Chen-Hao Lyu , Wen-Jun He , Peng Chen , Xin-Xin Jing , Guo-Shi Zhang , Run-Qin Zhang , Zi-Yan Li , Zhi-Guo Li , Yi Liu
{"title":"农田管理措施和全球变化因素对生态系统微生物坏死的不同影响:对土壤有机碳的影响","authors":"Chen-Hao Lyu , Wen-Jun He , Peng Chen , Xin-Xin Jing , Guo-Shi Zhang , Run-Qin Zhang , Zi-Yan Li , Zhi-Guo Li , Yi Liu","doi":"10.1016/j.catena.2025.109273","DOIUrl":null,"url":null,"abstract":"<div><div>Microbial necromass carbon (MNC) is a crucial contributor to Soil Organic Carbon (SOC), yet its responses to cropland management practices and global changes remain poorly understood. Here, a global <em>meta</em>-analysis was conducted to reveal general patterns of how MNC respond to these factors across major terrestrial ecosystems. Results showed that cropland management practices increased MNC by 6.5–29.4 %, with manure amendment having the largest effect (+29.4 %), followed by fertilization (+16.2 %), straw application (+13.1 %), no-tillage/reduced-tillage (NT/RT, +11.3 %), biochar amendment (+8.8 %), and cover crops (+6.5 %). In grasslands, warming increased MNC by 9.5 %, phosphorus (P) addition had negative effects on MNC, and nitrogen (N) addition had no effect. In forestlands, P addition increased MNC the most (+41.6 %), followed by NP (+33.4 %) and N addition (+11.3 %). Importantly, responses of MNC to management practices and global changes were influenced by climatic and edaphic factors. For example, fertilization and straw application increased necromass in humid and warm climates, while NT/RT and manure amendments were more effective in cooler climates or acidic soils. Fertilization, straw, and manure amendments led to greater MNC accumulation in soils with lower initial SOC levels. N addition had a more pronounced effect on necromass in humid forests, whereas P addition was more impactful in cooler climates. Furthermore, MNC was closely linked to SOC, highlighting the important role of microbial necromass in SOC sequestration. This study fills a key knowledge gap by synthesizing global evidence on how MNC responds to cropland management practices and global change factors, offering novel insights into optimizing land management strategies for soil carbon stabilization in future climate change.</div></div>","PeriodicalId":9801,"journal":{"name":"Catena","volume":"258 ","pages":"Article 109273"},"PeriodicalIF":5.7000,"publicationDate":"2025-07-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Divergent effects of cropland management practices and global change factors on microbial necromass across ecosystems: implications for soil organic carbon\",\"authors\":\"Chen-Hao Lyu , Wen-Jun He , Peng Chen , Xin-Xin Jing , Guo-Shi Zhang , Run-Qin Zhang , Zi-Yan Li , Zhi-Guo Li , Yi Liu\",\"doi\":\"10.1016/j.catena.2025.109273\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Microbial necromass carbon (MNC) is a crucial contributor to Soil Organic Carbon (SOC), yet its responses to cropland management practices and global changes remain poorly understood. Here, a global <em>meta</em>-analysis was conducted to reveal general patterns of how MNC respond to these factors across major terrestrial ecosystems. Results showed that cropland management practices increased MNC by 6.5–29.4 %, with manure amendment having the largest effect (+29.4 %), followed by fertilization (+16.2 %), straw application (+13.1 %), no-tillage/reduced-tillage (NT/RT, +11.3 %), biochar amendment (+8.8 %), and cover crops (+6.5 %). In grasslands, warming increased MNC by 9.5 %, phosphorus (P) addition had negative effects on MNC, and nitrogen (N) addition had no effect. In forestlands, P addition increased MNC the most (+41.6 %), followed by NP (+33.4 %) and N addition (+11.3 %). Importantly, responses of MNC to management practices and global changes were influenced by climatic and edaphic factors. For example, fertilization and straw application increased necromass in humid and warm climates, while NT/RT and manure amendments were more effective in cooler climates or acidic soils. Fertilization, straw, and manure amendments led to greater MNC accumulation in soils with lower initial SOC levels. N addition had a more pronounced effect on necromass in humid forests, whereas P addition was more impactful in cooler climates. Furthermore, MNC was closely linked to SOC, highlighting the important role of microbial necromass in SOC sequestration. This study fills a key knowledge gap by synthesizing global evidence on how MNC responds to cropland management practices and global change factors, offering novel insights into optimizing land management strategies for soil carbon stabilization in future climate change.</div></div>\",\"PeriodicalId\":9801,\"journal\":{\"name\":\"Catena\",\"volume\":\"258 \",\"pages\":\"Article 109273\"},\"PeriodicalIF\":5.7000,\"publicationDate\":\"2025-07-10\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Catena\",\"FirstCategoryId\":\"97\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0341816225005752\",\"RegionNum\":1,\"RegionCategory\":\"农林科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Catena","FirstCategoryId":"97","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0341816225005752","RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
Divergent effects of cropland management practices and global change factors on microbial necromass across ecosystems: implications for soil organic carbon
Microbial necromass carbon (MNC) is a crucial contributor to Soil Organic Carbon (SOC), yet its responses to cropland management practices and global changes remain poorly understood. Here, a global meta-analysis was conducted to reveal general patterns of how MNC respond to these factors across major terrestrial ecosystems. Results showed that cropland management practices increased MNC by 6.5–29.4 %, with manure amendment having the largest effect (+29.4 %), followed by fertilization (+16.2 %), straw application (+13.1 %), no-tillage/reduced-tillage (NT/RT, +11.3 %), biochar amendment (+8.8 %), and cover crops (+6.5 %). In grasslands, warming increased MNC by 9.5 %, phosphorus (P) addition had negative effects on MNC, and nitrogen (N) addition had no effect. In forestlands, P addition increased MNC the most (+41.6 %), followed by NP (+33.4 %) and N addition (+11.3 %). Importantly, responses of MNC to management practices and global changes were influenced by climatic and edaphic factors. For example, fertilization and straw application increased necromass in humid and warm climates, while NT/RT and manure amendments were more effective in cooler climates or acidic soils. Fertilization, straw, and manure amendments led to greater MNC accumulation in soils with lower initial SOC levels. N addition had a more pronounced effect on necromass in humid forests, whereas P addition was more impactful in cooler climates. Furthermore, MNC was closely linked to SOC, highlighting the important role of microbial necromass in SOC sequestration. This study fills a key knowledge gap by synthesizing global evidence on how MNC responds to cropland management practices and global change factors, offering novel insights into optimizing land management strategies for soil carbon stabilization in future climate change.
期刊介绍:
Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment.
Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.