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 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.

Loch Awe Quarry

[NC 250 158]

Introduction

The quarry at Loch Awe has yielded the most prolific trilobite fauna of the Fucoid Beds Member of the An t-Sròn Formation and is the type locality for one species, Olenellus hamoculus, which has been made the type species of the subgenus Olenellus (Angustolenellus) Palmer and Repina.

The sequence of rocks from quartzites to limestones has long been recognized in the Assynt area (e.g. Macculloch, 1836), although the first recognition of the Fucoid Beds as a separate unit was by Cunningham (1841). Nicol (1857), who examined the strata in the Loch Assynt region, recorded brown shale-like beds, with what appeared to be fucoid (seaweed) impressions, though today these are considered to be Planolites burrows. These, the Fucoid Beds Member of the An t-Sròn Formation, provide an important marker band in the stratigraphical sequence in the north-west Highlands of Scotland and are invaluable for mapping purposes. The biostratigraphically vital Olenellus fauna, indicative of a Lower Cambrian age, was detected by the Geological Survey at several localities (Peach et al., 1907, p. 628). Generally trilobites are rare and difficult to collect; however, while Bowie et al. (1966) were conducting research on the potash content of the Fucoid Beds, Brand (1965) found that beds at Loch Awe Quarry yield large numbers of Olenellus, which were described by Cowie and McNamara (1978).

Description

Loch Awe Quarry, situated by the road south of Inchnadamph, exposes about 7–8 m of the Fucoid Beds Member dipping WSW at about 30° (Figure 12.12). The Fucoid Beds generally consist of dolomitic siltstones, with some dolomitic sandstones and shales, carbonates and rare pisolitic ironstones. The lower part of the face at the back of the quarry shows 3–5 m of relatively massive strata, consisting of dolomitic siltstones and sandstones that are thickly bedded and weather brown. Calcite veins are common on joint surfaces. The sandstones and siltstones are generally a few centimetres thick and show sedimentary structures such as parallel lamination, cross-lamination and occasional wave rip- pies. Structureless, unlaminated mudstones are intercalated. Bioturbation is common, and both vertical burrows and horizontal Planolites burrows occur throughout. A few coarser sandstones show sharp erosive bases. Above the massive beds are 2–3 m of shalier strata, consisting of dark-grey dolomitic siltstones and shales with little internal structure. They break with a conchoidal fracture and contain occasional thin laminae of siltstone and fine sandstone.

This site has yielded a large number of trilobites from various horizons, the best-preserved specimens coming from an unbedded mudstone unit some 1.5 m above the top of the calcareous portion of the Fucoid Beds that forms the main mass of the quarry The dominant species is Olenellus reticulatus Peach (Cowie and McNamara, 1978, p. 625), with rarer O. lapworthi Peach and Horne and a few specimens of O. hamoculus Cowie and McNamara, for which this is the type and only known locality. The trilobites indicate the Bonnia–Olenellus Zone of late Lower Cambrian age, as discussed under Fuaran Mor (see site report). Hyolithids, echinoderm fragments (McKie and Donovan, 1992) and inarticulate brachiopods also occur. Faunal details can be found in Brand (1965), Cowie (1974) and Cowie and McNamara (1978).

Interpretation

The conditions of deposition of the Fucoid Beds are discussed under Fuaran Mor (see site report). The species of Olenellus described by Peach and Horne (1892) and Peach (1894) were based on few specimens, and it is evident from the discussion in Lake (1906–1946, pp. 238–44) that distinction among them was a matter of uncertainty. The large number of cranidia obtained from Loch Awe Quarry (more than 100 specimens of O. reticulatus) enabled Cowie and McNamara (1978) to describe the variation within the species of Olenellus and hence to delimit the species, including their new species O. hamoculus, with greater clarity.

Potash-rich beds are widespread on the western margin of the Iapetus Ocean. Bowie et al. (1966) suggested that the potash in the Fucoid Beds originated from a volcanic source in the underlying Precambrian rocks. However, Swett (1969) pointed to a general lack of volcanic sources in both the Lewisian and the Torridonian and suggested instead that potassium was released during dolomitization from illite, which is present in the overlying limestones.

Conclusions

Loch Awe Quarry is important palaeontologically, in that it exposes a fossiliferous bed that yields the trilobite Olenellus in exceptional abundance, enabling the study of populations of this genus. They are much the most useful fossils for dating the lower part of the north-west Highlands of Scotland as of Early Cambrian age and enable correlation with areas in Greenland, Canada and Spitsbergen.

References

(Figure 12.12) Loch Awe Quarry, showing the Fucoid Beds Member. The lower beds, massive dolomitic sandstones, are overlain by thinly bedded units which include fossiliferous beds with Olenellus (Photo: British Geological Survey photographic collection, D1284.)