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Antarctic Stream Ecosystems: Variability in Environmental Properties and Algal Community Structure
Author(s) -
HowardWilliams Clive,
Vincent Connie L.,
Broady Paul A.,
Vincent Warwick F.
Publication year - 1986
Publication title -
internationale revue der gesamten hydrobiologie und hydrographie
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.524
H-Index - 52
eISSN - 1522-2632
pISSN - 0020-9309
DOI - 10.1002/iroh.19860710405
Subject(s) - streams , environmental science , biomass (ecology) , nutrient , algal mat , ecosystem , substrate (aquarium) , periphyton , chlorophyll a , hydrology (agriculture) , lake ecosystem , diel vertical migration , ecology , oceanography , algae , geology , biology , botany , computer network , geotechnical engineering , computer science
The variability in physical, chemical and biological properties was examined for a number of glacier melt streams in south Victoria Land, Antarctica. Streams flowed for between one and two months. Stream water temperatures (range = 0–11°C) varied over short (hr) time scales whilst discharges varied considerably between streams (range 0.001–15 m 3 s −1 ) and over diel cycles. Solar radiation and air temperature were major determinants of stream discharge. Variability in discharge was reflected in variability in nutrient chemistry and sediment load. Nitrogen and phosphorus varied considerably between streams; the meltwaters early in summer contained 10–20 times higher levels of dissolved N and P than later in the season. Within stream nutrient levels were modified by dense algal growths and penguin rookeries. Epilithic algal communities were made up predominantly of cyanophyceae which formed mats and crusts. Longitudinal and horizontal variability of species in the communities in selected streams is described. Analyses of algal cover and biomass (chlorophyll a ) show that substrate type and flow rates are of greater importance than nutrients in influencing algal abundance and biomass. In some streams biomass values of over 20 μg Ch. a cm −2 were recorded, much of which remains viable but inactive over the antarctic winter.