Contrasting effects of acidification and warming on dimethylsulfide 2 concentrations during a temperate estuarine fall bloom mesocosm 3 experiment
- Autores
- Benard, Robin; Ferreyra, Gustavo Adolfo; Michael, Scarratt; Sonia, Michaud; Michel, Starr; Alfonso, Mucci; Ferreyra, Gustavo Adolfo; Gosselin, Michel; Tremblay, Jean-Éric; Lizotte, Martine; Yang, Gui Peng
- Año de publicación
- 2018
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- The effects of ocean acidification and warming on the concentrations of dimethylsulfoniopropionate (DMSP) and dimethylsulfide (DMS) were investigated during a mesocosm experiment in the Lower St. Lawrence Estuary (LSLE) in the fall of 2014. Twelve mesocosms covering a range of pHT (pH on the total hydrogen ion concentration scale) from 8.0 to 7.2, corresponding to a range of CO2 partial pressures (pCO2) from 440 to 2900 μatm, at two temperatures (in situ and C5 °C; 10 and 15 °C) were monitored during 13 days. All mesocosms were characterized by the rapid development of a diatom bloom dominated by Skeletonema costatum, followed by its decline upon the exhaustion of nitrate and silicic acid. Neither the acidification nor the warming resulted in a significant impact on the abundance of bacteria over the experiment. However, warming the water by 5 °C resulted in a significant increase in the average bacterial production (BP) in all 15 °C mesocosms as compared to 10 °C, with no detectable effect of pCO2 on BP. Variations in total DMSP (DMSPt DparticulateCdissolved DMSP) concentrations tracked the development of the bloom, although the rise in DMSPt persisted for a few days after the peaks in chlorophyll a. Average concentrations of DMSPt were not affected by acidification or warming. Initially low concentrations of DMS (< 1 nmol L-1) increased to reach peak values ranging from 30 to 130 nmol L-1 towards the end of the experiment. Increasing the pCO2 reduced the averaged DMS concentrations by 66%and 69%at 10 and 15 °C, respectively, over the duration of the experiment. On the other hand, a 5 °C warming increased DMS concentrations by an average of 240% as compared to in situ temperature, resulting in a positive offset of the adverse pCO2 impact. Significant positive correlations found between bacterial production and concentrations of DMS throughout our experiment point towards temperatureassociated enhancement of bacterial DMSP metabolism as a likely driver of the mitigating effect of warming on the negative impact of acidification on the net production of DMS in the LSLE and potentially the global ocean.
Fil: Benard, Robin. Laval University; Canadá
Fil: Ferreyra, Gustavo Adolfo. Laval University; Canadá
Fil: Michael, Scarratt. Maurice Lamontagne Institute, Fisheries And Oceans; Canadá
Fil: Sonia, Michaud. Maurice Lamontagne Institute, Fisheries And Oceans ; Canadá
Fil: Michel, Starr. Maurice Lamontagne Institute, Fisheries And Oceans; Canadá
Fil: Alfonso, Mucci. Université Mcgill; Canadá
Fil: Ferreyra, Gustavo Adolfo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina
Fil: Gosselin, Michel. Institut Des Sciences de la Mer de Rimouski; Canadá
Fil: Tremblay, Jean-Éric. Laval University; Canadá
Fil: Lizotte, Martine. Laval University; Canadá
Fil: Yang, Gui Peng. Ocean University; China - Materia
-
acidification
warming - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by/2.5/ar/
- Repositorio
.jpg)
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/127394
Ver los metadatos del registro completo
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Contrasting effects of acidification and warming on dimethylsulfide 2 concentrations during a temperate estuarine fall bloom mesocosm 3 experimentBenard, RobinFerreyra, Gustavo AdolfoMichael, ScarrattSonia, MichaudMichel, StarrAlfonso, MucciFerreyra, Gustavo AdolfoGosselin, MichelTremblay, Jean-ÉricLizotte, MartineYang, Gui Pengacidificationwarminghttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The effects of ocean acidification and warming on the concentrations of dimethylsulfoniopropionate (DMSP) and dimethylsulfide (DMS) were investigated during a mesocosm experiment in the Lower St. Lawrence Estuary (LSLE) in the fall of 2014. Twelve mesocosms covering a range of pHT (pH on the total hydrogen ion concentration