Diversity and Ecology of Diatoms in Pliocene Deposits of the Tunka Valley (Baikal Rift Zone)

Fossil diatoms are an excellent tool for reconstructing the palaeoenvironmental and palaeogeographic changes involving lacustrine systems. In this work, the diatom content of Pliocene sediments recovered from a core extracted in the Tunka Basin (Baikal Rift Zone, Russia) is described. Revealed by light and scanning electron microscopy, 170 species of diatoms were found. Benthic, alkaliphilic, indifferent, cosmopolitan, and oligosaprobe species predominated. Ecological, geographical, and stratigraphic analysis of diatoms showed two ecozones, differing in taxonomic diversity of species. From the data obtained, palaeoenvironmental conditions of these zone formations have been reconstructed. It was shown that during the period corresponding to sedimentation in Ecozone II, the reservoir was cooler, as suggested by the increase of arctic-alpine taxa. The absence of Baikal Pliocene endemics and the presence of local endemics in the Tunka core indicate that there was no geographical connection between the palaeolake of the Tunka Valley and Lake Baikal during the Pliocene.

Automated summary

This study described the diatom content in Pliocene sediments extracted from the Tunka Basin in Russia, revealing the formation of two ecozones with different taxonomic diversity and corresponding palaeoenvironmental conditions. Analysis of diatoms showed that the reservoir was cooler during sedimentation in Ecozone II, characterized by an increase in arctic-alpine taxa. The absence of Baikal Pliocene endemics and presence of local endemics in the Tunka core suggest no geographical connection between the Tunka Valley palaeolake and Lake Baikal during the Pliocene.