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Atlantic bottlenose dolphins housed in open ocean enclosures in San Diego Bay, California, developed nonpathogenic skin films consisting of a single diatom species belonging to the epizoic, monoraphid genus Epipellis R.W. Holmes. This diatom differs from the single known representative of this genus, E. oiketis R.W. Holmes, by its denser striae and marginal alveoli on both the raphe and araphid valves, a greater number of areolae rows on the marginal rim of the raphe valve, and the presence of an embossment of the external valve surface distal to the terminal raphe ends. Consequently, it is described here as a new species, E. heptunei Denys et Van Bonn. The new species occurs in more southern and warmer waters than E. oiketis and also appears to be the first endemic diatom reported from Atlantic bottlenose dolphins.

Herbarium material of aquatic macrophytes and old limnological samples provide the opportunity to obtain precisely dated samples of epiphytic, planktonic or sedimentary diatom assemblages from the more recent past. These allow an accurate assessment of former limnological conditions at specific sites, in particular types of surface waters or associated to certain macrophytes, and even in entire regions. Inferences made from diatom assemblage composition may range from species abundance and diversity estimates to a reliable reconstruction of important parameters (e.g. pH, nutrient concentrations, salinity) by the use of indicator values or calibration techniques. Such information can be used to determine appropriate goals for management and restoration (pre-deterioration conditions), to track temporal changes by comparison with more recent data and relate these to possible external influences (e.g. various forms of pollution), or to evaluate monitoring data in a broader time perspective. In many cases, the use of old samples may not allow to generate time series of similar length and resolution as the more commonly applied diatom analysis of sediment cores. This technique, however, does provide access to the history of waters that do not have a suitable sediment record (e.g. because of dredging or sediment disturbance), avoids the problems often encountered in dating core levels accurately, and - with comparable or less effort -can be applied to a score of waters from a certain area. Also, it may be used to corroborate conclusions derived from sediment core analyses. Furthermore, the shorter time averaging of environmental conditions by epiphyton or plankton compared to sediment assemblages can be used advantageously to study short-lived or abruptly occurring phenomena. Limitations are, of course, related to the availability of suitable samples, the fact that most samples post-date c. 1850, and the reliability or detail of the information on place and date of collection. Moreover, variability caused by substrate and small-scale spatial differences in ecological conditions may be difficult to account for. For these reasons, it is recommendable to examine multiple samples of different nature (epiphyton of different plant species, sediment from between the roots, ...) from a given site. So far, old samples and herbarium material of aquatic plants have been used for a number of diatom investigations on lentic waters in Flanders. These include a number of case studies on specific water bodies, e.g. the Blankaart reservoir (Woumen), pools in the "Fonteintjes" (Zeebrugge), a survey of pools in the region of Kalmthout prior to 1945, and a 'typological' study of standing waters throughout the entire Flemish region. In order to facilitate the selection of suitable material for such studies, an inventory was made of some of the most important herbarium and sample collections held by Belgian universities and research institutes (including the herbaria BR, GENT, LV, BRVU, ANTW and that of UCL, and the collections of Van Oye at RUG and RUCA, and of Adam & Goossens at KBIN).

The transition from the clastic Calais deposits to the main body of the Holland peat in the western Belgian coastal plain was investigated by means of diatom analyses of seven cores, from close to the present coastline up to the polder border. At all sites the peat was found to rest upon mudflat and saltmarsh deposits and not upon lagoonal sediments, as often supposed. Peat formation in the backswamps was apparently induced by the waterlogging of silted-up areas due to a considerable supply of fresh water, mainly of inland origin.

In the frame of a general introduction to diatom analysis, especially of Quaternary coastal deposits, the possibilities, problems and methods of this discipline are briefly discussed.