Ocean acidification increases susceptibility to sub-zero air temperatures in ecosystem engineers and limit poleward range shifts
- Aarhus University, Denmark
- University of Alberta, Canada
- University of British Columbia, Canada
- Université du Québec à Rimouski, Canada
Abstract
Ongoing climate change has caused rapidly increasing temperatures, and an unprecedented decline in seawater pH, known as ocean acidification. Increasing temperatures are redistributing species towards higher and cooler latitudes which are most affected by ocean acidification. Whilst the persistence of intertidal species in cold environments is related to their capacity to resist sub-zero air temperatures, studies have never considered the interacting impacts of ocean acidification and freeze stress on species survival and distribution. Here, a full-factorial experiment was used to study whether ocean acidification increases mortality in subtidal Mytilus trossulus and subtidal M. galloprovincialis, and intertidal M. trossulus following sub-zero air temperature exposure. We examined physiological processes behind variation in freeze tolerance using 1H NMR metabolomics, analyses of fatty acids, and amino acid composition. We show that low pH conditions (pH = 7.5) significantly decrease freeze tolerance in both intertidal and subtidal populations of Mytilus spp. Under current day pH conditions (pH = 7.9), intertidal M. trossulus was more freeze tolerant than subtidal M. trossulus and subtidal M. galloprovincialis. Conversely, under low pH conditions, subtidal M. trossulus was more freeze tolerant than the other mussel categories. Differences in the concentration of various metabolites (cryoprotectants), or in the composition of amino acids and cell membrane phospholipid fatty acids could not explain the decrease in survival. These results suggest that ocean acidification can offset the poleward range expansions facilitated by warming, and that reduced freeze tolerance could result in a range contraction if temperatures become lethal at the equatorward edge.
Data availability
All data produced and needed to replicate the work is deposited freely on the borealis data verse (https://borealisdata.ca) - https://doi.org/10.5683/SP3/DQ5PMQ
Article and author information
Author details
Funding
H2020 Marie Skłodowska-Curie Actions (797387)
- Jakob Thyrring
Danmarks Frie Forskningsfond (7027-00060B)
- Jakob Thyrring
Natural Sciences and Engineering Research Council of Canada (RGPIN-2019-04239)
- Katie E Marshall
Carlsbergfondet (CF21-0564)
- Jakob Thyrring
The funders had no role in study design, data collection and interpretation, or the decision to submit the work for publication.
Reviewing Editor
- David A. Donoso, Escuela Politécnica Nacional, Ecuador
Version history
- Received: June 15, 2022
- Preprint posted: July 3, 2022 (view preprint)
- Accepted: April 9, 2023
- Accepted Manuscript published: April 11, 2023 (version 1)
- Version of Record published: April 25, 2023 (version 2)
Copyright
© 2023, Thyrring et al.
This article is distributed under the terms of the Creative Commons Attribution License permitting unrestricted use and redistribution provided that the original author and source are credited.
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Ocean acidification increases susceptibility to sub-zero air temperatures in ecosystem engineers and limit poleward range shifts
eLife 12:e81080.
https://doi.org/10.7554/eLife.81080
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