Boreal larch forests of the alliance Roso acicularis–Laricion cajanderi all. nov. in the north-east of Russia

2016 ◽  
pp. 125-138 ◽  
Author(s):  
N. V. Sinelnikova

The floodplain forests occupy river valleys in the North-East of Yakutia, Magadan region, Chukotka and Kamchatka. Studies on their dynamics, syntaxonomy and typology based on various classification principles have been undertaken throughout the last 100 years (Vasyliyev, 1956; Tyulina, 1959; Neshatayeva, 2009; The Far North…, 2010). Some studies based on the Braun-Blanquet approach were made in the past two decades (Krestov et al., 2009; Sinelnikova, 1995, 2009).

2002 ◽  
Vol 29 (2) ◽  
pp. 117 ◽  
Author(s):  
P. D. Olsen ◽  
B. Doran

The Australian distribution of the grass owl (Tyto capensis) is poorly understood. It has been proposed that there are two centres of distribution: a resident coastal population in the north-east, and a less stable inland population from which there is Australia-wide dispersal when good seasons are followed by deteriorating conditions. We analysed records of the grass owl and modelled its bioclimatic profile and distribution, which was typically subtropical, warm to hot humid with no dry season or a dry winter. This predicted a north-east sub-coastal to coastal, permanently occupied, core distribution for the owl. We found no evidence for a permanent or isolated inland population, nor for inland populations being the sole source of dispersers, as has been suggested previously. Most inland and northern records were made in the 1970s when grass owls colonised the arid inland, the Kimberley and the far north of the country in association with events leading to the flooding of Lake Eyre. The data suggest that grass owls disperse from their core range after exceptionally good breeding seasons to areas made temporarily favourable by exceptional rainfall or flooding, only to disperse again when conditions become drier. These dispersal events are not tied uniquely to outbreaks of the long-haired rat (Rattus villosissimus), but to a variety of terrestrial prey with dynamic life histories driven by rainfall.


2021 ◽  
Vol 6 (2) ◽  
pp. 243-256
Author(s):  
Yulia Yu. Mageramova ◽  

The article describes a specific linguistic situation that developed in the Far North-East of Russia (CWS) using the example of the Magadan region in the late 20th – early 21st centuries. The study used theoretical and empirical general scientific methods (analysis, synthesis, observation and generalization), as well as proper linguistic and sociolinguistic modifications of general scientific methods (quantitative and conceptual analysis, inclusive observation, interviewing native speakers). The main extralinguistic factors, under the influence of which the modern linguistic situation was formed, were determined: harsh climatic conditions, low population density, poorly developed transport infrastructure, remoteness from centers of science and culture, the presence of an autochthonous population, a heterogeneous and unstable composition of inhabitants, etc. It is proved that the combination of the influence of extralinguistic factors with the action of internal linguistic laws has led to the formation of a special linguistic situation on the CWS, which is characterized by the following features: the presence of borrowings from the languages of the indigenous peoples of the North, minimization of dialectal influence, the existence of a particular Kolyma regional dialect functioning in the region. As an illustration, there are examples of lexemes borrowed from the languages of autochthonous ethnic groups in the Russian literary language, in old-time dialects, in the Kolyma region. The article covers the issue of old-timers' dialects that have survived in certain settlements of the Magadan region but do not have an impact on the speech of the Kolyma residents today. The structure of the lexical-semantic level of the Kolyma region is described, it is represented by several types of localisms: semantic, lexical, relative and substratum regionalisms. The conclusion is made about the formation of a special linguistic situation in the Far North-East of Russia, which, on the one hand, is in many respects specific, and on the other hand, corresponds to the global trends in the development of language systems.


