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Oxford Clay
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Oxford Clay is a Jurassic marine sedimentary rock underlying much of South East England, from as far west as Dorset and as far north as Yorkshire. The Oxford Clay is argillaceous (consists of clay) and is of Callovian to lower Oxfordian age.
Oxford Clay appears at the surface around Oxford, Peterborough and Weymouth and is exposed in many quarries around these areas. The top of the Lower Oxford Clay shows a lithological change, where fissile shale changes to grey mudstone.

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Encyclopedia
Oxford Clay is a Jurassic marine sedimentary rock underlying much of South East England, from as far west as Dorset and as far north as Yorkshire. The Oxford Clay is argillaceous (consists of clay) and is of Callovian to lower Oxfordian age.
Oxford Clay appears at the surface around Oxford, Peterborough and Weymouth and is exposed in many quarries around these areas. The top of the Lower Oxford Clay shows a lithological change, where fissile shale changes to grey mudstone. The Middle and Upper Oxford Clays differ slightly, as they are separated by an argillaceous limestone in the South Midlands.
The Callovo-Oxfordian Clay also occurs in the Paris basin (France) and it is a potential host formation to dispose high-level radioactive waste in France.
Palaeontology
The Oxford Clay is well known for its rich fossil record of fish and invertebrates. Many of the fossils are well preserved, occasionally some are found exceptionally well preserved. Animals which lived in the Oxford Clay Sea include ichthyosaurs, cephalopods (such as belemnites), bivalves (such as Gryphaea), and a variety of gastropods.
| Dinosaur incertae cedis of the Oxford Clay |
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| Taxa | Presence | Description | Images |
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Superorder:
- Eggs.
| Stratigraphically present in the Lower Oxford Clay. Geographically located in Cambridgeshire, England. | |
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Ornithischians
| Ornithischians of the Oxford Clay |
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| Taxa | Presence | Description | Images |
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Genus:
- Indeterminate remains.
| Stratigraphically present in the Lower Oxford Clay. Geographically located in Cambridgeshire, England. | |
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Genus:
- Possible indeterminate remains.
| Stratigraphically present in the Lower Oxford Clay. Geographically located in Cambridgeshire, England. | "(=Camptosaurus leedsi)" |
Genus:
- L. durobrivensis
| Stratigraphically present in the Lower Oxford Clay. Geographically located in Dorset and Cambridgeshire, England. | For the Cambridgeshire remains: "(=Stegosaurus priscus, Omosaurus leedsi partim)" |
Genus:
- S. leedsi
| Stratigraphically present in the Lower Oxford Clay. Geographically located in Cambridgeshire, England. | |
Infraorder:
- Indeterminate remains.
| Geographically located in Bedfordshire, England. | "(=?Lexovisaurus sp.)" | |
Sauropods
| Sauropods of the Oxford Clay |
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| Taxa | Presence | Description | Images |
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Genus:
- C. stewarti
| Stratigraphically present in the Lower Oxford Clay. Geographically located in Cambridgeshire, England. | |
Infraorder:
- Indeterminate remains.
- Indeterminate remains.
| Stratigraphically present in the Lower Oxford Clay. Geographically located in Cambridgeshire, England. Geographically located in Wiltshire, England. | "(=Ornithopsis leedsi)" "(=Cetiosaurus sp.)" | |
Theropods
| Theropods of the Oxford Clay |
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| Taxa | Presence | Description | Images |
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Genus:
- E. oxoniensis
| Stratigraphically present in the Middle Oxford Clay. Geographically located in Oxfordshire, England. | |
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Suborder:
- Indeterminate remains.
| Geographically located in Oxfordshire, England. | "(=Megalosaurus sp.)" | |
Uses
Oxford Clay has a porous consistency and is soft and is often used in the making of roads. It is also the source of the Fletton stock brick of which much of London is built. For brick making, the Oxford Clay has the advantage of containing carbon which provides part of the fuel required in firing it so reducing the requirement for an external fuel source.
See also
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