Testate amoebae communities from aquatic habitats in the Arctic

Summary Forty taxa of testate amoebae were found in 15 aquatic samples collected in East Greenland (Angmasssalik Region), Jan Mayen and N.W. Spitsbergen. The number of species per sample is rather small, and the contribution of strictly aquatic species to the fauna is limited. A geographical shift in the importance of some genera can be demonstrated. Centropyxis aerophila and Paraquadrula irregularis are two of the most frequent species. The first-named is characteristic for acidoligotrophic waters, while the latter belongs to an alkaline-mesotrophic community. A third community is named after the commonest species, Trinema lineare. It seems to prefer a somewhat intermediate type of water.     

Testate amoebae and environmental features of polygon tundra in the Indigirka lowland (East Siberia)

Polygon tundra characterizes large areas of arctic lowlands. The micro-relief pattern within polygons offers differentiated habitats for testate amoeba (testacean) communities. The objective of this study was to relate testacean species distribution within a polygon to the environmental setting. Therefore, testaceans from four cryosol pits dug at different locations within a low-centered polygon were studied in the context of pedological and pedochemical data, while ground temperature and ground moisture were measured over one summer season. The study site is located on the Berelekh River floodplain (Indigirka lowland, East Siberia). The environmental data sets reflect variations along the rim-to-center transect of the polygon and in different horizons of each pit. The testacean species distribution is mainly controlled by the soil moisture regime and pH. Most of the identified testaceans are cosmopolitans; eight species are described from an arctic environment for the first time. Differences in environmental conditions are controlled by the micro-relief of polygon tundra and must be considered in arctic lowland testacean research because they bias species composition and any further (paleo-)ecological interpretation.     

Testate amoebae community structure in the moss biotopes of streams

The specific composition and community structure of testate amoebae in the moss biotopes of streams were studied in the Sura River basin (Middle Volga region). Twenty-nine species and forms were identified. The eurybiont species Trinema enchelys, Euglypha ciliata glabra, Centropyxis aerophila, Tracheleuglypha dentata, Crythion dubium, Centropyxis cassis, Trinema complanatum, and Trinema lineare are dominant. The species richness varies from 2 to 11 species per sample, the abundance is 100 to 4000 ind./g of absolutely dry moss. The degree of forest covering in the basin, hydrochemical peculiarities (the amount of biogenic elements and water hardness) of streams, the size of streams, and environmental contamination are possible factors that determine the specific character of the composition and structure of testate amoebae communities.     

Testate amoebae inhabiting middle taiga bogs in Western Siberia

The population of testate amoebae from the most typical middle taiga bogs of Western Siberia have been studied. More than one hundred (103) species and intraspecific taxons of testate amoebae have been revealed in recent surface samples. The relation between ecological characteristics of habitats and the composition of a Protozoa population has been demonstrated. The ecological preferences of species concerning the index of wetness, ash level, and acidity have been revealed. Using the correspondence analysis, the ecological optimums and the tolerance of species and intraspecific taxons of testate amoebae have been established.     

Testate amoebae populations from moss and lichen habitats in the Arctic

Summary Forty-five taxa of testate amoebae were found in 53 samples from mosses and lichens collected in East Greenland (Angmagssalik region), Jan Mayen and N.W. Spitsbergen. It is possible to distinguish four associations, with a different responses in relation to the moisture content, the hydrogen-ion concentration and the increasing continentality with latitude. A trend of diminishing diversity and number of taxa towards the north is also shown.     

