Seawater carbonate chemistry and community structure of marine biofouling communities, supplement to: Brown, Norah E M; Milazzo, Marco; Rastrick, S P S; Hall-Spencer, Jason M; Therriault, Thomas W; Harley, Christopher D G (2018): Natural acidification changes the timing and rate of succession, alters community structure, and increases homogeneity in marine biofouling communities. Global Change Biology, 24(1), e112-e127
Ocean acidification may have far-reaching consequences for marine community and ecosystem dynamics, but its full impacts remain poorly understood due to the difficulty of manipulating pCO2 at the ecosystem level to mimic realistic fluctuations that occur on a number of different timescales. It is es...
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Format: | Dataset |
Language: | English |
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PANGAEA - Data Publisher for Earth & Environmental Science
2018
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Online Access: | https://dx.doi.org/10.1594/pangaea.892827 https://doi.pangaea.de/10.1594/PANGAEA.892827 |
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ftdatacite:10.1594/pangaea.892827 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Benthos CO2 vent Coast and continental shelf Community composition and diversity Entire community Field experiment Mediterranean Sea Rocky-shore community Temperate Type Identification Time in weeks Site Individuals Number of species Shannon Diversity Index Temperature, water Temperature, water, standard deviation Salinity Salinity, standard deviation pH pH, standard deviation Alkalinity, total Alkalinity, total, standard deviation Partial pressure of carbon dioxide water at sea surface temperature wet air Partial pressure of carbon dioxide, standard deviation Carbon, inorganic, dissolved Carbon, inorganic, dissolved, standard deviation Bicarbonate ion Bicarbonate ion, standard deviation Calcite saturation state Calcite saturation state, standard deviation Aragonite saturation state Aragonite saturation state, standard deviation Carbonate system computation flag Carbon dioxide Fugacity of carbon dioxide water at sea surface temperature wet air Carbonate ion Experiment Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. 2010 Ocean Acidification International Coordination Centre OA-ICC |
spellingShingle |
Benthos CO2 vent Coast and continental shelf Community composition and diversity Entire community Field experiment Mediterranean Sea Rocky-shore community Temperate Type Identification Time in weeks Site Individuals Number of species Shannon Diversity Index Temperature, water Temperature, water, standard deviation Salinity Salinity, standard deviation pH pH, standard deviation Alkalinity, total Alkalinity, total, standard deviation Partial pressure of carbon dioxide water at sea surface temperature wet air Partial pressure of carbon dioxide, standard deviation Carbon, inorganic, dissolved Carbon, inorganic, dissolved, standard deviation Bicarbonate ion Bicarbonate ion, standard deviation Calcite saturation state Calcite saturation state, standard deviation Aragonite saturation state Aragonite saturation state, standard deviation Carbonate system computation flag Carbon dioxide Fugacity of carbon dioxide water at sea surface temperature wet air Carbonate ion Experiment Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. 2010 Ocean Acidification International Coordination Centre OA-ICC Brown, Norah E M Milazzo, Marco Rastrick, S P S Hall-Spencer, Jason M Therriault, Thomas W Harley, Christopher D G Seawater carbonate chemistry and community structure of marine biofouling communities, supplement to: Brown, Norah E M; Milazzo, Marco; Rastrick, S P S; Hall-Spencer, Jason M; Therriault, Thomas W; Harley, Christopher D G (2018): Natural acidification changes the timing and rate of succession, alters community structure, and increases homogeneity in marine biofouling communities. Global Change Biology, 24(1), e112-e127 |
topic_facet |
Benthos CO2 vent Coast and continental shelf Community composition and diversity Entire community Field experiment Mediterranean Sea Rocky-shore community Temperate Type Identification Time in weeks Site Individuals Number of species Shannon Diversity Index Temperature, water Temperature, water, standard deviation Salinity Salinity, standard deviation pH pH, standard deviation Alkalinity, total Alkalinity, total, standard deviation Partial pressure of carbon dioxide water at sea surface temperature wet air Partial pressure of carbon dioxide, standard deviation Carbon, inorganic, dissolved Carbon, inorganic, dissolved, standard deviation Bicarbonate ion Bicarbonate ion, standard deviation Calcite saturation state Calcite saturation state, standard deviation Aragonite saturation state Aragonite saturation state, standard deviation Carbonate system computation flag Carbon dioxide Fugacity of carbon dioxide water at sea surface temperature wet air Carbonate ion Experiment Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. 2010 Ocean Acidification International Coordination Centre OA-ICC |
