scholarly journals Moth diversity, species composition, and distributional pattern in Aravalli Hill Range of Rajasthan, India

Author(s):  
Afaq Ahmad Dar ◽  
Khowaja Jamal
2017 ◽  
Vol 149 (5) ◽  
pp. 628-638 ◽  
Author(s):  
Julia Shrubovych ◽  
Maria Sterzyńska

AbstractThe biodiversity of transitional zones is unique, due to mixing and co-occurrence of biotic elements. Despite this, our basic knowledge on distributional patterns of soil microarthropods in areas where biogeographic regions overlap is insufficient. We studied the biogeographic patterns of Protura across three natural landforms in Ukraine within the Transcarpathia (Transcarpathian Lowland, Transcarpathian foothills, and Volcanic Ukrainian Carpathian), which are influenced by adjacent biogeographic areas (mainly Alpine and Pannonian). We hypothesised that these overlaps have brought about an increase in Protura diversity, due to inclusion of faunal elements from diverse origins and differing in geographical histories. Distinct differences in the species composition of Protura were found among lowland, foothill, and mountain sites within Transcarpathia. Mountain sites mainly have Protura species with a wide continental distribution, while species of the foothills mainly stem from the Pannonian biogeographic region. The highest number of proturan endemics was associated with the Transcarpathian foothills. We conclude that the Transcarpathian region can be defined as a biogeographical transition zone for soil microarthopods, exemplified by Protura, and that foothill sites such as the volcanic-tectonic mountain Chorna Hora is a local hotspot of diversity and endemism, representing the most valuable parts of Transcarpathia with respect to diversity and endemism.


Author(s):  
Shevchenko I.V.

The work is the first part of a series of articles intended to comprehensively describe the current state of Chironomidae fauna of the Lower Dnipro on the basis of the long-term studies of larval forms of this group of Diptera insects, widely represented in water bodies of this estuary. Based on the current research, the species composition of larvae of Diptera insects of the Tanypodinae (Diptera, Chironomidae) subfamily, represented in the benthic fauna of various water bodies of the Lower Dnipro, is described. The research was conducted on 18 water bodies, located in the delta and pre-delta areas of the Dnipro River. For the delta area, the following water bodies were researched: mainstream of the Dnipro River, the Viryovchina River, KhersonBilozerskyi floodplain area (the Koshova River, Lake Rohozuvate, Lake Bezmen, Lake Chychkuvate, Lake Stebliivskyi Liman), Kardashynskyi floodplain area (the Chaika River, the strait into Lake Kruhle, the Hadiuchka Strait, Lake Kruhle, Lake Kardashynskyi Liman), Velykyi Potyomkinskyi floodplain area (Lake Zakitne and Lake Nazarove-Pohorile) and Holoprystanskyi floodplain area (Lake Liahushache). For the pre-delta area, the mainstream of the Dnipro River, the Kozak River and Lake Sabetskyi Liman were researched. Based on the obtained data, a characteristic for each of the species of Tanypodinae is given, which includes: the distribution; the seasonality; indicators of quantitative development; the abiotic factors and the species of higher aquatic vegetation inherent in the places of detection of the larvae; the area. The mass and the less developed species of Tanypodinae subfamily and their distributional pattern in the water bodies have been determined. The indexes of occurrence in the benthic samples for the larvae of these species were determined. The comparisons of the indexes for individual water bodies, groups of water bodies (streaming system of the Dnipro River, the tributaries and the straits, the Viryovchina River, the pre-delta area, the delta floodplain areas) and for the water bodies as a whole, were made. The species composition of Tanypodinae larvae of anthropogenically polluted areas of the Lower Dnipro, in particular, its differences for the watercourses and lakes, were noted. Key words: Diptera, larvae, fauna, macrozoobenthos, Lower Dnipro, Chironomidae, Tanypodinae.


2017 ◽  
Vol 52 (6) ◽  
pp. 1279-1286
Author(s):  
G.P. Kononenko ◽  
◽  
E.A. Piryazeva ◽  
E.V. Zotova ◽  
A.A. Burkin ◽  
...  
Keyword(s):  

2014 ◽  
Vol 25 (3-4) ◽  
pp. 53-68
Author(s):  
I. V. Goncharenko ◽  
H. M. Holyk

