scholarly journals RESULTS OF STUDY OF FINE COLLECTION OF BLUE IN THE CONDITIONS OF MURMANSK REGION

2018 ◽  
Vol 44 ◽  
Author(s):  
Lyubov Vladimirovna Sukhareva ◽  
Author(s):  
A. Kartashova ◽  
◽  
E. Firsova ◽  
Keyword(s):  

Author(s):  
G. I. Tikhonova ◽  
M. S. Bryleva ◽  
T. Yu. Gorchakova

Standardized mortality rates of the male population aged 15-59 in Monchegorsk, where the Kola mining and metallurgical company is located, were higher relative to the Murmansk region and Russia: from diseases of the circulatory system by 34.8% and 52.1%, respectively, from malignant neoplasms by 26.3% and 19.4%, from diseases of the digestive system by 59.0% and 36.3%.


2001 ◽  
pp. 49-57 ◽  
Author(s):  
N. E. Koroleva

The paper deals with syntaxonomy of mountain mires in the lower oroarctic zone of Khibiny Mountains (Mur­mansk Re­gion). Six associations and one subassociation which belong to four alliances are described. Short characte­ristic of syntaxa and phytocoenological tables are given. Prevalence of mesophytic and hygro-meso­phytic species rather than true helophytic species is reported as a characteristic feature of these communities.


2008 ◽  
Vol 42 ◽  
pp. 189-197
Author(s):  
G. P. Urbanavichus ◽  
I. N. Urbanavichene

87 species of lichens and 14 species of lichenicolous fungi are cited as first recorded for Murmansk Region (31 species) or as very rare there. The annotated list is based on the authors’ collections made in 2003–2007 in the Lapland Reserve.


2017 ◽  
Vol 51 ◽  
pp. 242-250
Author(s):  
M. V. Dulin

Tetralophozia setiformis is a widespread species occurring usually without organs of sexual and asexual reproduction. Gemmae of Tetralophozia setiformis were observed for the second time in Russia and Eurasia in the Northern Urals, Komi Republic. They form compact masses over upper leaves. The compact masses consist largely (70 %) of immature gemmae. Description of gemmae and gemmiparous shoots from the Northern Urals and their comparison with those from the other known localities, namely British Columbia (Canada) and the Murmansk Region (European Russia) were carried out. The gemmiparous plants of T. setiformis from the Northern Urals have approximately the same width as plants without gemmae but they are shorter. The leaves of gemmiparous plants from the Northern Urals are similar to leaves of gemmiparous plants from British Columbia. The leaf shape in upper part of the gemmiparous shoots varies from the typical to ± modified from gemmae production. These leaf shape transitions include reduction of leaf size and lobe number from 4 to 2–3, suppression of development and disappearance of characteristic teeth at the base of sinus. Gemmae size (17 × 22 μm) of plants from the Northern Urals is within variability recorded for plants from the Murmansk Region and British Columbia.


2009 ◽  
Vol 43 ◽  
pp. 50-62
Author(s):  
D. A. Davydov

The results of studies of Cyanoprokaryota (Cyanophyta, Cyanobacteria) of the Murmansk Region are presented. The list of Chroococcales contains 78 species, 16 ones being reported as new records for the Murmansk Region, Gloeocapsopsis pleurocapsoides — as a new record for Russia.


2011 ◽  
Vol 45 ◽  
pp. 276-291 ◽  
Author(s):  
E. A. Borovichev

An annotated list of hepatics of Monche-tundra Mts. was compiled for the first time. It includes 123 species and 8 varieties. Lophoziopsis excisa var. elegans is reported as new for the Murmansk Region, Lejeunea cavifolia was recorded secondly for the region, and Scapania tundrae is new for Lapland State Nature Reserve. There are 18 species listed in the Red Data Book of Murmansk Region.


1968 ◽  
Vol 46 (10) ◽  
pp. S823-S824
Author(s):  
S. N. Vernov ◽  
A. N. Charakhchyan ◽  
T. N. Charakhchyan ◽  
Yu. J. Stozhkov

The results of the analysis of data obtained from measurements carried out by means of regular stratospheric launchings of cosmic-ray radiosondes over the Murmansk region and the Antarctic observatory in Mirny in 1963–66 are presented. The problem of the anisotropy of the primary component of low-energy cosmic rays and of temperature effects on the cosmic-ray intensity in the atmosphere are discussed.


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