description |
Ocean acidification may have far-reaching consequences for marine community and ecosystem dynamics, but its full impacts remain poorly understood due to the difficulty of manipulating pCO2 at the ecosystem level to mimic realistic fluctuations that occur on a number of different timescales. It is especially unclear how quickly communities at various stages of development respond to intermediate-scale pCO2 change and, if high pCO2 is relieved mid-succession, whether past acidification effects persist, are reversed by alleviation of pCO2 stress, or are worsened by departures from prior high pCO2 conditions to which organisms had acclimatized. Here, we used reciprocal transplant experiments along a shallow water volcanic pCO2 gradient to assess the importance of the timing and duration of high pCO2 exposure (i.e. discrete events at different stages of successional development vs. continuous exposure) on patterns of colonization and succession in a benthic fouling community. We show that succession at the acidified site was initially delayed (less community change by eight weeks) but then caught up over the next four weeks. These changes in succession led to homogenization of communities maintained in or transplanted to acidified conditions, and altered community structure in ways that reflected both short- and longer-term acidification history. These community shifts are likely a result of interspecific variability in response to increased pCO2 and changes in species interactions. High pCO2 altered biofilm development, allowing serpulids to do best at the acidified site by the end of the experiment, although early (pre-transplant), negative effects of pCO2 on recruitment of these worms was still detectable. The ascidians Diplosoma sp. and Botryllus sp. settled later and were more tolerant to acidification. Overall, transient and persistent acidification-driven changes in the biofouling community, via both past and more recent exposure, could have important implications for ecosystem function and food web dynamics. : In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2016) 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 2018-08-06. |
format |
Dataset |
author |
Brown, Norah E M Milazzo, Marco Rastrick, S P S Hall-Spencer, Jason M Therriault, Thomas W Harley, Christopher D G |
author_facet |
Brown, Norah E M Milazzo, Marco Rastrick, S P S Hall-Spencer, Jason M Therriault, Thomas W Harley, Christopher D G |
author_sort |
Brown, Norah E M |
title |
Seawater carbonate chemistry and community structure of marine biofouling communities, supplement to: Brown, Norah E M; Milazzo, Marco; Rastrick, S P S; Hall-Spencer, Jason M; Therriault, Thomas W; Harley, Christopher D G (2018): Natural acidification changes the timing and rate of succession, alters community structure, and increases homogeneity in marine biofouling communities. Global Change Biology, 24(1), e112-e127 |
title_short |
Seawater carbonate chemistry and community structure of marine biofouling communities, supplement to: Brown, Norah E M; Milazzo, Marco; Rastrick, S P S; Hall-Spencer, Jason M; Therriault, Thomas W; Harley, Christopher D G (2018): Natural acidification changes the timing and rate of succession, alters community structure, and increases homogeneity in marine biofouling communities. Global Change Biology, 24(1), e112-e127 |
title_full |
Seawater carbonate chemistry and community structure of marine biofouling communities, supplement to: Brown, Norah E M; Milazzo, Marco; Rastrick, S P S; Hall-Spencer, Jason M; Therriault, Thomas W; Harley, Christopher D G (2018): Natural acidification changes the timing and rate of succession, alters community structure, and increases homogeneity in marine biofouling communities. Global Change Biology, 24(1), e112-e127 |
title_fullStr |
Seawater carbonate chemistry and community structure of marine biofouling communities, supplement to: Brown, Norah E M; Milazzo, Marco; Rastrick, S P S; Hall-Spencer, Jason M; Therriault, Thomas W; Harley, Christopher D G (2018): Natural acidification changes the timing and rate of succession, alters community structure, and increases homogeneity in marine biofouling communities. Global Change Biology, 24(1), e112-e127 |
title_full_unstemmed |
Seawater carbonate chemistry and community structure of marine biofouling communities, supplement to: Brown, Norah E M; Milazzo, Marco; Rastrick, S P S; Hall-Spencer, Jason M; Therriault, Thomas W; Harley, Christopher D G (2018): Natural acidification changes the timing and rate of succession, alters community structure, and increases homogeneity in marine biofouling communities. Global Change Biology, 24(1), e112-e127 |
title_sort |
seawater carbonate chemistry and community structure of marine biofouling communities, supplement to: brown, norah e m; milazzo, marco; rastrick, s p s; hall-spencer, jason m; therriault, thomas w; harley, christopher d g (2018): natural acidification changes the timing and rate of succession, alters community structure, and increases homogeneity in marine biofouling communities. global change biology, 24(1), e112-e127 |
