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岩溶表层带水生动物研究进展

刘伟 周翠英 袁爱华 BRANCELJ Anton

中国岩溶2016,Vol.35Issue(6):712-719,8.
中国岩溶2016,Vol.35Issue(6):712-719,8.DOI:10.11932/karst20160614

岩溶表层带水生动物研究进展

Progress of research on aquatic fauna in epikarst

刘伟 1周翠英 2袁爱华 1BRANCELJ Anton2

作者信息

  • 1. 中山大学工学院,广州510275
  • 2. 中山大学岩土工程与信息技术研究中心,广州510275
  • 折叠

摘要

Abstract

This paper presents the latest progress of research on epikarstic aquifer fauna.The epikarst is not only an essential part of karst formations,but also the most active zone of karstification.It is also the ideal habitat for numerous living things in the karst aquifer.Most faunal samples are taken from percolating water in cave ceilings,water pools within the cave or fissures.The majority of species collected from epikarst are Copepods,as well as some other species,such as Amphipods and Ostracods.These are mainly stygobiont,and also some other terrestrial species.For instance,in the studied Slovenian caves,there are nine stygobiotic copepod species on average in each cave.In order to adapt the epikarstic condition,some parts of their bodies evolve properly.Several geological factors of epikarst,such as the thickness of cave ceiling,the connection between habitats and their size and hydrological factors,including hydrodynamic and hydrochemical characteristics,can impose impacts on the faunal composition and distribution.Although the uniqueness and importance of epikarst has been described by many geologists and biologists,some urgent questions remain unanswered.For example,how to explain the difference between the adjacent communities and how to evaluate the indicators of the copepods in the vadose flow are still expecting more scientific efforts.

关键词

岩溶表层带/淡水甲壳类生物/洞穴滴水/洞穴环境因子

Key words

epikarst/freshwater crustaceans/cave drip water/cave environmental factors

分类

生物科学

引用本文复制引用

刘伟,周翠英,袁爱华,BRANCELJ Anton..岩溶表层带水生动物研究进展[J].中国岩溶,2016,35(6):712-719,8.

基金项目

Slovenian Research Agency Funds (P1-0255) (P1-0255)

Slovenian Research Agency Funds for Young Researchers(1000-11-310196) (1000-11-310196)

中国岩溶

OA北大核心CSCDCSTPCD

1001-4810

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