Seasonal Variations in N‐Containing Bacteriohopanepolyols and Their Aerobic Methane Oxidation Implications in a Tropical Lake

Abstract Tropical lakes are significant sources of atmospheric methane. Understanding and reconstructing methane cycling in these systems is critical for constraining its climatic impact. Certain N‐containing bacteriohopanepolyols (BHPs), potentially associated with methane‐oxidizing bacteria (MOB), show promise as biomarkers for aerobic methane oxidation (AMO), yet their behavior in natural settings is not fully understood. Here, we present seasonal variations of BHPs, particularly MOB‐associated BHPs, from the seasonally stratified tropical Huguangyan maar lake (HGY maar lake) in China over a full year. Various BHPs were detected in this study. Bacteriohopanetetrol‐34S (BHT‐34S), 3‐methyl‐bacteriohopanetetrol (3Me‐BHT), and bacteriohopanepentol (BHpentol) peaked in summer, likely associated with bacterial biomass or increased water temperature. Nucleoside BHPs, including adenosylhopane, adenosylhopane HG‐diMe , and Me‐adenosylhopane HG‐Me , were more abundant in deep waters during several months with no relation with soil input, supporting in situ production. Importantly, alongside established MOB biomarkers such as aminopentol and aminotetrol, ethenolamine‐BHhexol and N‐formylated‐aminopentol also show high potential for tracing MOB. Their abundances were significantly elevated in bottom waters from May to September during stratification, with pronounced peaks during October overturn. Methylcarbamate‐aminoBHPs (MC‐aminoBHPs) showed somewhat distinct patterns, being enriched only in deep waters during stratification but without the pronounced October peak, potentially indicating different MOB communities or environmental conditions favoring their production under low‐oxygen and high‐ammonium conditions. MOB‐associated BHPs exhibited strong seasonal patterns aligning with dissolved methane concentrations and AMO variations in most seasonally stratified lakes. This study reveals, for the first time from a BHP perspective, the seasonal dynamics of AMO in HGY maar lake, including intensified AMO in the hypolimnion during stratification and lake‐wide AMO during October overturn. Our findings support the application of N‐containing BHPs as effective biomarkers for tracing AMO in lakes.

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Publication Details

Journal
Journal of Geophysical Research Biogeosciences
Published
2026-02-01
DOI
https://doi.org/10.1029/2025jg009501
Primary Topic
Methane Hydrates and Related Phenomena
Type
article
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article

Seasonal Variations in N‐Containing Bacteriohopanepolyols and Their Aerobic Methane Oxidation Implications in a Tropical Lake

Bingbing Wei, Manyu Kang, Fajin Chen, Nora Richter et al.
Journal of Geophysical Research Biogeosciences
Methane Hydrates and Related Phenomena
article

Seasonal Variations in N‐Containing Bacteriohopanepolyols and Their Aerobic Methane Oxidation Implications in a Tropical Lake

Bingbing Wei, Manyu Kang, Fajin Chen, Nora Richter, Nicole Bale, Darci Rush, Guodong Jia
article en

Abstract

Abstract Tropical lakes are significant sources of atmospheric methane. Understanding and reconstructing methane cycling in these systems is critical for constraining its climatic impact. Certain N‐containing bacteriohopanepolyols (BHPs), potentially associated with methane‐oxidizing bacteria (MOB), show promise as biomarkers for aerobic methane oxidation (AMO), yet their behavior in natural settings is not fully understood. Here, we present seasonal variations of BHPs, particularly MOB‐associated BHPs, from the seasonally stratified tropical Huguangyan maar lake (HGY maar lake) in China over a full year. Various BHPs were detected in this study. Bacteriohopanetetrol‐34S (BHT‐34S), 3‐methyl‐bacteriohopanetetrol (3Me‐BHT), and bacteriohopanepentol (BHpentol) peaked in summer, likely associated with bacterial biomass or increased water temperature. Nucleoside BHPs, including adenosylhopane, adenosylhopane HG‐diMe , and Me‐adenosylhopane HG‐Me , were more abundant in deep waters during several months with no relation with soil input, supporting in situ production. Importantly, alongside established MOB biomarkers such as aminopentol and aminotetrol, ethenolamine‐BHhexol and N‐formylated‐aminopentol also show high potential for tracing MOB. Their abundances were significantly elevated in bottom waters from May to September during stratification, with pronounced peaks during October overturn. Methylcarbamate‐aminoBHPs (MC‐aminoBHPs) showed somewhat distinct patterns, being enriched only in deep waters during stratification but without the pronounced October peak, potentially indicating different MOB communities or environmental conditions favoring their production under low‐oxygen and high‐ammonium conditions. MOB‐associated BHPs exhibited strong seasonal patterns aligning with dissolved methane concentrations and AMO variations in most seasonally stratified lakes. This study reveals, for the first time from a BHP perspective, the seasonal dynamics of AMO in HGY maar lake, including intensified AMO in the hypolimnion during stratification and lake‐wide AMO during October overturn. Our findings support the application of N‐containing BHPs as effective biomarkers for tracing AMO in lakes.

Journal of Geophysical Research BiogeosciencesVol. 131(2)
Tongji University (CN), Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung (DE), University of Bremen (DE), Royal Netherlands Institute for Sea Research (NL), Swiss Federal Institute of Aquatic Science and Technology (CH), Guangdong Ocean University (CN), College of Marin (US)
National Natural Science Foundation of China, Natural Science Foundation of Hainan Province
Openalex Percentile: Top 54%
Methane Hydrates and Related Phenomena
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