Oxford Clay Explained

Oxford Clay
Type:Geological formation
Age:Middle to Late Jurassic (Callovian-Oxfordian),
Period:Oxfordian
Prilithology:Claystone
Otherlithology:Mudstone
Namedfor:Oxford
Region:Oxford, Peterborough, Dorset, Yorkshire
Country:England
Unitof:Ancholme Group
Subunits:Peterborough Member, Stewartby Member, Weymouth Member
Underlies:West Walton Formation, Corallian Group
Overlies:Kellaways Formation, Osgodby Formation
Thickness:Up to 185 metres, typically 50 to 70 m on East Midlands Shelf

The Oxford Clay (or Oxford Clay Formation) is a Jurassic marine sedimentary rock formation underlying much of southeast England, from as far west as Dorset and as far north as Yorkshire. The Oxford Clay Formation dates to the Jurassic, specifically, the Callovian and Oxfordian ages,[1] and comprises two main facies. The lower facies comprises the Peterborough Member, a fossiliferous organic-rich mudstone. This facies and its rocks are commonly known as lower Oxford Clay. The upper facies comprises the middle Oxford Clay, the Stewartby Member, and the upper Oxford Clay, the Weymouth Member. The upper facies is a fossil poor assemblage of calcareous mudstones.

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.

Palaeontology

The Oxford Clay is well known for its rich fossil record of fish and invertebrates.[2] Many of the fossils are well preserved, occasionally some are found exceptionally well preserved. Animals which lived in the Oxford Clay Sea include plesiosaurs, marine crocodiles, ichthyosaurs, cephalopods (such as belemnites), bivalves (such as Gryphaea), and a variety of gastropods. Dinosaur eggs are stratigraphically present in the Lower Oxford Clay. Geographically, they are located in Cambridgeshire, England.

Ornithischians

Indeterminate euronithopod remains stratigraphically present in the Lower Oxford Clay and geographically located in Cambridgeshire, England.

Ornithischians of the Oxford Clay
GenusSpeciesLocationStratigraphic positionMaterialNotesImages
CallovosaurusC. leedsi
  • Cambridgeshire
Lower"Femur."[3] An iguanodontian dryosaur.
Lexovisaurus[4] L. durobivensis[5] LowerA holotype pelvis.A stegosaur
Indeterminate[8]
  • Bedfordshire[9]
LoricatosaurusL. priscus
  • Cambridgeshire
LowerA stegosaur.
SarcolestesS. leedsi
  • Cambridgeshire
Lower"Partial mandible."[10] An ankylosaur.

Saurischians

Saurischians of the Oxford Clay
GenusSpeciesLocationStratigraphic positionMaterialNotesImages
CetiosauriscusC. stewarti
  • Cambridgeshire
Lower"Rear half of a skeleton."[11]
Eustreptospondylus[12] E. oxoniensis
  • Oxfordshire
UpperDisarticulated skull and skeleton, with some referred limb elements.[13]
SauropodaIndeterminate
  • Wiltshire[14]
  • Cambridgeshire
The caudal vertebrae from Cambridgeshire were mistakenly considered part of the syntypic series of "Ornithopsis" leedsi by Upchurch and Martin (2003).[15]
TheropodaIndeterminate
  • Oxfordshire
Middle
MetriacanthosaurusM. parkeri
  • Weymouth
Upper

Plesiosaurs

GenusSpeciesLocationMemberAbundanceNotesImages
CryptoclidusC. eurymerusA cryptoclidid
C. richardsoniA cryptoclidid
EardasaurusE. powelliA thalassophonean pliosaurid
Liopleurodon L. feroxA thalassophonean pliosaurid
L. pachydeirusA thalassophonean pliosaurid
MarmornectesM. candrewiA pliosaurid
MuraenosaurusM. leedsiA cryptoclidid
PachycostasaurusP. dawniiA pliosaurid
PeloneustesP. philarchusA thalassophonean pliosaurid
PicrocleidusP. beloclisA cryptoclidid
PliosaurusP. andrewsiA thalassophonean pliosaurid; represents a new genus distinct from Pliosaurus
SimolestesS. voraxA thalassophonean pliosaurid
TricleidusT. seeleyiA cryptoclidid

