Karst Wetlands in the Dinaric Karst

2018 ◽  
pp. 1057-1065 ◽  
Author(s):  
Rosana Cerkvenik ◽  
Andrej Kranjc ◽  
Andrej Mihevc
Keyword(s):  
2016 ◽  
pp. 1-9
Author(s):  
Rosana Cerkvenik ◽  
Andrej Kranjc ◽  
Andrej Mihevc
Keyword(s):  

2016 ◽  
pp. 1-9
Author(s):  
Rosana Cerkvenik ◽  
Andrej Kranjc ◽  
Andrej Mihevc
Keyword(s):  

Author(s):  
Marina Vilenica ◽  
Andreja Brigić ◽  
Michel Sartori ◽  
Zlatko Mihaljević

Research examining mayfly ecology in karst streams and rivers has increased in recent years, though microhabitat preferences remain poorly characterized. We examined mayfly assemblage taxonomy, functional feeding groups and microhabitat preferences in two contrasting lotic Dinaric karst catchments, one pristine and one anthropogenically impacted. At monthly intervals over a one-year period, all major microhabitats (i.e. dominated by boulders, cobbles, sand, silt, mosses, or angiosperms) were sampled at sites spanning springs, upper, middle and lower river reaches, and tufa barriers. In both catchments, mayfly species richness was comparable among microhabitats, while mayfly abundance was highest on mosses and lowest on silt. NMDS ordination did not group assemblages according to microhabitat type, which may reflect the greater influence of physical and chemical water properties. In both catchments and all microhabitats, mayfly assemblages were dominated by grazers/scrapers at upstream sites and by detritivores at downstream sites. Active filter feeders were more abundant in microhabitats with silt substrates and lower current velocities. This study demonstrated that certain mayfly species strongly preferred a specific microhabitat type, reflecting their water current preferences and feeding strategies, while other species shifted between microhabitats, likely in search of food resources and shelter. The results emphasize the importance of habitat heterogeneity in supporting diverse communities in karst rivers.


1964 ◽  
Vol S7-VI (3) ◽  
pp. 382-388 ◽  
Author(s):  
Alexandre Grubic
Keyword(s):  

Abstract The Dinaric karst of Yugoslavia has many deposits of red and white bauxites ranging in age from Triassic to Tertiary. Some deposits in Slovenia and Bosnia are of undetermined age. The number of bauxite beds at different stratigraphic horizons in each locality was determined by the number of periods of emergence. The Ljesev stup-Bijele poljane and Budos areas remained emergent a long time, and have thick deposits. Several horizons of bauxite were formed in Dalmatia, Herzegovina, and Vojnik-Prekornica. A brief emergence resulted in single bauxite deposits in Velebit, Lika, Istria, Grmec, and Bespelj.


2012 ◽  
Vol 58 (No. 9) ◽  
pp. 410-424
Author(s):  
K. Rejšek ◽  
M. Mišič ◽  
F. Eichler

Relic karstic soils in nine localities in the Dinaric Karst in Slovenia, five localities in the Moravian Karst and four localities in the Bohemian Karst were sampled for soil scientific, mineralogical and petrological studies focused on the presentation of descriptive aspects of particular iron compounds. The macroscopy and microscopy of Fe<sup>2+</sup> and Fe<sup>3+ </sup>compounds were determined and an interpretation of these data was performed aimed at describing sources and their palaeotransports. The presented results show that the studied karstic soils have a heterogeneous petrographical and mineralogical composition when, depending on circumstances, hematite does not dominate and goethite prevails over it or it is an opposite. Results from the chosen methods reinforce sources of the new materials as the crucial factor for the studied karstic soils. &nbsp;


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