No description available.

No description available.

No description available.

Aeolian dune interdunes have been relatively ignored when compared with the research attention on the morphodynamics of the dune bodies themselves. This neglect is in spite of the possible significance of interdune dynamics for the geomorphology of the sand dune system as a whole, especially with regard to dune spacing. This project involved the collection of geomorphologically relevant airflow data for four relatively simple transverse dune interdunes. The study locations were chosen in order to sample interdunes with different size and surface type characteristics, the dynamics of which were investigated for when incident flow was normal to the upwind crest. The findings confirm existing models of aeolian dune lee-side flow in terms of flow re-attachment length and recovery attributes. A consistent pattern of increasing near-surface velocity downwind of re-attachment provides a mechanism for interdunes as sand-free features. Where studies for comparison from other aeolian examples are limited, the field-measured turbulence shows the importance of the shear layer as a source of turbulence, and agrees with studies from subaqueous bedforms. The importance of shear stress variability and the possible contribution of turbulence structures to the maintenance of sediment transport at re-attachment where velocity and mean stress is low or negative is also emphasised. At the downwind edge of interdunes, the mean and turbulent velocity properties, and therefore morphodynamics, vary according to the interdune size. In this case, interdune length leads to greater recovery, and a balance exists in this region between the recovering flow at the surface, dissipating wake from above and the obstacle effect of the dune. The flow dynamics are characterised for the different types of interdune observed. Dynamics accordant with the flow response model are seen to characterise the interdune setting with the closest spacing. The occurrence of other “extended” aeolian interdunes with a length well over that for flow separation demanded the development of a new descriptive model to characterise the dynamics therein. In this model, the variation in near-surface flow allowed process zones to be identified through the interdune. The geomorphological significance of the processes dominating each zone are discussed and comparisons are made between the flow response case and the new interdune model from this study

Thesis--Lund. / Bibliography: p. 221-228.

Thesis (Ph. D.)--University of Wisconsin--Madison, 1967. / Typescript. Vita. Description based on print version record. Includes bibliographical references (leaves 173-176).

Proposed thesis is focused on the role of soil microbial crusts in the extreme environmental conditions of high-elevation cold desert of W Himalaya. Despite the importance of microbial soil crusts in arid soils, the biodiversity of their microbial communities, their role and function are still unclear. Our knowledge about functioning of these outlying ecosystems in this part of the world is still very insufficient in general. The area of Ladakh is perfect place for studying the microbial soil crust arid climate and extreme elevation aroud 6000 m a.s.l. represents unique condition for well-developed soil crusts communities. The whole region is unaffected by human activities or plant invasions, so we can study soil crusts in pristine natural condition. Our investigations is focused on soil microbial community of BSCc in Ladakh region. It combines range of aspects connected with BSCs such as taxonomical composition, changes of diversity and activity in relation to environmental condition. The thesis is the first compilation of studies concerned on microbial communities in area of Ladakh and one of the first work investigating the ecophysiology of BCSs in cold desert.

No description available.

