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    In the given article we analyze the representation of the period from the recent history- Socialist Yugoslavia- through the case study of national history museum and private exhibition. Although both of the analyzed objects are located in Ljubljana, the metastories which they construct and display are based on the different cultural patterns. We compare the differences of the narratives being used by the private and state institution and apply the visual analysis method together with semi-structured interviews for these purposes. As a result of our research, we show how differs ‘official narration’ compared to the so-called ‘Yugonostalgic’ or ‘Titostalgic’ viewpoint and describe their main characteristics.

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    Innovative Issues and Approaches in Social Sciences
    Article . 2015 . Peer-reviewed
    License: CC BY NC
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      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ Digitala Vetenskapli...arrow_drop_down
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      Innovative Issues and Approaches in Social Sciences
      Article . 2015 . Peer-reviewed
      License: CC BY NC
      image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
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    Le noyau Borenshult-1, foré à proximité de Motala, à l'est du lac Vättern, dans le centre-sud de la Suède, comprend une succession bien datée et presque complète de carbonates marins marneux déposés relativement près de la terre. Les 34 échantillons de noyau analysés pour la palynologie englobent la partie supérieure du Darriwilian (calcaire de Furudal), l'ensemble du Sandbian (calcaire de Dalby, k-bentonite de Kinnekulle et calcaire de Skagen inférieur) et la partie inférieure du Katian (calcaire de Skagen). L'âge de cet intervalle est bien limité au Darriwilian tardif (tranche de stade Dw3)précoce Katian (Stage slice Ka1), basé sur les conodontes et la datation 206Pb/238U des dépôts de cendres volcaniques. Les échantillons ont produit principalement du phytoplancton marin à parois organiques, principalement des acritarches, avec des chitinozoaires subordonnés, des scolécodontes et des fragments de graptolites. Des palynomorphes terrestres épars, représentés par des cryptospores et des spores triletes, ont également été trouvés dans 23 des échantillons. Un total de 154 espèces d'acritarches correspondant à 53 genres a été identifié, ainsi que de faibles pourcentages de formes anormales (formes teratologiques) d'espèces d'acritarches à certains niveaux. La distribution graphique strati des genres et des espèces a permis trois assemblages palynologiques à distinguer : Assemblage A d'un âge Darriwilien tardif, Assemblage B d'un âge Sandbien (subdivisé en sous-assemblages B1 et B2), et Assemblage C daté comme Katian.Genera tels que Baltisphaeridium, Ordovicidium, Pachysphaeridium et Orthosphaeridum, qui sont communs dans les assemblages de phytoplancton Ordovicien moyen de Baltica, sont bien représentés, avec plusieurs espèces, principalement dans l'Assemblage A et le sous-assemblage B1, jusqu'au Sandbien inférieur.Toutefois, la présence d'une majorité de taxons avec une distribution mondiale soutient le cosmopolitisme des assemblages étudiés, déjà proposé de commencer près de la transition Darriwilian-Sandbian.Notamment, les taxons de phytoplancton avec des affinités siluriennes, précédemment connus de l'Hirnantien, apparaissent pour la première fois dans la partie tardive Darriwilian du noyau de forage Borenshult-1 (Dw3) .Les taxons importants sont Tylotopalla et Metaleiofusa, qui est définitivement établi depuis le début du Sandbian (Ordovicien tardif précoce), ainsi que la première apparition du genre Visbysphaera.Ces événements remettent en question la relation entre l'apparition de morphotypes de phytoplancton pionniers et la glaciation hirnantienne.Autres taxons sans enregistrements pré-siluriens tels que Visbysphaera pirifera subsp.minor, Petaloferidium cazurrum et Dorsennidium cf.D. estrellitae sont ici présents dans le Sandbien, où des lits de bentonite sont intercalés.Le genre Frankea est enregistré pour la première fois chez l'Ordovicien de Suède, suggérant une distribution latitudinale haute à moyenne au lieu d'une distribution périgondwanaise.La plus grande diversité correspond au Darriwilien et en partie aux assemblages de Sandbien, suivie d'un déclin significatif du Katien.Les principaux changements sont observés dans le Sandbien, avec une baisse significative de la diversité, ce qui est probablement lié à une activité volcanique intense ressentie par les lits de bentonite.La diversité ainsi que les taux d'origination et de renouvellement sont les plus bas de l'intervalle portant la suite de K-bentonites, en particulier près de la plus épaisse d'entre elles.La baisse marquée de la diversité dans la partie katienne de la succession, visible à la fois dans les faibles origines et l'abondance, est peut-être liée à une régression au début de la GICE (excursion carbone isotopique de Guttenberg), avec des conditions environnementales et climatiques moins favorables.Les changements dans les assemblages de phytoplancton ainsi que l'apparition de morphologies innovantes d'acritarques ont été précédemment interprétés comme une conséquence de l'environnement et les perturbations climatiques liées à la glaciation de l'Ordovicien. Nous montrons ici que les premières apparitions de ces taxons avancés ont déjà eu lieu environ 15 Ma plus tôt, suggérant qu'une combinaison possible de facteurs tels que les changements du niveau de la mer et le volcanisme a déclenché ces changements, au lieu d'un événement majeur tel que la glaciation hirnantienne. De plus, ces nouvelles découvertes remettent en question les modèles précédents d'évolution et de rayonnement du phytoplancton de l'Ordovicien et font de Baltica un nouveau domaine clé pour la recherche paléogéographique. El núcleo de Borenshult-1, perforado en las proximidades de Motala, al este del lago Vättern en el