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Weald Clay
Stratigraphic range: Hauterivian-Barremian, 136–125 Ma PreꞒ Ꞓ O S D C P T J K Pg N
Weald Clay exposed at Clock House Brickworks
Type	Geological formation
Unit of	Wealden Group
Sub-units	Horsham Stone Member
Underlies	Atherfield Clay Formation
Overlies	Tunbridge Wells Sand Formation
Thickness	up to 460 m
Lithology
Primary	Shale, Mudstone
Other	Siltstone, Sandstone, Limestone, Ironstone
Location
Region	England
Country	UK
Type section
Named for	Weald
Extent of the Weald Clay within the Weald Basin, shown with horizontal lines

Weald Clay or the Weald Clay Formation is a Lower Cretaceous sedimentary rock unit underlying areas of South East England, between the North and South Downs, in an area called the Weald Basin. It is the uppermost unit of the Wealden Group of rocks within the Weald Basin, and the upper portion of the unit is equivalent in age to the exposed portion of the Wessex Formation on the Isle of Wight. It predominantly consists of thinly bedded mudstone. The un-weathered form is blue/grey, and the yellow/orange is the weathered form, it is used in brickmaking.

The formation was deposited in lagoonal, lacustrine and alluvial conditions that varied from freshwater to brackish. The clay alternates with other subordinate lithologies, notably hard red-weathering beds of ironstone, limestone (Sussex Marble) and sandstones, notably including the calcareous sandstone unit referred to as the Horsham Stone. It has a gradual, conformable contact with the underlying Tunbridge Wells Sand Formation, and has a sharp, unconformable contact with the overlying Atherfield Clay Formation, a shallow marine unit deposited after marine transgression during the Aptian.

Physical properties

The weathered and unweathered forms of the Weald Clay have different physical properties. Blue looks superficially like a soft slate, is quite dry and hard and will support the weight of buildings quite easily. Because it is quite impermeable, and so dry, it does not get broken by tree roots. It is typically found at 750mm down below a layer of yellow clay. Yellow, found on the surface, absorbs water quite readily so becomes very soft in the winter. The two different types make quite different bricks.

Paleofauna

Vertebrates

Vertebrates reported from the Weald Clay
Genus	Species	Location	Stratigraphic position	Material	Notes	Images
Baryonyx	B. walkeri	Smokejack Clay Pit	Upper Weald Clay	Multiple partial skulls, one of which had an associated postcranial skeleton.	A spinosaurid
Horshamosaurus	H. rudgwickensis	Rudgwick Brickworks	Upper Weald Clay	"Vertebrae, partial fore and hindlimbs, osteoderms."	A dubious genus of nodosaurid ankylosaur belonging to Polacanthinae. Originally named as a species of Polacanthus.
Iguanodon	I. bernissartensis	Smokejack Clay Pit	Upper Weald Clay		Iguanodontian, also known from the Wessex Formation.
Mantellisaurus	M. atherfieldensis	Smokejack Clay Pit	Upper Weald Clay		Iguanodontian, also known from the Wessex Formation
Valdosaurus	V. canaliculatus	Heathfield	Lower Weald Clay		A dryosaurid, also known from the Wessex Formation
Leptocleidus	L. superstes			NHM R4828 (holotype)	Pliosauroid
Wyleyia	W. valdensis	West Sussex
Dorsetisaurus	Indeterminate	Keymer Tile Works
Sauropoda	Indeterminate	Smokejacks, Bexhill
Anura	Indeterminate	Keymer Tile Works	Lower	Maxillary fragment
Urodela	Indeterminate	Keymer Tile Works	Lower	Atlas vertebra	Has been suggested to have a close relationship with Balveherpeton from Germany.

Invertebrates

Numerous insect species are known from several localities in the Weald Clay, including Rudgwick Brickworks, Auclaye Brickworks, Smokejacks and Clockhouse Brickworks

See also

• Wealden District
• London Clay
• Oxford Clay
• List of dinosaur-bearing rock formations

