Post-LGM faulting in Central Europe: LiDAR detection of the >50 km-long Sub-Tatra fault, Western Carpathians

Geomorphology ◽  
2020 ◽  
Vol 364 ◽  
pp. 107248 ◽  
Author(s):  
Tomáš Pánek ◽  
Jozef Minár ◽  
Ladislav Vitovič ◽  
Michal Břežný
Zootaxa ◽  
2017 ◽  
Vol 4238 (4) ◽  
pp. 597 ◽  
Author(s):  
FABIO CIANFERONI ◽  
MARGHERITA NORBIATO ◽  
MARCO DOGLIOTTI

Salda henschii (Reuter, 1891) is a boreo-montane species of Saldidae (Hemiptera: Heteroptera) restricted to mountain bogs and streams in central Europe (e.g., Western Carpathians, Alps) and to freshwater wetlands in lowland coastal areas in northern Europe (Fennoscandia); it is a vicariant of the arctic (Holarctic) element S. sahlbergi Reuter, 1875 (Hoberlandt 1977; Schuh et al. 1987; Péricart 1990; Lindskog 1991; Vinokurov 2010). 


Volcanica ◽  
2021 ◽  
pp. 149-187
Author(s):  
Jacky Bouloton

Almandine-rich garnets from a Neogene andesite of Slovakia can be divided into two main types. Garnet megacrysts are magmatic and form a chemically homogeneous group that contains, on average, about 5 wt% CaO and 4.5 wt% MgO as petrogenetically significant components. Garnets occurring in lithic fragments and garnets aggregated in garnetite lenses are characterised by Ca-poor cores (CaO <= 2 wt%) that testify for a two-step history and correspond respectively to inherited pre-anatectic and peritectic garnets. Available experimental data show that the composition of magmatic garnet megacrysts is compatible with a peritectic origin, through the fluid-absent melting of an immature metasedimentary protolith or a tonalitic gneiss. However, thermal evolution evidenced by zircons shielded in garnet rather suggests that garnet nucleated and grew by cooling of a hybrid magma pool, resulting from the complete mixing of crust- and mantle-derived melts.


Palynology ◽  
2019 ◽  
Vol 44 (2) ◽  
pp. 355-368 ◽  
Author(s):  
Sambor Czerwiński ◽  
Włodzimierz Margielewski ◽  
Mariusz Gałka ◽  
Piotr Kołaczek

The Holocene ◽  
2017 ◽  
Vol 28 (4) ◽  
pp. 595-608 ◽  
Author(s):  
Piotr Kołaczek ◽  
Monika Karpińska-Kołaczek ◽  
Katarzyna Marcisz ◽  
Mariusz Gałka ◽  
Mariusz Lamentowicz

2011 ◽  
Vol 60 (2) ◽  
pp. 185-189 ◽  
Author(s):  
Vítězslav Plášek ◽  
Eva Novozámská

Historical and recent occurrence of epixylous moss Buxbaumia viridis in the Javorníky Mts. and the Vsetínské vrchy hills (Western Carpathians) The epixylous moss Buxbaumia viridis (Moug. ex Lam. & DC.) Brid. ex Moug. & Nestl. is considered an endangered or vulnerable species in all countries in the Central Europe. In the Czech part of the Western Carpathians the species was recorded very occasionally in the twentieth century. In 2011 field monitoring of the species on historically known localities in Javorníky Mts. and the Vsetínské vrchy hills was carried out. As a result, six localities of B. viridis have been recorded in this region. Precise localization, number of and ecological data are given.


2018 ◽  
Vol 49 (1) ◽  
pp. 243-246
Author(s):  
Andrea Lešová ◽  
Peter Lešo ◽  
Rudolf Kropil

Abstract A dead individual of C. leucodon was found in the Lower Tatra Mts. (Central Slovakia, Western Carpathians). The site is situated in the westernmost part of the main ridge of this mountain range at the altitude of 1,150 m a. s. l. The prevaling habitat is a mountain meadow surrounded by spruce and beach-maple forests. In Central Europe, the species usually occurs in lowland and hilly areas, records above 600 m a. s. l. are very rare. The finding of C. leucodon in the mountain ridge at this extraordinary altitude is the highest documented occurrence of the species in the Western Carpathians and Central Europe as well. It is probably related to expansion of the species range in the recent decades and its spreading to higher altitudes, which is more common at the southern border of its distribution area.


