New data on the fauna and the biogeographic structure of the Hydrozoa, Scyphozoa, Staurozoa and Alcyonacea (Anthozoa) of the Kara Sea

2021 ◽  
Vol 325 (2) ◽  
pp. 143-155
Author(s):  
N.E. Zhuravleva
Keyword(s):  
Cold Water ◽  
Kara Sea ◽  
Novaya Zemlya ◽  
The North ◽  
Anna Trough ◽  
New Material ◽  
Western Side ◽  
Academy Of Sciences ◽  
North Western ◽  
Arctic Fauna

The paper considers the species composition of the fauna of several cnidarian groups of the Kara Sea. The author presents a list of species of the studied groups and indicates the types of habitat for each species. The analysis was based on the literature data, the collections of the Zoological Institute of the Russian Academy of Sciences and material collected in the Kara Sea during the expedition to the R/V Professor Multanovsky in 2019. In total, 87 species of Hydrozoa, 3 species of Scyphozoa, 4 species of Staurozoa, and 5 species of the order Alcyonacea from the class Anthozoa were recorded for the fauna of the Kara Sea, based on the new material obtained by the author and published literature data. The report presents the biogeographic structure of the discussed cnidarian groups. According to the types of biogeographic ranges, the fauna of the above-mentioned cnidarian groups in the Kara Sea mostly consists of representatives of the Boreal-Arctic type of habitat (63%), the Boreal and Amphiboreal biogeographic groups each containing 12% of the total number of described species, and the Panoceanic and Arctic groups together accounting for only 9% and 4% of the fauna of the Kara Sea. Two species new for the Kara Sea, Neoturris pileata (Forsskål, 1775) and Neoturris pileata (Forsskål, 1775), are described. Neoturris pileata is an element of the warm-water Atlantic fauna that penetrated into the Kara Sea with waters of Atlantic genesis. Nausithoe werneri is an element of the cold-water Arctic fauna that penetrated into the Novaya Zemlya Trough of the Kara Sea from the north-western side from the St. Anna Trough, which was open to the Polar Basin.

scholarly journals Geochemical Features of the Thermal and Mineral Waters From the Apuseni Mountains (Romania)

2021 ◽  
Vol 9 ◽  
Author(s):  
Alin-Marius Nicula ◽  
Artur Ionescu ◽  
Ioan-Cristian Pop ◽  
Carmen Roba ◽  
Ferenc L. Forray ◽  
...  
Keyword(s):  
Pannonian Basin ◽  
Isotope Composition ◽  
Thermal Flux ◽  
Mineral Waters ◽  
Aquifer Recharge ◽  
Apuseni Mountains ◽  
The North ◽  
Western Side ◽  
North Western ◽  
Hydrochemical Type

The Apuseni Mountains are located between the large geothermal area of the Pannonian Basin and the low thermal flux Transylvanian Basin. Thermal and mineral waters have been sampled from 42 points along a NW-SE transect. The general chemistry and the water isotope (deuterium and oxygen-18) composition were analyzed. Most of the thermal aquifers are located in carbonate reservoirs. The waters mainly belong to the Ca-HCO3 hydrochemical type, excepting the western side, towards the Pannonian Basin, where the Na-HCO3 type may occur. The isotope composition indicates aquifer recharge from precipitation. The geochemical characteristics and the structural position of the study area suggest two distinct geothermal contexts. The Southern Apuseni area geothermal features are likely connected to the Neogene—Early Quaternary magmatic activity from the Mureş Valley and Zarand Depression. The geothermal manifestations in the north-western part of the study area, at the border between the Northern Apuseni and the Pannonian Depression, share features of the latter one.

scholarly journals Kalmyk causative constructions: case marking, syntactic relations and the speaker’s perspective

2013 ◽  
Vol 2013 (94) ◽  
Author(s):  
Sergey Say
Keyword(s):  
State University ◽  
Causative Constructions ◽  
The North ◽  
Essential Properties ◽  
The Republic ◽  
Syntactic Relations ◽  
Syntactic Properties ◽  
Academy Of Sciences ◽  
North Western ◽  
Direct Correspondence

