Effects of high temperature and CO2 on intracellular DMSP in the cold-water coral Lophelia pertusa
Significant warming and acidification of the oceans is projected to occur by the end of the century. CO2 vents, areas of upwelling and downwelling, and potential leaks from carbon capture and storage facilities may also cause localised environmental changes, enhancing or depressing the effect of glo...
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Format: | Dataset |
Language: | English |
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PANGAEA
2014
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.835430 https://doi.org/10.1594/PANGAEA.835430 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.835430 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Alkalinity total standard error Animalia Aragonite saturation state Benthic animals Benthos Bicarbonate ion Calcite saturation state Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Cnidaria Coast and continental shelf Containers and aquaria (20-1000 L or < 1 m**2) Dimethyl sulfide + dimethylsulfoniopropionate Dimethylsulfoniopropionate intracellular EXP Experiment Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Infrared spectrometric Laboratory experiment Lophelia pertusa Mingulay_Reef North Atlantic OA-ICC Ocean Acidification International Coordination Centre Other metabolic rates Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) pH Potentiometric titration Salinity |
spellingShingle |
Alkalinity total standard error Animalia Aragonite saturation state Benthic animals Benthos Bicarbonate ion Calcite saturation state Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Cnidaria Coast and continental shelf Containers and aquaria (20-1000 L or < 1 m**2) Dimethyl sulfide + dimethylsulfoniopropionate Dimethylsulfoniopropionate intracellular EXP Experiment Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Infrared spectrometric Laboratory experiment Lophelia pertusa Mingulay_Reef North Atlantic OA-ICC Ocean Acidification International Coordination Centre Other metabolic rates Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) pH Potentiometric titration Salinity Burdett, H L Carruthers, M Donohue, P J C Wicks, L C Hennige, Sebastian J Roberts, J Murray Kamenos, N A Effects of high temperature and CO2 on intracellular DMSP in the cold-water coral Lophelia pertusa |
topic_facet |
Alkalinity total standard error Animalia Aragonite saturation state Benthic animals Benthos Bicarbonate ion Calcite saturation state Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Cnidaria Coast and continental shelf Containers and aquaria (20-1000 L or < 1 m**2) Dimethyl sulfide + dimethylsulfoniopropionate Dimethylsulfoniopropionate intracellular EXP Experiment Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Infrared spectrometric Laboratory experiment Lophelia pertusa Mingulay_Reef North Atlantic OA-ICC Ocean Acidification International Coordination Centre Other metabolic rates Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) pH Potentiometric titration Salinity |
description |
Significant warming and acidification of the oceans is projected to occur by the end of the century. CO2 vents, areas of upwelling and downwelling, and potential leaks from carbon capture and storage facilities may also cause localised environmental changes, enhancing or depressing the effect of global climate change. Cold-water coral ecosystems are threatened by future changes in carbonate chemistry, yet our knowledge of the response of these corals to high temperature and high CO2 conditions is limited. Dimethylsulphoniopropionate (DMSP), and its breakdown product dimethylsulphide (DMS), are putative antioxidants that may be accumulated by invertebrates via their food or symbionts, although recent research suggests that some invertebrates may also be able to synthesise DMSP. This study provides the first information on the impact of high temperature (12 °C) and high CO2 (817 ppm) on intracellular DMSP in the cold-water