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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Bibliographic Details
Main Authors: Carey, Nicholas, Harianto, Januar, Byrne, Maria
Format: Dataset
Language:English
Published: PANGAEA 2016
Subjects:
EXP
pH
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.860079
https://doi.org/10.1594/PANGAEA.860079
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.860079
record_format openpolar
institution 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)