Sea urchins in a high CO2 world: partitioned effects of body-size, ocean warming and acidification on metabolic rate
Body-size and temperature are the major factors explaining metabolic rate, and the additional factor of pH is a major driver at the biochemical level. These three factors have frequently been found to interact, complicating the formulation of broad models predicting metabolic rates and hence ecologi...
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Language: | English |
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PANGAEA
2016
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.860079 https://doi.org/10.1594/PANGAEA.860079 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.860079 |
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openpolar |
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Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Alkalinity total standard deviation Animalia Aragonite saturation state Ash free dry mass Behaviour Benthic animals Benthos Bicarbonate ion Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calculated using CO2calc Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Coast and continental shelf Diameter Echinodermata EXP Experiment Feeding rate Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Heliocidaris erythrogramma Identification Laboratory experiment Little_Bay OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) pH |
spellingShingle |
Alkalinity total standard deviation Animalia Aragonite saturation state Ash free dry mass Behaviour Benthic animals Benthos Bicarbonate ion Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calculated using CO2calc Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Coast and continental shelf Diameter Echinodermata EXP Experiment Feeding rate Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Heliocidaris erythrogramma Identification Laboratory experiment Little_Bay OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) pH Carey, Nicholas Harianto, Januar Byrne, Maria Sea urchins in a high CO2 world: partitioned effects of body-size, ocean warming and acidification on metabolic rate |
topic_facet |
Alkalinity total standard deviation Animalia Aragonite saturation state Ash free dry mass Behaviour Benthic animals Benthos Bicarbonate ion Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calculated using CO2calc Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Coast and continental shelf Diameter Echinodermata EXP Experiment Feeding rate Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Heliocidaris erythrogramma Identification Laboratory experiment Little_Bay OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) pH |
description |
Body-size and temperature are the major factors explaining metabolic rate, and the additional factor of pH is a major driver at the biochemical level. These three factors have frequently been found to interact, complicating the formulation of broad models predicting metabolic rates and hence ecological functioning. In this first study of the effects of warming and ocean acidification, and their potential interaction, on metabolic rate across a broad body-size range (two-to-three orders of magnitude difference in body mass) we addressed the impact of climate change on the sea urchin Heliocidaris erythrogramma in context with climate projections for east Australia, an ocean warming hotspot. Urchins were gradually introduced to two temperatures (18 and 23 °C) and two pH (7.5 and 8.0), and maintained for two months. That a new physiological steady-state had been reached, otherwise know as acclimation, was validated through identical experimental trials separated by several weeks. The relationship between body-size, temperature and acidification on the metabolic rate of H. erythrogramma was strikingly stable. Both stressors caused increases in metabolic rate; 20% for temperature and 19% for pH. Combined effects were additive; a 44% increase in metabolism. Body-size had a highly stable relationship with metabolic rate regardless of temperature or pH. None of these diverse drivers of metabolism interacted or modulated the effects of the others, highlighting the partitioned nature of how each influences metabolic rate, and the importance of achieving a full acclimation state. Despite these increases in energetic demand there was very limited capacity for compensatory modulating of feeding rate; food consumption increased only in the very smallest specimens, and only in response to temperature, and not pH. Our data show that warming, acidification and body-size all substantially affect metabolism and are highly consistent and partitioned in their effects, and for H. erythrogramma near-future climate change will incur a ... |
format |
Dataset |
author |
Carey, Nicholas Harianto, Januar Byrne, Maria |
author_facet |
Carey, Nicholas Harianto, Januar Byrne, Maria |
author_sort |
Carey, Nicholas |
title |
Sea urchins in a high CO2 world: partitioned effects of body-size, ocean warming and acidification on metabolic rate |
title_short |
Sea urchins in a high CO2 world: partitioned effects of body-size, ocean warming and acidification on metabolic rate |
title_full |
Sea urchins in a high CO2 world: partitioned effects of body-size, ocean warming and acidification on metabolic rate |
title_fullStr |
