Wealden Group | |
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Stratigraphic range: LateBerriasian-Aptian,140–125 Ma | |
![]() Coastal exposure of the Wealden Group nearBexhill-on-Sea | |
Type | Group |
Sub-units | |
Underlies | Lower Greensand Group |
Overlies | Purbeck Group |
Thickness | Up to 850 m in Weald Basin, c. 500 m in Wessex basin, few m in marginal areas |
Location | |
Region | England |
Country | ![]() |
Type section | |
Named for | Weald |
TheWealden Group, occasionally also referred to as theWealden Supergroup, is agroup (a sequence ofrock strata) in thelithostratigraphy of southernEngland. The Wealden group consists ofparalic tocontinental (freshwater)faciessedimentary rocks ofBerriasian toAptian age and thus forms part of the EnglishLower Cretaceous. It is composed of alternatingsands andclays. The sandy units were deposited in aflood plain ofbraided rivers, the clays mostly in alagoonalcoastal plain.[1]
The Wealden Group can be found in almost all Early Cretaceousbasins of England: its outcrops curve from theWessex Basin in the south to theCleveland Basin in the northeast. It is not found in northwest England andWales, areas which were at the timetectonic highs where no deposition took place. The same is true for theLondon Platform around London andEssex. Offshore, the Wealden Group can reach a thickness of 700 metres.[1] The termsWealden andWealdenfacies are also used as generic terms referring to Early Cretaceous non-marine sequences elsewhere in Europe.
The Wealden Group liesstratigraphically on top of thePurbeck Group, which spans theJurassic-Cretaceous boundary. Within theWessex Basin, the Wealden Group consists of twoformations: theWessex Formation and overlyingVectis Formation. In theWeald Basin, the Wealden Group consists of four formations: theAshdown Formation, theWadhurst Clay Formation, theTunbridge Wells Sand Formation and theWeald Clay Formation.[2] The lower three formations are sometimes collectively referred to as theHastings Beds. InOxfordshire,Buckinghamshire andWiltshire, the Wealden Group is only found as anoutlier on top of hills and only consists of a single formation, theWhitchurch Sand Formation. In Yorkshire, the equivalently agedSpeeton Clay Formation, a marine unit, is present.
On top of the Wealden Group is theLower Greensand Group. The difference between these two groups has been formed by a majoreustatic (global)transgression of the sea. The Greensand (Aptian/Albian in age) consists of marine deposits.
The sequence in the Weald Basin has also been described as asupergroup, containing the Weald Clay Group and Hastings Group.[3]
The Wealden Group formsoutcrops covering a large part of south and south-easternEngland including theIsle of Wight. It takes its name from theWeald region ofKent,Sussex,Surrey andHampshire. It has yielded many fossils, includingdinosaurs likeIguanodon andHypsilophodon.[4] Apart from fossils, it shows many other signs of being deposited in a continental environment, such asmudcracks and -in some rare cases- dinosaur footprints. Taxa included in the table below have an uncertain provenance and cannot be placed into one of the constituent formations, thus they are placed here.
Pterosaurs reported from the Wealden Group | ||||||
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Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Coloborhynchus | C. clavirostris[5] |
| Hastings Beds | "Anterior portion of rostrum"[5] | Anornithocheirid pterosaur. | ![]() |
Dinosaurs reported from the Wealden Group | ||||||
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Genus | Species | Location | Stratigraphic position | Material | Notes | Images |
Thecospondylus[6] | T. horneri[6] |
| Hastings Beds | "Internal mold of sacrum."[7] | Dubious genus that has been variously classified as either a saurischian or ornithischian.[8] It is currently only tentatively regarded as dinosaurian.[6] | ![]() |
Therosaurus[9] | T. anglicus[9] |
| ||||
Altispinax[10] | A. dunkeri[10] |
| Hastings Beds | "Dorsal vertebrae."[11] | ![]() | |
Haestasaurus[12] | H. becklesii[10] |
| Hastings Beds | Forelimb | A ?basalmacronarian | |
Pleurocoelus[13] | P. valdensis[13] | A dubious basal titanosauriform[13] | ||||
Turiasauria | Indeterminate | Hasting beds?[14] | Vertebra[14] | |||
Theropoda | Indeterminate |
| ||||
Xenoposeidon | X. proneneukos | Arebbachisauridsauropod |
The term "Wealden" and "Wealden facies" has been applied to other Lower Cretaceous sequences in Europe, including the "German Wealden", comprising theBerriasian agedBückeberg Formation of the Lower Saxony Basin[16] and in Belgium, where "Wealden facies" has been used as a term to refer to the Barremian-Aptian aged sequences of the Mons Basin, including theSainte-Barbe Clays Formation where large numbers ofIguanodon were found in the 19th century.[17]