Arid sandy areas have great potential for producing solar power, so many solar photovoltaic (PV) systems have been constructed in desert regions. Hexi corridor, a typical and broadly representative desert ecosystem in northwestern China, is well-known for its abundant sunshine and great numbers of solar PV systems. However, spatial heterogeneity in vegetation and soil properties across different PV panel locations in Hexi Corridor remain unclear to date. To address this gap, we evaluated the spatial heterogeneity of the vegetation community, and soil properties in and near a PV station in a desert region of the Hexi corridor. Measurements were conducted at six locations under and around the panels, and at distances of 200 to 600 m from the panels. Results show that the aboveground biomass (AGB) and three plant diversity indices differed from locations inside and outside the PV station. Soil water contents to a depth of 30 cm were greatest under the panels. Soil organic carbon (SOC) inside the PV station was higher than outside the PV station, and was increased with increasing distance from the panels. On the contrary, total nitrogen (TN) contents inside the PV station was lower than those outside the PV station. The differences in plant diversity indices, SOC, and TN between inside and outside were generally not significant. Our results indicate that solar PV construction on sandy land of the Hexi Corridor impact the spatial distribution of vegetation and soil properties, and the positive effects of PV panels on vegetation and soil may outweigh the negative effects.

Given the increasing challenges posed by frequent extreme climatic events, understanding the climate–human connection between the climate system and the transitions of ancient civilizations is crucial for addressing future climatic challenges, especially when examining the relationship between the abrupt events of the Holocene and the Neolithic culture development. Compared with the globally recognized “4.2 ka collapse” of ancient cultures, the initial start time and the cultural significance of the 5.5 ka climatic fluctuation are more complex and ambiguous. The Hongshan culture (6.5–5.0 ka) is characterized by a complicated society evident in its grand public architecture and elaborate high-status tombs. However, the driving mechanisms behind cultural changes remain complex and subject to ongoing debate. This paper delves into the role of climatic change in Hongshan cultural shifts, presenting an integrated dataset that combines climatic proxy records with archaeological data from the Hongshan culture period. Based on synthesized aeolian, fluvial-lacustrine, loess, and stalagmite deposits, the study indicates a relatively cold and dry climatic fluctuation occurred during ~6.0–5.5 ka, which is widespread in the Horqin dune field and adjacent areas. Combining spatial analysis with ArcGis 10.8 on archaeological sites, we propose that the climatic fluctuation between ~6.0–5.5 ka likely triggered the migration of the Hongshan settlements and adjustment of survival strategies.