Abstract

Despite the long evolutionary history of this group, the challenges brought by the Anthropocene have been inflicting an extensive pressure over sharks and their relatives. Overexploitation has been driving a worldwide decline in elasmobranch populations, and rapid environmental change, triggered by anthropogenic activities, may further test this group's resilience. In this context, we searched the literature for peer-reviewed studies featuring a sustained (>24 h) and controlled exposure of elasmobranch species to warming, acidification, and/or deoxygenation: three of the most pressing symptoms of change in the ocean. In a standardized comparative framework, we conducted an array of mixed-model meta-analyses (based on 368 control-treatment contrasts from 53 studies) to evaluate the effects of these factors and their combination as experimental treatments. We further compared these effects across different attributes (lineages, climates, lifestyles, reproductive modes, and life stages) and assessed the direction of impact over a comprehensive set of biological responses (survival, development, growth, aerobic metabolism, anaerobic metabolism, oxygen transport, feeding, behavior, acid-base status, thermal tolerance, hypoxia tolerance, and cell stress). Based on the present findings, warming appears as the most influential factor, with clear directional effects, namely decreasing development time and increasing aerobic metabolism, feeding, and thermal tolerance. While warming influence was pervasive across attributes, acidification effects appear to be more context-specific, with no perceivable directional trends across biological responses apart from the necessary to achieve acid-base balance. Meanwhile, despite its potential for steep impacts, deoxygenation has been the most neglected factor, with data paucity ultimately precluding sound conclusions. Likewise, the implementation of multi-factor treatments has been mostly restricted to the combination of warming and acidification, with effects approximately matching those of warming. Despite considerable progress over recent years, research regarding the impact of these drivers on elasmobranchs lags behind other taxa, with more research required to disentangle many of the observed effects. Given the current levels of extinction risk and the quick pace of global change, it is further crucial that we integrate the knowledge accumulated through different scientific approaches into a holistic perspective to better understand how this group may fare in a changing ocean.

Highlights

  • The rise in anthropogenic greenhouse gas emissions since the Industrial Revolution, carbon dioxide (CO2), is likely to shape the future of life on Earth (Pecl et al, 2017; Bindoff et al, 2019)

  • The ocean has been assuaging the surface-level repercussions of increased emissions, namely by absorbing over 90% of the energy trapped by the excess greenhouse gases and up to 30% of the CO2 released to the atmosphere

  • Temperature has long been acknowledged as a key modulator of biological processes and its effects have been experimentally studied for decades (Britton, 1924; Neale et al, 1977)

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Summary

Introduction

The rise in anthropogenic greenhouse gas emissions since the Industrial Revolution, carbon dioxide (CO2), is likely to shape the future of life on Earth (Pecl et al, 2017; Bindoff et al, 2019). The consequences of this key service are brewing beneath the surface, with ocean warming (OW) and acidification (OA) emerging as major threats to marine life and dependent communities (Pecl et al, 2017; Bindoff et al, 2019; Collins et al, 2019). According to the most pessimistic forecasts by the Intergovernmental Panel on Climate Change [IPCC; representative concentration pathway (RCP) 8.5], mean sea surface temperatures are projected to increase up to nearly 4◦C, while mean pH may potentially drop by over 0.3 units by the end of the century (Abram et al, 2019). Rising temperatures have been instigating an additional facet of climate change with potentially widespread consequences: ocean deoxygenation (OD). Under the same RCP scenario and timeframe, mean dissolved O2 in the upper ocean layers is expected to decrease by up to 5% (Abram et al, 2019)

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