Sources and transformation processes of biogenic active gases in the ocean

Yang Guipeng; Zhang Honghai

doi:10.3969/j.issn.0253-4193.2018.10.002

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Yang Guipeng, Zhang Honghai. Sources and transformation processes of biogenic active gases in the ocean[J]. Haiyang Xuebao, 2018, 40(10): 14-21. doi: 10.3969/j.issn.0253-4193.2018.10.002

Citation:

Yang Guipeng, Zhang Honghai. Sources and transformation processes of biogenic active gases in the ocean[J]. Haiyang Xuebao, 2018, 40(10): 14-21. doi: 10.3969/j.issn.0253-4193.2018.10.002

Yang Guipeng, Zhang Honghai. Sources and transformation processes of biogenic active gases in the ocean[J]. Haiyang Xuebao, 2018, 40(10): 14-21. doi: 10.3969/j.issn.0253-4193.2018.10.002

Citation:

Yang Guipeng, Zhang Honghai. Sources and transformation processes of biogenic active gases in the ocean[J]. Haiyang Xuebao, 2018, 40(10): 14-21. doi: 10.3969/j.issn.0253-4193.2018.10.002

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Sources and transformation processes of biogenic active gases in the ocean

doi: 10.3969/j.issn.0253-4193.2018.10.002

College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China;Marine Ecology and Environmental Science Laboratory, Pilot National Laboratory for Marine Science and Technology(Qingdao), Qingdao 266237, China

Received Date: 2018-04-30
Rev Recd Date: 2018-06-29

Abstract

Abstract

Marine biogenic active gases mainly include dimethylsulfide (DMS), methane (CH₄), nitrous oxide (N₂O), carbon monoxide (CO), volatile halocarbons (VHCs) and non-methane hydrocarbons (NMHCs). These biogenic active gases are released into the atmosphere through the air-sea exchange and play critical roles not only in global cycling of carbon, nitrogen and sulfur but also in the direct and indirect influences on the climate and environmental changes. Some marine biogenic active gases belong to greenhouse gases (CH₄, N₂O, VHCs and CO), and others would participate in chemical reactions in the atmosphere and control atmospheric chemical equilibrium and ozone concentration (VHCs and NMHCs). By contrast, DMS is a negative greenhouse effect gas. It will be rapidly oxidized to produce sulfate aerosol in the atmosphere and influence cloudy formation and the Earth's radiative budget. The present research status of marine biogenic active gases is reviewed and the sources and sinks, sea-to-air fluxes of DMS, CH₄ and N₂O as well as their influencing factors are summarized. Finally, some problems existing in the field and future research directions are presented.
- marine biogenic active gas,
- biogeochemical process,
- migration and transformation,
- sea-to-air flux,
- China coastal seas

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