centro-sur de Suecia, comprende una sucesión bien datada y casi completa de carbonatos marrones marinos depositados relativamente cerca de la tierra. Las 34 muestras de núcleo analizadas para la palinología abarcan la parte superior del Darriwilian (piedra caliza furudal), todo el Sandbian (piedra caliza Dalby, la Kinnekulle K-bentonita y la piedra caliza Skagen inferior) y la parte inferior del Katian (piedra caliza Skagen). La edad de este intervalo está bien restringida al Darriwilian tardío (etapa Dw3)temprano Katian (Stage slice Ka1), basado en conodontes y datación 206Pb/238U de depósitos de ceniza volcánica. Las muestras arrojaron predominantemente fitoplancton de paredes orgánicas marinas, principalmente acritarcos, con quitinozoos subordinados, scolecodontos y fragmentos de graptolitos. También se encontraron palinomorfos terrestres dispersos, representados por criptosporas y esporas triletas, en 23 de las muestras. Se identificaron un total de 154 especies de acritarcos correspondientes a 53 géneros, así como bajos porcentajes de formas anormales (formas teratológicas) de especies de acritarcos en algunos niveles. La distribución gráfica estratigráfica de géneros y especies permitió tres ensamblajes palinológicos. a distinguir: el Ensamblaje A de una edad Darriwiliana tardía, el Ensamblaje B de una edad Sandbiana (subdividido en subensamblajes B1 y B2) y el Ensamblaje C fechado como Katian.Genera como Baltisphaeridium, Ordovicidium, Pachysphaeridium y Orthosphaeridum, que son comunes en los ensamblajes de fitoplancton del Ordovícico Medio de Báltica, están bien representados, con varias especies, principalmente en el Ensamblaje A y el subensamblaje B1, hasta el Sandbiano inferior. Sin embargo, la presencia de una mayoría de taxones con distribución mundial apoya el cosmopolitismo de los ensamblajes estudiados, ya propuesto para comenzar cerca de la transición Darriwilian-Sandbian. Cabe destacar que los taxones de fitoplancton con afinidades silúricas, previamente conocidos del Hirnantiense, aparecen por primera vez en la parte tardía del Darriwiliense del taladro Borenshult-1 (Dw3) .Los taxones importantes que se producen son Tylotopalla y Metaleiofusa, que se establece definitivamente desde el comienzo del Sandbiense (Ordovícico Tardío temprano), junto con la primera aparición del género Visbysphaera. Estas ocurrencias cuestionan la relación entre la aparición de morfotipos de fitoplancton pioneros y la glaciación Hirnantiana. Otros taxones sin registros pre-silúricos como Visbysphaera pirifera subsp.minor, Petaloferidium cazurrum y Dorsennidium cf.D. estrellitae están aquí presentes en el Sandbiano, donde los lechos de bentonita se intercalan. El género Frankea se registra por primera vez en el Ordovícico de Suecia, lo que sugiere una distribución latitudinal alta a media en lugar de una distribución peri-Gondwana. La mayor diversidad corresponde al Darriwiliano y en parte a los conjuntos Sandbianos, seguido de una disminución significativa en el Katiano. Los principales cambios se observan en el Sandbiano, con una caída significativa en la diversidad, que probablemente esté relacionado con la intensa actividad volcánica resentida por los lechos de bentonita. La diversidad, así como las tasas de originación y rotación, son las más bajas en el intervalo que soporta el conjunto de bentonitas K, particularmente cerca de las más gruesas. La marcada caída en la diversidad en la parte katiana de la sucesión, visible tanto en bajas originaciones como en abundancia, posiblemente esté relacionada con una regresión al inicio del GICE (excursión de carbono isotópica de Guttenberg), con condiciones ambientales y climáticas menos favorables. Los cambios en los ensamblajes de fitoplancton junto con el inicio de morfologías innovadoras de acritarcos se interpretaron previamente como consecuencia de la y las perturbaciones climáticas relacionadas con la glaciación del Ordovícico. Aquí mostramos que las primeras apariciones de estos taxones avanzados ya ocurrieron hace unos 15 Ma, lo que sugiere que una posible combinación de factores como los cambios en el nivel del mar y el vulcanismo desencadenaron estos cambios, en lugar de un evento importante como la glaciación de Hirnantian. Además, estos nuevos hallazgos desafían los modelos anteriores de evolución y radiación del fitoplancton del Ordovícico y establecen a Baltica como una nueva área clave para la investigación paleogeográfica. The Borenshult-1 core, drilled in the vicinity of Motala, east of Lake Vättern in south central Sweden, comprises a well-dated and nearly complete succession of marine marly carbonates deposited relatively close to land.The 34 core samples analyzed for palynology encompass the upper part of the Darriwilian (Furudal Limestone), the entire Sandbian (Dalby Limestone, the Kinnekulle K-bentonite and the lower Skagen Limestone) and the lower part of the Katian (Skagen Limestone).The age of this interval is well-constrained to the late Darriwilian (Stage slice Dw3)early Katian (Stage slice Ka1), based on conodonts and 206Pb/238U dating of volcanic ash deposits.The samples yielded predominantly marine organic-walled phytoplankton, mainly acritarchs, with subordinate chitinozoans, scolecodonts and fragments of graptolites.Sparse terrestrial palynomorphs, represented by cryptospores and trilete spores, were also found in 23 of the samples.A total of 154 acritarch species corresponding to 53 genera were identified, as well as low percentages of abnormal forms (teratological forms) of acritarch species at some levels.The strati graphic distribution of genera and species allowed for three palynological assemblages to be distinguished: Assemblage A of a late Darriwilian age, Assemblage B of a Sandbian age (further subdivided into sub-assemblages B1 and B2), and Assemblage C dated as Katian.Genera such as Baltisphaeridium, Ordovicidium, Pachysphaeridium and Orthosphaeridum, which are common in Middle Ordovician phytoplankton assemblages from Baltica, are well represented, with several species, mainly in Assemblage A and sub-assemblage B1, up to the lower