Abstract

Amazonian aquatic environments are complex, and their interaction promotes heterogeneous environments that in turn make it difficult to describe the development of patterns. Amazonian floodplain lakes have different environmental and biological responses in similar water periods due to the interannual variation. We evaluated if the interannual variations in the physical–chemical structure and the phytoplankton community promote environmentally and biologically contrasted conditions between similar hydrological periods. Phytoplankton community structure has differences between periods, but these differences do not necessarily promote dissimilarities. Most of the phytoplankton species belong to the same functional groups. The compositions of species and functional groups between sample units inside lakes are variable and may or may not have significant differences in dissimilarity, but both periods are equally heterogeneous. Beta diversity has shown that the replacement of species and functional groups causes a high level of variation between sites, which maintain a high heterogeneity between periods. These variations have different responses for different scales turning the interpretation of patterns for these environments a problematic task. Hence, scale and interannual variability are factors that need to be carefully considered when setting standards to describe the ecological dynamics of floodplain lakes in the Amazonian system.

Highlights

  • Wetlands are essential continental components with fundamental hydrological and ecological functions such as water storage, water-quality improvement, and biodiversity conservation (Mitsch & Gosselink, 2007)

  • The regional scale had the same classes between periods, but at local scales, the phytoplankton group’s representativeness differs between periods (Table 1)

  • We identified 14 functional groups (FGs) in LW1 and 19 functional groups in LW2 periods

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Summary

Introduction

Wetlands are essential continental components with fundamental hydrological and ecological functions such as water storage, water-quality improvement, and biodiversity conservation (Mitsch & Gosselink, 2007). They cover about 14% of the Amazon lowland basin, reaching to 800.000 km during flooding season (Hess et al, 2015). Along the main Solimões/Amazon corridor, floodplains have a predictable and monomodal flood pulse with four distinct periods (flooding, high water, flushing, and low water) commonly considered throughout the seasonal cycle (Prance, 1980; Bonnet et al, 2008; Rudorff et al, 2014a; Bonnet et al, 2017). Floodplain lake biodiversity conservation is a crucial challenge as they are considered as among the most diversified environments in the world (Junk et al, 2010) but increasingly threatened by land-use changes and dam proliferation in the basin (Forsberg et al, 2017)

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