Limited dependence on soil nitrogen fixation as subtropical forests develop

Soil nitrogen (N) fixation, driven by microbial reactions, is critical to support the entrance of nitrogen in nutrient poor and pioneer ecosystems. However, how and why N fixation and soil diazotrophs evolve as forests develop remain poorly understood. Here, we used a 60-year forest rewilding chrono...

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Published inMicrobiological research Vol. 285; p. 127757
Main Authors Fu, Ruoxian, Cao, Chaoyang, Liu, Li, Zhu, Hongguang, Malghani, Saadat, Yu, Yuanchun, Liao, Yangwenke, Delgado-Baquerizo, Manuel, Li, Xiaogang
Format Journal Article
LanguageEnglish
Published Germany Elsevier GmbH 01.08.2024
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Summary:Soil nitrogen (N) fixation, driven by microbial reactions, is critical to support the entrance of nitrogen in nutrient poor and pioneer ecosystems. However, how and why N fixation and soil diazotrophs evolve as forests develop remain poorly understood. Here, we used a 60-year forest rewilding chronosequence and found that soil N fixation activity gradually decreased with increasing forest age, experiencing dramatic drops of 64.8% in intermediate stages and 93.0% in the oldest forests. Further analyses revealed loses in diazotrophic diversity and a significant reduction in the abundance of important diazotrophs (e.g., Desulfovibrio and Pseudomonas) as forest develops. This reduction in N fixation, and associated shifts in soil microbes, was driven by acidification and increases in N content during forest succession. Our results provide new insights on the life history of one of the most important groups of soil organisms in terrestrial ecosystems, with consequences for understanding the buildup of nutrients as forest soil develops. [Display omitted]
Bibliography:ObjectType-Article-1
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content type line 23
ISSN:0944-5013
1618-0623
DOI:10.1016/j.micres.2024.127757