Bottom Communities of Semyachik Lagoon (Kronotskii Biosphere Reserve, Eastern Kamchatka)

Bottom communities of Potamogeton filiformis,Zostera marina+ Z. japonica+ Macoma balthica, Enteromorpha prolifera, and a stony block–boulder intertidal community were distinguished in Semyachik Lagoon. The macrobenthos associated with these communities is described. Generally, the biomass and occurrence frequency indices of the macrozoobenthic communities of the lagoon are an order of magnitude lower than those of macrophytobenthic communities (Kafanov, Plekhov, 1998); therefore, they do not play a significant role in bottom community structure. With the exception of the stony block–boulder intertidal community, their spatial distribution is entirely determined by the distribution of underwater vegetation, which is completely controlled by the geomorphological and hydrological features of the lagoon.     

Seasonal Dynamics of Soft Bottom Macrobenthic Communities of the Sublittoral in Peter the Great Bay, Sea of Japan

Seasonal dynamics of macrobenthos were studied at five stations located at depths of 10–60 min in the Far East State Marine Reserve (southern Peter the Great Bay) during 1984–1987. Sampling was conducted at stations once per season. Stable seasonal fluctuations of the population density and the biomass in basic taxonomic groups were found. As a rule, the quantitative parameters were augmented in spring and summer, and decreased in fall and winter. This was caused, first of all, by summer fluctuations of the number of small and short-lived species of polychaetes and bivalve molluscs. The amplitude of fluctuations decreased with increasing depth. Variation in the quantitative parameters was significant at the community level only at the most shallow-water stations. It was assumed that this phenomenon might be caused by the seasonal consumption of macrobenthos by bottom fish and by the periodicity of detritus supply to the bottom from the water column with a background of varying environmental temperature parameters and of mass settling of benthic larvae. The seasonal changes in parameters began and ceased earlier in 1986–1987 than 1984–1985, which was related to an appreciable decrease in water temperature in 1986. During the period of study, an increasing trend of parameters, apparently part of a long-term cycle, was recorded both for individual groups and for entire communities, and was the most appreciable at greater depths (47–60 m).     

On the Morphology of Arrowhead Flounders of the Genus Atheresthes in the Pacific Waters of the Northern Kuril Islands and Southeastern Kamchatka

This paper presents the results of studies on the morphology of arrowhead flounders, the Kamchatka flounder Atheresthes evermanni (35 specimens), and the American arrowtooth flounder A. stomias (37 specimens) collected in Pacific waters of the northern Kuril Islands and southeastern Kamchatka in 1998–1999. The morphology of the discussed species is compared with that of arrowtooth flounders from other areas. From this comparison, available information on the sharp increase in the density of the American arrowtooth flounder in the surveyed area (since 1997), and similarities in size compositions of the fish in Kuril and Aleutian waters, a conclusion has been made about the penetration of this species from Aleutian Pacific waters into the area of the northern Kuril Islands and southeastern Kamchatka. This is a result of expansion of the geographical range of this species due to general water warming in the northwestern Pacific during the second half of the 1990s.     

Microbial Silicification in Sinters from Two Terrestrial Hot Springs in the Uzon Caldera,Kamchatka, Russia

Silicification of microbial communities is the most pervasive form of mineralization in two terrestrial hot springs in the Uzon Caldera. X-ray diffraction and electron microscopy reveal a diverse sinter mineral assemblage dominated by opal-A with accessory sulfur, sulfides, alunite group minerals, oxides, and oxyhydroxides. Aluminum laminations (reported for the first time) noted in one deposit may slow opal-A transformational rates enabling mineralized microbial remnants to exist longer in the rock record. Although preservation of microbial forms decreases over time, the collective mineral assemblage and patterning suggests that they are the most persistent lines of evidence of life in the geologic record.     

Estimating the Abundance of Bottom Fish at the Shelf and Continental Slope in Northern Primorye

Journal of Ichthyology - Based on materials from bottom trawl surveys of 2009–2015, biomass and abundance of bottom fish of the Sea of ​​Japan between the Povorotny and Zolotoy...     

