Water mite (Acari: Hydrachnidia) diversity and distribution in undisturbed Dinaric karst springs

2018 ◽  
Vol 76 (1) ◽  
pp. 123-138 ◽  
Author(s):  
Ivana Pozojević ◽  
Andreja Brigić ◽  
Sanja Gottstein
Diversity ◽  
2020 ◽  
Vol 12 (9) ◽  
pp. 316
Author(s):  
Ivana Pozojević ◽  
Vladimir Pešić ◽  
Tom Goldschmidt ◽  
Sanja Gottstein

Many studies emphasized the role that water mites play within the invertebrate communities of spring ecosystems, regarding species diversity and its significance within the crenal food web, as well as the specific preferences water mites exhibit towards spring typology. In pristine natural springs with permanent flow, water mites are nearly always present and usually display high diversity. This study aimed to determine whether significant differences in water mite assemblages between rheocrene (river-forming springs with dominant riffle habitats) and limnocrene (lake-forming springs with dominant pool habitats) karst springs could be detected in terms of species richness, diversity and abundance, but also in different ratios of specific synecological groups: crenobiont (exclusively found in springs), crenophilous (associated with springs) and stygophilous (associated with groundwater) water mite taxa. Our research was carried out on four limnocrenes and four rheocrenes in the Dinaric karst region of Croatia. Seasonal samples (20 sub-samples per sampling) were taken at each spring with a 200-µm net, taking into consideration all microhabitat types with coverage of at least 5%. Water mite abundance was found not to differ between morphological spring types. Significantly higher values of species richness and diversity indices were found in rheocrenes compared to limnocrenes, like those usually reported for this type of springs. However, unlike the studies previously reported, in this case, the higher shares of crenophilous and crenobiont water mite individuals were found in limnocrenes. The differences between stygophilous water mite taxa ratios among spring morphotypes were not statistically significant, indicating that the degree of the groundwater/surface water interaction (and water mite interaction therein) does not seem to be directly influenced by spring morphotype. Within this research, 40% of identified water mite species (eight out of twenty) were recorded for the first time in Croatia, thus highlighting again a huge gap in water mite knowledge of karst springs.


2019 ◽  
Vol 28 (2) ◽  
pp. 417-424 ◽  
Author(s):  
Ivana Pozojević ◽  
◽  
Vladimir Pešić ◽  
Sanja Gottstein ◽  
◽  
...  

2013 ◽  
Vol 22 (2) ◽  
pp. 181-188
Author(s):  
P.V. Tuzovskij

Two new water mite species, Torrenticola amplexella and T. krasnodarensis, from running waters of the North Caucasus (Krasnodar Kray) are described with illustrations.


2010 ◽  
Vol 19 (1) ◽  
pp. 23-28
Author(s):  
P.V. Tuzovskij

A larva of the water mite Sperchonopsis reducta Sokolow, 1940 is described. The idiosoma of the larva bears 18 pairs of setae, the dorsal plate has a wide and slightly convex anterior margin and a pointed posterior end; the setae Fch are not longer than the trichobothria Fp and Oi, the setae Pe are shorter and thinner than the setae Pi; the urstigmae are with well developed caps; the capitulum has a long basis and a short rostrum; the pedipalpal tarsus bears three large serrate unequal setae, a single solenidion, and four thin short smooth setae.


2018 ◽  
Author(s):  
Chelsey Kipper ◽  
◽  
Patricia N. Kambesis ◽  
Jason S. Polk
Keyword(s):  

2019 ◽  
Author(s):  
Matthew L. Bell ◽  
◽  
Jill L. Riddell ◽  
Dorothy J. Vesper
Keyword(s):  

Water ◽  
2021 ◽  
Vol 13 (11) ◽  
pp. 1449
Author(s):  
Alena Gessert ◽  
Imrich Sládek ◽  
Veronika Straková ◽  
Mihály Braun ◽  
Enikő Heim ◽  
...  

Estimation of the catchment area of a karst spring is not possible in all areas for various reasons. The Slovak Karst is protected by the highest degree of protection and karst springs are used as a source of drinking water for the second largest city in Slovakia, Košice. From this reason, no results on ionic runoff or chemical denudation have been published from this area and the most appropriate way to obtain information about the denudation rate is to determine the ionic runoff. This paper provides an overview of ionic runoff results based on sampling and analysis of karst water from six springs in the period November 2013–October 2016 (three hydrological years) and periodic measurements. Springs have significantly fluctuated flow rates from 0 L/s in summer and autumn up to 192 L/s, and episodic events during the snow melting and heavy rain in the spring of 2013 are also known (more than 380 L/s). The total value of ionic runoff for the area of 40,847 m3/y.km2 is comparable with the Vracanska Plateau in Bulgaria, which lies at a similar altitude and with a similar amount of precipitation.


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