H
Hongmei Wang
Researcher at China University of Geosciences (Wuhan)
Publications - 74
Citations - 1339
Hongmei Wang is an academic researcher from China University of Geosciences (Wuhan). The author has contributed to research in topics: Cave & Karst. The author has an hindex of 16, co-authored 61 publications receiving 831 citations.
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Journal ArticleDOI
The Relationship between pH and Bacterial Communities in a Single Karst Ecosystem and Its Implication for Soil Acidification
Yuan Yun,Hongmei Wang,Baiying Man,Xing Xiang,Jianping Zhou,Xuan Qiu,Yong Duan,Annette Summers Engel +7 more
TL;DR: To evaluate the role of pH, total organic carbon, and other geochemical parameters in shaping bacterial communities within a single karst system in central China, samples were collected from the thin surface soils overlying Heshang Cave, cave sediments, and weathered cave passage rocks from the entrance, twilight, and dark zones, as well as from epikarstic drip waters inside the cave.
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Reduction of structural Fe(III) in nontronite by methanogen Methanosarcina barkeri
Deng Liu,Hailiang Dong,Hailiang Dong,Hailiang Dong,Michael E. Bishop,Hongmei Wang,Abinash Agrawal,Sarah J. Tritschler,Dennis D. Eberl,Shucheng Xie +9 more
TL;DR: In this article, the ability of methanogen Methanosarcina barkeri to reduce structural Fe(III) in iron-rich smectite (nontronite NAu-2) and the relationship between iron reduction and methanogenesis were investigated.
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Distribution of Bathyarchaeota Communities Across Different Terrestrial Settings and Their Potential Ecological Functions
TL;DR: It is suggested that Bathyarchaeota may play an important ecological role within archaeal communities via a potential symbiotic association with Methanomicrobia, and 9 indicator groups are identified among the 6 habitats with the most in the estuary sediments.
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Experimental evidence for abiotic formation of low-temperature proto-dolomite facilitated by clay minerals
TL;DR: In this paper, the authors demonstrate through laboratory carbonation experiments that highly negative-charged clay minerals such as illite and montmorillonite can aid the precipitation of abiotic proto-dolomite under ambient conditions, whereas nearly neutral charged kaolinite exerts negligible influence on such process.
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High salinity facilitates dolomite precipitation mediated by Haloferax volcanii DS52
TL;DR: The finding that more carboxyl groups were presented on the cell surface under high salinity conditions to resist the high osmotic pressure, which may result in the subsequent promotion of dolomite formation suggests a link between variations in the hydro-chemical conditions and the formation of dlomite via microbial metabolic activity.