Benton, M.J. & Spencer, P.S. 1995. Fossil Reptiles of Great Britain. Geological Conservation Review Series No. 10, JNCC, Peterborough, ISBN 0 412 62040 5.
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New Park Quarry is the source of specimens of fossil crocodiles and dinosaurs, including the theropod Megalosaurus, the sauropod Cetiosaurus and the stegosaur Lexovisaurus. The site is important as one of the oldest Bathonian sites in the world.
New Park Quarry, Longborough, 3 km NNW of Stow-on-the-Wold, has yielded the finest fauna of Mid Jurassic (Bathonian) dinosaurs in Britain this century. The quarry was in operation in the 1920s when the remains of several crocodiles came to light (Richardson, 1929). Around 1935, a collection of well-preserved dinosaur bones, representing several genera, was obtained (Gardiner, 1935), and the British Association for the Advancement of Science sponsored an excavation that produced many more specimens (Gardiner, 1937, 1938).
Reynolds (1939), Galton and Powell (1983) and Galton (1985b) described the stegosaur remains, some of the oldest of that group in the world, but the other material is yet to be studied. The quarry still offers good exposures in the Chipping Norton Limestone Member and could be re-excavated for further reptile finds
H.B. Woodward (1894, pp. 143–4) briefly described the geology of New Park Quarry, and Richardson (1929, p. 89) added a section. Arkell and Donovan (1952, p. 249) gave a fuller account with stratigraphic information:
| Thickness ft | in | |
| Chipping Norton Limestone | ||
| 6. Flaggy oyster limestone. Exogyra sp. | 2 | 0 |
| 5. Marl with oysters, chiefly Exogyra sp. | 10 | |
| 4. False-bedded, white, shelly oolite ?Roundhill Clay | c. 18 | 0 |
| 3. Impersistent seam of clay and locally sandy marl with small irony claystone pellets | nil to | 8 |
| Hook Norton Limestone | ||
| 2. Nodular buff limestones, with dark fossil bones 1–2 feet down. Parkinsonia neuffensis auct. from this bed, teste P.J. Channon | 5 | 0 |
| 1. Brownish and buff limestones with sandy marl partings | seen to 5 | 0 |
The Chipping Norton Limestone (5–6 m thick) consists of wavy-bedded white or cream coloured sandy limestone which weathers to a reddish colour in places. Low-angle cross-beds are present. The rock takes on a more nodular appearance in the lower portions. Richardson (1929, p. 89) reported that the 'black pebble-like bodies' (in bed 3 of Arkell and Donovan 1952) consisted of manganese, limonite, calcium carbonate and phosphate. The lower unit (1–2 m visible; bed 1 of Arkell and Donovan, 1952) is similar to the main limestone, but appears to be less nodular.
Richardson (1929, p. 89) noted crocodiles (9 fragments of a mandible of Steneosaurus and a scute of Teleosaurus subulidens) in the Chipping Norton Limestone (Arkell's bed 4), and the bones collected in the 1930s were found in a hard cream-coloured limestone which was worked for road metal (Reynolds, 1939, p. 193). Arkell and Donovan (1952, p. 249) clearly identify their bed 2 as the source of bones of Steneosaurus and Megalosaurus, and they indicate that the other bones in the British Museum and the Stroud Museum came from this horizon.
The sequence at New Park Quarry spans most of the Chipping Norton Formation, which is dated as belonging to the zigzag Zone, the basal zone of the Early Bathonian (Torrens, in Cope et al., 1980b). The Chipping Norton Limestone (=Chipping Norton Member) is ascribed to the yeovilensis Subzone of the zigzag Zone on the basis of specimens of the ammonite Oppelia (Torrens, 1969b, p. 74). The Hook Norton Limestone (=Hook Norton Member) at New Park Quarry has yielded specimens of the ammonites Parkinsonia neuffensis Oppel and P. subgalatea Buckman (Reynolds, 1939; Arkell, 1951–8, p. 160; Arkell and Donovan, 1952, p. 249), which indicate a zonal assignment to the convergens Subzone (Torrens, 1969b), the lowest Subzone of the zigzag Zone, hence earliest Bathonian (Torrens, 1969b; Cope et al., 1980b, fig. 6a). Thus, some of the crocodiles come from the top of the zigzag Zone, and the dinosaurs and some crocodiles from the base of the zigzag Zone.