Sea urchins in a high CO2 world: partitioned effects of body-size, ocean warming and acidification on metabolic rate |
title_full_unstemmed |
Sea urchins in a high CO2 world: partitioned effects of body-size, ocean warming and acidification on metabolic rate |
title_sort |
sea urchins in a high co2 world: partitioned effects of body-size, ocean warming and acidification on metabolic rate |
publisher |
PANGAEA |
publishDate |
2016 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.860079 https://doi.org/10.1594/PANGAEA.860079 |
op_coverage |
LATITUDE: -33.966670 * LONGITUDE: 151.250000 * DATE/TIME START: 2014-06-01T00:00:00 * DATE/TIME END: 2014-06-30T00:00:00 |
long_lat |
ENVELOPE(151.250000,151.250000,-33.966670,-33.966670) |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_source |
Supplement to: Carey, Nicholas; Harianto, Januar; Byrne, Maria (2016): Sea urchins in a high-CO2 world: partitioned effects of body size, ocean warming and acidification on metabolic rate. Journal of Experimental Biology, 219(8), 1178-1186, https://doi.org/10.1242/jeb.136101 |
op_relation |
Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse (2015): seacarb: seawater carbonate chemistry with R. R package version 3.0.8. https://cran.r-project.org/package=seacarb https://doi.pangaea.de/10.1594/PANGAEA.860079 https://doi.org/10.1594/PANGAEA.860079 |
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.86007910.1242/jeb.136101 |
_version_ |
1810469547269947392 |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.860079 2024-09-15T18:28:13+00:00 Sea urchins in a high CO2 world: partitioned effects of body-size, ocean warming and acidification on metabolic rate Carey, Nicholas Harianto, Januar Byrne, Maria LATITUDE: -33.966670 * LONGITUDE: 151.250000 * DATE/TIME START: 2014-06-01T00:00:00 * DATE/TIME END: 2014-06-30T00:00:00 2016 text/tab-separated-values, 3279 data points https://doi.pangaea.de/10.1594/PANGAEA.860079 https://doi.org/10.1594/PANGAEA.860079 en eng PANGAEA Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse (2015): seacarb: seawater carbonate chemistry with R. R package version 3.0.8. https://cran.r-project.org/package=seacarb https://doi.pangaea.de/10.1594/PANGAEA.860079 https://doi.org/10.1594/PANGAEA.860079 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Carey, Nicholas; Harianto, Januar; Byrne, Maria (2016): Sea urchins in a high-CO2 world: partitioned effects of body size, ocean warming and acidification on metabolic rate. Journal of Experimental Biology, 219(8), 1178-1186, https://doi.org/10.1242/jeb.136101 Alkalinity total standard deviation Animalia Aragonite saturation state Ash free dry mass Behaviour Benthic animals Benthos Bicarbonate ion Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calculated using CO2calc Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Coast and continental shelf Diameter Echinodermata EXP Experiment Feeding rate Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Heliocidaris erythrogramma Identification Laboratory experiment Little_Bay OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) pH dataset 2016 ftpangaea https://doi.org/10.1594/PANGAEA.86007910.1242/jeb.136101 2024-07-24T02:31:33Z Body-size and temperature are the major factors explaining metabolic rate, and the additional factor of pH is a major driver at the biochemical level. These three factors have frequently been found to interact, complicating the formulation of broad models predicting metabolic rates and hence ecological functioning. In this first study of the effects of warming and ocean acidification, and their potential interaction, on metabolic rate across a broad body-size range (two-to-three orders of magnitude difference in body mass) we addressed the impact of climate change on the sea urchin Heliocidaris erythrogramma in context with climate projections for east Australia, an ocean warming hotspot. Urchins were gradually introduced to two temperatures (18 and 23 °C) and two pH (7.5 and 8.0), and maintained for two months. That a new physiological steady-state had been reached, otherwise know as acclimation, was validated through identical experimental trials separated by several weeks. The relationship between body-size, temperature and acidification on the metabolic rate of H. erythrogramma was strikingly stable. Both stressors caused increases in metabolic rate; 20% for temperature and 19% for pH. Combined effects were additive; a 44% increase in metabolism. Body-size had a highly stable relationship with metabolic rate regardless of temperature or pH. None of these diverse drivers of metabolism interacted or modulated the effects of the others, highlighting the partitioned nature of how each influences metabolic rate, and the importance of achieving a full acclimation state. Despite these increases in energetic demand there was very limited capacity for compensatory modulating of feeding rate; food consumption increased only in the very smallest specimens, and only in response to temperature, and not pH. Our data show that warming, acidification and body-size all substantially affect metabolism and are highly consistent and partitioned in their effects, and for H. erythrogramma near-future climate change will incur a ... Dataset Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(151.250000,151.250000,-33.966670,-33.966670) |