Biomedical subjects
Publications and source records attributed to Uwe John.
One hundred diatom species have been selected for genome and transcriptome sequencing. The 100 Diatom Genomes Project aims to provide a scalable framework for understanding diatom biodiversity, ecology and evolution, and for investigating their use in biotechnology.
The application of molecular techniques has revolutionized freshwater and marine ecology, especially for plankton research. Methods, such as denatured gradient gel electrophoresis (DGGE), temperature gradient gel electrophoresis (TGGE), and single-strand conformation polymorphism (SSCP), together with environmental clone libraries, have unraveled an unexpected biodiversity of organisms in the water column. Molecular probes are just entering the field of commercialization for monitoring toxic algal blooms. Genomics and metagenomics were recently introduced into marine biology. At the basis of all molecular approaches is the isolation of nucleic acids from cultures, tissue, or environmental samples. Here, we summarize methods, quality controls, and hints for sample treatment to reliably isolate nucleic acids, both DNA and RNA, from environmental aqueous samples. This chapter not only is directed to researchers inexperienced with such methods but also is an aid to those already working in the field. It may be used as a step-by-step guide for nucleic acid isolation from field samples, and we make suggestions for subsequent use of the DNA/RNA.
Phylogenetic analyses of the Alexandrium tamarense species complex using ribosomal RNA sequences show a differentiation of ribotypes/clades into geographic areas and not into the three morphotypes/species A. tamarense, A. fundyense and A. catenella. Different parts of the rRNA operon have proven informative in revealing the existence and the relationships of these geographic clades, whereas even internal transcribed spacer (ITS) regions lack the resolution required to gain a deeper insight into the population structure of the species complex. Here, the utility of the DNA fingerprinting technique Amplified Fragment Length Polymorphism (AFLP) as a possible tool for such purposes was tested. A mixed sampling strategy was used in order to assess the amount of variation of AFLP banding patterns at the level of populations and geographic clades. We also describe optimized methods to achieve a good reproducibility. Our results suggest that AFLPs can provide useful information at the population level using clonal samples from a certain bloom, whereas the amount of variation that we found is too high to allow for meaningful comparisons of a few strains collected from different localities at different time points even though they belong to one geographic clade.
The cosmopolitan dinoflagellate genus Alexandrium, and especially the A. tamarense species complex, contain both toxic and nontoxic strains. An understanding of their evolution and paleogeography is a necessary precursor to unraveling the development and spread of toxic forms. The inclusion of more strains into the existing phylogenetic trees of the Alexandrium tamarense species complex from large subunit rDNA sequences has confirmed that geographic distribution is consistent with the molecular clades but not with the three morphologically defined species that constitute the complex. In addition, a new clade has been discovered, representing Mediterranean nontoxic strains. The dinoflagellates fossil record was used to calibrate a molecular clock: key dates used in this calibration are the origins of the Peridiniales (estimated at 190 MYA), Gonyaulacaceae (180 MYA), and Ceratiaceae (145 MYA). Based on the data set analyzed, the origin of the genus Alexandrium was estimated to be around late Cretaceous (77 MYA), with its earliest possible origination in the mid Cretaceous (119 MYA). The A. tamarense species complex potentially diverged around the early Neogene (23 MYA), with a possible first appearance in the late Paleogene (45 MYA). A paleobiogeographic scenario for Alexandrium is based on (1) the calculated possible ages of origination for the genus and its constituent groups; (2) paleogeographic events determined by plate movements, changing ocean configurations and currents, as well as climatic fluctuations; and (3) the present geographic distribution of the various clades of the Alexandrium tamarense species complex.