Paleobathymetric Zonation of the Middle–Upper Jurassic Deposits in the Ulyanovsk–Saratov Trough (Russian Platform) Based on Benthic Foraminifers

The environments, favorable for the development of benthic microfauna were predominant in the Jurassic Sea in the northeastern part of the Ulyanovsk–Saratov Trough (Russian Platform). Such parameters as the distribution and the taxonomic composition of the assemblage of Jurassic benthic foraminifers, their abundance, generic and species diversity, the occurrence of new species, a ratio of species with agglutinating and calcareous shells serve as a basis for developing the paleobathymetric zonation of the basin. The tracing of the variations in these parameters through the section enables us to construct a quantity paleobathymetric curve for the Middle-Late Jurassic and to distinguish the sequence–stratigraphic elements.     

Naked amoebae (Protozoa) of the Salton Sea, California

The Salton Sea is an inland lake in California with an average salinity of ca. 44 g l^–1. This productive water body, which supports substantial fish and migratory bird populations, is under threat because of increasing salinity levels. The present study was the first to examine the naked amoeboid protozoa of the Salton Sea and provide a first estimate of their numerical importance. Over a six-month sampling period (June–December, 1999), 45 different morphospecies (considered to be species) of amoebae were isolated. Wherever possible, isolates were identified to species or genus using diagnostic features recognizable by light microscopy. For each isolate, illustrations and brief notes on the diagnostic characters used in the identifications are given. These will allow this paper to be used as an identification guide to amoebae of the Salton Sea in future studies. Of the 45 taxa, around 18 of the isolates (i.e. 40%) are probably new to Science. Preliminary counts, based on enrichment cultivation methods, showed that amoebae in shoreline waters ranged from 14560 to 237120 cells l^–1 (mean 117312 ± 86075 S.D.). The ecological importance of high numbers and high diversity of amoebae is unknown. But it should be noted that several of the amoebae were actively grazing cyanobacterial and algal filaments and filaments of the bacterium Beggiatoa. Others were predominately associated with suspended particulates. As such, amoebae may be important in the cycling of carbon and nutrients in the Salton Sea.     

Hopper-crystal-growth, basis of test morphogenesis in Patellina corrugata Williamson (Foraminifera, Protozoa) (author's transl)

During the growth of Patellina corrugata's test platelike structures are formed showing typical characters of Hopper-crystals. These features indicate conditions of test development comparable to inorganic skeletal crystal growth. The whole test therefore can be regarded as a skeletal crystal (Hopper-crystal). Skeletal crystal growth is considered to be the basis of morphogenesis in the single-crystal test of Patellina.     

Impact of Polluted Bottom Deposits on the Species Structure and Abundance of Bivalves in Peter the Great Bay,Sea of Japan

Data from long-term (1979–1988) studies of bivalve fauna and of the content of priority pollutants in the bottom deposits of Peter the Great Bay have been analyzed. It was established that the biomass, population density, number of species, and the species diversity indexes of Shannon-Weiner and of the Pielou evenness of bivalves negatively correlated with the total pollution factor, TPF, of bottom sediments. Changes in the ecological parameters of bivalves with an increase in pollution occurred in spurts within the 3.4–3.6 interval of TPF values. The area of such values covered not only the coastal zone of Vladivostok, but also a considerable part of Amursky Bay.     

Deep-sea ecosystem variability of the Aegean Sea during the past 22 kyr as revealed by Benthic Foraminifera

