The results show a total area of 1,011,870 km2, or about 10.54% of China's total land area. This zone has shrunk by 3.10% over the past three decades, with a notable shift in its centroid of 228.76 km to the southwest.
The researchers observed a complex interplay between human activity and climate change in driving these changes. Forest areas within the ecotone have steadily increased, while grasslands and farmlands have decreased. However, some previous agriculture land has reverted to grassland, mitigating some of the overall loss.
Landscape fragmentation, a key indicator of habitat disturbance, showed a mixed pattern. While some areas showed a decrease in fragmentation, suggesting potential habitat improvement, others showed an increase. This fragmentation appears to be driven by human activities such as reforestation projects and farmland reclamation in the northern and central regions. Climate change, particularly variations in temperature and precipitation, appears to be the dominant factor in the southern areas of the ecotone.
"These data provide important support for the study of the ecotone and for decision-making on biodiversity conservation and ecological restoration projects," said Dr. WANG Zhenwen, lead author of the study.
Researchers from the Institute of Oceanology and their collaborators presented a continuous and high-resolution black carbon record of fire history of the Yangtze River Basin covering the last ~7 ka.
Researchers from the Institute of Atmospheric Physics and their collaborators found that human activities reduced the likelihood of extreme early-spring cold events over southeast Tibetan Plateau.
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