This study is primarily concerned with the syntactic organisation of Kalmyk clauses headed by verbs that contain a morphological causative marker. The data reported here have been compiled during the summers between 2006 and 2008 in the Republic of Kalmykia. The fieldwork was organised by St. Petersburg State University and the Institute for Linguistic Studies, Russian Academy of Sciences. This fieldwork has been conducted in several villages in the North-Western part of the Republic of Kalmykia. This region is supposed to be the area where the Dörböt dialect of the Kalmyk language is spoken; however, there is no clear indication that the data discussed below are different from the facts found in standard Kalmyk in any relevant respect. The main objective of the study reported here is two-fold. First, there is a descriptive goal. Available descriptions of Kalmyk causatives are mostly concerned with morphological issues and case assignment in canonical causative constructions, whereas a deeper analysis of syntactic properties of causative constructions, especially of their non-canonical uses, is generally lacking. The present study is intended to partially fill this gap. Second, there is a more theoretical goal. It will be shown that there are essential properties of Kalmyk causatives that can be hardly captured by the usual derivational approaches to causatives. Rather, causative verbs in Kalmyk will be viewed as a device for establishing a more or less direct correspondence between an event’s participants and syntactic slots. Although the scope of this paper is limited to one individual language, its findings can have broader typological relevance. In particular, I believe that taking the speaker’s perspective into account can deepen our understanding of causative constructions in other languages as well.

scholarly journals Carbon Dioxide Flux at the Water–Air Boundary at the Continental Slope in the Kara Sea

Oceanology ◽  
2021 ◽  
Vol 61 (5) ◽  
pp. 625-631
Author(s):  
A. A. Polukhin ◽  
M. V. Flint ◽  
I. B. Belikov ◽  
G. V. Gusak ◽  
U. A. Kazakova ◽  
...  
Keyword(s):  
Carbon Dioxide ◽  
Continental Slope ◽  
Frontal Zone ◽  
Field Studies ◽  
Carbon Dioxide Flux ◽  
Kara Sea ◽  
The North ◽  
Siberian Arctic ◽  
Continental Runoff ◽  
Anna Trough

Abstract The values and direction of carbon dioxide flux in the area of the continental slope in the north of the Kara Sea (St. Anna Trough) are calculated based on field studies in 2020 within the Siberian Arctic Sea Ecosystems program. The existence of a stable frontal zone in this area has been confirmed, which is formed by an alongslope current and limits the northward spread of surface waters freshened by the continental runoff. The simultaneous analysis of the carbonate system in the upper sea layer and the CO2 concentration in the surface air layer shows the CO2 flux with a rate of 0.2 to 22 mmol/m2 day to be directed from the atmosphere into the water in the area of the outer shelf, which is affected by the river runoff, and in the area of the continental slope, which is beyond this effect. The highest rates of CO2 absorption by the sea surface layer are localized above the continental slope. Local processes in the area of the slope frontal zone determine the CO2 emission into the atmosphere with a rate of 0.34 mmol/m2 day.

The Amphipod Crustacea of Ungava Bay, Canadian Eastern Arctic

1954 ◽  
Vol 11 (6) ◽  
pp. 709-798 ◽  
Author(s):  
M. J. Dunbar
Keyword(s):  
Kara Sea ◽  
Similar Species ◽  
Separate Species ◽  
The North ◽  
The North Sea ◽  
Western Side ◽  
Sea Area ◽  
First Time ◽  
Marine Zone ◽  
European Form

One hundred and fourteen species of amphipods are recorded from Ungava Bay, most of them for the first time from that area; 21 are new for North America, 5 new to science. Many of them show variations from the types, the types having been described from European or Greenland material. Such variations are to be expected in the Ungava Bay material since it represents a large extension in the known distribution of most of the species, and especially in groups such as the Gammarid and Caprellid amphipods which have no pelagic larvae.In two cases (Westwoodilla megalops and Haploops setosa) pairs of amphipod forms known from Europe as separate species are represented in Ungava Bay by forms which cannot without qualification be referred to either European form, showing characteristics of both, and the two species have therefore been brought into synonymy in each case, since the situation does not warrant the establishment of new species for the Ungava Bay specimens. Since in both cases the European forms were very close together in the first place, each of the two species now exists as three geographic variants; subspecific names have not been given to the variants. Evidence is produced in favour of bringing three species of Ischyrocerus (I. latipes, I. assimilis and I. pachtusovi) together into a similar species complex.The distribution of the Ungava Bay amphipods is analysed. They can be divided into (1) an Atlantic group, possibly endemic to the Atlantic, (2) a group whose distribution lies within the subarctic marine zone as here defined, (3) a large group which does not appear to extend south of the subarctic on the western side of the Atlantic but which is widely distributed in the boreal on the eastern side, in the North Sea area, (4) a small number of arctic forms which become less abundant in the subarctic, and (5) species probably of Pacific origin which are not known east of Greenland nor west of the Kara Sea.

