Experiment: Physiological responses of the calcifying rhodophyte, Corallina officinalis (L.), to future CO2 levels

Future atmospheric CO2 levels will most likely have complex consequences for marine organisms, particulary photosynthetic calcifying organisms. Corallina officinalis L. is an erect calcifying macroalga found in the inter- and subtidal regions of temperate rocky coastlines and provides important subs...

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Main Authors: Hofmann, Laurie C, Yildiz, Gamse, Hanelt, D, Bischof, Kai
Format: Dataset
Language:English
Published: PANGAEA 2012
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.830128
https://doi.org/10.1594/PANGAEA.830128
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.830128
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.830128 2023-05-15T17:35:23+02:00 Experiment: Physiological responses of the calcifying rhodophyte, Corallina officinalis (L.), to future CO2 levels Hofmann, Laurie C Yildiz, Gamse Hanelt, D Bischof, Kai 2012-02-27 text/tab-separated-values, 13244 data points https://doi.pangaea.de/10.1594/PANGAEA.830128 https://doi.org/10.1594/PANGAEA.830128 en eng PANGAEA Lavigne, Héloïse; Gattuso, Jean-Pierre (2011): seacarb: seawater carbonate chemistry with R. R package version 2.4. https://cran.r-project.org/package=seacarb https://doi.pangaea.de/10.1594/PANGAEA.830128 https://doi.org/10.1594/PANGAEA.830128 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Hofmann, Laurie C; Yildiz, Gamse; Hanelt, D; Bischof, Kai (2011): Physiological responses of the calcifying rhodophyte, Corallina officinalis (L.), to future CO2 levels. Marine Biology, 159(4), 783-792, https://doi.org/10.1007/s00227-011-1854-9 Alkalinity total Aragonite saturation state Benthos Bicarbonate ion BIOACID Biological Impacts of Ocean Acidification Calcification/Dissolution Calcified area Calcite saturation state Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Carbonic anhydrase activity Coast and continental shelf Containers and aquaria (20-1000 L or < 1 m**2) Corallina officinalis Date Electron transport rate Fluorescence maximum without dark adaptation minimum yield at any given time Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Gross oxygen evolution per chlorophyll a Group Growth/Morphology Growth rate Incubation duration Inorganic matter Irradiance Laboratory experiment Macroalgae Maximum photochemical quantum yield of photosystem II Net oxygen evolution Non photochemical quenching North Atlantic OA-ICC Ocean Acidification International Coordination Centre Dataset 2012 ftpangaea https://doi.org/10.1594/PANGAEA.830128 https://doi.org/10.1007/s00227-011-1854-9 2023-01-20T09:03:02Z Future atmospheric CO2 levels will most likely have complex consequences for marine organisms, particulary photosynthetic calcifying organisms. Corallina officinalis L. is an erect calcifying macroalga found in the inter- and subtidal regions of temperate rocky coastlines and provides important substrate and refugia for marine meiofauna. The main goal of the current study was to determine the physiological responses of C. officinalis to increased CO2 concentrations expected to occur within the next century and beyond. Our results show that growth and production of inorganic material decreased under high CO2 levels, while carbonic anhydrase activity was stimulated and negatively correlated to algal inorganic content. Photosynthetic efficiency based on oxygen evolution was also negatively affected by increased CO2. The results of this study indicate that C. officinalis may become less competitive under future CO2 levels, which could result in structural changes in future temperate intertidal communities. Dataset North Atlantic 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 Alkalinity
total
Aragonite saturation state
Benthos
Bicarbonate ion
BIOACID
Biological Impacts of Ocean Acidification
Calcification/Dissolution
Calcified area
Calcite saturation state
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
Carbonate ion
Carbonate system computation flag
Carbon dioxide
Carbonic anhydrase
activity
Coast and continental shelf
Containers and aquaria (20-1000 L or < 1 m**2)
Corallina officinalis
Date
Electron transport rate
Fluorescence
maximum
without dark adaptation
minimum
yield at any given time
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Gross oxygen evolution
per chlorophyll a
Group
Growth/Morphology
Growth rate
Incubation duration
Inorganic matter
Irradiance
Laboratory experiment
Macroalgae
Maximum photochemical quantum yield of photosystem II
Net oxygen evolution
Non photochemical quenching
North Atlantic
OA-ICC
Ocean Acidification International Coordination Centre
spellingShingle Alkalinity
total
Aragonite saturation state
Benthos
Bicarbonate ion
BIOACID
Biological Impacts of Ocean Acidification
