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The effect of sulfide on K+ influx pathways was measured in red blood cells (RBCs) of sulfide-sensitive rainbow trout ( Oncorhynchus mykiss) and sulfide-tolerant crucian carp ( Carassius carassius). In trout RBCs, maximal inhibition of Na+, K+-ATPase was attained at 10 μmol l−1 sulfide and amounted to 32% without being influenced by pH between 6.7 and 8.3. Ouabain-resistant K+ influx in the absence and presence of sulfide was insignificant at pH values between 6.7 and 7.7. At higher pH values ouabain-resistant K+ influx increased, but was inhibited to about 15% by 30 μmol l−1 sulfide. In RBCs of crucian carp neither Na+, K+-ATPase nor ouabain-resistant K+ influx were affected by sulfide concentrations up to 850 μmol l−1. Differences in sulfide-sensitivity of K+ influx between both species can be based upon different properties of the membrane transporter themselves. The reduced Na+, K+-ATPase activity in trout RBCs may also result from a slightly reduced (by 9%) ATP level after sulfide exposure. In addition, intracellular sulfide concentrations were higher in trout RBCs as compared to crucian carp. In trout, intracellular sulfide concentrations reached extracellular levels within 5 min of incubation whereas sulfide concentrations in crucian carp RBCs remained about 2-fold lower than extracellular concentrations. Although the physiological basis of sulfide-insensitive K+ influx in crucian carp RBCs is currently unknown it may contribute to the extremely high sulfide-tolerance of this species. [ABSTRACT FROM AUTHOR]

The article discusses the findings of a study conducted by Norwegian scientists Göran Nilsson and Stian Ellefsen which suggest that certain members of the Carassius could withstand long periods with little to no oxygen at low temperatures during winter beneath frozen lakes. Nilsson and Ellefsen found that Carassius muscle, the major ethanol-producing tissue during anoxia, expressed more of the E1α and E1β genes responsible for driving pyruvate towards ethanol synthesis.

AbstractOxygen bioavailability is declining in aquatic systems worldwide as a result of climate change and other anthropogenic stressors. For aquatic organisms, the consequences are poorly known but are likely to reflect both direct effects of declining oxygen bioavailability and interactions between oxygen and other stressors, including two-warming and acidification-that have received substantial attention in recent decades and that typically accompany oxygen changes. Drawing on the collected papers in this symposium volume ("An Oxygen Perspective on Climate Change"), we outline the causes and consequences of declining oxygen bioavailability. First, we discuss the scope of natural and predicted anthropogenic changes in aquatic oxygen levels. Although modern organisms are the result of long evolutionary histories during which they were exposed to natural oxygen regimes, anthropogenic change is now exposing them to more extreme conditions and novel combinations of low oxygen with other stressors. Second, we identify behavioral and physiological mechanisms that underlie the interactive effects of oxygen with other stressors, and we assess the range of potential organismal responses to oxygen limitation that occur across levels of biological organization and over multiple timescales. We argue that metabolism and energetics provide a powerful and unifying framework for understanding organism-oxygen interactions. Third, we conclude by outlining a set of approaches for maximizing the effectiveness of future work, including focusing on long-term experiments using biologically realistic variation in experimental factors and taking truly cross-disciplinary and integrative approaches to understanding and predicting future effects.

AbstractDespite the global ecological importance of climate change, controversy surrounds how oxygen affects the fate of aquatic ectotherms under warming. Disagreements extend to the nature of oxygen bioavailability and whether oxygen usually limits growth under warming, explaining smaller adult size. These controversies affect two influential hypotheses: gill oxygen limitation and oxygen- and capacity-limited thermal tolerance. Here, we promote deeper integration of physiological and evolutionary mechanisms. We first clarify the nature of oxygen bioavailability in water, developing a new mass-transfer model that can be adapted to compare warming impacts on organisms with different respiratory systems and flow regimes. By distinguishing aerobic energy costs of moving oxygen from environment to tissues from costs of all other functions, we predict a decline in energy-dependent fitness during hypoxia despite approximately constant total metabolic rate before reaching critically low environmental oxygen. A new measure of oxygen bioavailability that keeps costs of generating water convection constant predicts a higher thermal sensitivity of oxygen uptake in an amphipod model than do previous oxygen supply indices. More importantly, by incorporating size- and temperature-dependent costs of generating water flow, we propose that oxygen limitation at different body sizes and temperatures can be modeled mechanistically. We then report little evidence for oxygen limitation of growth and adult size under benign warming. Yet occasional oxygen limitation, we argue, may, along with other selective pressures, help maintain adaptive plastic responses to warming. Finally, we discuss how to overcome flaws in a commonly used growth model that undermine predictions of warming impacts.

