With the increasing attention on global climate change and glacier retreat, the study of glacier microbiota has gradually become an important field of research.
Prof. ZHANG Wei's research team from the Northwest Institute of Eco-Environment and Resources of the Chinese Academy of Sciences found that the processes of sequestration, release and colonization of glacier microbes alter the diversity and structure of glacier microbial communities, as well as the complexity of microbial networks.
The researchers used a Z-P plot of species topological roles to screen the keystone taxa of glacier microbial communities. The results indicated that the keystone taxa in the glacial microbial ecosystem of the Dongkemadi Glacier mainly belong to the genus Polaromonas.
They demonstrated that hierarchical interactions among different microorganisms increased the complexity of the bacterial-fungal-archaeal network, and this complexity increased sequentially with the processes of sequestration, release, and colonization of glacial microorganisms.
Furthermore, most keystone taxa in the glacial ecosystem are influenced by the combined properties of multiple environmental factors, suggesting that these keystone taxa are not severely lost due to sudden changes in individual environmental factors.
"As a sensitive area to climate change, the future temperature trend of the glacier area will significantly affect the structure of the glacier microbial community," said Prof. ZHANG.
The study was published in Environment International on May 31.
86-10-68597521 (day)
86-10-68597289 (night)
86-10-68511095 (day)
86-10-68512458 (night)
cas_en@cas.cn
52 Sanlihe Rd., Xicheng District,
Beijing, China (100864)
Copyright © 2002 - Chinese Academy of Sciences
