Weald Clay
| Weald Clay | |
|---|---|
| Stratigraphic range: Hauterivian-Barremian, | |
| File:Clay Pit, Clock House, near Capel - geograph.org.uk - 1779315.jpg 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 | United Kingdom |
| Type section | |
| Named for | Weald |
| File:Gallois Geological Map of Wealden District 1965.jpg 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.[1] 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.[2] The climate at the time of deposition is thought to have been semi-arid,[3] and prone to fire.[4] 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
[edit | edit source]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
[edit | edit source]Vertebrates
[edit | edit source]| Vertebrates reported from the Weald Clay | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
|
B. walkeri |
Smokejack Clay Pit | Upper Weald Clay |
Multiple partial skulls, one of which had an associated postcranial skeleton.[5] |
A spinosaurid |
| |
|
H. rudgwickensis |
Rudgwick Brickworks | Upper Weald Clay |
"Vertebrae, partial fore and hindlimbs, osteoderms."[6] |
A dubious[7] genus of nodosaurid ankylosaur belonging to Polacanthinae. Originally named as a species of Polacanthus.[8] |
||
| 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 |
| |
|
V. canaliculatus[9] |
Heathfield | Lower Weald Clay |
A dryosaurid, also known from the Wessex Formation |
|||
| Leptocleidus | L. superstes[10] | NHM R4828 (holotype) | Pliosauroid |
| ||
| Wyleyia[11] | W. valdensis[11] |
|
||||
| Dorsetisaurus | Indeterminate | Keymer Tile Works | ||||
| Sauropoda | Indeterminate | Smokejacks, Bexhill | ||||
| Anura | Indeterminate | Keymer Tile Works | Lower | Maxillary fragment[12] | ||
| Urodela | Indeterminate | Keymer Tile Works | Lower | Atlas vertebra | Has been suggested to have a close relationship with Balveherpeton from Germany.[13] | |
Invertebrates
[edit | edit source]Numerous insect species are known from several localities in the Weald Clay, including Rudgwick Brickworks,[14] Auclaye Brickworks,[15] Smokejacks[16] and Clockhouse Brickworks[17][18][19]
| Invertebrates reported from the Weald Clay | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
| Principiala[20] | P. rudgwickensis | Rudgwick Brickworks | Upper Weald Clay | Single partial fore-wing | An Ithonidae lacewing, the second in Principiala | |
| Englathauma | E. crabbi | Rudgwick Brickworks | BMB 021962/3 almost complete forewing | A englathaumatid scorpionfly | ||
| E. mellishae | Smokejacks | Wing and wing fragments | ||||
| Cretophasmomima[21] | C. traceyae | Smokejacks | Forewing | A stick insect | ||
| Valdicossus | V. mikewebsteri[22] | Smokejacks | Upper | Hindwing | A member of Palaeontinidae | |
| V. chesteri[23] | Cooden Beach | Lower | Hindwing | |||
| Ilerdocossus | I. prowsei [22] | Clockhouse Brickworks | Lower | A member of Palaeontinidae | ||
| Proraphidia | P. hopkinsi[24] | A member of Mesoraphidiidae | ||||
| Turanophlebia | T. anglicana[25] | Dragonfly, member of Tarsophlebiidae | ||||
| Brochocoleus | B. keenani[26] B. tobini | Smokejacks | Upper | Member of Ommatidae | ||
| Diluticupes | D. crowsonae | |||||
| Zygadenia | Z. tuberculata,[27] Z. angliae[28] | |||||
| Cionocoleus | C. elizabethae, C. watsoni [29] C. minimus | |||||
| Omma | O. elongatum | Keymer Tile Works | Lower | |||
Flora
[edit | edit source]| Plants reported from the Weald Clay | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
| Weichselia[4] | W. reticulata | A tree fern | ||||
| Brachyphyllum[4] | Conifer leaves | |||||
| Pagiophyllum[4] | Conifer leaves | |||||
| Pseudofrenelopsis[4] | P. parceramosa | A conifer belonging to the extinct family Cheirolepidiaceae | ||||
See also
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Footnotes
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- ^ a b c d e Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
- ^ "Table 4.1," in Weishampel, et al. (2004). Page 72.
- ^ "Table 17.1," in Weishampel, et al. (2004). Page 367.
- ^ 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
- ^ 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.
- ^ 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
- ^ Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value).
- ^ a b c "10.18 West Sussex, England; 1. Hastings Beds" in Weishampel, et al. (2004). Page 559.
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- ^ 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
- ^ 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
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- ^ 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
- ^ 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
[edit | edit source]- Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp. Lua error in Module:Citation/CS1/Configuration at line 2172: attempt to index field '?' (a nil value)..