publisher |
PANGAEA - Data Publisher for Earth & Environmental Science |
publishDate |
2018 |
url |
https://dx.doi.org/10.1594/pangaea.892827 https://doi.pangaea.de/10.1594/PANGAEA.892827 |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_relation |
https://cran.r-project.org/package=seacarb https://dx.doi.org/10.1111/gcb.13856 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.892827 https://doi.org/10.1111/gcb.13856 |
_version_ |
1766158154639343616 |
spelling |
ftdatacite:10.1594/pangaea.892827 2023-05-15T17:51:07+02:00 Seawater carbonate chemistry and community structure of marine biofouling communities, supplement to: Brown, Norah E M; Milazzo, Marco; Rastrick, S P S; Hall-Spencer, Jason M; Therriault, Thomas W; Harley, Christopher D G (2018): Natural acidification changes the timing and rate of succession, alters community structure, and increases homogeneity in marine biofouling communities. Global Change Biology, 24(1), e112-e127 Brown, Norah E M Milazzo, Marco Rastrick, S P S Hall-Spencer, Jason M Therriault, Thomas W Harley, Christopher D G 2018 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.892827 https://doi.pangaea.de/10.1594/PANGAEA.892827 en eng PANGAEA - Data Publisher for Earth & Environmental Science https://cran.r-project.org/package=seacarb https://dx.doi.org/10.1111/gcb.13856 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 CO2 vent Coast and continental shelf Community composition and diversity Entire community Field experiment Mediterranean Sea Rocky-shore community Temperate Type Identification Time in weeks Site Individuals Number of species Shannon Diversity Index Temperature, water Temperature, water, standard deviation Salinity Salinity, standard deviation pH pH, standard deviation Alkalinity, total Alkalinity, total, standard deviation Partial pressure of carbon dioxide water at sea surface temperature wet air Partial pressure of carbon dioxide, standard deviation Carbon, inorganic, dissolved Carbon, inorganic, dissolved, standard deviation Bicarbonate ion Bicarbonate ion, standard deviation Calcite saturation state Calcite saturation state, standard deviation Aragonite saturation state Aragonite saturation state, standard deviation Carbonate system computation flag Carbon dioxide Fugacity of carbon dioxide water at sea surface temperature wet air Carbonate ion Experiment Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. 2010 Ocean Acidification International Coordination Centre OA-ICC Supplementary Dataset dataset Dataset 2018 ftdatacite https://doi.org/10.1594/pangaea.892827 https://doi.org/10.1111/gcb.13856 2021-11-05T12:55:41Z Ocean acidification may have far-reaching consequences for marine community and ecosystem dynamics, but its full impacts remain poorly understood due to the difficulty of manipulating pCO2 at the ecosystem level to mimic realistic fluctuations that occur on a number of different timescales. It is especially unclear how quickly communities at various stages of development respond to intermediate-scale pCO2 change and, if high pCO2 is relieved mid-succession, whether past acidification effects persist, are reversed by alleviation of pCO2 stress, or are worsened by departures from prior high pCO2 conditions to which organisms had acclimatized. Here, we used reciprocal transplant experiments along a shallow water volcanic pCO2 gradient to assess the importance of the timing and duration of high pCO2 exposure (i.e. discrete events at different stages of successional development vs. continuous exposure) on patterns of colonization and succession in a benthic fouling community. We show that succession at the acidified site was initially delayed (less community change by eight weeks) but then caught up over the next four weeks. These changes in succession led to homogenization of communities maintained in or transplanted to acidified conditions, and altered community structure in ways that reflected both short- and longer-term acidification history. These community shifts are likely a result of interspecific variability in response to increased pCO2 and changes in species interactions. High pCO2 altered biofilm development, allowing serpulids to do best at the acidified site by the end of the experiment, although early (pre-transplant), negative effects of pCO2 on recruitment of these worms was still detectable. The ascidians Diplosoma sp. and Botryllus sp. settled later and were more tolerant to acidification. Overall, transient and persistent acidification-driven changes in the biofouling community, via both past and more recent exposure, could have important implications for ecosystem function and food web dynamics. : In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2016) 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 2018-08-06. Dataset Ocean acidification DataCite Metadata Store (German National Library of Science and Technology) |