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天然气水合物分解的甲烷对海洋生物的影响
引用本文:郭子豪,李灿苹,陈凤英,勾丽敏,汪洪涛,曾宪军,刘一林,田鑫裕.天然气水合物分解的甲烷对海洋生物的影响[J].现代地质,2023,37(1):138-152.
作者姓名:郭子豪  李灿苹  陈凤英  勾丽敏  汪洪涛  曾宪军  刘一林  田鑫裕
作者单位:1.广东海洋大学电子与信息工程学院,广东 湛江 5240882.中国地质大学(北京) 海洋学院,北京 1000833.中油测井天津分公司解释评价中心,天津 3004574.广州海洋地质调查局,广东 广州 510075
基金项目:国家重点研发计划资助项目“天然气水合物勘查开发技术联合研究”(2018YFE0208200);广东海洋大学“创新强校工程”特色创新项目(230419096);湛江市创新创业团队引育“领航计划”项目(211207157080994);国家自然科学基金项目(41306050)
摘    要:随着海底环境的变化以及全球变暖的加剧,天然气水合物分解释放出大量甲烷到海洋中,其中一部分甲烷会穿过海水释放到大气中,导致大气中的温室气体增加,从而加剧了全球暖化。本文从甲烷的释放和运移路径角度梳理和总结了甲烷对海洋生物的直接和间接影响。首先,水合物分解释放甲烷,在海底形成冷泉渗漏区,滋养了一批特殊的生物群落,而甲烷是其形成生命元素中不可或缺的要素,由此繁衍形成了冷泉生态系统。其次,甲烷释放到海水中会引起海水酸化,海水酸化不仅会导致钙化生物合成碳酸钙外壳受阻,还会加速已生成外壳的溶解。最后,甲烷作为强温室气体释放到大气中还会加剧全球变暖;此外,极地冻土层的融化也会使得冻土区天然气水合物分解,导致大量甲烷进入大气中,从而致使海水暖化,海水的暖化又会对海洋生物的生存、代谢、繁殖、发育和免疫应答等多种生命活动造成影响。以上认识为进一步研究甲烷对未来海洋生态系统的影响提供重要参考信息。

关 键 词:天然气水合物  甲烷  海洋生物  海洋酸化  海洋暖化
收稿时间:2022-04-12
修稿时间:2022-09-30

Effect of Methane from Natural Gas Hydrate Decomposition on Marine Life
GUO Zihao,LI Canping,CHEN Fengying,GOU Limin,WANG Hongtao,ZENG Xianjun,LIU Yilin,TIAN Xinyu.Effect of Methane from Natural Gas Hydrate Decomposition on Marine Life[J].Geoscience——Journal of Graduate School,China University of Geosciences,2023,37(1):138-152.
Authors:GUO Zihao  LI Canping  CHEN Fengying  GOU Limin  WANG Hongtao  ZENG Xianjun  LIU Yilin  TIAN Xinyu
Institution:1. School of Electronics and Information Engineering, Guangdong Ocean University, Zhanjiang, Guangdong 524088, China2. School of Ocean Sciences, China University of Geosciences, Beijing 100083, China3. The Interpretation and Evaluation Center of CNLC Tianjin Branch, Tianjin 300457, China4. Guangzhou Marine Geological Survey, Guangzhou, Guangdong 510075, China
Abstract:With changing seabed environment and the intensification of global warming, more natural gas hydrates have decomposed and released large amount of methane into the oceans. Some of the methane would ascend through the seawater and enter the atmosphere, which would increase the atmospheric greenhouse gas concentration, and thereby exacerbate global warming. From the perspective of methane release and migration pathways, the direct/indirect effects of methane on marine life are elucidated and summarized: (1) hydrates decompose to release methane, which is an indispensable compound in lifeform formation. This provides energy and material for autotrophic microorganisms, and supplies the food base of cold-spring biota. This maintains cold-spring biota based on a food chain of chemoautotrophic bacteria, which multiply in the cold-spring ecosystem; (2) some of the methane gas would diffuse and dissolve in the seawater, which causes seawater acidification. Seawater acidification would both affect the biosynthesis of calcium carbonate shells (calcification) and accelerate the shell dissolution; (3) as a strong greenhouse gas, the released methane in the atmosphere would exacerbate global warming. In addition, the melting of the polar permafrost would also release large amount of methane into the atmosphere, which generates an adverse cycle. The warming of seawater would affect the survival, metabolism, reproduction, development and immune response of marine life and other biological activities. Our findings provide important reference for future research on the impact of methane on marine ecosystem.
Keywords:natural gas hydrate  methane  marine life  ocean acidification  ocean warming  
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