Pachycormiformes

GenusSpeciesLocationMemberAbundanceNotesImages
Leedsichthys L. problematicus Giant filter feeding pachycormiform
MartillichthysM. renwickaeFilter feeding pachyocormiform
"Hypsocormus""H." tenuirostrisCarnivorous pachycormiform, not closely related to Hypsocormus, and more closely related to Orthocormus

Thalattosuchians

GenusSpeciesLocationMemberAbundanceNotesImages
LemmysuchusL. obtusidensA teleosauroid belonging to the Machimosauridae
CharitomenosuchusC. leedsiA machimosaurid teleosauroid
SteneosaurusS. edwardsiNow referred to Neosteneosaurus.
S. durobrivensisJunior synonym of N. edwardsi.
NeosteneosaurusN. edwardsiA machimosaurid teleosauroid
MycterosuchusM. leedsiA teleosaurid teleosauroid
MetriorhynchusM. superciliosusThis species was referred to a new genus, Thalattosuchus.[16]
ThalattosuchusT. superciliosusA metriorhynchine metriorhynchid
GracilineustesG. leedsiA metriorhynchine metriorhynchid
SuchodusS. brachyrhynchusA geosaurine metriorhynchid
S. durobrivensisA geosaurine metriorhynchid
Tyrannoneustes[17] T. lythrodectikosA geosaurine metriorhynchid

Economic use

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

References

Bibliography

Further reading

Notes and References

  1. Web site: Oxford Clay Formation . . The BGS Lexicon of Named Rock Units . 21 August 2017.
  2. Book: Martill , D.M. . Hudson J.D.. 1991. Fossils of the Oxford Clay. Palaeontological Association.
  3. "Table 18.1," in Weishampel, et al. (2004). Page 396.
  4. Weishampel, et al. (2004). Pages 539-540.
  5. "10.7 Dorset, England; 3. Lower Oxford Clay" and "cambridgeshire">"10.9 Cambridgeshire, England; 1. Lower Oxford Clay," in Weishampel, et al. (2004). Pages 539-540.
  6. "10.9 Cambridgeshire, England; 1. Lower Oxford Clay," in Weishampel, et al. (2004). Page 540.
  7. "10.7 Dorset, England; 3. Lower Oxford Clay," in Weishampel, et al. (2004). Page 539.
  8. Listed as "?Lexovisaurus sp." in "10.10 Bedfordshire, England; 1. Oxford Clay," in Weishampel, et al. (2004). Page 540.
  9. "10.10 Bedfordshire, England; 1. Oxford Clay," in Weishampel, et al. (2004). Page 540.
  10. "Table 17.1," in Weishampel, et al. (2004). Page 367.
  11. "Table 13.1," in Weishampel, et al. (2004). Page 265.
  12. "10.14 Oxfordshire, England; 8. Middle Oxford Clay," in Weishampel, et al. (2004). Page 540.
  13. "Table 4.1," in Weishampel, et al. (2004). Page 72.
  14. "10.14 Wiltshire, England; 4. Oxford Clay," in Weishampel, et al. (2004). Page 540.
  15. Noé LF, Liston JJ, Chapman SD. 2010. ‘Old bones, dry subject’: the dinosaurs and pterosaur collected by Alfred Nicholson Leeds of Peterborough, England. Geological Society, London, Special Publications 343: 49–77.
  16. Young . M.T. . Brignon . A. . Sachs . S. . Hornung . J. . Foffa . D. . Kitson . J.J.N. . Johnson . M.M. . Steel . L. . Cutting the Gordian knot: a historical and taxonomic revision of the Jurassic crocodylomorph Metriorhynchus . Zoological Journal of the Linnean Society . 2021. 192. 2. 510–553. 10.1093/zoolinnean/zlaa092 .
  17. Mark T. Young . Marco Brandalise de Andrade . Stephen L. Brusatte . Manabu Sakamoto . Jeff Liston . 2013 . The oldest known metriorhynchid super-predator: a new genus and species from the Middle Jurassic of England, with implications for serration and mandibular evolution in predacious clades . Journal of Systematic Palaeontology . 11 . 4 . 475–513 . 10.1080/14772019.2012.704948. 85276836 .