Microbial Metabolism and Environmental Controls of Acetate Cycling in the Northwest Pacific Ocean

Microbial acetate metabolism is an important part of marine carbon cycling. We present a comprehensive study to constrain microbial acetate metabolism and its regulation in surface seawater of the northwest Pacific Ocean. We found that acetate oxidation (rate constant k: 0.016–0.506 day−1) accounted...

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Published inGeophysical research letters Vol. 51; no. 17
Main Authors Mao, Shi‐Hai, Zhou, Zhen, Yan, Shi‐Bo, Xu, Gao‐Bin, Li, Xiao‐Jun, Zhang, Hong‐Hai, Yang, Gui‐Peng, Zhuang, Guang‐Chao
Format Journal Article
LanguageEnglish
Published Washington John Wiley & Sons, Inc 16.09.2024
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Abstract Microbial acetate metabolism is an important part of marine carbon cycling. We present a comprehensive study to constrain microbial acetate metabolism and its regulation in surface seawater of the northwest Pacific Ocean. We found that acetate oxidation (rate constant k: 0.016–0.506 day−1) accounted for 77.6%–99.4% of the total microbial acetate uptake, suggesting that acetate was predominantly used as a microbial energy source. Acetate also served as a significant biomass carbon source, as reflected by the elevated contribution of acetate assimilation to bacterial carbon production. Acetate turnover was largely influenced by water mass mixing and nutrient conditions. Atmospheric deposition was a source of acetate in surface water and this process can also impact the microbial acetate uptake. Microbial utilization of acetate could account for up to 25.9% of the bacterial carbon demand, suggesting the significant role of acetate metabolism in microbial carbon cycling in the open ocean. Plain Language Summary Acetate is a key metabolic intermediate during the mineralization of organic matter and microbial acetate metabolism plays a crucial role in marine carbon cycling. However, the microbial metabolism of acetate and its environmental controls in pelagic waters remain poorly understood. We investigated biogeochemical cycling of acetate in the Kuroshio‐Oyashio extension region of northwest Pacific Ocean. Acetate concentrations in surface waters were generally low and atmospheric deposition was a source of acetate in the upper ocean. Acetate was used preferentially as a microbial energy source and the proportion of acetate devoted to bacterial growth or respiration largely depended on local nutrient conditions. Rapid biological turnover of acetate contributed significantly to bacterial carbon demand, exceeding the contributions of other compounds such as methanol. These results constrain the atmospheric sources and microbial sinks of marine acetate and reveal the ecological significance of microbial acetate metabolism in the open ocean. Key Points Microbial uptake rates of acetate ranged from 1.7 to 495 nmol L−1 day−1 in surface waters of the northwest Pacific Ocean Acetate is used preferentially as a microbial energy source rather than as a biomass carbon source Microbial acetate metabolism is influenced by water mass mixing and atmospheric deposition
AbstractList Abstract Microbial acetate metabolism is an important part of marine carbon cycling. We present a comprehensive study to constrain microbial acetate metabolism and its regulation in surface seawater of the northwest Pacific Ocean. We found that acetate oxidation (rate constant k : 0.016–0.506 day −1 ) accounted for 77.6%–99.4% of the total microbial acetate uptake, suggesting that acetate was predominantly used as a microbial energy source. Acetate also served as a significant biomass carbon source, as reflected by the elevated contribution of acetate assimilation to bacterial carbon production. Acetate turnover was largely influenced by water mass mixing and nutrient conditions. Atmospheric deposition was a source of acetate in surface water and this process can also impact the microbial acetate uptake. Microbial utilization of acetate could account for up to 25.9% of the bacterial carbon demand, suggesting the significant role of acetate metabolism in microbial carbon cycling in the open ocean. Plain Language Summary Acetate is a key metabolic intermediate during the mineralization of organic matter and microbial acetate metabolism plays a crucial role in marine carbon cycling. However, the microbial metabolism of acetate and its environmental controls in pelagic waters remain poorly understood. We investigated biogeochemical cycling of acetate in the Kuroshio‐Oyashio extension region of northwest Pacific Ocean. Acetate concentrations in surface waters were generally low and atmospheric deposition was a source of acetate in the upper ocean. Acetate was used preferentially as a microbial energy source and the proportion of acetate devoted to bacterial growth or respiration largely depended on local nutrient conditions. Rapid biological turnover of acetate contributed significantly to bacterial carbon demand, exceeding the contributions of other compounds such as methanol. These results constrain the atmospheric sources and microbial sinks of marine acetate and reveal the ecological significance of microbial acetate metabolism in the open ocean. Key Points Microbial uptake rates of acetate ranged from 1.7 to 495 nmol L −1  day −1 in surface waters of the northwest Pacific Ocean Acetate is used preferentially as a microbial energy source rather than as a biomass carbon source Microbial acetate metabolism is influenced by water mass mixing and atmospheric deposition
Abstract Microbial acetate metabolism is an important part of marine carbon cycling. We present a comprehensive study to constrain microbial acetate metabolism and its regulation in surface seawater of the northwest Pacific Ocean. We found that acetate oxidation (rate constant k: 0.016–0.506 day−1) accounted for 77.6%–99.4% of the total microbial acetate uptake, suggesting that acetate was predominantly used as a microbial energy source. Acetate also served as a significant biomass carbon source, as reflected by the elevated contribution of acetate assimilation to bacterial carbon production. Acetate turnover was largely influenced by water mass mixing and nutrient conditions. Atmospheric deposition was a source of acetate in surface water and this process can also impact the microbial acetate uptake. Microbial utilization of acetate could account for up to 25.9% of the bacterial carbon demand, suggesting the significant role of acetate metabolism in microbial carbon cycling in the open ocean.