Specific responses of the regional deep-sea ecosystems to climatic and oceanographic processes during the last 22 kyr are revealed by benthic foraminiferal faunas from two cores in the northern and southern Aegean Sea. Under glacial boundary conditions, high-diversity benthic foraminiferal faunas and elevated benthic foraminiferal numbers indicate enhanced organic matter availability and well-ventilated deep-water masses in the whole Aegean Sea. The glacial termination is accompanied by significant fluctuations in productivity and deep-water ventilation. In the northern Aegean Sea, meltwater inflow from mountain glaciers during the Bølling/Allerød warm period resulted in a restriction of local deep-water formation, as mirrored by a dominance of bolivinids. During the deposition of sapropel S1, drops in benthic foraminiferal number and diversity are more significant in the southern Aegean Sea when compared to the north. This suggests the persistence of local deep-water formation in the northern Aegean Sea during S1 deposition. In addition, faunal fluctuations within S1 at both sites suggest the repeated influence of short-term cooling events on the re-ventilation and re-colonization of Aegean deep-sea ecosystems. During the middle and late Holocene, benthic foraminiferal faunas document the establishment of oligotrophic and well-ventilated conditions in the southern Aegean Sea. The corresponding faunas from the northern Aegean Sea reflect generally mesotrophic conditions and variable deep-water oxygenation. During the entire Holocene, the deep-sea ecosystems of this region responded very sensitively to short-term changes in humidity and temperature. These abrupt climate changes controlled the inflow of nutrients from rivers and the Black Sea and the formation of local deep-water masses.     

Life Strategies of Vyrezub Rutilus frisii (Cyprinidae) in the Black Sea Basin

Journal of Ichthyology - The intraspecific structure and diversity of ecological forms of vyrezub Rutilus frisii are considered in different water bodies of the Black Sea basin in the Late Holocene...     

Species composition and distribution of foraminifers in the Deryugin Basin (Sea of Okhotsk)

Analysis of the composition and quantitative distribution of foraminifers in bathyal sediments collected at 14 stations in the Deryugin Basin and at 11 stations in other regions of the Sea of Okhotsk, Sea of Japan, and North Pacific demonstrated specific foraminifer complex in the basin at depths from 1650 to 1800 m associated with cold barite/methane seeps. Oligomixed biocenosis with prevailing agglutinated foraminifers and Saccorhiza ramosa as the dominant was shown to develop in these zones.     

Periphyton (Aufwuchs) Communities of Ciliated Protozoa in Salt-Polluted Running Waters of the Weser River Basin — Their Structure and Indicator Value (Including Model Ecosystems)

The ciliates in aufwuchs communities on glass slides exposed to different amounts of salt pollution at several locations in the Weser River system were investigated. The results were compared with those from the study of model ecosystems exposed to salts. A comparison of the ciliate occurrence with a number of physical and chemical parameters showed that it is primarily the amount of salt present that determines which species are dominant. The number of species present decreases in the presence of high salt concentrations and in water flowing at a high velocity. A halobic index was formulated to indicate salt pollution quantitatively but turned out not to be useful due to the euryhaline potency of most of the ciliate species. The saprobic index can be used in rivers polluted with salt only if biological indicator species are present in sufficient number.     

First Record of the Peritrich Trichodina diaptomiBasson and Van As, 1991 (Protozoa: Ciliophora) on a South American Calanoid Notodiaptomus deitersi (Poppe, 1890) (Crustacea: Copepoda)

ABSTRACT. The ciliate Trichodina was recorded on the calanoid Notodiaptomus deitersi in a shallow, eutrophic reservoir, located in the centre‐west of Brazil. The species was confirmed as Trichodina diaptomi, a species widely distributed in Europe, Africa, Asia and Australia. It was observed moving freely over the carapace of the copepod, and using its adhesive disc. This is the first record for the species in the Americas.     

Spatial Patterns in the Distribution,Diversity and Abundance of Benthic Foraminifera around Moorea (Society Archipelago,French Polynesia)

