Purbeck Group

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Purbeck Group
Stratigraphic range: Tithonian–Berriasian
Purbeck Group.jpg
Strata of the Purbeck Group in Durlston Bay, Dorset
Type Group
Sub-units Lulworth Formation, Durlston Formation and Haddenham Formation
Underlies Wealden Group
Overlies Portland Group
Thickness45 to 120 m in South Dorset, 77 to 186 m in the Weald
Lithology
Primary Mudstone, Limestone
Other evaporites, chert
Location
Region Europe
CountryFlag of the United Kingdom.svg  UK
ExtentSouthern England
Type section
Named for Isle of Purbeck
Location Durlston Bay cliffs
Dorset Geology.png
Exposures of the Purbeck Group in Dorset shown in dark blue

The Purbeck Group is an Upper Jurassic to Lower Cretaceous lithostratigraphic group (a sequence of rock strata) in south-east England. The name is derived from the district known as the Isle of Purbeck in Dorset where the strata are exposed in the cliffs west of Swanage.

Contents

The Purbeck Group is famous for its fossils of reptiles and early mammals. This sequence of rocks has gone by various names in the past including amongst others the Purbeck Beds, Purbeck Formation, Purbeck Limestone Formation and Purbeck Stone. [1]

Rocks of this age have in the past been called the Purbeckian stage by European geologists. The Purbeckian corresponds with the Tithonian to Berriasian stages of the internationally used geologic timescale.

History and stratigraphy

The stratigraphic organisation of the Purbeck Group has varied significantly over time since it was first labelled in 1816 for a section of limestone on the Isle of Purbeck. The labels Purbeck Limestone, Purbeck stone, Purbeck series and Purbeck strata were all used by Webster in 1816, with Purbeck Beds first used by Sir William Buckland in 1818. Works from 136 to 1884 provided some descriptions and labels of the locally-known beds, and the divisions of the Purbeck into upper, middle, and lower units. The label of Lulworth Beds was given to the strata below the Cinder Bed in 1963 by Casey, who called the remaining section the Durlston Beds. These were elevated to the status of Lulworth and Durlston Formations by Thompson in 1975, who introduced the Purbeck Group as their parent unit. Cope and colleagues considered the Purbeck as a formation in 1980, naming it the Purbeck Limestone Formation, while El Shahat and West in 1993 called it the Purbeck Formation. Ensom in 1985 and Clements in 1993 detailed the stratigraphy of the Worbarrow Tout and Durlston Bay sections respectively, with the former considering there to be 12 members in the Purbeck Limestone Formation, while the latter had an additional two members within the Lulworth and Durlston Formations of the Purbeck Limestone Group. The Members of Ensom and Clements were lowered to the status of Beds by Westhead and Mather in 1996 as they were of limited applicability outside of their originally-observed sections, with them only recognizing five members of the Lulworth and Durlston Formations, each encompassing multiple of the Beds of earlier studies. [2]

The British Geological Survey recognises three formations and five members of the Purbeck Group, exposed differently across the span of southern England. In the Wessex Basin (or Vectian Basin) area of Dorset where the Purbeck was first recognized, the younger Durlston Formation can be divided into the Peveril Point Member and Stair Hole Member, while the older Lulworth Formation is divided into the Worbarrow Tout Member, Ridgeway Member, and Mupe Member. Within the Weald Basin, the Lulworth and Durlston Formations can be recognized, but their subdivisions are undifferentiated, while outside the Dorset region the oldest and lowermost Purbeck Limestone below the Lulworth in Wiltshire, Oxfordshire and Buckinghamshire has been given its own status as the Haddenham Formation. [1]