The reptile remains from New Park Quarry in museum collections have been prepared so that no matrix remains; hence, nothing can be said of the relationship of the bones to the sediment nor of the relative association of the bones. Nevertheless, it seems evident that all elements were disarticulated and must have been transported at least a short distance. There is no sign of major abrasion to the bones, although some delicate processes have been lost.
The reptilian fauna from New Park Quarry was described by Reynolds (1939), and the species are listed together with a note of major specimens in the BMNH, BGS(GSM) and SDM. The Stroud Museum display of these specimens is described by Walrond (1976):
Archosauria: Crocodylia: Thalattosuchia:
Steneosauridae
Steneosaurus cf. subulidens (Phillips, 1871) BMNH R.6307; BGS(GSM) 37520–2 (mentioned, Richardson 1929, p. 89); SDM 44.42, 44–8, 51–7, 59–68
Dinosauria: Saurischia: Theropoda:
Megalosauridae
Megalosaurus sp. BMNH R.9666–76, R.9678–9, R.9681–7, R.9689–700; SDM 44. 1, 4–10, 12–5, 18, 21, 23–6
Dinosauria: Saurischia: Sauropoda: Cetiosauridae
Cetiosaurus sp. SDM 44. 30–40
Dinosauria: Ornithischia: Stegosauria: Stegosauridae
Lexovisaurus? vetustus (Huene, 1910) SDM 44. 41; BMNH R.5838
The remains of the marine crocodile Steneosaurus include skull bones, a braincase, several partial snouts, isolated teeth, scutes, vertebrae and a scapula. The New Park crocodile evidently had a skull 0.3–0.6 m long and probably a total body length of 1.5–3.0 m, thus a fairly large animal. Comparisons are difficult because of the confused taxonomy of Jurassic marine long-snouted crocodiles and, in particular, the distinction between the genera Pelagosaurus, Steneosaurus and Teleosaurus and the multiplicity of their included species (Westphal, 1962; Steel, 1973). Bathonian species include S. boutilieri, T. cadomensis, T. geoffroyi and T. gladius from the 'Fullers Earth' and 'Great Oolite' of Normandy; S. brevidens, S. latifrons, T. cadomensis and T. subulidens from the 'Great Oolite' of Oxfordshire and Northamptonshire; and S. stephani from the Cornbrash of Closworth, Somerset. All of these specimens come from the Mid or Late Bathonian, younger than the New Park material.
The remains of Megalosaurus include a good sacrum, some caudal vertebrae, a rib, two coracoids, a scapula, a humerus, three ischia, a femur, a metatarsal and a partial lower jaw. The postcranial bones are well preserved, and the lower jaw shows seven teeth in various stages of growth. Other Mid Jurassic material of Megalosaurus is known from the Upper Inferior Oolite of Sherborne, Dorset (M. hesperis Waldman, 1974; M. nethercombensis Huene, 1923), the Stonesfield Slate (sensu lato) of Oxfordshire, Gloucestershire and Dorset (M. bucklandi Meyer, 1835; M. bradleyi Woodward, 1910; M. incognitus (Huene, 1932)), the Oxford Clay of Dorset (M. parkeri Huene, 1926) and the Bathonian of Morocco (M. mersensis Lapparent, 1955). The New Park material could belong to any of these species, or to some other.
The bones of the sauropod Cetiosaurus from New Park Quarry include ribs, a coracoid and a pair of ischia. Because of their size (the ischia are 1.0 m long), these specimens undoubtedly belong to Cetiosaurus, but they cannot be assigned to a species since the taxonomy is in need of revision. At least eleven species have been described from the Mid and Late Jurassic of England, France and Morocco, and the Early Cretaceous of England. The Mid Jurassic forms are C. rugulosus (Owen, 1841), C. oxoniensis Phillips, 1871 and C. glymptonensis Phillips, 1871 from the 'Great Oolite' of Wiltshire, Gloucestershire, Oxfordshire and Northamptonshire, and C. mogrebiensis Lapparent, 1955 from the Bathonian of Morocco. It has never been made clear what the diagnostic characters of each species are supposed to be. The New Park sauropod is slightly older than all of these forms.