Footnotes

1. "Wealden Clay Formation". The BGS Lexicon of Named Rock Units. British Geological Survey. Retrieved 14 December 2014.
2. Radley, Jonathan D (June 1999). "Weald Clay (Lower Cretaceous) palaeoenvironments in south-east England: molluscan evidence". Cretaceous Research. 20 (3): 365–368. doi:10.1006/cres.1999.0156.
3. "Table 4.1," in Weishampel, et al. (2004). Page 72.
4. "Table 17.1," in Weishampel, et al. (2004). Page 367.
5. Raven, T. J., P. M. Barrett, S. B. Pond, and S. C. R. Maidment. 2020. Osteology and taxonomy of British Wealden Supergroup (Berriasian–Aptian) ankylosaurs (Ornithischia, Ankylosauria). Journal of Vertebrate Paleontology. DOI: 10.1080/02724634.2020.1826956
6. Blows, W.T., 2015, British Polacanthid Dinosaurs – Observations on the History and Palaeontology of the UK Polacanthid Armoured Dinosaurs and their Relatives, Siri Scientific Press, 220 pp.
7. Galton, P.M., 2009, "Notes on Neocomian (Late Cretaceous) ornithopod dinosaurs from England - Hypsilophodon, Valdosaurus, "Camptosaurus", "Iguanodon" - and referred specimens from Romania and elsewhere", Revue de Paléobiologie 28(1): 211-273
8. "Reassessment of the Lower Cretaceous (Barremian) pliosauroid Leptocleidus superstes Andrews, 1922 and other plesiosaur remains from the nonmarine Wealden succession of southern England | Oxford Academic". academic.oup.com. Retrieved 16 November 2017.
9. ^ "10.18 West Sussex, England; 1. Hastings Beds" in Weishampel, et al. (2004). Page 559.
10. Sweetman, S.C; Evans, S. E. (2011). "Lissamphibians (frogs, salamanders and albanerpetontids)". English Wealden fossils. Palaeontological Association. ISBN 978-1-4443-6711-9. OCLC 777385514.{{cite book}}: CS1 maint: multiple names: authors list (link)
11. Skutschas, Pavel P.; Kolchanov, Veniamin V.; Schwermann, Achim H. (December 2020). "First salamander from the Lower Cretaceous of Germany". Cretaceous Research. 116: 104606. doi:10.1016/j.cretres.2020.104606. S2CID 225440583.
12. "Rudgwick Brickworks, Upper Weald Clay (Cretaceous of the United Kingdom)". fossilworks.org. Retrieved 17 December 2021.
13. "Auclaye Brickworks (BMB collection) (Cretaceous of the United Kingdom)". Paleobiology Database. Retrieved 26 January 2020.
14. "Smokejacks Brickworks (Cretaceous of the United Kingdom)". Paleobiology Database. Retrieved 26 January 2020.
15. "Clockhouse Brickworks (MNEMG collection) (Cretaceous of the United Kingdom)". fossilworks.org. Retrieved 17 December 2021.
16. "Clockhouse Brickworks (BMNH collection) (Cretaceous of the United Kingdom)". fossilworks.org. Retrieved 17 December 2021.
17. "Clockhouse Brickworks (BMB collection): Late/Upper Hauterivian, United Kingdom". Paleobiology Database. Retrieved 26 January 2020.
18. Jepson, JE; Makarkin, VN; Jarzembowski, E (2009). "New lacewings (Insecta: Neuroptera) from the Lower Cretaceous Wealden supergroup of Southern England". Cretaceous Research. 30 (5): 1325–1338. doi:10.1016/j.cretres.2009.07.012.
19. Xu, Chunpeng; Jarzembowski, Edmund A.; Fang, Yan (January 2020). "A new stick insect (Phasmatodea: Susumanioidea) from the Lower Cretaceous Wealden Group of southern England". Cretaceous Research. 112: 104387. doi:10.1016/j.cretres.2020.104387. S2CID 214327966.
20. ^ Li, Yuling; Jarzembowski, Edmund; Chen, Jun; Wang, Bo (March 2019). "New Palaeontinidae (Insecta: Hemiptera) from the Lower Cretaceous of southern England". Cretaceous Research. 95: 297–301. doi:10.1016/j.cretres.2018.11.019. S2CID 134479224.
21. WANG, BO; ZHANG, HAICHUN; JARZEMBOWSKI, EDMUND A. (16 April 2008). "A new genus and species of Palaeontinidae (Insecta: Hemiptera: Cicadomorpha) from the Lower Cretaceous of southern England". Zootaxa. 1751 (1): 65. doi:10.11646/zootaxa.1751.1.7. ISSN 1175-5334.
22. J. E. Jepson and E. A. Jarzembowski. 2008. Two new species of snakefly (Insecta: Raphidioptera) from the Lower Cretaceous of England and Spain with a review of other fossil raphidiopterans from the Jurassic/Cretaceous transition. Alavesia 2:193-201
23. G. Fleck, G. Bechly, X. Martínez-Delclòs, E. A. Jarzembowski, and A. Nel. 2004. A revision of the Upper Jurassic-Lower Cretaceous dragonfly family Tarsophlebiidae, with a discussion on the phylogenetic positions of the Tarsophlebiidae and Sieblosiidae (Insecta, Odonatoptera, Panodonata. Geodiversitas 26(1):33-59
24. Jarzembowski, Edmund A.; Yan, Evgeny V.; Wang, Bo; Zhang, Haichun (August 2013). "Brochocolein beetles (Insecta: Coleoptera) from the Lower Cretaceous of northeast China and southern England". Cretaceous Research. 44: 1–11. doi:10.1016/j.cretres.2013.03.003. ISSN 0195-6671.
25. Jarzembowski, Edmund A.; Wang, Bo; Zhang, Haichun; Fang, Yan (January 2015). "Boring beetles are not necessarily dull: New notocupedins (Insecta: Coleoptera) from the Mesozoic of Eurasia and East Gondwana". Cretaceous Research. 52: 431–439. doi:10.1016/j.cretres.2014.03.006. ISSN 0195-6671.
26. A. G. Ponomarenko. 2006. On the Types of Mesozoic Archostematan Beetles (Insecta, Coleoptera, Archostemata) in the Natural History Museum, London. Paleontological Journal 40(1):90-9
27. E. A. Jarzembowski, E. V. Yan, B. Wang and H. Zhang. 2013. Ommatin beetles (Insecta: Coleoptera) from the Lower Cretaceous of northeast China and southern England. Terrestrial Arthropod Reviews 6:135-161

References

• Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp. ISBN 0-520-24209-2.

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