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The Sahara Desert is characterized by extreme environmental conditions, which are a unique challenge for life. Cyanobacteria are key players in the colonization of bare soils and form assemblages with other microorganisms in the top millimetres, establishing biological soil crusts (biocrusts) that cover most soil surfaces in deserts, which have important roles in the functioning of drylands. However, knowledge of biocrusts from these extreme environments is limited. Therefore, to study cyanobacterial community composition in biocrusts from the Sahara Desert, we utilized a combination of methodologies in which taxonomic assignation, for next-generation sequencing of soil samples, was based on phylogenetic analysis (16S rRNA gene) in parallel with morphological identification of cyanobacteria in natural samples and isolates from certain locations. Two close locations that differed in microenvironmental conditions were analysed. One was a dry salt lake (a "chott"), and the other was an extension of sandy, slightly saline soil. Differences in cyanobacterial composition between the sites were found, with a clear dominance of spp. in the less saline site, while the chott presented a high abundance of heterocystous cyanobacteria as well as the filamentous non-heterocystous sp. and the unicellular cf. . The cyanobacteria found in our study area, such as and sp., are also widely distributed in other geographic locations around the world, where the conditions are less severe. Our results, therefore, indicated that some cyanobacteria can cope with polyextreme conditions, as confirmed by bioassays, and can be considered extremotolerant, being able to live in a wide range of conditions.
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http://dx.doi.org/10.3390/microorganisms9030487 | DOI Listing |
Rock doves () are the wild ancestor of domestic and feral pigeons and had a wide distribution across Eurasia and the northern part of Africa. West African rock doves have been identified as genetically distinct from all other populations, possibly representing a distinct species. This divergence is hypothesized to have arisen through cycles of allopatry during the dry and wet Sahara periods.
View Article and Find Full Text PDFBMC Plant Biol
August 2025
Crop Science Department, Faculty of Agriculture, Damanhour University, Damanhour, 22516, Egypt.
Background: One of the most widely consumed legumes worldwide is the common bean. Abiotic stress factors such as heat stress significantly reduce crop productivity, and climate change models predict rising temperatures in many agricultural regions. In the 2021 and 2022 seasons, two field trials were conducted in the Wadi El Natrun Region, El-Behera Governorate, Egypt.
View Article and Find Full Text PDFJ Environ Radioact
August 2025
Departamento de Física Aplicada I, E.T.S.I. Agronómica, University of Seville, Spain. Electronic address:
The Sahara Desert is the main source of global atmospheric mineral dust, with nearby regions, such as Algeria, within those with the highest dust deposition fluxes reported worldwide. This work aims to study environmental radioactivity and depositional fluxes in dust fallout in northern Algeria. Dust deposition samples were collected monthly using an artisan collector in Algiers from May 2014 to June 2018, and for six months in Chréa National Park.
View Article and Find Full Text PDFSci Rep
August 2025
Hydrobiology Lab, National Institute of Oceanography and Fisheries (NIOF), Cairo, Egypt.
Due to their small size and the extreme environmental conditions in hyper-arid regions, wells are highly susceptible to disturbances. Western Desert wells are scarcely studied concerning their ecological status and the environmental factors affecting their aquatic communities. This study aimed to assess groundwater trophic states based on the microbial, phytoplankton and zooplankton composition in three drains and seventeen wells.
View Article and Find Full Text PDFIn the 1970s and 1980s, the semi-arid Sahel, the southern edge of the Sahara Desert, experienced spatially uniform drought, from the Atlantic Ocean to the Red Sea. The recovery that ensued is projected to continue in the center and east, leaving the west out. We show that these two patterns-uniform variation and east-west contrast-are present in instrumental observations and in simulations with constant or time-varying external forcing.
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