The 'dermal plates of Stegosaurus' from New Park represent some of the earliest records of stegosaurid dinosaurs. Galton (1983c) and Galton and Powell (1983) described a dorsal vertebra (OUM J29770) and a cervical centrum (OUM J29827) from Sharps Hill, Oxfordshire as the oldest British stegosaurid, and this claim was repeated by Boneham and Forsey (1991) who reported further stegosaur remains from Sharps Hill. However, the Sharps Hill Member lies partly in the progracilis Zone, the earliest zone of the Mid Bathonian, and partly in the tenuiplicatus Zone, the topmost zone of the Early Bathonian (Torrens, 1968; Torrens in Cope et al., 1980b), hence above the Chipping Norton Formation. Therefore, the New Park stegosaur finds are one or two ammonite zones older than those from Sharps Hill, and in, any case, Tatisaurus oehleri, from the Lower Lufeng Formation (Sinemurian–Hettangian) of Yunnan Province, China, hitherto regarded as an unidentifiable ornithischian, may be a true stegosaur (Dong, 1990).
Reynolds (1939) referred the two large dermal plates to the North American genus Stegosaurus, but Galion et al. (1980, p. 41) disputed this referral and suggested that the plates were probably the sacral ribs of a sauropod. However, later, Galton and Powell (1983) and Galton (1985b), in their reviews of Bathonian stegosaurs from England, provisionally reassigned the specimens to the Stegosauridae. They noted that the plates were reasonably massive when compared with the complete series of plates of Stegosaurus and the few known plates of Lexovisaurus, and tentatively referred them to Lexovisaurus ?vetustus (Huene, 1910). The New Park stegosaur must have been large, since the plates are 0.25 m high.
Stegosaurs have been reported from higher in the British Mid Jurassic, from the Lower Oxford Clay (Callovian) of the Peterborough area. Hulke (1887) noted remains of a stegosaur which he termed Omosaurus (=Dacentrurus), believing it to come from the Kimmeridge Clay; these represent Lexovisaurus durobrivensis (Galion, 1985b). Hulke also reported armour plates, but these turn out to be from the giant teleost fish Leedsichthys (Martill, 1988). Stegosaur armour plates were later found in the area. A second Oxford Clay stegosaur was 'Stegosaurus' priscus from Fletton (Nopsca, 1911), synonymized by Galton (1985b) with L. durobrivensis. Other isolated remains of this species have been reported from the Lower Oxford Clay of Whittlesey and Weymouth.
The fossil reptile sites nearest in age to New Park are Oakham Quarry
Richardson (1929, p. 88) recorded a vertebra of Megalosaurus (BGS(GSM) 37523) from a quarry in the Chipping Norton Formation in a field near the Fosse Way ?
The New Park stegosaur (Lexovisaurus? vetustus) is also known from isolated remains in the Lower Cornbrash (discus Subzone, Late Bathonian of Oxfordshire) and from the Sharps Hill Formation, Oxfordshire (tenuiplicatus Zone; latest Early Bathonian) (Galion, 1985b).
Elsewhere, the crocodiles are comparable with those from the Fuller's Earth of Caen and Calvados, Normandy (?Early/Mid Bathonian), and the megalosaur and cetiosaur with remains of these forms from the Bathonian of El Mers in the Moyen Atlas of Morocco (Steel, 1970, pp. 36, 64–5).
New Park Quarry is a very important site for terrestrial fossil reptiles, especially in view of its age. Several other sites in the Chipping Norton Limestone have yielded isolated reptile remains, but the fauna from New Park Quarry is by far the richest for large-sized reptile remains. It is comparable to many of the younger and better known sites in the Mid and Late Bathonian north of Oxford and at Eyford, Gloucestershire. The preservation of the reptiles from New Park Quarry is excellent. They will be of great value in assessing the relationships of early theropods and sauropods. The dermal plates from New Park may be the oldest remains of true stegosaurids in the world. The fact that the fossils were discovered this century suggests that more may be forthcoming if the site is excavated and enhances the conservation value.