Fossil wood of Keteleerioxylon kamtschatkiense sp. nov. (Pinaceae) from the Cretaceous of the northwestern Kamchatka Peninsula

A new species, Keteleerioxylon kamtschatkiense, is described from the Cretaceous of the northwestern Kamchatka Peninsula on the basis of wood anatomy. Fossil wood showing anatomical characters of the modern genus Keteleeria is described from the Cretaceous of the Russian Far East for the first time.     

Habitat Use of Fish Communities in A Virginia Stream System

Fish habitat use during summer was examined at micro- and meso-levels, to determine species associations in the upper Roanoke River watershed, Virginia. Based on multivariate-mesohabitat analysis and examination of mean microhabitat use, seven habitat-use guilds were apparent. These included four rheophilic (fast-riffle, riffle/run, fast-generalist, and shallow-rheophilic) and three limnophilic guilds (pool/run, open-pool, and pool-cover) that were reasonably robust across two river segments and two years. Although simple-hydraulic, bottom-topographic, and turbulence variables all segregated fish habitat-use guilds, turbulence variables were redundant with simple-hydraulic variables, substratum use by limnophilic fishes was related to availability, and only one guild consistently selected high cover levels. At the family level, suckers, darters, and especially minnows were notable for occupying several habitat-use guilds, because of species differences in habitat preferences. Such formulation of guilds can simplify habitat-impact analyses in biodiverse, warmwater streams, via focus on habitat needs of guilds rather than on individual species.     

Fish Communities of the Lower Fraser River (Canada) and a 21-year Contrast

Fish communities were sampled at 14 sites along the lower 120km of the Fraser River, British Columbia by beach seine four times in 1972–1973 and three times in 1993–1994. Of the 37 species collected, peamouth chub, largescale sucker, starry flounder, and northern squawfish were predominant in either density or biomass. Densities and biomass of most species and all fish combined were higher in 1993–1994. Strong rank correlations of species abundance or biomass indicated that the overall fish community structure was very similar in both periods. At smaller spatial scales (reaches of 2–3 sites) and shorter time scales (by season), less than half the comparisons showed any significant correlation indicating changes in community composition. Largescale sucker, one of the largest contributors to biomass in both periods, showed decreased abundance, i.e., lower density, lower biomass, and large differences in the size-frequency distribution, specifically very low representation of small size classes. Other species, especially small-bodied forms, generally increased in numbers. Despite large changes in the lower Fraser River ecosystem in the past 21 years, the overall fish community has shown remarkably little change over that interval.     

Activity of bacteria in water of hot springs from Southern and Central Kamchatskaya geothermal provinces, Kamchatka Peninsula, Russia

The hot-spring waters of numerous hot springs at the Kamchatka Peninsula, Russia differ in their chemical characteristics and elemental composition. Total bacterial abundance (TBA) as well as enzymatically active and respiring bacteria was enumerated in water samples collected from the Nalychevskie, Oksinskie, Apapelskie, and Dachnye hot springs. 5-Carboxyfluorescein diacetate activity was detected in all water samples and comprised 29-65% of the TBA as determined by 4',6-diamidino-2-phenylindol staining. The respiratory activity of iron-oxidizing bacteria was assayed by 5-cyano-2,3-ditolyltetrazolium chloride reduction. Respiring cells accounted for 9-14% of the TBA, indicating a positive correlation with the number of iron-oxidizing bacteria from the hot-spring biomats. Enumeration of heterotrophic bacteria revealed a high-density bacterial population only in the water of the Apapelskie hot spring, which has a temperature of 36 degrees C. Therefore, it appears that heterotrophic and iron-oxidizing bacteria inhabiting the hot-spring waters are essential for the geochemical processes occurring in hydrothermal systems.     

