What goes up must come down: Diel vertical migration in the deep‐water sablefish (Anoplopoma fimbria) revealed by pop‐up satellite archival tags

The sablefish (Anoplopoma fimbria) is a long‐lived species with wide distribution throughout the North Pacific Ocean. While adult sablefish are considered a deep‐water fish, diet analyses suggest that they undergo vertical migrations that could be related to prey movement and feeding. Pop‐up satellite archival tags (PSATs) were used to observe the fine‐scale depth selection behavior of adult sablefish tagged off the Washington coast during the summer from June to August. Tags were physically retrieved after they surfaced using direction‐finding equipment so that complete datasets over the entire deployment were obtained from 14 tags. PSATs that recorded depth and temperature every 4 min during the deployment confirm that sablefish inhabit depths of 750 m or greater. However, a majority of the tagged fish underwent extensive vertical migrations that averaged 254.4 m overall and occurred at a 24 hr periodicity. Variations were observed among individuals in the amount of the deployment during which vertical migrations occurred, ranging from 12.37% to 63.48% of the time. During the vertical migration, fish ascended towards the surface at night and descended prior to daylight (i.e., diel vertical migration). Sablefish generally inhabited temperatures of 5°C but during the vertical migrations were found at temperatures from 6 to 10°C. Sablefish are opportunistic feeders with a large proportion of their diet being fish, euphausiids and cephalopods. Because these prey items also exhibit diel vertical migrations, it is possible that the vertical migratory behavior displayed by the sablefish was in response to the movements or the location of their prey.     

裸盖鱼幼鱼工厂化养殖试验

采用实验生态学的方法对裸盖鱼(Anoplopoma fimbria)幼鱼进行工厂化养殖试验,以了解和分析其生长特征。在地下海水温度(10.42±0.45)~(13.65±1.22)℃的条件下,经过210 d的养殖试验,裸盖鱼幼鱼由初始平均体重(33.27±5.82)g增长到(805.20±113.79)g,平均增重量最大值为(193.42±29.23)g/月,平均日增重量(3.68±0.61)g/d,最大日增重量(6.45±0.97)g/d。裸盖鱼幼鱼体长与体重呈幂函数关系,回归方程式为:W=0.017 4 L2.943 6(R2=0.973 1)。水温对裸盖鱼幼鱼的增重、存活率及饵料系数均有影响,结果显示,最适养殖水温为(11.32±0.75)~(12.68±0.92)℃,与1龄以上裸盖鱼的最适水温基本一致,在该水温范围内,裸盖鱼幼鱼生长迅速,饵料系数相对较低,存活率较高。研究表明,裸盖鱼喜低温,生长速度快,养殖效益显著,是极具开发前景的冷水性养殖鱼类。     

Decadal-scale patterns in the relative year class success of sablefish (Anoplopoma fimbria)

Climate–ocean regimes in the north-east Pacific translate into decadal-scale patterns in the relative success of sablefish ( Anoplopoma fimbria ). By combining estimates of year class abundance determined from commercial catches and research surveys for adults and juveniles, we were able to construct an index of year class success. Year classes from 1960 to 1976 were generally below average, with little indication of good year class success. The 1977 year class was exceptionally large and year classes from 1978 to 1990 were generally above average. Year classes following 1990 were generally below average. The periods with above-average year classes were generally characterized by intense Aleutian Lows, above-average frequency of south-westerly winds and warmer coastal sea surface temperatures off the west coast of Vancouver Island. Decadal-scale patterns in the production of sablefish suggest stability in long-term periods of similar recruitment but different mean levels of productivity across periods. However, rapid shifts between periods remain unpredictable and therefore complicate the incorporation of decadal-scale dynamics in management.     

Interannual changes in sablefish (Anoplopoma fimbria) recruitment in relation to oceanographic conditions within the California Current System

Sablefish (Anoplopoma fimbria) supports substantial fisheries in both the eastern and western Pacific Oceans. Juvenile recruitment along the west coast of the continental United States has been highly variable over the past three decades. Using a generalized additive model, we demonstrate that physical oceanographic variables within the California Current System have significant effects on sablefish recruitment. Significant relationships were found between juvenile recruitment and northward Ekman transport, eastward Ekman transport, and sea level during key times and at key locations within the habitat of this species. The model explains nearly 70% of the variability in sablefish recruitment between the years 1974 and 2000. The predictive power of the model was demonstrated by refitting without the last 5 yr of data and subsequent prediction of those years. Bootstrap assessments of bias associated with parameter estimates and jackknife‐after‐bootstrap assessments of the influence of individual data on parameter estimates are presented and discussed. Using this model, it is possible to draw preliminary conclusions concerning year‐class strength of cohorts not yet available to the survey gear as well as historic year‐class strengths. We discuss changes in zooplankton abundance and shifts in species of copepods associated with fluctuations in the physical variables that appear to have a major influence on sablefish recruitment.     

