GRAZER CONTROL AND NUTRIENT LIMITATION OF PHYTOPLANKTON BIOMASS IN 2 AUSTRALIAN RESERVOIRS

Citation
V. Matveev et L. Matveeva, GRAZER CONTROL AND NUTRIENT LIMITATION OF PHYTOPLANKTON BIOMASS IN 2 AUSTRALIAN RESERVOIRS, Freshwater Biology, 38(1), 1997, pp. 49-65
Citations number
46
Categorie Soggetti
Zoology,"Marine & Freshwater Biology
Journal title
ISSN journal
00465070
Volume
38
Issue
1
Year of publication
1997
Pages
49 - 65
Database
ISI
SICI code
0046-5070(1997)38:1<49:GCANLO>2.0.ZU;2-8
Abstract
1. Grazer and nutrient controls of phytoplankton biomass were tested o n two reservoirs of different productivity to assess the potential for zooplankton grazing to affect chlorophyll/phosphorus regression model s under Australian conditions. Experiments with zooplankton and nutrie nts manipulated in enclosures, laboratory feeding trials, and the anal ysis oi in-lake plankton time series were performed. 2. Enclosures wit h water from the more productive Lake Hume (chlorophyll a = 3-17.5 mu g I-1), revealed significant zooplankton effects on chlorophyll a in 3 /6, phosphorus limitation in 4/6 and nitrogen limitation in 1/6 of exp eriments conducted throughout the year. Enclosures with water from the less productive Lake Dartmouth (chlorophyll a = 0.8-3.5 mu g 1(-1)), revealed significant zooplankton effects in 5/6, phosphorus limitation in 5/6 and nitrogen limitation in 2/6 of experiments. 3. While Lake H ume enclosure manipulations of the biomass of cladocerans (Daphnia and Diaphanosoma) and large copepods (Boeckella) had negative effects, sm all copepods (Mesocyclops and Calamoecia) could have positive effects on chlorophyll a. 4. In Lake Hume, total phytoplankton biovolume was n egatively correlated with cladoceran biomass, positively with copepod biomass and was uncorrelated with total crustacean biomass. In Lake Da rtmouth, total phytoplankton biovolume was negatively correlated with cladoceran biomass, copepod biomass and total crustacean biomass. 5. I n both reservoirs, temporal variation in the biomass of Daphnia carina ta alone could explain more than 50% of the observed variance in total phytoplankton biovolume. 6. During a period of low phytoplankton biov olume in Lake Hume in spring-summer 1993-94, a conservative estimate o f cladoceran community grazing reached a maximum of 0.80 day-1, sugges ting that Cladocera made an important contribution to the development of the observed clear-water phase. 7. Enclosure experiments predicted significant grazing when the Cladocera/ Phytoplankton biomass ratio wa s greater than 0.1; this threshold was consistently exceeded during cl ear water phase in Lake Hume. 8. Crustacean length had a significant e ffect on individual grazing rates in bottle experiments, with large Da phnia having highest rates. In both reservoirs, mean crustacean length was negatively correlated with phytoplankton biovolume. The observed upper limit of its variation was nearly twice as high compared to othe r world lakes.