Experiment: Physiological responses of the calcifying rhodophyte, Corallina officinalis (L.), to future CO2 levels, 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
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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ftdatacite:10.1594/pangaea.830128 2023-05-15T17:37:14+02:00 Experiment: Physiological responses of the calcifying rhodophyte, Corallina officinalis (L.), to future CO2 levels, 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 Hofmann, Laurie C Yildiz, Gamse Hanelt, D Bischof, Kai 2012 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.830128 https://doi.pangaea.de/10.1594/PANGAEA.830128 en eng PANGAEA - Data Publisher for Earth & Environmental Science https://cran.r-project.org/package=seacarb https://dx.doi.org/10.1007/s00227-011-1854-9 https://cran.r-project.org/package=seacarb Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 CC-BY Benthos Calcification/Dissolution Coast and continental shelf Containers and aquaria 20-1000 L or < 1 m**2 Corallina officinalis Growth/Morphology Laboratory experiment Macroalgae North Atlantic Plantae Primary production/Photosynthesis Rhodophyta Single species Temperate Species Treatment Group Replicate Incubation duration Date Time of day Maximum photochemical quantum yield of photosystem II Irradiance Gross oxygen evolution, per chlorophyll a Net oxygen evolution, per chlorophyll a Calcified area Growth rate Carbonic anhydrase, activity Organic matter Inorganic matter Fluorescence, yield at any given time Electron transport rate Yield Photochemical quenching Non photochemical quenching Fluorescence, maximum, without dark adaptation Fluorescence, minimum, without dark adaptation Temperature, water Salinity pH pH, standard error Partial pressure of carbon dioxide water at sea surface temperature wet air Partial pressure of carbon dioxide, standard deviation Carbonate system computation flag Carbon dioxide Fugacity of carbon dioxide water at sea surface temperature wet air Bicarbonate ion Carbonate ion Carbon, inorganic, dissolved Alkalinity, total Aragonite saturation state Calcite saturation state Calculated using seacarb after Nisumaa et al. 2010 Biological Impacts of Ocean Acidification BIOACID Ocean Acidification International Coordination Centre OA-ICC Dataset dataset Supplementary Dataset 2012 ftdatacite https://doi.org/10.1594/pangaea.830128 https://doi.org/10.1007/s00227-011-1854-9 2022-02-09T13:11:39Z 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. : In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Lavigne and Gattuso, 2011) was used to compute a complete and consistent set of carbonate system variables, as described by Nisumaa et al. (2010). In this dataset the original values were archived in addition with the recalculated parameters (see related PI). The date of carbonate chemistry calculation by seacarb is 2014-02-11. Dataset North Atlantic Ocean acidification DataCite Metadata Store (German National Library of Science and Technology) Hofmann ENVELOPE(160.600,160.600,-82.667,-82.667) Laurie ENVELOPE(-44.616,-44.616,-60.733,-60.733) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Benthos Calcification/Dissolution Coast and continental shelf Containers and aquaria 20-1000 L or < 1 m**2 Corallina officinalis Growth/Morphology Laboratory experiment Macroalgae North Atlantic Plantae Primary production/Photosynthesis Rhodophyta Single species Temperate Species Treatment Group Replicate Incubation duration Date Time of day Maximum photochemical quantum yield of photosystem II Irradiance Gross oxygen evolution, per chlorophyll a Net oxygen evolution, per chlorophyll a Calcified area Growth rate Carbonic anhydrase, activity Organic matter Inorganic matter Fluorescence, yield at any given time Electron transport rate Yield Photochemical quenching Non photochemical quenching Fluorescence, maximum, without dark adaptation Fluorescence, minimum, without dark adaptation Temperature, water Salinity pH pH, standard error Partial pressure of carbon dioxide water at sea surface temperature wet air Partial pressure of carbon dioxide, standard deviation Carbonate system computation flag Carbon dioxide Fugacity of carbon dioxide water at sea surface temperature wet air Bicarbonate ion Carbonate ion Carbon, inorganic, dissolved Alkalinity, total Aragonite saturation state Calcite saturation state Calculated using seacarb after Nisumaa et al. 2010 Biological Impacts of Ocean Acidification BIOACID Ocean Acidification International Coordination Centre OA-ICC |
spellingShingle |
