Climate warming is predicted to reduce omega‐3, long‐chain, polyunsaturated fatty acid production in phytoplankton. (6th June 2016)

• Record Type: Journal Article
• Authors: Hixson, Stefanie M.; Arts, Michael T.
• Is Part Of: Global change biology. Volume 22:Number 8(2016:Aug.)
• Page Start: 2744
• Page End: 2755
• Publication Date: 2016-06-06
• Subjects: climate change -- docosahexaenoic acid -- eicosapentaenoic acid -- global warming -- omega‐3 long‐chain polyunsaturated fatty acids; Climatic changes -- Environmental aspects -- Periodicals; Troposphere -- Environmental aspects -- Periodicals; Biodiversity conservation -- Periodicals; Eutrophication -- Periodicals; 551.5
• DOI: 10.1111/gcb.13295
• Languages: English
• ISSNs: 1354-1013

Abstract

Abstract: Phytoplankton are the main source of energy and omega‐3 (n‐3) long‐chain essential fatty acids (EFA) in aquatic ecosystems. Their growth and biochemical composition are affected by surrounding environmental conditions, including temperature, which continues to increase as a result of climate warming. Increasing water temperatures may negatively impact the production of EFA by phytoplankton through the process of homeoviscous adaptation. To investigate this, we conducted an exploratory data synthesis with 952 fatty acid (FA) profiles from six major groups of marine and freshwater phytoplankton. Temperature was strongly correlated with a decrease in the proportion of n‐3 long‐chain polyunsaturated FA (LC‐PUFA) and an increase in omega‐6 FA and saturated FA. Based on linear regression models, we predict that global n‐3 LC‐PUFA production will be reduced by 8.2% for eicosapentaenoic acid (EPA) and 27.8% for docosahexaenoic acid (DHA) with an increase in water temperature of 2.5 °C. Using a previously published estimate of the global production of EPA by diatoms, which contribute to most of the world's supply of EPA, we predict a loss of 14.2 Mt of EPA annually as a result of ocean warming. The n‐3 LC‐PUFA are vitally important for an array of key physiological functions in aquatic and terrestrial organisms, and these FA are mainly produced by phytoplankton. Therefore, reduced production of these EFA, as a consequence of climate warming, is predicted to negatively affect species that depend on these compounds for optimum physiological function. Such profound changes in the biochemical composition of phytoplankton cell membranes can lead to cascading effects throughout the world's ecosystems.