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  • Andren, M., et al. (author)
  • Coupling between mineral reactions, chemical changes in groundwater, and earthquakes in Iceland
  • 2016
  • In: Journal of Geophysical Research-Solid Earth. - : American Geophysical Union (AGU). - 2169-9313. ; 121:4, s. 2315-2337
  • Journal article (peer-reviewed)abstract
    • Chemical analysis of groundwater samples collected from a borehole at Hafralaekur, northern Iceland, from October 2008 to June 2015 revealed (1) a long-term decrease in concentration of Si and Na and (2) an abrupt increase in concentration of Na before each of two consecutive M 5 earthquakes which occurred in 2012 and 2013, both 76km from Hafralaekur. Based on a geochemical (major elements and stable isotopes), petrological, and mineralogical study of drill cuttings taken from an adjacent borehole, we are able to show that (1) the long-term decrease in concentration of Si and Na was caused by constant volume replacement of labradorite by analcime coupled with precipitation of zeolites in vesicles and along fractures and (2) the abrupt increase of Na concentration before the first earthquake records a switchover to nonstoichiometric dissolution of analcime with preferential release of Na into groundwater. We attribute decay of the Na peaks, which followed and coincided with each earthquake to uptake of Na along fractured or porous boundaries between labradorite and analcime crystals. Possible causes of these Na peaks are an increase of reactive surface area caused by fracturing or a shift from chemical equilibrium caused by mixing between groundwater components. Both could have been triggered by preseismic dilation, which was also inferred in a previous study by Skelton et al. (2014). The mechanism behind preseismic dilation so far from the focus of an earthquake remains unknown.
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  • Gislason, S.R., et al. (author)
  • Environmental pressure from the 2014–15 eruption of Bárðarbunga volcano, Iceland
  • 2015
  • In: Geochemical Perspectives Letters. - : European Association of Geochemistry. - 2410-3403 .- 2410-339X. ; 1:2015, s. 84 - 93
  • Journal article (peer-reviewed)abstract
    • The effusive six months long 2014-2015 Bárðarbunga eruption (31 August-27 February) was the largest in Iceland for more than 200 years, producing 1.6 ± 0.3 km3 of lava. The total SO2 emission was 11 ± 5 Mt, more than the amount emitted from Europe in 2011. The ground level concentration of SO2 exceeded the 350 μg m−3 hourly average health limit over much of Iceland for days to weeks. Anomalously high SO2 concentrations were also measured at several locations in Europe in September. The lowest pH of fresh snowmelt at the eruption site was 3.3, and 3.2 in precipitation 105 km away from the source. Elevated dissolved H2SO4, HCl, HF, and metal concentrations were measured in snow and precipitation. Environmental pressures from the eruption and impacts on populated areas were reduced by its remoteness, timing, and the weather. The anticipated primary environmental pressure is on the surfacewaters, soils, and vegetation of Iceland.
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  • Librado, P., et al. (author)
  • The origins and spread of domestic horses from the Western Eurasian steppes
  • 2021
  • In: Nature. - : Springer Science and Business Media LLC. - 0028-0836 .- 1476-4687. ; 598, s. 634-640
  • Journal article (peer-reviewed)abstract
    • Analysis of 273 ancient horse genomes reveals that modern domestic horses originated in the Western Eurasian steppes, especially the lower Volga-Don region. Domestication of horses fundamentally transformed long-range mobility and warfare(1). However, modern domesticated breeds do not descend from the earliest domestic horse lineage associated with archaeological evidence of bridling, milking and corralling(2-4) at Botai, Central Asia around 3500 bc(3). Other longstanding candidate regions for horse domestication, such as Iberia(5) and Anatolia(6), have also recently been challenged. Thus, the genetic, geographic and temporal origins of modern domestic horses have remained unknown. Here we pinpoint the Western Eurasian steppes, especially the lower Volga-Don region, as the homeland of modern domestic horses. Furthermore, we map the population changes accompanying domestication from 273 ancient horse genomes. This reveals that modern domestic horses ultimately replaced almost all other local populations as they expanded rapidly across Eurasia from about 2000 bc, synchronously with equestrian material culture, including Sintashta spoke-wheeled chariots. We find that equestrianism involved strong selection for critical locomotor and behavioural adaptations at the GSDMC and ZFPM1 genes. Our results reject the commonly held association(7) between horseback riding and the massive expansion of Yamnaya steppe pastoralists into Europe around 3000 bc(8,9) driving the spread of Indo-European languages(10). This contrasts with the scenario in Asia where Indo-Iranian languages, chariots and horses spread together, following the early second millennium bc Sintashta culture(11,12).
