Seawater carbonate chemistry and resource allocation and extracellular acid-base status in the sea urchin Strongylocentrotus droebachiensis during experiments, 2012

Anthropogenic CO2 emission will lead to an increase in seawater pCO2 of up to 80-100 Pa (800-1000 µatm) within this century and to an acidification of the oceans. Green sea urchins (Strongylocentrotus droebachiensis) occurring in Kattegat experience seasonal hypercapnic and hypoxic conditions alread...

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Main Authors: Stumpp, Meike, Trübenbach, Katja, Brennecke, Dennis, Hu, Marian Y, Melzner, Frank
Format: Dataset
Language:English
Published: PANGAEA 2012
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.779697
https://doi.org/10.1594/PANGAEA.779697
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.779697
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.779697 2023-05-15T17:51:16+02:00 Seawater carbonate chemistry and resource allocation and extracellular acid-base status in the sea urchin Strongylocentrotus droebachiensis during experiments, 2012 Stumpp, Meike Trübenbach, Katja Brennecke, Dennis Hu, Marian Y Melzner, Frank 2012-04-21 text/tab-separated-values, 489 data points https://doi.pangaea.de/10.1594/PANGAEA.779697 https://doi.org/10.1594/PANGAEA.779697 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.779697 https://doi.org/10.1594/PANGAEA.779697 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Stumpp, Meike; Trübenbach, Katja; Brennecke, Dennis; Hu, Marian Y; Melzner, Frank (2012): Resource allocation and extracellular acid-base status in the sea urchin Strongylocentrotus droebachiensis in response to CO2 induced seawater acidification. Aquatic Toxicology, 110-111, 194-207, https://doi.org/10.1016/j.aquatox.2011.12.020 Alkalinity total standard deviation Animalia Aragonite saturation state Behaviour Benthic animals Benthos Bicarbonate ion BIOACID Biological Impacts of Ocean Acidification Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calculated see reference(s) Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide partial pressure Coast and continental shelf Echinodermata ECO2 EPOCA EUR-OCEANS European network of excellence for Ocean Ecosystems Analysis European Project on Ocean Acidification Experimental treatment Flow rate Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Gonad stage developing Dataset 2012 ftpangaea https://doi.org/10.1594/PANGAEA.779697 https://doi.org/10.1016/j.aquatox.2011.12.020 2023-01-20T08:53:52Z Anthropogenic CO2 emission will lead to an increase in seawater pCO2 of up to 80-100 Pa (800-1000 µatm) within this century and to an acidification of the oceans. Green sea urchins (Strongylocentrotus droebachiensis) occurring in Kattegat experience seasonal hypercapnic and hypoxic conditions already today. Thus, anthropogenic CO2 emissions will add up to existing values and will lead to even higher pCO2 values >200 Pa (>2000 µatm). To estimate the green sea urchins' potential to acclimate to acidified seawater, we calculated an energy budget and determined the extracellular acid base status of adult S. droebachiensis exposed to moderately (102 to 145 Pa, 1007 to 1431 µatm) and highly (284 to 385 Pa, 2800 to 3800 µatm) elevated seawater pCO2 for 10 and 45 days. A 45 - day exposure to elevated pCO2 resulted in a shift in energy budgets, leading to reduced somatic and reproductive growth. Metabolic rates were not significantly affected, but ammonium excretion increased in response to elevated pCO2. This led to decreased O:N ratios. These findings suggest that protein metabolism is possibly enhanced under elevated pCO2 in order to support ion homeostasis by increasing net acid extrusion. The perivisceral coelomic fluid acid-base status revealed that S. droebachiensis is able to fully (intermediate pCO2) or partially (high pCO2) compensate extracellular pH (pHe) changes by accumulation of bicarbonate (maximum increases 2.5 mM), albeit at a slower rate than typically observed in other taxa (10 day duration for full pHe compensation). At intermediate pCO2, sea urchins were able to maintain fully compensated pHe for 45 days. Sea urchins from the higher pCO2 treatment could be divided into two groups following medium-term acclimation: one group of experimental animals (29%) contained remnants of food in their digestive system and maintained partially compensated pHe (+2.3 mM HCO3), while the other group (71%) exhibited an empty digestive system and a severe metabolic acidosis (-0.5 pH units, -2.4 mM HCO3). There ... Dataset Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science Kattegat ENVELOPE(9.692,9.692,63.563,63.563)
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
Behaviour
Benthic animals
Benthos
Bicarbonate ion
BIOACID
Biological Impacts of Ocean Acidification
Bottles or small containers/Aquaria (<20 L)
Calcite saturation state
Calculated
see reference(s)
Calculated using CO2SYS
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
Carbonate ion
Carbonate system computation flag
Carbon dioxide
partial pressure
Coast and continental shelf
Echinodermata
ECO2
EPOCA
EUR-OCEANS
European network of excellence for Ocean Ecosystems Analysis
European Project on Ocean Acidification
Experimental treatment
Flow rate
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Gonad stage
developing
spellingShingle Alkalinity
total
standard deviation
Animalia
Aragonite saturation state
Behaviour
Benthic animals
Benthos
Bicarbonate ion
BIOACID
Biological Impacts of Ocean Acidification
Bottles or small containers/Aquaria (<20 L)
Calcite saturation state
Calculated