scale) from 8.0 to 7.2, corresponding to a range of CO2 partial pressures (pCO2) from 440 to 2900 μatm, at two temperatures (in situ and C5 °C; 10 and 15 °C) were monitored during 13 days. All mesocosms were characterized by the rapid development of a diatom bloom dominated by Skeletonema costatum, followed by its decline upon the exhaustion of nitrate and silicic acid. Neither the acidification nor the warming resulted in a significant impact on the abundance of bacteria over the experiment. However, warming the water by 5 °C resulted in a significant increase in the average bacterial production (BP) in all 15 °C mesocosms as compared to 10 °C, with no detectable effect of pCO2 on BP. Variations in total DMSP (DMSPt DparticulateCdissolved DMSP) concentrations tracked the development of the bloom, although the rise in DMSPt persisted for a few days after the peaks in chlorophyll a. Average concentrations of DMSPt were not affected by acidification or warming. Initially low concentrations of DMS (< 1 nmol L-1) increased to reach peak values ranging from 30 to 130 nmol L-1 towards the end of the experiment. Increasing the pCO2 reduced the averaged DMS concentrations by 66%and 69%at 10 and 15 °C, respectively, over the duration of the experiment. On the other hand, a 5 °C warming increased DMS concentrations by an average of 240% as compared to in situ temperature, resulting in a positive offset of the adverse pCO2 impact. Significant positive correlations found between bacterial production and concentrations of DMS throughout our experiment point towards temperatureassociated enhancement of bacterial DMSP metabolism as a likely driver of the mitigating effect of warming on the negative impact of acidification on the net production of DMS in the LSLE and potentially the global ocean.Fil: Benard, Robin. Laval University; CanadáFil: Ferreyra, Gustavo Adolfo. Laval University; CanadáFil: Michael, Scarratt. Maurice Lamontagne Institute, Fisheries And Oceans; CanadáFil: Sonia, Michaud. Maurice Lamontagne Institute, Fisheries And Oceans ; CanadáFil: Michel, Starr. Maurice Lamontagne Institute, Fisheries And Oceans; CanadáFil: Alfonso, Mucci. Université Mcgill; CanadáFil: Ferreyra, Gustavo Adolfo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; ArgentinaFil: Gosselin, Michel. Institut Des Sciences de la Mer de Rimouski; CanadáFil: Tremblay, Jean-Éric. Laval University; CanadáFil: Lizotte, Martine. Laval University; CanadáFil: Yang, Gui Peng. Ocean University; ChinaCopernicus Publications2018-08info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/127394Benard, Robin; Ferreyra, Gustavo Adolfo; Michael, Scarratt; Sonia, Michaud; Michel, Starr; et al.; Contrasting effects of acidification and warming on dimethylsulfide 2 concentrations during a temperate estuarine fall bloom mesocosm 3 experiment; Copernicus Publications; Biogeosciences; 16; 6; 8-2018; 1167-11851726-41701726-4189CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://bg.copernicus.org/articles/16/1167/2019/info:eu-repo/semantics/altIdentifier/doi/10.5194/bg-16-1167-2019info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-11-26T08:50:23Zoai:ri.conicet.gov.ar:11336/127394instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-11-26 08:50:23.494CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
| dc.title.none.fl_str_mv |
Contrasting effects of acidification and warming on dimethylsulfide 2 concentrations during a temperate estuarine fall bloom mesocosm 3 experiment |
| title |
Contrasting effects of acidification and warming on dimethylsulfide 2 concentrations during a temperate estuarine fall bloom mesocosm 3 experiment |
| spellingShingle |
Contrasting effects of acidification and warming on dimethylsulfide 2 concentrations during a temperate estuarine fall bloom mesocosm 3 experiment Benard, Robin acidification warming |
| title_short |
Contrasting effects of acidification and warming on dimethylsulfide 2 concentrations during a temperate estuarine fall bloom mesocosm 3 experiment |
| title_full |
Contrasting effects of acidification and warming on dimethylsulfide 2 concentrations during a temperate estuarine fall bloom mesocosm 3 experiment |
| title_fullStr |
