Zhejiang Tiantong Forest Ecosystem National Observation and Research Station, School of Ecological and Environmental Sciences, East China Normal University, Shanghai, 200062, China.
Northeast Asia ecosystem Carbon sink research Center (NACC), Center for Ecological Research, Key Laboratory of Sustainable Forest Ecosystem Management-Ministry of Education, School of Forestry, Northeast Forestry University, Harbin, 150040, China.
Nat Commun. 2022 Aug 20;13(1):4914. doi: 10.1038/s41467-022-32671-9.
Biomass allocation in plants is fundamental for understanding and predicting terrestrial carbon storage. Yet, our knowledge regarding warming effects on root: shoot ratio (R/S) remains limited. Here, we present a meta-analysis encompassing more than 300 studies and including angiosperms and gymnosperms as well as different biomes (cropland, desert, forest, grassland, tundra, and wetland). The meta-analysis shows that average warming of 2.50 °C (median = 2 °C) significantly increases biomass allocation to roots with a mean increase of 8.1% in R/S. Two factors associate significantly with this response to warming: mean annual precipitation and the type of mycorrhizal fungi associated with plants. Warming-induced allocation to roots is greater in drier habitats when compared to shoots (+15.1% in R/S), while lower in wetter habitats (+4.9% in R/S). This R/S pattern is more frequent in plants associated with arbuscular mycorrhizal fungi, compared to ectomycorrhizal fungi. These results show that precipitation variability and mycorrhizal association can affect terrestrial carbon dynamics by influencing biomass allocation strategies in a warmer world, suggesting that climate change could influence belowground C sequestration.
植物生物量分配对于理解和预测陆地碳储存至关重要。然而,我们对于升温对根冠比(R/S)影响的认识仍然有限。在这里,我们进行了一项荟萃分析,其中包括 300 多项研究,涵盖了被子植物和裸子植物以及不同的生物群落(农田、沙漠、森林、草原、苔原和湿地)。荟萃分析表明,平均升温 2.50°C(中位数=2°C)显著增加了生物量向根部的分配,R/S 平均增加了 8.1%。有两个因素与这种对升温的响应显著相关:年平均降水量和与植物相关的菌根真菌类型。与叶片相比,在较干燥的生境中,升温诱导的根系分配增加更多(R/S 增加 15.1%),而在较湿润的生境中增加较少(R/S 增加 4.9%)。与外生菌根真菌相比,与丛枝菌根真菌相关的植物中更常出现这种 R/S 模式。这些结果表明,降水变异性和菌根关联可以通过影响生物量分配策略来影响陆地碳动态,表明气候变化可能会影响地下 C 封存。