scholarly journals The genetic structure of Norway

2020 ◽  
Author(s):  
Morten Mattingsdal ◽  
S. Sunna Ebenesersdóttir ◽  
Kristjan H. S. Moore ◽  
Ole A. Andreassen ◽  
Thomas F. Hansen ◽  
...  

AbstractThe aim of the present study was to describe the genetic structure of the Norwegian population using genotypes from 6369 unrelated individuals with detailed information about places of residence. Using standard single marker- and haplotype-based approaches, we report evidence of two regions with distinctive patterns of genetic variation, one in the far northeast, and another in the south of Norway, as indicated by fixation indices, haplotype sharing, homozygosity and effective population size. We detect and quantify a component of Uralic Sami ancestry that is enriched in the North. On a finer scale, we find that rates of migration have been affected by topography like mountain ridges. In the broader Scandinavian context, we detect elevated relatedness between the mid- and northern border areas towards Sweden. The main finding of this study is that despite Norway’s long maritime history and as a former Danish territory, the region closest to mainland Europe in the south appears to have been the most isolated region in Norway, highlighting the open sea as a barrier to gene flow.

Author(s):  
Morten Mattingsdal ◽  
S. Sunna Ebenesersdóttir ◽  
Kristjan H. S. Moore ◽  
Ole A. Andreassen ◽  
Thomas F. Hansen ◽  
...  

AbstractThe aim of the present study was to describe the genetic structure of the Norwegian population using genotypes from 6369 unrelated individuals with detailed information about places of residence. Using standard single marker- and haplotype-based approaches, we report evidence of two regions with distinctive patterns of genetic variation, one in the far northeast, and another in the south of Norway, as indicated by fixation indices, haplotype sharing, homozygosity, and effective population size. We detect and quantify a component of Uralic Sami ancestry that is enriched in the North. On a finer scale, we find that rates of migration have been affected by topography like mountain ridges. In the broader Scandinavian context, we detect elevated relatedness between the mid- and northern border areas towards Sweden. The main finding of this study is that despite Norway’s long maritime history and as a former Danish territory, the region closest to mainland Europe in the south appears to have been an isolated region in Norway, highlighting the open sea as a barrier to gene flow into Norway.


2021 ◽  
Vol 233 ◽  
pp. 03035
Author(s):  
Zhuzhu Yu ◽  
Zhiguo He ◽  
Li Li ◽  
Taoyan Ye ◽  
Yuezhang Xia

Based on FVCOM hydrodynamic numerical model and coastline topographic data in 2013, a three-dimensional numerical model of fine sediment transport in Hangzhou Bay has been established to explore the water and sediment exchange mechanism between Hangzhou Bay and the open sea at different typical sections. The results of validation with measured and satellite retrieved data show that the model can well simulate the process of water and sediment movement in Hangzhou Bay. Compared with the calculation results of the coastline topographic data of Hangzhou Bay in 1974 and 2020, the influence mechanism of shoreline change on the water and sediment exchange mechanism between Hangzhou Bay and the open sea has been studied. The results show that the sediment transport inside and outside the Hangzhou Bay is generally in the pattern of north-inflow and south-discharge. Compared with the coastline in 1974, the sediment transport from Yangshan port in the north of Hangzhou Bay and Zhoushan Islands in the middle of Hangzhou Bay increases when the coastline is pushed into the bay in 2020, while the outward sediment transport from Jintang Channel in the South decreases. The overall trend features that the sediment transport into the bay increases, with the bay mouth silting. In the three sections extending from Hangzhou Bay to the open sea, the inflowing water and sediment of the horizontal section on the north side is decreasing, while the discharged sediment from the south side and the inflowing water and discharged sediment from the vertical section at the east side are increasing.


