Environmental and chemical measurements, and coral calcification rates in Bermuda from 2010 to 2012
Modern reef-building corals sustain a wide range of ecosystem services because of their ability to build calcium carbonate reef systems. The influence of environmental variables on coral calcification rates has been extensively studied, but our understanding of their relative importance is limited b...
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Format: | Dataset |
Language: | English |
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PANGAEA
2017
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.892130 https://doi.org/10.1594/PANGAEA.892130 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.892130 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Alkalinity total Animalia Aragonite saturation state Benthic animals Benthos Bicarbonate ion Brightness Calcification/Dissolution Calcification rate Calcite saturation state Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Chlorophyll a Cnidaria Coast and continental shelf Crescent_Reef Date Diploria labyrinthiformis Entire community Event label EXP Experiment Field observation Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Hog_Reef LATITUDE LONGITUDE Month North Atlantic OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) pH Porites astreoides Rocky-shore community Salinity Score on PC1 Single species Temperate Temperature water Type Years |
spellingShingle |
Alkalinity total Animalia Aragonite saturation state Benthic animals Benthos Bicarbonate ion Brightness Calcification/Dissolution Calcification rate Calcite saturation state Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Chlorophyll a Cnidaria Coast and continental shelf Crescent_Reef Date Diploria labyrinthiformis Entire community Event label EXP Experiment Field observation Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Hog_Reef LATITUDE LONGITUDE Month North Atlantic OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) pH Porites astreoides Rocky-shore community Salinity Score on PC1 Single species Temperate Temperature water Type Years Courtney, Travis A Lebrato, Mario Bates, Nicolas R Collins, Andrew de Putron, Samantha J Garley, Rebecca Johnson, Rod Molinero, Juan-Carlos Noyes, Timothy J Sabine, Christopher L Andersson, Andreas J Yang, Yan Environmental and chemical measurements, and coral calcification rates in Bermuda from 2010 to 2012 |
topic_facet |
Alkalinity total Animalia Aragonite saturation state Benthic animals Benthos Bicarbonate ion Brightness Calcification/Dissolution Calcification rate Calcite saturation state Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Chlorophyll a Cnidaria Coast and continental shelf Crescent_Reef Date Diploria labyrinthiformis Entire community Event label EXP Experiment Field observation Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Hog_Reef LATITUDE LONGITUDE Month North Atlantic OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) pH Porites astreoides Rocky-shore community Salinity Score on PC1 Single species Temperate Temperature water Type Years |
description |
Modern reef-building corals sustain a wide range of ecosystem services because of their ability to build calcium carbonate reef systems. The influence of environmental variables on coral calcification rates has been extensively studied, but our understanding of their relative importance is limited by the absence of in situ observations and the ability to decouple the interactions between different properties. We show that temperature is the primary driver of coral colony (Porites astreoides and Diploria labyrinthiformis) and reef-scale calcification rates over a 2-year monitoring period from the Bermuda coral reef. On the basis of multimodel climate simulations (Coupled Model Intercomparison Project Phase 5) and assuming sufficient coral nutrition, our results suggest that P. astreoides and D. labyrinthiformis coral calcification rates in Bermuda could increase throughout the 21st century as a result of gradual warming predicted under a minimum CO2 emissions pathway [representative concentration pathway (RCP) 2.6] with positive 21st-century calcification rates potentially maintained under a reduced CO2 emissions pathway (RCP 4.5). These results highlight the potential benefits of rapid reductions in global anthropogenic CO2 emissions for 21st-century Bermuda coral reefs and the ecosystem services they provide. |
format |
Dataset |
author |
Courtney, Travis A Lebrato, Mario Bates, Nicolas R Collins, Andrew de Putron, Samantha J Garley, Rebecca Johnson, Rod Molinero, Juan-Carlos Noyes, Timothy J Sabine, Christopher L Andersson, Andreas J Yang, Yan |
author_facet |
Courtney, Travis A Lebrato, Mario Bates, Nicolas R Collins, Andrew de Putron, Samantha J Garley, Rebecca Johnson, Rod Molinero, Juan-Carlos Noyes, Timothy J Sabine, Christopher L Andersson, Andreas J Yang, Yan |
author_sort |
Courtney, Travis A |
title |
Environmental and chemical measurements, and coral calcification rates in Bermuda from 2010 to 2012 |
title_short |
Environmental and chemical measurements, and coral calcification rates in Bermuda from 2010 to 2012 |
title_full |
Environmental and chemical measurements, and coral calcification rates in Bermuda from 2010 to 2012 |
title_fullStr |
Environmental and chemical measurements, and coral calcification rates in Bermuda from 2010 to 2012 |
title_full_unstemmed |
Environmental and chemical measurements, and coral calcification rates in Bermuda from 2010 to 2012 |
title_sort |
environmental and chemical measurements, and coral calcification rates in bermuda from 2010 to 2012 |
publisher |
PANGAEA |
