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Palaeoclimatic and site-specific conditions in the early Permian fossil forest of Chemnitz—Sedimentological, geochemical and palaeobotanical evidence
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文摘

Chemnitz fossil forest represents a wet spot in a semi-arid to semi-humid climate.

Different lines of evidence from the palaeosol indicate strong seasonality.

Geochemical data provides MAP of 800–1100 mm/a, but a low amount of weathering.

Palaeosol witnessed different root adaptations of the hygrophilous plant community.

Multi-aged woody arboreal plants show different kinds of tree rings.

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