The seaward movement of Atlantic salmon smolts in the Usk estuary, Wales, as inferred from power station catches

The greatest numbers of Atlantic salmon smolts were caught at Uskmouth power station during the day on the flood tide and the least on an ebbing night tide. Catch rates during the day on an ebb tide and at night on a flood tide represented an intermediate state. The results, together with tracking data, suggest that salmon smolts prefer to migrate seaward through the lower Usk estuary during the night Oncc an ebbing tide.     

Examining mummichog growth and movement: Are some individuals making intra-season migrations to optimize growth?

We used a combination of field experiments and stable isotopes to examine mummichog growth and movement within a New England estuary. We documented physical and biological patterns within the estuary by caging individually-marked fish in enclosures at four locations along a coastal river and measuring environmental parameters (e.g., salinity, tidal inundation) and fish characteristics (e.g., gut-contents, growth, and stable isotope values) at each location. The upstream location was fresh (1 ppt) at low tide, and the downstream location was saline at high tide (32 ppt). The upstream and downstream locations had more tidal inundation than the intermediate location. Fish gut contents were dominated by terrestrial insects at the upstream location, by algae and detritus at the intermediate locations, and by aquatic insects at the downstream location. Fish grew fastest at the upstream location and slowest at the downstream location. Stable isotope values (δ¹³C and δ¹⁵N) of fish held in cages were significantly different at upstream, intermediate, and downstream locations. We transferred fish from one location to another in order to document how stable isotope values change when fish switch diets by moving within this estuary. Because differences in rates at which different tissue types approach the isotopic value of new diet sources can be used as a way to estimate the time since diet shift, we used the δ¹³C and δ¹⁵N values of liver and muscle as indicators of short term previous diet (liver) and longer term previous diet (muscle). We collected wild (uncaged) mummichogs from each location, and we compared their liver and muscle isotope values to values of fish that were transferred among locations. When fish were transferred from one location to another, their stable isotope values were intermediate between expected values at the previous and current locations. The liver approached stable isotope values representative of current location faster than muscle. Wild fish showed greater variation in stable isotope values than fish held in cages. Wild fish from the upstream location showed patterns in liver and muscle stable isotope values that were consistent with patterns in fish that were transferred from the downstream location to the upstream location (∼ 10 km away). These patterns in stable isotope values could have multiple causes including intra-season movement between downstream and upstream locations.     

Larval and juvenile fishes occurring with flood tides on an intertidal mudflat in the Tama River estuary, central Japan

Intertidal movements of fish larvae and juveniles on a mudflat in the Tama River estuary, central Japan, were investigated by comparing the abundance and sizes of fishes caught in the intertidal zone during flood tides with those in the subtidal zone during low tides. A total of 28465 individuals, belonging to 9 families and 20 species, were collected by small purse seine. Among the abundant species, planktonic larvae and juveniles of gobiids and Konosirus punctatus were more abundant in the intertidal zone at flood tide than the subtidal zone at low tide. Similar occurrence patterns were found in juvenile Plecoglossus altivelis altivelis and Lateolabrax japonicus, having fully developed swimming abilities. In contrast to these species, much higher abundances of epibenthic juveniles of 2 gobiids (Acanthogobius flavimanus and Gymnogobius macrognathos) were found in the subtidal zone at low tide, although they also utilized the intertidal zone at flood tide.     

Tidal and diel timing of river entry by adult Atlantic salmon returning to the Aberdeenshire Dee, Scotland

The timing of salmon migration from the estuary of the Aberdeenshire Dee into the river in relation to tidal phase and time of day was studied by combined acoustic and radio-tracking of individual fish and by analysing records of untagged fish from a resistivity fish counter 0.8 km upstream from the tidal limit. Up-estuary movements that led to river entry were predominantly nocturnal and tended to occur during the ebb tide. Penetration into the non-tidal reaches of the river also tended to occur at night, but the timing of salmon movements was no longer significantly associated with tidal phase. The tracking data suggested that the reduction in the strength of the association between salmon migration and tidal phase resulted from variability in rates of progress from the estuary to the river. This variability may have been random, or related to changes in migratory behaviour during entry to fresh water. A simulation of upstream progress by groups of salmon illustrated the decay of the relationship between salmon movements and tidal phase and the advance of the average tidal phase of observed salmon movements with increasing distance of the observation point from where movements were initiated. The magnitude of these effects depended on the average rate of upstream progress and variability in the rate of progress, being greatest when upstream progress was slow and variable. These results highlight a limitation of point observations of migration with regard to identifying environmental stimuli for migration and quantifying their effects.     

