Hasil untuk "North Germanic. Scandinavian"

S. Jore, S. Vanwambeke, Daniel Slunge et al.

ABSTRACT Tick-borne diseases are emerging and re-emerging threats causing public health concerns in Europe and North America. Prevention and control requires understanding of human exposure and behaviour. The aim was to measure exposure to tick bites across Scandinavia, its spatial distribution and the associated risk factors. Methods We sent a web-based survey to a randomly chosen population and analysed answers by Principal Component Analysis and Chi-Square. Individual responses were aggregated at the municipality level to assess the spatial distribution of bites. Results Nearly 60% of adults reported bites at low levels (1-5 bites); however, the majority were not in their resident municipality. We found two spatial profiles: In their home municipalities, people were most often bitten in less, but not the least, urbanized areas. When visiting other municipalities, people were most frequently bitten in peri-urban areas. Running/walking in the forest, gardening, and paddling/rowing were activities most strongly associated with bites. Conclusion Tick bites affect the entire Scandinavian population, with a higher risk in Sweden compared to Denmark and Norway. The frequency of observation of ticks in the environment or on pets might be used as a proxy for the actual risk of exposure to tick bites. Our results indicates that urban-dwelling outdoor enthusiasts and inhabitants of rural areas must be equally targeted for prevention campaigns.

M. Osadchuk, Svistunov Aa, A. Zolotovitskaya et al.

Ключевые слова: дивертикулярная болезнь толстой кишки, аденоматозные полипы, колоректальный рак, Ki-67, α-SMA Литература/references 1. Lichte Ph., Oberbeck R., Binnebösel М., Wildenauer R., Pape H., Kobbe Ph. A civilian perspective on ballistic trauma and gunshot injuries. Scandinavian Journal of Trauma, Resuscitation and Emergency Medicine. 2010;18:35. https://doi.org/10.1186/1757-7241-18-35 2. Manring M. M., Hawk A., Calhoun J. H., Andersen R. C. Treatment of War Wounds: A Historical Review. Clin. Orthop. Relat. Res. 2009; 467:2168-2191. https://doi.org/10.1007/s11999-009-0738-5 3. Bala M., Gazalla S., Faroja M., Bloom A., Zamir G. [et al.]. Complications of high grade liver injuries: management and outcomewith focus on bile leaks. Scandinavian Journal of Trauma, Resuscitation and Emergency Medicine. 2012;20:20. https://doi.org/10.1186/1757-7241-20-20 4. Гаин Ю. М., Александрова О. С., Гапанович В. Н. Современные методы местного гемостаза при повреждениях паренхиматозных органов живота. Новости хирургии. 2009;4(17):160-170. [Gain Yu. M., Aleksandrova O. S., Gapanovich V. N. Modern methods of local hemostasis in injuries of parenchymal abdominal organs. Novosti khirurgii. – Surgery News. 2009;4(17):160-170. (In Russ.)]. 5. Бабич И. И., Черкасов М. Ф., Шилов Г. Л., Лукаш Ю. В. Особенности патогенеза и хирургического лечения посттравматического панкреатита у детей. Медицинский вестник Северного Кавказа. 2018;13(2):436-440. [Babich I. I., Cherkasov M. F., Shilov G. L., Lukash Yu. V. Pathogenesis and surgical treatment of posttraumatic pancreatitis in children. Meditsinskii vestnik Severnogo Kavkaza. – Medical News of North Caucasus. 2018;13(2):436440. (In Russ.)]. https://doi.org/10.14300/mnnc.2018.13071 6. Feng G., Liu J., Zhao X., Wei J., Ou W. [et al.]. Hemostatic Effects of Microbubble-Enhanced Low-Intensity Ultrasound in a Liver Avulsion Injury Model. PLoS ONE. 2014;9(5):e95589. https://doi.org/10.1371/journal.pone.0095589

D. Zanchettin, C. Timmreck, H. Graf et al.

F. Muschitiello, F. Pausata, J. Watson et al.

Sources and timing of freshwater forcing relative to hydroclimate shifts recorded in Greenland ice cores at the onset of Younger Dryas, ∼12,800 years ago, remain speculative. Here we show that progressive Fennoscandian Ice Sheet (FIS) melting 13,100–12,880 years ago generates a hydroclimate dipole with drier–colder conditions in Northern Europe and wetter–warmer conditions in Greenland. FIS melting culminates 12,880 years ago synchronously with the start of Greenland Stadial 1 and a large-scale hydroclimate transition lasting ∼180 years. Transient climate model simulations forced with FIS freshwater reproduce the initial hydroclimate dipole through sea-ice feedbacks in the Nordic Seas. The transition is attributed to the export of excess sea ice to the subpolar North Atlantic and a subsequent southward shift of the westerly winds. We suggest that North Atlantic hydroclimate sensitivity to FIS freshwater can explain the pace and sign of shifts recorded in Greenland at the climate transition into the Younger Dryas. Resolving the sources and timing of freshwater forcing during the Last Termination is key to evaluate the North Atlantic Ocean response to freshwater perturbations. Here, the authors that the North Atlantic climate system was highly sensitive to Scandinavian meltwater discharge shortly before the Younger Dryas.

R. Howell

D. Gee, P. Andreasson, H. Lorenz et al.

B. Robroek, E. Wubs, M. Martí et al.

A. Clarke

A. Ramos, M. Lorenzo, L. Gimeno

Eva Carding, D. Hirst

E. Rasmussen, C. Heilmann-Clausen, R. Waagstein et al.

This chapter provides a lithostratigraphic correlation and the present knowledge of the depositional history of the Tertiary succession of the Scandinavian countries. The succession records an initial phase of carbonate deposition in the early Paleocene. This was succeeded by deposition of deep marine clays with intercalation of sand-rich mass-flow deposits during most of the Paleocene and Eocene. Volcanic activity in the North Atlantic was extensive at the transition from the Paleocene to the Eocene resulting in widespread sedimentation of ash-rich layers in the North Sea area. During the Oligocene, the first prograding deltaic complex developed, sourced from the Fennoscandian Shield. Late Oligocene‐Early Miocene inversion and uplift of Norway and the Shetland Platform resulted in major progradation of coastal and delta plain systems. At the end of the Tertiary most of the North Sea basin was filled and the Fennoscandian Shield was flanked to the west by a broad, coalesced coastal plain.

A. Westerbergh, A. Saura

D. Bazard, R. Butler, G. Gehrels et al.

I. Nordal, B. Jonsell

J. Haywood

A. Landa, J. Tufto, R. Franzén et al.

R. Essex, L. Gromet

D. Six, L. Reynaud, Anne Letréguilly

M. Nesje, K. Røed, D. Bell et al.

L. Hamberg, G. Dam, C. Wilhelmson et al.