Sandbian.However, the presence of a majority of taxa with worldwide distribution supports the cosmopolitanism of the studied assemblages, already proposed to begin near the Darriwilian-Sandbian transition.Notably, phytoplankton taxa with Silurian affinities, previously known from the Hirnantian, appear for the first time in the late Darriwilian part of the Borenshult-1 drillcore (Dw3).Important taxa occurring are Tylotopalla and Metaleiofusa, which is definitively established from the beginning of the Sandbian (early Late Ordovician), together with the first appearance of the genus Visbysphaera.These occurrences question the relationship between the appearance of pioneering phytoplankton morphotypes and the Hirnantian glaciation.Other taxa with no pre-Silurian records such as Visbysphaera pirifera subsp.minor, Petaloferidium cazurrum and Dorsennidium cf.D. estrellitae are here present in the Sandbian, where bentonite beds are intercalated.The genus Frankea is recorded for the first time from the Ordovician of Sweden, suggesting a high to middle latitudinal distribution instead of a peri-Gondwanan distribution.The highest diversity corresponds to the Darriwilian and partly to the Sandbian assemblages, followed by a significant decline in the Katian.The main changes are observed in the Sandbian, with a significant drop in diversity, which is probably related to intense volcanic activity rep resented by the bentonite beds.Diversity as well as origination and turnover rates are the lowest in the interval bearing the suite of K-bentonites, particularly near the thickest of them.The marked drop in diversity in the Katian part of the succession, visible in both low originations and abundance, is possibly related to a regression at the onset of the GICE (Guttenberg isotope carbon excursion), with less favorable environmental and climatic conditions.Changes in phytoplankton assemblages together with the onset of innovative morphologies of acritarchs were previously interpreted as a consequence of environmental and climatic perturbations related to the Ordovician glaciation.Here we show that the first appearances of these advanced taxa already occurred ca 15 Ma earlier, suggesting that a possible combination of factors such as sea level changes and volcanism triggered these changes, instead of a major event such as the Hirnantian glaciation.Additionally, these new findings challenge previous models of evolution and radiation of the Ordovician phytoplankton and set up Baltica as a new key area for paleogeographical research. يشتمل قلب Borenshult -1، الذي تم حفره بالقرب من Motala، شرق بحيرة Vättern في جنوب وسط السويد، على تعاقب جيد وكامل تقريبًا من كربونات المارلي البحرية المودعة بالقرب من الأرض نسبيًا. وتشمل العينات الأساسية الـ 34 التي تم تحليلها لعلم الحفريات الجزء العلوي من Darriwilian (الحجر الجيري الفروي)، و Sandbian بأكمله (Dalby Limestone، و Kinnekulle K - bentonite و Skagen Limestone السفلي) والجزء السفلي من Katian (Skagen Limestone). عمر هذه الفترة مقيد جيدًا بالراحل Darriwilian (شريحة Stage Dw3) في وقت مبكر كاتيان (شريحة المرحلة Ka1)، استنادًا إلى المخروطيات و 206Pb/238U التي يرجع تاريخها إلى رواسب الرماد البركاني. أسفرت العينات في الغالب عن العوالق النباتية البحرية ذات الجدران العضوية، وخاصة أكريتاركس، مع الكيتينوزانات التابعة، والسكولودونات وشظايا الجريبتوليت. كما تم العثور على أشكال أرضية متباينة، ممثلة في أبواغ خفية وأبواغ ثلاثية، في 23 من العينات. تم تحديد ما مجموعه 154 نوعًا من أنواع النرجسية المقابلة لـ 53 جنسًا، بالإضافة إلى نسب مئوية منخفضة من الأشكال غير الطبيعية (الأشكال المسخية) لأنواع النرجسية على بعض المستويات. سمح التوزيع الرسومي الطبقي للأجناس والأنواع بثلاثة تجمعات حركية ليتم تمييزها: التجميع أ في أواخر العصر الدارويلي، التجميع ب في العصر الرملي (مقسم أيضًا إلى تجميعات فرعية B1 و B2)، والتجميع ج المؤرخ بالكاتية .الجنس مثل Baltisphaeridium و Ordovicidium و Pachysphaeridium و Orthosphaeridum، وهي شائعة في تجمعات العوالق النباتية الأوردوفية الوسطى من Baltica، ممثلة تمثيلاً جيدًا، مع العديد من الأنواع، بشكل رئيسي في التجميع أ والتجميع الفرعي B1، حتى Sandbian السفلي. ومع ذلك، فإن وجود غالبية الأصناف ذات التوزيع العالمي يدعم عالمية التجمعات المدروسة، تم اقتراحها بالفعل للبدء بالقرب من التحول الداريويلي- الساندبي. بشكل ملحوظ، تظهر أصناف العوالق النباتية ذات الانتماءات السيلورية، والمعروفة سابقًا من الهيرنانتية، لأول مرة في الجزء الداريويلي المتأخر من النواة الحفرية بورنشولت-1 (Dw3). والأصناف الهامة التي تحدث هي تايلوتوبالا وميتاليوفوسا، والتي تم تأسيسها بشكل نهائي من بداية الساندبيان (الأوردوفيشي المتأخر المبكر)، إلى جانب الظهور الأول لجنس Visbysphaera.The these occurrences question the relationship between the appearance of pioneering phytoplankton morphotypes and the Hirnantian glaciation.Other taxa with no pre - Silurian records such as Visbysphaera pirifera sub.minor, Petaloferidium cazurrum and Dorsennidium cf.D. estrellitae موجودة هنا في Sandbian، حيث يتم إقحام أسرة البنتونيت. يتم تسجيل جنس Frankea لأول مرة من الأوردوفيشي السويدي، مما يشير إلى توزيع خط العرض العالي إلى المتوسط بدلاً من توزيع شبه جندواني. يتوافق أعلى تنوع مع Darriwilian وجزئيًا مع تجمعات Sandbian، يليه انخفاض كبير في Katian. لوحظت التغييرات الرئيسية في Sandbian، مع انخفاض كبير في التنوع، والذي ربما يكون مرتبطًا بممثل النشاط البركاني المكثف المستاء من طبقات البنتونيت. التنوع وكذلك معدلات المنشأ والدوران هي الأدنى في الفترة التي تحمل مجموعة البنتونيت K، خاصة بالقرب من سمكه. من المحتمل أن يكون الانخفاض الملحوظ في التنوع في الجزء الكاتاني من الخلافة، المرئي في كل من المنشأ المنخفض والوفرة، مرتبطًا بالانحدار في بداية GICE (رحلة الكربون بنظائر Guttenberg)، مع ظروف بيئية ومناخية أقل ملاءمة. تم تفسير التغيرات في تجمعات العوالق النباتية جنبًا إلى جنب مع بداية المورفولوجيات المبتكرة للنرجس الصخري سابقًا كنتيجة للظروف البيئية والاضطرابات المناخية المتعلقة بالتجلد الأوردوفيشي. هنا نظهر أن المظاهر الأولى لهذه الأصناف المتقدمة حدثت بالفعل قبل 15 مليون سنة مضت، مما يشير إلى أن مجموعة محتملة من العوامل مثل تغيرات مستوى سطح البحر والبراكين تسببت في هذه التغييرات، بدلاً من حدث كبير مثل التجلد الهيرنانتي. بالإضافة إلى ذلك، تتحدى هذه النتائج الجديدة النماذج السابقة لتطور وإشعاع العوالق النباتية الأوردوفيشية وتضع البلطيقا كمنطقة رئيسية جديدة للبحث في الجغرافيا القديمة.

