Cleal, C.J. & Thomas, B.A. 1996 British Upper Carboniferous Stratigraphy. Geological Conservation Review Series No. 11, JNCC, Peterborough, ISBN 0 412 72780 3.
The original source material for these web pages has been made available by the JNCC under the Open Government Licence 3.0. Full details in the JNCC Open Data Policy
Orchard Farm is the proposed international stratotype for the base of the Yeadonian Stage.
This site, in the southern part of the Pennines Basin, is along a small stream on Orchard Common, 8 km WNW of Longnor, Staffordshire
About 30 m of strata are exposed here
Two bands of mudstone within the Rough 'Rock Formation here have yielded marine fossils. The lowest occurs 13.5 m above the Ringinglow Seam, and contains the ammonoid Cancelloceras cancellatum (Bisat). According to Ramsbottom (1981), three successive assemblages can be recognized within this mudstone: 1 — at the base, containing only Cancelloceras branneroides (Bisat); 2 — in the middle, a mixture of C. cancellatum and Bilinguites superbilinguis Bisat; 3 — at the top, a mixture of C. cancellatum and Agastrioceras carinatum (Frech). This is the classic succession of ammonoids within this marine band, as outlined by Ramsbottom (1969b). It marks the base of the C. cancellatum Zone in the European biostratigraphy, and the base of the Cancelloceras–Branneroceras Superzone.
About 8 m above this, a second band of mudstones has yielded anunonoids. Ramsbottom (1981) does not record identifications, although it is claimed that it is the Cumbriense Marine Band.
Ramsbottom (1981) details pollen and spores derived from 28 levels within this section. The abundant occurrence of Ahrenisporites beeleyensis Neves and Raistrickia fulva Artiiz suggests that the sequence belongs to the Raistrickia fulva–Reticulatisporites reticulatus Zone (Owens in Ramsbottom et al., 1979). No major change can be recognized through the sequence exposed here. This is not surprising, as the base of the fulva–reticulatus Zone is in the middle Marsdenian (Owens et al., 1977), at a rather lower stratigraphical level than is represented here. Perhaps significantly, however, Florinites antiquus Schopf comes in at a short distance below the Cancellatum Marine Band, as its lowest occurrence is usually at about the base of the Yeadonian Stage (Owens, 1982).
The base of the Yeadonian Stage is defined at 'the base of the marine band containing the faunas of the Gastrioceras cancellatum Marine Band' (Ramsbottom, 1981). This is the lower of the two marine bands exposed here.
The Yeadonian Stage was proposed by Hudson (1945), for those strata containing the lowest of the species then assigned to Gastrioceras (the interval then referred to as the G1 Zone). It was named after Yeadon Brick and Tile Works, near Leeds, which provides a good exposure of these strata (see Chapter 9). However, the basal part of the Cancellatum Marine Band seems to be missing from Yeadon, and so the section at Orchard Farm has instead been selected as the proposed stratotype (Ramsbottom, 1981).
The base of the Yeadonian can be identified in many parts of the country by the presence of the marine band containing C. cancellatum. In the Culm Trough, it occurs at Clovelly Coast (see Chapter 3), while in South Wales it occurs on both the south crop, at Tenby–Saundersfoot Coast, and north crop, at Marros Sands and the Vale of Neath (see Chapter 4). In the Central Province it is also very widely distributed. Further north, however, on the Askrigg and Alston blocks, and in Scotland, this marine band is missing.
Orchard Farm is an internationally recognized standard for defining a time plane, 316 million years before the present, and marking the start of the Yeadonian Age.