Les zones arides couvrent environ un tiers de la surface terrestre de la planète. Des études visant à comprendre la dispersion microbienne dans les déserts ont été réalisées. En effet, les communautés microbiennes du sable des déserts peuvent jouer un rôle important dans la stabilité des sols. Le pyroséquençage pour les ARNr 16S à partir de l’ADN total extrait des sols des échantillons de sable peut donner des renseignements clés sur la structure des communautés bactériennes qui les composent. Dans cette étude, la diversité et la structure des communautés bactériennes de la surface du sol des déserts des l'États de l'Utah et du Maine ont été mises en évidence. Nous avons mise en œuvre une procédure permettant l'analyse des séquences de l’ADNr 16S en combinant des outils préexistants dédiés à la métagénomique. Ainsi, des corrélations entre certains facteurs environnementaux et la diversité bactérienne dans les deux déserts, ont pu être établis.Le désert du Maine situé dans le nord-est Etats-Unis est une étendue de boue glaciaire, entourée par une forêt de pins. Le sol de ce désert possède les caractéristiques d’on sable avec de très faibles capacités de rétention d'eau, d’une rétention des éléments nutritifs, ainsi qu’une valeur de pH relativement faible (pH 5,09). Les échantillons provenant de ce site présentent donc des propriétés particulièrement intéressantes à étudier en lieu avec la diversité bactérienne. Deux échantillons de sable de la surface du désert du Maine ont été obtenus, et le pyroséquençage des gènes d'ADNr 16S obtenus après amplification par PCR à partir de l'ADN total extrait a été utilisé pour évaluer la diversité bactérienne, la structure de la communauté bactérienne et l'abondance relative des principaux taxons. Nous avons observé que les échantillons de sol provenant du désert du Maine présentent une diversité bactérienne singulière, avec une prédominance de Proteobacteria et Actinobacteria. Les bactéries du genre le plus abondant, Acidiphilium, représentent 12,5% du total des séquences d'ADNr 16S. Au total, 1 394 OTU ont été comptabilisées. En comparant les résultats de notre population bactérienne avec des études portant sur des sols avec caractéristiques similaires, nous avons constaté que les échantillons du Maine contiennent une faible diversité du phylum Acidobacteria que les sols acides des certains forêts, et moins de Firmicutes ainsi que plus de Proteobacteria que les sols des déserts oligotrophes.Le Désert de l'Utah présente des caractéristiques géographiques qui ressemblent à Mars. En effet il est caractérisé par la présence de collines de couleur rouge et de sols constitués de grès. Les sites d'échantillonnage couvrent le Gobblin Valley State Park et autour, notamment sur le plateau du Colorado. Avec des approches similaires à ceux utilisés pour le désert du Maine, des corrélations entre facteurs environnementaux (paramètres physico-chimiques) et diversité de structure des communautés bactériennes obtenus, ont été étudiés. Les phylums prédominants sont les Proteobacteria, Actinobacteria, Bacteroidetes et Gemmatimonadetes. Les genres les plus abondants dans nos échantillons sont Cesiribacter, Lysobacter, Adhaeribacter, Microvirga et Pontibacter. Mais de façon notable, il semble que l'abondance relative des Alphaproteobacteria et des Gemmatimonadetes est significativement corrélée aux certains facteurs environnementaux des sols, par exemple de pH et des concentration des matières organiques. / Aridity is the dominant climatic factor over approximately 30% of the land surface of the world. Research concerning microbial populations in two U.S. deserts has been performed to determine the diversity of these bacteria. Pyrosequencing-based profiling of 16S rRNA amplicons from surface soils of sand samples can provide key insights into the structure of bacterial communities and their diversity. In this study, we demonstrated the bacterial diversity and community structures of surface soil in the Corolado Plateau in the Utah State and the Desert of Maine using pyrosequencing of 16S rRNA amplicons. We built our pipeline for the analysis of 16S rRNA pyrosequencing data by combining several existing tools of metagenomics. We also examined correlations between certain environmental factors and bacterial diversity in the two deserts.The Desert of Maine is a tract of glacial silt, surrounded by a pine forest, in the state of Maine located in the northeastern USA. The soil of the Desert of Maine has a sandy texture with poor water holding abilities, nutrient retention capabilities and a relatively low pH value (pH 5.09). Samples from this site thus present an interesting place to examine the bacterial diversity in mineral sandy loam soils with an acidic pH and low concentrations of organic materials. Two surface sand samples from the Desert of Maine were obtained, and pyrosequencing of PCR amplified 16S rDNA genes from total extracted DNA was used to assess bacterial diversity, community structure and the relative abundance of major bacterial taxa. We found that the soil samples from the Desert of Maine showed high levels of bacterial diversity, with a predominance of members belonging to the Proteobacteria and Actinobacteria phyla. Bacteria from the most abundant genus, Acidiphilium, represent 12.5% of the total 16S rDNA sequences. In total, 1394 OTUs were observed in the two samples, with the number of common OTUs observed in both samples being 668. By comparing our bacterial population results with studies on related soil environments, we found that the samples contained less Acidobacteria than soils from acid soil forests, and less Firmicutes plus more Proteobacteria than soils from oligotrophic deserts.Deserts in Utah has geographic features that resemble Mars, characterized by red-colored hills, soils and sandstones. Our sample sites cover the Goblin Valley State Park and nearby regions on the Colorado Plateau. We also examined physicochemical parameters of soil from the sample sites to investigate correlations between bacterial community structure and environmental drivers. The predominant phyla of the samples represent members of the Proteobacteria, Actinobacteria, Bacteroidetes, and Gemmatimonadetes. The most abundant genera in our samples are Cesiribacter, Lysobacter, Adhaeribacter, Microvirga and Pontibacter. We found that the relative abundance of Alphaproteobacteria and Gemmatimonadetes are significantly correlated to some environmental factors of soils, such as pH and concentration of organic matters.

Despite high taxonomic diversity elsewhere in North America during the Pleistocene, vertebrate faunas are exceedingly rare in the region of northern Mexico. Térapa, a unique fossil site located in the present-day desert of Northcentral Sonora, Mexico (29°41́N, 109°39́W, 605. m elevation), contributes to our understanding of the paleoecology and paleoclimate of the region during the Late Pleistocene, ca. 43,000-40,000. cal.yr BP. At least 60 vertebrate taxa, including amphibians, turtles, a crocodilian, snakes, birds and many mammals, have been recovered from an 11-m thick sequence of fossiliferous sediments. The diversity and tropical affinity of these taxa suggest a more-forested environment than the thornscrub desert habitat present in this region today.Isotopic analyses of tooth enamel carbonate from ancient mammalian herbivores suggest that the Sonoran desert has undergone considerable climate change since the Late Pleistocene. Bulk carbon (́13C) and oxygen (́18O) isotopes from nine mammalian fossils indicate a habitat mosaic with variations in diet that include browsers, mixed feeders and C4 hyper-grazers (́13C range of -10‰ to 2‰). Unique to this site are 13C tooth enamel values of -6.1 and -5.6 ‰ for the deer Odocoileus, which suggest a more variable diet than strict browsing, including possibly feeding on CAM and/or C4 plants. Serial sampling of carbon (δ13C) and oxygen (δ18O) isotopes for ancient mammal teeth with hypsodont dentitions (fossil Equus and Bison,) as well as δ18O meteroric water estimates from well-supported climatic models suggest a cooler and more equable environment at Térapa during the Late Pleistocene. These results also support previous habitat reconstructions inferred from the macrobotanical and packrat midden records of northern Sonora (Mexico). High-resolution stable isotope geochemistry indicates that: 1) ancient Térapa was covered with forest and grassland habitats that extended northward into Mexico by about 350km relative to their present-day northern limits during the Late Pleistocene; and 2) an Amount Effect (AE) is demonstrated in the fossil record at Térapa even though the climate was less seasonal compared to the modern desert habitat.