Testate amoebae communities in the southern tundra and forest-tundra of Western Siberia

The species composition and community structure of soil-inhabiting testate amoebae communities have been studied in biotopes of different types in the southern tundra and forest-tundra of the Tazovskaya Lowland, Western Siberia. A total of 93 species and forms have been identified. It has been found that the species richness of testate amoebae is much lower in dry than in moist biotopes due to a lower level of beta-diversity, with alpha diversity being the same (on average, 16.9 and 17.1 species per sample, respectively). Factors acting at the microbiotope level (biotope type and moisture) play the most important role in the formation of species richness; biotope features (soils and vegetation) are second in importance. In moist habitats, local communities of testate amoebae from different microbiotopes (mosses, lichens, or litter) are fairly similar in species structure, and communities from different moist biotopes are heterogeneous. In dry areas, the opposite situation is observed: local communities differ at the microbiotope level but are similar at the biotope level. The abundance of testate amoebae in moist biotopes reaches 200 × 10³ ind./g dry soil, being an order of magnitude lower in dry biotopes.     

Testate amoebae community pattern in different types of boundary structures at the water-land contact zone

The patterns of changes in the species richness, abundance, species composition, and species structure of the testate amoebae community along six different types of water-land boundaries in the Medveditsa River (Don river Basin) were studied, namely, a new boundary, terrigenous and reogeneous edges, reogeneous and terrigenous hemiecotones, and the full ecotone. The testate amoebae communities are divided into terrestrial and aquatic variants for all types of boundaries. Hydrophilic species of the genera Arcella, Diffugia, Cyphoderia, and Pseudodifflugia dominate in the aquatic types of communities while pedobiont and eurybiont groups from the genera Centropyxis, Euglypha, Plagiopyxis, and Trinema are characteristic of the terrestrial communities. A decrease in the abundance and species richness of testate amoebae in the boundary zones was detected.     

Testate amoebae and nutrient cycling: peering into the black box of soil ecology

In some areas of ecology and evolution, such as the behavioural ecology of many well-studied bird species, it is increasingly difficult to make surprising new discoveries. However, this is not the case in many areas of soil and/or microbial ecology. Two recent studies suggest that the testate amoebae, a microbial group unfamiliar to most biologists, might play a much larger role in soil nutrient cycling than has hitherto been suspected.     

Zygnemataceae in quaternary Columbian sediments

Spores of Zygnemataceae are described from Lower Pleistocene, Upper Pleistocene and Holocene sediments from the Colombian Andes. About ten types could be distinguished, most of them referable to the genera Mougeotia, Spirogyra and Debarya. In addition records of Bulbochaete (Oedogoniaceae) and of Closterium (Desmidiaceae) are reported.Spores of Zygnemataceae appear to be of considerable importance for palaeoecological studies. Debarya aff. D. glyptosperma and several other types were up to now found only in deposits associated with a cold to cool high-mountain climate.     

Testate amoebae community analysis as a tool to assess biological impacts of peatland use

As most ecosystems, peatlands have been heavily exploited for different human purposes. For example, in Finland the majority is under forestry, agriculture or peat mining use. Peatlands play an important role in carbon storage, water cycle, and are a unique habitat for rare organisms. Such properties highlight their environmental importance and the need for their restoration. To monitor the success of peatland restoration sensitive indicators are needed. Here we test whether testate amoebae can be used as a reliable bioindicator for assessing peatland condition. To qualify as reliable indicators, responses in testate amoebae community structure to ecological changes must be stronger than random spatial and temporal variation. In this study, we simultaneously assessed differences between the effects of seasonality, intermediate scale spatial variation and land uses on living testate amoebae assemblages in natural, forested and restored peatlands. We expected the effects of seasonality on testate amoebae communities to be less pronounced than those of land use and within site variation. On average, natural sites harboured the highest richness and density, while the lowest numbers were found at forestry sites. Despite small changes observed in taxa dominance and differences in TA community structure between seasons and years at some sites, spatial heterogeneity, temperature, pH, nor water table depth seemed to significantly affect testate amoebae communities. Instead, observed differences were related to type of land use, which explained 75% of the community variation. Our results showed that testate amoebae community monitoring is a useful tool to evaluate impacts of human land use on boreal peatlands.     