Flow-carried and active swimming migration of the glass eel(Anguilla anguilla) in the tidal area of a small estuary on the French Atlantic coast

The study of the migration dynamics of glass eels(Anguilla anguilla) in a small estuary of the French Atlantic coast shows a two-stage sequence: (1) From November to March, the glass eels migrate upstream by using the tidal currents. The estuarine hydrology leads to a natural trapping of migrants in a typical area where the current speed slows down. The location of this zone depends on hydraulic conditions. The greater the tide is the farther upstream this area will be. This phenomenon leads to an increasing catchability of elvers. (2) From April onwards, when the water temperature reaches 10–12 °C, the glass eels swim actively upstream in the estuary. Then, fish concentrate just below the first dam. This behaviour shift shows the beginning of the colonization process of the whole riverine system.     

The seasonal occurrence of postlarval stages of yellowfin bream, Acanthopagrus australis (Gunther), and some factors affecting their movement into an estuary

Planktonic postlarvae of yellow fin bream Acanthopagrus australis were found at surf bar entrances to Moreton Bay, a large subtropical estuarine system on the east coast of Australia. The postlarvae occurred from April to September with peak abundance during July to September. Most postlarvae entered the estuary at night during the full moon. They were more abundant on the flood and full tides than on the ebb tide. The transition from planktonic to littoral existence occurs from August to November when the fish are 13-14 mm in length. Young yellow fin bream in littoral areas reach a modal length in excess of 100 mm after 1 year.     

Physiological preparedness and performance of Atlantic salmon Salmo salar smolts in relation to behavioural salinity preferences and thresholds

This study investigated the relationships between behavioural responses of Atlantic salmon Salmo salar smolts to saltwater (SW) exposure and physiological characteristics of smolts in laboratory experiments. It concurrently described the behaviour of acoustically tagged smolts with respect to SW and tidal cycles during estuary migration. Salmo salar smolts increased their use of SW relative to fresh water (FW) from April to June in laboratory experiments. Mean preference for SW never exceeded 50% of time in any group. Preference for SW increased throughout the course of smolt development. Maximum continuous time spent in SW was positively related to gill Na⁺, K⁺‐ATPase (NKA) activity and osmoregulatory performance in full‐strength SW (measured as change in gill NKA activity and plasma osmolality). Smolts decreased depth upon reaching areas of the Penobscot Estuary where SW was present, and all fish became more surface oriented during passage from head of tide to the ocean. Acoustically tagged, migrating smolts with low gill NKA activity moved faster in FW reaches of the estuary than those with higher gill NKA activity. There was no difference in movement rate through SW reaches of the estuary based on gill NKA activity. Migrating fish moved with tidal flow during the passage of the lower estuary based on the observed patterns in both vertical and horizontal movements. The results indicate that smolts select low‐salinity water during estuary migration and use tidal currents to minimize energetic investment in seaward migration. Seasonal changes in osmoregulatory ability highlight the importance of the timing of stocking and estuary arrival.     

River and estuary movements of yellow‐stage American eels Anguilla rostrata,using a hydrophone array

Patterns of summertime movement and habitat use of yellow‐stage American eels Anguilla rostrata within York River and estuary and Gaspé Bay (Gaspesia, Québec, Canada) were examined using acoustic telemetry. Fifty fish were tagged with acoustic transmitters and released, either in the river or in the upper estuary, and their patterns of movement and habitat use were monitored at short spatial and temporal scales during the summer months using a dense hydrophone array. Approximately half of the fish released in the river swam to the estuary; two‐thirds of the fish released within the estuary did not move out of the estuary. Anguilla rostrata were detected more frequently and had a greater areal range of detections during night, suggesting greater nocturnal activity. Longitudinal movements within the estuary tended to occur nocturnally, with upstream movements from early to late evening, and downstream movements from late evening to early morning. Approximately one‐third of fish showed a regular pattern of movement, tending to reside in the deeper, downstream part of the estuary during day and in the shallower, more upstream part of the estuary during night. Approximately a quarter of fish, located in the upper estuary, remained upstream during both night and day. The remaining fish showed patterns intermediate between these two.     