Introduction; and Addendum

1957 ◽  
Vol 52 ◽  
pp. 193-194 ◽  
Author(s):  
A. J. B. Wace
Keyword(s):  
National Museum ◽  
The North ◽  
Large Numbers ◽  
Western Side ◽  
Vertical Joint ◽  
Northern Wall ◽  
North Western

In 1956 the Greek Archaeological Council decided that there should be no excavations at Mycenae. The Anastelosis Department was still busy with the rebuilding of the Cyclopean walls of the Citadel along the western side and along the stretch of ashlar work in conglomerate from the Lion Gate to the north-western angle. At the actual north-western angle the Cyclopean work of the northern wall of the acropolis had originally met the conglomerate work in ashlar with a straight vertical joint. This has now been obscured in the rebuilding. The Archaeological Service was also planning and preparing to put into effect various measures to protect the site from damage by the large numbers of tourists who visit it every year.Since we were thus not able to excavate, we devoted ourselves to studying and preparing for publication the finds from the excavations of previous years in the museums at Athens and Nauplia. In Athens the Director of the National Museum, Dr. Karouzos, and his wife, Mrs. Semne Karouzou, made us very welcome and afforded us every possible facility. Mrs. Sakellariou and Mr. Papathanasopoulos, assistant curators in the museum, also gave us much friendly help. At Nauplia Mr. N. Verdeles, the Inspector of Antiquities, and Miss Protonotariou, the Epimeletes, made special arrangements for our work and gave us every support.

First record of Hylomyscus walterverheyeni (Rodentia: Muridae) on the north-western side of the Sanaga River (western Cameroon)

Zootaxa ◽  
2009 ◽  
Vol 2044 (1) ◽  
pp. 46-60 ◽  
Author(s):  
ALAIN DIDIER MISSOUP ◽  
VIOLAINE NICOLAS ◽  
WIM WENDELEN ◽  
CHARLES FELIX BILONG BILONG ◽  
CORINNE CRUAUD ◽  
...  
Keyword(s):  
Phylogenetic Analyses ◽  
First Record ◽  
Mountain Forests ◽  
North West ◽  
The North ◽  
16S Gene ◽  
Discriminant Analyses ◽  
Western Side ◽  
North Western

We used both molecular and craniometrical data to test the presence of Hylomyscus walterverheyeni in the Cameroon Volcanic Line (CVL). Our molecular (cytochrome b and 16S gene sequencing) and morphometrical data (discriminant analyses) clearly show the presence of H. walterverheyeni in the CVL, north-west of the Sanaga River. Hylomyscus walterverheyeni occupies both lowland and mountain forests (up to 2000m asl). In our phylogenetic analyses, the CVL specimens form a monophyletic group. This clade seems to reflect the role of the Sanaga River as a barrier to gene flow within the species.

The Diorites and Associated Rocks of the Glen Tilt Complex, Perthshire

1938 ◽  
Vol 75 (4) ◽  
pp. 174-184 ◽  
Author(s):  
W. A. Deer
Keyword(s):  
Small Area ◽  
Biotite Granite ◽  
Reasonable Doubt ◽  
The South ◽  
The North ◽  
South West ◽  
Granitic Intrusion ◽  
Western Side ◽  
Basic Rocks ◽  
North Western