Effects of ontogeny, temperature, and light on vertical movements of larval Pacific cod (Gadus macrocephalus)

The role of behavior, especially vertical migration, is recognized as a critical component of realistic models of larval fish dispersion. Unfortunately, our understanding of these behaviors lags well behind our ability to construct three-dimensional flow-field models. Previous field studies of vertical behavior of larval Pacific cod ( Gadus macrocephalus ) were limited to small, preflexion stages (≤11 mm SL) in a narrow range of thermal conditions. To develop a more complete picture of larval behavior, we examined the effects of ontogeny, temperature, and light on vertical responses of larval Pacific cod in experimental columns. While eggs were strictly demersal, yolk-sac larvae displayed a strong surface orientation as early as 1 day post hatch (∼ 5 mm SL). Consistent with field observations, small preflexion larvae (<10 mm SL) showed no response to varying light levels. However, there was a direct effect of temperature on larval behavior: Pacific cod larvae exhibited a stronger surface orientation at 4°C than at 8°C. The behavior of larger, postflexion larvae (>15 mm SL) in experimental columns was consistent with a diel vertical migration and independent of water temperature: fish were more widely distributed in the column, and median positions were consistently deeper at higher light levels. These laboratory observations are combined with observations from discrete-depth (MOCNESS) sampling in the Gulf of Alaska to characterize the vertical distribution of larval Pacific cod and contrast ontogenetic patterns with walleye pollock ( Theragra chalcogramma ). The vertical movements of larval Pacific cod described here will be applied in the development of dispersal projections from Gulf of Alaska spawning grounds.     

采用声学方法研究2016年秋季布兰斯菲尔德海峡南极磷虾群昼夜垂直移动特征及其影响因素

近年来,南极磷虾渔业过于集中于布兰斯菲尔德海峡,这也使得该海区磷虾资源状况及其生态学特征日益受到关注。南极磷虾群具有较为明显的昼夜垂直移动特征,开展此方面的研究可为探索其渔场形成机制提供基础数据,并为磷虾渔业反馈式管理提供参考。基于磷虾渔船上Simrad EK80记录的相关声学数据,使用Echoview软件判别声学数据中的磷虾群体,对2016年秋季布兰斯菲尔德海峡南极磷虾群昼夜垂直移动特征进行分析,并进一步分析影响磷虾群昼夜垂直移动的因素。结果显示,3月和4月磷虾群深度基本维持在250 m以浅,虾群最大深度出现在日升时分的频次最高（22.9%）,而最浅深度出现在夜间时分的频次最高（36.0%）,同时在日升时分,虾群厚度达到最大值;白天磷虾群多集中在较深水层,夜间会上浮到较浅水层。随着月份的推移,磷虾群平均深度总体呈现加深的趋势。光强和海底深度是影响磷虾群深度变化的2个主要因素。     

Diel vertical migration of myctophid fishes (Family Myctophidae) in the transitional waters of the western North Pacific

The diel vertical migration patterns of adult myctophid fishes were determined in the transitional waters of the western North Pacific off Japan, using day–night sampling from 20 to 700 m depths with a commercial otter trawl in the summer of 1995. A total of 12 species belonging to 9 genera were collected. Four patterns were recognized in the diel vertical migration of 11 of the 12 species. (1) Migrants showing clear day–night habitat separation with peak abundance above 200 m at night: Symbolophorus californiensis, Tarletonbeania taylori, Notoscopelus japonicus, Diaphus theta, Ceratoscopelus warmingi, and Diaphus gigas. (2) Semi-migrants, in which part of the population often remains in the daytime habitat at night. The distribution depths of migratory and nonmigratory individuals do not overlap: Stenobrachius leucopsarus . (3) Passive-migrants, in which there is no separation of day–night habitats, but the upper limit of daytime distribution depth shifts to a shallower layer at night, probably as the fish follow migratory prey: Lampanyctus jordani . (4) Nonmigrants: Stenobrachius nannochir, Lampanyctus regalis (> 140 mm SL), and Protomyctophum thompsoni . The day–night habitat temperature ranges are also given for the 11 species. No remarkable east–west differences were seen in the vertical migration patterns compared with previous knowledge of eight of these species in the eastern Pacific. The diel migration patterns are newly described for three other species endemic to the western Pacific. The standing stock of myctophids in the study area was conservatively estimated at 18.5 ± 4.7 g m⁻² (avg. ± SD).     

