Premium
Brackish water faunas from the St Maughans Formation: The Old Red Sandstone section at Ammons Hill, Hereford and Worcester, UK, re‐examined
Author(s) -
Barclay W. J.,
Rathbone P. A.,
White D. E.,
Richardson J. B.
Publication year - 1994
Publication title -
geological journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.721
H-Index - 54
eISSN - 1099-1034
pISSN - 0072-1050
DOI - 10.1002/gj.3350290405
Subject(s) - geology , devonian , facies , fluvial , paleontology , section (typography) , fauna , deposition (geology) , brackish water , transgressive , archaeology , oceanography , geography , sediment , ecology , salinity , structural basin , advertising , business , biology
The disused railway cutting at Ammons Hill, Hereford and Worcester, exposes a sequence of beds belonging to the Devonian St Maughans Formation of Lochkovian (Gedinnian) age. The beds are of Old Red Sandstone facies, but contain brackish water faunas. These faunas occur at a level generally considered to be above the level of marine influence that affected the older Raglan Mudstone Formation of mainly Přídolí Series age. The section, described by King in 1934, is now overgrown, but was excavated in 1986 by the British Geological Survey during its survey of the Worcester 1:50000 sheet. The evidence of the section calls for slight amendment of Allen's (1985) model of an interrupted transition from marine deposition in Ludlow time to freshwater deposition in Gedinnian time that was complete by the time of the formation of a regionally extensive calcrete palaeosol, the Psammosteus Limestone. Subsequent transgressive events took place before the establishment of apparently wholly fluvial and floodplain environments.