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

被引:1
|
作者
Fernández P.A. [1 ]
Amsler C.D. [2 ]
Hurd C.L. [3 ]
Díaz P.A. [4 ]
Gaitán-Espitia J.D. [5 ]
Macaya E.C. [6 ,7 ]
Schmider-Martínez A. [4 ]
Garrido I. [7 ,8 ,9 ]
Murúa P. [10 ]
Buschmann A.H. [1 ]
机构
[1] Centro i∼mar, CeBiB & MASH, Universidad de Los Lagos, Camino a Chinquihue km6, Puerto Montt
[2] University of Alabama at Birmingham, Department of Biology, Birmingham, 35233, AL
[3] Institute for marine and Antarctic Studies (IMAS), University of Tasmania, 7001, TAS
[4] Centro i∼mar, Universidad de Los Lagos, Camino a Chinquihue km6, Puerto Montt
[5] The Swire Institute of Marine Science, School of Biological Sciences, The University of Hong Kong, Pok Fu Lam Road
[6] Departamento de Oceanografía, Universidad de Concepción, Concepción
[7] Centro FONDAP de Investigación Dinámica de Ecosistemas Marinos de Altas Latitudes (IDEAL), Valdivia
[8] Laboratorio Costero de Recursos Acuáticos de Calfuco (LCRAC), Instituto Ciencias Marinas y Limnológicas (ICML), Facultad de Ciencias, Universidad Austral de Chile, Valdivia
[9] Department of Biology and Québec-Océan, Laval University, QC, G1V 0A6, Québec
[10] Laboratorio de Macroalgas y Ficopatologia, Instituto de Acuicultura, Universidad Austral de Chile, Sede Puerto Montt, Puerto Montt
关键词
Antarctic; Carbon concentrating mechanisms; Carbon dioxide; Carbon uptake strategies; Climate change; Macroalgae;
D O I
10.1016/j.scitotenv.2024.174006
中图分类号
学科分类号
摘要
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. © 2024 Elsevier B.V.
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