Testate amoebae analysis in ecological and paleoecological studies of wetlands: past, present and future

Testate amoebae are an abundant and diverse polyphyletic group of shelled protozoa living in aquatic to moist habitats ranging from estuaries to lakes, rivers, wetlands, soils, litter, and moss habitats. Owing to the preservation of shells in sediments, testate amoebae are useful proxy indicators complementary to long-established indicators such as pollen and spores or macrofossils. Their primary use to date has been for inferring past moisture conditions and climate in ombrotrophic peatlands and, to a lesser extent, to infer pH in peatlands and the trophic or nutrient status of lakes. Recent research on these organisms suggests other possible uses in paleoecology and ecology such as sea-level reconstruction in estuarine environments, as indicators of soil or air pollution, and monitoring recovery of peatland. We review the past and present use of testate amoebae, the challenges in current research, and provide some ideas on future research directions.     

The climate-related diachronous disappearance of Pulleniatina obliquiloculata in late quaternary sediments of the Atlantic and Caribbean

The planktonic foraminifera Pulleniatina obliquiloculata (Parker and Jones) undergoes several climatically controlled disappearances and reappearances in the equatorial Atlantic and Caribbean sediments during Late Quaternary time. One such disappearance occurs near the middle of the last glacial (Middle Wisconsin, middle Y zone, O¹⁶ stage 3). The age of this disappearances is time transgressive from approximately 60, 000 yr in the Gulf of Mexico, to 50, 000 yr in the western Caribbean, to 35, 000 yr in the equatorial Atlantic. The time-transgressive transgressive nature of P. obliquiloculata's disappearance from the Atlantic is thought to represent the decreasing “width” of P. obliquiloculata's adaptive zone as surface water salinities progressively increased during the glacial intervals due to expanding continental glaciers. A simple ecologic model predicts that P. obliquiloculata should disappear first from areas of high salinity and is consistent with observations that both modern sea-surface salinity and the age of the P. obliquiloculata biohorizon increase from the equatorial Atlantic to the Gulf of Mexico.The biohorizon, Y_{P. obliq}, is a subdivision of Ericson's Y zone and occurs throughout the western equatorial Atlantic as well as throughout most of the Caribbean and Gulf of Mexico. Here, the horizon is useful for correlating and determining accumulation rates in continental margin sediments where rapid deposition often prevents piston cores from penetrating through the last glacial interval. Along the coast of Africa, in areas of coastal upwelling and the equatorward transport of cold water, the biohorizon does not occur.     

On the fauna of Scathophagidae (Diptera) of Yakutia

The fauna of the family Scathophagidae of Yakutia, including 44 species of 15 genera, was studied. 23 species are recorded from the territory for the first time. The Arctic and subarctic zones of Yakutia have been still poorly studied, and additional species are found there. The scathophagid fauna of Yakutia was compared with the faunas of the neighboring regions using the dendrogram similarity method based on calculation of the Czekanowski–Sørensen coefficient.     

Clay minerals in Cenozoic sediments off Cape Roberts (McMurdo Sound, Antarctica) reveal palaeoclimatic history

The clay mineral assemblages of the ca. 1600 m thick Cenozoic sedimentary succession recovered at the CRP-1, CRP-2/2A and CRP-3 drill sites off Cape Roberts on the McMurdo Sound shelf, Antarctica, were analysed in order to reconstruct the palaeoclimate and the glacial history of this part of Antarctica. The sequence can be subdivided into seven clay mineral units that reflect the transition from humid to subpolar and polar conditions. Unit I (35-33.6 Ma) is characterised by an almost monomineralic assemblage consisting of well crystalline, authigenic smectite, and therefore does not allow a palaeoclimatic reconstruction. Unit II (33.6-33.1 Ma) has also a monomineralic clay mineral composition. However, the assemblage consists of variably crystallized smectite that, at least in part, is of detrital origin and indicates chemical weathering under a humid climate. The main source area for the clays was in the Transantarctic Mountains. Minor amounts of illite and chlorite appear for the first time in Unit III (33.1-31 Ma) and suggest subordinate physical weathering. The sediments of Unit IV (31-30.5 Ma) have strongly variable smectite and illite concentrations indicating an alternation of chemical weathering periods and physical weathering periods. Unit V (30.5-24.2 Ma) shows a further shift towards physical weathering. Unit VI (24.2-18.5 Ma) indicates strong physical weathering under a cold climate with persistent and intense illite formation. Unit VII (18.5 Ma to present) documents an additional input of smectite derived from the McMurdo Volcanic Group in the south.     

