On the ability of proglacial lake diatoms to reconstruct Antarctic past ozone changes
Fig 5
Ozone reconstruction model from the modern to the middleHolocene period based on diatom assemblages.
Blue line is the total ozone (DU) measured ar the Faraday/Vernadsky Station, Antarctica. The black line is ozone reconstructed based on four diatom taxa (Gomphonema sp., Humidophila tabellariaeformis, Pinnularia borealis, and Nitzschia cf. kleinteichiana) from Profound lake (left side) and Geographensee lake (right side). Bar charts refer to the relative abundance of diatoms.