scholarly journals Noteworthy lichen species in Poland collected in the Świętokrzyski National Park

2014 ◽  
Vol 38 (1-2) ◽  
pp. 137-147 ◽  
Author(s):  
Anna Łubek

In this paper 25 species of the lichens new to the Świętokrzyski National Park are presented on the basis of recent collection and revision of the herbarial material from this arc. Some of these species are new to the Świętokrzykie Mountains and one have not been recorded in Poland so far.

2014 ◽  
Vol 37 (1-2) ◽  
pp. 93-100 ◽  
Author(s):  
Anna Łubek

Sixteen species of lichenicolous fungi occurring in the Świętokrzyski National Park and its protective zone are presented on the base of recent collection and revision of the herbarial material from this area. Two of the recorded fungi, <em>Stigmidium congestum</em> and <em>Muellerella lichenicola</em>, are very rare in Poland. All presented species are new to thc Świętokrzyskie Mountains.


2014 ◽  
Vol 31 (2) ◽  
pp. 171-174
Author(s):  
Jan Bystrek

A new lichen species <i>Usnea christhinae</i> Bystrek is described from the Patagonia Andes, the reserve upon lake Onelli in the National Park Los Glaciares. It belongs to subgenus <i>Protousnea</i> Motyka emend. Bystrek and is closely related to <i>U. cavernosa</i> Tucker.


Evansia ◽  
2015 ◽  
Vol 32 (4) ◽  
pp. 195 ◽  
Author(s):  
Sarah E. Stehn ◽  
James K. Walton ◽  
Peter R. Nelson ◽  
Celia J. Hampton-Miller ◽  
Carl A. Roland

2015 ◽  
Vol 34 (1) ◽  
pp. 55-63 ◽  
Author(s):  
Tadeusz Ciupa ◽  
Roman Suligowski ◽  
Grzegorz Wałek

Abstract The research described in the paper utilized GIS methods and comparative cartography in order to analyze changes in forest cover in the period 1800-2011 in the Świętokrzyski National Park (76.26 km²) and its buffer zone (207.86 km²). The research was done for predefined elevation intervals, slope gradients, and genetic soil types. Source materials included historical maps as well as a digital elevation model. Changes in forest cover were noted in spatial and temporal terms and were usually linked to morphology and soil type. While the 19th century was characterized by intense deforestation, this process reversed starting in the early 20th century. Nevertheless, forest cover in the study area has still not returned to its state from 1800.


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