Biotic interactions enhance survival and fitness in the caddisfly <Emphasis Type="Italic">Micropterna sequax</Emphasis> (Trichoptera: Limnephilidae)

Fish-based index of biotic integrity (F-IBI) is widely used to assess river ecosystems. With survey data from the Yellow River fishery resources in the 1980s and 2008, fish composition and abundance, vertical distribution, trophic structure, reproductive guilds and tolerance in the river’s upstream, midstream, downstream, and estuary were examined, and F-IBI systems were established for each reach to assess river ecosystem health. Results showed that compared to the 1980s, the number of fish species in 2008 sharply declined in the midstream and downstream reaches, percentage of benthic fish species decreased in upstream and estuary, the number and percentage of omnivorous species decreased in all reaches, and percentage of tolerant fish species increased 15 times in upstream but decreased in midstream and downstream. The F-IBI scores in the four reaches in the 1980s were all higher than those in 2008 and decreased from upstream to estuary; the healthy conditions indicated by F-IBI scores in the 1980s were “good,” “fair,” “poor,” and “fair” from upstream to estuary and “degraded” to “poor” in all the reaches in 2008. This indicated that the river ecosystem has degraded from the 1980s to 2008. This was also shown by variations in water chemistry.     

Larval life history strategies of sub-tropical southern African estuarine brachyuran crabs and implications for tidal inlet management

Soon after hatching the larvae of many estuarine crabs migrate from estuaries to adjacent coastal waters soon, where larval development is completed before the post larval stages recruit to estuaries to settle. This study investigated the larval flux of several brachyuran crabs resident within a subtropical estuary on the east coast of South Africa. Plankton sampleswere collected over two intensive sampling periods during the spring of1997 (19 days) and the summer of 1998 (26 days). Larvae were releasedmaximally when high tide within the estuary was crepuscular, whilerecruitment occurred during nocturnal flood tides, with peak abundanceson the maximum amplitude nocturnal flood tides. The data are discussedin relation to freshwater inflow problems facing South African estuaries andthe active management of the tidal inlets of affected systems.     

The turbidity maximum in the Tamar estuary

Many estuaries of medium to high tidal range exhibit an accumulation of fine cohesive material in their upper reaches in the region of the limit of saline intrusion. Much, or all, of this material is suspended each tidal cycle and the entire region undergoes a seasonal variation which appears to depend on fluvial input. Two factors which are throught to influence the formation and maintenance of turbidity maxima are the differing magnitudes of the bed shear stress (τ₀) on flood and ebb tides and the large vertical density gradient which developes on the ebb tide. Crucial to the importance of the first factor is that τ₀ exceeds a critical value, at which erosion occurs, for a greater period on the flood than on the ebb. The effect of the density gradient is that upward propagation of bed generated eddies is inhibited and the sediment is not transported into the upper part of the flow where it will be most effectively transported. It is not clear which, if either, of these mechanisms is dominant. Data consisting of vertical profiles of velocity, salinity and suspended solids were collected at four stations in the Tamar estuary during a high range tidal cycle. One station, at which the depth mean salinity (S _d ) varied from 0.0 to ∼ 12.0‰, was occupied permanently. The other stations were occupied such that data were collected asS _d varied in the range 0.0 to ∼ 4.0‰. In this way each station was occupied for a period of time on the ebb and flood tide. Observations show that during the early ebb, when the flow is relatively deep and slow, stratification persist untilS _d ∼ 0.0‰ and that no significant transport occurs while the flow is saline but that there is a rapid increase in suspended solids concentrations after this time. During the later ebb the shallower faster flow allowed the density gradient to be erode and significant transport was observed atS _d ∼ 5.0‰. On the flood tide the flow in the low salinity region is well-mixed troughout. Computation of the fluxes and total transport per unit breath of estuary show that on the ebb tide the quantity of solid material being transported by the low salinity (0–3‰) region remains nearly constant as this region of the flow is advebted seaward. On the flood tide, however, as the same region is advected landward the quantity of material being transported increases. It is concluded that in the Tamar estuary the early ebb tide stratification contributed to the formation and maintenance of a turbidity maximum which is strongly associated with the low salinity region of the flow. It is also speculated that the differences in the ebb and flood tide transport are caused by differences in the availability of mobile material on the bed at different stages of the tidal cycle.     