The speciose mammalian order Eulipotyphla (moles, shrews, hedgehogs, solenodons) combines an unusual diversity of semi-aquatic, semi-fossorial, and fossorial forms that arose from terrestrial forbearers. However, our understanding of the ecomorphological pathways leading to these lifestyles has been confounded by a fragmentary fossil record, unresolved phylogenetic relationships, and potential morphological convergence, calling for novel approaches. The net surface charge of the oxygen-storing muscle protein myoglobin (Z Mb ), which can be readily determined from its primary structure, provides an objective target to address this question due to mechanistic linkages with myoglobin concentration. Here, we generate a comprehensive 71 species molecular phylogeny that resolves previously intractable intra-family relationships and then ancestrally reconstruct Z Mb evolution to identify ancient lifestyle transitions based on protein sequence alone. Our phylogenetically informed analyses confidently resolve fossorial habits having evolved twice in talpid moles and reveal five independent secondary aquatic transitions in the order housing the world's smallest endothermic divers., Competing Interests: KH, TE, HC, SL, AS, SK, MS, MB, KC No competing interests declared, (© 2021, He et al.)

After the Devonian tetrapod land invasion, groups of terrestrial air-breathing and endothermic mammals repeatedly went back to live in the sea, relying on air intake at the surface for extended breath-hold dives to forage underwater, often at great depths and even in the coldest oceans. Studies on the physiological mechanisms behind prolonged breath-hold diving have a long history, including August Krogh's estimates of the maximal dive duration of the blue whale. Yet the molecular underpinnings of such extreme physiological adaptations are only beginning to be understood. The present review focuses on the molecular properties of the respiratory protein myoglobin that has repeatedly evolved an elevated net positive surface charge in several distantly related groups of diving mammals. This has enabled substantial increases of maximal myoglobin concentration in muscle cells, and hence muscle oxygen storage capacity and maximal dive duration. Using myoglobin net surface charge as a marker has allowed unprecedented insights into the evolution of mammal diving capacity and into the general mechanisms of adaptive protein evolution. From these findings it is argued, in an extension of the August Krogh principle, that for a large number of problems in molecular and evolutionary physiology there will be some protein of choice, or a few such proteins, on which it can be most conveniently studied., (Crown Copyright © 2020. Published by Elsevier Inc. All rights reserved.)

The retina has a very high energy demand but lacks an internal blood supply in most vertebrates. Here we explore the hypothesis that oxygen diffusion limited the evolution of retinal morphology by reconstructing the evolution of retinal thickness and the various mechanisms for retinal oxygen supply, including capillarization and acid-induced haemoglobin oxygen unloading. We show that a common ancestor of bony fishes likely had a thin retina without additional retinal oxygen supply mechanisms and that three different types of retinal capillaries were gained and lost independently multiple times during the radiation of vertebrates, and that these were invariably associated with parallel changes in retinal thickness. Since retinal thickness confers multiple advantages to vision, we propose that insufficient retinal oxygen supply constrained the functional evolution of the eye in early vertebrates, and that recurrent origins of additional retinal oxygen supply mechanisms facilitated the phenotypic evolution of improved functional eye morphology., Competing Interests: CD, HL, AF, JT, TD, DC, PM, DH, NP, HD, AB, HW, EW, TW, JN, MB, MB No competing interests declared, (© 2019, Damsgaard et al.)