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

• Published in: PloS one Vol. 15; no. 4; p. e0230969
• Main Authors: Cong, Mingyang, Xu, Yueyue, Tang, Luyan, Yang, Wenjing, Jian, Minfei
• Format: Journal Article
• Language: English
• Published: United States Public Library of Science 06.04.2020; Public Library of Science (PLoS)
• Subjects: Bioclimatology; Biology and Life Sciences; Bogs; Carbon; Carbon cycle; Carbon dioxide; Climate change; Computer simulation; Conservation; Datasets; Distribution centres; Distribution patterns; Earth Sciences; Ecology and Environmental Sciences; Ecosystems; Entropy; Environmental factors; Geographical distribution; Geography; Glacial periods; Global temperature changes; Habitats; Interglacial periods; Last Glacial Maximum; Maximum entropy; Mean temperatures; Mountains; Natural resources; Niches; Peatlands; People and Places; Precipitation; Resource conservation; Resource management; Social Sciences; Sphagnum; Variables; China
• DOI: 10.1371/journal.pone.0230969
• ISSN: 1932-6203

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.