Liss, P. S., Malin, G. ORCID: https://orcid.org/0000-0002-3639-9215, Turner, S. M. and Holligan, P. (1994) Dimethyl sulphide and Phaeocystis: A review. Journal of Marine Systems, 5 (1). pp. 41-53.
Full text not available from this repository. (Request a copy)Abstract
Dimethyl sulphide (DMS) is the dominant sulphur gas found in surface marine waters and there is compelling evidence that it is formed biologically in these environments. In all areas so far investigated the oceans are found to be highly supersaturated (typically by two orders of magnitude) with respect to atmospheric levels of DMS, which indicates a net flux of the gas out of the oceans. In this paper, we first briefly review the environmental importance of the gas and particularly the role of its sea-to-air flux on atmospheric chemistry and physics. Then we discuss what is known of its mode of formation and cycling in seawater, before looking more specifically at the role and significance of Phaeocystis as a producer of DMS.
Item Type: | Article |
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Uncontrolled Keywords: | sdg 14 - life below water ,/dk/atira/pure/sustainabledevelopmentgoals/life_below_water |
Faculty \ School: | Faculty of Science > School of Environmental Sciences |
UEA Research Groups: | Faculty of Science > Research Groups > Climatic Research Unit Faculty of Science > Research Groups > Centre for Ocean and Atmospheric Sciences Faculty of Science > Research Groups > Marine and Atmospheric Sciences (former - to 2017) Faculty of Science > Research Groups > Climate, Ocean and Atmospheric Sciences (former - to 2017) Faculty of Science > Research Centres > Centre for Ecology, Evolution and Conservation Faculty of Science > Research Groups > Environmental Biology Faculty of Science > Research Groups > Resources, Sustainability and Governance (former - to 2018) |
Depositing User: | Rosie Cullington |
Date Deposited: | 07 Jun 2011 07:55 |
Last Modified: | 27 Mar 2024 17:30 |
URI: | https://ueaeprints.uea.ac.uk/id/eprint/31900 |
DOI: | 10.1016/0924-7963(94)90015-9 |
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