2013年冬季南乔治亚岛南极磷虾群昼夜垂直移动研究

关于冬季南极磷虾群昼夜垂直移动方面的研究可为探索其渔场形成机制提供基础数据,并为其越冬策略研究提供参考。基于2013年冬季南乔治亚岛南极磷虾渔业调查期间收集的相关数据,对冬季南乔治亚岛南极磷虾群昼夜垂直移动进行了研究。结果发现,磷虾群平均深度维持在表层以下100～300 m,磷虾群最深出现在日升时分,而最浅则出现在夜间时分;7—9月,随时间的推移,磷虾群所处水层呈加深趋势。夜间、白天和黄昏时段磷虾群平均深度呈现较为明显的月份差异。白天磷虾群多集中在较深水层,夜间会上浮到较浅水层。     

Bottom-up forcing and the decline of Steller sea lions (Eumetopias jubatus) in Alaska: assessing the ocean climate hypothesis

Declines of Steller sea lion (Eumetopias jubatus) populations in the Aleutian Islands and Gulf of Alaska could be a consequence of physical oceanographic changes associated with the 1976–77 climate regime shift. Changes in ocean climate are hypothesized to have affected the quantity, quality, and accessibility of prey, which in turn may have affected the rates of birth and death of sea lions. Recent studies of the spatial and temporal variations in the ocean climate system of the North Pacific support this hypothesis. Ocean climate changes appear to have created adaptive opportunities for various species that are preyed upon by Steller sea lions at mid‐trophic levels. The east–west asymmetry of the oceanic response to climate forcing after 1976–77 is consistent with both the temporal aspect (populations decreased after the late 1970s) and the spatial aspect of the decline (western, but not eastern, sea lion populations decreased). These broad‐scale climate variations appear to be modulated by regionally sensitive biogeographic structures along the Aleutian Islands and Gulf of Alaska, which include a transition point from coastal to open‐ocean conditions at Samalga Pass westward along the Aleutian Islands. These transition points delineate distinct clusterings of different combinations of prey species, which are in turn correlated with differential population sizes and trajectories of Steller sea lions. Archaeological records spanning 4000 yr further indicate that sea lion populations have experienced major shifts in abundance in the past. Shifts in ocean climate are the most parsimonious underlying explanation for the broad suite of ecosystem changes that have been observed in the North Pacific Ocean in recent decades.     

Effects of rearing temperature on growth and survival of larval sablefish (Anoplopoma fimbria)

The effects of three different rearing temperatures (12, 15 and 18°C) on growth and survival of sablefish larvae (Anoplopoma fimbria) were examined from 5 days poststocking to weaned subjuveniles. First‐feeding larvae were stocked into 960‐L circular tanks at a density of 15 larvae/L (n = 3 per temperature treatment). Feeding, increases in light and water flow and other changes during the experiment were based on a degree‐day (°Cday) schedule to adjust for time and temperature. The larvae were weaned on calendar day 41, 34 and 30 in the 12, 15 and 18°C treatments respectively. Survival to weaning was greater at 15 than 12 or 18°C. Calendar day and degree‐day length and dry weight were greater in the 18°C treatment. The larvae were weaned 7 days earlier at 15°C and 11 days earlier at 18°C compared to larvae at 12°C. Sablefish larvae can be reared at 15°C with faster growth and good survival compared to 12°C and at an approximately 17% reduction in cost and labour. Sablefish grew even faster but had higher mortality rates at 18°C compared to 15°C. Results from genotyping strongly suggest that there is a genetic basis for performing differentially at varying rearing temperatures and would also suggest that selection for faster growth and higher survival could be accomplished in a broodstock programme.     