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    Estonian Journal of Earth Sciences
    Article . 2023 . Peer-reviewed
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    https://doi.org/10.60692/hkf88...
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      Estonian Journal of Earth Sciences
      Article . 2023 . Peer-reviewed
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      https://doi.org/10.60692/hkf88...
      Other literature type . 2023
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      https://doi.org/10.60692/vnwz5...
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    Authors: Overud, Johanna;

    This article considers colonial rhetoric manifested in representations of early settlement in the mining town of Kiruna in northernmost Sweden. Kiruna was founded more than 100 years ago by the LKAB Company with its centre the prosperous mine on Sami land. Continued iron ore mining has made it necessary to relocate the town centre a few kilometres north-east of its original location to ensure the safety of the people. The ongoing process of the town’s transformation due to industrial expansion has given rise to the creation of a memorial park between the town and the mine, in which two historical photographs have been erected on huge concrete blocks. For the Swedish Sami, the indigenous people, the transformation means further exploitation of their reindeer grazing lands and forced adaption to industrial expansion. The historical photographs in the memorial park fit into narratives of colonial expansion and exploration that represent the town’s colonial past. Both pictures are connected to colonial, racialised and gendered space during the early days of industrial colonialism. The context has been set by discussions about what Kiruna “is”, and how it originated. My aim is to study the role of collective memory in mediating a colonial past, by exploring the representations that are connected to and evoked by these pictures. In this progressive transformation of the town, what do these photographic memorials represent in relation to space? What are the values made visible in these photographs? I also discuss the ways in which Kiruna’s history becomes manifested in the town’s transformation and the use of history in urban planning. I argue that, in addressing the colonial history of Kiruna, it is timely to reconsider how memories of a town are communicated into the future by references to the past. I also claim that memory, history, and remembrance and forgetting are represented in this process of history-making and that they intersect gender, class and ethnicity.

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    Culture Unbound: Journal of Current Cultural Research
    Article . 2019 . Peer-reviewed
    License: CC BY NC
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      Culture Unbound: Journal of Current Cultural Research
      Article . 2019 . Peer-reviewed
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    Authors: Andrej Kotljarchuk;

    AbstractThousands of Roma were killed in Ukraine by the Nazis and auxiliary police on the spot. There are more than 50,000 Roma in today’s Ukraine, represented by second and third generation decendants of the genocide survivors. The discussion on Roma identity cannot be isolated from the memory of the genocide, which makes the struggle over the past a reflexive landmark that mobilizes the Roma movement. About twenty Roma genocide memorials have been erected in Ukraine during last decade, and in 2016 the national memorial of the Roma genocide was opened in Babi Yar. However, scholars do not have a clear picture of memory narratives and memory practices of the Roma genocide in Ukraine. A comprehensive analysis of the contemporary situation is not possible without an examination of the history and memory of the Roma genocide before 1991.

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    Nationalities Papers
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    Nationalities Papers
    Article . 2021 . Peer-reviewed
    License: CC BY
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      Nationalities Papers
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      Nationalities Papers
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    Authors: Liljas, Juvas Marianne;

    ”A new form of musical upbringing”: Pretenses of reform pedagogy content in the Siljan schoolIn this article, I describe the Siljan school in Tällberg as a Swedish example of alternative pedagogy. The overall questions relate to the reform pedagogy content of the school and its ability to give Swedish music teaching a new form of musical upbringing. An important issue is how the Siljan school as a model for Swedish reform has been inspired by the reform pedagogy movements in USA and Germany. The analysis is thus based on the Alm couple’s ability to give the school an international character which shines light on Swedish reforms in the greater context of reform pedagogy. With its basis in discursive education of the 1930s, two main questions are discussed: what perspective on musical education can be identified in the personal development ethos of the Siljan school? How can the school’s relation to the reform pedagogy music movement during the start of the 1900s be understood? From a hermeneutic perspective, the article contributes by investigating how the Siljan school can have affected decisions in education politics, Swedish schooling, and Swedish musical life. In summary, the article contributes with new knowledge on a chapter in the history of Swedish music pedagogy.

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    Nordic Journal of Educational History
    Article . 2016 . Peer-reviewed
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    Nordic Journal of Educational History
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      Nordic Journal of Educational History
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    Authors: Prytz, Johan;

    The aim of this paper is to revise a standard narrative about governance of the Swedish school system in the period of 1910-1908. According to this narrative, the Swedish school system was centralized during this period. However, this narrative does not fit the history of Swedish mathematics education (years 7-9). The research questions are: where in the school system was change initiated and how was change enforced? On the basis of studies of syllabi, textbooks, teaching literature, teacher journals and reports from investigations and development projects, different modes of governance of school mathematics are identified. The main results are that textbook producers rather than national syllabi and exams were drivers of change in the period 1910-1960. Moreover, the centralized attempts to change school mathematics, prepared in the 1960s, were soon abandoned in the early 1970s. Thus, centralized governance of Swedish school mathematics, with the ambition to achieve change, was something that took effect relatively late and during a very short period of time.

