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Article: Diverse inorganic carbon uptake strategies in Antarctic seaweeds: Revealing species-specific responses and implications for Ocean Acidification

TitleDiverse inorganic carbon uptake strategies in Antarctic seaweeds: Revealing species-specific responses and implications for Ocean Acidification
Authors
KeywordsAntarctic
Carbon concentrating mechanisms
Carbon dioxide
Carbon uptake strategies
Climate change
Macroalgae
Issue Date16-Jun-2024
PublisherElsevier
Citation
Science of the Total Environment, 2024, v. 945 How to Cite?
Abstract

Seaweeds are important components of coastal benthic ecosystems along the Western Antarctic Peninsula (WAP), providing refuge, food, and habitat for numerous associated species. Despite their crucial role, the WAP is among the regions most affected by global climate change, potentially impacting the ecology and physiology of seaweeds. Elevated atmospheric CO2 concentrations have led to increased dissolved inorganic carbon (Ci) with consequent declines in oceanic pH and alterations in seawater carbonate chemistry, known as Ocean Acidification (OA). Seaweeds possess diverse strategies for Ci uptake, including CO2 concentrating mechanisms (CCMs), which may distinctly respond to changes in Ci concentrations. Conversely, some seaweeds do not operate CCMs (non-CCM species) and rely solely on CO2. Nevertheless, our understanding of the status and functionality of Ci uptake strategies in Antarctic seaweeds remains limited. Here, we investigated the Ci uptake strategies of seaweeds along a depth gradient in the WAP. Carbon isotope signatures (δ13C) and pH drift assays were used as indicators of the presence or absence of CCMs. Our results reveal variability in CCM occurrence among algal phyla and depths ranging from 0 to 20 m. However, this response was species specific. Among red seaweeds, the majority relied solely on CO2 as an exogenous Ci source, with a high percentage of non-CCM species. Green seaweeds exhibited depth-dependent variations in CCM status, with the proportion of non-CCM species increasing at greater depths. Conversely, brown seaweeds exhibited a higher prevalence of CCM species, even in deep waters, indicating the use of CO2 and HCO3. Our results are similar to those observed in temperate and tropical regions, indicating that the potential impacts of OA on Antarctic seaweeds will be species specific. Additionally, OA may potentially increase the abundance of non-CCM species relative to those with CCMs.


Persistent Identifierhttp://hdl.handle.net/10722/343995
ISSN
2023 Impact Factor: 8.2
2023 SCImago Journal Rankings: 1.998

 

DC FieldValueLanguage
dc.contributor.authorFernández, Pamela A-
dc.contributor.authorAmsler, Charles D-
dc.contributor.authorHurd, Catriona L-
dc.contributor.authorDiaz, Patricio A-
dc.contributor.authorGaitán-Espitia, Juan Diego-
dc.contributor.authorMacaya, Erasmo C-
dc.contributor.authorSchmider, Andreas-
dc.contributor.authorGarrido, Ignacio-
dc.contributor.authorMurúa, Pedro-
dc.contributor.authorBuschmann, Alejandro H-
dc.date.accessioned2024-06-25T03:29:29Z-
dc.date.available2024-06-25T03:29:29Z-
dc.date.issued2024-06-16-
dc.identifier.citationScience of the Total Environment, 2024, v. 945-
dc.identifier.issn0048-9697-
dc.identifier.urihttp://hdl.handle.net/10722/343995-
dc.description.abstract<p>Seaweeds are important components of coastal benthic ecosystems along the Western Antarctic Peninsula (WAP), providing refuge, food, and habitat for numerous associated species. Despite their crucial role, the WAP is among the regions most affected by global climate change, potentially impacting the ecology and physiology of seaweeds. Elevated atmospheric CO<sub>2</sub> concentrations have led to increased dissolved inorganic carbon (Ci) with consequent declines in oceanic pH and alterations in seawater carbonate chemistry, known as Ocean Acidification (OA). Seaweeds possess diverse strategies for Ci uptake, including CO<sub>2</sub> concentrating mechanisms (CCMs), which may distinctly respond to changes in Ci concentrations. Conversely, some seaweeds do not operate CCMs (non-CCM species) and rely solely on CO<sub>2</sub>. Nevertheless, our understanding of the status and functionality of Ci uptake strategies in Antarctic seaweeds remains limited. Here, we investigated the Ci uptake strategies of seaweeds along a depth gradient in the WAP. Carbon isotope signatures (δ<sup>13</sup>C) and pH drift assays were used as indicators of the presence or absence of CCMs. Our results reveal variability in CCM occurrence among algal phyla and depths ranging from 0 to 20 m. However, this response was species specific. Among red seaweeds, the majority relied solely on CO<sub>2</sub> as an exogenous Ci source, with a high percentage of non-CCM species. Green seaweeds exhibited depth-dependent variations in CCM status, with the proportion of non-CCM species increasing at greater depths. Conversely, brown seaweeds exhibited a higher prevalence of CCM species, even in deep waters, indicating the use of CO<sub>2</sub> and HCO<sub>3</sub><sup>−</sup>. Our results are similar to those observed in temperate and tropical regions, indicating that the potential impacts of OA on Antarctic seaweeds will be species specific. Additionally, OA may potentially increase the abundance of non-CCM species relative to those with CCMs.</p>-
dc.languageeng-
dc.publisherElsevier-
dc.relation.ispartofScience of the Total Environment-
dc.subjectAntarctic-
dc.subjectCarbon concentrating mechanisms-
dc.subjectCarbon dioxide-
dc.subjectCarbon uptake strategies-
dc.subjectClimate change-
dc.subjectMacroalgae-
dc.titleDiverse inorganic carbon uptake strategies in Antarctic seaweeds: Revealing species-specific responses and implications for Ocean Acidification-
dc.typeArticle-
dc.identifier.doi10.1016/j.scitotenv.2024.174006-
dc.identifier.scopuseid_2-s2.0-85196149834-
dc.identifier.volume945-
dc.identifier.eissn1879-1026-
dc.identifier.issnl0048-9697-

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