Abstract

This study verified the existence of longitudinal patterns in species composition, richness, density and biomass of flagellate protozoan in tropical streams and investigated whether the possible zonation patterns are different between two periods of the year. For this, samplings were carried out in three regions from 10 streams, during the summer and winter. The flagellate community may be considered species-rich, because it was represented by 106 taxa, belonging to 8 orders and 1 residual group. The values of density and biomass are greater than those commonly found in other lotic environments, with mean values close to 2.3x104 cels. mL-1 and 150.8 µgC L-1. We did not observe any conspicuous and significant longitudinal pattern of the attributes from flagellates community. Only temporal variations of these attributes were verified. The Pearson Correlation evidenced that this temporal patterns was mainly driven by the nutrients availability, temperature and dissolved oxygen, since, the higher values of species richness, density and biomass were recorded during the winter, when the higher concentrations of nutrients and dissolved oxygen and lower temperatures were registered. In summary, the absence of patterns may be ascribed to the unidirectional and continuous flow from lotic environments.

Highlights

  • Rivers and streams have been considered as open, unidirectional, structurally unstable ecosystems, dynamic in space and in time and with constant interactions with the terrestrial system (STANFORD; WARD, 1993; GILLER; MALMQVIST, 1998)

  • Several authors state that these ecosystems must be studied in three spatial dimensions: horizontal, vertical and lateral (GILLER; MALMQVIST, 1998; PETTS, 2000)

  • The horizontal dimension is one of the main studied (WARD; TOCKNER, 2001; THORP et al, 2006), probably because among the most important theories developed in rivers, the river continuum concept (VANNOTE et al, 1980) was one of the first to be postulated

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Summary

Introduction

Rivers and streams have been considered as open, unidirectional, structurally unstable ecosystems, dynamic in space and in time and with constant interactions with the terrestrial system (STANFORD; WARD, 1993; GILLER; MALMQVIST, 1998). Due to these traits, these ecosystems support a unique and highly specialized biota Several authors state that these ecosystems must be studied in three spatial dimensions: horizontal, vertical and lateral (GILLER; MALMQVIST, 1998; PETTS, 2000). The horizontal dimension is one of the main studied (WARD; TOCKNER, 2001; THORP et al, 2006), probably because among the most important theories developed in rivers, the river continuum concept (VANNOTE et al, 1980) was one of the first to be postulated.

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