Abstract:Greenland halibut (Reinhardtius hippoglossoides), especially juveniles, are frequently found in severely hypoxic areas (18%–25% saturation) of the St. Lawrence Estuary. We investigated the tolerance of this species to hypoxia and evaluated the consequences of low oxygen levels on metabolic capacity. At 5 °C, juveniles had a higher critical oxygen threshold than adults (15% versus 11% saturation), indicating that they were less tolerant to hypoxia. Severe hypoxia (19% saturation) did not affect the juveniles' s… Show more
“…Therefore, deep water renewal must occur often enough to prevent hypoxia. As hypoxia threshold definitions vary [ Hofmann et al ., ], here a midvalue of 20% dissolved oxygen (DO) saturation will be used, which is within the range that Greenland Halibut have been found elsewhere [ Dupont‐Prinet et al ., ]. For Cumberland Sound's bottom temperatures, 20% DO saturation corresponds to an oxygen concentration of roughly 3 mg L −1 .…”
Section: Resultsmentioning
confidence: 99%
“…Even though no oxygen measurements have been previously reported in Cumberland Sound, based on the existence of a bottom‐dwelling population of Greenland Halibut in the sound [ Peklova et al ., ], we can assume that the deepest regions are not hypoxic. However, oxygen levels may be low, as Greenland Halibut have been found in regions with 18−25% oxygen saturation and can survive down to 15% in laboratory studies [ Dupont‐Prinet et al ., ].…”
Cumberland Sound, host to a commercially viable fish population in the deepest depths, is a large embayment on the southeast coast of Baffin Island that opens to Davis Strait. Conductivity, temperature, and depth profiles were collected during three summer field seasons (2011–2013), and two moorings were deployed during 2011–2012. Within the sound, salinity increases with increasing depth while water temperature cools reaching a minimum of −1.49°C at roughly 100 m. Below 100 m, the water becomes both warmer and saltier. Temperature‐salinity curves for each year followed a similar pattern, but the entire water column in Cumberland Sound cooled from 2011 to 2012, and then warmed through the summer of 2013. Even though the sound's maximum depth is over a kilometer deeper than its sill, water in the entire sound is well oxygenated. A comparison of water masses within the sound and in Davis Strait shows that, above the sill, the sound is flooded with cold Baffin Island Current water following an intermittent geostrophic flow pattern entering the sound along the north coast and leaving along the south. Below the sill, replenishment is infrequent and includes water from both the Baffin Island Current and the West Greenland Current. Deep water replenishment occurred more frequently on spring tides, especially in the fall of 2011. Although the sound's circulation is controlled by outside currents, internal water modifying processes occur such as estuarine flow and wind‐driven mixing.
“…Therefore, deep water renewal must occur often enough to prevent hypoxia. As hypoxia threshold definitions vary [ Hofmann et al ., ], here a midvalue of 20% dissolved oxygen (DO) saturation will be used, which is within the range that Greenland Halibut have been found elsewhere [ Dupont‐Prinet et al ., ]. For Cumberland Sound's bottom temperatures, 20% DO saturation corresponds to an oxygen concentration of roughly 3 mg L −1 .…”
Section: Resultsmentioning
confidence: 99%
“…Even though no oxygen measurements have been previously reported in Cumberland Sound, based on the existence of a bottom‐dwelling population of Greenland Halibut in the sound [ Peklova et al ., ], we can assume that the deepest regions are not hypoxic. However, oxygen levels may be low, as Greenland Halibut have been found in regions with 18−25% oxygen saturation and can survive down to 15% in laboratory studies [ Dupont‐Prinet et al ., ].…”
Cumberland Sound, host to a commercially viable fish population in the deepest depths, is a large embayment on the southeast coast of Baffin Island that opens to Davis Strait. Conductivity, temperature, and depth profiles were collected during three summer field seasons (2011–2013), and two moorings were deployed during 2011–2012. Within the sound, salinity increases with increasing depth while water temperature cools reaching a minimum of −1.49°C at roughly 100 m. Below 100 m, the water becomes both warmer and saltier. Temperature‐salinity curves for each year followed a similar pattern, but the entire water column in Cumberland Sound cooled from 2011 to 2012, and then warmed through the summer of 2013. Even though the sound's maximum depth is over a kilometer deeper than its sill, water in the entire sound is well oxygenated. A comparison of water masses within the sound and in Davis Strait shows that, above the sill, the sound is flooded with cold Baffin Island Current water following an intermittent geostrophic flow pattern entering the sound along the north coast and leaving along the south. Below the sill, replenishment is infrequent and includes water from both the Baffin Island Current and the West Greenland Current. Deep water replenishment occurred more frequently on spring tides, especially in the fall of 2011. Although the sound's circulation is controlled by outside currents, internal water modifying processes occur such as estuarine flow and wind‐driven mixing.
