Abstract

The frequency of short-term oceanic warming events (‘marine heatwaves’ [MHWs] or heat spikes) has increased over the past century and is projected to further increase because of anthropogenic climate change. Given that marine organisms are strongly influenced by temperature, an increased occurrence of warming events could alter the structure of populations, communities and ecosystems. The distribution and ecophysiological performance of kelp species – globally important foundation species that play significant roles in nutrient cycling and habitat creation in temperate coastal systems – is particularly constrained by temperature. However, their photophysiological responses to warming events remains unclear, which hinders attempts to understand and predict the effects of ocean warming on kelp populations and the ecosystems they underpin. Here, we experimentally simulated a heat spike (+2°C and +4°C in magnitude, 3 days in duration, compared with ambient controls) and examined the photophysiological responses of two canopy-forming kelp species widely distributed across the northeast Atlantic - Laminaria digitata and L. hyperborea. Both species were resilient to the realistic warming treatments in terms of their photosynthetic characteristics. However, we found that L. digitata individuals, which were collected from populations found towards the upper limit of this species’ thermal range, exhibited increased oxygen production at higher temperatures, particularly after multiple days of exposure to the warming event. Laminaria digitata also exhibited a greater poise for dissipating excess energy through non-photochemical pathways. In contrast, L. hyperborea, which extends further south into warmer waters and tends to occupy deeper reefs that are almost constantly submerged, appeared to be photo-physiologically insensitive to the heat spike. This study enhances our mechanistic understanding of the photophysiological and photoprotective responses of kelps to short-term acute warming events – features which are likely to emerge as important drivers of ecological change in coming decades.

Highlights

  • The upper layers of the global ocean have warmed at a rate of ∼0.1◦C per decade since the mid-20th century, albeit with pronounced regional, and seasonal variability (IPCC, 2013)

  • Both Laminaria digitata and L. hyperborea were collected by removing whole plants from their in situ environment; individuals were carefully removed by prising the holdfast from the rocky substratum

  • On L. digitata, daily mean temperatures in the treatments during the 3-day warming event were: T0 = 15.7 ± 0.1◦C, T1 = 18.4 ± 0.0◦C, and T2 = 19.9 ± 0.0◦C, which corresponded to ambient conditions, +2.7◦C and +4.2◦C treatments, respectively

Read more

Summary

Introduction

The upper layers of the global ocean have warmed at a rate of ∼0.1◦C per decade since the mid-20th century, albeit with pronounced regional, and seasonal variability (IPCC, 2013). Recent climatic changes have caused changes in the distribution of species (Pinsky et al, 2013; Poloczanska et al, 2013), the structure of communities and ecosystems (Vergés et al, 2014; Wernberg et al, 2016), and the provision of ecosystem services (Pecl et al, 2017). As the distribution of marine species is highly constrained by temperature, with many populations persisting toward the upper limits of species’ thermal niches (Sunday et al, 2012), continuation of both long- and short-term warming will drive redistribution of species, and reconfiguration of communities and ecosystems at the global scale (García Molinos et al, 2016; Hughes et al, 2017)

Objectives
Methods
Results
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call