coral Lophelia pertusa from the Mingulay Reef Complex, Scotland (56°49' N, 07°23' W), where in situ environmental conditions are meditated by tidally induced downwellings. An increase in intracellular DMSP under high CO2 conditions was observed, whilst water column particulate DMS + DMSP was reduced. In both high temperature treatments, intracellular DMSP was similar to the control treatment, whilst dissolved DMSP + DMS was not significantly different between any of the treatments. These results suggest that L. pertusa accumulates DMSP from the surrounding water column; uptake may be up-regulated under high CO2 conditions, but mediated by high temperature. These results provide new insight into the biotic control of deep-sea biogeochemistry and may impact our understanding of the global sulphur cycle, and the survival of cold-water corals under projected global change. |
format |
Dataset |
author |
Burdett, H L Carruthers, M Donohue, P J C Wicks, L C Hennige, Sebastian J Roberts, J Murray Kamenos, N A |
author_facet |
Burdett, H L Carruthers, M Donohue, P J C Wicks, L C Hennige, Sebastian J Roberts, J Murray Kamenos, N A |
author_sort |
Burdett, H L |
title |
Effects of high temperature and CO2 on intracellular DMSP in the cold-water coral Lophelia pertusa |
title_short |
Effects of high temperature and CO2 on intracellular DMSP in the cold-water coral Lophelia pertusa |
title_full |
Effects of high temperature and CO2 on intracellular DMSP in the cold-water coral Lophelia pertusa |
title_fullStr |
Effects of high temperature and CO2 on intracellular DMSP in the cold-water coral Lophelia pertusa |
title_full_unstemmed |
Effects of high temperature and CO2 on intracellular DMSP in the cold-water coral Lophelia pertusa |
title_sort |
effects of high temperature and co2 on intracellular dmsp in the cold-water coral lophelia pertusa |
publisher |
PANGAEA |
publishDate |
2014 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.835430 https://doi.org/10.1594/PANGAEA.835430 |
op_coverage |
LATITUDE: 56.816670 * LONGITUDE: -7.383330 * DATE/TIME START: 2012-07-01T00:00:00 * DATE/TIME END: 2012-07-30T00:00:00 |
long_lat |
ENVELOPE(-7.383330,-7.383330,56.816670,56.816670) |
genre |
Lophelia pertusa North Atlantic Ocean acidification |
genre_facet |
Lophelia pertusa North Atlantic Ocean acidification |
op_relation |
Burdett, H L; Carruthers, M; Donohue, P J C; Wicks, L C; Hennige, Sebastian J; Roberts, J Murray; Kamenos, N A (2014): Effects of high temperature and CO2 on intracellular DMSP in the cold-water coral Lophelia pertusa. Marine Biology, 161(7), 1499-1506, https://doi.org/10.1007/s00227-014-2435-5 Burdett, H L; Carruthers, M; Donohue, P J C; Wicks, L C; Hennige, Sebastian; Roberts, J Murray; Kamenos, N A (2014): Impacts of increased CO2 and temperature upon DMSP production in the cold-water coral, Lophelia pertusa, from short-term experiments carried out on cruise D366/7 [dataset]. British Oceanographic Data Centre, Natural Environment Research Council, https://doi.org/10.5285/f1a75a9f-95c9-57c1-e044-000b5de50f38 UKOA project Theme C (URI: https://www.bodc.ac.uk/data/documents/nodb/226210/) Lavigne, Héloïse; Epitalon, Jean-Marie; Gattuso, Jean-Pierre (2014): seacarb: seawater carbonate chemistry with R. R package version 3.0 [webpage]. https://cran.r-project.org/package=seacarb https://doi.pangaea.de/10.1594/PANGAEA.835430 https://doi.org/10.1594/PANGAEA.835430 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.83543010.1007/s00227-014-2435-510.5285/f1a75a9f-95c9-57c1-e044-000b5de50f38 |
_version_ |