publishDate |
2017 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.892130 https://doi.org/10.1594/PANGAEA.892130 |
op_coverage |
MEDIAN LATITUDE: 32.443044 * MEDIAN LONGITUDE: -64.825339 * SOUTH-BOUND LATITUDE: 32.400780 * WEST-BOUND LONGITUDE: -64.834760 * NORTH-BOUND LATITUDE: 32.457330 * EAST-BOUND LONGITUDE: -64.797470 * DATE/TIME START: 2010-09-01T00:00:00 * DATE/TIME END: 2012-08-09T00:00:00 |
long_lat |
ENVELOPE(-64.834760,-64.797470,32.457330,32.400780) |
genre |
North Atlantic Ocean acidification |
genre_facet |
North Atlantic Ocean acidification |
op_source |
Supplement to: Courtney, Travis A; Lebrato, Mario; Bates, Nicolas R; Collins, Andrew; de Putron, Samantha J; Garley, Rebecca; Johnson, Rod; Molinero, Juan-Carlos; Noyes, Timothy J; Sabine, Christopher L; Andersson, Andreas J (2017): Environmental controls on modern scleractinian coral and reef-scale calcification. Science Advances, 3(11), e1701356, https://doi.org/10.1126/sciadv.1701356 |
op_relation |
Andersson, Andreas J; Bates, Nicolas R (2018): Dataset: Bermuda Structural Equation Modeling Data. Biological and Chemical Oceanography Data Management Office, https://www.bco-dmo.org/dataset/720788 Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse; Orr, James C; Gentili, Bernard; Proye, Aurélien; Soetaert, Karline; Rae, James (2016): seacarb: seawater carbonate chemistry with R. R package version 3.1. https://cran.r-project.org/package=seacarb https://doi.pangaea.de/10.1594/PANGAEA.892130 https://doi.org/10.1594/PANGAEA.892130 |
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.892130 https://doi.org/10.1126/sciadv.1701356 |
_version_ |
1766136622741454848 |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.892130 2023-05-15T17:36:57+02:00 Environmental and chemical measurements, and coral calcification rates in Bermuda from 2010 to 2012 Courtney, Travis A Lebrato, Mario Bates, Nicolas R Collins, Andrew de Putron, Samantha J Garley, Rebecca Johnson, Rod Molinero, Juan-Carlos Noyes, Timothy J Sabine, Christopher L Andersson, Andreas J Yang, Yan MEDIAN LATITUDE: 32.443044 * MEDIAN LONGITUDE: -64.825339 * SOUTH-BOUND LATITUDE: 32.400780 * WEST-BOUND LONGITUDE: -64.834760 * NORTH-BOUND LATITUDE: 32.457330 * EAST-BOUND LONGITUDE: -64.797470 * DATE/TIME START: 2010-09-01T00:00:00 * DATE/TIME END: 2012-08-09T00:00:00 2017-07-04 text/tab-separated-values, 2280 data points https://doi.pangaea.de/10.1594/PANGAEA.892130 https://doi.org/10.1594/PANGAEA.892130 en eng PANGAEA Andersson, Andreas J; Bates, Nicolas R (2018): Dataset: Bermuda Structural Equation Modeling Data. Biological and Chemical Oceanography Data Management Office, https://www.bco-dmo.org/dataset/720788 Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse; Orr, James C; Gentili, Bernard; Proye, Aurélien; Soetaert, Karline; Rae, James (2016): seacarb: seawater carbonate chemistry with R. R package version 3.1. https://cran.r-project.org/package=seacarb https://doi.pangaea.de/10.1594/PANGAEA.892130 https://doi.org/10.1594/PANGAEA.892130 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Courtney, Travis A; Lebrato, Mario; Bates, Nicolas R; Collins, Andrew; de Putron, Samantha J; Garley, Rebecca; Johnson, Rod; Molinero, Juan-Carlos; Noyes, Timothy J; Sabine, Christopher L; Andersson, Andreas J (2017): Environmental controls on modern scleractinian coral and reef-scale calcification. Science Advances, 3(11), e1701356, https://doi.org/10.1126/sciadv.1701356 Alkalinity total Animalia Aragonite saturation state Benthic animals Benthos Bicarbonate ion Brightness Calcification/Dissolution Calcification rate Calcite saturation state Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Chlorophyll a Cnidaria Coast and continental shelf Crescent_Reef Date Diploria labyrinthiformis Entire community Event label EXP Experiment Field observation Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Hog_Reef LATITUDE LONGITUDE Month North Atlantic OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) pH Porites astreoides Rocky-shore community Salinity Score on PC1 Single species Temperate Temperature water Type Years Dataset 2017 ftpangaea https://doi.org/10.1594/PANGAEA.892130 https://doi.org/10.1126/sciadv.1701356 2023-01-20T09:11:17Z Modern reef-building corals sustain a wide range of ecosystem services because of their ability to build calcium carbonate reef systems. The influence of environmental variables on coral calcification rates has been extensively studied, but our understanding of their relative importance is limited by the absence of in situ observations and the ability to decouple the interactions between different properties. We show that temperature is the primary driver of coral colony (Porites astreoides and Diploria labyrinthiformis) and reef-scale calcification rates over a 2-year monitoring period from the Bermuda coral reef. On the basis of multimodel climate simulations (Coupled Model Intercomparison Project Phase 5) and assuming sufficient coral nutrition, our results suggest that P. astreoides and D. labyrinthiformis coral calcification rates in Bermuda could increase throughout the 21st century as a result of gradual warming predicted under a minimum CO2 emissions pathway [representative concentration pathway (RCP) 2.6] with positive 21st-century calcification rates potentially maintained under a reduced CO2 emissions pathway (RCP 4.5). These results highlight the potential benefits of rapid reductions in global anthropogenic CO2 emissions for 21st-century Bermuda coral reefs and the ecosystem services they provide. Dataset North Atlantic Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-64.834760,-64.797470,32.457330,32.400780) |