Belowground biomass of alpine shrublands across the northeast Tibetan Plateau. Issue 12 (19th April 2020)

• Record Type: Journal Article
• Authors: Xiuqing, Nie; Wang, Dong; Lucun, Yang; Li, Fan; Guoying, Zhou
• Is Part Of: Ecology and evolution. Volume 10:Issue 12(2020)
• Page Start: 5315
• Page End: 5322
• Publication Date: 2020-04-19
• Subjects: alpine shrublands -- belowground biomass -- mean annual precipitation -- mean annual temperature -- Tibetan Plateau; Ecology -- Periodicals; Evolution -- Periodicals; 577.05
• DOI: 10.1002/ece3.6275
• Languages: English
• ISSNs: 2045-7758

Abstract

Abstract: Although belowground biomass (BGB) plays an important role in global cycling, the storage of BGB and climatic effects on it are remaining unclear. With data from 49 sites, we aimed to investigate BGB and its climatic controls in alpine shrublands in the Tibetan Plateau. Our study showed that the BGB (both grass‐layer and shrub‐layer biomass) storage in the alpine shrublands was 67.24 Tg, and the mean BGB density and shrublands area were 1, 567.38 g/m 2 and 4.29 × 10 4 km 2, respectively. Shrub layer had a larger BGB stock and accounted for 66% of total BGB this area, while only 34% was accumulated in the grass layer. BGB of the grass layer in the Tibetan Plateau shrublands was larger than that of Tibetan alpine grasslands, indicating that shrubland ecosystem played a critical importance role in carbon cycle on the Tibetan Plateau. The BGB in the grass layer and shrub layer demonstrated different correlations with climatic factors. Specifically, the effects from mean annual temperature on shrub‐layer BGB were not significant, similarly to the relationship between mean annual precipitation and grass‐layer BGB. But shrub‐layer BGB had a significantly positive relationship with mean annual precipitation ( p < .05), while grass‐layer BGB showed a trend of decrease with increasing mean annual temperature ( p < .05). Consequently, the actual and potential increases of BGB varied due to different increases of mean annual precipitation and temperature among different areas of the Tibetan Plateau. Therefore, in the warmer and wetter scenario, due to contrary relationships from mean annual precipitation and temperature on shrub‐layer BGB and grass‐layer BGB, it is necessary to conduct a long‐term monitoring about dynamic changes to increase the precision of assessment of BGB carbon sequestration in the Tibetan Plateau alpine shrublands. Abstract : The BGB storage (both shrub layer biomass and grass layer biomass) in the alpine shrublands as 67.24 ± 26.34 Tg. The BGB in grasslands layer and shrublands layer have different responses to changing climatic factors.