In East Sussex the Purbeck Group is formally subdivided into the Blues and Greys Limestones members [3] The sequence was traditionally divided into three, though along different lines viz. Upper, Middle and Lower. The Upper Purbeck comprises 50 to 60 ft (15 to 18 m). of fresh-water clays and shales with limestones, the Purbeck marble and Unio-bed, in the lower part. The Middle division (50 ft (15 m)), mainly thin limestones with shaly partings, contains the principal building stones of the Swanage district; near the base of this subdivision there is a 5 in (13 cm), bed from which an interesting suite of mammalian remains has been obtained; in this portion of the Purbeck Group there are some marine bands. The Lower Purbeck consists of fresh-water and terrestrial deposits, marls, and limestones (the famous Portland limestone) with several fossil soils known as dirt beds. This division is very extensively exposed on the Isle of Portland, where many of the individual beds are known by distinctive names. The chief building stones of Upwey belong to this part of the Purbeck Group.

Subdivisions of the Purbeck Group in Dorset [1] [2]
Purbeck Group Durlston Formation Peveril Point Member"Upper Purbeck"Upper "Cypris" Clays and Shales Bed
Unio Bed
Broken Shell Limestone Bed
Stair Hole Member"Middle Purbeck"Chief Beef Bed
Corbula Bed
Scallop Bed
Intermarine Bed
Cinder Bed
Lulworth Formation Worbarrow Tout MemberCherty Freshwater Bed
Marly Freshwater Bed
"Lower Purbeck"Soft Cockle Bed
Hard Cockle Bed
Ridgeway Member"Cypris" Freestones Bed
Mupe MemberBroken Beds and basal beds

Correlations

In the past, many geologists have ranged the Purbeck Group with the overlying Lower Cretaceous Wealden Group on account of the similarity of its fresh-water faunas; but the marine fossils, including the fishes, ally the Purbeck more closely with the Upper Jurassic rocks of other parts, and it may be regarded as the equivalent of the upper Volgian of Russia. Contemporaneous rocks are also present in the neighbourhood of Boulogne-sur-Mer, where they are characterized by thin limestones with Cyrena and gypsiferous marls. These French outcrops occur, just like those in England, in the core of the Weald-Artois anticline. Purbeckian aged deposits occur even further south in the Charente. In north-west Germany three subdivisions are recognized in strata of the same age: in descending order Purbeck Kalk, Serpulit and Münder Mergel.

Lithology

Purbeck quarry in southern England Purbeck Quarry - Southern England.jpg
Purbeck quarry in southern England

The Purbeck Group outcrops follow the line of the Jurassic outcrop from Dorset, through the Vale of Wardour, Swindon, Garsington, Brill and Aylesbury. In East Sussex, the Purbeck Group outcrops at three locations north and northwest west of Battle, East Sussex and at Netherfield. They also occur at several other locations east of Heathfield, East Sussex and at Beak's Wood near Burwash. Deposits of evaporite minerals such as gypsum and anhydrite, within the Purbeck Group are mined and processed in Mountfield, East Sussex. [4] In Lincolnshire they are represented in part by the Spilsby Sands and in Yorkshire by portions of the Speeton Clay.

The rocks predominantly comprise calcareous mudstones though also include clays, shales and marls with marly, tuffaceous and shelly limestones, occasional oolitic and sandy strata, and evaporites. Nodules of chert are present in some of the limestones.

The thickness of the formation in Wiltshire is 80 to 90 ft (27 m), but in Dorset it is typically between 45 and 120 metres (148 and 394 ft) thick. In the Weald of East Sussex the Purbeck Group has a typical thickness of between 77 and 186 metres (253 and 610 ft). [5] In most places the Purbeck Group rests conformably upon the Portland Group and it is conformably overlaid by the Wealden Group; but there are in some districts distinct indications that the Portland Group was uplifted and worn away to some extent prior to the deposition of the Purbeck Group.

Use in construction

The building stones of the Purbeck Group have already been mentioned; the Purbeck or Paludina "marble", a grey or greenish limestone full of shells, was formerly extensively employed in cathedrals and churches. Stone tiles or slats were once used locally for roofing from the Lower Purbeck of Portland, Swanage and Swindon. Gypsum was formerly worked from the Lower Purbeck at Swanage.

