Seawater carbonate chemistry and growth rate of Emiliania huxleyi in lab experiment
Predicting the impacts of environmental change on marine organisms, food webs, and biogeochemical cycles presently relies almost exclusively on short-term physiological studies, while the possibility of adaptive evolution is often ignored. Here, we assess adaptive evolution in the coccolithophore Em...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.823153 2024-09-15T18:24:10+00:00 Seawater carbonate chemistry and growth rate of Emiliania huxleyi in lab experiment Lohbeck, Kai T Riebesell, Ulf Collins, Sinéad Reusch, Thorsten B H 2013 text/tab-separated-values, 4800 data points https://doi.pangaea.de/10.1594/PANGAEA.823153 https://doi.org/10.1594/PANGAEA.823153 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.823153 https://doi.org/10.1594/PANGAEA.823153 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Lohbeck, Kai T; Riebesell, Ulf; Collins, Sinéad; Reusch, Thorsten B H (2013): Functional genetic divergence in high CO2 adapted Emiliania Huxleyi populations. Evolution, 67(7), 1892-1900, https://doi.org/10.1111/j.1558-5646.2012.01812.x Alkalinity total Aragonite saturation state Bicarbonate ion BIOACID Biological Impacts of Ocean Acidification 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 Emiliania huxleyi Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Generation Growth/Morphology Growth rate Haptophyta Laboratory experiment Laboratory strains Light North Atlantic OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos pH Phytoplankton Population Potentiometric titration Replicates Salinity Single species Species Temperature water Treatment dataset 2013 ftpangaea https://doi.org/10.1594/PANGAEA.82315310.1111/j.1558-5646.2012.01812.x 2024-07-24T02:31:32Z Predicting the impacts of environmental change on marine organisms, food webs, and biogeochemical cycles presently relies almost exclusively on short-term physiological studies, while the possibility of adaptive evolution is often ignored. Here, we assess adaptive evolution in the coccolithophore Emiliania huxleyi, a well-established model species in biological oceanography, in response to ocean acidification. We previously demonstrated that this globally important marine phytoplankton species adapts within 500 generations to elevated CO2. After 750 and 1000 generations, no further fitness increase occurred, and we observed phenotypic convergence between replicate populations. We then exposed adapted populations to two novel environments to investigate whether or not the underlying basis for high CO2-adaptation involves functional genetic divergence, assuming that different novel mutations become apparent via divergent pleiotropic effects. The novel environment "high light" did not reveal such genetic divergence whereas growth in a low-salinity environment revealed strong pleiotropic effects in high CO2 adapted populations, indicating divergent genetic bases for adaptation to high CO2. This suggests that pleiotropy plays an important role in adaptation of natural E. huxleyi populations to ocean acidification. Our study highlights the potential mutual benefits for oceanography and evolutionary biology of using ecologically important marine phytoplankton for microbial evolution experiments. 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 Bicarbonate ion BIOACID Biological Impacts of Ocean Acidification 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 Emiliania huxleyi Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Generation Growth/Morphology Growth rate Haptophyta Laboratory experiment Laboratory strains Light North Atlantic OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos pH Phytoplankton Population Potentiometric titration Replicates Salinity Single species Species Temperature water Treatment |
spellingShingle |
Alkalinity total Aragonite saturation state Bicarbonate ion BIOACID Biological Impacts of Ocean Acidification 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 Emiliania huxleyi Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Generation Growth/Morphology Growth rate Haptophyta Laboratory experiment Laboratory strains Light North Atlantic OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos pH Phytoplankton Population Potentiometric titration Replicates Salinity Single species Species Temperature water Treatment Lohbeck, Kai T Riebesell, Ulf Collins, Sinéad Reusch, Thorsten B H Seawater carbonate chemistry and growth rate of Emiliania huxleyi in lab experiment |
topic_facet |
Alkalinity total Aragonite saturation state Bicarbonate ion BIOACID Biological Impacts of Ocean Acidification 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 Emiliania huxleyi Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Generation Growth/Morphology Growth rate Haptophyta Laboratory experiment Laboratory strains Light North Atlantic OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos pH Phytoplankton Population Potentiometric titration Replicates Salinity Single species Species Temperature water Treatment |
description |
Predicting the impacts of environmental change on marine organisms, food webs, and biogeochemical cycles presently relies almost exclusively on short-term physiological studies, while the possibility of adaptive evolution is often ignored. Here, we assess adaptive evolution in the coccolithophore Emiliania huxleyi, a well-established model species in biological oceanography, in response to ocean acidification. We previously demonstrated that this globally important marine phytoplankton species adapts within 500 generations to elevated CO2. After 750 and 1000 generations, no further fitness increase occurred, and we observed phenotypic convergence between replicate populations. We then exposed adapted populations to two novel environments to investigate whether or not the underlying basis for high CO2-adaptation involves functional genetic divergence, assuming that different novel mutations become apparent via divergent pleiotropic effects. The novel environment "high light" did not reveal such genetic divergence whereas growth in a low-salinity environment revealed strong pleiotropic effects in high CO2 adapted populations, indicating divergent genetic bases for adaptation to high CO2. This suggests that pleiotropy plays an important role in adaptation of natural E. huxleyi populations to ocean acidification. Our study highlights the potential mutual benefits for oceanography and evolutionary biology of using ecologically important marine phytoplankton for microbial evolution experiments. |
format |
Dataset |
author |
Lohbeck, Kai T Riebesell, Ulf Collins, Sinéad Reusch, Thorsten B H |
author_facet |
Lohbeck, Kai T Riebesell, Ulf Collins, Sinéad Reusch, Thorsten B H |
author_sort |
Lohbeck, Kai T |
title |
Seawater carbonate chemistry and growth rate of Emiliania huxleyi in lab experiment |
title_short |
Seawater carbonate chemistry and growth rate of Emiliania huxleyi in lab experiment |
title_full |
Seawater carbonate chemistry and growth rate of Emiliania huxleyi in lab experiment |
title_fullStr |
Seawater carbonate chemistry and growth rate of Emiliania huxleyi in lab experiment |
title_full_unstemmed |
Seawater carbonate chemistry and growth rate of Emiliania huxleyi in lab experiment |
title_sort |
seawater carbonate chemistry and growth rate of emiliania huxleyi in lab experiment |
publisher |
PANGAEA |
publishDate |
2013 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.823153 https://doi.org/10.1594/PANGAEA.823153 |
genre |
North Atlantic Ocean acidification |
genre_facet |
North Atlantic Ocean acidification |
op_source |
Supplement to: Lohbeck, Kai T; Riebesell, Ulf; Collins, Sinéad; Reusch, Thorsten B H (2013): Functional genetic divergence in high CO2 adapted Emiliania Huxleyi populations. Evolution, 67(7), 1892-1900, https://doi.org/10.1111/j.1558-5646.2012.01812.x |
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.823153 https://doi.org/10.1594/PANGAEA.823153 |
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.82315310.1111/j.1558-5646.2012.01812.x |
_version_ |
1810464469160034304 |