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Weald Clay

Geological formation in England


Geological formation in England

FieldValue
nameWeald Clay
imageClay Pit, Clock House, near Capel - geograph.org.uk - 1779315.jpg
captionWeald Clay exposed at Clock House Brickworks
typeGeological formation
ageHauterivian-Barremian,
periodBarremian
prilithologyShale, Mudstone
otherlithologySiltstone, Sandstone, Limestone, Ironstone
namedforWeald
regionEngland
countryUnited Kingdom
unitofWealden Group
subunitsHorsham Stone Member
underliesAtherfield Clay Formation
overliesTunbridge Wells Sand Formation
thicknessup to 460 m
mapGallois_Geological_Map_of_Wealden_District_1965.jpg
map_captionExtent 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 ClayGenusSpeciesLocationStratigraphic positionMaterialNotesImages
Smokejack Clay PitUpper Weald ClayA spinosaurid
Rudgwick BrickworksUpper Weald Clay
IguanodonI. bernissartensisSmokejack Clay PitUpper Weald ClayIguanodontian, also known from the Wessex Formation.
MantellisaurusM. atherfieldensisSmokejack Clay PitUpper Weald ClayIguanodontian, also known from the Wessex Formation
HeathfieldLower Weald Clay
Leptocleidus L. superstesNHM R4828 (holotype)Pliosauroid
WyleyiaW. valdensis
DorsetisaurusIndeterminateKeymer Tile Works
SauropodaIndeterminateSmokejacks, Bexhill
AnuraIndeterminateKeymer Tile WorksLowerlast=Sweetman, S.C; Evans, S. E.title=English Wealden fossilsdate=2011publisher=Palaeontological Associationisbn=978-1-4443-6711-9chapter=Lissamphibians (frogs, salamanders and albanerpetontids)oclc=777385514chapter-url=https://www.researchgate.net/publication/258090858}}
UrodelaIndeterminateKeymer Tile WorksLowerAtlas vertebraHas 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 ClayGenusSpeciesLocationStratigraphic positionMaterialNotesImages
last1=Jepsonfirst1=JElast2=Makarkinfirst2=VNlast3=Jarzembowskifirst3=Eyear=2009title=New lacewings (Insecta: Neuroptera) from the Lower Cretaceous Wealden supergroup of Southern Englandjournal=Cretaceous Researchvolume=30issue=5pages=1325–1338doi=10.1016/j.cretres.2009.07.012}}P. rudgwickensisRudgwick BrickworksUpper Weald ClaySingle partial fore-wingAn Ithonidae lacewing, the second in Principiala
EnglathaumaE. crabbiRudgwick BrickworksBMB 021962/3 almost complete forewingA englathaumatid scorpionfly
E. mellishaeSmokejacksWing and wing fragments
CretophasmomimaC. traceyaeSmokejacksForewingA stick insect
Valdicossuslast1=Lifirst1=Yulinglast2=Jarzembowskifirst2=Edmundlast3=Chenfirst3=Junlast4=Wangfirst4=Bodate=March 2019title=New Palaeontinidae (Insecta: Hemiptera) from the Lower Cretaceous of southern Englandjournal=Cretaceous Researchlanguage=envolume=95pages=297–301doi=10.1016/j.cretres.2018.11.019s2cid=134479224 }}SmokejacksUpperHindwingA member of Palaeontinidae
V. chesteriCooden BeachLowerHindwing
IlerdocossusI. prowseiClockhouse BrickworksLowerA member of Palaeontinidae
ProraphidiaP. hopkinsiA member of Mesoraphidiidae
TuranophlebiaT. anglicanaDragonfly, member of Tarsophlebiidae
BrochocoleusB. keenani B. tobiniSmokejacksUpperMember of Ommatidae
DiluticupesD. crowsonae
ZygadeniaZ. tuberculata, Z. angliae
CionocoleusC. elizabethae, C. watsoni C. minimus
OmmaO. elongatumKeymer Tile WorksLower

Flora

Plants reported from the Weald ClayGenusSpeciesLocationStratigraphic positionMaterialNotesImages
last=Battenfirst=David J.date=June 1998title=Palaeonenvironmental implications of plant, insect and other organic-walled microfossils in the Weald Clay Formation (Lower Cretaceous) of southeast Englandurl=https://linkinghub.elsevier.com/retrieve/pii/S0195667198901161journal=Cretaceous Researchlanguage=envolume=19issue=3-4pages=279–315doi=10.1006/cres.1998.0116url-access=subscription }}W. reticulataA tree fern
BrachyphyllumConifer leaves
PagiophyllumConifer leaves
PseudofrenelopsisP. parceramosaA 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

  1. "Wealden Clay Formation". British Geological Survey.
  2. Radley, Jonathan D. (June 1999). "Weald Clay (Lower Cretaceous) palaeoenvironments in south-east England: molluscan evidence". Cretaceous Research.
  3. 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.
  4. "Table 4.1," in Weishampel, et al. (2004). Page 72.
  5. "Table 17.1," in Weishampel, et al. (2004). Page 367.
  6. 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
  7. 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.
  8. 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
  9. "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. "10.18 West Sussex, England; 1. Hastings Beds" in Weishampel, et al. (2004). Page 559.
  11. Sweetman, S.C; Evans, S. E.. (2011). "English Wealden fossils". Palaeontological Association.
  12. (December 2020). "First salamander from the Lower Cretaceous of Germany". Cretaceous Research.
  13. "Rudgwick Brickworks, Upper Weald Clay (Cretaceous of the United Kingdom)".
  14. "Auclaye Brickworks (BMB collection) (Cretaceous of the United Kingdom)".
  15. "Smokejacks Brickworks (Cretaceous of the United Kingdom)".
  16. "Clockhouse Brickworks (MNEMG collection) (Cretaceous of the United Kingdom)".
  17. "Clockhouse Brickworks (BMNH collection) (Cretaceous of the United Kingdom)".
  18. "Clockhouse Brickworks (BMB collection): Late/Upper Hauterivian, United Kingdom".
  19. (2009). "New lacewings (Insecta: Neuroptera) from the Lower Cretaceous Wealden supergroup of Southern England". Cretaceous Research.
  20. (January 2020). "A new stick insect (Phasmatodea: Susumanioidea) from the Lower Cretaceous Wealden Group of southern England". Cretaceous Research.
  21. (March 2019). "New Palaeontinidae (Insecta: Hemiptera) from the Lower Cretaceous of southern England". Cretaceous Research.
  22. (2008-04-16). "A new genus and species of Palaeontinidae (Insecta: Hemiptera: Cicadomorpha) from the Lower Cretaceous of southern England". Zootaxa.
  23. 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
  24. 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
  25. (August 2013). "Brochocolein beetles (Insecta: Coleoptera) from the Lower Cretaceous of northeast China and southern England". Cretaceous Research.
  26. (January 2015). "Boring beetles are not necessarily dull: New notocupedins (Insecta: Coleoptera) from the Mesozoic of Eurasia and East Gondwana". Cretaceous Research.
  27. 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
  28. 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
  29. 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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