Microbial acetate metabolism is an important part of marine carbon cycling. We present a comprehensive study to constrain microbial acetate metabolism and its regulation in surface seawater of the northwest Pacific Ocean. We found that acetate oxidation (rate constant k: 0.016–0.506 day−1) accounted for 77.6%–99.4% of the total microbial acetate uptake, suggesting that acetate was predominantly used as a microbial energy source. Acetate also served as a significant biomass carbon source, as reflected by the elevated contribution of acetate assimilation to bacterial carbon production. Acetate turnover was largely influenced by water mass mixing and nutrient conditions. Atmospheric deposition was a source of acetate in surface water and this process can also impact the microbial acetate uptake. Microbial utilization of acetate could account for up to 25.9% of the bacterial carbon demand, suggesting the significant role of acetate metabolism in microbial carbon cycling in the open ocean.
Microbial acetate metabolism is an important part of marine carbon cycling. We present a comprehensive study to constrain microbial acetate metabolism and its regulation in surface seawater of the northwest Pacific Ocean. We found that acetate oxidation (rate constant k: 0.016–0.506 day−1) accounted for 77.6%–99.4% of the total microbial acetate uptake, suggesting that acetate was predominantly used as a microbial energy source. Acetate also served as a significant biomass carbon source, as reflected by the elevated contribution of acetate assimilation to bacterial carbon production. Acetate turnover was largely influenced by water mass mixing and nutrient conditions. Atmospheric deposition was a source of acetate in surface water and this process can also impact the microbial acetate uptake. Microbial utilization of acetate could account for up to 25.9% of the bacterial carbon demand, suggesting the significant role of acetate metabolism in microbial carbon cycling in the open ocean. Plain Language Summary Acetate is a key metabolic intermediate during the mineralization of organic matter and microbial acetate metabolism plays a crucial role in marine carbon cycling. However, the microbial metabolism of acetate and its environmental controls in pelagic waters remain poorly understood. We investigated biogeochemical cycling of acetate in the Kuroshio‐Oyashio extension region of northwest Pacific Ocean. Acetate concentrations in surface waters were generally low and atmospheric deposition was a source of acetate in the upper ocean. Acetate was used preferentially as a microbial energy source and the proportion of acetate devoted to bacterial growth or respiration largely depended on local nutrient conditions. Rapid biological turnover of acetate contributed significantly to bacterial carbon demand, exceeding the contributions of other compounds such as methanol. These results constrain the atmospheric sources and microbial sinks of marine acetate and reveal the ecological significance of microbial acetate metabolism in the open ocean. Key Points Microbial uptake rates of acetate ranged from 1.7 to 495 nmol L−1 day−1 in surface waters of the northwest Pacific Ocean Acetate is used preferentially as a microbial energy source rather than as a biomass carbon source Microbial acetate metabolism is influenced by water mass mixing and atmospheric deposition
Author Zhou, Zhen
Mao, Shi‐Hai
Zhang, Hong‐Hai
Li, Xiao‐Jun
Zhuang, Guang‐Chao
Xu, Gao‐Bin
Yan, Shi‐Bo
Yang, Gui‐Peng
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  organization: Ocean University of China
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Snippet Microbial acetate metabolism is an important part of marine carbon cycling. We present a comprehensive study to constrain microbial acetate metabolism and its...
Abstract Microbial acetate metabolism is an important part of marine carbon cycling. We present a comprehensive study to constrain microbial acetate metabolism...
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SubjectTerms acetate
acetate metabolism
Acetates
Acetic acid
Bacteria
Biogeochemical cycles
Biological effects
Biomass energy production
Carbon
Carbon cycle
Carbon sources
Deposition
Energy metabolism
Energy sources
Environmental control
Kuroshio‐Oyashio extension
Marine biology
marine carbon cycling
Metabolism
Microorganisms
Mineralization
northwest Pacific Ocean
Nutrients
Oceans
Organic matter
Oxidation
Seawater
Surface water
Upper ocean
Water mass mixing
Water masses
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Title Microbial Metabolism and Environmental Controls of Acetate Cycling in the Northwest Pacific Ocean
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