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N-alkane shape distinctive microbial patterns in Kuroshio Extension.
Hu, Xin; Zhao, Shanshan; Li, Haoshuai; Pan, Yaping; Fan, Zhongxiang; Lu, Jinren; Li, Yiming; Song, Guodong; Zhang, Honghai; Liu, Qian; Bao, Mutai.
Affiliation
  • Hu X; Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao, Shandong Province 266100, China; College of Chemistry & Chemical Engineering, Ocean University of China, Qing
  • Zhao S; Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao, Shandong Province 266100, China; College of Chemistry & Chemical Engineering, Ocean University of China, Qing
  • Li H; Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao, Shandong Province 266100, China; College of Chemistry & Chemical Engineering, Ocean University of China, Qing
  • Pan Y; Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao, Shandong Province 266100, China; College of Chemistry & Chemical Engineering, Ocean University of China, Qing
  • Fan Z; Physical Oceanography Laboratory, Ocean University of China, Qingdao, Shandong Province 266100, China.
  • Lu J; Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao, Shandong Province 266100, China; College of Chemistry & Chemical Engineering, Ocean University of China, Qing
  • Li Y; Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao, Shandong Province 266100, China; College of Chemistry & Chemical Engineering, Ocean University of China, Qing
  • Song G; Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao, Shandong Province 266100, China; College of Chemistry & Chemical Engineering, Ocean University of China, Qing
  • Zhang H; Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao, Shandong Province 266100, China; College of Chemistry & Chemical Engineering, Ocean University of China, Qing
  • Liu Q; Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao, Shandong Province 266100, China; College of Chemistry & Chemical Engineering, Ocean University of China, Qing
  • Bao M; Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Laboratory of Marine Chemistry Theory and Technology Ministry of Education, Ocean University of China, Qingdao, Shandong Province 266100, China; College of Chemistry & Chemical Engineering, Ocean University of China, Qing
Environ Int ; 188: 108757, 2024 Jun.
Article in En | MEDLINE | ID: mdl-38795659
ABSTRACT
Marine microorganisms are primary drivers of the elemental cycling. The interaction between heterotrophic prokaryotes and biomarker (n-alkane) in Kuroshio Extension (KE) remains unclear. Here, we categorize KE into three characteristic areas based on ocean temperatures and nutrient conditions Cold Water Area (CWA), Mixed Area (MA), and Warm Water Area (WWA). A total of 49 samples were collected during two-year voyage to identify the source of n-alkane and associated degrading microorganisms. Total n-alkane concentrations (Σn-Alk) in surface water (SW) spanned from 1,308 ng L-1 to 1,890 ng L-1, it was significantly higher (Tukey-Kramer test, p < 0.05) in MA than CWA and WWA. The Σn-Alk in surface sediments (SS) gradually increased from north to south, ranging from 5,982 ng g-1 to 37,857 ng g-1. Bacteria and algae were the primary sources of n-alkane in both SW and SS. Proteobacteria was the most widely distributed among three areas. The presence of Rhodobacteraceae with alkB was the primary reason affecting n-alkane concentrations in SW. The Gammaproteobacteria with alkB and alkR chiefly affected n-alkane concentrations in SS. In summary, n-alkane s serve as an energy source for particular microorganisms, shaping the unique oceanographic patterns.
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Full text: 1 Collection: 01-internacional Database: MEDLINE Main subject: Seawater / Alkanes Country/Region as subject: Asia Language: En Journal: Environ Int Year: 2024 Document type: Article

Full text: 1 Collection: 01-internacional Database: MEDLINE Main subject: Seawater / Alkanes Country/Region as subject: Asia Language: En Journal: Environ Int Year: 2024 Document type: Article
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