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Wealden Group

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(Redirected fromHastings Beds)
Stratigraphic Group in England

Wealden Group
Stratigraphic range:
LateBerriasian-Aptian,140–125 Ma
Coastal exposure of the Wealden Group nearBexhill-on-Sea
TypeGroup
Sub-units
UnderliesLower Greensand Group
OverliesPurbeck Group
ThicknessUp to 850 m in Weald Basin, c. 500 m in Wessex basin, few m in marginal areas
Location
RegionEngland
Country UK
Type section
Named forWeald

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.

Stratigraphy

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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]

Palaeontology

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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

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Pterosaurs reported from the Wealden Group
GenusSpeciesLocationStratigraphic positionMaterialNotesImages
ColoborhynchusC. clavirostris[5]
  • St.-Leonards-on-Sea[5]
Hastings Beds"Anterior portion of rostrum"[5]Anornithocheirid pterosaur.
Coloborhynchus

Dinosaurs

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Dinosaurs reported from the Wealden Group
GenusSpeciesLocationStratigraphic positionMaterialNotesImages
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 BedsForelimbA ?basalmacronarian

Pleurocoelus[13]P. valdensis[13]A dubious basal titanosauriform[13]
TuriasauriaIndeterminateHasting beds?[14]Vertebra[14]
TheropodaIndeterminate
  • West Sussex, East Sussex, Kent[15]
XenoposeidonX. proneneukosArebbachisauridsauropod

Wealden elsewhere in Europe

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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]

References

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  1. ^abJackson (2008)
  2. ^Hopson PM, Wilkinson IP, Woods MA (2008)."A stratigraphical framework for the Lower Cretaceous of England"(PDF). British Geological Survey Research Report , RR/08/03. British Geological Survey.
  3. ^Benson RB, Brusatte SL, Hutt S, Naish D (2009)."A new large basal tetanuran (Dinosauria: Theropoda) from the Wessex Formation (Barremian) of the Isle Of Wight, England".Journal of Vertebrate Paleontology.29 (2):612–615.Bibcode:2009JVPal..29..612B.doi:10.1671/039.029.0202.S2CID 83869634.
  4. ^Weishampelet al. (2004)
  5. ^abcRodrigues T, Kellner AW (2013)."Taxonomic review of the Ornithocheirus complex (Pterosauria) from the Cretaceous of England".ZooKeys (308):1–112.Bibcode:2013ZooK..308....1R.doi:10.3897/zookeys.308.5559.PMC 3689139.PMID 23794925.
  6. ^abcd"10.21 Kent, England; 1. Hastings Beds"in Weishampel, et al. (2004). Page 559.
  7. ^"Table 2.1," in Weishampel, et al. (2004). Page 26.
  8. ^Huene, 1909. Skizze zu einer Systematik und Stammesgeschichte der Dinosaurier [Sketch of the systematics and origins of the dinosaurs]. Centralblatt für Mineralogie, Geologie und Paläontologie. 1909, 12-22.
  9. ^abcd"10.18 West Sussex, England; 1. Hastings Beds" in Weishampel, et al. (2004). Page 559.
  10. ^abcdef"10.19 East Sussex, England; 1. Hastings Beds" in Weishampel, et al. (2004). Page 559.
  11. ^"Table 4.1," in Weishampel, et al. (2004). Page 73.
  12. ^Paul Upchurch, Philip D. Mannion & Michael P. Taylor (2015) The Anatomy and Phylogenetic Relationships of “Pelorosaurus“ becklesii (Neosauropoda, Macronaria) from the Early Cretaceous of England. PLoS ONE 10(6): e0125819. doi:10.1371/journal.pone.0125819http://journals.plos.org/plosone/article?id=10.1371/journal.pone.0125819
  13. ^abc"10.19 East Sussex, England; 1. Hastings Beds" and "10.18 West Sussex, England; 1. Hastings Beds" in Weishampel, et al. (2004). Page 559.
  14. ^abMannion PD (24 January 2019)."A turiasaurian sauropod dinosaur from the Early Cretaceous Wealden Supergroup of the United Kingdom".PeerJ.7: e6348.doi:10.7717/peerj.6348.PMC 6348093.PMID 30697494.
  15. ^"10.19 East Sussex, England; 1. Hastings Beds" and "10.18 West Sussex, England; 1. Hastings Beds" and "10.21 Kent, England; 1. Hastings Beds"in Weishampel, et al. (2004). Page 559.
  16. ^Richter, Annette (2012)."The 'German Wealden' and the Obernkirchen Sandstone – an Introduction".Dinosaur Tracks 2011: an international symposium, Obernkirchen, April 14-17, 2011 : abstract volume and field guide to excursions. Göttingen: Universitätsverlag Göttingen.ISBN 978-3-86395-105-4.OCLC 852208407.
  17. ^Dejax, J.; Pons, D.; Yans, J. (1 April 2007)."Palynology of the dinosaur-bearing Wealden facies in the natural pit of Bernissart (Belgium)"(PDF).Review of Palaeobotany and Palynology. Aspects of the Jurassic and Cretaceous palynology.144 (1):25–38.Bibcode:2007RPaPa.144...25D.doi:10.1016/j.revpalbo.2005.10.004.ISSN 0034-6667.

Further reading

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  • Jackson AA (2008).Bedrock geology UK south. An explanation of the bedrock geology map of England and Wales - 1:625,000 edition. Keyworth, Nottingham:British Geological Survey.ISBN 978-0-85272-586-3.
  • Weishampel DB, Barrett PM, Coria RA, Le Loeuff J, Xu X, Zhao X, Sahni A, Gomani EM, Noto CR (2004). "Dinosaur distribution". In Weishampel DB, Dodson P, Osmólska H (eds.).The Dinosauria.University of California Press, Berkeley. pp. 517–606.

See also

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