Detrital source diversity moderates decomposition and nutrient release in current and future ocean conditions

Le résumé fourni par la source

The complex interactions between detrital diversity and ocean climate change are not well understood. Here, we used sixteen outdoor raceways to test the hypothesis that ocean warming, and acidification would increase rates of decomposition and nutrient release from detritus of common macroalgae, but the magnitude of change would vary for single detrital sources compared to mixed sources. Our litter-bag experiment to test this hypothesis had six types of macroalgal detritus: (i) Ecklonia radiata, (ii) Sargassum vestitum , (iii) Caulerpa filiformis , (iv) Ecklonia and Sargassum mix, (v) Ecklonia and Caulerpa mix, and (vi) Sargassum and Caulerpa mix. The experimental design also had an orthogonal set of treatments testing effects of ocean warming and acidification, individually and combined, based on the RCP 8.5 climate model for 2081–2100. The identity of detrital sources significantly influenced decomposition rates, carbon liberation and nutrient release. The treatments with two detrital sources did not have increased rates of decomposition and nutrient release compared to single sources. However, detrital source mixing significantly moderated variation in decomposition and nutrient release rates. While ocean acidification had little effect on the decomposition of macroalgal detritus, ocean warming tended to increase rates of decomposition. Given that excessive decomposition can lead to severe anoxia, the results suggest the risk of this occurring will be greater in the warmer oceans of coming decades. In such circumstances, the moderating force of detrital diversity may become increasingly important in maintaining benthic oxygen concentrations and detritus-based production. • The decomposition of mixed and single detrital sources was assessed in current and future ocean conditions. • The identity of detrital sources significantly influenced decomposition rates, and carbon and nutrient release. • Detrital mixing significantly decreased variation in mass loss and nitrogen release. • Ocean warming sometimes increased rates of decomposition of macrophyte detritus. • Ocean acidification did not significantly influence detrital mass loss or nutrient release.

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