Palaeoenvironment

Animals by the Purbeck lagoon Purbeck lagoon.jpg
Animals by the Purbeck lagoon

Palaeobiota

Thrombolites in the basal part of the Purbeck Group, Isle of Portland PurbeckFormationPortland.jpg
Thrombolites in the basal part of the Purbeck Group, Isle of Portland

No zonal fossil has been recognized for the British Purbeckian strata, but the horizon is approximately equivalent to that of Pensphinctes transilorius of the European continent. The Purbeckian equivalents of Spilsby and Speeton are in the zone of Belemnites lateralis . Other marine fossils are Hemicidaris purbeckensis and Ostrea distonta , the latter being abundant in the Cinder bed of the Middle Purbeck. The fresh-water mollusca include Viviparus (Paludina), Planorbis , Melanopsis , Unio , Cyrena . A large number of insect genera has been found in the Middle and Lower Purbeck Group.

Dinosaurs ( Owenodon , Echinodon [known from "Isolated skull elements of at least [three] individuals." [6] ]), crocodylians ( Goniopholis , Petrosuchus ), Cimoliosaurus , the plesiosaurs and the chelonians (Chelone, Pleurosternum ) are representative reptiles. The mammals, mostly determined from lower jaws, found in the beds mentioned above include Plagiaulax , Amblotherium , Stylodon , Dorsetodon , Triconodon , Spalacotherium and several others. The isopod crustacean Archaeoniscus brodiei is very common in the Purbeck of the Vale of Wardour.

Reptile remains diagnostic to the genus level (Megalosaurus sp (theropod indet), Opisthias ) are among the fossils that have been recovered from the formation. [7]

Fossil eggs referable to the oogenus Mycomorphoolithus are also known from the Purbeck Group. [8]

The silicified stumps and trunks of cycads and coniferous trees, often surrounded by great masses of calcareous concretions (burrs), are very noticeable in the dirt beds of Portland and near Lulworth. Chara is found in the fresh-water cherts of the Middle Purbeck.

See also

Related Research Articles

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<span class="mw-page-title-main">Isle of Purbeck</span> Peninsula in Dorset, England

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<span class="mw-page-title-main">Durdle Door</span> Natural limestone arch on the Jurassic coast of England

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<i>Owenodon</i> Extinct genus of dinosaurs

Owenodon is a genus of iguanodontian dinosaur known from a partial lower jaw discovered in Early Cretaceous-age rocks of Dorset, United Kingdom, and possibly also Romania and Spain. The first and only definitive specimen was found in the Lulworth Formation of the Purbeck Limestone Group, dating to the middle Berriasian stage. It was first described by Richard Owen as a species Iguanodon, I. hoggii, honouring naturalist A.J. Hogg who had originally collected the fossil. Owen described the mandible as it was, partially embedded in a limestone block, but it was given to the Natural History Museum, London where it was accessioned as NHMUK PV R 2998 and further prepared. Some damage occurred to a tooth crown and part of the bone while stored in the collections. Redescription of I. hoggii by David Norman and Paul Barrett subsequently transferred the species to Camptosaurus in 2002, as well as tentatively referring other camptosaur-like material from the Purbeck beds to the species. The identity of the species was questioned, with Kenneth Carpenter and Yvonne Wilson, and Greg Paul, separating "C." hoggi from Camptosaurus as an intermediate ornithopod, until Peter Galton named the new genus Owenodon for it in 2009. Galton removed the material assigned by Norman and Barrett from Owenodon, but referred isolated teeth from the Bauxite of Cornet, Romania, and the El Castellar Formation of Spain to O. hoggii. The taxon, believed by Galton to be intermediate between Camptosaurus and Iguanodon, is of uncertain relationships, with the limited material preventing clear understanding of its position within ornithopod evolution. Phylogenetic studies have found Owenodon to be more primitive, equivalent to, or more derived than Camptosaurus, but it is often excluded to improve results.

