Composition Of Fish Fauna Research Articles

Does the composition of the demersal fish assemblages in temperate coastal waters change with depth and undergo consistent seasonal changes?

The aim of this study was to determine whether the composition of the demersal fish fauna in coastal marine waters in temperate Australia changes markedly with increasing water depth and distance from the shore and whether the composition of the fish fauna in water depths of 5 to 35 m undergoes cyclic, seasonal changes. Samples of demersal fishes were therefore collected by trawling over the predominantly sandy substrate at nine sites located in water depths of 5 to 15 m or 20 to 35 m and within 20 km of the shore in four regions along ~200 km on the lower west coast of Australia. The sampling regime involved trawling for fishes at each site at night in seven consecutive seasons between the summer of 1990/1991 and winter of 1992. A total of 72 435 fishes, representing 77 families, 143 genera and 172 species was caught. The compositions of the fish faunas in offshore waters with depths of 5 to 35 m were shown to differ markedly from those previously recorded for nearshore marine waters in the same regions. However, as some species; such as Sillago burrus, S. vittata, S. bassensis and Rhabdosargus sarba, increase in size, they move out from their nursery areas in nearshore waters into deeper and more offshore waters, where spawning occurs. Ordination showed that, in each of the four regions, the composition of the fish fauna in depths of 5 to 15 m differs from that in depths of 20 to 35 m. This difference is attributable to the fact that some species, such as S. burrus, S. vittata and Upeneichthys lineatus, are far more abundant in depths of 5 to 15 m, whereas other species, such as S. robusta, U. stotti and Lepidotrigla modesta, occur predominantly in depths of 20 to 35 m. However, the samples collected from the single site that was inshore but in deeper water demonstrate that the composition of the fish fauna is influenced by distance from shore as well as by water depth. The compositions of the fish faunas differed with latitude, largely due to the fact that some subtropical species, such as Polyspina piosae, S. burrus and S. robusta, did not extend down into the more southern regions. Ordination also showed that the composition of the fish faunas at all but one of the nine sites underwent pronounced and consistent cyclic, seasonal changes. This seasonal cyclicity at the different sites was attributable to sequential patterns of immigrations and emigrations by a number of fish species during the course of the year. These seasonal migrations involved, inter alia (1) movements of certain species from their nursery areas into these deeper waters, e.g. S. bassensis and Scobinichthys granulatus; (2) migrations into and off the sandy areas of the inner continental shelf, e.g. Arnoglossus muelleri; (3) migrations to spawning areas, e.g. Sillago robusta; and (4) movements into areas where detached macrophytes accumulate in winter, e.g. Cnidoglanis macrocephalus and Apogon rueppellii.

Restructuring of Fish Assemblages in Swedish Lakes Following Amelioration of Acid Stress through Liming

A large‐scale liming program was initiated in Sweden in the mid‐1970s to ameliorate the effects of acidification and to restore acidified lakes and rivers to conditions present before acidification. I compared the fish fauna composition and biomass among limed, acidified, and consistently circumneutral lakes. The study focused on (1) recolonization and fish assemblage development and (2) fish biomass and assemblage composition. Time‐series data from 14 limed, 5 acid, and 10 circumneutral lakes, and a data set of 323 limed and 346 nonlimed circumneutral lakes, are analyzed. Long‐term monitoring revealed that fish species richness increased after liming and was of the same magnitude in limed lakes as in nonlimed circumneutral lakes after 10–20 years. Species proportions differed between limed and nonlimed lakes, and the relative biomass of Perca fluviatilis (Eurasian perch) was in general higher, whereas cyprinid and pelagic species were less important in the limed lakes than in the nonlimed circumneutral lakes. Recolonization of fish species was found to be a crucial factor for the development of the fish assemblages after liming, and in several limed lakes the reintroduction of fish species has accelerated the recovery of pre‐acidification fish assemblages.