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    Espacio, Tiempo y Educación
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    Espacio, Tiempo y Educación
    Article . 2017
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    Espacio, Tiempo y Educación
    Article . 2017 . Peer-reviewed
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      Espacio, Tiempo y Educación
      Article . 2017
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      Espacio, Tiempo y Educación
      Article . 2017 . Peer-reviewed
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    Authors: Sundin, Jan;

    ‘Public health’ investigates the determinants of health, born during the Enlightenment in the seventeenth/eighteenth century. But ‘public health’ is also policies, aiming at the improvement of a population’s health. There is a mutual interchange between public health as science and as politics. A brief historical background is followed by an analysis of the impacts of political changes during the first two decades of the twenty first century in Sweden. In 2005, a policy document accepted by all political parties except for the Moderate Party highlighted socio-economic factors and structural reforms to decrease the health gaps in the population. The general election in September 2006 resulted in a new majority in the parliament and a center-right coalition government, including the Moderates and three parties that had approved of the 2005 document. In 2007 a “new public health policy” was introduced. Its priority lists stressed individual behavior and the new policy should be incentives to work instead of “allowances”. The Public Health Institute got instructions in accordance with the new policy. The ten years following this policy change has seen public health policies and attitudes to research shifting almost year by year. The new policy met a counter-stream from the very beginning. Influenced by Michael Marmot’s WHO Commission on health inequalities, regional commissions started in Sweden, Recommendations how to decrease social health gaps was adopted with almost no opposition by regional health boards in 2012–2013. But new problems were now occupying politicians and media—how to finance the growth of the old, multi-sick part of the population and increasing costs for new medical technologies and drugs. Public health as an academic discipline was in the middle of this fluctuating political landscape with direct effects on what has been considered worth listening to or support by public money.

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    Article . 2019 . Peer-reviewed
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    Authors: Josephson, Peter; Lundgren, Frans;
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  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/
    Authors: Weronika Axelsson Linkowski; Marie Kvarnström; Anna Westin; Jon Moen; +1 Authors

    During the twenty-first century, large carnivores have increased in human dominated landscapes after being extinct or nearly extinct. This has resulted in increasing numbers of livestock killed by large carnivores. The intent of this paper is to give a land use-historical perspective on the recent livestock–carnivore conflict in boreal Sweden. More specifically we address: (1) depredation risks (livestock killed by carnivores) and (2) local knowledge of how to protect livestock from predation and whether it survived among pastoralists until the present. This study provides numeric information on carnivores, livestock and depredation, combined with oral information from summer farmers about livestock protection. We compare recent (since 1998) and historical (late nineteenth century) depredation rates in two Swedish counties. In Dalarna recent depredation rates are higher than historical rates while the opposite pattern is seen in Jämtland. Recent depredation rates in Dalarna are twice the recent rates in Jämtland, in contrast to the historical situation. Recent and historical depredation rates are of the same order. Summer farmers traditionally graze their livestock in forested areas where carnivores reside. Interviews show that traditional knowledge of how to protect livestock from carnivores was lost during the twentieth century, but recently new knowledge has developed leading to changes in summer farming practices. The carnivore–livestock situation today differs from the historical situation, not so much in levels of depredation, but mainly regarding the possibilities of farmers to face challenges associated with increasing carnivore populations.

    image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/ Epsilon Open Archivearrow_drop_down
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    Article . 2017
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    Authors: Emma Nilsing Strid; Frida Gustafson; Anneli Peolsson; Anna Hermansen;

    Objective Neck-specific exercises for individuals with chronic whiplash-associated disorders (WAD) have shown promising results, but there is also a need for more efficient and flexible ways of rehabilitation, such as use of digital health tools. Understanding physiotherapists’ experiences of an internet-based tool may help to improve digital tools within physiotherapy. The purpose of this study was to describe how physiotherapists’ experience an internet-based neck-specific exercise program for patients with chronic WAD. Methods This study has a qualitative design. Focus group discussions were held with physiotherapists who have been treating patients with chronic WAD, using an internet-based neck-specific exercises program in a randomized controlled multi-center trial in south and central Sweden. Three focus groups were held with three participants in each group. Phenomenography was applied as a research approach for data analysis. Results One main category was identified as “internet-based program as a complement to regular rehabilitation,” with five descriptive sub-categories: (a) support in patient work; (b) usefulness based on a patient's prerequisites and preferences; (c) physiotherapist and patient interaction; (d) increasing efficiency in rehabilitation; and (e) enabling patient participation, autonomy and self-management. Conclusions From a physiotherapy perspective, an internet-based program could work as a method of complementary support to the standard rehabilitation treatment for patients with chronic WAD, as long as it is interactive and adjustable to the individual. The internet-based program could lead to increased autonomy and self-efficacy, and save resources and time for physiotherapists and patients. Further, more research is needed to strengthen these digital tools within the healthcare system.

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    Digital Health
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    Digital Health
    Article . 2022
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    Digital Health; PubMed Central
    Article . Other literature type . 2023 . Peer-reviewed
    License: CC BY NC
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      Digital Health
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  • image/svg+xml art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos Open Access logo, converted into svg, designed by PLoS. This version with transparent background. http://commons.wikimedia.org/wiki/File:Open_Access_logo_PLoS_white.svg art designer at PLoS, modified by Wikipedia users Nina, Beao, JakobVoss, and AnonMoos http://www.plos.org/

    In the given article we analyze the representation of the period from the recent history- Socialist Yugoslavia- through the case study of national history museum and private exhibition. Although both of the analyzed objects are located in Ljubljana, the metastories which they construct and display are based on the different cultural patterns. We compare the differences of the narratives being used by the private and state institution and apply the visual analysis method together with semi-structured interviews for these purposes. As a result of our research, we show how differs ‘official narration’ compared to the so-called ‘Yugonostalgic’ or ‘Titostalgic’ viewpoint and describe their main characteristics.