Calcification/Dissolution
Calcified area
Calcite saturation state
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
Carbonate ion
Carbonate system computation flag
Carbon dioxide
Carbonic anhydrase
activity
Coast and continental shelf
Containers and aquaria (20-1000 L or < 1 m**2)
Corallina officinalis
Date
Electron transport rate
Fluorescence
maximum
without dark adaptation
minimum
yield at any given time
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Gross oxygen evolution
per chlorophyll a
Group
Growth/Morphology
Growth rate
Incubation duration
Inorganic matter
Irradiance
Laboratory experiment
Macroalgae
Maximum photochemical quantum yield of photosystem II
Net oxygen evolution
Non photochemical quenching
North Atlantic
OA-ICC
Ocean Acidification International Coordination Centre
Hofmann, Laurie C
Yildiz, Gamse
Hanelt, D
Bischof, Kai
Experiment: Physiological responses of the calcifying rhodophyte, Corallina officinalis (L.), to future CO2 levels
topic_facet Alkalinity
total
Aragonite saturation state
Benthos
Bicarbonate ion
BIOACID
Biological Impacts of Ocean Acidification
Calcification/Dissolution
Calcified area
Calcite saturation state
Calculated using seacarb after Nisumaa et al. (2010)
Carbon
inorganic
dissolved
Carbonate ion
Carbonate system computation flag
Carbon dioxide
Carbonic anhydrase
activity
Coast and continental shelf
Containers and aquaria (20-1000 L or < 1 m**2)
Corallina officinalis
Date
Electron transport rate
Fluorescence
maximum
without dark adaptation
minimum
yield at any given time
Fugacity of carbon dioxide (water) at sea surface temperature (wet air)
Gross oxygen evolution
per chlorophyll a
Group
Growth/Morphology
Growth rate
Incubation duration
Inorganic matter
Irradiance
Laboratory experiment
Macroalgae
Maximum photochemical quantum yield of photosystem II
Net oxygen evolution
Non photochemical quenching
North Atlantic
OA-ICC
Ocean Acidification International Coordination Centre
description Future atmospheric CO2 levels will most likely have complex consequences for marine organisms, particulary photosynthetic calcifying organisms. Corallina officinalis L. is an erect calcifying macroalga found in the inter- and subtidal regions of temperate rocky coastlines and provides important substrate and refugia for marine meiofauna. The main goal of the current study was to determine the physiological responses of C. officinalis to increased CO2 concentrations expected to occur within the next century and beyond. Our results show that growth and production of inorganic material decreased under high CO2 levels, while carbonic anhydrase activity was stimulated and negatively correlated to algal inorganic content. Photosynthetic efficiency based on oxygen evolution was also negatively affected by increased CO2. The results of this study indicate that C. officinalis may become less competitive under future CO2 levels, which could result in structural changes in future temperate intertidal communities.
format Dataset
author Hofmann, Laurie C
Yildiz, Gamse
Hanelt, D
Bischof, Kai
author_facet Hofmann, Laurie C
Yildiz, Gamse
Hanelt, D
Bischof, Kai
author_sort Hofmann, Laurie C
title Experiment: Physiological responses of the calcifying rhodophyte, Corallina officinalis (L.), to future CO2 levels
title_short Experiment: Physiological responses of the calcifying rhodophyte, Corallina officinalis (L.), to future CO2 levels
title_full Experiment: Physiological responses of the calcifying rhodophyte, Corallina officinalis (L.), to future CO2 levels
title_fullStr Experiment: Physiological responses of the calcifying rhodophyte, Corallina officinalis (L.), to future CO2 levels
title_full_unstemmed Experiment: Physiological responses of the calcifying rhodophyte, Corallina officinalis (L.), to future CO2 levels
title_sort experiment: physiological responses of the calcifying rhodophyte, corallina officinalis (l.), to future co2 levels
publisher PANGAEA
publishDate 2012
url https://doi.pangaea.de/10.1594/PANGAEA.830128
https://doi.org/10.1594/PANGAEA.830128
genre North Atlantic
Ocean acidification
genre_facet North Atlantic
Ocean acidification
op_source Supplement to: Hofmann, Laurie C; Yildiz, Gamse; Hanelt, D; Bischof, Kai (2011): Physiological responses of the calcifying rhodophyte, Corallina officinalis (L.), to future CO2 levels. Marine Biology, 159(4), 783-792, https://doi.org/10.1007/s00227-011-1854-9
op_relation Lavigne, Héloïse; Gattuso, Jean-Pierre (2011): seacarb: seawater carbonate chemistry with R. R package version 2.4. https://cran.r-project.org/package=seacarb
https://doi.pangaea.de/10.1594/PANGAEA.830128
https://doi.org/10.1594/PANGAEA.830128
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.830128
https://doi.org/10.1007/s00227-011-1854-9
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