Palaeobotany ◽  
2019 ◽  
Vol 10 ◽  
pp. 13-179
Author(s):  
L. B. Golovneva

The Chingandzha flora comes from the volcanic-sedimentary deposits of the Chingandzha Formation (the Okhotsk-Chukotka volcanic belt, North-East of Russia). The main localities of the Chingandzha flora are situated in the Omsukchan district of the Magadan Region: on the Tap River (basin of the middle course of the Viliga River), on the Kananyga River, near the mouth of the Rond Creek, and in the middle reaches of the Chingandzha River (basin of the Tumany River). The Chingandzha flora includes 23 genera and 33 species. Two new species (Taxodium viligense Golovn. and Cupressinocladus shelikhovii Golovn.) are described, and two new combinations (Arctopteris ochotica (Samyl.) Golovn. and Dalembia kryshtofovichii (Samyl.) Golovn.) are created. The Chingandzha flora consists of liverworts, horsetails, ferns, seed ferns, ginkgoaleans, conifers, and angiosperms. The main genera are Arctop teris, Osmunda, Coniopteris, Cladophlebis, Ginkgo, Sagenoptepis, Sequoia, Taxodium, Metasequoia, Cupressinocladus, Protophyllocladus, Pseudoprotophyllum, Trochodendroides, Dalembia, Menispermites, Araliaephyllum, Quereuxia. The Chingandzha flora is distinct from other floras of the Okhotsk-Chukotka volcanic belt (OCVB) in predominance of flowering plants and in absence of the Early Cretaceous relicts such as Podozamites, Phoenicopsis and cycadophytes. According to its systematic composition and palaeoecological features, the Chingandzha flora is similar to the Coniacian Kaivayam and Tylpegyrgynay floras of the North-East of Russia, which were distributed at coastal lowlands east of the mountain ridges of the OCVB. Therefore, the age of the Chingandzha flora is determined as the Coniacian. This flora is assigned to the Kaivayam phase of the flora evolution and to the Anadyr Province of the Siberian-Canadian floristic realm. The Chingandzha flora is correlated with the Coniacian Aleeky flora from the Viliga-Tumany interfluve area and with other Coniacian floras of the OCVB: the Chaun flora of the Central Chukotka, the Kholchan flora of the Magadan Region and the Ul’ya flora of the Ul’ya Depression.


2019 ◽  
pp. 77-94
Author(s):  
I. A. Likhanova ◽  
G. S. Shushpannikova ◽  
L. P. Turubanova

The results of floristic classification of technogenic vegetation (alliance Chamerio angustifolii–Matricarion hookeri A. Ishbirdin et al. 1996, order Chamerio–Betuletalia nanae Khusainov et al. in Sumina 2012, class Matricario–Poetea arcticae A. Ishbirdin in Sumina 2012) conducted by the Braun-Blanquet method (Braun-Blanquet, 1964; Mirkin, Naumova, 1998) are given. 98 geobotanical relevés, made in 1981–2013 on areas of oil fields and suburbs of the Usinsk city (Komi Republic) (56–60о N, 67–66о E), were involved into analysis (Fig. 1). The ecological parameters like moisture (F) and mineral nitrogen soil enrichment (N) were assessed using the Ellenberg ecological scales (Ellenberg, 1974).


1925 ◽  
Vol 15 (3) ◽  
pp. 257-271 ◽  
Author(s):  
James Hendrick ◽  
George Newlands

1. Previous investigations showed that certain Scottish soils were of glacial drift origin, that they were comparatively rich in unweathered silicates and therefore in reserves of plant-food, that they showed considerable variation in such silicates and were capable of classification accordingly. Some indication was also shown that the glacial drift, and hence the resulting soil, was sometimes of local origin, its character being determined by the underlying rock. In the present investigation a more extensive survey of Scottish soils has been made in order to discover to what extent these preliminary findings might be applicable generally.2. For this purpose soils have been collected from various localities in the north, north-east, west and south of Scotland, and have been analysed mechanically and the “fine sand” fraction examined mineralogically.


1945 ◽  
Vol 82 (6) ◽  
pp. 267-273 ◽  
Author(s):  
W. Anderson

Formerly there were several surface brine springs in the North-East Coalfield; to-day there are none. From the many accounts of their occurrence nothing has been learned of their exact position, and very little of the composition of their waters. The earliest record, made in 1684, described the Butterby spring (Todd, 1684), and then at various times during the next two centuries brine springs at Framwellgate, Lumley, Birtley, Walker, Wallsend, Hebburn, and Jarrow were noted. In particular the Birtley salt spring is often mentioned, and on the 6-in. Ordnance map, Durham No. 13, 1862 edition, it is sited to the south-east of the village. Although no record has been found there must have been either a brine spring or well at Gateshead, for the name of the present-day suburb, Saltwell, is very old, and brine springs are still active in the coal workings of that area.


2008 ◽  

From the late Sixties on, industrial development in Italy evolved through the spread of small and medium sized firms, aggregated in district networks, with an elevated propensity to enterprise and the marked presence of owner-families. Installed within the local systems, the industrial districts tended to simulate large-scale industry exploiting lower costs generated by factors that were not only economic. The districts are characterised in terms of territorial location (above all the thriving areas of the North-east and Centre) and sector, since they are concentrated in the "4 As" (clothing-fashion, home-decor, agri-foodstuffs, automation-mechanics), with some overlapping with "Made in Italy". How can this model be assessed? This is the crucial question in the debate on the condition and prospects of the Italian productive system between the supporters of its capacity to adapt and the critics of economic dwarfism. A dispassionate judgement suggests that the prospects of "small is beautiful" have been superseded, but that the "declinist" view, that sees only the dangers of globalisation and the IT revolution for our SMEs is risky. The concept of irreversible crisis that prevails at present is limiting, both because it is not easy either to "invent", or to copy, a model of industrialisation, and because there is space for a strategic repositioning of the district enterprises. The book develops considerations in this direction, showing how an evolution of the district model is possible, focusing on: gains in productivity, scope economies (through diversification and expansion of the range of products), flexibility of organisation, capacity to meld tradition and innovation aiming at product quality, dimensional growth of the enterprises, new forms of financing, active presence on the international markets and valorisation of the resources of the territory. It is hence necessary to reactivate the behavioural functions of the entrepreneurs.