First results with a new estuarine fish tracking system

A 'sonar buoy' tracking system has been developed at the MAFF Fisheries Laboratory based upon acoustic transmitting tags and relay units which retransmit the pulsed acoustic signal as a radio signal. The output from several such 'sonar buoys' is monitored by a single automatic recording station on the shore. The system has been used on salmon in the estuary of the River Fowey in Cornwall, providing useful data on the behaviour of returning adults before they enter the river. The tags also transmit a radio frequency signal to allow tracking in the river itself. Of fourteen fish tagged in 1985, six were recorded entering the river between 12 h and 41 days after being released. Another fish was recaptured in a coastal net 160 km to the east. These few preliminary results indicated two distinct patterns of behaviour: one fish remained in deep water in the lower estuary for several days, often lying near moored ships or jetties; at other times fish made extensive excursions up the estuary with the tide, usually returning with the ebb.     

The vertical and transverse distribution of larval herring in the River Blackwater estuary, Essex

The vertical and transverse distributions of spring-spawned larval herring were studied in the River Blackwater estuary, Essex. Sampling was undertaken during May when larval densities within the estuary were at a maximum for the year. At this time, larval lengths were in the range 7–16 mm. No clear diel pattern in the vertical distribution was found, although larval distribution at night was more even.
The tides were found to influence the vertical distribution. Surface waters (< 1.5 m in depth) were avoided during both flood and ebb tides, but used during slack water. Larval densities at ebb were higher near the sea bed than during the flood tide. It was concluded that this behaviour will tend to transport larvae into and retain them within the estuary.     

Tidal transport of the bay anchovy, Anchoa mithchilli, in darkness

Transport of the adult bay anchovy, Anchoa mitchilli , in darkness was studied in laboratory and field experiments. In a hydraulic flume, anchovy schooling ceased in darkness and, at a current speed of 30cms⁻¹, 99% of all fish were transported to the end of the flume. In field experiments, fish marked with neutral red dye and released in a creek at flood tide were recaptured 5–1 km upstream 4 h after release at night, and were recaptured within 200m of the release site 3 h after release in daylight. It is concluded that in the neutral environment, bay anchovy schools break up at night and individual fish are transported by currents, whereas in daylight, bay anchovy schools maintain a relatively fixed location. This nocturnal transport phenomena may also exist in other marine and estuarine pelagic fishes, and may help in understanding behaviour and distribution of peiagic estuarine fishes.     

Environmental capacity of receiving water as basis for regulating intensity of milkfish (Chanos chanos Forsskal) culture

