Experiment: changing carbonate chemistry influence on coccoliths formed by Emiliania huxleyi ...
The coccolithophore Emiliania huxleyi is a marine phytoplankton species capable of forming small calcium carbonate scales (coccoliths) which cover the organic part of the cell. Calcification rates of E. huxleyi are known to be sensitive to changes in seawater carbonate chemistry. It has, however, no...
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Online Access: | https://dx.doi.org/10.1594/pangaea.829081 https://doi.pangaea.de/10.1594/PANGAEA.829081 |
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ftdatacite:10.1594/pangaea.829081 2024-09-09T20:01:38+00:00 Experiment: changing carbonate chemistry influence on coccoliths formed by Emiliania huxleyi ... Bach, Lennart Thomas 2014 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.829081 https://doi.pangaea.de/10.1594/PANGAEA.829081 en eng PANGAEA https://dx.doi.org/10.5194/bg-9-3449-2012 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Treatment Carbon, inorganic, dissolved Alkalinity, total pH Carbon dioxide, partial pressure Bicarbonate ion Carbonate ion Carbon dioxide Calcite saturation state Aragonite saturation state Cell size Carbon, inorganic, particulate, production per cell Mass Mass, standard deviation - Production Surface area Surface area, standard deviation Length Length, standard deviation Width Width, standard deviation Height/width ratio Height/width ratio, standard deviation Coccoliths, malformed and incomplete Coccoliths, malformed and incomplete, standard deviation Measured Biological Impacts of Ocean Acidification BIOACID dataset Supplementary Dataset Dataset 2014 ftdatacite https://doi.org/10.1594/pangaea.82908110.5194/bg-9-3449-2012 2024-06-17T10:47:13Z The coccolithophore Emiliania huxleyi is a marine phytoplankton species capable of forming small calcium carbonate scales (coccoliths) which cover the organic part of the cell. Calcification rates of E. huxleyi are known to be sensitive to changes in seawater carbonate chemistry. It has, however, not yet been clearly determined how these changes are reflected in size and weight of individual coccoliths and which specific parameter(s) of the carbonate system drive morphological modifications. Here, we compare data on coccolith size, weight, and malformation from a set of five experiments with a large diversity of carbonate chemistry conditions. This diversity allows distinguishing the influence of individual carbonate chemistry parameters such as carbon dioxide (CO2), bicarbonate (HCO3- ), carbonate ion (CO32-), and protons (H+) on the measured parameters. Measurements of fine-scale morphological structures reveal an increase of coccolith malformation with decreasing pH suggesting that H+ is the major factor ... : Supplement to: Bach, Lennart Thomas; Bauke, Christine; Meier, K J Sebastian; Riebesell, Ulf; Schulz, Kai Georg (2012): Influence of changing carbonate chemistry on morphology and weight of coccoliths formed by Emiliania huxleyi. Biogeosciences, 9(8), 3449-3463 ... Dataset Ocean acidification DataCite Meier ENVELOPE(-45.900,-45.900,-60.633,-60.633) |
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Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Treatment Carbon, inorganic, dissolved Alkalinity, total pH Carbon dioxide, partial pressure Bicarbonate ion Carbonate ion Carbon dioxide Calcite saturation state Aragonite saturation state Cell size Carbon, inorganic, particulate, production per cell Mass Mass, standard deviation - Production Surface area Surface area, standard deviation Length Length, standard deviation Width Width, standard deviation Height/width ratio Height/width ratio, standard deviation Coccoliths, malformed and incomplete Coccoliths, malformed and incomplete, standard deviation Measured Biological Impacts of Ocean Acidification BIOACID |
spellingShingle |
Treatment Carbon, inorganic, dissolved Alkalinity, total pH Carbon dioxide, partial pressure Bicarbonate ion Carbonate ion Carbon dioxide Calcite saturation state Aragonite saturation state Cell size Carbon, inorganic, particulate, production per cell Mass Mass, standard deviation - Production Surface area Surface area, standard deviation Length Length, standard deviation Width Width, standard deviation Height/width ratio Height/width ratio, standard deviation Coccoliths, malformed and incomplete Coccoliths, malformed and incomplete, standard deviation Measured Biological Impacts of Ocean Acidification BIOACID Bach, Lennart Thomas Experiment: changing carbonate chemistry influence on coccoliths formed by Emiliania huxleyi ... |
topic_facet |
Treatment Carbon, inorganic, dissolved Alkalinity, total pH Carbon dioxide, partial pressure Bicarbonate ion Carbonate ion Carbon dioxide Calcite saturation state Aragonite saturation state Cell size Carbon, inorganic, particulate, production per cell Mass Mass, standard deviation - Production Surface area Surface area, standard deviation Length Length, standard deviation Width Width, standard deviation Height/width ratio Height/width ratio, standard deviation Coccoliths, malformed and incomplete Coccoliths, malformed and incomplete, standard deviation Measured Biological Impacts of Ocean Acidification BIOACID |
description |
The coccolithophore Emiliania huxleyi is a marine phytoplankton species capable of forming small calcium carbonate scales (coccoliths) which cover the organic part of the cell. Calcification rates of E. huxleyi are known to be sensitive to changes in seawater carbonate chemistry. It has, however, not yet been clearly determined how these changes are reflected in size and weight of individual coccoliths and which specific parameter(s) of the carbonate system drive morphological modifications. Here, we compare data on coccolith size, weight, and malformation from a set of five experiments with a large diversity of carbonate chemistry conditions. This diversity allows distinguishing the influence of individual carbonate chemistry parameters such as carbon dioxide (CO2), bicarbonate (HCO3- ), carbonate ion (CO32-), and protons (H+) on the measured parameters. Measurements of fine-scale morphological structures reveal an increase of coccolith malformation with decreasing pH suggesting that H+ is the major factor ... : Supplement to: Bach, Lennart Thomas; Bauke, Christine; Meier, K J Sebastian; Riebesell, Ulf; Schulz, Kai Georg (2012): Influence of changing carbonate chemistry on morphology and weight of coccoliths formed by Emiliania huxleyi. Biogeosciences, 9(8), 3449-3463 ... |
format |
Dataset |
author |
Bach, Lennart Thomas |
author_facet |
Bach, Lennart Thomas |
author_sort |
Bach, Lennart Thomas |
title |
Experiment: changing carbonate chemistry influence on coccoliths formed by Emiliania huxleyi ... |
title_short |
Experiment: changing carbonate chemistry influence on coccoliths formed by Emiliania huxleyi ... |
title_full |
Experiment: changing carbonate chemistry influence on coccoliths formed by Emiliania huxleyi ... |
title_fullStr |
Experiment: changing carbonate chemistry influence on coccoliths formed by Emiliania huxleyi ... |
title_full_unstemmed |
Experiment: changing carbonate chemistry influence on coccoliths formed by Emiliania huxleyi ... |
title_sort |
experiment: changing carbonate chemistry influence on coccoliths formed by emiliania huxleyi ... |
publisher |
PANGAEA |
publishDate |
2014 |
url |
https://dx.doi.org/10.1594/pangaea.829081 https://doi.pangaea.de/10.1594/PANGAEA.829081 |
long_lat |
ENVELOPE(-45.900,-45.900,-60.633,-60.633) |
geographic |
Meier |
geographic_facet |
Meier |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_relation |
https://dx.doi.org/10.5194/bg-9-3449-2012 |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.1594/pangaea.82908110.5194/bg-9-3449-2012 |
_version_ |
1809933514064265216 |