Terrestrial bugs (Heteroptera) in high mountains of the Suntar-Khayata Range (Eastern Yakutia)

Thirty-nine species of bugs, representing meso-and xerophilic inhabitants of open tundra, meadow, and steppe landscapes, were collected within the altitude range of 1260–1850 m above sea level in the upper Kyubyume River basin (63°13′N, 139°36′E, the Indigirka River basin). In the sub-golets sparse forest zone (up to 1550 m), 37 species were recorded, the dominant form being Chlamydatus pullus. The bugs were rare in most of the habitats; their species richness and abundance increased distinctly only on the south-facing slopes, reaching the maximum in the cryophytic steppe. The specific features of these complexes manifested themselves in the prevalence of Capnoda nigroaenea, a xerophilic species of alpine mountain steppes. The rest of the dominants comprised the ecologically flexible Emblethis brachynotus, Chlamydatus pullus, and Galeatus spinifrons. In the goletstundra zone, 8 species were found, half of them being arctic forms (Calacanthia trybomi, Orthotylus artemisiae, Ch. wilkinsoni, and Ch. opacus). Ch. wilkinsoni was the most common species. The species composition of bug groups in the dry lichen-dryad communities within this zone resembled that of similar communities of zonal tundra, whereas the humid habitats remained unpopulated, unlike their plain analogues. Comparison of the heteropteran fauna of mountain tundras in different regions of the Verkhoyansk-Kolyma mountain country attests to significant variations of its species composition. The possible reasons for these differences are discussed.     

Marking Activities of the Moose (Alces alces) in Central Yakutia

Biology Bulletin - Abstract—The marking behavior and mediated communication of male moose in central Yakutia are studied. During rut, moose damage tree and shrub vegetation with their antlers...     

Grassflies (Diptera, Chloropidae) in the middle Lena valley (Central Yakutia)

Sixty-one species of grassflies (Diptera, Chloropidae) have been found in the meadows in the middle Lena valley, Central Yakutia. Differences between the grassfly taxocenoses of different parts of the valley depend on specific features of a particular plant community. The dominant and subdominant chloropid species are distinguished. The differences of the riparian fauna from the complexes inhabiting the alases in Yakutia are shown. Six species of grassflies are recorded for Yakutia for the first time, all of them belonging to the subfamily Oscinellinae: Polyodaspis ruficornis Macquart, Tricimba cincta Meigen, Aphanotrigonum trilineatum Meigen, Trachysiphonella scutellata v. Roser, Rhopalopterum anthracinum Meigen, and Rh. fasciolum Meigen     

The occurrence and fission-track ages of late neogene and quaternary volcanic sediments,Siwalik group,Northern Pakistan

Volcanic sediments, now mostly bentonites and bentonitic mudstones, occur throughout the Late Neogene and Quaternary Siwalik Group of northern Pakistan. A number of these deposits have been dated by the fission-track method, utilizing zircon phenocrysts from these deposits, and provide the chronometric constraints upon which a paleomagnetic stratigraphy is developed for the Siwalik Group. Notable in the occurrence of these altered tuff horizons is an apparent mode in their stratigraphic development from approximately 3.0 to 1.5 m.y. B.P. which coincides with the period of activity of the Dacht-e-Nawar volcanic complex of east-central Afghanistan. Fission-track ages of certain tuffs for critical areas of northern Pakistan are reported herein.