Biomarker and carbon isotope data from the 1st Mid-Polish and 2nd Lusatian lignite seams of the Konin Basin (Poland) re-evaluated to reconstruct vegetation dynamics during the Miocene Climatic Optimum
Abstract
This study re-evaluates previous results based on analyses of fossil wood (xylites) from the 2nd Lusatian lignite seam (LLS-2) and xylites and detritic lignite samples from the 1st Mid-Polish lignite seam (MPLS-1), and outlines temporal and spatial differences in vegetation and depositional environments. Evidence for varying contributions of gymnosperms and angiosperms during peat accumulation comes from the biomarker and carbon isotopic composition of detritic lignite from MPLS-1. The investigated woody macrofossils (xylites) from all deposits (Lubstów, Adamów, Jóźwin IIB, Tomisławice) were derived from conifers. Slightly lower contributions of Cupressaceae and a greater contribution of Pinaceae in the peat-forming environment during deposition of LLS-2 are indicated by higher average abundance of tricyclic diterpanes (abietane-type) and lower contents of phyllocladanes. A higher groundwater table in the area of the Jóźwin IIB mine is indicated by enhanced gelification and lower cellulose content of xylites. Cellulose decomposition and contamination by inherent detritic lignite affect the δ13C values of fossil wood. Variations in δ13C values of wood cellulose were most probably caused by differences in water availability to conifers, associated with highly dynamic landscape evolution, including changing river flow directions, flood frequency, and crevasse-splay formation. Slightly higher average δ13C values of fossil wood cellulose during deposition of LLS-2, together with a similar trend observed in tree stumps from the Lower Rhine Basin, suggest episodically lower groundwater tables in the mires, probably related to variations in precipitation.
© 2026 Achim Bechtel, Doris Groß, Andreas Lücke, published by Adam Mickiewicz University
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