Seawater carbonate chemistry and calcification response of a tropical scleractinian coral to seasonal upwelling conditions
Natural processes such as upwelling of deeper-water masses change the physical-chemical conditions of the water column creating localized ocean acidification events that can have an impact on the natural communities. This study was performed in a coral reef system of an archetypical bay within the T...
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2023
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.960154 2023-08-20T04:08:34+02:00 Seawater carbonate chemistry and calcification response of a tropical scleractinian coral to seasonal upwelling conditions Gómez, C E Acosta-Chaparro, Andrés Bernal, Cesar A Gómez-López, Diana I Navas-Camacho, Raúl Alonso, David LATITUDE: 11.333300 * LONGITUDE: -74.133300 * DATE/TIME START: 2020-12-02T00:00:00 * DATE/TIME END: 2021-05-14T00:00:00 * MINIMUM DEPTH, water: 11.0 m * MAXIMUM DEPTH, water: 13.5 m 2023 text/tab-separated-values, 791 data points https://doi.pangaea.de/10.1594/PANGAEA.960154 https://doi.org/10.1594/PANGAEA.960154 en eng PANGAEA Gómez, Carlos E; Acosta-Chaparro, Andrés; Bernal, Cesar A; Gómez-López, Diana I; Navas-Camacho, Raúl; Alonso, David (2023): Seasonal Upwelling Conditions Modulate the Calcification Response of a Tropical Scleractinian Coral. Oceans, 4(2), 170-184, https://doi.org/10.3390/oceans4020012 Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse; Orr, James; Gentili, Bernard; Hagens, Mathilde; Hofmann, Andreas; Mueller, Jens-Daniel; Proye, Aurélien; Rae, James; Soetaert, Karline (2022): seacarb: seawater carbonate chemistry with R. R package version 3.3.1. https://cran.r-project.org/web/packages/seacarb/index.html https://doi.pangaea.de/10.1594/PANGAEA.960154 https://doi.org/10.1594/PANGAEA.960154 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess Alkalinity total Aragonite saturation state Benthos Bicarbonate ion Calcification/Dissolution Calcite saturation state Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Chamber volume Coast and continental shelf Coral fragments DATE/TIME DEPTH water Entire community EXP Experiment Field observation Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Net calcification rate of calcium carbonate Net dissolution rate of calcium carbonate North Atlantic OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) pH Rocky-shore community Salinity Tayrona_National_Natural_Park Temperature Time in minutes Tropical Type of study Upwelling Volume Dataset 2023 ftpangaea https://doi.org/10.1594/PANGAEA.96015410.3390/oceans4020012 2023-07-31T10:23:12Z Natural processes such as upwelling of deeper-water masses change the physical-chemical conditions of the water column creating localized ocean acidification events that can have an impact on the natural communities. This study was performed in a coral reef system of an archetypical bay within the Tayrona National Natural Park (PNNT) (Colombia), and aimed to quantify net calcification rates of a foundational coral species within a temporal context (6 months) taking into account the dynamics of seasonal upwelling that influence the study area. Net calcification rates of coral fragments were obtained in situ by the alkalinity anomaly technique in short-term incubations (~2.5 h). We found a significant effect of the upwelling on net calcification rates (Gnet) (p < 0.05) with an 42% increase in CaCO3 accretion compared to non-upwelling season. We found an increase in total alkalinity (AT) and dissolved inorganic carbon (DIC) with decreased aragonite saturation (Ωara) for the upwelling months, indicating an influence of the Subtropical Under Water mass (SAW) in the PNNT coral community. Significant negative correlations between net calcification with temperature and Ωara, which indicates a positive response of M. auretenra with the upwelling conditions, thus, acting as “enhancer” of resilience for coral calcification. Dataset North Atlantic Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-74.133300,-74.133300,11.333300,11.333300) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Alkalinity total Aragonite saturation state Benthos Bicarbonate ion Calcification/Dissolution Calcite saturation state Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Chamber volume Coast and continental shelf Coral fragments DATE/TIME DEPTH water Entire community EXP Experiment Field observation Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Net calcification rate of calcium carbonate Net dissolution rate of calcium carbonate North Atlantic OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) pH Rocky-shore community Salinity Tayrona_National_Natural_Park Temperature Time in minutes Tropical Type of study Upwelling Volume |
spellingShingle |