2019 ◽  
Vol 96 (8) ◽  
pp. 766-769 ◽  
Author(s):  
Inessa V. Averyanova ◽  
S. I. Vdovenko ◽  
A. L. Maksimov

Natural and climatic conditions of the environment of Northeast Russia and particularly Magadan region are the very factor mostly influencing adaptive responses by individuals inhabiting the region. Compensatory and adaptive responses in indigenes and newcomers of the region can be assumed to have their specific features. In 2009 there was executed the examination of the cardiovascular and respiratory systems and gas exchange in 392 cases aged of 17-19 years, including Europeans (Caucasians) born in the North in the 1st-2nd generation and indigenes. The methodologically similar study was carried out in 2014 in 265 persons, referred to the same cohorts of North-born Caucasians and Indigenes from the Magadan region. The results of the study executed in 2009 testified to a small number of physiological parameters that were reliably different in Caucasians vs. Indigene subjects. In 2014 no difference was found between the two examined cohorts throughout the observed parameters. The revealed changes in gas exchange, external respiration and cardiovascular systems demonstrated by modern young Indigenes of Northeast Russia testified to the fall in the effectiveness of their breathing. All that makes them farther from the classic “polar metabolic type” and their morphofunctional status becomes closer to European male subjects of Northeast Russia. Thus, we can observe a clear tendency towards “convergence in programs” of the adaptive changes between populations of the North residents undergoing similar natural, environmental and social factors.


2020 ◽  
Vol 16 (47) ◽  
pp. 84-110
Author(s):  
Elena Malaya ◽  

The article is devoted to ideas about the Soviet era, widespread in а village in the north-east of Crimea. The paper offers an analysis of how the community, formed around a partially preserved state farm, builds its own picture of historical time, expands the imaginary boundaries of the Soviet period, and also thinks of it not so much as the past, but as the past future. Particular attention is paid to the object that organizes its temporality — а time capsule, which was laid twice in the studied village (in 1967 and in 2017), as well as its connection with the teleology of modernism. The article compares letters to descendants, sealed in two time capsules, as well as additional documents sent to the future. The text of the 1967 letter is based on a progressive narrative and contains a list of economic indicators of the success of the Soviet economy. By contrast, the 2017 text creates a picture of an unstable time of change, in which the focus is not on the predictable future, but on the vague past and present. The author of the article explains the nostalgia for the Soviet era in the studied community by the reaction to the changes and crises of the post-Soviet period, and suggests using temporal logic in the research of post-socialism.


2021 ◽  
Vol 10 (1) ◽  
pp. 157-162
Author(s):  
Vera Valentinovna Solovieva

The study covered 10 small rivers in the North-Eastern part of the Samara Volga region. The author studied the vegetation cover, which is understood as a set of phytocoenoses and their constituent plant species. On the territory of Pokhvistnevsky District, there are two groups of river valleys that are heterogeneous in geobotanical terms. The first group includes the rivers with forested valleys (Kutlugush, Murakla, Karmalka). Their slopes are more or less symmetrical and steep. The vegetation cover of an undeveloped floodplain is usually uniform, and there is usually no belt. The valleys of the second group are treeless; their slopes are sharply asymmetrical (Amanak, Tergala, Talkish). The right-bank tributary of the Maly Kinel River the Lozovka River with its length of 20 km and the left tributary Kuvayka River with its length of 16 km were studied on the territory of Kinel-Cherkassky District. The Padovka and Zaprudka rivers and the right tributaries of the Bolshoi Kinel River (Kinelsky District) were also studied. The most common associations are (Salix fragilis heteroherbosa, Scirpus sylvaticus purum, Agrostis stolonifera Amoria repens, Elytrigia repens + Poa angustifolia heteroherbosa). In total, 19 types of phytocoenoses were noted, 4 of them are found in half of the studied rivers. In the plant communities of small river valleys there are 232 species of higher wild plants, which belong to 139 genera from 48 families. This is 60% of the total number of higher plants registered in the flora of small river valleys of the Samara Region. Rare protected plant species are registered here: Adonis volgensis Steven ex DC., Cacalia hastata L., Delphinium cuneatum Stev. ex DC., Globularia punctata Lapeyr.


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