As a critical ecological barrier in the arid and semi-arid regions of northwestern China, the spatio-temporal evolution of vegetation carbon sequestration in the Hexi Corridor is of great significance to the ecological security of this region. Based on multi-source remote sensing and meteorological data, this study integrated second-order partial correlation analysis, ridge regression, and other methods to reveal the spatio-temporal evolution patterns of Gross Primary Productivity (GPP) in the Hexi Corridor from 2003 to 2022, as well as the response characteristics of GPP to air temperature, precipitation, and Vapor Pressure Deficit (VPD). From 2003 to 2022, GPP in the Hexi Corridor showed an overall increasing trend, the spatial distribution of GPP showed a pattern of being higher in the east and lower in the west. In the central oasis region, intensive irrigation agriculture supported consistently high GPP values with sustained growth. Elevated air temperatures extended the growing season, further promoting GPP growth. Due to irrigation and sufficient soil moisture, the contributions of precipitation and VPD were relatively low. In contrast, desert and high-altitude permafrost areas, constrained by water and heat limitations, exhibited consistently low GPP values, which further declined due to climate fluctuations. In desert regions, high air temperatures intensified evaporation, suppressing GPP, while precipitation and VPD played more significant roles. This study provides a detailed analysis of the spatio-temporal change patterns of GPP in the Hexi Corridor and its response to climatic factors. In the future, the Hexi Corridor needs to adopt dual approaches of natural restoration and precise regulation, coordinate ecological security, food security, and economic development, and provide a scientific paradigm for carbon neutrality and ecological barrier construction in arid areas of Northwest China.

The Hexi Corridor is an arid region in northwestern China, where hypoliths are widely distributed, resulting from large amounts of translucent stone pavements. In this region, the water and heat distributions are uneven, with a descent gradient from east to west, which can affect the area's biological composition. The impact of environmental heterogeneity on the distribution of hypolithic microbial communities in this area is poorly understood, and this is an ideal location to investigate the factors that may influence the composition and structure of hypolithic microbial communities. An investigation of different sites with differences in precipitation between east and west revealed that the colonization rate decreased from 91.8% to 17.5% in the hypolithic community. Environmental heterogeneity influenced both the structure and function of the hypolithic community, especially total nitrogen (TN) and soil organic carbon (SOC). However, the effect on taxonomic composition was greater than that on ecological function. The dominant bacterial phyla in all sample sites were Cyanobacteria, Actinobacteria, Proteobacteria, and Deinococcus-Thermus, but the abundances varied significantly between the sampling sites. The eastern site had the highest relative abundance of Proteobacteria (18.43%) and Bacteroidetes (6.32%), while the western site had a higher relative abundance in the phyla Cyanobacteria (62%) and Firmicutes (1.45%); the middle site had a higher relative abundance of Chloroflexi (8.02%) and Gemmatimonadetes (1.87%). The dominant phylum in the fungal community is Ascomycota. Pearson correlation analysis showed that the soil's physicochemical properties were also associated with changes in community diversity at the sample sites. These results have important implications for better understanding the community assembly and ecological adaptations of hypolithic microorganisms.

Desert soil around the black stones is highly complex, which substantially affects the diversity and composition of inhabiting microbes. The existence of black stones in the southern part of the Black Gobi desert of China could provide microhabitats for diverse bacterial communities that remain unexplored. Hence, Illumina MiSeq sequencing was used to determine the differences in bacterial communities associated within microhabitats in three sites of the Black Gobi desert, China. Our results show that bacterial communities are significantly affected by each microhabitat. For instance, the a-diversity of bacterial communities indicated more remarkable diversity and richness in these microhabitats. Considering beta-diversity, variances were reported mainly in the Proteobacteria (30%), Actinobacteria (26%), Chloroflexi (19%), and Firmicutes (9%). Firmicutes were markedly enriched in the upper surface, especially in site 1. Compared to other microhabitats, the relative abundance of Proteobacteria was greater in the subsurface, and they were also more dominant in the other two sites. Network analysis of soil factors and bacterial genera showed that the most significant-occurrences were positively correlated, demonstrating potential synergistic interactions. Collective with the predicted function profiles and the redundancy analysis, these results indicated the highest variances in bacterial community structure and function in Black Gobi Desert ecosystems. These differences are likely closely related to the soil parameters, mainly water content, total carbon, and total nitrogen, and might be associated with black stones. This study concludes that microhabitats formed by black stones support highly diverse and biologically active bacterial communities. These microhabitats with extreme environmental conditions deliver new opportunities to explore soil bacterial communities at relevant spatial scales in the Black Gobi desert.