期刊
ENVIRONMENTAL MICROBIOLOGY
卷 23, 期 4, 页码 2152-2168出版社
WILEY
DOI: 10.1111/1462-2920.15383
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资金
- Swiss National Science Foundation (SNSF) [31BD30_172464]
- Swiss Polar Institute (SPI)
- Swiss National Science Foundation (SNF) [31BD30_172464] Funding Source: Swiss National Science Foundation (SNF)
Alpine ecosystems are rapidly changing due to climate warming, with upward migrations of plants leading to an increase in easily decomposable substrates that strongly affect soil microbiomes. Microbial communities in high alpine ecosystems are sensitive to these changes, with shifts in community structure potentially impacting biogeochemical processes. The addition of artificial root exudates in incubation experiments resulted in elevated respiration, decreased alpha diversity, and significant changes in microbial community structure.
Due to climate warming, alpine ecosystems are changing rapidly. Ongoing upward migrations of plants and thus an increase of easily decomposable substrates will strongly affect the soil microbiome. To understand how belowground communities will respond to such changes, we set up an incubation experiment with permafrost and active soil layers from northern (NW) and southern (SE) slopes of a mountain ridge on Muot da Barba Peider in the Swiss Alps and incubated them with or without artificial root exudates (AREs) at two temperatures, 4 degrees C or 15 degrees C. The addition of AREs resulted in elevated respiration across all soil types. Bacterial and fungal alpha diversity decreased significantly, coinciding with strong shifts in microbial community structure in ARE-treated soils. These shifts in bacterial community structure were driven by an increased abundance of fast-growing copiotrophic taxa. Fungal communities were predominantly affected by AREs in SE active layer soils and shifted towards fast-growing opportunistic yeast. In contrast, in the colder NW facing active layer and permafrost soils fungal communities were more influenced by temperature changes. These findings demonstrate the sensitivity of soil microbial communities in high alpine ecosystems to climate change and how shifts in these communities may lead to functional changes impacting biogeochemical processes.
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