Hostname: page-component-78c5997874-xbtfd Total loading time: 0 Render date: 2024-11-05T13:47:30.314Z Has data issue: false hasContentIssue false

Planktonic rotifers of a saline-lowland river :the Salado River (Argentina)

Published online by Cambridge University Press:  15 March 2009

N. Neschuk
Affiliation:
Institute of Limnology «Dr. R. Ringuelet» (CONICET - UNLP), Av. Calchaqui km 23,5 1888 Florencio Varela, Argentina
M. Claps
Affiliation:
Institute of Limnology «Dr. R. Ringuelet» (CONICET - UNLP), Av. Calchaqui km 23,5 1888 Florencio Varela, Argentina
N. Gabellone
Affiliation:
Institute of Limnology «Dr. R. Ringuelet» (CONICET - UNLP), Av. Calchaqui km 23,5 1888 Florencio Varela, Argentina
Get access

Abstract

Seasonal samples of zooplankton were taken during 1997-1999 at fifteen stations in the Salado River basin, and analysed inorder to study the rotifer fauna. Spatio-temporal changes in the rotifer plankton composition were examined in the main channeland its tributaries. The majority of species found are tolerant of a wide range of pH, whereas others prefer neutral to alkalinevalues. The total rotifer plankton density increased downstream from the headwaters to the middle sector of the river. Theassociated shallow lakes and tributaries were an important source of species. Variations in density and number of species wereshown to be associated with conductivity, and species tolerant of high conductivity conditions were especially prevalent (upper7,000 µS cm-1). Rotifer density was influenced by hydrological conditions, which promoted maximum values during low waterperiods and in the high water condition promoted the incorporation of species from shallow lakes connected with the river duringflood events. The species associations found are related to such water parameters as conductivity and nutrient availability andto the presence of ponds and shallow, waterlogged depressions connected in varying extent to the main channel.

Type
Research Article
Copyright
© Université Paul Sabatier, 2002

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)