see reference(s)
Calculated using CO2SYS
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
Carbonate ion
Carbonate system computation flag
Carbon dioxide
partial pressure
Coast and continental shelf
Echinodermata
ECO2
EPOCA
EUR-OCEANS
European network of excellence for Ocean Ecosystems Analysis
European Project on Ocean Acidification
Experimental treatment
Flow rate
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Gonad stage
developing
Stumpp, Meike
Trübenbach, Katja
Brennecke, Dennis
Hu, Marian Y
Melzner, Frank
Seawater carbonate chemistry and resource allocation and extracellular acid-base status in the sea urchin Strongylocentrotus droebachiensis during experiments, 2012
topic_facet Alkalinity
total
standard deviation
Animalia
Aragonite saturation state
Behaviour
Benthic animals
Benthos
Bicarbonate ion
BIOACID
Biological Impacts of Ocean Acidification
Bottles or small containers/Aquaria (<20 L)
Calcite saturation state
Calculated
see reference(s)
Calculated using CO2SYS
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
Carbonate ion
Carbonate system computation flag
Carbon dioxide
partial pressure
Coast and continental shelf
Echinodermata
ECO2
EPOCA
EUR-OCEANS
European network of excellence for Ocean Ecosystems Analysis
European Project on Ocean Acidification
Experimental treatment
Flow rate
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Gonad stage
developing
description Anthropogenic CO2 emission will lead to an increase in seawater pCO2 of up to 80-100 Pa (800-1000 µatm) within this century and to an acidification of the oceans. Green sea urchins (Strongylocentrotus droebachiensis) occurring in Kattegat experience seasonal hypercapnic and hypoxic conditions already today. Thus, anthropogenic CO2 emissions will add up to existing values and will lead to even higher pCO2 values >200 Pa (>2000 µatm). To estimate the green sea urchins' potential to acclimate to acidified seawater, we calculated an energy budget and determined the extracellular acid base status of adult S. droebachiensis exposed to moderately (102 to 145 Pa, 1007 to 1431 µatm) and highly (284 to 385 Pa, 2800 to 3800 µatm) elevated seawater pCO2 for 10 and 45 days. A 45 - day exposure to elevated pCO2 resulted in a shift in energy budgets, leading to reduced somatic and reproductive growth. Metabolic rates were not significantly affected, but ammonium excretion increased in response to elevated pCO2. This led to decreased O:N ratios. These findings suggest that protein metabolism is possibly enhanced under elevated pCO2 in order to support ion homeostasis by increasing net acid extrusion. The perivisceral coelomic fluid acid-base status revealed that S. droebachiensis is able to fully (intermediate pCO2) or partially (high pCO2) compensate extracellular pH (pHe) changes by accumulation of bicarbonate (maximum increases 2.5 mM), albeit at a slower rate than typically observed in other taxa (10 day duration for full pHe compensation). At intermediate pCO2, sea urchins were able to maintain fully compensated pHe for 45 days. Sea urchins from the higher pCO2 treatment could be divided into two groups following medium-term acclimation: one group of experimental animals (29%) contained remnants of food in their digestive system and maintained partially compensated pHe (+2.3 mM HCO3), while the other group (71%) exhibited an empty digestive system and a severe metabolic acidosis (-0.5 pH units, -2.4 mM HCO3). There ...
format Dataset
author Stumpp, Meike
Trübenbach, Katja
Brennecke, Dennis
Hu, Marian Y
Melzner, Frank
author_facet Stumpp, Meike
Trübenbach, Katja
Brennecke, Dennis
Hu, Marian Y
Melzner, Frank
author_sort Stumpp, Meike
title Seawater carbonate chemistry and resource allocation and extracellular acid-base status in the sea urchin Strongylocentrotus droebachiensis during experiments, 2012
title_short Seawater carbonate chemistry and resource allocation and extracellular acid-base status in the sea urchin Strongylocentrotus droebachiensis during experiments, 2012
title_full Seawater carbonate chemistry and resource allocation and extracellular acid-base status in the sea urchin Strongylocentrotus droebachiensis during experiments, 2012
title_fullStr Seawater carbonate chemistry and resource allocation and extracellular acid-base status in the sea urchin Strongylocentrotus droebachiensis during experiments, 2012
title_full_unstemmed Seawater carbonate chemistry and resource allocation and extracellular acid-base status in the sea urchin Strongylocentrotus droebachiensis during experiments, 2012
title_sort seawater carbonate chemistry and resource allocation and extracellular acid-base status in the sea urchin strongylocentrotus droebachiensis during experiments, 2012
publisher PANGAEA
publishDate 2012
url https://doi.pangaea.de/10.1594/PANGAEA.779697
https://doi.org/10.1594/PANGAEA.779697
long_lat ENVELOPE(9.692,9.692,63.563,63.563)
geographic Kattegat
geographic_facet Kattegat
genre Ocean acidification
genre_facet Ocean acidification
op_source Supplement to: Stumpp, Meike; Trübenbach, Katja; Brennecke, Dennis; Hu, Marian Y; Melzner, Frank (2012): Resource allocation and extracellular acid-base status in the sea urchin Strongylocentrotus droebachiensis in response to CO2 induced seawater acidification. Aquatic Toxicology, 110-111, 194-207, https://doi.org/10.1016/j.aquatox.2011.12.020
op_relation https://doi.pangaea.de/10.1594/PANGAEA.779697
https://doi.org/10.1594/PANGAEA.779697
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.779697
https://doi.org/10.1016/j.aquatox.2011.12.020
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