Buffer Capacity, Ecosystem Feedbacks, and Seawater Chemistry under Global Change

Ocean acidification (OA) results in reduced seawater pH and aragonite saturation state (Ωarag), but also reduced seawater buffer capacity. As buffer capacity decreases, diel variation in seawater chemistry increases. However, a variety of ecosystem feedbacks can modulate changes in both average seaw...

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Published in:Water
Main Authors: Robert J. Toonen, Marlin J. Atkinson, Florence I.M. Thomas, Christopher P. Jury
Format: Article in Journal/Newspaper
Language:English
Published: MDPI AG 2013
Subjects:
pH
Online Access:https://doi.org/10.3390/w5031303
https://doaj.org/article/7b4646c7880742e481faa6c45e0a7657
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spelling ftdoajarticles:oai:doaj.org/article:7b4646c7880742e481faa6c45e0a7657 2023-05-15T17:50:35+02:00 Buffer Capacity, Ecosystem Feedbacks, and Seawater Chemistry under Global Change Robert J. Toonen Marlin J. Atkinson Florence I.M. Thomas Christopher P. Jury 2013-09-01T00:00:00Z https://doi.org/10.3390/w5031303 https://doaj.org/article/7b4646c7880742e481faa6c45e0a7657 EN eng MDPI AG http://www.mdpi.com/2073-4441/5/3/1303 https://doaj.org/toc/2073-4441 doi:10.3390/w5031303 2073-4441 https://doaj.org/article/7b4646c7880742e481faa6c45e0a7657 Water, Vol 5, Iss 3, Pp 1303-1325 (2013) ocean acidification climate change coral reef ecosystem modeling calcification aragonite saturation carbonate pH Hydraulic engineering TC1-978 Water supply for domestic and industrial purposes TD201-500 article 2013 ftdoajarticles https://doi.org/10.3390/w5031303 2022-12-31T14:26:03Z Ocean acidification (OA) results in reduced seawater pH and aragonite saturation state (Ωarag), but also reduced seawater buffer capacity. As buffer capacity decreases, diel variation in seawater chemistry increases. However, a variety of ecosystem feedbacks can modulate changes in both average seawater chemistry and diel seawater chemistry variation. Here we model these effects for a coastal, reef flat ecosystem. We show that an increase in offshore pCO2 and temperature (to 900 µatm and + 3 °C) can increase diel pH variation by as much as a factor of 2.5 and can increase diel pCO2 variation by a factor of 4.6, depending on ecosystem feedbacks and seawater residence time. Importantly, these effects are different between day and night. With increasing seawater residence time and increasing feedback intensity, daytime seawater chemistry becomes more similar to present-day conditions while nighttime seawater chemistry becomes less similar to present-day conditions. Recent studies suggest that carbonate chemistry variation itself, independent of the average chemistry conditions, can have important effects on marine organisms and ecosystem processes. Better constraining ecosystem feedbacks under global change will improve projections of coastal water chemistry, but this study shows the importance of considering changes in both average carbonate chemistry and diel chemistry variation for organisms and ecosystems. Article in Journal/Newspaper Ocean acidification Directory of Open Access Journals: DOAJ Articles Water 5 3 1303 1325
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic ocean acidification
climate change
coral reef
ecosystem modeling
calcification
aragonite saturation
carbonate
pH
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
spellingShingle ocean acidification
climate change
coral reef
ecosystem modeling
calcification
aragonite saturation
carbonate
pH
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
Robert J. Toonen
Marlin J. Atkinson
Florence I.M. Thomas
Christopher P. Jury
Buffer Capacity, Ecosystem Feedbacks, and Seawater Chemistry under Global Change
topic_facet ocean acidification
climate change
coral reef
ecosystem modeling
calcification
aragonite saturation
carbonate
pH
Hydraulic engineering
TC1-978
Water supply for domestic and industrial purposes
TD201-500
description Ocean acidification (OA) results in reduced seawater pH and aragonite saturation state (Ωarag), but also reduced seawater buffer capacity. As buffer capacity decreases, diel variation in seawater chemistry increases. However, a variety of ecosystem feedbacks can modulate changes in both average seawater chemistry and diel seawater chemistry variation. Here we model these effects for a coastal, reef flat ecosystem. We show that an increase in offshore pCO2 and temperature (to 900 µatm and + 3 °C) can increase diel pH variation by as much as a factor of 2.5 and can increase diel pCO2 variation by a factor of 4.6, depending on ecosystem feedbacks and seawater residence time. Importantly, these effects are different between day and night. With increasing seawater residence time and increasing feedback intensity, daytime seawater chemistry becomes more similar to present-day conditions while nighttime seawater chemistry becomes less similar to present-day conditions. Recent studies suggest that carbonate chemistry variation itself, independent of the average chemistry conditions, can have important effects on marine organisms and ecosystem processes. Better constraining ecosystem feedbacks under global change will improve projections of coastal water chemistry, but this study shows the importance of considering changes in both average carbonate chemistry and diel chemistry variation for organisms and ecosystems.
format Article in Journal/Newspaper
author Robert J. Toonen
Marlin J. Atkinson
Florence I.M. Thomas
Christopher P. Jury
author_facet Robert J. Toonen
Marlin J. Atkinson
Florence I.M. Thomas
Christopher P. Jury
author_sort Robert J. Toonen
title Buffer Capacity, Ecosystem Feedbacks, and Seawater Chemistry under Global Change
title_short Buffer Capacity, Ecosystem Feedbacks, and Seawater Chemistry under Global Change
title_full Buffer Capacity, Ecosystem Feedbacks, and Seawater Chemistry under Global Change
title_fullStr Buffer Capacity, Ecosystem Feedbacks, and Seawater Chemistry under Global Change
title_full_unstemmed Buffer Capacity, Ecosystem Feedbacks, and Seawater Chemistry under Global Change
title_sort buffer capacity, ecosystem feedbacks, and seawater chemistry under global change
publisher MDPI AG
publishDate 2013
url https://doi.org/10.3390/w5031303
https://doaj.org/article/7b4646c7880742e481faa6c45e0a7657
genre Ocean acidification
genre_facet Ocean acidification
op_source Water, Vol 5, Iss 3, Pp 1303-1325 (2013)
op_relation http://www.mdpi.com/2073-4441/5/3/1303
https://doaj.org/toc/2073-4441
doi:10.3390/w5031303
2073-4441
https://doaj.org/article/7b4646c7880742e481faa6c45e0a7657
op_doi https://doi.org/10.3390/w5031303
container_title Water
container_volume 5
container_issue 3
container_start_page 1303
op_container_end_page 1325
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