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, A129. Cambel B. 1951: Ultrabasic rock from Sedlice and serpentines of the closest surrounding. [Ultrabázická hornina od Sedlíc a hadce najbližšieho okolia.] Geol. Zbor. Slovak. Akad. Vied 2, 1-91 (in Slovak). Choi S.H., Shervais J.W. & Mukasa S.B. 2008: Supra-subduction and abyssal mantle peridotites of the Coast Range ophiolite, California. Contr. Mineral. Petrology 156, 551-576. Dallmeyer R.D., Neubauer F., Handler R., Fritz H., Müller W., Pana D. & Putiš M. 1996: Tectonothermal evolution of the in- ternal Alps and Carpathians: Evidence from 40Ar/39Ar mineral

communities in serpentines of Serbia. (Tri endemicne zajednice na serpentinskoj podlozi u Srbiji). Acta Botanica Croatica 28: 43–47. Bornmüller, J. 1923: Über eine neue Tulpe der Flora Mazedoniens. Feddes Repertorium 19: 199–200. Brown, J.H. & Lomolino, M.V. 1998: Biogeography, 2nd edn. Sinauer Associates. Inc. Publishers, Sunderland, MA. 43 pp. Butchart, S.H.M., Walpole, M., Collen, B., van Strien, A., Scharlemann, J.P.W., Almond, R.E.A., Baillie, J.E.M., Bomhard, B., Brown, C., Bruno, J., Carpenter, K.E., Carr, G.M., Chanson, J., Chenery, A.M., Csirke, J., Davidson, N

-Dissertation... von Hans Peter Cornelius. E. Schweizerbart, 1912. [44] T. Peters, “A water-bearing andradite from the Totalp serpentine (Davos, Switzerland): American Mineralogist”, Journal of Earth and Planetary Materials, Vol. 50(9), Pp. 1482-1486, 1965. [45] V. Trommsdorff, B.W. Evans, and H.R. Pfeifer, “Ophicarbonate rocks-metamorphic reactions and possible origin”, Archives des Sciences, Vol. 33, Pp. 361-364, 1980. [46] D. Lavoie, and P.A. Cousineau, “Ordovician ophicalcites of southern Quebec Appalachians; a proposed early seafloor tectonosedimentary and hydrothermal origin

Abstract

Primary cutaneous B- cell lymphomas (PCBLs) are B-cell malignant neoplasms that originate in the skin, and have no extracutaneous manifestations of disease at the time of diagnosis. PCBLs are classified into three main types: primary cutaneous marginal zone lymphoma (PCMZL), primary cutaneous follicle center lymphoma (PCFCL), and primary cutaneous diffuse large B-cell lymphoma, leg type (PCDLBCL- LT). Dermoscopic characterization of PCBLs has been limited and dermoscopy may help to augment the clinical recognition of PCBLs with the most common dermoscopic findings of salmon colored areas and serpentine vessels. Recognition of dermoscopic features of primary cutaneous B- cell lymphomas can improve the early diagnosis of these tumors and their proper management.

Abstract

The aim of this study was to assess the condition of soil after serpentine fertilisation by determining the activity of phosphatase and some physicochemical properties of soil. The study was conducted in southern Poland in the Wisła Forest District (49°8’12.92N 18°58’56.36E). The following variants: C - control - no fertiliser; S - ground serpentinite; SN - serpentinite + nitrogen; SP - ground serpentinite + P; SNP - ground serpentinite + NP; SNPK - ground serpentinite + NP (as above) + K. Fertilisation of serpentinite stimulates the activity of phosphatase in soil under spruce stands. The positive impact is reflected in the organic horizon. Less activity was noted in the humus-mineral horizon (AE) in all the fertiliser combinations three years after the fertilisation. Fertilisation of serpentinite improves the chemical properties - pH was increased, reduction of molar ratio of exchangeable calcium to magnesium form was noted.

Tectonic evolution of the southeastern part of the Pohorje Mountains (Eastern Alps, Slovenia)

Field relations and deformation structures in the southeastern part of the Pohorje Mountains constrain the tectonic evolution of the Austroalpine high-pressure/ultrahigh pressure (HP/UHP) terrane. The Slovenska Bistrica Ultramafic Complex (SBUC) forms a large (ca. 8 × 1 km size) body of serpentinized harzburgite and dunite including minor garnet peridotite and is associated with partly amphibolitized eclogite bodies. The SBUC occurs in the core of an isoclinal, recumbent, northward closing antiform and is mantled by metasedimentary rocks, mostly gneisses and a few marbles, including isolated eclogite/amphibolite lenses. Before this folding, the SBUC formed the deepest part of the exposed terrane. We interpret the SBUC to be derived from near-MOHO, uppermost mantle which was intruded by gabbros in the subsurface of a Permian rift zone. During Cretaceous intracontinental subduction, the SBUC was most likely part of the footwall plate which experienced HP to UHP metamorphism and was folded during exhumation. In the Miocene, the Pohorje Pluton intruded and, subsequently, the metamorphic rocks together with the pluton were deformed probably due to east-west extension and contemporaneous north-south shortening, thus forming an antiformal metamorphic core complex.

Abstract

The paper presents results of floristic investigation conducted within the territory of waste dumps in Lower Silesia: landfill of municipal waste Wrocław-Maślice, post-metallurgic waste heap in Siechnice, serpentine dumping grounds in Grochów and slag heaps in Bielawa.

The investigated flora was analyzed with regard to species composition, participation of geographical-historical groups, live forms (according to classification by Raunkiaer), as well as selected ecological factors: light indicator (L), thermal indicator (T), soil moisture (W), trophic indicator (Tr), soil reaction (pH), value of resistance to increased heavy metals content (M). On 4 waste dumps there were found 269 species of vascular plants, belonging to 51 families. Only 5 species occurred on 4 sites, which provides for 2% of all plants recorded. The most numerous families are Asteraceae, Poaceae and Fabaceae. Apophytes dominate in waste dumps flora Hemicryptophytes are the most numerous group.

Analysis of the floras (selected ecological factors) of investigated objects has shown general similarities, but also apparent differences. The most significant differences concerned two parameters: trophism (Tr) and resistance to increased heavy metals content (M).

R eferences [1] WU, R. B.—CHAO, F. L. : Laddering Wave in Serpentine Delay Line, IEEE Trans. Components, Packag. Manuf. Technol. Part B, Adv. Packag 18 (1995), 644–650,, doi:10.1109/96.475270. [2] SHIUE, G. H.—CHAO, C. Y.—WU, R. B. : Guard Trace Design for Improvement on Transient Waveforms and Eye Diagrams of Serpentine Delay Lines, IEEE Trans. Adv. Packag. 33 (2010), 1051–1060, doi:10.1109/TADVP.2010.2064165. [3] BRUCE, A. : Importance and Process of Validation for All Levels of Modeling Problems, in: IEEE Int. Symp. EMC, 2009. [4] TOPSAKAL, E.—VOLAKIS, J

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hysteresis behaviour and random vibration applications, Journal of Vibration, Acoustics, Stress and Reliability in Design, 108 (1986), (4), 411-420. [5] F. Dal Corso, D. Misseroni, N. M. Pugno, A. B. Movchan, N. V., Movchan, D. Bigoni, Serpentine locomotion through elastic energy release, Journal of the Royal Society Interface, 14 : 20170055 (2017). [6] G. Groza, N. Pop, A numerical method for solving of the boundary value problems for ordinary difierential equations, Result. Math., 53 (2009), No. 3-4, 295-302. [7] G. Groza, M. Jianu, N. Pop, Infinitely difierentiable