CAS Engineering Laboratory for Vegetation Ecosystem Restoration on Islands and Coastal Zones / Key Laboratory of Vegetation Restoration and Management of Degraded Ecosystems, South China Botanical Garden, Chinese Academy of Sciences, Guangzhou, 510650, China.
University of Rhode Island, Department of Mechanical, Industrial and Systems Engineering, 2 East Alumni Avenue, Kingston, RI, 02881, USA.
J Environ Manage. 2021 Feb 15;280:111647. doi: 10.1016/j.jenvman.2020.111647. Epub 2020 Nov 24.
Soil organisms play essential roles in maintaining multiple ecosystem processes, but our understanding of the dynamics of these communities during forest succession remains limited. In this study, the dynamics of soil organism communities were measured along a 3-step succession sequence of subtropical forests (i.e., a conifer forest, CF; a mixed conifer and broad-leaved forest, MF; and a monsoon evergreen broad-leaved forest, BF). The eco-exergy evaluation method was used as a complement to the classic community structure index system to reveal the holistic dynamics of the bio-thermodynamic health of soil organism communities in a forest succession series. Association between the self-organization of soil organisms, soil properties, and plant factors were explored through redundancy analyses (RDA). The results indicated that the biomass of soil microbes progressively increased in the dry season, from 0.75 g m in CF to 1.75 g m in BF. Microbial eco-exergy showed a similar pattern, while the community structure and the specific eco-exergy remained constant. Different trends for the seasons were observed for the soil fauna community, where the community biomass increased from 0.72 g m to over 1.97 g m in the dry season, but decreased from 3.94 g m to 2.36 g m in the wet season. Faunal eco-exergies followed a similar pattern. Consequently, the average annual biomass of the soil faunal community remained constant (2.17-2.39 g m) along the forest succession sequence, while the significant seasonal differences in both faunal biomass and eco-exergy observed at the early successional stage (CF) were insignificant in the middle and late forest successional stages (MF and BF). Both the dynamics of soil microbes and soil fauna were tightly correlated with tree biomass and with soil physicochemical properties, especially soil pH, moisture, total nitrogen, nitrate nitrogen, and organic matter content.
土壤生物在维持多种生态系统过程中发挥着至关重要的作用,但我们对这些群落在森林演替过程中的动态变化的理解仍然有限。在这项研究中,我们沿着亚热带森林的 3 个演替阶段(即针叶林、针阔混交林和季风常绿阔叶林)测量了土壤生物群落的动态变化。我们使用生态能评估方法作为经典群落结构指数系统的补充,以揭示森林演替系列中土壤生物群落生物热力学健康的整体动态变化。我们通过冗余分析(RDA)探讨了土壤生物的自组织、土壤特性和植物因素之间的关联。结果表明,土壤微生物的生物量在旱季逐渐增加,从 CF 中的 0.75 g·m到 BF 中的 1.75 g·m。微生物生态能也呈现出相似的趋势,而群落结构和特定生态能保持不变。土壤动物群落的季节变化趋势不同,其中群落生物量在旱季从 0.72 g·m增加到 1.97 g·m以上,但在雨季从 3.94 g·m减少到 2.36 g·m。动物生态能也呈现出相似的趋势。因此,在森林演替序列中,土壤动物群落的平均年生物量保持不变(2.17-2.39 g·m),而在早期演替阶段(CF)观察到的动物生物量和生态能的显著季节性差异在中晚期森林演替阶段(MF 和 BF)并不明显。土壤微生物和土壤动物的动态变化与树木生物量和土壤理化性质密切相关,特别是土壤 pH 值、水分、总氮、硝酸盐氮和有机质含量。