This paper presents the results of the assessment of the environmental condition of a receiving water and demonstrates how the environmental capacity of the system can be estimated based on effluent discharge from milkfish ponds and water criteria from scientific literature and other studies. An estuary (average volume, 295 333 m³; average depth, 1.9 m) in Punta Pulao, Dumangas, Iloilo, Philippines served as discharge and irrigation system for commercial milkfish ponds and experimental/verification ponds owned by the Southeast Asian Fisheries Development Center. Total ammonia nitrogen, nitrite, nitrate, phosphate, and chlorophyll a (chl a) were determined monthly (during spring tide) for 4 months. Samples were taken at low and high tides that coincided with the draining and flooding of ponds, respectively. Monthly concentrations of these water quality variables generally increased from the first to fourth month of sampling (April–July 2001) during low tide. Very slight increases were observed during high tide. The magnitude of changes in the diurnal patterns of phosphate, chl a, and dissolved oxygen appeared to be higher at spring tide than at neap tide. This indicates that the inflowing river at low tide (during spring tide) brought effluents containing high amounts of nutrients from ponds located upstream. The water, salt, dissolved inorganic nitrogen (DIN), and phosphate (DIP) budgets of the entire estuary were determined following the one‐box model by LOICZ‐IGBP (2000, LOICZ biochemical budgeting procedure: a tutorial pamphlet. L. T. David, M. L. San Diego‐McGlone, C. J. Crossland and S. V. Smith (Eds). Publ. for LOICZ International Project Office, the Netherlands, 29 pp.). The budgets indicate that the system is net heterotrophic and nitrogen (N) fixing during the dry months, but that there could be no environmental impact during the rainy months because of short water exchange time. Results further suggest that the system is a source of N and phosphorus (P) during the dry and rainy months; the condition is largely influenced by the high amount of nutrient inputs in to the river. Linear regression analysis was performed to determine relationship between nutrient concentrations in the system and total DIN or DIP input to the system at low tide. Environmental capacity in terms of the maximum amount of DIN or DIP input to the system was predicted using regression analysis and following set criteria for nutrients, i.e. nitrite, nitrate, and phosphate. At present, the estuarine water quality has already reached its environmental capacity during the dry months. About 945 ha of commercial milkfish ponds are operating upstream, mostly as extensive systems. If these ponds are converted to semi‐intensive or intensive systems, it is recommended that the pond area be reduced to 122 ha if the DIP criterion is to be followed so as not to exceed the environmental capacity. Exceeding this environmental capacity may affect production through reduction of fish growth, occurrence of diseases, and fish mortalities.     

The influence of freshwater flows on two estuarine resident fish species show differential sensitivity to the impacts of drought,flood and climate change

Estuaries are particularly susceptible to climate change and drought resulting in atypical changes to freshwater flows. How such changes in flow impact on the ecology of estuarine fishes may depend on how a species moves in response to changing flow conditions. Acoustic telemetry was used to interpret fine-scale movements of two co-inhabiting estuarine fish species, black bream, Acanthopagrus butcheri and estuary perch, Macquaria colonorum in relation to freshwater flows, season and moon phase. We found black bream to be highly mobile, regularly travelling the length of the estuary and into the neighbouring estuaries. In contrast, estuary perch had particular home ranges and made occasional, upstream or downstream movements. Possibly influenced by freshwater flows, estuary perch moved at greater rates in the Tambo compared to fish in the Mitchell. Black bream resided in the upper estuary during winter and spring and the lower estuary during summer and autumn, whereas estuary perch remained in the upper estuary throughout the year, with occasional downstream movements in winter and spring. This study revealed 1) significantly large increases in freshwater flows result in mass downstream movements in both species, 2) fish moved upstream during full moons and 3) there are contrasting spatio-temporal patterns in movement between species. The results from this study highlight that estuarine fishes are likely to show differential sensitivity to the impacts of drought and climate change and illustrate how acoustic telemetry methods can be used to determine the environmental needs of fishes and help efforts to conserve and manage estuaries worldwide.     

Sources of fish in the ephemeral western iishana region of the Cuvelai–Etosha Basin in Angola and Namibia

The triangle between the Kavango and Kunene rivers is drained by the Cuvelai, an ephemeral and deltaic drainage system covering more than 100 000 km². In good rainfall years, the area becomes populated by fish communities dominated by five species migrating southward towards the endorheic Etosha Pan, the basin’s terminal sump. When water dries up, fish subsequently die-off and their sudden appearance in rainy years has captivated scientists for decades. The current study was prompted by hitherto untapped indigenous knowledge through narratives of opportunistic fish harvesting of migrating fish at temporary connections between the Kunene River and the Cuvelai- Etosha Basin. A reconnaissance fish survey in 2017 was complemented by digital satellite images and elevation data analyses. Results support the presence of at least three major ephemeral fish migration routes. The dominant fish genera migrating upstream in Kunene tributaries comprise Enteromius, Oreochromis and Clarias, all eurytopic and known to undertake upstream, lateral and downstream migrations on floodplains. Although other notable fish refugia in the Cuvelai–Etosha Basin are yet to be identified, there is a necessity for the protection and management of these migration routes in tandem with studies on the nature and extent of this inter-basin fish migration under climate change and variability.     