A Large-scale Comparative Analysis of Riffle and Pool Fish Communities in an Upland Stream System

Fishes were sampled in riffle and pool habitats at 74 upland localities in the Little River system, southeastern Oklahoma and southwestern Arkansas, U.S.A. I asked how these two habitat-defined communities differed with regard to species abundance and incidence patterns, and how these differences varied along othree environmental gradients: elevation, stream gradient, and stream size. Riffle and pool communities showed distinct and significant differences when ordinated in multivariate space defined by species abundance patterns. Sites with similar pool communities did not have similar riffle communities, and riffle and pool communities responded to environmental gradients in different ways. Elevation was the best predictor of pool community structure, whereas stream size was the best predictor of riffle communities. Overall, riffle habitats had fewer species than pool habitats and formed significant subsets of pool communities at 12 of 74 sites. I predicted that at small stream localities where riffles were unstable, riffle species would form subsets of the pool species communities, and both community types should show high similarities. The presence of faunal subsets was not associated with stream size, but faunal similarities were significantly higher at small stream localities. At the species level, 14 species were significantly associated with pool habitats, while only two were associated with riffle habitats. Riffle and pool communities, although linked by a continuous habitat gradient at the local scale, responded differently to large-scale environmental gradients. Local differences between these communities were predictable based on stream size.     

Structure of Littoral-zone Fish Communities in Relation to Habitat, Physical, and Chemical Gradients in a Southern Reservoir

How the distribution and abundance of organisms vary across environmental gradients can reveal factors important in structuring aquatic communities. We sampled the littoral-zone fish community in a large reservoir (Lake Texoma) on the Texas–Oklahoma (U.S.A.) border that has pronounced environmental gradients from up- to downlake and between major tributary arms. Our objective was to evaluate the predictability of the littoral-zone fish-community structure from a suite of environmental variables. A stepwise multiple-regression model, with environmental factors at independent variables, explained 64% of the variation in fish species richness across sample sites. The number of species was positively associated with water-column productivity and total Kjedahl nitrogen, and negatively associated with Secchi depth and benthic productivity. Canonical correspondence analysis, with environmental factors as independent variables, explained 63% of the variation in fish-community structure across sites. Equal proportions of the variation in community structure were explained by variables that have strong gradients within the reservoir (e.g., Secchi depth and water-column productivity) and those that represent local habitat variables (e.g., shoreline aspect and substrate type).     

Feeding of the Snailfish Careproctus roseofuscus in Pacific Waters of the Northern Kuril Islands and Southeastern Kamchatka

The paper describes the feeding of two phenotypically different forms of the snailfish Careproctus roseofuscus (Scorpaeniformes, Liparidae) from the Pacific waters of the northern Kuril Islands and southeastern Kamchatka. The diet in the first form is comprised of actiniae. The second form mostly feeds on fish eggs and the amphipod Metopa majuscula Gurjanova. The second form is supposed to be confined to the biocenosis of Ophiopholis aculeata + Spongia.     

The status of the West African fish Gobius nigricinctus with reference to New World autochthones and an Old World colour-analogue

The systematic features of a small West African marine gobiid fish, Gobius nigricinctus Delais 1951, are redescribed from the holotype with special emphasis on the head lateral-line canal and sensory papillae (tree neuromast) systems. A junior synonym is found to be Gobius lepidogenys Robins 1970. The status of G. nigricinctus is best expressed in a new monotypic genus, Gorogobius , with closest affinity to the Atlantic-Mediterranean Corcyrogobius and Odondebuenia , Similarities in head sensory papillae arrangement exist between Gorogobius and certain 'seven-spined' genera of the New World tropical insular fauna, but G. nigricinctus is shown not to be a recent transatlantic immigrant. The validity of the tribe Gobiosomini as a natural grouping endemic to the Americas is questioned. Close resemblance in striped coloration between Gorogobius and small Indo-West Pacific gobies, especially Quisquilius eugenius , is shown to be the result of convergent evolution.     

Coastal States in the South China Sea and Submissions on the Outer Limits of the Continental Shelf

The purpose of this article is to examine the outer continental shelf submissions made by the coastal states of the South China Sea and their potential impact on legal and political developments in the South China Sea. In accordance with the United Nations Convention on the Law of the Sea of 1982 and the guidelines of the Commission on the Limits of the Continental Shelf, coastal states are to establish the outer limits of their continental shelf where it extends beyond 200 nautical miles. Meeting this obligation is complicated in enclosed or semienclosed seas where there are maritime disputes such as in the South China Sea.     