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    Le noyau Borenshult-1, foré à proximité de Motala, à l'est du lac Vättern, dans le centre-sud de la Suède, comprend une succession bien datée et presque complète de carbonates marins marneux déposés relativement près de la terre. Les 34 échantillons de noyau analysés pour la palynologie englobent la partie supérieure du Darriwilian (calcaire de Furudal), l'ensemble du Sandbian (calcaire de Dalby, k-bentonite de Kinnekulle et calcaire de Skagen inférieur) et la partie inférieure du Katian (calcaire de Skagen). L'âge de cet intervalle est bien limité au Darriwilian tardif (tranche de stade Dw3)précoce Katian (Stage slice Ka1), basé sur les conodontes et la datation 206Pb/238U des dépôts de cendres volcaniques. Les échantillons ont produit principalement du phytoplancton marin à parois organiques, principalement des acritarches, avec des chitinozoaires subordonnés, des scolécodontes et des fragments de graptolites. Des palynomorphes terrestres épars, représentés par des cryptospores et des spores triletes, ont également été trouvés dans 23 des échantillons. Un total de 154 espèces d'acritarches correspondant à 53 genres a été identifié, ainsi que de faibles pourcentages de formes anormales (formes teratologiques) d'espèces d'acritarches à certains niveaux. La distribution graphique strati des genres et des espèces a permis trois assemblages palynologiques à distinguer : Assemblage A d'un âge Darriwilien tardif, Assemblage B d'un âge Sandbien (subdivisé en sous-assemblages B1 et B2), et Assemblage C daté comme Katian.Genera tels que Baltisphaeridium, Ordovicidium, Pachysphaeridium et Orthosphaeridum, qui sont communs dans les assemblages de phytoplancton Ordovicien moyen de Baltica, sont bien représentés, avec plusieurs espèces, principalement dans l'Assemblage A et le sous-assemblage B1, jusqu'au Sandbien inférieur.Toutefois, la présence d'une majorité de taxons avec une distribution mondiale soutient le cosmopolitisme des assemblages étudiés, déjà proposé de commencer près de la transition Darriwilian-Sandbian.Notamment, les taxons de phytoplancton avec des affinités siluriennes, précédemment connus de l'Hirnantien, apparaissent pour la première fois dans la partie tardive Darriwilian du noyau de forage Borenshult-1 (Dw3) .Les taxons importants sont Tylotopalla et Metaleiofusa, qui est définitivement établi depuis le début du Sandbian (Ordovicien tardif précoce), ainsi que la première apparition du genre Visbysphaera.Ces événements remettent en question la relation entre l'apparition de morphotypes de phytoplancton pionniers et la glaciation hirnantienne.Autres taxons sans enregistrements pré-siluriens tels que Visbysphaera pirifera subsp.minor, Petaloferidium cazurrum et Dorsennidium cf.D. estrellitae sont ici présents dans le Sandbien, où des lits de bentonite sont intercalés.Le genre Frankea est enregistré pour la première fois chez l'Ordovicien de Suède, suggérant une distribution latitudinale haute à moyenne au lieu d'une distribution périgondwanaise.La plus grande diversité correspond au Darriwilien et en partie aux assemblages de Sandbien, suivie d'un déclin significatif du Katien.Les principaux changements sont observés dans le Sandbien, avec une baisse significative de la diversité, ce qui est probablement lié à une activité volcanique intense ressentie par les lits de bentonite.La diversité ainsi que les taux d'origination et de renouvellement sont les plus bas de l'intervalle portant la suite de K-bentonites, en particulier près de la plus épaisse d'entre elles.La baisse marquée de la diversité dans la partie katienne de la succession, visible à la fois dans les faibles origines et l'abondance, est peut-être liée à une régression au début de la GICE (excursion carbone isotopique de Guttenberg), avec des conditions environnementales et climatiques moins favorables.Les changements dans les assemblages de phytoplancton ainsi que l'apparition de morphologies innovantes d'acritarques ont été précédemment interprétés comme une conséquence de l'environnement et les perturbations climatiques liées à la glaciation de l'Ordovicien. Nous montrons ici que les premières apparitions de ces taxons avancés ont déjà eu lieu environ 15 Ma plus tôt, suggérant qu'une combinaison possible de facteurs tels que les changements du niveau de la mer et le volcanisme a déclenché ces changements, au lieu d'un événement majeur tel que la glaciation hirnantienne. De plus, ces nouvelles découvertes remettent en question les modèles précédents d'évolution et de rayonnement du phytoplancton de l'Ordovicien et font de Baltica un nouveau domaine clé pour la recherche paléogéographique. El núcleo de Borenshult-1, perforado en las proximidades de Motala, al este del lago Vättern en el centro-sur de Suecia, comprende una sucesión bien datada y casi completa de carbonatos marrones marinos depositados relativamente cerca de la tierra. Las 34 muestras de núcleo analizadas para la palinología abarcan la parte superior del Darriwilian (piedra caliza furudal), todo el Sandbian (piedra caliza Dalby, la Kinnekulle K-bentonita y la piedra caliza Skagen inferior) y la parte inferior del Katian (piedra caliza Skagen). La edad de este intervalo está bien restringida al Darriwilian tardío (etapa Dw3)temprano Katian (Stage slice Ka1), basado en conodontes y datación 206Pb/238U de depósitos de ceniza volcánica. Las muestras arrojaron predominantemente fitoplancton de paredes orgánicas marinas, principalmente acritarcos, con quitinozoos subordinados, scolecodontos y fragmentos de graptolitos. También se encontraron palinomorfos terrestres dispersos, representados por criptosporas y esporas triletas, en 23 de las muestras. Se identificaron un total de 154 especies de acritarcos correspondientes