQuoid

Viability of phytoplankton resting stages in the sediments of a coastal Swedish fjord

Viable diatom and dinoflagellate resting stages were recovered from sediments in Koljö Fjord on the west coast of Sweden. To determine the maximum survival time of buried resting stages, samples from sediment depths down to 50 cm were incubated at temperatures of 3, 10 and 18 °C. Sediment cores were dated by 210Pb and the age of samples containing viable resting stages was determined using the constant rate of supply model. Dilution cultures of surface sediments allowed semiquantitative estimates of the potential seed bank. Dinoflagellate cysts from species such as Diplopsalis sp., Gymnodinium nolleri, Oblea rotunda and Protoceratium reticulatum were viable down to 15 cm depth, or 37 years old. Spores and resting cells of the diatoms Chaetoceros spp., Detonula confervacea and Skeletonema costatum were viable to over 40 cm depth, and may have been buried for many decades. The seed bank of living resting stages in surficial sediments was found to be rich (c. 57000 diatom resting stages g−1 wet weight and c. 200 dinoflagellate cysts g−1 wet weight), and the percentage of viable resting stages was higher for spore- and cyst-forming species. The oxygen-deficient sediments in Koljö Fjord appear to be a natural conservator of cell viability, a condition not easily simulated in laboratory studies. These results are ecologically important since spores and cysts are a repository of genetic material able to repopulate waters if resuspended and exposed to suitable light, temperature and nutrients.

COMPARISON OF THREE COMMON MOLECULAR TOOLS FOR DISTINGUISHING AMONG GEOGRAPHICALLY SEPARATED CLONES OF THE DIATOM SKELETONEMA MARINOI SARNO ET ZINGONE (BACILLARIOPHYCEAE)1

Skeletonema marinoi Sarno et Zingone is a planktonic marine diatom with a widespread geographic distribution. Different populations of this species may show distinct genetic signatures. We have evaluated the utility of three common molecular methods for distinguishing clones of S. marinoi from different geographic regions. Clonal cultures were isolated from the Canadian west coast, south west Portugal, and the east and west coasts of Sweden. All strains originated from resting stages in sediment. More than 90% of the individually isolated chains grew to densities suitable for DNA extraction. Genetic signatures of clones from each sample location were assessed by sequencing variable domains (D1–D3) of the nuclear large subunit (LSU) rRNA gene and internal transcriber spacer (ITS) (ITS‐1, 5.8S and ITS‐2) regions, and also by analysis of randomly amplified polymorphic DNA patterns. Analysis of molecular variance showed that strains from the four geographic areas were significantly separated by all three methods but that differences among European samples were best resolved by ITS 2 sequences.

PELAGIC AND BENTHIC ENVIRONMENTAL CONTROLS ON THE SPATIAL DISTRIBUTION OF A VIABLE DIATOM PROPAGULE BANK ON THE SWEDISH WEST COAST1

The distribution of viable diatom resting stages in sediments on the Swedish west coast was assessed by the most probable number (MPN) culture technique. Multivariate analyses correlated benthic and pelagic environmental factors to the observed spatial variations in the size and taxonomic composition of the propagule bank. Viable diatom resting stages were plentiful (0.2–4.8 million cells·g− 1 dry weight) and were dominated by the genera Skeletonema, Detonula, Chaetoceros, and Thalassiosira. Size of the propagule bank was primarily related to planktonic biomass (measured as chl a) and was highest in the Orust‐Tjörn fjord system. Species composition in this fjord system was dominated by D. confervacea (Cleve) Gran and T. nordenskioeldii Cleve in contrast to stations on the outer coast, which contained more cells of T. minima Gaarder, Asterionellopsis glacialis (Castracane) Round, and Leptocylindrus danicus Cleve. These taxonomic variations were principally influenced by deep water oxygen concentrations and water column stability. Benthic resting cells of S. costatum (Greville) Cleve were abundant all along the coast but showed reduced viability in low oxygen environments. Calculations based on MPN values estimated that resuspension of sediment could provide a sizable inoculum to the plankton, although the development of planktonic blooms will also depend on forces of hydrography and weather. Although benthic resting stages may not be absolutely necessary for survival of all diatoms, these cells may be important in determining species cycles, succession, and the spatial distribution of diatoms.

The species concept in a marine diatom: LSU rDNA-based phylogenetic differentiation in Skeletonema marinoi /dohrnii (Bacillariophyceae) is not reflected in morphology

M. Ellegaard, A. Godhe, K. Härnström and M. McQuoid. 2008. The species concept in a marine diatom: LSU rDNA–based phylogenetic differentiation in Skeletonema marinoi/dohrnii (Bacillariophyceae) is not reflected in morphology. Phycologia 47: 156–167. DOI: 10.2216/07-09.1 The ubiquitous marine diatom genus Skeletonema includes several newly described species. This paper presents a study of morphology and LSU sequence diversity of one of these new species, Skeletonema marinoi. The 15 monoclonal strains (from the Swedish west coast, the Swedish east coast, Portugal and Canada) included in the study showed differences in LSU rDNA sequence within the morphospecies, with differences seen even among clones established from a single plankton net sample. Morphologically, all clones were indistinguishable from each other and from the closely related species Skeletonema dohrnii. In the original description of these two species, they were differentiated by the structure of the girdle bands. However, the girdle band types of both species were found within single samples of almost all clones of S. marinoi in this study. The LSU-based phylogeny is consistent with the split into two species, and there may be a difference in their biogeographical distribution. We therefore do not at present suggest that the two species be merged. Questions regarding species delimitation and cryptic species within protists often arise from such studies that include data from both morphological and DNA sequence analysis, and such questions are addressed here.

Environmental influence on the diatom and silicoflagellate assemblages in Koljö Fjord (Sweden) over the last two centuries

Throughout the last century, the Swedish coasts, have been exposed to climatic variation and human influence, and this has altered the biota in some areas. Diatoms and silicoflagellates in a periodically-laminated sediment core from Koljö Fjord (Swedish west coast) were examined to assess recent changes in the microalgal community. The most notable changes in the plankton occurred at the beginning of a long period of water column stratification in the fjord that extended from 1930 to 1980. The planktonic flora changed from a community dominated byBacterosira bathyomphala andThalassionema nitzschioides during the 1800s to a community dominated byDetonula confervacea, T. nitzschioides, andThalassiosira spp. after 1930. Silicoflagellates, were more abundant after 1940. Planktonic variations corresponded to oscillations in climate, hydrography, and weather, which determine water column stability in the fjord. The tychopelagic species,Paralia sulcata, was more abundant in unlaminated sections of the core, indicating preference for a vertically mixed water column. No direct effects of increased nutrient loading on the plankton could be established. Epiphytic diatoms show a period of decline from the 1950s to 1990s. This trend probably follows a shift in the macroalgal community to less-suitable host species. To what extent this pattern has been influenced or reinforced by humans cannot be determined at the present time. The results from Koljö Fjord, in particular the exploration of meteorological and physical oceanographic influences on algal dynamics, emphasize the importance of distinguishing between natural and humaninduced changes in the environment.