Multilocus sequence analysis of homologous recombination and diversity in Arthrobacter sensu lato named species and glacier-inhabiting strains

Members of the bacterial genus Arthrobacter sensu lato are Gram-positive actinomycetes distributed worldwide and found in numerous environments including soil, water, glacier ice, and sewage. Homologous recombination is an important driving force in bacterial evolution, but its impact on Arthrobacter sensu lato evolution is poorly understood. We evaluated homologous recombination among 41 Arthrobacter sensu lato named species, using multilocus sequence analysis (MLSA). A high level of recombination was found, associated with strong diversification and a reticulate evolutionary pattern of Arthrobacter sensu lato. We also collected a total of 31 cold-adapted Arthrobacter sensu lato strains from two cold glaciers located in northwest China and two temperate glaciers in southwest China, and evaluated their diversity and population structure by MLSA. The glacier strains displayed high diversity, but rates of recombination among the four glacier groups were quite low, indicating that barriers to homologous recombination formed in the past among the populations on different glaciers. Our findings indicate that historical glaciation events shaped the contemporary distributions, taxonomic relationships, and phylogeographic patterns of Arthrobacter sensu lato species on glaciers.     

Late-glacial and Holocene vegetation and climate change at the Palü glacier, Bernina Pass, Grisons Canton, Switzerland

Pollen and macrofossil data from Alpe PAlü, south-eastern Switzerland, are presented. On the basis of these data and the geomorphological evidence for local glacier movement, Holocene climatic oscillations and vegetation change at this upland site (1940 m asl), are reconstructed. The morainic deposits and glacial clays, as well as the pollen data from the base of the pollen profile, clearly show that the Palü glacier, after its retreat from the Cavaglia (Egesen) stade, readvanced once again shortly before the mid-Preboreal. This re-advance was considerably greater than that dating to the Little Ice Age. This early Holocene climatic event is referred to as the Palü Oscillation (Palü-Schwankung) and is considered to be broadly contemporaneous with the previously described Schlaten Oscillation (Schlate n-Schwankung) in the Austrian Alps. The reforestation of the forefield of the moraine was interrupted at least twice during this oscillation, and, compared with neighbouring sites at the same altitude, it appears to be at least 500–700 years younger, i. e. it post-dates 9400 B.P. Though the Palü Oscillation is a Holocene phenomenon, the associated vegetation changes are Late-glacial in character, e.g.Arlemisia and Chenopodiaceae increase andHippophaë is recorded.Alnus viridis replacesBelula andSalix, which were important in the earlier part of the Holocene, at about 5000 B.P. There is no clear evidence that forest burning is attributable to human activity. The use ofLarix-dominated areas as pasture (Lärchwiesen) begins in the mid-Bronze Age. A strong decline inPicea (spruce) andLarix (larch), and an increase in Poaceae,Plantago and other herbs in the uppermost horizons reflect more intensive pastoral farming that began in the high Middle Ages.     

Plant succession and soil development on the foreland of the Morteratsch glacier (Pontresina,Switzerland): Straight forward or chaotic?

As study area we selected the glacier foreland of Morteratsch (approx. 1900–2100 m a.s.l.) near Pontresina northwest of the Bernina pass, Upper Engadine, Grisons (Switzerland). The aim of this study is a multimethodological approach using floristic inventories, vegetation and soil mapping of the pro-glacial area in order to detect crucial parameters controlling plant resettlement in recently deglaciated areas as related to time, local microtopography and soil development.     

Wind dispersal of alpine plant species: A comparison with lowland species

Question: The prominent role of wind dispersal in alpine habitats has been recognized early but has rarely been quantified. The aim of this study is to compare wind dispersal under alpine and lowland conditions and to analyse whether differences are caused by species traits, e.g. terminal velocity of seeds (V_term) or weather conditions. Location and Methods: We characterized wind dispersal potential of > 1100 Central European species using measured V_term To quantify the habitat effect on wind dispersal, we measured meteorological key‐parameters and simulated dispersal distance spectra of nine selected species under typical alpine conditions (foreland of the Scaletta‐glacier, Switzerland) and typical lowland conditions (grassland in Bad Lippspringe, Germany). Results: Lowland species had higher V_term compared to alpine species. However, this difference is absent when only species of species of open habitats are concerned. The meteorological measurements showed that the alpine habitat was mainly characterized by higher frequency and strength of updrafts. The simulations showed that under alpine conditions long distance dispersal occurred much more frequent. Conclusions: More than 50 % of the alpine species have a fair chance to be dispersed by wind over long distances, while this proportion is less than 25 % for species from open habitats in the lowland. The more prominent role of wind dispersal in alpine habitats is mainly a result of differences in environmental conditions, namely more intense vertical turbulence in the alpine habitat, and does not result from prominent differences in plant traits, namely V_term, between alpine and lowland species.