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Carbon, Nitrogen and Sulphur concentration and δ13C, δ15N values in Hypogymnia physodes within the montane area – preliminary data

] Biazrov, L.G. 2012a. Stable Nitrogen Isotopes (δ 15 N) in Thalli of the Lichen Hypogymnia physodes along a Altitudinal Gradient in the Khangai Plateau, Mongolia. Russ. J. Ecol. , 43(3): 185–190. [5] Biazrov, L.G. 2012b. Values of Stable Carbon Isotopes (δ 13 C) in the Thalli of the Arid Vagrant Lichen Xanthoparmelia camtschadalis along an Altitudinal Gradient in the Khangai Plateau as a Reflection of the Spatial and Ecological Heterogeneity of the Semiarid Region of Mongolia. Arid Ecosystems , 2(1): 54–60. [6] Boltersdorf S.H., Werner, W. 2014. Lichens

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Dissolution of lead matte and copper slag upon exposure to rhizosphere-like conditions

–181. [41] Sandnes A., Eldhuset T.D., Wollebæk G. (2005). Organic acids in root exudates and soil solution of Norway spruce and silver birch. Soil Biology and Biochemistry 37(2), 259–269. [42] Schmukat A., Duester L., Ecker D., Schmid H., Heil C., Heininger P., Ternes T.A. (2012). Leaching of metal(loid)s from a construction material: Influence of the particle size, specific surface area and ionic strength. Journal of Hazardous Materials (227), 257–264. [43] Seignez N., Gauthier A., Bulteel D., Bautier M., Recourt P., Damidot D., Potdevin J.L. (2007

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Serpentinite in the Śnieżnik Massif: petrology and ecological impact

directive 92/43/EEC of 21 May 1992 on the conservation of natural habitats and of wild fauna and flora. OJ L 206, 22.7.1992: 1–66. [4] Don J., Dumicz M., Wojciechowska I., Żelaźniewicz A. 1990. Lithology and tectonics of the Orlica-Śnieżnik Dome, Sudetes – recent state of knowledge. Neues Jahrbuch für Geologie und Paläontologie – Abhandlungen, 179: 159–188. [5] Dubińska E., Bylina P., Kozłowski A., Wolfgang D., Nejbert K., Schastok J., Kulicki C. 2004. U-Pb dating of serpentinization: hydrothermal zircon from a metasomatic rodingite shell (Sudetic ophiolite, SW Poland

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Clinopyroxene phenocrysts from the Księginki nephelinite (SW Poland)

-phase lherzolites II. New thermobarometers, and practical assessment of existing thermobarometers. J. Petrol., 31, 6: 1353–1378. [7] Cajz V., Valečka J. 2010. Tectonic settings of the Ohře/Eger Grabem between the central part of the České středohoří Mts. And the Most basin, a regional study. J. Geosci., 55: 201–215. [8] Dobosi G., Schultz-Giittler R., Kurat G., Kracher A. 1991. Pyroxene chemistry and evolution of alkali basaltic rocks from Burgenland and Styria, Austria. Mineral. Petr., 43: 275–292. [9] Downes H. 2001. Formation and modification of the shallow subcontinental

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Anti-predator adaptations in a great scallop (Pecten maximus) – a palaeontological perspective

A.V., Li G., Fernandez C.Z. 2010. Shell microstructures in early Mollusks. The Festivus, XLII, 4: 43–54. [35] Vermeij G.J. 1977. The Mesozoic marine revolution: Evidence from snails, predators and grazers. Paleobiology, 3: 245–258. [36] Vermeij G.J. 1987. Evolution and Escalation. An Ecological History of Life, 1–527. Princeton University Press, Princeton. [37] Yang W., Kashani N., Li X.W., Zhang G.P., Meyers M.A. 2011a. Structural characterization and mechanical behavior of a bivalve shell (Saxidomus purpuratus). Materials Science and Engineering: C, 31: 724

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