Seawater carbonate chemistry and community composition and production of of algal communities

Long‐term exposure to CO2‐enriched waters can considerably alter marine biological community development, often resulting in simplified systems dominated by turf algae that possess reduced biodiversity and low ecological complexity. Current understanding of the underlying processes by which ocean ac...

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Main Authors: Harvey, Ben P, Kon, Koetsu, Agostini, Sylvain, Wada, Shigeki, Hall-Spencer, Jason M
Format: Dataset
Language:English
Published: PANGAEA 2021
Subjects:
EXP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.930056
https://doi.org/10.1594/PANGAEA.930056
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.930056
record_format openpolar
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Abundance
Alkalinity
total
standard deviation
Aragonite saturation state
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
CO2 vent
Coast and continental shelf
Community composition and diversity
Complexity
Coverage
Entire community
EXP
Experiment
Experiment duration
Field experiment
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Gross community production of oxygen
Net community production
oxygen
North Pacific
OA-ICC
Ocean Acidification International Coordination Centre
Partial pressure of carbon dioxide
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
spellingShingle Abundance
Alkalinity
total
standard deviation
Aragonite saturation state
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
CO2 vent
Coast and continental shelf
Community composition and diversity
Complexity
Coverage
Entire community
EXP
Experiment
Experiment duration
Field experiment
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Gross community production of oxygen
Net community production
oxygen
North Pacific
OA-ICC
Ocean Acidification International Coordination Centre
Partial pressure of carbon dioxide
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
Harvey, Ben P
Kon, Koetsu
Agostini, Sylvain
Wada, Shigeki
Hall-Spencer, Jason M
Seawater carbonate chemistry and community composition and production of of algal communities
topic_facet Abundance
Alkalinity
total
standard deviation
Aragonite saturation state
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
CO2 vent
Coast and continental shelf
Community composition and diversity
Complexity
Coverage
Entire community
EXP
Experiment
Experiment duration
Field experiment
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Gross community production of oxygen
Net community production
oxygen
North Pacific
OA-ICC
Ocean Acidification International Coordination Centre
Partial pressure of carbon dioxide
Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)
description Long‐term exposure to CO2‐enriched waters can considerably alter marine biological community development, often resulting in simplified systems dominated by turf algae that possess reduced biodiversity and low ecological complexity. Current understanding of the underlying processes by which ocean acidification alters biological community development and stability remains limited, making the management of such shifts problematic. Here, we deployed recruitment tiles in reference (pHT 8.137 +/- 0.056 SD) and CO2‐enriched conditions (pHT 7.788 +/- 0.105 SD) at a volcanic CO2 seep in Japan to assess the underlying processes and patterns of algal community development. We assessed (i) algal community succession in two different seasons (Cooler months: January–July, and warmer months: July–January), (ii) the effects of initial community composition on subsequent community succession (by reciprocally transplanting preestablished communities for a further 6 months), and (iii) the community production of resulting communities, to assess how their functioning was altered (following 12 months recruitment). Settlement tiles became dominated by turf algae under CO2‐enrichment and had lower biomass, diversity and complexity, a pattern consistent across seasons. This locked the community in a species‐poor early successional stage. In terms of community functioning, the elevated pCO2 community had greater net community production, but this did not result in increased algal community cover, biomass, biodiversity or structural complexity. Taken together, this shows that both new and established communities become simplified by rising CO2 levels. Our transplant of preestablished communities from enriched CO2 to reference conditions demonstrated their high resilience, since they became indistinguishable from communities maintained entirely in reference conditions. This shows that meaningful reductions in pCO2 can enable the recovery of algal communities. By understanding the ecological processes responsible for driving shifts in ...
