英文摘要: | Ocean acidification negatively affects many marine species and is predicted to cause widespread changes to marine ecosystems. Similarly, freshwater ecosystems may potentially be affected by climate-change-related acidification; however, this has received far less attention. Freshwater fish represent 40% of all fishes, and salmon, which rear and spawn in freshwater, are of immense ecosystem, economical and cultural importance. In this study, we investigate the impacts of CO2-induced acidification during the development of pink salmon, in freshwater and following early seawater entry. At this critical and sensitive life stage, we show dose-dependent reductions in growth, yolk-to-tissue conversion and maximal O2 uptake capacity; as well as significant alterations in olfactory responses, anti-predator behaviour and anxiety under projected future increases in CO2 levels. These data indicate that future populations of pink salmon may be at risk without mitigation and highlight the need for further studies on the impact of CO2-induced acidification on freshwater systems.
Future predicted increases in CO2 have been demonstrated to cause a wide range of sublethal effects on a variety of marine fish species. Effects include changes in olfactory responses to predator, prey and substrate cues1, 2, 3, interference with neurotransmitter function4, 5, alterations in behavioural lateralization4, 6 and heightened anxiety5. Despite the growing body of work on the effects of ocean acidification (OA) on marine systems, less is known about the future patterns and dynamics of CO2 in freshwater, making it difficult to infer how freshwater ecosystems will respond to climate-change-related acidification. Nevertheless, elevated CO2 in both marine and freshwater systems is a likely scenario in the future7. Although freshwater comprises only 0.8% of the water on the Earth’s surface, freshwater ecosystems support almost 40% of all fish species8. Therefore, investigating the effects of CO2-mediated acidification in freshwater systems may provide important insights into how almost half of the world’s fishes and associated communities will respond to climate change. Salmon are a keystone species in many marine, freshwater and terrestrial ecosystems because of their role in supporting food webs9, 10 and, as such, may help link distinct and relatively isolated systems. All salmon initially rear in freshwater but spend the majority of their juvenile and adult lives in seawater, before returning to their freshwater natal streams to spawn11. Thus, the freshwater environment is crucial to their life history. In comparison to all other Pacific salmon, pink salmon (Oncorhynchus gorbuscha) are the most abundant and widely distributed and, consequently, considered an important indicator of ecosystem health12. Unlike most other anadromous salmonids, pink salmon migrate to sea soon after emergence and, at approximately 0.2 g, are by far the smallest at the time of seawater entry13, 14. As seawater entry is a time of heightened mortality for all species of salmon15, 16, 17, their small size and high ratio of surface area to volume may make pink salmon especially vulnerable to environmental stressors, including OA. Here, we show negative effects of CO2-induced acidification on the growth, metabolism, olfactory responses and anti-predator behaviour in the early life stages of pink salmon during freshwater development and post-seawater entry using predicted future levels of CO2. Unlike other studies, we also incorporated a fluctuating CO2 treatment to reflect naturally occurring CO2 fluctuations in freshwater and coastal ecosystems18, 19, 20. Two weeks before hatch, eyed embryos were transferred into one of four freshwater treatments (constant 450 μatm (present-day control), constant 1,000 μatm (100-year projection), constant 2,000 μatm, and diurnal fluctuating 450–2,000 μatm) for ten weeks. Growth, routine (RMR) and maximum (MMR) metabolic rate were measured throughout freshwater development and, at the end of ten weeks, their levels of anxiety and olfactory and anti-predator responses to conspecific alarm cues were measured. When fish reached yolk sac absorption (week 10 post-CO2 exposure), fish reared in freshwater at constant 450 μatm CO2 were transferred to one of three different seawater treatments of 450, 1,600 (future coastal conditions) and a diurnal 450–1,600 μatm CO2 treatment. A subset of fish reared at constant 2,000 μatm CO2 in freshwater were also transferred into 1,600 μatm seawater (Supplementary Information). Growth and metabolic rates were measured over the subsequent two weeks post-seawater transfer. During freshwater development, there was a significant negative effect of CO2 on fork length, production efficiencies, total wet mass and total tissue mass (yolk removed) and no significant effect of CO2 on RMR and MMR (Supplementary Information). At yolk sac absorption (week 10), total wet mass (F3 = 4.0157, p = 0.0218), total dry mass (F3 = 4.7993, p = 0.0112), production efficiencies (F3 = 4.5412, p = 0.0139) and fork lengths (F3 = 8.0345, p = 0.0010) were significantly different among groups (see Fig. 1). Production efficiencies (% of yolk converted into tissue) near yolk sac absorption were 25% lower in the high-CO2 group compared to the control (p = 0.0064). Similarly, fork lengths were significantly reduced at 1,000 and 2,000 μatm compared to control levels (p = 0.0292 and p = 0.0004, respectively).
Our results show that future increases in CO2 in seawater may impair early seawater survival of migrating pink salmon fry through impacts on subsequent growth and MMR. Growth rates were negative in groups transferred into high-CO2 seawater, whereas control fish continued to grow throughout our seawater exposure. Fish were not fed; however, internal yolk stores were still present, which were presumably drawn on for growth. This suggests that tissue production may be impaired at high CO2. However, because growth rates are based on total wet mass, the inability to hypo-osmoregulate efficiently at high pCO2 could also have contributed to the apparent negative growth rate estimates (due to water loss) during the transition to seawater. If the lower growth rates at high pCO2 are associated with impaired hypo-osmoregulatory ability, then the osmoregulatory challenge of seawater entry may be further compounded by OA. Following seawater transfer, an increase in CO2 reduced MMR in pink salmon fry. These results indicate that pink salmon fry may be particularly sensitive to climate-change-related acidification during exercise, which may have implications on the success of their seaward migration and early ocean survival. Pink salmon migrate to sea soon after emergence and this heightened capacity for activity may be crucial to their survival in a predator-dense environment. However, elevated pCO2 may reduce the capacity for maximal O2 uptake and exercise of migrating fry, making them more susceptible to predation and reducing their foraging success at a time when yolk reserves become limiting.
This study demonstrates that pink salmon may be faced with numerous sublethal impacts of acidification on their physiology and behaviour under predicted future increases in pCO2. However, carbonate chemistry data of inland waters suggests that some freshwater ecosystems are at present exposed to temporal elevations in pCO2 (ref. 45). For example, pCO2 in the Columbia River, which hosts runs of various salmon species, ranges from 541 to 981 μatm (ref. 46). Similarly, recent oceanic surveys of the West Coast of North America suggest that our coastal ecosystems temporally experience large elevations in CO2, which may exceed 1,000 μatm and persist for months in some locations20, 47, 48, URL: | http://www.nature.com/nclimate/journal/v5/n10/full/nclimate2694.html
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