PeerJ ◽  
2018 ◽  
Vol 6 ◽  
pp. e4173 ◽  
Author(s):  
Cristian B. Canales-Aguirre ◽  
Sandra Ferrada-Fuentes ◽  
Ricardo Galleguillos ◽  
Fernanda X. Oyarzun ◽  
Cristián E. Hernández

Previous studies of population genetic structure inDissostichus eleginoideshave shown that oceanographic and geographic discontinuities drive in this species population differentiation. Studies have focused on the genetics ofD.eleginoidesin the Southern Ocean; however, there is little knowledge of their genetic variation along the South American continental shelf. In this study, we used a panel of six microsatellites to test whetherD.eleginoidesshows population genetic structuring in this region. We hypothesized that this species would show zero or very limited genetic structuring due to the habitat continuity along the South American shelf from Peru in the Pacific Ocean to the Falkland Islands in the Atlantic Ocean. We used Bayesian and traditional analyses to evaluate population genetic structure, and we estimated the number of putative migrants and effective population size. Consistent with our predictions, our results showed no significant genetic structuring among populations of the South American continental shelf but supported two significant and well-defined genetic clusters ofD.eleginoidesbetween regions (South American continental shelf and South Georgia clusters). Genetic connectivity between these two clusters was 11.3% of putative migrants from the South American cluster to the South Georgia Island and 0.7% in the opposite direction. Effective population size was higher in locations from the South American continental shelf as compared with the South Georgia Island. Overall, our results support that the continuity of the deep-sea habitat along the continental shelf and the biological features of the study species are plausible drivers of intraspecific population genetic structuring across the distribution ofD.eleginoideson the South American continental shelf.


2019 ◽  
Vol 60 (5) ◽  
pp. 1115-1128
Author(s):  
Taisir Ghanem Zaki Al Mafraji ◽  
Aiad Ali Hussien Al-Zaidy

The Yamama Formation belongs to the late Berriasian-Aptian succession, which was deposited during the Lower Cretaceous period within the main shallow marine depositional environment. Petrographic study and microfacies analysis enabled the recognition of six main microfacies for three association facies. These are the Semi-restricted, Shallow open marine and Shoal environments. The study succession represents deposition of three third order cycles, these cycles where deposited during successive episodes of relative sea level rises and still stand. The presence of shoal association facies (oolitic packstone microfaces) between the Sulaiy and Yamama formations refer to continue the deposition during the same stage, and may suggest the end of Sulaiy Formation was maximum flooding surface (mfs). The first stage started with occurrence of the shallow open marine association facies underlain by semi-restricted association and then shoal association facies. There are three cycles of this sequence consistently in the south of the study area, so that it continues to the lower part of the Ratawi Formation to be the upper contact of the Yamama Formation of a conformable and continuous in sedimentation To the north of the study area (near of Rf-1 and  Hf-5 wells) the shoal association was only shown once at the bottom of the Yamama Formation and these cycles to became unclear.  This suggest that the paleo-high was developed to the south of studied area, while the open sea was characterized the northern part.


1965 ◽  
Vol S7-VII (3) ◽  
pp. 479-486 ◽  
Author(s):  
Michel Prager

Abstract The Saint-Guiral-Liron granite consists of a porphyritic granodiorite intruded into folded Paleozoic schists of the Cevennes mountains to the north and the Vigan nappe area to the south. The composition of the granodiorite is homogeneous and nearly isotropic. Metamorphism at the northern border of the granodiorite resulted in the formation of gneiss, and at the southern border, of flint. The southern contact indicates extremely intense emplacement with development of an aureole of exothermal contact metamorphism. The joint systems of the northern and southern borders are described and interpreted.