format Dataset
author Harvey, Ben P
Kon, Koetsu
Agostini, Sylvain
Wada, Shigeki
Hall-Spencer, Jason M
author_facet Harvey, Ben P
Kon, Koetsu
Agostini, Sylvain
Wada, Shigeki
Hall-Spencer, Jason M
author_sort Harvey, Ben P
title Seawater carbonate chemistry and community composition and production of of algal communities
title_short Seawater carbonate chemistry and community composition and production of of algal communities
title_full Seawater carbonate chemistry and community composition and production of of algal communities
title_fullStr Seawater carbonate chemistry and community composition and production of of algal communities
title_full_unstemmed Seawater carbonate chemistry and community composition and production of of algal communities
title_sort seawater carbonate chemistry and community composition and production of of algal communities
publisher PANGAEA
publishDate 2021
url https://doi.pangaea.de/10.1594/PANGAEA.930056
https://doi.org/10.1594/PANGAEA.930056
op_coverage LATITUDE: 34.319170 * LONGITUDE: 139.205000
long_lat ENVELOPE(139.205000,139.205000,34.319170,34.319170)
geographic Pacific
geographic_facet Pacific
genre Ocean acidification
genre_facet Ocean acidification
op_relation Harvey, Ben P; Kon, Koetsu; Agostini, Sylvain; Wada, Shigeki; Hall-Spencer, Jason M (2021): Ocean acidification locks algal communities in a species‐poor early successional stage. Global Change Biology, https://doi.org/10.1111/gcb.15455
Harvey, Ben P; Kon, Koetsu; Agostini, Sylvain; Wada, Shigeki; Hall-Spencer, Jason M (2020): Biological Data and Carbonate Chemistry used in 'Ocean acidification locks algal communities in a species-poor early successional stage'. Zenodo, https://doi.org/10.5281/zenodo.4280018
Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse; Orr, James (2021): seacarb: seawater carbonate chemistry with R. R package version 3.2.16. https://cran.r-project.org/web/packages/seacarb/index.html
https://doi.pangaea.de/10.1594/PANGAEA.930056
https://doi.org/10.1594/PANGAEA.930056
op_rights CC-BY-4.0: Creative Commons Attribution 4.0 International
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.930056
https://doi.org/10.1111/gcb.15455
https://doi.org/10.5281/zenodo.4280018
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spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.930056 2023-05-15T17:51:12+02:00 Seawater carbonate chemistry and community composition and production of of algal communities Harvey, Ben P Kon, Koetsu Agostini, Sylvain Wada, Shigeki Hall-Spencer, Jason M LATITUDE: 34.319170 * LONGITUDE: 139.205000 2021-04-07 text/tab-separated-values, 2614 data points https://doi.pangaea.de/10.1594/PANGAEA.930056 https://doi.org/10.1594/PANGAEA.930056 en eng PANGAEA Harvey, Ben P; Kon, Koetsu; Agostini, Sylvain; Wada, Shigeki; Hall-Spencer, Jason M (2021): Ocean acidification locks algal communities in a species‐poor early successional stage. Global Change Biology, https://doi.org/10.1111/gcb.15455 Harvey, Ben P; Kon, Koetsu; Agostini, Sylvain; Wada, Shigeki; Hall-Spencer, Jason M (2020): Biological Data and Carbonate Chemistry used in 'Ocean acidification locks algal communities in a species-poor early successional stage'. Zenodo, https://doi.org/10.5281/zenodo.4280018 Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse; Orr, James (2021): seacarb: seawater carbonate chemistry with R. R package version 3.2.16. https://cran.r-project.org/web/packages/seacarb/index.html https://doi.pangaea.de/10.1594/PANGAEA.930056 https://doi.org/10.1594/PANGAEA.930056 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Abundance Alkalinity total standard deviation Aragonite saturation state 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 CO2 vent Coast and continental shelf Community composition and diversity Complexity Coverage Entire community EXP Experiment Experiment duration Field experiment Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Gross community production of oxygen Net community production oxygen North Pacific OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Dataset 2021 ftpangaea https://doi.org/10.1594/PANGAEA.930056 https://doi.org/10.1111/gcb.15455 https://doi.org/10.5281/zenodo.4280018 2023-01-20T09:14:45Z Long‐term exposure to CO2‐enriched waters can considerably alter marine biological community development, often resulting in simplified systems dominated by turf algae that possess reduced biodiversity and low ecological complexity. Current understanding of the underlying processes by which ocean acidification alters biological community development and stability remains limited, making the management of such shifts problematic. Here, we deployed recruitment tiles in reference (pHT 8.137 +/- 0.056 SD) and CO2‐enriched conditions (pHT 7.788 +/- 0.105 SD) at a volcanic CO2 seep in Japan to assess the underlying processes and patterns of algal community development. We assessed (i) algal community succession in two different seasons (Cooler months: January–July, and warmer months: July–January), (ii) the effects of initial community composition on subsequent community succession (by reciprocally transplanting preestablished communities for a further 6 months), and (iii) the community production of resulting communities, to assess how their functioning was altered (following 12 months recruitment). Settlement tiles became dominated by turf algae under CO2‐enrichment and had lower biomass, diversity and complexity, a pattern consistent across seasons. This locked the community in a species‐poor early successional stage. In terms of community functioning, the elevated pCO2 community had greater net community production, but this did not result in increased algal community cover, biomass, biodiversity or structural complexity. Taken together, this shows that both new and established communities become simplified by rising CO2 levels. Our transplant of preestablished communities from enriched CO2 to reference conditions demonstrated their high resilience, since they became indistinguishable from communities maintained entirely in reference conditions. This shows that meaningful reductions in pCO2 can enable the recovery of algal communities. By understanding the ecological processes responsible for driving shifts in ... Dataset Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science Pacific ENVELOPE(139.205000,139.205000,34.319170,34.319170)