Limited dependence on soil nitrogen fixation as subtropical forests develop

9 páginas.- 6 figuras.- referencias.- Supplementary data associated with this article can be found in the online version at doi:10.1016/j.micres.2024.127757

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.

This work was financially supported by the National Key Research and Development Program of China [grant numbers 2022YFD2201900, 2021YDF22011202], the National Natural Science Foundation of China [grant numbers 32122056], Jiangsu Special Fund on Technology Innovation of Carbon Dioxide Peaking and Carbon Neutrality [grant number BE2022420] and Postgraduate Research & Practice Innovation Program of Jiangsu Province [grant number KYCX23_1121

Peer reviewed