a 53 géneros, así como bajos porcentajes de formas anormales (formas teratológicas) de especies de acritarcos en algunos niveles. La distribución gráfica estratigráfica de géneros y especies permitió tres ensamblajes palinológicos. a distinguir: el Ensamblaje A de una edad Darriwiliana tardía, el Ensamblaje B de una edad Sandbiana (subdividido en subensamblajes B1 y B2) y el Ensamblaje C fechado como Katian.Genera como Baltisphaeridium, Ordovicidium, Pachysphaeridium y Orthosphaeridum, que son comunes en los ensamblajes de fitoplancton del Ordovícico Medio de Báltica, están bien representados, con varias especies, principalmente en el Ensamblaje A y el subensamblaje B1, hasta el Sandbiano inferior. Sin embargo, la presencia de una mayoría de taxones con distribución mundial apoya el cosmopolitismo de los ensamblajes estudiados, ya propuesto para comenzar cerca de la transición Darriwilian-Sandbian. Cabe destacar que los taxones de fitoplancton con afinidades silúricas, previamente conocidos del Hirnantiense, aparecen por primera vez en la parte tardía del Darriwiliense del taladro Borenshult-1 (Dw3) .Los taxones importantes que se producen son Tylotopalla y Metaleiofusa, que se establece definitivamente desde el comienzo del Sandbiense (Ordovícico Tardío temprano), junto con la primera aparición del género Visbysphaera. Estas ocurrencias cuestionan la relación entre la aparición de morfotipos de fitoplancton pioneros y la glaciación Hirnantiana. Otros taxones sin registros pre-silúricos como Visbysphaera pirifera subsp.minor, Petaloferidium cazurrum y Dorsennidium cf.D. estrellitae están aquí presentes en el Sandbiano, donde los lechos de bentonita se intercalan. El género Frankea se registra por primera vez en el Ordovícico de Suecia, lo que sugiere una distribución latitudinal alta a media en lugar de una distribución peri-Gondwana. La mayor diversidad corresponde al Darriwiliano y en parte a los conjuntos Sandbianos, seguido de una disminución significativa en el Katiano. Los principales cambios se observan en el Sandbiano, con una caída significativa en la diversidad, que probablemente esté relacionado con la intensa actividad volcánica resentida por los lechos de bentonita. La diversidad, así como las tasas de originación y rotación, son las más bajas en el intervalo que soporta el conjunto de bentonitas K, particularmente cerca de las más gruesas. La marcada caída en la diversidad en la parte katiana de la sucesión, visible tanto en bajas originaciones como en abundancia, posiblemente esté relacionada con una regresión al inicio del GICE (excursión de carbono isotópica de Guttenberg), con condiciones ambientales y climáticas menos favorables. Los cambios en los ensamblajes de fitoplancton junto con el inicio de morfologías innovadoras de acritarcos se interpretaron previamente como consecuencia de la y las perturbaciones climáticas relacionadas con la glaciación del Ordovícico. Aquí mostramos que las primeras apariciones de estos taxones avanzados ya ocurrieron hace unos 15 Ma, lo que sugiere que una posible combinación de factores como los cambios en el nivel del mar y el vulcanismo desencadenaron estos cambios, en lugar de un evento importante como la glaciación de Hirnantian. Además, estos nuevos hallazgos desafían los modelos anteriores de evolución y radiación del fitoplancton del Ordovícico y establecen a Baltica como una nueva área clave para la investigación paleogeográfica. The Borenshult-1 core, drilled in the vicinity of Motala, east of Lake Vättern in south central Sweden, comprises a well-dated and nearly complete succession of marine marly carbonates deposited relatively close to land.The 34 core samples analyzed for palynology encompass the upper part of the Darriwilian (Furudal Limestone), the entire Sandbian (Dalby Limestone, the Kinnekulle K-bentonite and the lower Skagen Limestone) and the lower part of the Katian (Skagen Limestone).The age of this interval is well-constrained to the late Darriwilian (Stage slice Dw3)early Katian (Stage slice Ka1), based on conodonts and 206Pb/238U dating of volcanic ash deposits.The samples yielded predominantly marine organic-walled phytoplankton, mainly acritarchs, with subordinate chitinozoans, scolecodonts and fragments of graptolites.Sparse terrestrial palynomorphs, represented by cryptospores and trilete spores, were also found in 23 of the samples.A total of 154 acritarch species corresponding to 53 genera were identified, as well as low percentages of abnormal forms (teratological forms) of acritarch species at some levels.The strati graphic distribution of genera and species allowed for three palynological assemblages to be distinguished: Assemblage A of a late Darriwilian age, Assemblage B of a Sandbian age (further subdivided into sub-assemblages B1 and B2), and Assemblage C dated as Katian.Genera such as Baltisphaeridium, Ordovicidium, Pachysphaeridium and Orthosphaeridum, which are common in Middle Ordovician phytoplankton assemblages from Baltica, are well represented, with several species, mainly in Assemblage A and sub-assemblage B1, up to the lower Sandbian.However, the presence of a majority of taxa with worldwide distribution supports the cosmopolitanism of the studied assemblages, already proposed to begin near the Darriwilian-Sandbian transition.Notably, phytoplankton taxa with Silurian affinities, previously known from the Hirnantian, appear for the first time in the late Darriwilian part of the Borenshult-1 drillcore (Dw3).Important taxa occurring are Tylotopalla and Metaleiofusa, which is definitively established from the beginning of the Sandbian (early Late Ordovician), together with the first appearance of the genus Visbysphaera.These occurrences question the relationship between the appearance of pioneering