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Biocenotical Classification of the Lithorheophilous Communities in the Karst Running Waters According to the Macro Benthic Fauna

Biocenotical Classification of the Lithorheophilous Communities in the Karst Running Waters... This paper analyses the biocenotical structure of the macro benthic fauna in lithorheophilous communities of karst rivers. A lithorheophilous community on different types of stony substrate was biocenotically defined on the basis of population density and determination of the index of dominance for particular representatives. Accepting today's limnological and biocenotical classifications of running waters (SHADIN; ILLIES; STEFFAN; WACHS) a lithorheophilous community in this work is taken as a choriocenosis (“Teilbiozönose”) which is a composite bio‐association of rhithron eco‐biocenosis. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Acta hydrochimica et hydrobiologica Wiley

Biocenotical Classification of the Lithorheophilous Communities in the Karst Running Waters According to the Macro Benthic Fauna

Acta hydrochimica et hydrobiologica , Volume 15 (5) – Jan 1, 1987

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References (8)

Publisher
Wiley
Copyright
Copyright © 1987 Wiley Subscription Services, Inc., A Wiley Company
ISSN
0323-4320
eISSN
1521-401X
DOI
10.1002/aheh.19870150510
Publisher site
See Article on Publisher Site

Abstract

This paper analyses the biocenotical structure of the macro benthic fauna in lithorheophilous communities of karst rivers. A lithorheophilous community on different types of stony substrate was biocenotically defined on the basis of population density and determination of the index of dominance for particular representatives. Accepting today's limnological and biocenotical classifications of running waters (SHADIN; ILLIES; STEFFAN; WACHS) a lithorheophilous community in this work is taken as a choriocenosis (“Teilbiozönose”) which is a composite bio‐association of rhithron eco‐biocenosis.

Journal

Acta hydrochimica et hydrobiologicaWiley

Published: Jan 1, 1987

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