Evaluating the adaptive capacity of the giant panda in response to climate change since the last glacial maximum

被引:0
|
作者
Xu, Yadong [1 ,2 ]
He, Wen [1 ,2 ]
Yang, Xintian [1 ,3 ]
Li, Yunqiu [1 ,3 ]
Yu, Xiaoping [1 ,2 ,4 ]
Ye, Xinping [1 ,3 ,4 ]
机构
[1] Shaanxi Normal Univ, Coll Life Sci, Xian 710119, Peoples R China
[2] Shaanxi Normal Univ, Res Ctr UAV Remote Sensing, Xian 710062, Peoples R China
[3] Shaanxi Normal Univ, Changqing Field Stn Ecol Res & Educ, Xian 710119, Peoples R China
[4] Shaanxi Prov Field Observat & Res Stn Golden Monke, Giant Panda & Biodivers, Xian 710032, Peoples R China
基金
中国国家自然科学基金;
关键词
Ailuropoda melanoleuca; Bioclimatic velocity; Climate change; Climatic velocity; Ensemble species distribution model; SPECIES DISTRIBUTION MODELS; DISTRIBUTION SHIFTS; QINLING MOUNTAINS; VELOCITY; VULNERABILITY; ENVIRONMENTS; CONSERVATION; ACCURACY; IMPACTS; ABILITY;
D O I
10.1016/j.ecolind.2024.112781
中图分类号
X176 [生物多样性保护];
学科分类号
090705 ;
摘要
Evaluating the adaptive capacity of species to past climate change is a crucial component in understanding how species respond to climatic shifts. This information serves as a vital foundation for guiding conservation practices under future environmental changes. We reconstructed the potential suitable habitat maps for giant pandas (Ailuropoda melanoleuca) during the Last Glacial Maximum (LGM, similar to 22 ka) and mid-Holocene (MH, similar to 6 ka) climates via an ensemble species distribution modelling approach, and compared them to the potential suitable habitats at current stage, we also estimated and compared the bioclimatic velocity of giant pandas to the climatic velocities since LGM. The results showed that the suitable habitat area for giant pandas has increased by 12.47 % from LGM to MH, and then decreased by 5.37 % from MH to current stage. The estimated climatic velocity over the suitable habitats for giant pandas was 16.00 +/- 5.83 km center dot kyr(-1) from LGM to MH and 46.13 +/- 18.96 km center dot kyr(-1) from MH to nowadays. The bioclimatic velocities for these two periods were 0.55 +/- 0.55 km center dot kyr(-1) and 8.47 +/- 10.45 km center dot kyr(-1), respectively. The result indicated that giant pandas have successfully adapted to the climate changes since LGM by migrating at a rate that lags behind the speed of climate change within their current distribution range. However, this does not imply that giant pandas possess sufficient migratory capabilities to cope with future climate crises, as the current rate of climate change exceeds that of any historical periods.
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页数:9
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