Bacterial populations as components of oceanic ecosystems

The production of bacterioplankton in tropical waters is shown to be a major food source for filter feeders. Since this production greatly exceeds autotrophic production by phytoplankton, the external energy source is believed to be soluble organic material transported from temperate latitudes. In the latter environment this material is produced as part of excessive autotrophic production, but its destruction by bacteria is inhibited at low temperature. The organic material is transported by global circulation to warm tropical waters, where it is utilized to form particulate organic aggregates which serve as food for filter feeders.     

Data on biological productivity of the Western tropical Pacific Ocean

Vertical distribution and production of phytoplankton and planktonic bacteria were studied in the pelagic and neritic regions of the Western tropical Pacific Ocean and in temperate waters of the Japan Sea. The stable, layering structure of the community and its daily fluctuations caused by grazing are described. Data on the integral daily production of communities under 1 m² are presented. The data obtained are discussed with respect to the trophical relations in planktonic communities of the stratified sea basins.     

The heterotrophic phase of plankton succession in the Japan Sea

The vertical structure, composition and productivity of a plankton community was studied in the Japan Sea in June, 1972 during a period of thermocline formation; the parameters measured were: phytoplankton production and biomass; number, biomass, and production of planktonic bacteria; biomass of phagotrophic flagellates, ciliates and remaining microzooplankton. The concentration of micro- and mesozooplankton attained a basic maximum in a layer near the upper part of the thermocline. The biomass and calculated production of the heterotrophic part of the community exceeded considerably the amount of primary production. The heterotrophic phase of the seasonal succession of a plankton community in a temperate sea is described, when heterotrophic metabolism and production predominate. Heterotrophs at this stage use mostly energy from organic matter accumulated during the previous spring phytoplankton bloom.     

Analysis of experiments on ion-induced nucleation and aerosol formation in the presence of UV light and ionizing radiation

Under typical atmospheric conditions, sulfuric acid and water vapors are likely most important species in the nucleation of new aerosol particles. The main source of H₂SO₄ in the atmosphere is oxidation of SO₂. Hence, an understanding of the subsequent chemical reactions followed by aerosol-particles formation is of fundamental importance. Here we analyze the results of laboratory experiments in Svensmark et al. (2007) in which (i) the formation of neutral aerosol particles was observed at reported sulfuric acid concentrations well below the range where the binary homogeneous nucleation in a mixture of H₂SO₄–H₂O vapors could be important and (ii) an electron catalytic effect on particle nucleation was suggested as an explanation of the experimental results and as a potential source of aerosol-particles formation in the Earth's atmosphere. In the article we give an interpretation of these experimental data based on a known mechanism of the neutral particles formation via ion-induced nucleation followed by recombination of charged clusters. The main results of our investigation are the following: (i) the observed neutral particles were likely formed via the recombination of ion clusters; (ii) the phenomena of electron photodetachment from ion clusters under UV radiation was improbable in conditions of this experiment and likely unrealized for typical negative ion clusters found in the Earth's atmosphere. In total, these experiments and model investigations show that far more and specially directed laboratory experiments are needed to clarify the ways by which cosmic rays and solar radiation may link to the Earth's climate.     

The vertical structure of a pelagic community in the tropical ocean

The vertical structure of the ecosystem in the euphotic zone of the western Equatorial Pacific has been studied. The studies were based on a continuous sounding of the bioluminescence field, with simultaneous, vertically aimed sampling made with the aid of a 5l water bottle and plankton nets. The bioluminescence field has a two-maxima structure with a more pronounced and permanent lower maximum found in the oligotrophic regions as deep as 60 to 100 m. In the narrow (10 m) layer of maximum bioluminescence, the concentration of zooplankton, as well as the concentration, activity and production of bacteria and phytoplankton, are several times higher than those in immediately adjacent waters at greater or lesser depth. At the same time, the concentration of nutrient salts in that layer diminishes sharply and approaches zero in the overlying water. Analysis of the data obtained shows that the production processes above the lower maximum layer are dependent not only on the turbulent influx of nutrient salts from the underlying layers, but also on the horizontal supply from the zone of upwelling. A pelagic community, in its different time aspects from the moment of water ascending until its sinking in the convergence zone, is suggested as a common system for modelling.     

Dynamics of floristic composition of communities dominated by Carex acuta in the northern Volga-Akhtuba floodplain

The floristic composition of plant communities dominated by Carex acuta in the northern Volga-Akhtuba floodplain has been analyzed over the period from 1928 to 2009. It has been shown that, in 2008 to 2009, some hygrophytes disappeared from these phytocenoses; simultaneously, their composition was enriched with mesophytes and adventive species. Ramenskii??s ecological scales have indicated a decrease in water supply to habitats of the communities studied.     

A New Analytical Approach to the Study of the Spatial Structure of the Amur Leopard (Panthera pardus orientalis) Population

Based on data from camera traps installed throughout the model territory in southwest Primorye, information was received during an annual cycle on the presence of individually identified Amur leopards in the area of study. Analysis of the data using a combination of different techniques has determined the mutual spatial arrangement and sizes of approximated home ranges for both male and female leopards. The dataset of individually identified animals proves sufficient in describing the social organization of the studied group of Amur leopard using the spatial overlapping of individual home ranges as a characteristic of social relationships. Each individual home range overlaps with several home ranges belonging to both individuals of the opposite and same sex, with the overlapped portion larger in males than in females.