Contrasting effects of acidification and warming on dimethylsulfide 2 concentrations during a temperate estuarine fall bloom mesocosm 3 experiment |
| title_full_unstemmed |
Contrasting effects of acidification and warming on dimethylsulfide 2 concentrations during a temperate estuarine fall bloom mesocosm 3 experiment |
| title_sort |
Contrasting effects of acidification and warming on dimethylsulfide 2 concentrations during a temperate estuarine fall bloom mesocosm 3 experiment |
| dc.creator.none.fl_str_mv |
Benard, Robin Ferreyra, Gustavo Adolfo Michael, Scarratt Sonia, Michaud Michel, Starr Alfonso, Mucci Ferreyra, Gustavo Adolfo Gosselin, Michel Tremblay, Jean-Éric Lizotte, Martine Yang, Gui Peng |
| author |
Benard, Robin |
| author_facet |
Benard, Robin Ferreyra, Gustavo Adolfo Michael, Scarratt Sonia, Michaud Michel, Starr Alfonso, Mucci Gosselin, Michel Tremblay, Jean-Éric Lizotte, Martine Yang, Gui Peng |
| author_role |
author |
| author2 |
Ferreyra, Gustavo Adolfo Michael, Scarratt Sonia, Michaud Michel, Starr Alfonso, Mucci Gosselin, Michel Tremblay, Jean-Éric Lizotte, Martine Yang, Gui Peng |
| author2_role |
author author author author author author author author author |
| dc.subject.none.fl_str_mv |
acidification warming |
| topic |
acidification warming |
| purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
| dc.description.none.fl_txt_mv |
The effects of ocean acidification and warming on the concentrations of dimethylsulfoniopropionate (DMSP) and dimethylsulfide (DMS) were investigated during a mesocosm experiment in the Lower St. Lawrence Estuary (LSLE) in the fall of 2014. Twelve mesocosms covering a range of pHT (pH on the total hydrogen ion concentration scale) from 8.0 to 7.2, corresponding to a range of CO2 partial pressures (pCO2) from 440 to 2900 μatm, at two temperatures (in situ and C5 °C; 10 and 15 °C) were monitored during 13 days. All mesocosms were characterized by the rapid development of a diatom bloom dominated by Skeletonema costatum, followed by its decline upon the exhaustion of nitrate and silicic acid. Neither the acidification nor the warming resulted in a significant impact on the abundance of bacteria over the experiment. However, warming the water by 5 °C resulted in a significant increase in the average bacterial production (BP) in all 15 °C mesocosms as compared to 10 °C, with no detectable effect of pCO2 on BP. Variations in total DMSP (DMSPt DparticulateCdissolved DMSP) concentrations tracked the development of the bloom, although the rise in DMSPt persisted for a few days after the peaks in chlorophyll a. Average concentrations of DMSPt were not affected by acidification or warming. Initially low concentrations of DMS (< 1 nmol L-1) increased to reach peak values ranging from 30 to 130 nmol L-1 towards the end of the experiment. Increasing the pCO2 reduced the averaged DMS concentrations by 66%and 69%at 10 and 15 °C, respectively, over the duration of the experiment. On the other hand, a 5 °C warming increased DMS concentrations by an average of 240% as compared to in situ temperature, resulting in a positive offset of the adverse pCO2 impact. Significant positive correlations found between bacterial production and concentrations of DMS throughout our experiment point towards temperatureassociated enhancement of bacterial DMSP metabolism as a likely driver of the mitigating effect of warming on the negative impact of acidification on the net production of DMS in the LSLE and potentially the global ocean. Fil: Benard, Robin. Laval University; Canadá Fil: Ferreyra, Gustavo Adolfo. Laval University; Canadá Fil: Michael, Scarratt. Maurice Lamontagne Institute, Fisheries And Oceans; Canadá Fil: Sonia, Michaud. Maurice Lamontagne Institute, Fisheries And Oceans ; Canadá Fil: Michel, Starr. Maurice Lamontagne Institute, Fisheries And Oceans; Canadá Fil: Alfonso, Mucci. Université Mcgill; Canadá Fil: Ferreyra, Gustavo Adolfo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Austral de Investigaciones Científicas; Argentina Fil: Gosselin, Michel. Institut Des Sciences de la Mer de Rimouski; Canadá Fil: Tremblay, Jean-Éric. Laval University; Canadá Fil: Lizotte, Martine. Laval University; Canadá Fil: Yang, Gui Peng. Ocean University; China |
| description |
