scholarly journals Alder-ash and willow communities and their diversity in the Pogórze Strzyżowskie foothills (Western Carpathians)

2011 ◽  
Vol 77 (4) ◽  
pp. 327-338
Author(s):  
Alina Stachurska-Swakoń ◽  
Krystyna Towpasz

The results of phytosociological studies on the diversity of alder-ash and willow communities in the Pogórze Strzyżowskie foothills are presented. These communities, especially <em>Carici remotae-Fraxinetum</em> are increasingly rare in the landscape of the Carpathians. The paper supports new data allowing better understanding of the diversity of the <em>Carici remotae-Fraxinetum</em> in the southern Poland. On the basis of 59 phytosociological releves two sub-associations were identified: <em>C.r.-F. chrysosplenietosum</em> and <em>C. r.-F. equisetetosum maximii</em> and the form with <em>Alnus incana</em>. The association <em>Carici remotae-Fraxinetum</em> belongs to submontane regional form and to East Carpathian variant. The significance of <em>Caltha palustris-Chaerophyllum hirsutum</em> community is also presented, along with the role of <em>Carex pendula</em> and <em>Matteucia struthiopteris</em>. The paper provides also documentary data on sporadic occurrence of <em>Salicetum triandro-viminalis</em> and <em>Salicetum albo-fragilis</em> communities.

2021 ◽  
Vol 0 (0) ◽  
Author(s):  
Marcin Szeliga ◽  
Zsolt Kasztovszky ◽  
Grzegorz Osipowicz ◽  
Veronika Szilágyi

Abstract The inflow of the Carpathian obsidian into the areas on the northern side of the Carpathians and the Sudetes is confirmed as early as in the Palaeolithic. However, its greatest intensity occurred in the Early Neolithic, i. e. in the late 6th and in the first half of 5th millennia BC. During that period, the phenomenon was closely related with the development of the Danubian cultural groups in the upper Vistula river basin, including especially Linear Pottery culture (LBK) and Malice Culture. The constant presence of this raw material products in mentioned areas is documented from the classical (musical-note) phase of LBK, constituting one of the most expressive pieces of evidence of permanent and intense intercultural contacts with communities of the northern Carpathian Basin. This phenomenon has been repeatedly emphasized in the literature. One of the most numerous LBK obsidian inventories in the upper Vistula river basin was obtained at site 6 in Tominy, located in southern Poland, in the non-loess zone of the Sandomierz Upland northern foreground. The above-mentioned collection, its non-destructive elemental analysis, using Prompt Gamma Activation Analysis (PGAA) and also traceological analysis, is the subject of this article. The results supplement the published data to a significant extent, simultaneously providing partial verification and updating of the current state of knowledge on the basic issues related to the Early Neolithic obsidian inflow into areas located North of the Carpathians, including primarily the origin of the raw material, the scale of its processing and distribution ways, as well as the range of its use by the LBK communities.


Author(s):  
Dede Eka Putri ◽  
Endang Sri Markamah ◽  
Sadiman Sadiman

<p class="Bab"><strong><em>This research aims to improve understanding of service and figure role Indonesian independence concept at 5th grade student of elementary school in Surakarta by application of Teams Games Tournament (TGT) model helped by rotar media.This research was classroom action resarch which was held i two cycles, there were four stage in each cycle, which planning, implementation, observation, and reflection. The subjects were a teacher and 34 students. The data sources are form the teacher and student. The technics of collecting data are test, interview, observation, and documentary. Data analysis were interactive analysis.</em> <em>According to the research conclusion, Teams Games Tournament model helped by rotar media could improve understanding of service and figure role of independence concept at 5th grade student of elementary school in Surakarta academic year 2017/2018. That improvement could be Pre-action, the percentage of class attainment is only 5,88% then at second cycle, the percentage of class attainment increases to 88,24%</em></strong></p>


2020 ◽  
Vol 20 (11) ◽  
pp. 2433-2447
Author(s):  
Barbara Błaszczak ◽  
Natalia Zioła ◽  
Barbara Mathews ◽  
Krzysztof Klejnowski ◽  
Krzysztof Słaby

2018 ◽  
Vol 226 ◽  
pp. 280-287 ◽  
Author(s):  
Piotr Skórka ◽  
Michał Żmihorski ◽  
Emilia Grzędzicka ◽  
Rafał Martyka ◽  
William J. Sutherland

Plants ◽  
2020 ◽  
Vol 9 (12) ◽  
pp. 1678
Author(s):  
Carmelo Maria Musarella ◽  
Salvatore Brullo ◽  
Gianpietro Giusso del Galdo

The results of a phytosociological investigation regarding the orophilous cushion-like vegetation occurring in the top of the high mountains of central-southern Greece and in some Ionian (Lefkas, Cephalonia) and Aegean Islands (Euboea, Samos, Lesvos, Chios and Thassos) are provided. Based on 680 phytosociological relevès (460 unpublished and 220 from literature), a new syntaxonomical arrangement is proposed with the description of a new class, including two new orders, eight new alliances, and several associations (many of them new). Compared to the previous hierarchical framework usually followed in the literature, this study provides a more realistic and clear phytosociological characterization of this peculiar and archaic vegetation type, which is exclusive to the high mountains of the north-eastern Mediterranean. The new arrangement is mainly based on the phytogeographical role of the orophytes featuring this very specialized vegetation, which is essentially represented by endemics or rare species belonging to the ancient Mediterranean Tertiary flora. In addition, taxonomic research on the orophilous flora occurring in these plant communities allowed to identify six species new to science (i.e., Astragalus corinthiacus, Allium cremnophilum, A. cylleneum, A. orosamium, A. karvounis, and A. lefkadensis) and a new subspecies (i.e., Allium hirtovaginatum subsp. samium), and two new combinations (i.e., Astragalus rumelicus subsp. euboicus and subsp. taygeticus) are proposed.


2017 ◽  
Vol 68 (2) ◽  
pp. 119-129 ◽  
Author(s):  
Jakub Jirásek ◽  
Zdeněk Dolníček ◽  
Dalibor Matýsek ◽  
Tomáš Urubek

AbstractBarite is a relatively uncommon phase in vein and amygdule mineralizations hosted by igneous rocks of the teschenite association in the Silesian Unit (Western Carpathians). In macroscopically observable sizes, it has been reported from 10 sites situated only in the Czech part of the Silesian Unit. Microscopic barite produced by the hydrothermal alteration of rock matrix and also by the supergene processes is more abundant. We examined four samples of barite by mineralogical and geochemical methods. Electron microprobe analyses proved pure barites with up to 0.038 apfu Sr and without remarkable internal zonation. Fluid inclusion and sulphur isotope data suggests that multiple sources of fluid components have been involved during barite crystallization. Barite contains primary and secondary aqueous all-liquid (L) or less frequent two-phase (L+V) aqueous fluid inclusions with variable salinity (0.4-2.9 wt. % NaCl eq.) and homogenization temperatures between 77 and 152 °C. The higher-salinity fluid endmember was probably Cretaceous seawater and the lower-salinity one was probably diagenetic water derived from surrounding flysch sediments during compaction and thermal alteration of clay minerals. The δ34S values of barite samples range between -1.0 ‰ and +16.4 ‰ CDT suggesting participation of two sources of sulphate, one with a near-zero δ34S values probably derived from wall rocks and another with high δ34S values being most probably sulphate from the Cretaceous seawater. All results underline the role of externally derived fluids during post-magmatic alteration of bodies of rock of the teschenite association.


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