phytoplankton morphotypes and the Hirnantian glaciation.Other taxa with no pre-Silurian records such as Visbysphaera pirifera subsp.minor, Petaloferidium cazurrum and Dorsennidium cf.D. estrellitae are here present in the Sandbian, where bentonite beds are intercalated.The genus Frankea is recorded for the first time from the Ordovician of Sweden, suggesting a high to middle latitudinal distribution instead of a peri-Gondwanan distribution.The highest diversity corresponds to the Darriwilian and partly to the Sandbian assemblages, followed by a significant decline in the Katian.The main changes are observed in the Sandbian, with a significant drop in diversity, which is probably related to intense volcanic activity rep resented by the bentonite beds.Diversity as well as origination and turnover rates are the lowest in the interval bearing the suite of K-bentonites, particularly near the thickest of them.The marked drop in diversity in the Katian part of the succession, visible in both low originations and abundance, is possibly related to a regression at the onset of the GICE (Guttenberg isotope carbon excursion), with less favorable environmental and climatic conditions.Changes in phytoplankton assemblages together with the onset of innovative morphologies of acritarchs were previously interpreted as a consequence of environmental and climatic perturbations related to the Ordovician glaciation.Here we show that the first appearances of these advanced taxa already occurred ca 15 Ma earlier, suggesting that a possible combination of factors such as sea level changes and volcanism triggered these changes, instead of a major event such as the Hirnantian glaciation.Additionally, these new findings challenge previous models of evolution and radiation of the Ordovician phytoplankton and set up Baltica as a new key area for paleogeographical research. يشتمل قلب Borenshult -1، الذي تم حفره بالقرب من Motala، شرق بحيرة Vättern في جنوب وسط السويد، على تعاقب جيد وكامل تقريبًا من كربونات المارلي البحرية المودعة بالقرب من الأرض نسبيًا. وتشمل العينات الأساسية الـ 34 التي تم تحليلها لعلم الحفريات الجزء العلوي من Darriwilian (الحجر الجيري الفروي)، و Sandbian بأكمله (Dalby Limestone، و Kinnekulle K - bentonite و Skagen Limestone السفلي) والجزء السفلي من Katian (Skagen Limestone). عمر هذه الفترة مقيد جيدًا بالراحل Darriwilian (شريحة Stage Dw3) في وقت مبكر كاتيان (شريحة المرحلة Ka1)، استنادًا إلى المخروطيات و 206Pb/238U التي يرجع تاريخها إلى رواسب الرماد البركاني. أسفرت العينات في الغالب عن العوالق النباتية البحرية ذات الجدران العضوية، وخاصة أكريتاركس، مع الكيتينوزانات التابعة، والسكولودونات وشظايا الجريبتوليت. كما تم العثور على أشكال أرضية متباينة، ممثلة في أبواغ خفية وأبواغ ثلاثية، في 23 من العينات. تم تحديد ما مجموعه 154 نوعًا من أنواع النرجسية المقابلة لـ 53 جنسًا، بالإضافة إلى نسب مئوية منخفضة من الأشكال غير الطبيعية (الأشكال المسخية) لأنواع النرجسية على بعض المستويات. سمح التوزيع الرسومي الطبقي للأجناس والأنواع بثلاثة تجمعات حركية ليتم تمييزها: التجميع أ في أواخر العصر الدارويلي، التجميع ب في العصر الرملي (مقسم أيضًا إلى تجميعات فرعية B1 و B2)، والتجميع ج المؤرخ بالكاتية .الجنس مثل Baltisphaeridium و Ordovicidium و Pachysphaeridium و Orthosphaeridum، وهي شائعة في تجمعات العوالق النباتية الأوردوفية الوسطى من Baltica، ممثلة تمثيلاً جيدًا، مع العديد من الأنواع، بشكل رئيسي في التجميع أ والتجميع الفرعي B1، حتى Sandbian السفلي. ومع ذلك، فإن وجود غالبية الأصناف ذات التوزيع العالمي يدعم عالمية التجمعات المدروسة، تم اقتراحها بالفعل للبدء بالقرب من التحول الداريويلي- الساندبي. بشكل ملحوظ، تظهر أصناف العوالق النباتية ذات الانتماءات السيلورية، والمعروفة سابقًا من الهيرنانتية، لأول مرة في الجزء الداريويلي المتأخر من النواة الحفرية بورنشولت-1 (Dw3). والأصناف الهامة التي تحدث هي تايلوتوبالا وميتاليوفوسا، والتي تم تأسيسها بشكل نهائي من بداية الساندبيان (الأوردوفيشي المتأخر المبكر)، إلى جانب الظهور الأول لجنس Visbysphaera.The these occurrences question the relationship between the appearance of pioneering phytoplankton morphotypes and the Hirnantian glaciation.Other taxa with no pre - Silurian records such as Visbysphaera pirifera sub.minor, Petaloferidium cazurrum and Dorsennidium cf.D. estrellitae موجودة هنا في Sandbian، حيث يتم إقحام أسرة البنتونيت. يتم تسجيل جنس Frankea لأول مرة من الأوردوفيشي السويدي، مما يشير إلى توزيع خط العرض العالي إلى المتوسط بدلاً من توزيع شبه جندواني. يتوافق أعلى تنوع مع Darriwilian وجزئيًا مع تجمعات Sandbian، يليه انخفاض كبير في Katian. لوحظت التغييرات الرئيسية في Sandbian، مع انخفاض كبير في التنوع، والذي ربما يكون مرتبطًا بممثل النشاط البركاني المكثف المستاء من طبقات البنتونيت. التنوع وكذلك معدلات المنشأ والدوران هي الأدنى في الفترة التي تحمل مجموعة البنتونيت K، خاصة بالقرب من سمكه. من المحتمل أن يكون الانخفاض الملحوظ في التنوع في الجزء الكاتاني من الخلافة، المرئي في كل من المنشأ المنخفض والوفرة، مرتبطًا بالانحدار في بداية GICE (رحلة الكربون بنظائر Guttenberg)، مع ظروف بيئية ومناخية أقل ملاءمة. تم تفسير التغيرات في تجمعات العوالق النباتية جنبًا إلى جنب مع بداية المورفولوجيات المبتكرة للنرجس الصخري سابقًا كنتيجة للظروف البيئية والاضطرابات المناخية المتعلقة بالتجلد الأوردوفيشي. هنا نظهر أن المظاهر الأولى لهذه الأصناف المتقدمة حدثت بالفعل قبل 15 مليون سنة مضت، مما يشير إلى أن مجموعة محتملة من العوامل مثل تغيرات مستوى سطح البحر والبراكين تسببت في هذه التغييرات، بدلاً من حدث كبير مثل التجلد الهيرنانتي. بالإضافة إلى ذلك، تتحدى هذه النتائج الجديدة النماذج السابقة لتطور وإشعاع العوالق النباتية الأوردوفيشية وتضع البلطيقا كمنطقة رئيسية جديدة للبحث في الجغرافيا القديمة.

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    Estonian Journal of Earth Sciences
    Article . 2023 . Peer-reviewed
    Data sources: DOAJ; Crossref
    https://doi.org/10.60692/hkf88...
    Other literature type . 2023
    Data sources: Datacite
    https://doi.org/10.60692/vnwz5...
    Other literature type . 2023
    Data sources: Datacite