The effects of ocean acidification and warming on the concentrations of dimethylsulfoniopropionate (DMSP) and dimethylsulfide (DMS) were investigated during a mesocosm experiment in the Lower St. Lawrence Estuary (LSLE) in the fall of 2014. Twelve mesocosms covering a range of pHT (pH on the total hydrogen ion concentration scale) from 8.0 to 7.2, corresponding to a range of CO2 partial pressures (pCO2) from 440 to 2900 μatm, at two temperatures (in situ and C5 °C; 10 and 15 °C) were monitored during 13 days. All mesocosms were characterized by the rapid development of a diatom bloom dominated by Skeletonema costatum, followed by its decline upon the exhaustion of nitrate and silicic acid. Neither the acidification nor the warming resulted in a significant impact on the abundance of bacteria over the experiment. However, warming the water by 5 °C resulted in a significant increase in the average bacterial production (BP) in all 15 °C mesocosms as compared to 10 °C, with no detectable effect of pCO2 on BP. Variations in total DMSP (DMSPt DparticulateCdissolved DMSP) concentrations tracked the development of the bloom, although the rise in DMSPt persisted for a few days after the peaks in chlorophyll a. Average concentrations of DMSPt were not affected by acidification or warming. Initially low concentrations of DMS (< 1 nmol L-1) increased to reach peak values ranging from 30 to 130 nmol L-1 towards the end of the experiment. Increasing the pCO2 reduced the averaged DMS concentrations by 66%and 69%at 10 and 15 °C, respectively, over the duration of the experiment. On the other hand, a 5 °C warming increased DMS concentrations by an average of 240% as compared to in situ temperature, resulting in a positive offset of the adverse pCO2 impact. Significant positive correlations found between bacterial production and concentrations of DMS throughout our experiment point towards temperatureassociated enhancement of bacterial DMSP metabolism as a likely driver of the mitigating effect of warming on the negative impact of acidification on the net production of DMS in the LSLE and potentially the global ocean. |
| publishDate |
2018 |
| dc.date.none.fl_str_mv |
2018-08 |
| dc.type.none.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion http://purl.org/coar/resource_type/c_6501 info:ar-repo/semantics/articulo |
| format |
article |
| status_str |
publishedVersion |
| dc.identifier.none.fl_str_mv |
http://hdl.handle.net/11336/127394 Benard, Robin; Ferreyra, Gustavo Adolfo; Michael, Scarratt; Sonia, Michaud; Michel, Starr; et al.; Contrasting effects of acidification and warming on dimethylsulfide 2 concentrations during a temperate estuarine fall bloom mesocosm 3 experiment; Copernicus Publications; Biogeosciences; 16; 6; 8-2018; 1167-1185 1726-4170 1726-4189 CONICET Digital CONICET |
| url |
http://hdl.handle.net/11336/127394 |
| identifier_str_mv |
Benard, Robin; Ferreyra, Gustavo Adolfo; Michael, Scarratt; Sonia, Michaud; Michel, Starr; et al.; Contrasting effects of acidification and warming on dimethylsulfide 2 concentrations during a temperate estuarine fall bloom mesocosm 3 experiment; Copernicus Publications; Biogeosciences; 16; 6; 8-2018; 1167-1185 1726-4170 1726-4189 CONICET Digital CONICET |
| dc.language.none.fl_str_mv |
eng |
| language |
eng |
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info:eu-repo/semantics/altIdentifier/url/https://bg.copernicus.org/articles/16/1167/2019/ info:eu-repo/semantics/altIdentifier/doi/10.5194/bg-16-1167-2019 |
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info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/2.5/ar/ |
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openAccess |
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https://creativecommons.org/licenses/by/2.5/ar/ |
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application/pdf application/pdf |
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Copernicus Publications |
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Copernicus Publications |
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CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas |
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dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar |
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