盐度
湿地
土壤盐分
环境科学
古细菌
环境化学
碱土
铵
产甲烷
甲烷
土壤水分
农学
生态学
化学
土壤科学
生物
基因
生物化学
有机化学
作者
Feng Li,Huiju Li,Huihui Su,Yong Du,Zhongyan Gao,Huajun Liu,Hong Liang,Dawen Gao
出处
期刊:Research Square - Research Square
日期:2023-05-03
标识
DOI:10.21203/rs.3.rs-2754768/v1
摘要
Abstract The increase in temperature caused by global climate change has promoted the salinization of wetlands. Inland saline-alkaline wetlands have an environment of over-humidity and shallow water and are hot spots for CH 4 emissions. However, there are few reports on the effect of salinity on CH 4 emissions in inland saline-alkaline wetlands. This study revealed the effects of salinity, habitat, and their interactions on CH 4 emissions, and explored the response of methanogenic archaea to salinity. Overall, salinity inhibited CH 4 emissions. But there were different responses in the three habitat soils. Salinity decreased the relative abundance of methanogenic archaea and changed the community structure. In addition, salinity changed soil pH and dissolved organic carbon (DOC) and ammonium (NH 4 + ) concentrations, which were significantly correlated with methanogenic archaea. Our study showed that salinity changed the soil physicochemical properties and characteristics of the methanogenic archaeal community, affecting CH 4 emissions.
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