Alkalinity total Aragonite saturation state Benthos Bicarbonate ion Calcification/Dissolution Calcite saturation state Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Chamber volume Coast and continental shelf Coral fragments DATE/TIME DEPTH water Entire community EXP Experiment Field observation Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Net calcification rate of calcium carbonate Net dissolution rate of calcium carbonate North Atlantic OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) pH Rocky-shore community Salinity Tayrona_National_Natural_Park Temperature Time in minutes Tropical Type of study Upwelling Volume Gómez, C E Acosta-Chaparro, Andrés Bernal, Cesar A Gómez-López, Diana I Navas-Camacho, Raúl Alonso, David Seawater carbonate chemistry and calcification response of a tropical scleractinian coral to seasonal upwelling conditions |
topic_facet |
Alkalinity total Aragonite saturation state Benthos Bicarbonate ion Calcification/Dissolution Calcite saturation state Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Chamber volume Coast and continental shelf Coral fragments DATE/TIME DEPTH water Entire community EXP Experiment Field observation Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Net calcification rate of calcium carbonate Net dissolution rate of calcium carbonate North Atlantic OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) pH Rocky-shore community Salinity Tayrona_National_Natural_Park Temperature Time in minutes Tropical Type of study Upwelling Volume |
description |
Natural processes such as upwelling of deeper-water masses change the physical-chemical conditions of the water column creating localized ocean acidification events that can have an impact on the natural communities. This study was performed in a coral reef system of an archetypical bay within the Tayrona National Natural Park (PNNT) (Colombia), and aimed to quantify net calcification rates of a foundational coral species within a temporal context (6 months) taking into account the dynamics of seasonal upwelling that influence the study area. Net calcification rates of coral fragments were obtained in situ by the alkalinity anomaly technique in short-term incubations (~2.5 h). We found a significant effect of the upwelling on net calcification rates (Gnet) (p < 0.05) with an 42% increase in CaCO3 accretion compared to non-upwelling season. We found an increase in total alkalinity (AT) and dissolved inorganic carbon (DIC) with decreased aragonite saturation (Ωara) for the upwelling months, indicating an influence of the Subtropical Under Water mass (SAW) in the PNNT coral community. Significant negative correlations between net calcification with temperature and Ωara, which indicates a positive response of M. auretenra with the upwelling conditions, thus, acting as “enhancer” of resilience for coral calcification. |
format |
Dataset |
author |
Gómez, C E Acosta-Chaparro, Andrés Bernal, Cesar A Gómez-López, Diana I Navas-Camacho, Raúl Alonso, David |
author_facet |
Gómez, C E Acosta-Chaparro, Andrés Bernal, Cesar A Gómez-López, Diana I Navas-Camacho, Raúl Alonso, David |
author_sort |
Gómez, C E |
title |
Seawater carbonate chemistry and calcification response of a tropical scleractinian coral to seasonal upwelling conditions |
title_short |
Seawater carbonate chemistry and calcification response of a tropical scleractinian coral to seasonal upwelling conditions |
title_full |
Seawater carbonate chemistry and calcification response of a tropical scleractinian coral to seasonal upwelling conditions |
title_fullStr |
Seawater carbonate chemistry and calcification response of a tropical scleractinian coral to seasonal upwelling conditions |
title_full_unstemmed |
Seawater carbonate chemistry and calcification response of a tropical scleractinian coral to seasonal upwelling conditions |
title_sort |
seawater carbonate chemistry and calcification response of a tropical scleractinian coral to seasonal upwelling conditions |
publisher |
PANGAEA |
publishDate |
2023 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.960154 https://doi.org/10.1594/PANGAEA.960154 |
op_coverage |
LATITUDE: 11.333300 * LONGITUDE: -74.133300 * DATE/TIME START: 2020-12-02T00:00:00 * DATE/TIME END: 2021-05-14T00:00:00 * MINIMUM DEPTH, water: 11.0 m * MAXIMUM DEPTH, water: 13.5 m |
long_lat |
ENVELOPE(-74.133300,-74.133300,11.333300,11.333300) |
genre |
North Atlantic Ocean acidification |
genre_facet |
North Atlantic Ocean acidification |
op_relation |
Gómez, Carlos E; Acosta-Chaparro, Andrés; Bernal, Cesar A; Gómez-López, Diana I; Navas-Camacho, Raúl; Alonso, David (2023): Seasonal Upwelling Conditions Modulate the Calcification Response of a Tropical Scleractinian Coral. Oceans, 4(2), 170-184, https://doi.org/10.3390/oceans4020012 Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse; Orr, James; Gentili, Bernard; Hagens, Mathilde; Hofmann, Andreas; Mueller, Jens-Daniel; Proye, Aurélien; Rae, James; Soetaert, Karline (2022): seacarb: seawater carbonate chemistry with R. R package version 3.3.1. https://cran.r-project.org/web/packages/seacarb/index.html https://doi.pangaea.de/10.1594/PANGAEA.960154 https://doi.org/10.1594/PANGAEA.960154 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.96015410.3390/oceans4020012 |
_version_ |
1774720894320508928 |