“…In contrast, in northwestern Greenland, whereas fish also moved to the inner section of the fjord, this occurred during the summer ice-free period, although fishing effort may have biased the observed distribution pattern (Boje 2002). While Greenland halibut and flatfish generally have a low aerobic scope when compared with pelagic fishes (Dupont-Prinet et al 2013) and are reported to occur in high abundances at low The left panels (a, c, and e) are environmental variables recorded in the southern region of Cumberland Sound, including bottom dissolved oxygen and percent ice cover data for the entire deep water southern region (see Appendix S2; both significant factors in the GLMM) and temperature readings from near the mouth of the Sound (SMOUTH, Fig. Boje et al (2014) reported Greenland halibut occupying colder waters during the winter months in the deep inner icefjord of Disko Bay, a similar trend observed in this and a previous study in Cumberland Sound (Peklova et al 2012).…”
Section: Telemetry To Understand the Ecology Of Deep-water Marine Spementioning
confidence: 99%
“…In the southern deep region, fish occupied waters with oxygen concentrations of ~3.6-3.7 mg/L, similar to the values recorded during peak fish occurrence in the northern region. While Greenland halibut and flatfish generally have a low aerobic scope when compared with pelagic fishes (Dupont-Prinet et al 2013) and are reported to occur in high abundances at low Fig. 7.…”
Section: Telemetry To Understand the Ecology Of Deep-water Marine Spementioning
Management boundaries that define populations or stocks of fish form the basis of fisheries planning. In the Arctic, decreasing sea ice extent is driving increasing fisheries development, highlighting the need for ecological data to inform management. In Cumberland Sound, southwest Baffin Island, an indigenous community fishery was established in 1987 targeting Greenland halibut (Reinhardtius hippoglossoides) through the ice. Following its development, the Cumberland Sound Management Boundary (CSMB) was designated and a total allowable catch (TAC) assigned to the fishery. The CSMB was based on a sink population of Greenland halibut resident in the northern section of the Sound. Recent fishing activities south of the CSMB, however, raised concerns over fish residency, the effectiveness of the CSMB and the sustainability of the community-based winter fishery. Through acoustic telemetry monitoring at depths between 400 and 1200 m, and environmental and fisheries data, this study examined the movement patterns of Greenland halibut relative to the CSMB, the biotic and abiotic factors driving fish movement and the dynamics of the winter fishery. Greenland halibut undertook clear seasonal movements between the southern and northern regions of the Sound driven by temperature, dissolved oxygen, and sea ice cover with most fish crossing the CSMB on an annual basis. Over the lifespan of the fishery, landfast ice cover initially declined and then became variable, limiting accessibility to favored fisher locations. Concomitantly, catch per unit effort declined, reflecting the effect of changing ice conditions on the location and effort of the fishery. Ultimately, these telemetry data revealed that fishers now target less productive sites outside of their favored areas and, with continued decreases in ice, the winter fishery might cease to exist. In addition, these novel telemetry data revealed that the CSMB is ineffective and led to its relocation to the entrance of the Sound in 2014. The community fishery can now develop an open-water fishery in addition to the winter fishery to exploit the TAC, which will ensure the longevity of the fishery under projected climate-change scenarios. Telemetry shows great promise as a tool for understanding deep-water species and for directly informing fisheries management of these ecosystems that are inherently complex to study.
“…Intertidal invertebrates may be more tolerant as they are adapted to fluctuating environmental conditions (Leiva et al , ). By contrast, Vaquer‐Sunyer & Duarte () found that crustaceans were the least tolerant to hypoxia of all organisms they tested and that some tolerant groups such as bivalves may benefit from hypoxia due to reduced predation and competition, in a similar way to R. hippoglossoides (Mejri et al , ; Dupont‐Prinet et al , 2013 b ). Although bivalves may be more tolerant, sessile organisms will be generally more vulnerable as they cannot usually move to localities with higher oxygen concentrations if they need to, unlike mobile species such as fin fishes.…”
As a result of long-term climate change, regions of the ocean with low oxygen concentrations are predicted to occur more frequently and persist for longer periods of time in the future. When low levels of oxygen are present, this places additional pressure on marine organisms to meet their metabolic requirements, with implications for growth, feeding and reproduction. Extensive research has been carried out on the effects of acute hypoxia, but far less on long-term chronic effects of low oxygen zones, especially with regard to commercially important fishes and shellfishes. To provide further understanding on how commercial species could be affected, the results of relevant experiments must support population and ecosystem models. This is not easy because individual effects are wide-ranging; for example, studies to date have shown that low oxygen zones can affect predator-prey relationships as some species are able to tolerate low oxygen more than others. Some fishes may move away from areas until oxygen levels return to acceptable levels, while others take advantage of a reduced start response in prey fishes and remain in the area to feed. Sessile or less mobile species such as shellfishes are unable to move out of depleted oxygen zones. Some species can tolerate low oxygen levels for only short periods of time, while others are able to acclimatize. To advance the knowledge-base further, a number of promising technological and modelling-based developments and the role of physiological data within these, are proposed. These include advances in remote telemetry (tagging) and sensor technologies, trait-based analyses to provide insight into how whole assemblages might respond in the future, research into long-term adaptability of species, population and ecosystem modelling techniques and quantification of economic effects. In addition, more detailed oxygen monitoring and projections are required to better understand the likely temporal and local-scale changes in oxygen.
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