Bivalve shell formation in a naturally CO2-enriched habitat: Unraveling the resilience mechanisms from elemental signatures
Marine bivalves inhabiting naturally pCO2-enriched habitats can likely tolerate high levels of acidification. Consequently, elucidating the mechanisms behind such resilience can help to predict the fate of this economically and ecologically important group under near-future scenarios of CO2-driven o...
Published in: | Chemosphere |
---|---|
Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2018
|
Subjects: | |
Online Access: | http://hdl.handle.net/21.11116/0000-0000-F9D6-6 |
id |
ftpubman:oai:pure.mpg.de:item_2566842 |
---|---|
record_format |
openpolar |
spelling |
ftpubman:oai:pure.mpg.de:item_2566842 2023-08-27T04:11:22+02:00 Bivalve shell formation in a naturally CO2-enriched habitat: Unraveling the resilience mechanisms from elemental signatures Zhao, L. Milano, S. Walliser, E. Schöne, B. 2018-07 http://hdl.handle.net/21.11116/0000-0000-F9D6-6 eng eng info:eu-repo/semantics/altIdentifier/doi/10.1016/j.chemosphere.2018.03.180 http://hdl.handle.net/21.11116/0000-0000-F9D6-6 Chemosphere info:eu-repo/semantics/article 2018 ftpubman https://doi.org/10.1016/j.chemosphere.2018.03.180 2023-08-02T01:24:49Z Marine bivalves inhabiting naturally pCO2-enriched habitats can likely tolerate high levels of acidification. Consequently, elucidating the mechanisms behind such resilience can help to predict the fate of this economically and ecologically important group under near-future scenarios of CO2-driven ocean acidification. Here, we assess the effects of four environmentally realistic pCO2 levels (900, 1500, 2900 and 6600 μatm) on the shell production rate of Mya arenaria juveniles originating from a periodically pCO2-enriched habitat (Kiel Fjord, Western Baltic Sea). We find a significant decline in the rate of shell growth as pCO2 increases, but also observe unchanged shell formation rates at moderate pCO2 levels of 1500 and 2900 μatm, the latter illustrating the capacity of the juveniles to partially mitigate the impact of high pCO2. Using recently developed geochemical tracers we show that M. arenaria exposed to a natural pCO2 gradient from 900 to 2900 μatm can likely concentrate HCO3– in the calcifying fluid through the exchange of HCO3–/Cl– and simultaneously maintain the pH homeostasis through active removal of protons, thereby being able to sustain the rate of shell formation to a certain extent. However, with increasing pCO2 beyond natural maximum the bivalves may have limited capacity to compensate for changes in the calcifying fluid chemistry, showing significant shell growth reduction. Findings of the present study may pave the way for elucidating the underlying mechanisms by which marine bivalves acclimate and adapt to high seawater pCO2. Article in Journal/Newspaper Ocean acidification Max Planck Society: MPG.PuRe Chemosphere 203 132 138 |
institution |
Open Polar |
collection |
Max Planck Society: MPG.PuRe |
op_collection_id |
ftpubman |
language |
English |
description |
Marine bivalves inhabiting naturally pCO2-enriched habitats can likely tolerate high levels of acidification. Consequently, elucidating the mechanisms behind such resilience can help to predict the fate of this economically and ecologically important group under near-future scenarios of CO2-driven ocean acidification. Here, we assess the effects of four environmentally realistic pCO2 levels (900, 1500, 2900 and 6600 μatm) on the shell production rate of Mya arenaria juveniles originating from a periodically pCO2-enriched habitat (Kiel Fjord, Western Baltic Sea). We find a significant decline in the rate of shell growth as pCO2 increases, but also observe unchanged shell formation rates at moderate pCO2 levels of 1500 and 2900 μatm, the latter illustrating the capacity of the juveniles to partially mitigate the impact of high pCO2. Using recently developed geochemical tracers we show that M. arenaria exposed to a natural pCO2 gradient from 900 to 2900 μatm can likely concentrate HCO3– in the calcifying fluid through the exchange of HCO3–/Cl– and simultaneously maintain the pH homeostasis through active removal of protons, thereby being able to sustain the rate of shell formation to a certain extent. However, with increasing pCO2 beyond natural maximum the bivalves may have limited capacity to compensate for changes in the calcifying fluid chemistry, showing significant shell growth reduction. Findings of the present study may pave the way for elucidating the underlying mechanisms by which marine bivalves acclimate and adapt to high seawater pCO2. |
format |
Article in Journal/Newspaper |
author |
Zhao, L. Milano, S. Walliser, E. Schöne, B. |
spellingShingle |
Zhao, L. Milano, S. Walliser, E. Schöne, B. Bivalve shell formation in a naturally CO2-enriched habitat: Unraveling the resilience mechanisms from elemental signatures |
author_facet |
Zhao, L. Milano, S. Walliser, E. Schöne, B. |
author_sort |
Zhao, L. |
title |
Bivalve shell formation in a naturally CO2-enriched habitat: Unraveling the resilience mechanisms from elemental signatures |
title_short |
Bivalve shell formation in a naturally CO2-enriched habitat: Unraveling the resilience mechanisms from elemental signatures |
title_full |
Bivalve shell formation in a naturally CO2-enriched habitat: Unraveling the resilience mechanisms from elemental signatures |
title_fullStr |
Bivalve shell formation in a naturally CO2-enriched habitat: Unraveling the resilience mechanisms from elemental signatures |
title_full_unstemmed |
Bivalve shell formation in a naturally CO2-enriched habitat: Unraveling the resilience mechanisms from elemental signatures |
title_sort |
bivalve shell formation in a naturally co2-enriched habitat: unraveling the resilience mechanisms from elemental signatures |
publishDate |
2018 |
url |
http://hdl.handle.net/21.11116/0000-0000-F9D6-6 |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_source |
Chemosphere |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.chemosphere.2018.03.180 http://hdl.handle.net/21.11116/0000-0000-F9D6-6 |
op_doi |
https://doi.org/10.1016/j.chemosphere.2018.03.180 |
container_title |
Chemosphere |
container_volume |
203 |
container_start_page |
132 |
op_container_end_page |
138 |
_version_ |
1775354069859172352 |