The Glen Tilt Complex, one of the larger masses of the Newer Granites of the Central Highlands, is included in sheet 64 of the Geological Survey of Scotland. The greater part of this complex is a granite which is bounded on the south-west and southeast by an earlier series of intermediate and basic rocks. The granites described in this contribution are restricted to a small area at the south-eastern margin of the large granitic intrusion generally known as the Beinn Dearc granite. The smaller and independent intrusion of the Sron a ‘Chro’ granite and a number of smaller masses of granite associated with the marginal strip of diorites on the north-western side of Glen Tilt have also been examined. These small isolated areas appear to be contemporaneous with the intrusion of the main Beinn Dearc mass and have been intruded between the earlier diorites and the margin of the intrusion, a feature not uncommon in many of the other Scottish Newer Granites. A small independent mass of muscovite-biotite-granite intruded into quartz-mica-diorite occurs on Conlach Mhor. Although these rocks are completely isolated from both the biotite- and muscovite-biotite-granites of the main Beinn Dearc intrusion their essential similarity with the latter leaves no reasonable doubt of their common origin.

scholarly journals The earliest public green areas connected with Jelenia Góra, part. 2

1970 ◽  
Vol 14 (3) ◽  
pp. 109-118
Author(s):  
Marzanna Jagiełło ◽  
Wojciech Brzezowski
Keyword(s):  
18Th Century ◽  
17Th Century ◽  
Public Parks ◽  
Natural Landscape ◽  
The Third ◽  
The North ◽  
Green Areas ◽  
Western Side ◽  
The City ◽  
North Western

In the third part of the 18th century the earliest public landscape gardens began to appear in the area of suburban Jelenia Góra. They were the first public parks in Silesia. When establishing them, the natural landscape features of the area were used (Karkonosze). Two of them, Hausberg and Helkon, were created at the end of the 17th century on the north-western side of the city.

scholarly journals Parentage Atlas of Italian Grapevine Varieties as Inferred From SNP Genotyping

2021 ◽  
Vol 11 ◽  
Author(s):  
Claudio D’Onofrio ◽  
Giorgio Tumino ◽  
Massimo Gardiman ◽  
Manna Crespan ◽  
Cristina Bignami ◽  
...  
Keyword(s):  
Central Italy ◽  
Snp Genotyping ◽  
Parental Relationships ◽  
The North ◽  
Magna Graecia ◽  
Adriatic Coast ◽  
Geographically Distributed ◽  
Western Side ◽  
High Level ◽  
North Western

The Italian grape germplasm is characterized by a high level of richness in terms of varieties number, with nearly 600 wine grape varieties listed in the Italian National Register of Grapevine Varieties and with a plethora of autochthonous grapes. In the present study an extended SNP genotyping has been carried out on Italian germplasm of cultivated Vitis vinifera subsp. sativa and Vitis hybrids. Several hundred Italian varieties maintained in the repositories of scientific Institutions and about one thousand additional varieties derived from previous studies on European, Southern Italy, Magna Graecia and Georgian germplasm were considered. The large genotyping data obtained were used to check the presence of homonyms and synonyms, determine parental relationships, and identify the main ancestors of traditional Italian cultivars and closely-related accessions. The parentage among a set of 1,232 unique varieties has been assessed. A total of 92 new parent-offspring (PO) pairs and 14 new PO trios were identified. The resulted parentage network suggested that the traditional Italian grapevine germplasm originates largely from a few central varieties geographically distributed into several areas of genetic influence: “Strinto porcino” and its offspring “Sangiovese”, “Mantonico bianco” and “Aglianico” mainly as founder varieties of South-Western Italy (IT-SW); Italian Adriatic Coast (IT-AC); and Central Italy with most varieties being offsprings of “Visparola”, “Garganega” and “Bombino bianco”; “Termarina (Sciaccarello)” “Orsolina” and “Uva Tosca” as the main varieties of North-Western Italy (IT-NW) and Central Italy. The pedigree reconstruction by full-sib and second-degree relationships highlighted the key role of some cultivars, and, in particular, the centrality of “Visparola” in the origin of Italian germplasm appeared clear. An hypothetical migration of this variety within the Italian Peninsula from South to North along the eastern side, as well as of “Sangiovese” from South to Central Italy along the Western side might be supposed. Moreover, it was also highlighted that, among the main founders of muscat varieties, “Moscato bianco” and “Zibibbo (Muscat of Alexandria)” have spread over the whole Italy, with a high contribution by the former to germplasm of the North-Western of the peninsula.

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