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99-574: The Greensand Ridge Walk is a long-distance walk of 40 miles (64 km) that traverses the county of Bedfordshire in England, with brief sections in the neighbouring counties of Cambridgeshire and Buckinghamshire . Its southern endpoint is at Leighton Buzzard and the route runs north-east to finish at Gamlingay . As can be inferred from the name, the walk follows the Bedfordshire Greensand Ridge (not to be confused with

198-646: A 40-mile (64  km) walk traversing the county from Leighton Buzzard at the southern endpoint and Sandy, Bedfordshire / Gamlingay in southern Cambridgeshire to the east; this is called the Greensand Ridge Walk . For cyclists, there is a parallel route called the Greensand Cycle Way that follows minor country roads. Jurassic The start of the Jurassic was marked by the major Triassic–Jurassic extinction event , associated with

297-655: A 70 km diameter impact structure buried beneath the Kalahari desert in northern South Africa. The impact is dated to the Tithonian, approximately 146.06 ± 0.16 Mya. Another major structure is the Puchezh-Katunki crater , 40 kilometres in diameter, buried beneath Nizhny Novgorod Oblast in western Russia. The impact has been dated to the Sinemurian, 195.9 ± 1.0 Ma. At the beginning of the Jurassic, all of

396-499: A dominant component of Jurassic floras. The Late Triassic and Jurassic was a major time of diversification of conifers, with most modern conifer groups appearing in the fossil record by the end of the Jurassic, having evolved from voltzialean ancestors. Araucarian conifers have their first unambiguous records during the Early Jurassic, and members of the modern genus Araucaria were widespread across both hemispheres by

495-683: A key part in the life of the British nation during the Second World War as the church of the BBC. The Millbrook Proving Ground , near Junction 13 of the M1, has 70 kilometres (43 miles) of varied vehicle test tracks. Bedfordshire is home to Premier League team Luton Town F.C. and the Ampthill RUFC and Bedford Blues rugby teams, amongst other various sporting teams. Bedfordshire boasts

594-647: A kink in one of the plate boundaries, resulting in the formation of the Pacific Plate at the centre of the junction. During the Middle to early Late Jurassic, the Sundance Seaway , a shallow epicontinental sea , covered much of northwest North America. The eustatic sea level is estimated to have been close to present levels during the Hettangian and Sinemurian, rising several tens of metres during

693-576: A range of further education courses. Additionally, Stella Mann College is a private college which offers a range of further education courses relating to the performing arts . There are a number of independent schools , many of which have links to the Harpur Trust . These include Bedford School , Bedford Modern School and Bedford Girls' School . In Central Bedfordshire, the school systems in Dunstable and Sandy have been re-organised into

792-453: A result of high ocean acidity and temperature inhibiting its mineralisation into apatite; the abundance of phosphorus in marine environments caused further eutrophication and consequent anoxia in a positive feedback loop. The end-Jurassic transition was originally considered one of eight mass extinctions, but is now considered to be a complex interval of faunal turnover, with the increase in diversity of some groups and decline in others, though

891-449: A three-tier education system, though its organisation of infant, junior and high schools mirrors the traditional transfer age into secondary education of 11 years. However, most of Luton's high schools do not offer sixth-form education. Instead, this is handled by Luton Sixth Form College , though Barnfield College and Cardinal Newman Catholic School also offer a range of further education courses. There are two universities based in

990-492: Is Austrohamia minuta from the Early Jurassic (Pliensbachian) of Patagonia, known from many parts of the plant. The reproductive structures of Austrohamia have strong similarities to those of the primitive living cypress genera Taiwania and Cunninghamia . By the Middle to Late Jurassic Cupressaceae were abundant in warm temperate–tropical regions of the Northern Hemisphere, most abundantly represented by

1089-477: Is Luton (225,262), and Bedford is the county town . The county has an area of 1,235 km (477 sq mi) and had a population of 704,736 at the 2021 census. Its other towns include Leighton Buzzard , Dunstable , Biggleswade , Houghton Regis , and Flitwick . Much of the county is rural. For local government purposes, Bedfordshire comprises three unitary authority areas: Bedford , Central Bedfordshire , and Luton. The county's highest point

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1188-466: Is 243 m (797 ft) on Dunstable Downs in the Chilterns . The first recorded use of the name in 1011 was " Bedanfordscir ", meaning the shire or county of Bedford, which itself means "Beda's ford" (river crossing). Bedfordshire was historically divided into nine hundreds : Barford , Biggleswade , Clifton , Flitt , Manshead , Redbornestoke , Stodden , Willey , Wixamtree , along with

