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With the continuing consumption of resources and increasingly prominent environmental issues, microalgal resource utilization has received extensive attention. In this study, based on the microalgal investigation in desert biological soil crusts (BSCs) using pyrosequencing technology, the cultivated crust microalgae were further isolated in order to obtain high quality microalgae for resource utilization. The results showed that with crust development and succession, microalgal diversity gradually decreased, including the number of operational taxonomic units (OTUs) and genus, although Microcoleus always was the dominant genera. Pyrosequencing obtained 630 OTUs of cyanobacteria, 25 OTUs of green algae and 9 OTUs of diatom; however, part of cultivated microalgae still could not yet be detected due to the DNA extraction preferences and errors caused by PCR amplification. After isolation, four strains were purified and cultivated, including two filamentous cyanobacteria Microcoleus vaginatus BSC-06 and Scytonema javanicum BSC-39, and two unicellular green algae Chlorella sp. BSC-24 and Monoraphidium dybowskii BSC-81. The two green algae grew fast (>250 mg L -1  d -1 ), and achieved high lipid productivity up to 75–85 mg L -1  d -1 , with lipid content of 28.7–39.0%, thus was considered as promising feedstock for biodiesel production. In addition, the two crust cyanobacteria could be used to construct artificial cyanobacterial soil crusts in desertification control, although their biomass accumulation was not as high as that in the green algae. Ultimately, combining biodiesel production with desertification control would not only improve desert environments, but also provide ideal places for the local microalgal resource exploitation, further promoting desert socioeconomic development. [ABSTRACT FROM AUTHOR]

The carbon cycle (C-cycle) is the most important and complex biogeochemical cycle in soil ecosystems, but our understanding of C-cycle at the community level remains limited. Biocrusts are known ecosystem engineers and represent ideal model systems for biogeochemical cycling studies. Here, metagenomic sequencing based on five repeated collections of four types of biocrusts revealed a low abundance of genes related to light-driven inorganic carbon fixation, and high abundance of genes related to the chemical energy-driven degradation of macromolecular organic carbon (OC), fermentation, aerobic respiration, and CO oxidation. For OC decomposition, genes mediating starch/glycogen and cellulose degradation were most abundant during the initial complex OC degradation, as were genes mediating fermentation during terminal steps of OC decomposition. To assess successional changes in carbon cycle, the metagenomic data were combined with absolute quantification via GeoChip, as well as key enzyme activity measurements. Inorganic carbon fixation, fermentation, CH 4 oxidation, and both starch/glycogen and peptidoglycan degradation decreased during succession. However, several high efficiency processes, as well as CO oxidation and most types of OC degradation, increased. Co-occurrence networks revealed that C-cycle in biocrusts consists of an assimilation module, akin to primary production, and a dissimilation module, comparable to secondary production; dynamic changes in the relationships between C-cycle pathways and microbial community composition occurred during succession. The two C-cycle modules were connected by the Calvin-Benson-Bassham cycle, as well as ethanol and propionate fermentation; the modules were balanced by drought and salinity. Collectively, these results improve our understanding of C-cycle pathways and regulatory mechanisms in biocrust succession, and provide a basis for future multi-omics studies of these systems. • Inorganic carbon fixation was low, with trace gases as energy supplement. • The carbon cycle in biocrusts showed significant dynamics during succession. • Two essential modules in the carbon cycle were found with co-occurrence network. • Carbon assimilation and dissimilation were balanced by drought and salinity. [ABSTRACT FROM AUTHOR]