Use of juvenile salmon growth and temperature change indices to predict groundfish post age‐0 yr class strengths in the Gulf of Alaska and eastern Bering Sea

Juvenile marine growth (SW1) of salmon and a new temperature change (TC) index were evaluated as ecosystem indicators and predictors for the post age‐0 year class strength (YCS) of groundfish in the Gulf of Alaska (GOA) and eastern Bering Sea (EBS). Our hypothesis was that SW1, as measured on the scales of adult Pacific salmon (Oncorhynchus spp.), is a proxy for ocean productivity on the continental shelf, a rearing area for young salmon and groundfish. Less negative TC index values are the result of a cool late summer followed by a warm spring, conditions favorable for groundfish YCS. In the GOA, SW1 was a positive predictor of age‐1 pollock (Theragra chalcogramma), but not age‐2 sablefish (Anoplopoma fimbria) YCS, indicating that the growth of the Karluk River sockeye salmon that enter Shelikof Strait is a proxy for ocean conditions experienced by age‐0 pollock. Contrary to our hypotheses, the TC index was a negative predictor of GOA pollock YCS; and the SW1 a negative predictor of EBS pollock and cod YCS since the 1980s. Recent fisheries oceanography survey results provide insight into possible mechanisms to support the inverse SW1 and YCS relationship. For the EBS, the TC index was a significant positive predictor for pollock and cod YCS, supporting the hypothesis that a cool late summer followed by a warm spring maximizes the over‐wintering survival of pollock and cod (Gadus macrocephalus), especially since the 1980s. The TC and SW1 index showed value for the assessment of pollock and cod, but not sablefish.     

Evaluation of cold‐pressed flaxseed oil as an alternative dietary lipid source for juvenile sablefish (Anoplopoma fimbria)

This study was undertaken to determine the suitability of using cold‐pressed flaxseed oil (FO) as a major source of lipid in place of anchovy oil (AO) in the diet of juvenile sablefish (Anoplopoma fimbria), a relatively new marine species to aquaculture. Sablefish were fed one of four diets twice daily to satiation for 15 weeks. The test diets were identical in composition, except for the source of supplemental lipid which was either 100% AO (100AO), or increasing replacement of AO with FO i.e., 75AO:25FO, 50AO:50 FO or 25AO:75FO. Sablefish growth parameters, whole body and fillet proximate constituent concentrations and apparent digestibility coefficients were uninfluenced by diet treatment. There were also no adverse effects of the diet treatments on fish health, as determined from analysis of various haematological and innate immunological parameters. Terminal fillet fatty acid compositions generally reflected the dietary fatty acid compositions, while flesh contaminant concentration decreased with increasing dietary flaxseed oil content. Results indicated that FO may comprise up to 75% of the supplemental lipid in a grower diet for sablefish, while still providing humans with a rich dietary source of highly unsaturated fatty acids.     

Biogeography of pelagic food webs in the North Pacific

The tufted puffin (Fratercula cirrhata) is a generalist seabird that breeds throughout the North Pacific and eats more than 75 different prey species. Using puffins as samplers, we characterized the geographic variability in pelagic food webs across the subarctic North Pacific from the composition of ~10,000 tufted puffin meals (~56,000 prey items) collected at 35 colonies in the Gulf of Alaska (GoA) and Aleutian Archipelago. Cluster analysis of diet species composition suggested three distinct forage fish communities: (i) in the northern GoA, multiple age‐classes of coastal and shelf residents such as capelin, sand lance and herring dominated the food web, (ii) in the western GoA to eastern Aleutians, the shelf community was dominated by transient age‐0 walleye pollock, and (iii) in the western Aleutians, shelf‐edge and mesopelagic forage species such as squid, lanternfish, and Atka mackerel were prevalent. Geographic patterns of abundance of capelin and sand lance in tufted puffin diets were corroborated by independent research fisheries and diets of piscivorous fish, indicating that puffin diets reflect the local abundance of forage species, not just selection of favored species. Generalized additive models showed that habitat characteristics predict, in a non‐linear fashion, forage species distribution and abundance across two large marine ecosystems. We conclude that major biogeographic patterns in forage fish distribution follow gradients in key habitat features, and puffin diets reflect those patterns.     