2003 ◽  
Vol 54 (7) ◽  
pp. 833 ◽  
Author(s):  
David Gopurenko ◽  
Jane M. Hughes ◽  
Lynda Bellchambers

Mud crabs (Portunidae; Scylla spp.) have become established recently in some south-west Australian estuaries – almost 1000 km south of their recorded distribution. Colonisation may have occurred by a natural range expansion from the north-west or by translocation from source(s) within the Indo-West Pacific. To identify the species and the potential source population(s), genetic analyses was used to compare south-west crabs (N = 32) to other populations. Levels of diversity at two independent genetic markers were also compared to obtain relative estimates of effective population size between colonist and suspected source population(s). Comparisons of mitochondrial DNA sequences (COI) indicated that all south-west crabs were Scylla serrata. Indeed, the sole haplotype found among colonists was identical to one prevalent but endemic to more diverse north-west Australian populations. In contrast, source and colonist populations had equally high levels of genetic diversity at two microsatellite loci. It is argued that the south-west region was colonised by large numbers of S. serrata from north-west Australia through a recruitment event enhanced by the strong 1999/2000 Leeuwin Current. Differences in diversity among nuclear and mitochondrial loci may reflect different responses to the colonisation process; it is predicted that such differences are prevalent among plankton-dispersed species.


1952 ◽  
Vol 47 ◽  
pp. 171-212 ◽  
Author(s):  
G. E. Bean ◽  
J. M. Cook

‘Their land lies towards the open sea—and this is the part which is called Triopion—but begins at the Bybassian Chersonese; and the whole of the Cnidia except for a little bit is surrounded by water, the part facing the north wind being bounded by the Ceramic Gulf, and that on the south by the sea towards Syme and Rhodes. This little bit, then, which is about five stades across, the Cnidians began to dig while Harpagus was conquering Ionia, with the intention of making their land an island. The whole of it was to lie inside; for where the Cnidian land terminates at the mainland, there is the isthmus which they began to dig’ (Hdt. I 174).The Cnidian peninsula measures 63 km. from base to tip. It consists of two mountain masses joined by an isthmus not much more than 2 km. broad. That on the east is rugged and almost uninhabited; but the greater western massif, though barren and sheer on the north side and at the west tip, has fertile land to offer in the small coastal plains of the south and especially in the valley which traverses the interior from Zeytincik to beyond Yaziköy, with its main outlet below Kumyer and a backdoor at Barkaz. A low ridge runs the length of the isthmus with a gentle slope towards the Gulf of Syme and an easy crossing from Reşadiye to the Ceramic Gulf at Körmen Limani.


