Pyritisation of plant microfossils from the Devonian Hunsrück Slate of Germany

The extraordinary pyritised fossils of the Hunsrück Slate of Germany provide critical information on marine life in the Devonian. Evidence for terrestrial life is confined mainly to rare incomplete plant macrofossils, often of uncertain affinity. The discovery of plant microfossils preserved as pyrite in-fills of cells with decay-resistant organic walls provides additional evidence of life on land around the margins of the Hunsrück Slate sea. The microfossils include groups of elongate water-conducting cells: some show annular or helical indentations which represent thickenings of the original cell wall, others show casts of bordered pits. Spores, possible sporangia, and marine acritarchs are also present. In most cases pyritisation was rapid enough to prevent collapse of the cells, and they retain their original 3-dimensionality. Wall structures subsequently decayed except where they were resistant enough to survive as an organic residue.