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 led by Prof. LIU Yu from the Institute of Earth Environment and their collaborators reconstructed natural runoff history for the middle reach of the YR from 1492 to 2013 CE to assess the effects of human activities.
The evidence for a new geological epoch which marks the impact of human activity on the Earth is now overwhelming according to a recent paper by an international group of geoscientists. The Anthropocene, which is argued to start in the mid-20th Century, is marked by the s...
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