Jing Li
Current Organizations / Institutes
The organizations/institutes from the scholar's latest article
Jing Li has a total of 16 co-authors. Here are the top co-authors by number of shared publications:
Changling Liu
The Key Laboratory of Gas Hydrate of the Ministry of Natural Resources, Qingdao Institute of Marine Geology, Qingdao, China
1 shared publication- Changling Liu
The Key Laboratory of Gas Hydrate, Ministry of Natural Resources, Qingdao Institute of Marine Geology, Qingdao 266071, China
1 shared publication Gao-Wei Hu
1 shared publication- Hailong Tian
Key Laboratory of Groundwater Resources and Environment, Ministry of Education, Jilin University, Changchun 130021, China
1 shared publication - Keqi Bei
Jilin Univ, Key Lab Groundwater Resources & Environm, Minist Educ, Changchun 130021, Peoples R China
1 shared publication Neng-You Wu
1 shared publication
Latest Publications
- 1 October 2025
- Published by Springer Nature in Acta Oceanologica Sinica
- Vol. 44 (10) , 88-100
Regulation of aerobic methane oxidation by methane concentration: insights from cultivation experiments
- 1 October 2025
- Published by Springer Nature in Acta Oceanologica Sinica
- Vol. 44 (10) , 88-100
Regulation of aerobic methane oxidation by methane concentration: insights from cultivation experiments
- 1 January 2022
- Published by China Geology in China Geology
- Vol. 5 (2) , 1-8
Identification of functionally active aerobic methanotrophs and their methane oxidation potential in sediments from the Shenhu area, South China Sea
Large amounts of gas hydrate are distributed in the northern slope of the South China Sea, which is a potential threat of methane leakage. Aerobic methane oxidation by methanotrophs, significant methane biotransformation that occurs in sediment surface and water column, can effectively reduce atmospheric emission of hydrate-decomposed methane. To identify active aerobic methanotrophs and their methane oxidation potential in sediments from the Shenhu area in the South China Sea, multi-day enrichment incubations were conducted in this study. The results show that the methane oxidation rates in the studied sediments were 2.03‒2.36 μmol/gdw/d, which were higher than those obtained by sediment incubations from other areas in marine ecosystems. Thus we suspect that the methane oxidation potential of methanotrophs was relatively higher in sediments from the Shenhu area. After the incubations family Methylococcaea (type I methanotrophs) mainly consisted of genus Methylobacter and Methylococcaea_Other were predominant with an increased proportion of 70.3%, whereas Methylocaldum decreased simultaneously in the incubated sediments. Collectively, this study may help to gain a better understanding of the methane biotransformation in the Shenhu area.
- 1 January 2022
- Published by China Geology in China Geology
- Vol. 5 (2) , 1-8
Identification of functionally active aerobic methanotrophs and their methane oxidation potential in sediments from the Shenhu area, South China Sea
Large amounts of gas hydrate are distributed in the northern slope of the South China Sea, which is a potential threat of methane leakage. Aerobic methane oxidation by methanotrophs, significant methane biotransformation that occurs in sediment surface and water column, can effectively reduce atmospheric emission of hydrate-decomposed methane. To identify active aerobic methanotrophs and their methane oxidation potential in sediments from the Shenhu area in the South China Sea, multi-day enrichment incubations were conducted in this study. The results show that the methane oxidation rates in the studied sediments were 2.03‒2.36 μmol/gdw/d, which were higher than those obtained by sediment incubations from other areas in marine ecosystems. Thus we suspect that the methane oxidation potential of methanotrophs was relatively higher in sediments from the Shenhu area. After the incubations family Methylococcaea (type I methanotrophs) mainly consisted of genus Methylobacter and Methylococcaea_Other were predominant with an increased proportion of 70.3%, whereas Methylocaldum decreased simultaneously in the incubated sediments. Collectively, this study may help to gain a better understanding of the methane biotransformation in the Shenhu area.