Benthos Calcification/Dissolution Coast and continental shelf Containers and aquaria 20-1000 L or < 1 m**2 Corallina officinalis Growth/Morphology Laboratory experiment Macroalgae North Atlantic Plantae Primary production/Photosynthesis Rhodophyta Single species Temperate Species Treatment Group Replicate Incubation duration Date Time of day Maximum photochemical quantum yield of photosystem II Irradiance Gross oxygen evolution, per chlorophyll a Net oxygen evolution, per chlorophyll a Calcified area Growth rate Carbonic anhydrase, activity Organic matter Inorganic matter Fluorescence, yield at any given time Electron transport rate Yield Photochemical quenching Non photochemical quenching Fluorescence, maximum, without dark adaptation Fluorescence, minimum, without dark adaptation Temperature, water Salinity pH pH, standard error Partial pressure of carbon dioxide water at sea surface temperature wet air Partial pressure of carbon dioxide, standard deviation Carbonate system computation flag Carbon dioxide Fugacity of carbon dioxide water at sea surface temperature wet air Bicarbonate ion Carbonate ion Carbon, inorganic, dissolved Alkalinity, total Aragonite saturation state Calcite saturation state Calculated using seacarb after Nisumaa et al. 2010 Biological Impacts of Ocean Acidification BIOACID Ocean Acidification International Coordination Centre OA-ICC Hofmann, Laurie C Yildiz, Gamse Hanelt, D Bischof, Kai Experiment: Physiological responses of the calcifying rhodophyte, Corallina officinalis (L.), to future CO2 levels, 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 |
topic_facet |
Benthos Calcification/Dissolution Coast and continental shelf Containers and aquaria 20-1000 L or < 1 m**2 Corallina officinalis Growth/Morphology Laboratory experiment Macroalgae North Atlantic Plantae Primary production/Photosynthesis Rhodophyta Single species Temperate Species Treatment Group Replicate Incubation duration Date Time of day Maximum photochemical quantum yield of photosystem II Irradiance Gross oxygen evolution, per chlorophyll a Net oxygen evolution, per chlorophyll a Calcified area Growth rate Carbonic anhydrase, activity Organic matter Inorganic matter Fluorescence, yield at any given time Electron transport rate Yield Photochemical quenching Non photochemical quenching Fluorescence, maximum, without dark adaptation Fluorescence, minimum, without dark adaptation Temperature, water Salinity pH pH, standard error Partial pressure of carbon dioxide water at sea surface temperature wet air Partial pressure of carbon dioxide, standard deviation Carbonate system computation flag Carbon dioxide Fugacity of carbon dioxide water at sea surface temperature wet air Bicarbonate ion Carbonate ion Carbon, inorganic, dissolved Alkalinity, total Aragonite saturation state Calcite saturation state Calculated using seacarb after Nisumaa et al. 2010 Biological Impacts of Ocean Acidification BIOACID Ocean Acidification International Coordination Centre OA-ICC |
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. : In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Lavigne and Gattuso, 2011) was used to compute a complete and consistent set of carbonate system variables, as described by Nisumaa et al. (2010). In this dataset the original values were archived in addition with the recalculated parameters (see related PI). The date of carbonate chemistry calculation by seacarb is 2014-02-11. |
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, 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 |
title_short |
Experiment: Physiological responses of the calcifying rhodophyte, Corallina officinalis (L.), to future CO2 levels, 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 |
title_full |
Experiment: Physiological responses of the calcifying rhodophyte, Corallina officinalis (L.), to future CO2 levels, 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 |
title_fullStr |
Experiment: Physiological responses of the calcifying rhodophyte, Corallina officinalis (L.), to future CO2 levels, 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 |
title_full_unstemmed |
Experiment: Physiological responses of the calcifying rhodophyte, Corallina officinalis (L.), to future CO2 levels, 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 |
title_sort |
experiment: physiological responses of the calcifying rhodophyte, corallina officinalis (l.), to future co2 levels, 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 |
publisher |
PANGAEA - Data Publisher for Earth & Environmental Science |
publishDate |
2012 |
url |
https://dx.doi.org/10.1594/pangaea.830128 https://doi.pangaea.de/10.1594/PANGAEA.830128 |
long_lat |
ENVELOPE(160.600,160.600,-82.667,-82.667) ENVELOPE(-44.616,-44.616,-60.733,-60.733) |
geographic |
Hofmann Laurie |
geographic_facet |
Hofmann Laurie |
genre |
North Atlantic Ocean acidification |
genre_facet |
North Atlantic Ocean acidification |
op_relation |
https://cran.r-project.org/package=seacarb https://dx.doi.org/10.1007/s00227-011-1854-9 https://cran.r-project.org/package=seacarb |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/pangaea.830128 https://doi.org/10.1007/s00227-011-1854-9 |
_version_ |
1766137034433363968 |