Abstract

Concurrent ocean warming and acidification demand experimental approaches that assess biological sensitivities to combined effects of these potential stressors. Here, we summarize five CO2 × temperature experiments on wild Atlantic silverside, Menidia menidia, offspring that were reared under factorial combinations of CO2 (nominal: 400, 2200, 4000, and 6000 µatm) and temperature (17, 20, 24, and 28 °C) to quantify the temperature-dependence of CO2 effects in early life growth and survival. Across experiments and temperature treatments, we found few significant CO2 effects on response traits. Survival effects were limited to a single experiment, where elevated CO2 exposure reduced embryo survival at 17 and 24 °C. Hatch length displayed CO2 × temperature interactions due largely to reduced hatch size at 24 °C in one experiment but increased length at 28 °C in another. We found no overall influence of CO2 on larval growth or survival to 9, 10, 15 and 13–22 days post-hatch, at 28, 24, 20, and 17 °C, respectively. Importantly, exposure to cooler (17 °C) and warmer (28 °C) than optimal rearing temperatures (24 °C) in this species did not appear to increase CO2 sensitivity. Repeated experimentation documented substantial inter- and intra-experiment variability, highlighting the need for experimental replication to more robustly constrain inherently variable responses. Taken together, these results demonstrate that the early life stages of this ecologically important forage fish appear largely tolerate to even extreme levels of CO2 across a broad thermal regime.

Highlights

  • The current anthropogenic increase in atmospheric and oceanic carbon dioxide (CO2 )concentrations has been unparalleled over the past 66 million years [1]

  • Mean embryo survival ranged from 46–96%

  • There was a significant effect of experiment (F(4, 118) = 33.581, p < 0.001), because in experiment 1, high CO2 reduced embryo survival (two-way analysis of variance (ANOVA), F(2, 28) = 18.965, p < 0.001) by 11% at 17 ◦ C (LSD, p = 0.003) and 24 ◦ C

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Summary

Introduction

The current anthropogenic increase in atmospheric and oceanic carbon dioxide (CO2 )concentrations has been unparalleled over the past 66 million years [1]. Laboratory experiments have played an important role in quantifying these CO2 sensitivities, suggesting that they are greater in sessile, calcifying invertebrates than in active, non-calcifying vertebrates, and greater in early life stages than adults [6,7,8]. The latter has been well documented for marine fish, where adults are largely tolerant of acute high-CO2 levels far exceeding predicted OA conditions [9,10]. Experiments showing no discernible CO2 effects are common [20,21,22,23,24]

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