Rushton, A.W.A., Owen, A.W., Owens, R.M. & Prigmore, J.K. 2000. British Cambrian to Ordovician Stratigraphy. Geological Conservation Review Series No. 18, JNCC, Peterborough, ISBN 1 86107 4727.
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The limestones and flags exposed here form part of the 'Narberth Group' of Addison, and until his work in the early 1970s (largely unpublished), they were considered to be wholly of Llandeilian age. In the upper part of the sequence Addison recognized trilobite faunas with taxa common to the Costonian Stage of the Caradoc of south Shropshire (see Coston site report). This section has thereby acquired national importance as one that shows the relationship of the type Llandeilo sequence of South Wales with that of the Caradoc of Shropshire in a continuous succession in the shelly facies. Its significance has been enhanced by more recent work on other groups, such as conodonts and ostracods.
The limestones of the Narberth Group were long quarried in the vicinity of Llan-mill and Lampeter Velfrey (Strahan et al., 1914, p. 32), and a composite succession can be constructed from the numerous disused quarries in the area. Murchison (1839; p. 396) recognized their Llandeilo age, and Strahan et al. (1914) also included them within the Llandeilo Series. However, the faunas were little studied until Spjeldnaes (1963) described silicified fossils (trilobites, bryozoans and ostracods) from a slab of limestone from an unspecified locality at Llan-mill. On the basis of the trilobites and unsilicified brachiopods he suggested a late Llanvirn or early Llandeilo age (now Abereiddian–Llandeilian) but noted that the ostracods and bryozoans resembled more those from the Caradoc. Addison (1974) described the geology of the area in detail in an unpublished PhD thesis, although his main conclusions were published as a note in Williams et al. (1972, p. 36) and reported in Bassett et al. (1974, p. 13), who reproduced Addison's geological map of the area. Addison recognized the presence at Bryn-banc of trilobites like those from the lowest Caradoc Sandstone (Costonian Substage) of south Shropshire. Thus this section affords a critical link between Shropshire and South Wales, and along with other sections nearby (see below) demonstrates in a shelly facies the passage from the classic Llandeilo into the Caradoc, whose base is unconformable in Shropshire.
The importance of Addison's work at Bryn-banc and nearby localities has been emphasized by subsequent work on, for example, the conodonts by Bergström et al. (1987) and the ostracods by Jones (1986–1987), and on its potential as a boundary stratotype by Whittington et al. (1984), and Fortey et al. (1991 and 1995). If the recommendations of the latter are accepted, the base of the Caradoc Series will be drawn formally at the base of the gracilis Zone, a level well down in the Llandeilo succession in South Wales. However, Bryn-banc remains the prime candidate to define the base of the Costonian, which, on the recommendations of Fortey et al. (1995) becomes the upper substage of the Aurelucian Stage.
Some 70 m of argillaceous limestones and flags, faulted in places, are exposed at Bryn-banc Quarry and have yielded a diverse fauna of trilobites, brachiopods, ostracods, conodonts and bryozoa. From beds near the top of the sequence, Addison (in Williams et al., 1972; in Bassett et al., 1974) reported the trinucleid trilobite Costonia elegans Dean and also other unde-scribed marrolithine trinucleids that are different from any from the Llandeilo Flags at Llandeilo. C. elegans occurs in the Costonian of south Shropshire, whilst an undescribed mar-rolithine resembles Marrolithus ventriculatus Whittard, which occurs in the Costonian Spy Wood Grit in the Shelve area (see site reports for Spy Wood and Aldress dingles). Dr R. Bettley (pers. comm., March 1998) has recovered Orthograptus apiculatus Elles and Wood from the upper part of the quarry; he notes that the presence of this species also affords correlation with the Spy Wood Grit and is a good indicator for the top of the gracilis Zone (see also Hughes, 1989, p. 67). Further, an undescribed species of Marrolithoides from the middle of the Bryn-banc sequence occurs at the top of the Llandeilo Flags at Llandeilo.
Bergström et al. (1987) provided data which suggest that the base of the Amorphognathus tvaerensis conodont zone lies in the middle to upper part of the Bryn-banc sequence; the position in the evolutionary range of specimens of Eoplacognathus elongatus (Bergström) from this locality places them within the lower part of the Baltognathus variabilis Subzone, which is coeval with the middle part of the gracilis graptolite zone. The ostracods contain species that range throughout the sequence (e.g. Gunnaropsis narberthensis Jones and Latebina pseudantra Jones) or are confined to the 'Costonian' part (e.g. Varilatella (Redacta) coronata Jones and Conchoprimitiella papilalata Jones) (Jones, 1986–1987). Although these species have not been reported outside South Wales, Piretopsis (Protallinnella) salopiensis (Harper), which occurs in the Narberth Group at Lampeter Velfrey at the same horizon as that exposed in Bryn-banc, has been recorded from the Costonian Stage in the Shelve and south Shropshire areas.
Taken together, the trilobite, conodont and ostracod evidence indicates firmly the presence of correlatives of the Costonian Stage at Bryn-banc. Together with nearby sections at HenIlan
Wherever the base of the Caradoc Series is formally drawn, the Bryn-banc section will remain vital in the regional correlation between successions in South Wales and in Shropshire; it is likely to become the stratotype for the base of the Costonian Substage. Bassett and Hughes (in Fortey et al. 1991, p. 17) pointed out that selection of the base of the tvaerensis Biozone at Bryn-banc as the base of the Caradoc Series would protect the traditional interpretation of the boundary between the Caradoc and Llandeilo series. Although this is now unlikely to be adopted, following the proposal by Fortey et al. (1995) to adopt a lower level for this boundary, Bryn-banc remains an important section for securing the correlations given above.
Bryn-banc Quarry is nationally valuable because it provides faunas critical for correlating the Aurelucian successions in South Wales and Shropshire and is the principal candidate section for defining the base of the Costonian Substage.