Evidence for female-biased juvenile dispersal in corophiid amphipods from a New Zealand estuary

This study examined the distribution and dispersal of corophiid amphipods (Paracorophium spp.) in a temperate New Zealand estuary. Individuals in the sediment (resident population) and those caught in bed-load (local-scale movement) and suspended-load (larger-scale movement) were counted, measured, and sexed, during two tidal cycles at 4-6 week intervals spanning 13 months. Gravid females and juveniles were present in the resident population on all sample dates suggesting near continuous reproduction. Juveniles (< 2.2 mm body length) accounted for 49.8% of individuals in the sediment, compared to 65.4% of those caught in the bed-load and suspended-load traps. For the majority of sample dates, there was a net export of juveniles from the estuary. The total number of juveniles captured in suspended-load traps was significantly greater during the ebb tide relative to the flood tide (n = 541 versus 256), whereas no significant differences were found for adults. Similarly, numbers in the bed-load traps were significantly greater for juveniles during the ebb versus the flood tide (n = 900 versus 484), and also for adult females (n = 180 versus 86). Juvenile sex ratios were female biased in the sediment (9.8:1) and in suspended-load traps (7.6:1) and both were significantly more female-biased than that recorded for juveniles caught in bed-load traps (5.8:1). By contrast, there was a significantly lower proportion of adult females to adult males found in bed-load traps (1.7:1) and in suspended-load traps (0.98:1) compared to the resident population in the sediment (3.6:1). The mean size of juvenile females caught on a flood tide was significantly larger compared to those on the ebb tide, yet juvenile males were not significantly different, suggesting that smaller females were not returning on the flood tide. We suggest that female-biased juvenile dispersal for estuarine Paracorophium spp. lowers the risk of inbreeding and reduces competition. This may have evolved in response to a polygamous breeding system with little or no social organisation where a female produces more female offspring to maximise her inclusive fitness.     

Movements of juvenile Dover sole, Solea solea (L.), in the Tamar Estuary, South-western England

Solea solea start to appear in the Tamar Estuary in April–May when they are 10 mm long. The majority of young sole move into the estuary in June–July. Most sole leave the estuary towards the end of their second year in October–November, when they have reached a total length of 150–200 mm. The young O-group fish remain in the main channel, whereas the I-group move with the tide onto the mud-flats.
Approximately 7000 fish were marked by freeze-branding or dye-injection. The recaptures showed that there was an up-estuary migration in May–June. Most of the recaptures were taken at the site of original capture and there was only a limited movement of fish between adjacent mud-flat areas. Average growth rate tends to be greater in sole inhabiting the upper reaches of the estuary.     

Changes of fish assemblages after construction of an estuary barrage in the lower Nakdong River,South Korea

In the Nakdong River, an estuary barrage was constructed in 1987, and it divided the freshwater and the seawater, resulting in a change in the ecosystem. To estimate the impact of barrage construction on fish assemblages, we evaluated 20 years of monitoring data before and after the construction of the estuary barrage, and evaluated the role of fishways. The barrage construction generated entire changes of fish assemblages. After construction, the number of fish species dropped sharply, and 36 species disappeared. Conversely, 18 species appeared at this site, including eight freshwater species, seven of which were exotic or translocated species. Barrage construction affected freshwater fish more severely than it did estuarine and marine species because of the existence of an estuarine environment below the barrage. We did not detect any evidence of recovery of fish assemblages. A total of 31 species were collected at fishways, and the number of individuals collected at each fishway was positively correlated with the amount of discharge from the estuary barrage, mean daily tide level, and water temperature. Migratory fish using a fishway had obvious occurrence periods. Therefore, the efficiency of fishway use can be increased if an appropriate management plan is prepared and implemented.