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Effects of low oxygen concentrations on aerobic methane oxidation in seasonally hypoxic coastal waters

机译:低氧浓度对季节性缺氧沿海水域有氧甲烷氧化的影响

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Coastal seas may account for more than 75?% of global oceanic methane emissions. There, methane is mainly produced microbially in anoxic sediments from which it can escape to the overlying water column. Aerobic methane oxidation (MOx) in the water column acts as a biological filter, reducing the amount of methane that eventually evades to the atmosphere. The efficiency of the MOx filter is potentially controlled by the availability of dissolved methane and oxygen, as well as temperature, salinity, and hydrographic dynamics, and all of these factors undergo strong temporal fluctuations in coastal ecosystems. In order to elucidate the key environmental controls, specifically the effect of oxygen availability, on MOx in a seasonally stratified and hypoxic coastal marine setting, we conducted a 2-year time-series study with measurements of MOx and physico-chemical water column parameters in a coastal inlet in the south-western Baltic Sea (Eckernf?rde Bay). We found that MOx rates generally increased toward the seafloor, but were not directly linked to methane concentrations. MOx exhibited a strong seasonal variability, with maximum rates (up to 11.6?nmol?L?1?d?1) during summer stratification when oxygen concentrations were lowest and bottom-water temperatures were highest. Under these conditions, 2.4–19.0 times more methane was oxidized than emitted to the atmosphere, whereas about the same amount was consumed and emitted during the mixed and oxygenated periods. Laboratory experiments with manipulated oxygen concentrations in the range of 0.2–220?μmol?L?1 revealed a submicromolar oxygen optimum for MOx at the study site. In contrast, the fraction of methane–carbon incorporation into the bacterial biomass (compared to the total amount of oxidized methane) was up to 38-fold higher at saturated oxygen concentrations, suggesting a different partitioning of catabolic and anabolic processes under oxygen-replete and oxygen-starved conditions, respectively. Our results underscore the importance of MOx in mitigating methane emission from coastal waters and indicate an organism-level adaptation of the water column methanotrophs to hypoxic conditions.
机译:沿海海洋可能占全球海洋甲烷排放量的75多个。在那里,甲烷主要在缺氧沉积物中微生物生产,从中可以逸出到上覆的水柱。水柱中的有氧甲烷氧化(MOX)用作生物过滤器,减少最终蒸发到大气中的甲烷量。 MOX过滤器的效率可能通过溶解的甲烷和氧气以及温度,盐度和水文动力学来控制,以及所有这些因素在沿海生态系统中进行强烈的时间波动。为了阐明关键的环境管制,特别是氧气可用性的影响,对摩泽在季节性分层和缺氧沿海海洋环境中,我们进行了2年的时间序列研究,测量MOX和物理化学水柱参数西南波罗的海(Eckernf?RDE Bay)的沿海入口。我们发现Mox率通常朝向海底增加,但与甲烷浓度没有直接连接。 MOX在夏季分层期间表现出强烈的季节性变异性,最大速率(最多11.6?Nmol?1?1?1)当氧浓度最低,底水温度最高时。在这些条件下,甲烷氧化的2.4-19.0倍而不是发射到大气中,而在混合和含氧期间消耗和发射约相同的量。操纵氧浓度在0.2-220Ωμmolα1的实验室实验α1α1显示了在研究部位的MOX最佳的亚微粒摩尔氧。相反,甲烷 - 碳掺入到细菌生物量(与氧化甲烷的总量相比)在饱和氧浓度下高达38倍,表明在氧气 - 填充下的分解代谢和代谢过程的不同分配氧饥饿条件分别。我们的结果强调了MOX在沿海水域减轻甲烷排放的重要性,并表明水柱甲蛋白酶对缺氧条件的生物水平适应。

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