文献类型：期刊文献

英文题名：Canopy gap impacts on soil organic carbon and nutrient dynamic: a meta-analysis

作者：Tong, Ran[1] Ji, Biyong[2] Wang, G. Geoff[3] Lou, Chenyang[1] Ma, Cong[1] Zhu, Nianfu[1] Yuan, Wenwen[1] Wu, Tonggui[1]

第一作者：童冉

通信作者：Wu, TG[1]

机构：[1]Chinese Acad Forestry, Res Inst Subtrop Forestry, East China Coastal Forest Ecosyst Long Term Res St, Hangzhou 311400, Zhejiang, Peoples R China;[2]Zhejiang Forest Resource Monitoring Ctr, 71 East Fengqi Rd, Hangzhou 310020, Peoples R China;[3]Clemson Univ, Dept Forestry & Environm Conservat, Clemson, SC 29634 USA

年份：2024

卷号：81

期号：1

外文期刊名：ANNALS OF FOREST SCIENCE

收录：;Scopus(收录号：2-s2.0-85186547558);WOS:【SCI-EXPANDED(收录号:WOS:001179754000002)】；

基金：We sincerely thank all the scientists whose data and work were included in this meta-analysis.

语种：英文

外文关键词：Canopy gaps; Soil organic matter; Nutrient cycling; Topsoil properties; Climate effects; Forest ecosystems

摘要：Key messageThe forest canopy gaps, formed by natural or anthropogenic factors, have been found to reduce soil carbon content and increase nutrient availability. The magnitudes of these effects have been observed to increase with gap age and size, and are largely influenced by changes in temperature, precipitation, and solar radiation.ContextLocal studies have illustrated the influence of canopy gaps on the spatial heterogeneity of soil carbon and nutrients, playing a pivotal role in driving forest regeneration and succession. Nevertheless, it remains largely unknown whether the response of soil carbon and nutrient content to gap formation is consistent across forest ecosystems at global scale.AimsThe aim of this paper is to assess the homogeneity of the observed responses of soil carbon and nutrients following gap formation among a wide array of forest ecosystems and climatic regions.MethodsWe performed a meta-analysis synthesizing 2127 pairwise observations from 52 published articles to quantify the changes in in soil physical, chemical, and microbial variables resulting from gap creation in natural forests and plantations spanning tropical to boreal regions.ResultsCanopy gaps resulted in significant decrease of soil organic carbon (Corg) and microbial carbon (Cmic). The concentrations of ammonium (NH4+), nitrate (NO3-), and available phosphorus (available P) increased following gap creation. These changes mainly occurred in the growing season and in the mineral soil layer, becoming more pronounced with increasing gap age and size. The change in Corg was negatively regulated by mean annual precipitation, and was associated with the changes in Nt and Nmic. The change in NH4+ was positively regulated by mean annual temperature, and was associated with the changes in available P and oxidoreductases (Ox-EEAs). The model explaining the change in soil carbon content exhibited a higher explanatory power than the one accounting for changes in soil nutrient availability.ConclusionThe results indicated that forest canopy gaps resulted in a reduction in soil carbon content and an increase in nutrient availability. These findings contribute to a better understanding of the role of small-scale disturbances as drivers of forest ecosystem succession.