Effects of Temperature and Light on Methane Production of Widespread Marine Phytoplankton
Methane (CH4) production in the ocean surface mixed layer is a widespread but still largely unexplained phenomenon. In this context marine algae have recently been described as a possible source of CH4 in surface waters. In the present study we investigated the effects of temperature and light inten...
| Autores: | , , , , , , |
|---|---|
| Tipo de recurso: | artículo |
| Fecha de publicación: | 2020 |
| País: | España |
| Institución: | Universitat Autònoma de Barcelona |
| Repositorio: | Dipòsit Digital de Documents de la UAB |
| Idioma: | inglés |
| OAI Identifier: | oai:ddd.uab.cat:293440 |
| Acceso en línea: | https://ddd.uab.cat/record/293440 https://dx.doi.org/urn:doi:10.1029/2020JG005793 |
| Access Level: | acceso abierto |
| Palabra clave: | SDG 14 - Life Below Water |
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Effects of Temperature and Light on Methane Production of Widespread Marine PhytoplanktonKlintzsch, Thomas|||0000-0002-0006-2944Langer, Gerald|||0000-0002-7211-4889Wieland, Anna|||0000-0001-7483-8170Geisinger, HannaLenhart, Katharina|||0000-0001-5226-492XNehrke, Gernot|||0000-0002-2851-3049Keppler, Frank|||0000-0003-2766-8812SDG 14 - Life Below WaterMethane (CH4) production in the ocean surface mixed layer is a widespread but still largely unexplained phenomenon. In this context marine algae have recently been described as a possible source of CH4 in surface waters. In the present study we investigated the effects of temperature and light intensity (including daylength) on CH4 formation from three widespread marine algal species Emiliania huxleyi, Phaeocystis globosa, and Chrysochromulina sp. Rates of E. huxleyi increased by 210% when temperature increased in a range from 10°C to 21.5°C, while a further increase in temperature (up to 23.8°C) showed reduction of CH4 production rates. Our results clearly showed that CH4 formation of E. huxleyi is controlled by light: When light intensity increased from 30 to 2,670 μmol m-2 s-1, CH4 emission rates increased continuously by almost 1 order of magnitude and was more than 1 order of magnitude higher when the daylength (light period) was extended from 6/18 hr light-dark cycle to continuous light. Furthermore, light intensity is also an important factor controlling CH4 emissions of Chrysochromulina sp. and P. globosa and could therefore be a species-independent regulator of phytoplankton CH4 production. Based on our results, we might conclude that extensive blooms of E. huxleyi could act as a main regional source of CH4 in surface water, since blooming of E. huxleyi is related to the seasonal increase in both light and temperature, which also stimulate CH4 production. Under typical global change scenarios, E. huxleyi will increase its CH4 production in the future. 22020-01-0120202020-01-01Articlehttp://purl.org/coar/resource_type/c_6501VoRhttp://purl.org/coar/version/c_970fb48d4fbd8a85info:eu-repo/semantics/articleapplication/pdfhttps://ddd.uab.cat/record/293440https://dx.doi.org/urn:doi:10.1029/2020JG005793reponame:Dipòsit Digital de Documents de la UABinstname:Universitat Autònoma de BarcelonaInglésengopen accesshttp://purl.org/coar/access_right/c_abf2Aquest document està subjecte a una llicència d'ús Creative Commons. Es permet la reproducció total o parcial, la distribució, la comunicació pública de l'obra i la creació d'obres derivades, fins i tot amb finalitats comercials, sempre i quan es reconegui l'autoria de l'obra original.https://creativecommons.org/licenses/by/4.0/info:eu-repo/semantics/openAccessoai:ddd.uab.cat:2934402026-06-06T12:50:31Z |
| dc.title.none.fl_str_mv |
Effects of Temperature and Light on Methane Production of Widespread Marine Phytoplankton |
| title |
Effects of Temperature and Light on Methane Production of Widespread Marine Phytoplankton |
| spellingShingle |
Effects of Temperature and Light on Methane Production of Widespread Marine Phytoplankton Klintzsch, Thomas|||0000-0002-0006-2944 SDG 14 - Life Below Water |
| title_short |
Effects of Temperature and Light on Methane Production of Widespread Marine Phytoplankton |
| title_full |
Effects of Temperature and Light on Methane Production of Widespread Marine Phytoplankton |
| title_fullStr |
Effects of Temperature and Light on Methane Production of Widespread Marine Phytoplankton |
