Ecological traits of dragonfly (Odonata) assemblages along an oligotrophic Dinaric karst hydrosystem
Autor: | Marina Vilenica |
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Rok vydání: | 2017 |
Předmět: |
0106 biological sciences
geography River ecosystem geography.geographical_feature_category biology Ecology 010604 marine biology & hydrobiology Fauna 010501 environmental sciences Aquatic Science Onychogomphus forcipatus biology.organism_classification Odonata Karst Dragonfly 01 natural sciences Habitat Tufa case study tufa barriers environmental factors microhabitats 0105 earth and related environmental sciences |
Zdroj: | Annales de Limnologie - International Journal of Limnology. 53:377-389 |
ISSN: | 2100-000X 0003-4088 |
DOI: | 10.1051/limn/2017019 |
Popis: | Ecological traits of dragonfly larvae in tufa- depositing habitats of the Dinaric karst were studied monthly over a one-year period (2007– 2008). The study encompassed various lotic karst habitats (springs, mountainous rivers, streams, tufa barriers) and microhabitats (angiosperms, mosses, cobbles, sand, silt with leaf litter). The aims of the study were to identify dragonfly composition, abundance and spatial distribution, their habitat and microhabitat preferences, and to determine the most important environmental factors explaining dragonfly assemblages in the studied hydrosystem. The dragonfly fauna was composed of eight species, Onychogomphus forcipatus (Linnaeus, 1758) was the most widespread and the most numerous. Water temperature, ammonium and oxygen concentrations had the highest influence on dragonfly assemblages. The most favorable habitat type were tufa barriers, less favorable were lower lotic habitats, while dragonflies were almost completely absent from upper lotic habitats and their springs. Dragonfly larvae preferred microhabitats with inorganic substrates (i.e. cobbles and sand) and slower water velocity, while they mostly avoided mosses associated with the strongest current. This study provides an important contribution to the knowledge of dragonfly ecology in lotic habitats of the Dinaric karst. |
Databáze: | OpenAIRE |
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