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Ocean acidification reduces thallus strength in a non-calcifying foundation seaweed
Tjärnö Marine Laboratory, Department of Marine Sciences, University of Gothenburg, SE-452 96 Strömstad, Sweden, SE-452 96.
Tjärnö Marine Laboratory, Department of Marine Sciences, University of Gothenburg, SE-452 96 Strömstad, Sweden, SE-452 96.
Tjärnö Marine Laboratory, Department of Marine Sciences, University of Gothenburg, SE-452 96 Strömstad, Sweden, SE-452 96.
KTH, Skolan för kemi, bioteknologi och hälsa (CBH), Fiber- och polymerteknologi, Polymerteknologi.ORCID-id: 0000-0002-1631-1781
Vise andre og tillknytning
2023 (engelsk)Inngår i: Current Biology, ISSN 0960-9822, E-ISSN 1879-0445, Vol. 33, nr 18, s. 941-942Artikkel i tidsskrift (Fagfellevurdert) Published
Abstract [en]

Climate change is causing unprecedented changes in terrestrial and aquatic ecosystems through the emission of greenhouse gases, including carbon dioxide (CO2). Approximately 30% of CO2 is taken up by the ocean (‘ocean acidification’, OA)1, which has profound effects on foundation seaweed species. Negative physical effects on calcifying algae are clear2, but studies on habitat-forming fleshy seaweeds have mainly focused on growth and less on thallus strength3,4. We exposed the habitat-forming brown seaweed Fucus vesiculosus to OA corresponding to projected climate change effects for the year 2100, and observed reduced apical thallus strength and greater loss of exposed individuals in the field. The tissue contained less calcium and magnesium, both of which are important for creating structural alginate matrices. Scanning electron microscopy (SEM) revealed tissue voids in the OA samples that were not present in seaweeds grown under ambient pCO2. We conclude that under OA, weakened F. vesiculosus will be at a significantly higher risk of physical damage and detachment.

sted, utgiver, år, opplag, sider
Elsevier BV , 2023. Vol. 33, nr 18, s. 941-942
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URN: urn:nbn:se:kth:diva-338396DOI: 10.1016/j.cub.2023.07.056ISI: 001085217000001PubMedID: 37751702Scopus ID: 2-s2.0-85172341737OAI: oai:DiVA.org:kth-338396DiVA, id: diva2:1806889
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QC 20231024

Tilgjengelig fra: 2023-10-24 Laget: 2023-10-24 Sist oppdatert: 2025-02-01bibliografisk kontrollert

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