2021 ◽  
Vol 55 (2) ◽  
Author(s):  
Piotr Mleczko ◽  
Maciej Kozak ◽  
Filip Karpowicz

Investigations carried out in recent years have provided new data on the localities of some rare hypogeous fungi in Central Europe. In this study, we present new localities of <em>Leucangium carthusianum</em>, <em>Melanogaster luteus</em>, and <em>Rhizopogon </em><em>melanogastroides</em>, two of which are new for Poland. Sporocarps of <em>L. carthusianum </em>were found in seven new localities in mixed and coniferous forests in the Western Carpathians as well as in Sudetes. In Poland, the species was also recorded in a mixed forest in the Kraków-Częstochowa Upland. Fir, <em>Abies alba</em>, accompanied the fungus in almost all known localities. Three localities of <em>M. luteus </em>were found in the Polish Western and Eastern Carpathians in <em>Alnus incana </em>communities mostly associated with streams. Knowledge of the distribution of this species in Europe is incomplete due to the complicated taxonomic history; nevertheless, it is regarded as rare, despite its wide distribution. One new locality of <em>R. melanogastroides </em>recorded in the Tatra Mts, Western Carpathians, is the fourth known to date. This species is mostly associated with <em>Pinus mugo </em>in high mountain localities (the Alps, the Tatra Mts). In this study, detailed descriptions and illustrations of the macro- and micromorphological features of the species are provided.


2020 ◽  
Author(s):  
Carmen-Andreea Bădăluță ◽  
Aurel Perșoiu

&lt;p&gt;Ice cores are key archives in the quest to reconstruct and understand past climate variability. They are generally found in polar and high latitude regions, but caves in the Carpathian Mountains (East-central Europe) host several glaciers thousands of years old. Here, we present a reconstruction of summer and winter air temperatures during the last millennium based on the d&lt;sup&gt;18&lt;/sup&gt;O and d&lt;sup&gt;2&lt;/sup&gt;H values measured in ice cores drilled in the glaciers hosted by Focul Viu (FV) and Sc&amp;#259;ri&amp;#537;oara Ice Caves (SIC), both in the Western Carpathians (East-Central Europe, Romania). In order to understand the climatic signal locked in the two cores, we analyzed the stable isotope composition of the rainfall water, which was subsequently compared with that of the cave ice. Accordingly, d&lt;sup&gt;18&lt;/sup&gt;O in ice in SIC is a proxy for late-autumn through early winter air temperature, while that in FV for summer air temperatures. The analysis of d&lt;sup&gt;18&lt;/sup&gt;O values indicate that on centennial scales, air temperature variability during the last 1000 years was controlled by changes during the winter season, summer temperatures being relatively constant (on these time scales). Contrary, short-term variability (decadal to multi-decadal) was well expressed in both seasons. In summer, the main controlling factors seem to be changes in solar radiation and possibly in the strength of the Atlantic Multidecadal Oscillation, while in winter, the strength of the Siberian High could have acted as the main forcing factor.&lt;/p&gt;


Forests ◽  
2019 ◽  
Vol 10 (9) ◽  
pp. 798 ◽  
Author(s):  
Marian Gabor ◽  
Pavel Beracko ◽  
Vladimir Faltan ◽  
Igor Matecny ◽  
Lukas Karlik ◽  
...  

Managed broadleaf deciduous forests are an important type of forest vegetation in Central Europe, also in the Western Carpathians. These forests are both economically and environmentally valuable. However, little is known about ecological species groups and the inter-specific associations of dominant species in temperate deciduous managed forests in Central Europe. Since the forest stands are in a managed landscape, they are not consistent with the traditionally recognized and used vegetation associations in the Western Carpathians. For these reasons our research contributes to understanding the consequences of broadleaf deciduous forest management. The aim of this research was the determination of ecological species groups and an investigation into the main environmental drivers, in order to explain the distribution of ecological species groups. The numerical TWINSPAN classification was selected to distribute 146 relevés to the five ecological species groups. Of these, 77 relevés were divided into two groups with Fagus sylvatica dominant, while 63 relevés were Quercus petraea dominant. Carpinus betulus, Tilia cordata and Fraxinus excelsior were dominant in 19 relevés. Constrained Analysis of Principal Components was used to explain the vegetation–environment relationship on three transects in the Male Karpaty Mountains. Altitude, pH, Ca, C, K and Mg were selected as the significant environmental drivers responsible for a large part of the species group variability (31.8%). The main requirement for sustainable forest management is knowledge of the vegetation–environment relationship and this research was focused on gaining such understanding. This knowledge can be used as a decision support tool for sustainable management in managed deciduous forests.


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