Coral reefs are now subject to global threats and influences from numerous anthropogenic sources. Foraminifera, a group of unicellular shelled organisms, are excellent indicators of water quality and reef health. Thus we studied a set of samples taken in 1992 to provide a foraminiferal baseline for future studies of environmental change. Our study provides the first island-wide analysis of shallow benthic foraminifera from around Moorea (Society Archipelago). We analyzed the composition, species richness, patterns of distribution and abundance of unstained foraminiferal assemblages from bays, fringing reefs, nearshore and back- and fore-reef environments. A total of 380 taxa of foraminifera were recorded, a number that almost doubles previous species counts. Spatial patterns of foraminiferal assemblages are characterized by numerical abundances of individual taxa, cluster groups and gradients of species richness, as documented by cluster, Fisher α, ternary plot and Principal Component Analyses (PCA). The inner bay inlets are dominated by stress-tolerant, mostly thin-shelled taxa of Bolivina, Bolivinella, Nonionoides, Elongobula, and Ammonia preferring low-oxygen and/or nutrient-rich habitats influenced by coastal factors such as fresh-water runoff and overhanging mangroves. The larger symbiont-bearing foraminifera (Borelis, Amphistegina, Heterostegina, Peneroplis) generally live in the oligotrophic, well-lit back- and fore-reef environments. Amphisteginids and peneroplids were among the few taxa found in the bay environments, probably due to their preferences for phytal substrates and tolerance to moderate levels of eutrophication. The fringing reef environments along the outer bay are characterized by Borelis schlumbergeri, Heterostegina depressa, Textularia spp. and various miliolids which represent a hotspot of diversity within the complex reef-lagoon system of Moorea. The high foraminiferal Fisher α and species richness diversity in outer bay fringing reefs is consistent with the disturbance-mosaic (microhabitat heterogeneity) hypothesis.Calculations of the FORAM Index (FI), a single metric index to assess reef vitality, indicate that all fore- and most back-reef environments support active carbonate accretion and provide habitat suitability for carbonate producers dependent on algal symbiosis. Lowest suitability values were recorded within the innermost bays, an area where natural and increasing anthropogenic influences continue to impact the reefs. The presence of habitat specific assemblages and numerical abundance values of individual taxa show that benthic foraminifera are excellent recorders of environmental perturbations and good indicators useful in modern and ancient ecological and environmental studies.     

Species of the Paramecium aurelia complex (Protozoa, Ciliophora) in the Middle Sudetes of Poland

Four species of the Paramecium aurelia complex were found in the studied territory (Klodzko Basin) of the Middle Sudetes in Poland, i.e. Paramecium primaurelia, P. biaurelia, P. tetraurelia and P. novaurelia . Of these, P. biaurelia and P. novaurelia appeared with greater frequency than P. primaurelia . Both species dominated over P. primaurelia in the number of determined habitats, as well as in the number of examined clones. Paramecium tetraurelia was rare in the area, being found in only one habitat.     

Expansion of the Range of the Black Sea Snail <Emphasis Type="Italic">Lithoglyphus naticoides</Emphasis> (C. Pfieffer, 1828) (Mollusca: Gastropoda: Lithoglyphidae) and Associated Trematode Species in the Upper Volga Basin

The Black Sea snail Lithoglyphus naticoides (C. Pfieffer, 1828) (Mollusca: Gastropoda: Lithoglyphidae) was first recorded in the Uglich Reservoir in the summer of 2013. By 2015, several new local settlements of the snail had been found in the Uglich and Rybinsk reservoirs, indicating its successful naturalization in the Upper Volga basin. Parasitological studies of L. naticoides from these habitats reveal the parthenitae of three trematode species.     

Benthic communities along a littoral of the Central Adriatic Sea (Italy)

Bacteria, meio- and macrofauna were investigated at different depths in a coastal area of the Central Adriatic Sea, yielding information about the composition and abundance of the benthic community. In particular, 14 nematode genera were recorded for the first time in the Upper Adriatic Sea. All communities resulted as being significantly different between inshore and offshore stations, especially when the season interaction was considered. Sediment grain size seemed to be the main natural variable, along with trophic resources, affecting the distribution and composition of these benthic components, whilst there was no clear evidence of competition for food sources and predatory pressure between the communities. Meiofauna appeared the most useful community for detecting disturbances and river influences. In particular, the lowest copepod abundance in the shallow waters seemed to be related to a greater anthropogenic disturbance inshore, whilst meiofaunal abundance and diversity together with the nematode maturity index suggest the influence of the Foglia and Metauro rivers and the small stream Arzilla.     