1810456153574866944 |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.835430 2024-09-15T18:18:01+00:00 Effects of high temperature and CO2 on intracellular DMSP in the cold-water coral Lophelia pertusa Burdett, H L Carruthers, M Donohue, P J C Wicks, L C Hennige, Sebastian J Roberts, J Murray Kamenos, N A LATITUDE: 56.816670 * LONGITUDE: -7.383330 * DATE/TIME START: 2012-07-01T00:00:00 * DATE/TIME END: 2012-07-30T00:00:00 2014 text/tab-separated-values, 1114 data points https://doi.pangaea.de/10.1594/PANGAEA.835430 https://doi.org/10.1594/PANGAEA.835430 en eng PANGAEA Burdett, H L; Carruthers, M; Donohue, P J C; Wicks, L C; Hennige, Sebastian J; Roberts, J Murray; Kamenos, N A (2014): Effects of high temperature and CO2 on intracellular DMSP in the cold-water coral Lophelia pertusa. Marine Biology, 161(7), 1499-1506, https://doi.org/10.1007/s00227-014-2435-5 Burdett, H L; Carruthers, M; Donohue, P J C; Wicks, L C; Hennige, Sebastian; Roberts, J Murray; Kamenos, N A (2014): Impacts of increased CO2 and temperature upon DMSP production in the cold-water coral, Lophelia pertusa, from short-term experiments carried out on cruise D366/7 [dataset]. British Oceanographic Data Centre, Natural Environment Research Council, https://doi.org/10.5285/f1a75a9f-95c9-57c1-e044-000b5de50f38 UKOA project Theme C (URI: https://www.bodc.ac.uk/data/documents/nodb/226210/) Lavigne, Héloïse; Epitalon, Jean-Marie; Gattuso, Jean-Pierre (2014): seacarb: seawater carbonate chemistry with R. R package version 3.0 [webpage]. https://cran.r-project.org/package=seacarb https://doi.pangaea.de/10.1594/PANGAEA.835430 https://doi.org/10.1594/PANGAEA.835430 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Alkalinity total standard error Animalia Aragonite saturation state Benthic animals Benthos Bicarbonate ion Calcite saturation state Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Cnidaria Coast and continental shelf Containers and aquaria (20-1000 L or < 1 m**2) Dimethyl sulfide + dimethylsulfoniopropionate Dimethylsulfoniopropionate intracellular EXP Experiment Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Infrared spectrometric Laboratory experiment Lophelia pertusa Mingulay_Reef North Atlantic OA-ICC Ocean Acidification International Coordination Centre Other metabolic rates Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) pH Potentiometric titration Salinity dataset 2014 ftpangaea https://doi.org/10.1594/PANGAEA.83543010.1007/s00227-014-2435-510.5285/f1a75a9f-95c9-57c1-e044-000b5de50f38 2024-07-24T02:31:32Z Significant warming and acidification of the oceans is projected to occur by the end of the century. CO2 vents, areas of upwelling and downwelling, and potential leaks from carbon capture and storage facilities may also cause localised environmental changes, enhancing or depressing the effect of global climate change. Cold-water coral ecosystems are threatened by future changes in carbonate chemistry, yet our knowledge of the response of these corals to high temperature and high CO2 conditions is limited. Dimethylsulphoniopropionate (DMSP), and its breakdown product dimethylsulphide (DMS), are putative antioxidants that may be accumulated by invertebrates via their food or symbionts, although recent research suggests that some invertebrates may also be able to synthesise DMSP. This study provides the first information on the impact of high temperature (12 °C) and high CO2 (817 ppm) on intracellular DMSP in the cold-water coral Lophelia pertusa from the Mingulay Reef Complex, Scotland (56°49' N, 07°23' W), where in situ environmental conditions are meditated by tidally induced downwellings. An increase in intracellular DMSP under high CO2 conditions was observed, whilst water column particulate DMS + DMSP was reduced. In both high temperature treatments, intracellular DMSP was similar to the control treatment, whilst dissolved DMSP + DMS was not significantly different between any of the treatments. These results suggest that L. pertusa accumulates DMSP from the surrounding water column; uptake may be up-regulated under high CO2 conditions, but mediated by high temperature. These results provide new insight into the biotic control of deep-sea biogeochemistry and may impact our understanding of the global sulphur cycle, and the survival of cold-water corals under projected global change. Dataset Lophelia pertusa North Atlantic Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-7.383330,-7.383330,56.816670,56.816670) |