The cellular stress response (CSR) is pervasive to all domains of life. It has shaped the interaction between organisms and their environment since the origin of the first cell. Although the CSR has been subject to a myriad of nuanced modifications in the various branches of life present today, its core features remain preserved. The scientific literature covering the CSR is enormous and the broad scope of this brief overview was challenging. However, it is critical to conceptually understand how cells respond to stress in a holistic sense and to point out how fundamental aspects of the CSR framework are integrated. It was necessary to be extremely selective and not feasible to even mention many interesting and important developments in this expansive field. The purpose of this overview is to sketch out general and emerging CSR concepts with an emphasis on the initial cellular strain resulting from stress (macromolecular damage) and the evolutionarily most highly conserved elements of the CSR. Examples emphasize fish and aquatic invertebrates to highlight what is known in organisms beyond mammals, yeast, and other common models. Nonetheless, select pioneering studies using canonical models are also considered and the concepts discussed are applicable to all cells. More detail on important aspects of the CSR in aquatic animals is provided in the accompanying articles of this special issue.
Salinity stress occurs when salt concentration in the environment changes rapidly, for example because of tidal water flow, rainstorms, drought, or evaporation from small bodies of water. However, gradual changes in salt concentration can also cause osmotic stress in aquatic habitats if levels breach thresholds that reduce the fitness of resident organisms. The latter scenario is exemplified by climate change driven salinization of estuaries and by dilution of ocean surface salinity through changes in the water cycle. In this review, we discuss how fish employ the evolutionarily conserved cellular stress response (CSR) to cope with these different forms of salinity stress. Macromolecular damage is identified as the cause of impaired physiological performance during salinity stress and serves as the signal for inducing a CSR. Basic aspects of the CSR have been observed in fish exposed to salinity stress, including repair and protection of cellular macromolecules, reallocation of energy, cell cycle arrest, and in severe cases, programmed cell death. Osmosensing and signal transduction events that regulate these aspects of the CSR provide a link between environmental salinity and adaptive physiological change required for survival. The CSR has evolved to broaden the range of salinities tolerated by certain euryhaline fish species, but is constrained in stenohaline species that are sensitive to changes in environmental salinity. Knowledge of how the CSR diverges between euryhaline and stenohaline fish enables understanding of physiological mechanisms that underlie salt tolerance and facilitates predictions as to the relative vulnerabilities of different fish species to a rapidly changing hydrosphere.
more » « less- Award ID(s):
- 1656371
- NSF-PAR ID:
- 10134192
- Publisher / Repository:
- Wiley Blackwell (John Wiley & Sons)
- Date Published:
- Journal Name:
- Journal of Experimental Zoology Part A: Ecological and Integrative Physiology
- Volume:
- 333
- Issue:
- 6
- ISSN:
- 2471-5638
- Page Range / eLocation ID:
- p. 421-435
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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How diatoms respond to fluctuations in osmotic pressure is important from both ecological and applied perspectives. It is well known that osmotic stress affects photosynthesis and can result in the accumulation of compounds desirable in pharmaceutical and alternative fuel industries. Gene expression responses to osmotic stress have been studied in short‐term trials, but it is unclear whether the same mechanisms are recruited during long‐term acclimation. We used RNA‐seq to study the genome‐wide transcription patterns in the euryhaline diatom,
Cyclotella cryptica , following long‐term acclimation to salinity that spanned the natural range of fresh to oceanic water. Long‐term acclimatedC. cryptica exhibited induced synthesis or repressed degradation of the osmolytes glycine betaine, taurine and dimethylsulfoniopropionate (DMSP). Although changes in proline concentration is one of the main responses in short‐term osmotic stress, we did not detect a transcriptional change in proline biosynthetic pathways in our long‐term experiment. Expression of membrane transporters showed a general tendency for increased import of potassium and export of sodium, consistent with the electrochemical gradients and dependence on co‐transported molecules. Our results show substantial between‐genotype differences in growth and gene expression reaction norms and suggest that the regulation of proline synthesis important in short‐term osmotic stress might not be maintained in long‐term acclimation. Further examination using time‐course gene expression experiments, metabolomics and genetic validation of gene functions would reinforce patterns inferred from RNA‐seq data. -
Abstract Background Spawning migrations are a widespread phenomenon among fishes, often occurring in response to environmental conditions prompting movement into reproductive habitats (migratory cues). However, for many species, individual fish may choose not to migrate, and research suggests that conditions preceding the spawning season (migratory primers) may influence this decision. Few studies have provided empirical descriptions of these prior conditions, partly due to a lack of long-term data allowing for robust multi-year comparisons. To investigate how primers and cues interact to shape the spawning migrations of coastal fishes, we use acoustic telemetry data from Common Snook ( Centropomus undecimalis ) in Everglades National Park, Florida, USA. A contingent of Snook migrate between rivers and coastal spawning sites, varying annually in both the proportion of the population that migrates and the timing of migration within the spawning season. However, the specific environmental factors that serve as migratory primers and cues