Author(s):  
Valeriy Rudenko ◽  
Kateryna Grek

The creative work of Dr. Myron Korduba (1876 - 1947) is revealed in his fundamental geographical research "Territory and population of Ukraine" (1918). The article covers the well-grounded and clearly defined by scientists the boundaries of the ethnographic territory of Ukraine as a whole, as a foundation for establishing the political boundaries of the future Ukrainian state.  Only those counties (which are the primary territorial unit of assessment) where the proportion of Ukrainians exceeds 50% of the total population, or when the Ukryayans in these counties are quantitatively dominant, are the first among other nationalities, are referred to the "continuous Ukrainian ethnographic territory" by Dr. Myron Korduba. The basis for determining the boundaries of "ethnographic Ukraine" by Dr. Myron Korduba was the materials of the all-Russian 1897 population census and a similar population census in Austria-Hungary in 1900. In the ethnographic borders of Ukraine defined by scholars, almost 9/10 of the total territory accounted for "Russian Ukraine", about 8% - for "Austrian", less than 2% - for "Hungarian Ukraine". The population of Ukraine within its ethnographic borders, according to Myron Korduba, in January 1914 amounted to more than 46 million souls, of which 86% lived within Tsarist Russia, about 13% - in "Austrian Ukraine", more than 1% - in "Hungarian Ukraine. ". The ethnic composition of the population of "ethnographic Ukraine": 71.0% - Ukrainians, 11.7% - Great Russians, 8.2% - Jews, 4.5% - Poles, 1.9% - Germans, 0.9% - Volokhs, 1.8% - other nationalities. The most important result of Dr. Myron Korduba's geographical study is the definition of the northern, eastern, southern and western borders of the "continuous Ukrainian territory", the so-called "ethnographic borders of Ukraine". In the north-west, scientists outline them as follows: Brest, Kobrin, Bielsk counties of Grodno province; in the north - Pinsk and the southern part of Mozyr district of Minsk province, then - northeast of Ovruch - the northern border of Kiev province to the Dnieper - then along the Dnieper to the north of its tributary Sozh and the basin of the river Snov. The Great Russian-Ukrainian border stretched: from the upper Snov to the mouth of the Sudota River, which flows into the Desna, then - east along the administrative border between Chernihiv and Orel provinces, then - Ukrainian were Grayvoronsky, Novo-Oskolsky, Putivelsky and the southern part of Sudzhansky district of Kursk. province. In the southern part of the Voronezh province - in Biryuchensky, Bogucharsky, Valuysky, Ostrogodsky and in the south of Pavlovsky counties Ukrainians "live in continuous masses…". Then the border ran along the watershed of the Potudan and Saena rivers to the Don, and in the Don Army Region Ukrainians predominated only in Rostov and Taganrog counties. Myron Korduba referred to the Kuban region, Blagodarensky and Svyatokhrestovsky districts of Stavropol as "continuous Ukrainian territory". "Ethnographic Ukraine" in the south included Berdyansk, Melitopol and Dnieper counties of the Tavriya province, all counties of the Kherson province (except Odessa). In Austria-Hungary, the Ukrainian-Wallachian border ran west from Novoselytsia near Chernivtsi to the Suceava-Zolota Bystritsa River. In Hungary, the Ukrainian ethnographic territory included separate parts of the Maramarosky, Ugotsky, Berezky, Uzhsky, Zemplinsky, Sharyshsky, and Spysky counties. The south-western and western wedges of the Ukrainian ethnic territory were located on the right bank of the Poprad - Hrybiv - Horlytsia - Zhmyhorod - Yasolky - Ivanych - Rymaniv - north of Sanok - upper Xiang - Dinov - stream Rokytnytsia - Sinyava - mouth of Zolota - north to the Russian-Galician . Finally, in the northwest, in the newly formed Kholm province, Ukrainians constituted an absolute majority in Bielsko, Volodavsk, Hrubieszów, and Konstantinów, with an overwhelming majority in Kholm and Zamość counties. Key words: Myron Korduba, ethnographic borders and population of Ukraine.


1941 ◽  
Vol 7 (1) ◽  
pp. 39-47 ◽  
Author(s):  
Doris Stone ◽  
Conchita Turnbull

On the western end of the north coast of Honduras, the outstanding river is the Ulúa, whose basin is formed by the plain of Sula. In the south, the gradually descending steps of the Cordilleras with the open avenues of the Ulúa on the west and her tributaries, the Lindo due south and the Comayagua at the east, bring contact to the wet valley of Sula from the semi-arid interior. Eastward lies the low margin of coast and the lagoons and river systems of the Pijol range. West and southwest is mountain land with an important river valley, the Chamelicon, which merges into the Sula plain. At the north is the open sea, bringing to this region varied influences from many and distant places.


2016 ◽  
Vol 12 (15) ◽  
pp. 365
Author(s):  
Anas Emran ◽  
Fida Medina

Structural study of the recent deformations of the Eç-çour area, located on the southern slope of the massif ancien of the High Atlas, has allowed us to obtain the following results: (1) In the Ait Maghlif plateau, on the northern border of the Siroua volcanic massif, the N-S structures that are bounded by the reverse Imini fault to the north and the left-lateral Tawyalt−Agandiy fault in the south, correspond to forced folds on reverse faults and related folds related to a NW-SE compression, some of which were former normal syndepositional faults that were active in Cretaceous times; an intermediate phase corresponding to a NNE-SSW compression which is thought to have triggered the Siroua volcanism; (2) along de South Atlas Fault, the recent tectonism is expressed by folding and faulting of several Quaternary alluvial fans, some of which bear reverse/dextral slickensides.


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