“…Since 1950, the Qinghai-Tibet Plateau has experienced significantly warming, which has led to the accelerated degradation of permafrost, reduced solid water reserves, and increased precipitation (Zhao et al, 2020;Zhang Q. et al, 2022), which makes the stability of the marsh wetland ecosystem in the YRSR worse; simultaneously, human activities, such as overgrazing, expansion of construction land, and peat mining have intensified (Liu et al, 2019;Pan et al, 2020); the marsh wetland in the YRSR have been degraded to varying degrees, with serious landscape fragmentation and decreased species diversity, posing a serious threat to the aquatic ecological function, frozen soil, and ecological environment in this area (Xiang et al, 2009;Li et al, 2018). With the strengthening of ecological environment protection and the regulation of relevant policies, the Chinese government has implemented a series of ecological protection and restoration projects since 2000, including turning grazing land back to green and establishing the Sanjiangyuan National Ecological Protection Area, especially the construction of the Yellow River Source National Park, which has improved the ecological environment in the YRSR (Du et al, 2015;Shao et al, 2017;Ma et al, 2022). However, the exact mechanism of the change in marsh wetland in the YRSR is still unknown because of the mutual interference and interaction between climate change and human activities.…”