Body size trends along vertical and thermal gradients of chum salmon in the Bering Sea during summer

Relationships between the vertical distribution and thermal habitat, and body size of chum salmon Oncorhynchus keta were studied in the Bering Sea in summer using trawl surveys at various depths. Chum salmon abundance decreased with increasing depth, but the patterns of decrease differed between size groups. The abundance of small salmon fell rapidly with depth, whereas that of large salmon decreased gradually to 40 m depth, and abruptly below that. The average fork length of chum salmon collected from each trawl correlated positively with trawl net depth and negatively with water temperature. Since the optimal temperature for growth decreases with body size in this species, the observed body size‐related vertical habitat use by chum salmon may indicate size‐dependent thermal preferences.     

The influence of diel vertical migration on zooplankton transport and recruitment in an upwelling region: estimates from a coupled behavioral-physical model

Diel vertical migration (DVM) is a common zooplankton behavior in which organisms reside in surface or near‐surface waters at night and at deeper depths during the day. In many upwelling regions, DVM reduces the transport of organisms away from the region. It is unclear, however, what role DVM plays in recruitment (the arrival of larvae or juveniles to locations where they will become reproducing adults) to upwelling regions. In this study, we estimate the influence of DVM on zooplankton transport, the level of recruitment of locally produced propagules (self‐recruitment), and sources of recruits in the upwelling region near Monterey Bay, California, by simulating the trajectories of fixed‐depth and vertically migrating organisms with a drifter‐tracking algorithm driven by climatological velocity fields from a three‐dimensional hydrodynamic model. Our simulations suggest that DVM into subsurface poleward and onshore currents during the day does not fully compensate for equatorward and offshore transport in the surface Ekman layer at night and does not retain zooplankton in the Monterey Bay region. Our simulations also suggest that DVM decreases the ability of zooplankton to return to the region after being transported away and shifts source regions for recruits closer to the bay. While DVM does not appear to substantially increase the potential for self‐recruitment to the region, this study indicates that other mechanisms, such as transport during non‐upwelling periods, continuous transport below the surface, increases in mean transport depth over time, or seasonal changes in hydrography, may still enable relatively high levels of self‐recruitment to this highly advective region.     

Lipids,buoyancy and the seasonal vertical migration of Calanus finmarchicus

The copepod Calanus finmarchicus remains in diapause for up to 5 months in the cold (<0.5°C) deep (>700 m) waters of the Faroe–Shetland Channel of the north-western approaches to the North Sea. While in diapause, C. finmarchicus has a high lipid content, up to 76% of dry weight, mostly in the form of wax esters. The question we address here is how copepods with such a high content of buoyant lipids can remain in diapause at depth for an extended period of time? The corollary to this is how this lipid content hinders and/or assists the copepods in their seasonal vertical migration? Part of the answer is due to the physical properties of wax esters. These have a thermal expansion and compressibility higher than that of sea water. Thus, depending on their relative composition (i.e. wax esters/water/protein/chitin), a copepod that is positively buoyant in warm surface waters can become neutrally buoyant in cold deep water. We develop a simple three component physical model of a copepod to explore how and where they attain neutral buoyancy, how the lipid content can aid in their ascent, and what fraction of the lipids can be utilized in ascent in gonad/egg formation while maintaining observed ascent rates. As well as being an energy reserve, the results show that rather than being a barrier to vertical migration, wax esters serve as an important regulator of buoyancy.     

Lipids, buoyancy and the seasonal vertical migration of Calanus finmarchicus

The copepod Calanus finmarchicus remains in diapause for up to 5 months in the cold (<0.5°C) deep (>700 m) waters of the Faroe–Shetland Channel of the north-western approaches to the North Sea. While in diapause, C. finmarchicus has a high lipid content, up to 76% of dry weight, mostly in the form of wax esters. The question we address here is how copepods with such a high content of buoyant lipids can remain in diapause at depth for an extended period of time? The corollary to this is how this lipid content hinders and/or assists the copepods in their seasonal vertical migration? Part of the answer is due to the physical properties of wax esters. These have a thermal expansion and compressibility higher than that of sea water. Thus, depending on their relative composition (i.e. wax esters/water/protein/chitin), a copepod that is positively buoyant in warm surface waters can become neutrally buoyant in cold deep water. We develop a simple three component physical model of a copepod to explore how and where they attain neutral buoyancy, how the lipid content can aid in their ascent, and what fraction of the lipids can be utilized in ascent in gonad/egg formation while maintaining observed ascent rates. As well as being an energy reserve, the results show that rather than being a barrier to vertical migration, wax esters serve as an important regulator of buoyancy.