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Lunnomidinium scaniense Lindstrom, gen. et sp nov., a new suessiacean dinoflagellate cyst from the Rhaetian of Scania, southern Sweden
Human impact on the fish diversity in the four largest lakes of Sweden
Autosomal dominant retinitis pigmentosa with a rhodopsin mutation (Arg-135–Trp): Disease phenotype in a Swedish family
Using resistivity measurements for dam safety evaluation at Enemossen tailings dam in southern Sweden
Internal erosion is a major reason for embankment dam failures. Resistivity measurements is an essentially non-destructive technique, which may have the possibility of detecting internal erosion processes and anomalous seepage at an early stage before the safety of the dam is at stake. This paper presents results from part of a dam safety investigation conducted at the Enemossen tailings dam in so
Soil properties affecting the frost sensitivity of beech bark in southern Sweden
Swedish word accents in a ‘confirmation’ context
Dental and vertebral morphology of the enigmatic mosasaur Dollosaurus (Reptilia, Mosasauridae) from the lower Campanian (Upper Cretaceous) of southern Sweden
Abundance of owls and bramblings Fringilla montifringilla in relation to mast seeding in south-eastern Sweden.
Second-generation hepatitis C Elisa antibody tests confirmed by the four-antigen recombinant immunoblot assay correlate well with hepatitis C viremia and chronic liver disease in Swedish blood donors
Preferences and frequencies of visits to public facilities in old age-a pilot study in a Swedish town center.
Numbers of mute swans and Whooper Swans in Sweden, 1967-2000
Phenotype in a Swedish family with X-linked retinitis pigmentosa caused by a novel splice defect in the RPGR gene
The Swedish knee arthroplasty register. A nation-wide study of 30,003 knees 1976-1992
Petrographic classification of middle ordovician fossil meteorites from Sweden
The maximum diameter of chromite (FeCr2O4) grains within L chondrites reflects the petrographic type of the sample. On the basis of our measurements of nine recent L chondrites, L3 chromite D-mac = 34-50 mu m, L4 = 87-150 mu m, L5 = 76-158 mu m, and L6 = 253-638 mu m. This variation reflects the crystallization of the chromite grains during parent body thermal metamorphism.We use this calibration