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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Main Authors: Burdett, H L, Carruthers, M, Donohue, P J C, Wicks, L C, Hennige, Sebastian J, Roberts, J Murray, Kamenos, N A
Format: Dataset
Language:English
Published: PANGAEA 2014
Subjects:
EXP
pH
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.835430
https://doi.org/10.1594/PANGAEA.835430
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.835430
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)