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Weald Clay
Geological formation in England
Geological formation in England
| Field | Value |
|---|---|
| name | Weald Clay |
| image | Clay Pit, Clock House, near Capel - geograph.org.uk - 1779315.jpg |
| caption | Weald Clay exposed at Clock House Brickworks |
| type | Geological formation |
| age | Hauterivian-Barremian, |
| period | Barremian |
| prilithology | Shale, Mudstone |
| otherlithology | Siltstone, Sandstone, Limestone, Ironstone |
| namedfor | Weald |
| region | England |
| country | United Kingdom |
| unitof | Wealden Group |
| subunits | Horsham Stone Member |
| underlies | Atherfield Clay Formation |
| overlies | Tunbridge Wells Sand Formation |
| thickness | up to 460 m |
| map | Gallois_Geological_Map_of_Wealden_District_1965.jpg |
| map_caption | 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 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 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 | |||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Smokejack Clay Pit | Upper Weald Clay | A spinosaurid | ||||||||||||
| Rudgwick Brickworks | Upper Weald Clay | |||||||||||||
| 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 | ||||||||||
| Heathfield | Lower Weald Clay | |||||||||||||
| Leptocleidus | L. superstes | NHM R4828 (holotype) | Pliosauroid | |||||||||||
| Wyleyia | W. valdensis | |||||||||||||
| Dorsetisaurus | Indeterminate | Keymer Tile Works | ||||||||||||
| Sauropoda | Indeterminate | Smokejacks, Bexhill | ||||||||||||
| Anura | Indeterminate | Keymer Tile Works | Lower | last=Sweetman, S.C; Evans, S. E. | title=English Wealden fossils | date=2011 | publisher=Palaeontological Association | isbn=978-1-4443-6711-9 | chapter=Lissamphibians (frogs, salamanders and albanerpetontids) | oclc=777385514 | chapter-url=https://www.researchgate.net/publication/258090858}} | |||
| 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
| Invertebrates reported from the Weald Clay | Genus | Species | Location | Stratigraphic position | Material | Notes | Images | |||||||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| last1=Jepson | first1=JE | last2=Makarkin | first2=VN | last3=Jarzembowski | first3=E | year=2009 | title=New lacewings (Insecta: Neuroptera) from the Lower Cretaceous Wealden supergroup of Southern England | journal=Cretaceous Research | volume=30 | issue=5 | pages=1325–1338 | doi=10.1016/j.cretres.2009.07.012}} | 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 | C. traceyae | Smokejacks | Forewing | A stick insect | ||||||||||||||||||
| Valdicossus | last1=Li | first1=Yuling | last2=Jarzembowski | first2=Edmund | last3=Chen | first3=Jun | last4=Wang | first4=Bo | date=March 2019 | title=New Palaeontinidae (Insecta: Hemiptera) from the Lower Cretaceous of southern England | journal=Cretaceous Research | language=en | volume=95 | pages=297–301 | doi=10.1016/j.cretres.2018.11.019 | s2cid=134479224 }} | Smokejacks | Upper | Hindwing | A member of Palaeontinidae | ||
| V. chesteri | Cooden Beach | Lower | Hindwing | |||||||||||||||||||
| Ilerdocossus | I. prowsei | Clockhouse Brickworks | Lower | A member of Palaeontinidae | ||||||||||||||||||
| Proraphidia | P. hopkinsi | A member of Mesoraphidiidae | ||||||||||||||||||||
| Turanophlebia | T. anglicana | Dragonfly, member of Tarsophlebiidae | ||||||||||||||||||||
| Brochocoleus | B. keenani B. tobini | Smokejacks | Upper | Member of Ommatidae | ||||||||||||||||||
| Diluticupes | D. crowsonae | |||||||||||||||||||||
| Zygadenia | Z. tuberculata, Z. angliae | |||||||||||||||||||||
| Cionocoleus | C. elizabethae, C. watsoni C. minimus | |||||||||||||||||||||
| Omma | O. elongatum | Keymer Tile Works | Lower |
Flora
| Plants reported from the Weald Clay | Genus | Species | Location | Stratigraphic position | Material | Notes | Images | |||||||||||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| last=Batten | first=David J. | date=June 1998 | title=Palaeonenvironmental implications of plant, insect and other organic-walled microfossils in the Weald Clay Formation (Lower Cretaceous) of southeast England | url=https://linkinghub.elsevier.com/retrieve/pii/S0195667198901161 | journal=Cretaceous Research | language=en | volume=19 | issue=3-4 | pages=279–315 | doi=10.1006/cres.1998.0116 | url-access=subscription }} | W. reticulata | A tree fern | |||||
| Brachyphyllum | Conifer leaves | |||||||||||||||||
| Pagiophyllum | Conifer leaves | |||||||||||||||||
| Pseudofrenelopsis | P. parceramosa | A conifer belonging to the extinct family Cheirolepidiaceae |
Footnotes
References
- Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp. .
