Antarctic emerald rockcod have the capacity to compensate for warming when uncoupled from CO 2 ‐acidification

• Published in: Global Change Biology
• Main Authors: Davis, Brittany E., Flynn, Erin E., Miller, Nathan A., Nelson, Frederick A., Fangue, Nann A., Todgham, Anne E.
• Other Authors: Division of Polar Programs, National Science Foundation, Division of Agriculture and Natural Resources, University of California
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2017
• Subjects: Antarctic; Southern Ocean; Antarc*; Ocean acidification
• Online Access: http://dx.doi.org/10.1111/gcb.13987; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fgcb.13987; https://onlinelibrary.wiley.com/doi/pdf/10.1111/gcb.13987; https://onlinelibrary.wiley.com/doi/full-xml/10.1111/gcb.13987; https://onlinelibrary.wiley.com/doi/am-pdf/10.1111/gcb.13987

Abstract Increases in atmospheric CO 2 levels and associated ocean changes are expected to have dramatic impacts on marine ecosystems. Although the Southern Ocean is experiencing some of the fastest rates of change, few studies have explored how Antarctic fishes may be affected by co‐occurring ocean changes, and even fewer have examined early life stages. To date, no studies have characterized potential trade‐offs in physiology and behavior in response to projected multiple climate change stressors (ocean acidification and warming) on Antarctic fishes. We exposed juvenile emerald rockcod Trematomus bernacchii to three P CO 2 treatments (~450, ~850, and ~1,200 μatm P CO 2 ) at two temperatures (−1 or 2°C). After 2, 7, 14, and 28 days, metrics of physiological performance including cardiorespiratory function (heart rate [ f H ] and ventilation rate [ f V ]), metabolic rate ( ), and cellular enzyme activity were measured. Behavioral responses, including scototaxis, activity, exploration, and escape response were assessed after 7 and 14 days. Elevated P CO 2 independently had little impact on either physiology or behavior in juvenile rockcod, whereas warming resulted in significant changes across acclimation time. After 14 days, f H , f V and significantly increased with warming, but not with elevated P CO 2 . Increased physiological costs were accompanied by behavioral alterations including increased dark zone preference up to 14%, reduced activity by 12%, as well as reduced escape time suggesting potential trade‐offs in energetics. After 28 days, juvenile rockcod demonstrated a degree of temperature compensation as f V , , and cellular metabolism significantly decreased following the peak at 14 days; however, temperature compensation was only evident in the absence of elevated P CO 2 . Sustained increases in f V and after 28 days exposure to elevated P CO 2 indicate additive ( f V ) and synergistic ( ) interactions occurred in combination with warming. Stressor‐induced energetic trade‐offs in physiology and ...