Pteropods make thinner shells in the upwelling region of the California Current Ecosystem

Abstract Shelled pteropods are widely regarded as bioindicators for ocean acidification, because their fragile aragonite shells are susceptible to increasing ocean acidity. While short-term incubations have demonstrated that pteropod calcification is negatively impacted by ocean acidification, we kn...

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Autores principales: Lisette Mekkes, Willem Renema, Nina Bednaršek, Simone R. Alin, Richard A. Feely, Jef Huisman, Peter Roessingh, Katja T. C. A. Peijnenburg
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Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/44c8e37109c74af5b1becdb126ebe6f0
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spelling oai:doaj.org-article:44c8e37109c74af5b1becdb126ebe6f02021-12-02T13:56:48ZPteropods make thinner shells in the upwelling region of the California Current Ecosystem10.1038/s41598-021-81131-92045-2322https://doaj.org/article/44c8e37109c74af5b1becdb126ebe6f02021-01-01T00:00:00Zhttps://doi.org/10.1038/s41598-021-81131-9https://doaj.org/toc/2045-2322Abstract Shelled pteropods are widely regarded as bioindicators for ocean acidification, because their fragile aragonite shells are susceptible to increasing ocean acidity. While short-term incubations have demonstrated that pteropod calcification is negatively impacted by ocean acidification, we know little about net calcification in response to varying ocean conditions in natural populations. Here, we examine in situ calcification of Limacina helicina pteropods collected from the California Current Ecosystem, a coastal upwelling system with strong spatial gradients in ocean carbonate chemistry, dissolved oxygen and temperature. Depth-averaged pH ranged from 8.03 in warmer offshore waters to 7.77 in cold CO2-rich waters nearshore. Based on high-resolution micro-CT technology, we showed that shell thickness declined by ~ 37% along the upwelling gradient from offshore to nearshore water. Dissolution marks covered only ~ 2% of the shell surface area and were not associated with the observed variation in shell thickness. We thus infer that pteropods make thinner shells where upwelling brings more acidified and colder waters to the surface. Probably the thinner shells do not result from enhanced dissolution, but are due to a decline in calcification. Reduced calcification of pteropods is likely to have major ecological and biogeochemical implications for the cycling of calcium carbonate in the oceans.Lisette MekkesWillem RenemaNina BednaršekSimone R. AlinRichard A. FeelyJef HuismanPeter RoessinghKatja T. C. A. PeijnenburgNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 11, Iss 1, Pp 1-11 (2021)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Lisette Mekkes
Willem Renema
Nina Bednaršek
Simone R. Alin
Richard A. Feely
Jef Huisman
Peter Roessingh
Katja T. C. A. Peijnenburg
Pteropods make thinner shells in the upwelling region of the California Current Ecosystem
description Abstract Shelled pteropods are widely regarded as bioindicators for ocean acidification, because their fragile aragonite shells are susceptible to increasing ocean acidity. While short-term incubations have demonstrated that pteropod calcification is negatively impacted by ocean acidification, we know little about net calcification in response to varying ocean conditions in natural populations. Here, we examine in situ calcification of Limacina helicina pteropods collected from the California Current Ecosystem, a coastal upwelling system with strong spatial gradients in ocean carbonate chemistry, dissolved oxygen and temperature. Depth-averaged pH ranged from 8.03 in warmer offshore waters to 7.77 in cold CO2-rich waters nearshore. Based on high-resolution micro-CT technology, we showed that shell thickness declined by ~ 37% along the upwelling gradient from offshore to nearshore water. Dissolution marks covered only ~ 2% of the shell surface area and were not associated with the observed variation in shell thickness. We thus infer that pteropods make thinner shells where upwelling brings more acidified and colder waters to the surface. Probably the thinner shells do not result from enhanced dissolution, but are due to a decline in calcification. Reduced calcification of pteropods is likely to have major ecological and biogeochemical implications for the cycling of calcium carbonate in the oceans.
format article
author Lisette Mekkes
Willem Renema
Nina Bednaršek
Simone R. Alin
Richard A. Feely
Jef Huisman
Peter Roessingh
Katja T. C. A. Peijnenburg
author_facet Lisette Mekkes
Willem Renema
Nina Bednaršek
Simone R. Alin
Richard A. Feely
Jef Huisman
Peter Roessingh
Katja T. C. A. Peijnenburg
author_sort Lisette Mekkes
title Pteropods make thinner shells in the upwelling region of the California Current Ecosystem
title_short Pteropods make thinner shells in the upwelling region of the California Current Ecosystem
title_full Pteropods make thinner shells in the upwelling region of the California Current Ecosystem
title_fullStr Pteropods make thinner shells in the upwelling region of the California Current Ecosystem
title_full_unstemmed Pteropods make thinner shells in the upwelling region of the California Current Ecosystem
title_sort pteropods make thinner shells in the upwelling region of the california current ecosystem
publisher Nature Portfolio
publishDate 2021
url https://doaj.org/article/44c8e37109c74af5b1becdb126ebe6f0
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