References
- "Wealden Clay Formation". British Geological Survey.
- Radley, Jonathan D. (June 1999). "Weald Clay (Lower Cretaceous) palaeoenvironments in south-east England: molluscan evidence". Cretaceous Research.
- Akinlotan, Oladapo O.. (July 2022). "Clay mineral formation and transformation in non-marine environments and implications for Early Cretaceous palaeoclimatic evolution: The Weald Basin, Southeast England". Journal of Palaeogeography.
- "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
- "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".
- "10.18 West Sussex, England; 1. Hastings Beds" in Weishampel, et al. (2004). Page 559.
- Sweetman, S.C; Evans, S. E.. (2011). "English Wealden fossils". Palaeontological Association.
- (December 2020). "First salamander from the Lower Cretaceous of Germany". Cretaceous Research.
- "Rudgwick Brickworks, Upper Weald Clay (Cretaceous of the United Kingdom)".
- "Auclaye Brickworks (BMB collection) (Cretaceous of the United Kingdom)".
- "Smokejacks Brickworks (Cretaceous of the United Kingdom)".
- "Clockhouse Brickworks (MNEMG collection) (Cretaceous of the United Kingdom)".
- "Clockhouse Brickworks (BMNH collection) (Cretaceous of the United Kingdom)".
- "Clockhouse Brickworks (BMB collection): Late/Upper Hauterivian, United Kingdom".
- (2009). "New lacewings (Insecta: Neuroptera) from the Lower Cretaceous Wealden supergroup of Southern England". Cretaceous Research.
- (January 2020). "A new stick insect (Phasmatodea: Susumanioidea) from the Lower Cretaceous Wealden Group of southern England". Cretaceous Research.
- (March 2019). "New Palaeontinidae (Insecta: Hemiptera) from the Lower Cretaceous of southern England". Cretaceous Research.
- (2008-04-16). "A new genus and species of Palaeontinidae (Insecta: Hemiptera: Cicadomorpha) from the Lower Cretaceous of southern England". Zootaxa.
- J. E. Jepson and E. A. Jarzembowski. 2008. [https://www.researchgate.net/publication/242734354_Two_new_species_of_snakefly_Insecta_Raphidioptera_from_the_Lower_Cretaceous_of_England_and_Spain_with_a_review_of_other_fossil_raphidiopterans_from_the_JurassicCretaceous_transition 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
- (August 2013). "Brochocolein beetles (Insecta: Coleoptera) from the Lower Cretaceous of northeast China and southern England". Cretaceous Research.
- (January 2015). "Boring beetles are not necessarily dull: New notocupedins (Insecta: Coleoptera) from the Mesozoic of Eurasia and East Gondwana". Cretaceous Research.
- 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
- Batten, David J.. (June 1998). "Palaeonenvironmental implications of plant, insect and other organic-walled microfossils in the Weald Clay Formation (Lower Cretaceous) of southeast England". Cretaceous Research.
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