id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.830736
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.830736 2024-09-15T18:27:47+00:00 Ocean acidification induces budding in larval sea urchins Chan, Kit Yu Karen Grünbaum, Daniel Arnberg, Maj Thorndyke, Mike Dupont, Sam 2013 text/tab-separated-values, 2643 data points https://doi.pangaea.de/10.1594/PANGAEA.830736 https://doi.org/10.1594/PANGAEA.830736 en eng PANGAEA Lavigne, Héloïse; Gattuso, Jean-Pierre (2011): seacarb: seawater carbonate chemistry with R. R package version 2.4 [webpage]. https://cran.r-project.org/package=seacarb https://doi.pangaea.de/10.1594/PANGAEA.830736 https://doi.org/10.1594/PANGAEA.830736 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Chan, Kit Yu Karen; Grünbaum, Daniel; Arnberg, Maj; Thorndyke, Mike; Dupont, Sam (2012): Ocean acidification induces budding in larval sea urchins. Marine Biology, 160(8), 2129-2135, https://doi.org/10.1007/s00227-012-2103-6 Age Alkalinity total standard error Animalia Aragonite saturation state Benthic animals Benthos Bicarbonate ion Bottles or small containers/Aquaria (<20 L) 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 Coast and continental shelf Echinodermata ECO2 Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Identification Laboratory experiment North Pacific OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Particle density normalized Percentage pH Potentiometric dataset 2013 ftpangaea https://doi.org/10.1594/PANGAEA.83073610.1007/s00227-012-2103-6 2024-07-24T02:31:32Z Ocean acidification (OA), the reduction of ocean pH due to hydration of atmospheric CO2, is known to affect growth and survival of marine invertebrate larvae. Survival and transport of vulnerable planktonic larval stages play important roles in determining population dynamics and community structures in coastal ecosystems. Here, we show that larvae of the purple urchin, Strongylocentrotus purpuratus, underwent high-frequency budding (release of blastula-like particles) when exposed to elevated pCO2 level (>700 µatm). Budding was observed in >50 % of the population and was synchronized over short periods of time (~24 h), suggesting this phenomenon may be previously overlooked. Although budding can be a mechanism through which larval echinoids asexually reproduce, here, the released buds did not develop into viable clones. OA-induced budding and the associated reduction in larval size suggest new hypotheses regarding physiological and ecological tradeoffs between short-term benefits (e.g. metabolic savings and predation escape) and long-term costs (e.g. tissue loss and delayed development) in the face of climate change. Dataset Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Age
Alkalinity
total
standard error
Animalia
Aragonite saturation state
Benthic animals
Benthos
Bicarbonate ion
Bottles or small containers/Aquaria (<20 L)
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
Coast and continental shelf
Echinodermata
ECO2
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Identification
Laboratory experiment
North Pacific
OA-ICC
Ocean Acidification International Coordination Centre
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
Particle density
normalized
Percentage
pH
Potentiometric
spellingShingle Age
Alkalinity
total
standard error
Animalia
Aragonite saturation state
Benthic animals
Benthos
Bicarbonate ion
Bottles or small containers/Aquaria (<20 L)
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
Coast and continental shelf
Echinodermata
ECO2
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Identification
Laboratory experiment
North Pacific
OA-ICC
Ocean Acidification International Coordination Centre
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
Particle density
normalized
Percentage
pH
Potentiometric
Chan, Kit Yu Karen
Grünbaum, Daniel
Arnberg, Maj
Thorndyke, Mike
Dupont, Sam
Ocean acidification induces budding in larval sea urchins
topic_facet Age
Alkalinity
total
standard error
Animalia
Aragonite saturation state
Benthic animals
Benthos
Bicarbonate ion
Bottles or small containers/Aquaria (<20 L)
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
Coast and continental shelf
Echinodermata
ECO2
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Identification
Laboratory experiment
North Pacific
OA-ICC
Ocean Acidification International Coordination Centre
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
Particle density
normalized
Percentage
pH
Potentiometric
description Ocean acidification (OA), the reduction of ocean pH due to hydration of atmospheric CO2, is known to affect growth and survival of marine invertebrate larvae. Survival and transport of vulnerable planktonic larval stages play important roles in determining population dynamics and community structures in coastal ecosystems. Here, we show that larvae of the purple urchin, Strongylocentrotus purpuratus, underwent high-frequency budding (release of blastula-like particles) when exposed to elevated pCO2 level (>700 µatm). Budding was observed in >50 % of the population and was synchronized over short periods of time (~24 h), suggesting this phenomenon may be previously overlooked. Although budding can be a mechanism through which larval echinoids asexually reproduce, here, the released buds did not develop into viable clones. OA-induced budding and the associated reduction in larval size suggest new hypotheses regarding physiological and ecological tradeoffs between short-term benefits (e.g. metabolic savings and predation escape) and long-term costs (e.g. tissue loss and delayed development) in the face of climate change.
format Dataset
author Chan, Kit Yu Karen
Grünbaum, Daniel
Arnberg, Maj
Thorndyke, Mike
Dupont, Sam
author_facet Chan, Kit Yu Karen
Grünbaum, Daniel
Arnberg, Maj
Thorndyke, Mike
Dupont, Sam
author_sort Chan, Kit Yu Karen
title Ocean acidification induces budding in larval sea urchins
title_short Ocean acidification induces budding in larval sea urchins
title_full Ocean acidification induces budding in larval sea urchins
title_fullStr Ocean acidification induces budding in larval sea urchins
title_full_unstemmed Ocean acidification induces budding in larval sea urchins
title_sort ocean acidification induces budding in larval sea urchins
publisher PANGAEA
publishDate 2013
url https://doi.pangaea.de/10.1594/PANGAEA.830736
https://doi.org/10.1594/PANGAEA.830736
genre Ocean acidification
genre_facet Ocean acidification
op_source Supplement to: Chan, Kit Yu Karen; Grünbaum, Daniel; Arnberg, Maj; Thorndyke, Mike; Dupont, Sam (2012): Ocean acidification induces budding in larval sea urchins. Marine Biology, 160(8), 2129-2135, https://doi.org/10.1007/s00227-012-2103-6
op_relation Lavigne, Héloïse; Gattuso, Jean-Pierre (2011): seacarb: seawater carbonate chemistry with R. R package version 2.4 [webpage]. https://cran.r-project.org/package=seacarb
https://doi.pangaea.de/10.1594/PANGAEA.830736
https://doi.org/10.1594/PANGAEA.830736
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.83073610.1007/s00227-012-2103-6
_version_ 1810469050500775936