文献类型： 外文期刊

作者： Sun, Feng ¹ ; Fan, Linan ¹ ; Deng, Guangyan ¹ ; Kuzyakov, Yakov ² ; Zhang, Yue ¹ ; Wang, Jinchuang ⁴ ; Li, Yingwen ⁵ ; Wang, Faming ⁵ ; Li, Zhian ⁵ ; Tariq, Akash ⁷ ; Sardans, Jordi ⁸ ; Penuelas, Josep ⁸ ; Wang, Mei ¹⁰ ; Peng, Changlian ¹ ;

作者机构： 1.South China Normal Univ, Sch Life Sci, Guangdong Prov Key Lab Biotechnol Plant Dev, Guangzhou Key Lab Subtrop Biodivers & Biomonitorin, Guangzhou 510631, Guangdong, Peoples R China

2.Univ Gottingen, Dept Soil Sci Temperate Ecosyst, Dept Agr Soil Sci, Gottingen, Germany

3.RUDN Univ, Peoples Friendship Univ Russia, Moscow, Russia

4.Chinese Acad Trop Agr Sci, Environm & Plant Protect Inst, Haikou, Hainan, Peoples R China

5.South China Bot Garden, CAS Engn Lab Ecol Restorat Isl & Coastal Ecosyst, Xiaoliang Res Stn Trop Coastal Ecosyst, Guangzhou 510000, Peoples R China

6.Southern Marine Sci & Engn Guangdong Lab Guangzhou, Guangzhou 510000, Peoples R China

7.Chinese Acad Sci, Xinjiang Inst Ecol & Geog, State Key Lab Desert & Oasis Ecol, Urumqi 830011, Peoples R China

8.UAB, CSIC, Global Ecol Unit, CREAF, Barcelona 08193, Catalonia, Spain

9.CREAF, Barcelona 08193, Catalonia, Spain

10.South China Normal Univ, Sch Geog Sci, Guangzhou 510631, Peoples R China

关键词： Tropical forest; Rainfall changes; Soil carbon fractions; Microbial necromass; Lignin phenols; Mineral bound carbon

期刊名称：SOIL BIOLOGY & BIOCHEMISTRY （ 影响因子：9.8； 五年影响因子：10.4 ）

ISSN： 0038-0717

年卷期： 2024 年 197 卷

页码：

收录情况： SCI

摘要： Subsoils contain more than half of global soil organic matter (SOM) stocks. Given that sequestration and turnover processes of SOM are slower in the subsoil than in the topsoil, subsoil carbon (C) stocks are likely to be vulnerable to shifts in precipitation patterns. Therefore, we investigated the responses of different sources of tropical forest soil organic C (SOC) pools to a delayed onset and increased intensity of seasonal precipitation in a 10-year rainfall manipulation experiment. While total SOC varied with soil depth, regardless of shifts in rainfall pattern, we observed that changes in precipitation patterns affected the composition of SOC pools. A delayed wet season increased both the content and proportion of the light fraction C in the SOC at the 0 -10 cm depth, potentially due to a decrease in the light fraction decomposition. The delayed wet season also led to a higher content of iron (Fe)-bound organic C, due to impacts on free iron (Fe 3 + ) and aluminum oxides. In addition, wetter wet season led to a higher content of lignin phenols in the top- and subsoil (0 -70 cm), due to anoxic conditions preventing lignin decomposition. However, this precipitation shift decreased both the content and proportion of fungal necromass in the SOC in the subsoil (50 -70 cm), this was attributed to fungal necromass decomposition by microorganisms facilitated by increased N-acquisition enzyme activity. Overall, greater precipitation intensity increased the vulnerability of subsoil C to losses, primarily due to greater microbial decomposition under increased N limitation. Our study demonstrates the subsoil C-cycling processes in shaping SOM stocks to global changes in precipitation patterns.