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  • Tay, J., et al. (author)
  • Pre-transplant marital status and hematopoietic cell transplantation outcomes
  • 2020
  • In: Current Oncology. - : MULTIMED INC. - 1198-0052 .- 1718-7729. ; 27:6, s. E596-E606
  • Journal article (peer-reviewed)abstract
    • Background Evidence about the impact of marital status before hematopoietic cell transplantation (HCT) on outcomes after HCT is conflicting. Methods We identified patients 40 years of age and older within the Center for International Blood and Marrow Transplant Research registry who underwent HCT between January 2008 and December 2015. Marital status before HCT was declared as one of: married or living with a partner, single (never married), separated or divorced, and widowed. We performed a multivariable analysis to determine the association of marital status with outcomes after HCT. Results We identified 10,226 allogeneic and 5714 autologous HCT cases with, respectively, a median follow-up of 37 months (range: 1-102 months) and 40 months (range: 1-106 months). No association between marital status and overall survival was observed in either the allogeneic (p = 0.58) or autologous (p = 0.17) setting. However, marital status was associated with grades 2-4 acute graft-versus-host disease (GVHD), p < 0.001, and chronic GVHD, p = 0.04. The risk of grades 2-4 acute GVHD was increased in separated compared with married patients [hazard ratio (FIR): 1.13; 95% confidence interval (CI): 1.03 to 1.24], and single patients had a reduced risk of grades 2-4 acute GVHD (FIR: 0.87; 95% CI: 0.77 to 0.98). The risk of chronic GVHD was lower in widowed compared with married patients (FIR: 0.82; 95% CI: 0.67 to 0.99). Conclusions Overall survival after HCT is not influenced by marital status, but associations were evident between marital status and grades 2-4 acute and chronic GVHD. To better appreciate the effects of marital status and social support, future research should consider using validated scales to measure social support and patient and caregiver reports of caregiver commitment, and to assess health-related quality of life together with health care utilization.
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  • Aad, G., et al. (author)
  • 2012
  • swepub:Mat__t (peer-reviewed)
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  • Aad, G., et al. (author)
  • 2013
  • Journal article (peer-reviewed)
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  • Aad, G., et al. (author)
  • 2012
  • swepub:Mat__t (peer-reviewed)
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  • Aad, G., et al. (author)
  • 2013
  • In: The European Physical Journal C. - : Springer Science and Business Media LLC. - 1434-6052. ; 73:1
  • Journal article (peer-reviewed)
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  • Aad, G., et al. (author)
  • 2012
  • swepub:Mat__t (peer-reviewed)
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  • Aad, G., et al. (author)
  • 2012
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  • Aad, G., et al. (author)
  • 2012
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  • Aad, G., et al. (author)
  • 2012
  • swepub:Mat__t (peer-reviewed)
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  • Aad, G., et al. (author)
  • 2012
  • swepub:Mat__t (peer-reviewed)
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  • Aad, G., et al. (author)
  • 2012
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  • Aad, G., et al. (author)
  • 2013
  • In: The European Physical Journal C. - : Springer Science and Business Media LLC. - 1434-6052. ; 73:3
  • Journal article (peer-reviewed)
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  • Aad, G., et al. (author)
  • 2013
  • In: New Journal of Physics. - : IOP Publishing. - 1367-2630. ; 15
  • Journal article (peer-reviewed)
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  • Aad, G., et al. (author)
  • 2012
  • swepub:Mat__t (peer-reviewed)
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  • Aad, G., et al. (author)
  • 2012
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  • Aad, G., et al. (author)
  • 2012
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  • Aad, G., et al. (author)
  • 2012
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  • Aad, G., et al. (author)
  • 2012
  • In: Nuclear Physics, Section B. - : Elsevier BV. - 0550-3213 .- 1873-1562. ; 864:3, s. 341-381
  • Journal article (peer-reviewed)
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  • Aad, G., et al. (author)
  • 2012
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  • Aad, G., et al. (author)
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  • Aad, G., et al. (author)
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  • Aad, G., et al. (author)
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  • Aad, G., et al. (author)
  • 2012
  • swepub:Mat__t
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  • Aad, G., et al. (author)
  • 2012
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  • Aad, G., et al. (author)
  • 2012
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  • Aad, G., et al. (author)
  • 2013
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  • Aad, G., et al. (author)
  • 2012
  • In: The European Physical Journal C. - : Springer Science and Business Media LLC. - 1434-6052. ; 72:10
  • Journal article (peer-reviewed)
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  • Aad, G., et al. (author)
  • 2012
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  • Aad, G., et al. (author)
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  • Aad, G., et al. (author)
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  • Aad, G., et al. (author)
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  • Aad, G., et al. (author)
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  • Aad, G., et al. (author)
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  • Aad, G., et al. (author)
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  • Aad, G., et al. (author)
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  • Aad, G., et al. (author)
  • 2013
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