Predicting the dynamic distribution of Sphagnum bogs in China under climate change since the last interglacial period

被引:33
|
作者
Cong, Mingyang [1 ,2 ]
Xu, Yueyue [3 ]
Tang, Luyan [4 ]
Yang, Wenjing [5 ]
Jian, Minfei [2 ]
机构
[1] Jiangxi Normal Univ, Analyt & Testing Ctr, Nanchang, Jiangxi, Peoples R China
[2] Jiangxi Normal Univ, Jiangxi Prov Key Lab Protect & Utilizat Subtrop P, Nanchang, Jiangxi, Peoples R China
[3] Nanchang Univ, Sch Econ & Management, Nanchang, Jiangxi, Peoples R China
[4] Guizhou Normal Univ, Coll Life Sci, Guiyang, Guizhou, Peoples R China
[5] Jiangxi Normal Univ, Key Lab Poyang Lake Wetland & Watershed Res, Minist Educ, Nanchang, Jiangxi, Peoples R China
来源
PLOS ONE | 2020年 / 15卷 / 04期
基金
中国国家自然科学基金;
关键词
POTENTIAL DISTRIBUTION; DOMINATED PEATLANDS; CHANGE IMPACTS; NORTH-AMERICA; PLANT; BRYOPHYTES; RESPONSES; MAXIMUM; FUTURE; GIS;
D O I
10.1371/journal.pone.0230969
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Sphagnum bogs possess irreplaceable ecological and economic value, and they are scarce in China, with a fragmented distribution. Based on 19 high-resolution bioclimatic environmental datasets and 71 bog center point locations, we employed a maximum entropy model (MaxEnt) to reconstruct and predict the spatial-temporal geographical distribution patterns of Sphagnum bogs from the last interglacial (LIG) period to two typical CO2 representative concentration pathway scenarios (RCP2.6, RCP8.5) in the future. We further computed the migratory paths of the distribution center points. Finally, a jackknife test was used to uncover the crucial environmental factors restricting the geographical distribution of the bogs. Our data indicated that the MaxEnt niche model had a high simulation precision with an area under the ROC curve value of 0.957. Spatially, the suitable bog habitats are currently centralized in northeastern China, including the Greater Khingan Mountains, the Lesser Khingan Mountains, and the Changbai Mountains, as well as peripheral areas of the Sichuan Basin. Temporally, the contours of Sphagnum bogs were similar to the present and rendered from the last glacial maximum (LMG) period, and had much more total area than the current. The total area in LIG was nearly the same as the current because of the similar climate. It was worth noting that there would be a reduction of the total area in the future. Loss of area occurred at the edges of bogs, especially under RCP8.5. The distribution center of bogs will shift to the northwest in the immediate future. The precipitation of driest month, the mean temperature of warmest quarter and the precipitation of warmest quarter were identified as crucial climatic factors affecting the distribution of Sphagnum bogs. Overall, our research provides scientific evidence for the long-term protection and effective management of these rare, precious natural resources and suggestions for in situ conservation.
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收藏
页数:15
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