The fish community of a high mountain stream in Taiwan and its relation to dam design

The fish community of a high mountain stream in Taiwan was studied from 1988 to 1990 in a 16 km section of Ta-chia river where a new dam is planned for construction. There were 16 species of fish belonging to 7 families; 15 genera were recorded. Six species are endemic to Taiwan. The dominant species wereZacco pachycephalus, Acrosscheileus paradoxus andRhinogobius brunneus. The composition of fish fauna was different between the eight study sites. Adjacent sites did not show a higher similarity than remote ones. AdultZ. pachycephalus andA. paradoxus showed seasonal aggregation behavior in the stream. At two distinct sites, Kukan and Tungmau, these two species had similar breeding and stock composition patterns with an intensified production period of juveniles from late autumn to early winter and a low, but continuous production period of juveniles in summer months. This information suggest that fishes in the river have special adaptations to the typhoon season in summer and benthic algal blooming in winter. The similarity of fish community and the independent breeding sites of endemic fishes in Kukan and Tungmau also suggest that these are important factors to consider for conservation when the flooding area of a high mountain dam is designed.

Changes in species composition of demersal fish fauna of Southeast Gulf of Carpentaria, Australia, after 20 years of fishing

The changes in a tropical demersal fish community in the southeast Gulf of Carpentaria, Australia, were examined by comparing the results of a survey undertaken in 1964 before the area was fished, with two surveys in 1985 and 1986 after 20 yr of commercial trawl fishing. The numerical abundance of 52 of the 82 fish taxa had not changed significantly, but that of 18 had decreased while 12 had increased. One taxon (Paramonacanthus spp.) had decreased by more than 500 times and another (Saurida micropectoralis) had increased substantially in abundance. The changes occurred throughout the area surveyed, but the largest changes were offshore. In the pre-trawling community most taxa were caught mainly during the night, while in the post-trawling community most were caught in the same numbers during day and night. In 10 of the 30 taxa that changed in abundance, changes were within a family and could not be explained. For the remaining 20, the changes could be related to their position in the water column: benthic taxa decreased and bentho-pelagic taxa increased. The changes were assessed in relation to fishing effort, and changes in the mud content of the substrate in the study area. Although the changes did not correlate with the fishing effort among three zones in the study area, it is suggested that fishing effort and discarding of the by-catch caused the change in 18 taxa. The magnitude of the decreases of some species might be related to changes in the sediment or possibly other long-term environmental change. There was also a change in the diel behaviour in the fish community that perhaps may be related to the effects of fishing on a tropical multispecies fish community.

Evolution of the Antarctic fish fauna with emphasis on the Recent notothenioids

Abstract The composition of the Antarctic fish fauna has undergone remarkable changes through time. Fossil fishes are known from Devonian, Jurassic, Cretaceous and early Tertiary deposits of the region. The Recent fauna does not appear to be derived from any part of any of the known fossil faunas. The Devonian fish fauna includes agnathans, placoderms, acanthodians, chondrichthyans and osteichthyans all belonging to families now extinct. The Jurassic fauna is known by only one species, a neopterygian of the now extinct family Archaeomaenidae. Both the Palaeozoic and early Mesozoic fish faunas known from Antarctica indicate Australian biogeographic affinities based on other ( i.e. , non-Antarctic) known Palaeozoic and Mesozoic fish faunas. Late Cretaceous and early Tertiary species from the Antarctic region (Seymour Island) belong largely to families of fishes that today live in other regions of the world, but are extinct in the Antarctic region. The Recent (extant) fish fauna is drastically different from any of the fossil faunas and is dominated by perciforms of the suborder Notothenioidei. To date the fossil record has provided no fossils identifiable as notothenioids, or even species closely related to the group. It is unlikely that low water temperatures were directly respnsible for the local extinction of the Tertiary Seymour Island ichthyofauna or for the lack of diversity in the Recent fauna. The decline of suitable substrate and trophic factors may have been more important in changing the composition of the fish fauna. There is considerable morphological, physiological and ecological diversification within the Notothenioidei. Although the emergence of this group was probably not a direct response to cooling, the subsequent radiation of notothenioids was associated with a variety of specializations related to low water temperature.