| title_full_unstemmed |
Effects of Temperature and Light on Methane Production of Widespread Marine Phytoplankton |
| title_sort |
Effects of Temperature and Light on Methane Production of Widespread Marine Phytoplankton |
| dc.creator.none.fl_str_mv |
Klintzsch, Thomas|||0000-0002-0006-2944 Langer, Gerald|||0000-0002-7211-4889 Wieland, Anna|||0000-0001-7483-8170 Geisinger, Hanna Lenhart, Katharina|||0000-0001-5226-492X Nehrke, Gernot|||0000-0002-2851-3049 Keppler, Frank|||0000-0003-2766-8812 |
| author |
Klintzsch, Thomas|||0000-0002-0006-2944 |
| author_facet |
Klintzsch, Thomas|||0000-0002-0006-2944 Langer, Gerald|||0000-0002-7211-4889 Wieland, Anna|||0000-0001-7483-8170 Geisinger, Hanna Lenhart, Katharina|||0000-0001-5226-492X Nehrke, Gernot|||0000-0002-2851-3049 Keppler, Frank|||0000-0003-2766-8812 |
| author_role |
author |
| author2 |
Langer, Gerald|||0000-0002-7211-4889 Wieland, Anna|||0000-0001-7483-8170 Geisinger, Hanna Lenhart, Katharina|||0000-0001-5226-492X Nehrke, Gernot|||0000-0002-2851-3049 Keppler, Frank|||0000-0003-2766-8812 |
| author2_role |
author author author author author author |
| dc.subject.none.fl_str_mv |
SDG 14 - Life Below Water |
| topic |
SDG 14 - Life Below Water |
| description |
Methane (CH4) production in the ocean surface mixed layer is a widespread but still largely unexplained phenomenon. In this context marine algae have recently been described as a possible source of CH4 in surface waters. In the present study we investigated the effects of temperature and light intensity (including daylength) on CH4 formation from three widespread marine algal species Emiliania huxleyi, Phaeocystis globosa, and Chrysochromulina sp. Rates of E. huxleyi increased by 210% when temperature increased in a range from 10°C to 21.5°C, while a further increase in temperature (up to 23.8°C) showed reduction of CH4 production rates. Our results clearly showed that CH4 formation of E. huxleyi is controlled by light: When light intensity increased from 30 to 2,670 μmol m-2 s-1, CH4 emission rates increased continuously by almost 1 order of magnitude and was more than 1 order of magnitude higher when the daylength (light period) was extended from 6/18 hr light-dark cycle to continuous light. Furthermore, light intensity is also an important factor controlling CH4 emissions of Chrysochromulina sp. and P. globosa and could therefore be a species-independent regulator of phytoplankton CH4 production. Based on our results, we might conclude that extensive blooms of E. huxleyi could act as a main regional source of CH4 in surface water, since blooming of E. huxleyi is related to the seasonal increase in both light and temperature, which also stimulate CH4 production. Under typical global change scenarios, E. huxleyi will increase its CH4 production in the future. |
| publishDate |
2020 |
| dc.date.none.fl_str_mv |
2 2020-01-01 2020 2020-01-01 |
| dc.type.none.fl_str_mv |
Article http://purl.org/coar/resource_type/c_6501 VoR http://purl.org/coar/version/c_970fb48d4fbd8a85 |
| dc.type.openaire.fl_str_mv |
info:eu-repo/semantics/article |
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article |
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https://ddd.uab.cat/record/293440 https://dx.doi.org/urn:doi:10.1029/2020JG005793 |
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https://ddd.uab.cat/record/293440 https://dx.doi.org/urn:doi:10.1029/2020JG005793 |
| dc.language.none.fl_str_mv |
Inglés eng |
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Inglés |
| language |
eng |
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open access http://purl.org/coar/access_right/c_abf2 https://creativecommons.org/licenses/by/4.0/ |
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info:eu-repo/semantics/openAccess |
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open access http://purl.org/coar/access_right/c_abf2 https://creativecommons.org/licenses/by/4.0/ |
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openAccess |
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application/pdf |
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reponame:Dipòsit Digital de Documents de la UAB instname:Universitat Autònoma de Barcelona |
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Universitat Autònoma de Barcelona |
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