A New Species of Snailfishes (Liparidae) of the Genus Careproctus from the Northern Slope of the Aleutin Basin (Bering Sea)

Journal of Ichthyology - A new species of snailfishes Careproctus schmidti sp. nov. from the northwestern part of the Bering Sea is described. The specimen was caught in the mesobenthal of the...     

The Yellow Sea Cold Bottom Water--an oversummering site for Calanus sinicus (Copepoda, Crustacea)

The vertical distribution and stage-specific abundance of Calanussinicus were investigated on three key transects in the southernYellow Sea and the northern East China Sea in August 1999. Theresults showed that in summer C. sinicus shrank its distributionarea to the central cold (     

Microbial Communities in the Chemocline of a Hypersaline Deep-Sea Basin (Urania Basin, Mediterranean Sea)

The Urania basin is a hypersaline sulfidic brine lake at the bottom of the eastern Mediterranean Sea. Since this basin is located at a depth of ~3,500 m below the sea surface, it receives only a small amount of phytoplankton organic carbon. In the present study, the bacterial assemblages at the interface between the hypersaline brine and the overlaying seawater were investigated. The sulfide concentration increased from 0 to 10 mM within a vertical interval of 5 m across the interface. Within this chemocline, the total bacterial cell counts and the exoenzyme activities were elevated. Employing 11 cultivation methods, we isolated a total of 70 bacterial strains. The 16S ribosomal DNA sequences of 32 of the strains were identical to environmental sequences detected in the chemocline by culture-independent molecular methods. These strains were identified as flavobacteria, Alteromonas macleodii, and Halomonas aquamarina. All 70 strains could grow chemoorganoheterotrophically under oxic conditions. Sixty-six strains grew on peptone, casein hydrolysate, and yeast extract, whereas only 15 strains did not utilize polymeric carbohydrates. Twenty-one of the isolates could grow both chemoorganotrophically and chemolithotrophically. While the most probable numbers in most cases ranged between 0.006 and 4.3% of the total cell counts, an unsually high value of 54% was determined above the chemocline with media containing amino acids as the carbon and energy source. Our results indicate that culturable bacteria thriving at the oxic-anoxic interface of the Urania basin differ considerably from the chemolithoautotrophic bacteria typical of other chemocline habitats.     

Distribution of the Paramecium aurelia Species Complex (Protozoa,Ciliophora) in the Carpathian Chain of Poland*

Four species of the Paramecium aurelia complex were found in the Carpathian chain: P. primaurelia, P. biaurelia, P. tetraurelia and P. novaurelia. However, variation in the frequency of settlement of these species in the region was observed; P. biaurelia and P. novaurelia appeared with the greatest frequency, P. Primaurelia occurred less frequently. while P. tetraurelia was rather rare being found only in the Tatras.     

Growth dynamics of Zostera in Sevastopol Bay (Crimea,Black Sea)

Density, biomass and primary productivity of eelgrass (Zostera marina L.) and density and biomass of Zostera noltii Hornem. were studied at three locations in Sevastopol Bay, Crimean Peninsula, Ukraine, in April 2002, late September 2002, and late January 2003 at 3 m and 5 m depths. All three growth parameters varied by station, depth, and month. The aboveground biomass (AGB) was greater in September than in April or January at 3 m. It was greater at 5 m than at 3 m in April at one station. For Z. noltii, results were more variable as to month. For belowground biomass (BGB), month and station relationships were not clear cut. It was generally true that total biomass was greatest in September. Significant differences in density, AGB and total biomass were observed for station and month in eelgrass, while in BGB, these differences were significant for depth and for month. Primary production in eelgrass was greatest at both depths in April as compared to September or January. Reproductive shoots were found only during April. Overall, seedlings were found in all collection periods and depths, but were most abundant at the three stations in April.