Late Silurian and Early Devonian biostratigraphy in the Hill End Trough and the Limekilns area, New South Wales

The first recorded graptolites from the Chesleigh Formation of the Limekiln s district are Monograptus prognatus, ?M. transgrediens, Pristiograptus sp. cf. P. shearsbyi and Linograptus posthumus, which unequivocally indicate a Pridoli (Late Silurian) age for the formation. The Silurian-Devonian bound ary appears best placed at approximately the boundary between the Chesleigh Formation and the overlying Cookman Formation, despite the presence of the early Lochkovian graptolite Monograptus uniformis uniformis much higher st ratigraphically in the Limekilns Formation. In the Hill End Trough succession, the Turondale Formation has yielded cono donts including Amydrotaxis praejohnsoni, which indicates the delta to pesa vis conodont Zones of late Lochkovian (Early Devonian) age. Conodonts from the upper part of the Cunningham Formation, at a locality in the Trough wes t of Mudgee, include Polygnathus nothoperbonus I P. inversus, indicating th e perbonus zone of middle Emsian age. The base of the Cunningham Formation is diachronous, being late Lochkovian (delta Zone) - the same age as the Tu rondale Formation - on the west flank of the Trough as previously reported, and late Pragian in the east. The youngest faunas found in the unit are la te Emsian.