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Weald Clay or the Weald Clay Formation is a unit underlying areas of South East , between the and , in an area called the . It is the uppermost unit of the of rocks within the Weald Basin, and the upper portion of the unit is equivalent in age to the exposed portion of the 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 .

The formation was deposited in , lacustrine and conditions that varied from freshwater to . The climate at the time of deposition is thought to have been semi-arid, and prone to fire. The clay alternates with other subordinate lithologies, notably hard red-weathering beds of , limestone () and sandstones, notably including the calcareous sandstone unit referred to as the . 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 .


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
B. walkeriSmokejack Clay Pit Upper Weald ClayMultiple partial skulls, one of which had an associated postcranial skeleton."Table 4.1," in Weishampel, et al. (2004). Page 72.A
H. rudgwickensisRudgwick Brickworks Upper Weald Clay"Vertebrae, partial fore and hindlimbs, osteoderms.""Table 17.1," in Weishampel, et al. (2004). Page 367.A dubiousRaven, 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 genus of nodosaurid belonging to . Originally named as a species of .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.
I. bernissartensisSmokejack Clay PitUpper Weald Clay Iguanodontian, also known from the .
M. atherfieldensisSmokejack Clay PitUpper Weald Clay Iguanodontian, also known from the Wessex Formation
V. canaliculatusGalton, 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): 211-273Heathfield Lower Weald Clay A , also known from the Wessex Formation
L. superstes NHM R4828 (holotype)Pliosauroid
"10.18 West Sussex, England; 1. Hastings Beds" in Weishampel, et al. (2004). Page 559.W. valdensis
  • West Sussex
IndeterminateKeymer Tile Works
IndeterminateSmokejacks, Bexhill
IndeterminateKeymer Tile WorksLowerMaxillary fragment
(2025). 9781444367119, Palaeontological Association.
IndeterminateKeymer Tile WorksLowerAtlas vertebraHas been suggested to have a close relationship with from Germany.


Invertebrates
Numerous insect species are known from several localities in the Weald Clay, including Rudgwick Brickworks, Brickworks, Smokejacks and Clockhouse Brickworks
P. rudgwickensisRudgwick BrickworksUpper Weald ClaySingle partial fore-wingAn lacewing, the second in Principiala !
E. crabbiRudgwick BrickworksBMB 021962/3 almost complete forewingA englathaumatid
E. mellishaeSmokejacksWing and wing fragments
C. traceyaeSmokejacksForewingA !
V. mikewebsteriSmokejacksUpperHindwingA member of !
V. chesteriCooden BeachLowerHindwing !
I. prowsei Clockhouse BrickworksLower A member of Palaeontinidae !
P. hopkinsiJ. 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 A member of !
T. anglicanaG. 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 Dragonfly, member of !
B. keenani B. tobiniSmokejacksUpper Member of !
D. crowsonae
Z. tuberculata, Z. angliaeA. 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!
C. elizabethae, C. watsoni 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 C. minimus!
O. elongatumKeymer Tile WorksLower!


Flora
W. reticulata A tree fern
Conifer leaves
Conifer leaves
PseudofrenelopsisP. parceramosa A conifer belonging to the extinct family Cheirolepidiaceae


See also


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

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