A review of the chronostratigraphical ages of Middle Triassic to Late Jurassic dinoflagellate cyst biozones of the North West Shelf of Australia

The chronostratigraphical ages of the 20 dinoflagellate cyst zones and one dinoflagellate cyst assemblage for the Middle Triassic (Ladinian) to the Jurassic-Cretaceous transition of the North West Shelf of Australia are comprehensively reviewed. Evidence from macro- and micropalaeontology, palynology and strontium isotopes made available after the establishment of these biozones in the 1980s has been used to reassess the ages of this important zonal scheme and to calibrate it to the international stratigraphical stages. The Shublikodinium Superzone is renamed herein as the Rhaetogonyaulax Superzone, and based on conodont evidence is determined to span the Ladinian to Early Sinemurian. This is significantly shorter in duration than was originally envisaged (Late Anisian to Late Pliensbachian). The Luehndea Assemblage is a low diversity dinoflagellate cyst association which marks a eustatic rise; it is subdivided into two subzones. It is of latest Pliensbachian to Early Toarcian age, based largely on palynological evidence. The Bajocian to earliest Oxfordian Pareodinia ceratophora Superzone represents the inception of a continuous Mesozoic-Cenozoic dinoflagellate cyst record in Australia. It comprises seven zones, which are considered to be slightly older than originally interpreted. The overlying Pyxidiella Superzone is characterised by diverse dinoflagellate cyst associations. It is Early Oxfordian to Kimmeridgian in age, and comprises three zones. The bases of the Wanaea spectabilis and Wanaea clathrata zones are reinterpreted as being slightly older than originally proposed. The superjacent Fromea cylindrica Superzone is Tithonian to earliest Valanginian and modified ages are indicated for four of the nine zones. This unit is dominated by endemic dinoflagellate cysts, reflecting a global trend towards provincialism at this time due to a regressive eustatic regime.     

Feeding habits the Pacific cod <Emphasis Type="Italic">Gadus macrocephalus</Emphasis> in oceanic waters of the Northern Kuril Islands and Southeast Kamchatka

This study examines the feeding habits of the Pacific cod Gadus macrocephalus in waters off the eastern coast of the northern Kuril Islands and southern Kamchatka. In November–December 1996, the cod primarily consumed fish, which made up 47.6% of the total food mass. The proportion of cephalopods, fishery offal discarded from fishing vessels, and decapods did not exceed 18.5, 17.4, and 12.2%, respectively. Among fishes, the main prey item of the cod was atka mackerel (15.4%); among cephalopods, octopus (16.8%); among fishery offal, heads of atka mackerel (14.2%); and among decapods, majid crabs (6.4%). The rather low percentage of walleye pollock (7.3%) in the cod diet was due to the decline of the east-Kamchatka walleye pollock stock.     

Aerobic Methanotrophic Communities in the Bottom Sediments of Lake Baikal

The results of the first systematical investigation into the aerobic methanotrophic communities inhabiting the bottom sediments of Lake Baikal have been reported. Use of the radioisotopic method revealed methane consumption in 12 10- to 50-cm-long sediment cores. The maximum methane consumption rates (495–737 µl/(dm³ day) were recorded in sediments in the regions of hydrothermal vents and oil and gas occurrence. Methane consumption was most active in the surface layers of the sediments (0–4 cm); it decreased with the sediment depth and became negligible or absent at depths below 20 cm. The number of methanotrophic bacteria usually ranged from 100 to 1000 cells/cm³ of sediment and reached 1 million cells/cm³ in the regions of oil and gas occurrence. The seventeen enrichment cultures obtained were represented mainly by morphotype II methanotrophs. Phylogenetic analysis of the enrichment cultures in terms of the amino acid sequence of the α subunit of the membrane-bound methane monooxygenase (MMO) revealed the predominance of methanotrophs of the genus Methylocystis. The results obtained suggest the presence of an active aerobic methanotrophic community in Lake Baikal.__________Translated from Mikrobiologiya, Vol. 74, No. 4, 2005, pp. 562–571.Original Russian Text Copyright © 2005 by Gainutdinova, Eshinimaev, Tsyrenzhapova, Dagurova, Suzina, Khmelenina, Namsaraev, Trotsenko.     

