Dynamics of seawater carbonate chemistry, production, and calcification of a coral reef flat, central Great Barrier Reef

Ocean acidification is projected to shift coral reefs from a state of net accretion to one of net dissolution this century. Presently, our ability to predict global-scale changes to coral reef calcification is limited by insufficient data relating seawater carbonate chemistry parameters to in situ r...

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Published in:Biogeosciences
Main Authors: Albright, R., Langdon, C., Anthony, K. R. N.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/bg-10-6747-2013
https://www.biogeosciences.net/10/6747/2013/
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spelling ftcopernicus:oai:publications.copernicus.org:bg19837 2023-05-15T17:51:57+02:00 Dynamics of seawater carbonate chemistry, production, and calcification of a coral reef flat, central Great Barrier Reef Albright, R. Langdon, C. Anthony, K. R. N. 2018-09-27 application/pdf https://doi.org/10.5194/bg-10-6747-2013 https://www.biogeosciences.net/10/6747/2013/ eng eng doi:10.5194/bg-10-6747-2013 https://www.biogeosciences.net/10/6747/2013/ eISSN: 1726-4189 Text 2018 ftcopernicus https://doi.org/10.5194/bg-10-6747-2013 2019-12-24T09:54:56Z Ocean acidification is projected to shift coral reefs from a state of net accretion to one of net dissolution this century. Presently, our ability to predict global-scale changes to coral reef calcification is limited by insufficient data relating seawater carbonate chemistry parameters to in situ rates of reef calcification. Here, we investigate diel and seasonal trends in carbonate chemistry of the Davies Reef flat in the central Great Barrier Reef and relate these trends to benthic carbon fluxes by quantifying net ecosystem calcification (nec) and net community production (ncp). Results show that seawater carbonate chemistry of the Davies Reef flat is highly variable over both diel and seasonal cycles. pH (total scale) ranged from 7.92 to 8.17, p CO 2 ranged from 272 to 542 μatm, and aragonite saturation state (Ω arag ) ranged from 2.9 to 4.1. Diel cycles in carbonate chemistry were primarily driven by ncp, and warming explained 35% and 47% of the seasonal shifts in p CO 2 and pH, respectively. Daytime ncp averaged 37 ± 19 mmol C m −2 h −1 in summer and 33 ± 13 mmol C m −2 h −1 in winter; nighttime ncp averaged −30 ± 25 and −7 ± 6 mmol C m −2 h −1 in summer and winter, respectively. Daytime nec averaged 11 ± 4 mmol CaCO 3 m −2 h −1 in summer and 8 ± 3 mmol CaCO 3 m −2 h −1 in winter, whereas nighttime nec averaged 2 ± 4 mmol and −1 ± 3 mmol CaCO 3 m −2 h −1 in summer and winter, respectively. Net ecosystem calcification was highly sensitive to changes in Ω arag for both seasons, indicating that relatively small shifts in Ω arag may drive measurable shifts in calcification rates, and hence carbon budgets, of coral reefs throughout the year. Text Ocean acidification Copernicus Publications: E-Journals Biogeosciences 10 10 6747 6758
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collection Copernicus Publications: E-Journals
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language English
description Ocean acidification is projected to shift coral reefs from a state of net accretion to one of net dissolution this century. Presently, our ability to predict global-scale changes to coral reef calcification is limited by insufficient data relating seawater carbonate chemistry parameters to in situ rates of reef calcification. Here, we investigate diel and seasonal trends in carbonate chemistry of the Davies Reef flat in the central Great Barrier Reef and relate these trends to benthic carbon fluxes by quantifying net ecosystem calcification (nec) and net community production (ncp). Results show that seawater carbonate chemistry of the Davies Reef flat is highly variable over both diel and seasonal cycles. pH (total scale) ranged from 7.92 to 8.17, p CO 2 ranged from 272 to 542 μatm, and aragonite saturation state (Ω arag ) ranged from 2.9 to 4.1. Diel cycles in carbonate chemistry were primarily driven by ncp, and warming explained 35% and 47% of the seasonal shifts in p CO 2 and pH, respectively. Daytime ncp averaged 37 ± 19 mmol C m −2 h −1 in summer and 33 ± 13 mmol C m −2 h −1 in winter; nighttime ncp averaged −30 ± 25 and −7 ± 6 mmol C m −2 h −1 in summer and winter, respectively. Daytime nec averaged 11 ± 4 mmol CaCO 3 m −2 h −1 in summer and 8 ± 3 mmol CaCO 3 m −2 h −1 in winter, whereas nighttime nec averaged 2 ± 4 mmol and −1 ± 3 mmol CaCO 3 m −2 h −1 in summer and winter, respectively. Net ecosystem calcification was highly sensitive to changes in Ω arag for both seasons, indicating that relatively small shifts in Ω arag may drive measurable shifts in calcification rates, and hence carbon budgets, of coral reefs throughout the year.
format Text
author Albright, R.
Langdon, C.
Anthony, K. R. N.
spellingShingle Albright, R.
Langdon, C.
Anthony, K. R. N.
Dynamics of seawater carbonate chemistry, production, and calcification of a coral reef flat, central Great Barrier Reef
author_facet Albright, R.
Langdon, C.
Anthony, K. R. N.
author_sort Albright, R.
title Dynamics of seawater carbonate chemistry, production, and calcification of a coral reef flat, central Great Barrier Reef
title_short Dynamics of seawater carbonate chemistry, production, and calcification of a coral reef flat, central Great Barrier Reef
title_full Dynamics of seawater carbonate chemistry, production, and calcification of a coral reef flat, central Great Barrier Reef
title_fullStr Dynamics of seawater carbonate chemistry, production, and calcification of a coral reef flat, central Great Barrier Reef
title_full_unstemmed Dynamics of seawater carbonate chemistry, production, and calcification of a coral reef flat, central Great Barrier Reef
title_sort dynamics of seawater carbonate chemistry, production, and calcification of a coral reef flat, central great barrier reef
publishDate 2018
url https://doi.org/10.5194/bg-10-6747-2013
https://www.biogeosciences.net/10/6747/2013/
genre Ocean acidification
genre_facet Ocean acidification
op_source eISSN: 1726-4189
op_relation doi:10.5194/bg-10-6747-2013
https://www.biogeosciences.net/10/6747/2013/
op_doi https://doi.org/10.5194/bg-10-6747-2013
container_title Biogeosciences
container_volume 10
container_issue 10
container_start_page 6747
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