<span class="mw-page-title-main">Geology of East Sussex</span> Overview of the geology of East Sussex

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<span class="mw-page-title-main">Portland Group (geology)</span>

The Portland Group is a Late Jurassic (Tithonian) lithostratigraphic group in South East England. The name is derived from the Isle of Portland in Dorset where the strata are exposed and have been extensively worked. Rocks of this age have in the past been called the Portlandian stage by geologists, which corresponds with the late Tithonian stage of the internationally used geological timescale.

<span class="mw-page-title-main">Geography of Dorset</span>

Dorset is a county located in the middle of the south coast of England. It lies between the latitudes 50.512°N and 51.081°N and the longitudes 1.682°W and 2.958°W, and occupies an area of 2,653 km2. It spans 90 kilometres (56 mi) from east to west and 63 kilometres (39 mi) from north to south.

<span class="mw-page-title-main">Lulworth Formation</span>

The Lulworth Formation is a geologic formation in England. It dates from the late Tithonian to the mid Berriasian. It is a subunit of the Purbeck Group. In Dorset, it consists of three members, which are in ascending order, the Mupe Member, the Ridgway Member, and the Warbarrow Tout Member. The Mupe Member is typically 11 to 16 m thick and largely consists of marls and micrites with interbeds of calcareous mudstone. The Ridgeway Member is about 3 to 7 m thick and consists of in its western portion carbonaceous muds, marls and micrites, in the east the muds are replaced by micritic limestone. The Warbarrow Tout Member is 17 to 39 m thick and consists of limestone at the base and micrite and mudstone for the rest of the sequence, this member is the primary source of the vertebrate fossils within the formation. Elsewhere the unit is undifferentiated.

The geology of West Sussex in southeast England comprises a succession of sedimentary rocks of Cretaceous age overlain in the south by sediments of Palaeogene age. The sequence of strata from both periods consists of a variety of sandstones, mudstones, siltstones and limestones. These sediments were deposited within the Hampshire and Weald basins. Erosion subsequent to large scale but gentle folding associated with the Alpine Orogeny has resulted in the present outcrop pattern across the county, dominated by the north facing chalk scarp of the South Downs. The bedrock is overlain by a suite of Quaternary deposits of varied origin. Parts of both the bedrock and these superficial deposits have been worked for a variety of minerals for use in construction, industry and agriculture.

References

  1. 1 2 3 Hopson, P.M.; Wilkinson, I.P.; Woods, M.A. (2008). "A stratigraphical framework for the Lower Cretaceous of England" (PDF). British Geological Survey Research Report. RR/08/03: 1–77.
  2. 1 2 Ensom, P.C. (2002). "The Purbeck Limestone Group of Dorset, southern England: a guide to lithostratigraphic terms". Special Papers in Palaeontology. 68 (Life and Environments in Purbeck Times): 7–12.
  3. Howitt, Frank (1964). "Stratigraphy and structure of the Purbeck inliers of Sussex (England)". Quarterly Journal of the Geological Society. 120 (1–4): 77–113. doi:10.1144/gsjgs.120.1.0077. S2CID   128814647 . Retrieved 26 September 2010.
  4. Codd, J.W. (2007) Analysis of the distribution and characteristics of landslips in the Weald of East Sussex. MSc dissertation, University of Brighton.
  5. "The BGS Lexicon of Named Rock Units - Purbeck Group". The British Geological Survey. Retrieved 26 September 2010.
  6. "Table 18.1," in Weishampel, et al. (2004). Page 394.
  7. Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp.  ISBN   0-520-24209-2.
  8. Miguel Moreno-Azanza, Jose Ignacio Canudo, and Jose Manuel Gasca. (2015) "Enigmatic Early Cretaceous ootaxa from Western Europe with signals of extrinsic eggshell degradation" Cretaceous Research 56: 617-627.

Wikisource-logo.svg This article incorporates text from a publication now in the public domain :  Chisholm, Hugh, ed. (1911). "Purbeckian". Encyclopædia Britannica . Vol. 22 (11th ed.). Cambridge University Press. pp. 657–658.