On the Vertical Distribution of the Metazoan Meiofauna in Shelf Break and Upper Slope Habitats of the NE Atlantic

The metazoan meiofauna of nine stations in shelf break and upper slope areas (70 to 1500 m water depth) of the N.E. Atlantic were investigated in order to assess which environmental factors are important in the control of densities and sediment profiles. Total meiofaunal densities (ranging between 368 and 1523 ind/10 cm²) were correlated with bacterial densities, an important food source for meiofauna. However, considering sediment vertical distribution profiles, the relative importance of both food and oxygen on the meiofauna became obvious. A combination of both bacterial densities and oxygen supply could explain about 95% of the variability in the vertical profiles of the meiofauna densities. Meiofauna numbers increase in proportion to food availability in the surface sediment layers, but this relationship breaks down in deeper sediment layers where the oxygen supply is often limiting, particularly in fine sediments.     

Convergence of Differentially Invaded Systems toward Invader-dominance: Time-lagged Invasions as a Predictor in Desert Fish Communities

To what extent do patterns of invasion in one region generalize to other regions? Answering this question is a key goal of invasion biology because it underlies whether we can make progress via comparative studies or must instead cope with a large set of unique cases. Here we quantify similarities and differences in the historical development of nonnative fish assemblages of two North American desert drainages, one with many nonnative fishes (Gila Basin, principally southwestern USA), and one with few (Yaqui Basin, principally northwestern Mexico). The two river basins are similar in size, physiography, and ecology, but because of differences in the timing of regional development, we hypothesized that richness and geographic spread of nonnative fishes in the Yaqui are time-lagged relative to the Gila, and that a slow, but steady increase of nonnative fish occurrence is underway in the Yaqui, similar to what has already occurred in the Gila. Using the comprehensive SONFISHES database, we found that increases in the regional richness of extant nonnative species over time have been roughly linear in both basins. Meanwhile, previously established species have continued to spread spatially, such that the cumulative number of reach records for nonnative species has increased roughly exponentially in both systems. The current status of nonnatives in the Yaqui is remarkably similar to what was evident from the Gila in the past at a comparable level of sampling effort. For all measures of invasion dynamics we examined, a time lag of ～ 40–50 years exists between the Gila and Yaqui. The majority of extant nonnative fishes are known piscivores, and many have high levels of parental care, a life history trait that affords considerable advantages over native fishes. These results predict that, absent strong action now, the presently abundant native fish fauna of the Yaqui may become increasingly imperiled over the next several years, with a future similar to the Gila, where most native fishes are either extirpated, threatened, or substantially reduced in range, at least partially due to nonnative fishes. We recommend immediate actions to identify and protect high priority portions of the Yaqui Basin from further nonnative fish invasion before further degradation occurs.     

吉林西部野生罗布麻生长季内土壤水盐变化趋势的研究

对吉林西部野生罗布麻分布区0~50 cm深度的土壤水盐变化趋势进行了研究,结果发现:土壤水分在水平格局的3个区有所不同,密集区和边缘区土壤水份含量和变化趋势相近,空白区土壤水份高于前两个区,垂直格局中,水份波动幅度随深度的增加而递减;土壤全盐量在水平格局的3个区含量不同,密集区边缘区空白区,在垂直格局中,密集区随深度增加,全盐量的波幅递减,边缘区和空白区是20~30 cm层含量高、波幅大,其它二层含量低波幅小;水平格局3个区的pH值是:密集区边缘区空白区,垂直格局中,密集和边缘两个区的20~30 cm层pH值高于其他两层,空白区pH值随深度增加呈递减趋势。正常生长的罗布麻土壤水份含量在9%~20%之间;全盐量在0.05%~0.25%之间;pH值在7.8~9.4之间。当生长季内大部分时间水份低于5%或高于21%、全盐量在0.35%以上、pH值高于9.8时,罗布麻不能生长。罗布麻根系发达,能贮存较多水分以应对干旱环境。该植物适于栽培在垄高为20~30 cm的环境中。苗期能耐受较高的全盐量和pH值,是一种适合于干旱盐碱环境的经济植物。