The youngest Palaeozoic deposits of Bornholm are exclusively exposed on the
sea floor at its southeastern coast. Six lithotypes are recognized and gen
etically interpreted: (1) laminated siltstones, (2) mudstones, (3) micro-sc
ale flaser to lenticular bedded siltmudstones, (4) limestones, (5) graded s
andstones and (6) tuffs. Palaeoenvironmental interpretation suggests an off
shore deposition in a deep-water foreland basin influenced by gravity curre
nts and associated sediment reworking processes. The graptolite assemblages
in the mudstones and Pb-Pb dating of single zircons from the tuffs indicat
e a Late Wenlock (Silurian) age. The influence of Caledonian orogenesis on
sedimentation, palaeoenvironment and provenance of the Middle Silurian depo
sits on Bornholm as well as the geological development at the southwest mar
gin of Baltica are discussed generally.