remain unknown. Methods We used eight years of acoustic telemetry data (2012–2019) from 173 tagged Common Snook to investigate how primers and cues influence migratory patterns at different temporal scales. We hypothesize that (1) interannual differences in hydrologic conditions preceding the spawning season contribute to the number of individuals migrating each year, and (2) specific environmental cues trigger the timing of migrations during the spawning season. We used GLMMs to model both the annual and seasonal migratory response in relation to flow characteristics (water level, rate of change in water level), other hydrologic/abiotic conditions (temperature, salinity), fish size, and phenological cues independent of riverine conditions (photoperiod, lunar cycle). Results We found that the extent of minimum marsh water level prior to migration and fish size influence the proportion of Snook migrating each year, and that high river water level and daily rates of change serve as primary cues triggering migration timing. Conclusion Our findings illustrate how spawning migrations are shaped by environmental factors acting at different temporal scales and emphasize the importance of long-term movement data in understanding these patterns. Research providing mechanistic descriptions of conditions that promote migration and reproduction can help inform management decisions aimed at conserving ecologically and economically important species.more » « less
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Otolith chemistry has gained increasing attention as a tool for analyzing various aspects of fish biology, such as stock dynamics, migration patterns, hypoxia and pollution exposure, and connectivity between habitats. While these studies often assume otolith elemental concentrations reflect environmental conditions, physiological processes are increasingly recognized as a modulating and/or controlling factor. In particular, biomineralization—the complex, enzyme-regulated construction of CaCO3 crystals scaffolded by proteins—is believed to play a critical role in governing otolith chemical patterns. This review aims to summarize the knowledge on otolith composition and biophysical drivers of biomineralization, present hypotheses on how biomineralization should affect element incorporation, and test the validity thereof with selected case studies. Tracers of environmental history are assumed to be dominated by elements that substitute for Ca during crystal growth or that occur randomly trapped within the crystal lattice. Strontium (Sr) and barium (Ba) largely comply with the biomineralization-based hypotheses that otolith element patterns reflect environmental concentrations, without additional effects of salinity, but can be influenced by physiological processes, typically exhibiting decreasing incorporation with increasing growth. Conversely, tracers of physiology are assumed to be elements under physiological control and primarily occur protein-bound in the otolith’s organic matrix. Physiological tracers are hypothesized to reflect feeding rate and/or growth, decrease with fish age, and exhibit minimal influence of environmental concentration. The candidate elements phosphorus (P), copper (Cu) and zinc (Zn) confirm these hypotheses. Magnesium (Mg) is believed to be randomly trapped in the crystal structure and hence a candidate for environmental reconstruction, but the response to all examined drivers suggest Mg to be coupled to growth. Manganese (Mn) substitutes for Ca, but is also a co-factor in matrix proteins, and therefore exhibits otolith patterns reflecting both environmental (concentration and salinity) and physiological (ontogeny and growth) histories. A consistent temperature response was not evident across studies for either environmental or physiological tracers, presumably attributable to variable relationships between temperature and fish behavior and physiology (e.g., feeding rate, reproduction). Biomineralization thus has a controlling effect on otolith element concentrations for elements that are linked with somatic growth, but not for elements that substitute for Ca in the crystal lattice. Interpretation of the ecological significance of patterns from field samples therefore needs to consider the impact of the underlying biomineralization processes of the element in question as well as physiological processes regulating the availability of ions for inclusion in the growing crystal lattice. Such understanding will enhance the utility of this technique to address fisheries management questions.more » « less
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null (Ed.)Euryhaline fish tolerate a wide range of environmental salinity by employing molecular mechanisms for coping with the associated osmotic stress. We have previously shown that osmotic stress transcription factor 1 (OSTF1) is part of these mechanisms. OSTF1 is transiently and rapidly upregulated in gill epithelial cells of tilapia (Oreochromis mossambicus) exposed to hyperosmolality. Hyperosmotic induction of OSTF1 in tilapia gills was reproduced in the tilapia OmB cell neuroepithelial cell line. OSTF1 shares the signature sequence of the TSC-22 family suggesting that it is a transcriptional repressor. If, in fact, OSTF1 is a transcription factor, we hypothesize that it will localize to the nucleus during hyperosmotic stress. Using standard cloning procedures, OSTF1 was tagged with enhanced green fluorescent protein (EGFP) at either the C- or N-terminus. Using fluorescent microscopy we show that the fusion proteins are retained in the cytosol under iso-osmotic conditions. To evaluate potential nuclear translocation of OSTF1 during hyperosmotic stress, we subjected OmB cells expressing the OSTF1:EGFP fusion protein to hyperosmotic media and imaged at time intervals from 5 minutes to 4 hours using a Leica Dmi8 microscope with automated scanning stage. At four hours and 650 mOsmol/kg, subcellular localization quantified by LASX image analysis (Leica) demonstrated that OSTF1:EGFP was mostly localized to the nucleus. This result supports our hypothesis that OSTF1 is indeed an osmotically inducible transcription factor. Current work evaluates influence of specific OSTF1 domains on nuclear localization.more » « less