Cenotic diversity and leading ecological factors of its floristic differentiation were studied on an example of two areas – Kyiv parks "Nivki" and "Teremki". It is shown that in megalopolis the Galeobdoloni-Carpinetum impatientosum parviflorae subassociation is formed under anthropogenic pressure on the typical ecotope of near-Dnieper hornbeam oak forests on fresh gray-forest soils. The degree of anthropogenic transformation of cenofloras can be estimated by the number of species of Robinietea and Galio-Urticetea classes, as well as neophytes and cultivars. Phytoindication for hemeroby index may be also used in calculation. We propose the modified index of biotic dispersion (normalized by alpha-diversity) for the estimation of ecophytocenotic range (beta-diversity) of releves series. We found that alpha-diversity initially increases (due to the invasion of antropophytes) at low level of antropogenic pressure, then it decreases (due to the loss of aboriginal species) secondarily with increasing of human impact. Also we found that beta-diversity (differential diversity) decreases, increasing homogeneity of plant cover, under the influence of anthropogenic factor. Vegetation classification was completed by a new original method of cluster analysis, designated as DRSA («distance-ranked sorting assembling»). The classification quality is suggested to be validated on the "seriation" diagram, which is а distance matrix between objects with gradient filling. Dark diagonal blocks confirm clusters’ density (intracluster compactness), uncolored off-diagonal blocks are evidence in favor of clusters’ isolation (intercluster distinctness). In addition, distinction of clusters (syntaxa) in ordination area suggests their independence. For phytoindication we propose to include only species with more than 10% constancy. Furthermore, for the description of syntaxonomic amplitude we suggest to use 25%-75% interquartile scope instead of mean and standard deviation. It is shown that comparative analysis of syntaxa for each ecofactor is convenient to carry out by using violin (bulb) plots. A new approach to the phytoindication of syntaxa, designated as R-phytoindication, was proposed for our study. In this case, the ecofactor values, calculated for individual releves, are not taken into account, however, the composition of cenoflora with species constancies is used that helps us to minimize for phytoindication the influence of non-typical species. We suggested a syntaxon’s amplitude to be described by more robust statistics: for the optimum of amplitude (central tendency) – by a median (instead of arithmetic mean), and for the range of tolerance – by an interquartile scope (instead of standard deviation). We assesses amplitudes of syntaxa by phytoindication method for moisture (Hd), acidity (Rc), soil nitrogen content (Nt), wetting variability (vHd), light regime (Lc), salt regime (Sl). We revealed no significant differences on these ecofactors among ecotopes of our syntaxa, that proved the variant syntaxonomic rank for all syntaxa. We found that the core of species composition of our phytocenoses consists of plants with moderate requirements for moisture, soil nitrogen, light and salt regime. We prove that the leading factor of syntaxonomic differentiation is hidden anthropogenic, which is not subject to direct measurement. But we detect that hidden factor of "human pressure" was correlated with phytoindication parameters (variables) that can be measured "directly" by species composition of plant communities. The most correlated factors were ecofactors of soil nitrogen, wetting variability, light regime and hemeroby. The last one is the most indicative empirically for the assessment of "human impact". We establish that there is a concept of «hemeroby of phytocenosis» (tolerance to human impact), which can be calculated approximately as the mean or the median of hemeroby scores of individual species which are present in it.


2013 ◽  
Vol 25 (1-2) ◽  
pp. 136-148
Author(s):  
I. V. Gryb

The concept of an explosion in freshwater ecosystems as a result of the release of accumulated energy, accompanied by the destruction of the steady climax successions of hydrocenoses is presented. The typification of local explosions as well as methods for assessing their risk during the development of river basins are shown. The change in atmospheric circulation, impaired phases of the hydrological regime of rivers, increasing the average temperature of the planet, including in Polesie to 0,6 ºC, deforestation leads to concentration and release of huge amounts of unmanaged terrestrial energy, which manifests itself in the form of disasters and emergencies. Hydroecological explosion is formed as a result of multifactorial external influence (natural and anthropogenic) on the water body in a certain period of time. Moreover, its level at wastewater discharge depends on the mass of recycled impurities and behaved processing capacity of the reservoir, and the mass of dumped on biocides and the possibility of the water flow to their dilution and to the utilization of non-toxic concentrations. In all these cases the preservation of "centers of life" in the tributaries of the first order – local fish reproduction areas contributed to ecosystem recovery, and the entire ecosystem has evolved from equilibrium to non-equilibrium with further restructuring after the explosion and environmental transition to a new trophic level. It means that hydroecological explosion can be researched as the logical course of development of living matter in abiotic environmental conditions, ending abruptly with the formation of new species composition cenoses and new bio-productivity. The buffer capacity of the water environment is reduced due to re-development and anthropic transformation of geobiocenoses of river basins, which leads to a weakening of life resistance. This applies particularly to the southern industrial regions of Ukraine, located in the arid zone that is even more relevant in the context of increased average temperature due to the greenhouse effect, as well as to Polesie (Western, Central and Chernihiv), had been exposed to large-scale drainage of 60-80th years, which contributed to the degradation of peatlands and fitostroma. Imposing the western trace of emissions from the Chernobyl accident to these areas had created the conditions of prolonged hydroecological explosion in an intense process of aging water bodies, especially lakes, change in species composition of fish fauna and the occurrence of neoplasms at the organismal level. Under these conditions, for the existence of man and the environment the vitaukta should be strengthened, i.e. buffer resistance and capacitance the aquatic environment, bioefficiency on the one hand and balanced using the energy deposited - on the other. This will restore the functioning of ecosystems "channel-floodplain", "riverbed-lake", reducing the energy load on the aquatic environment. Hydroecological explosions of natural origin can not be considered a pathology – it is a jump process of natural selection of species of biota. Another thing, if they are of anthropogenic origin and if the magnitude of such an impact is on the power of geological factors. Hydroecological explosions can be regarded as a manifestation of environmental wars that consciously or unconsciously, human society is waging against themselves and their kind in the river basins, so prevention of entropy increase in the aquatic environment and the prevention of hydroecological explosions is a matter of human survival. While the man - is not the final link in the development of living matter, it can develop without him, as matter is eternal, and the forms of its existence are different.


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