Water mass mixing controls methane cycling and emission in highly hydrodynamic regions of the open ocean.

IF 6.1 Q1 ECOLOGY
ISME communications Pub Date : 2025-07-10 eCollection Date: 2025-01-01 DOI:10.1093/ismeco/ycaf114
Xiao-Jun Li, Jinyan Wang, Hao-Nan Wang, Shuang Li, Zhen Zhou, Zhao-Hui Chen, Jiarui Liu, Gui-Ling Zhang, Hong-Hai Zhang, Gui-Peng Yang, Jonathan D Todd, Guang-Chao Zhuang
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Abstract

Ocean circulations and water mass exchange can exert significant influences on seawater biogeochemistry, microbial communities, and carbon cycling in marine systems. However, the detailed mechanisms of the impacts of physical processes in the open ocean on the cycle of greenhouse gases, particularly methane, remain poorly understood. In this study, we integrated high-resolution underway observations, experimental incubations, radioisotope labelling, and molecular analysis to constrain the controls of methanogenic pathways, methanotrophic activity, and emission fluxes in the highly hydrodynamic Kuroshio and Oyashio Extension (KOE) region of the Northwest Pacific. The mixing of high-temperature, nutrient-rich Kuroshio waters with methane-rich Oyashio currents significantly affected not only methane abundance, but also methane production pathways and oxidation rates. Water mass mixing caused changes in the dominance of phytoplankton communities to Bacillariophyta, with less production of the methane precursor dimethylsulphoniopropionate, thus reducing dimethylsulphoniopropionate-dependent methanogenesis. The alteration of nutrient levels due to mixing of Kuroshio and Oyashio at KOE is also likely to affect microbial utilization of dissolved organic phosphorus, thus influencing methane production from the C-P cleavage of methylphosphonate. Furthermore, the abundances of methanotrophs, such as Methylocystis and Methylosinus, were much higher at the KOE sites than those observed at the Oyashio Extension, which contributed to elevated methane oxidation rates in the mixing region. Microbial oxidation as a biological sink of methane accounted for ~43.7% ± 28.8% of the total methane loss, which reduced methane emissions to the atmosphere. These data highlight the physical controls on biogeochemical methane cycling, indicating that intensive mixing of water masses may regulate methane emissions from the open oceans.

水团混合控制着开放海洋中高度水动力区域的甲烷循环和排放。
海洋环流和水团交换对海水生物地球化学、微生物群落和海洋系统碳循环具有重要影响。然而,对于开放海洋中物理过程对温室气体,特别是甲烷循环的影响的详细机制,人们仍然知之甚少。在这项研究中,我们综合了高分辨率的海上观测、实验孵化、放射性同位素标记和分子分析,以限制西北太平洋高流体动力学的黑潮和孤潮延伸区(KOE)的甲烷生成途径、甲烷营养活动和排放通量的控制。高温、富营养化的黑潮水体与富甲烷的潮流混合,不仅显著影响甲烷丰度,而且影响甲烷生成途径和氧化速率。水体质量混合改变了浮游植物群落对硅藻门的优势地位,减少了甲烷前体二甲基磺酰丙酸的产生,从而减少了依赖二甲基磺酰丙酸的甲烷生成。黑潮和重潮混合导致的营养水平变化也可能影响微生物对溶解有机磷的利用,从而影响甲基膦酸盐C-P裂解产生的甲烷。此外,KOE位点甲烷氧化菌(如Methylocystis和Methylosinus)的丰度远高于oyashhio伸展区,这导致混合区甲烷氧化速率升高。微生物氧化作为甲烷的生物汇占甲烷总损失的~43.7%±28.8%,减少了甲烷向大气的排放。这些数据强调了生物地球化学甲烷循环的物理控制,表明水体的强烈混合可能调节着开放海洋的甲烷排放。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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