1287-460: Is a stub . You can help Misplaced Pages by expanding it . Bedfordshire Bedfordshire ( / ˈ b ɛ d f ər d ʃ ɪər , - ʃ ər / ; abbreviated Beds ) is a ceremonial county in the East of England . It is bordered by Northamptonshire to the north, Cambridgeshire to the north-east, Hertfordshire to the south and the south-east, and Buckinghamshire to the west. The largest settlement

1386-558: Is also one motorway service station in the county: Toddington Services. Former trunk roads, now local roads managed by the local highway authorities, include the A428 (Cambridge-Coventry) running east–west through Bedford Borough, and the A6 from Luton to Carlisle . Three of England's main lines pass through Bedfordshire. The West Coast Main Line has but a short section where it passes through

1485-726: Is another local delicacy. A chocolate tart , Chocolate Toothpaste consists of a gritty chocolate filling (said to resemble the texture of toothpaste) within a pastry tart, commonly finished with a swirl of whipped cream on top. Bedfordshire lies on many of the main transport routes which link London to the Midlands , Northern England and the rest of the UK. Two of England's six main trunk roads pass through Bedfordshire. The A1 London to Edinburgh road (the Great North Road) runs close by Biggleswade and Sandy, and Watling Street ,

1584-654: Is based in Houghton Regis and Costa Coffee is now based in Dunstable . UltraVision is based in Leighton Buzzard , while Moto Hospitality is based at Toddington service station. The " Bedfordshire clanger " is a local dish consisting of a suet crust pastry filled with meat in one end and a fruit preserve in the other. It was traditionally a farm labourers' meal, designed so as to produce no waste as well as two separate meals. Chocolate Toothpaste

1683-442: Is divided into seven constituencies, each returning a single Member of Parliament (MP): The present constituencies date from 1997 . The boundaries were slightly modified for the 2010 general election . This is a chart of trend of regional gross value added of Bedfordshire at current basic prices published (pp. 240–253) by Office for National Statistics with figures in millions of British Pounds Sterling. Bedfordshire

1782-494: Is divided into three epochs : Early, Middle, and Late. Similarly, in stratigraphy , the Jurassic is divided into the Lower Jurassic , Middle Jurassic , and Upper Jurassic series . Geologists divide the rocks of the Jurassic into a stratigraphic set of units called stages , each formed during corresponding time intervals called ages. Stages can be defined globally or regionally. For global stratigraphic correlation,

1881-565: Is followed by the Kimmeridgian Warm Interval (KWI) between 164 and 150 million years ago. Based on fossil wood distribution, this was one of the wettest intervals of the Jurassic. The Pangaean interior had less severe seasonal swings than in previous warm periods as the expansion of the Central Atlantic and Western Indian Ocean provided new sources of moisture. A prominent drop in temperatures occurred during

1980-470: Is fourth order, with a periodicity of approximately 410,000 years. During the Early Jurassic the world's oceans transitioned from an aragonite sea to a calcite sea chemistry, favouring the dissolution of aragonite and precipitation of calcite . The rise of calcareous plankton during the Middle Jurassic profoundly altered ocean chemistry, with the deposition of biomineralized plankton on

2079-475: Is marked by a globally documented high amplitude negative carbon isotope excursion, as well as the deposition of black shales and the extinction and collapse of carbonate-producing marine organisms, associated with a major rise in global temperatures. The TOAE is often attributed to the eruption of the Karoo-Ferrar large igneous provinces and the associated increase of carbon dioxide concentration in

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2178-522: Is named after the city of Oxford in England and was named by Alcide d'Orbigny in 1844 in reference to the Oxford Clay . The base of the Oxfordian lacks a defined GSSP. W. J. Arkell in studies in 1939 and 1946 placed the lower boundary of the Oxfordian as the first appearance of the ammonite Quenstedtoceras mariae (then placed in the genus Vertumniceras ). Subsequent proposals have suggested

2277-636: Is provided by BBC East and ITV Anglia from Cambridge , the southern part of the county such as Luton can also receive BBC London & ITV London meaning the area can get news and television programmes from Cambridge and London . Local radio stations are BBC Three Counties Radio (broadcast from Dunstable ), Heart East , Greatest Hits Radio Bucks, Beds and Herts (formerly Mix 96), BigglesFM (covering Biggleswade , Potton and Sandy ), In2beats ( Bedford ) and Radio LaB ( Luton ). The state education system for all of Bedfordshire used to be organised by Bedfordshire County Council. Unlike most of

2376-702: Is the location of a number of notable UK and international companies who have either headquarters or major bases in the county. Autoglass , Boxclever and Charles Wells Pubs are all based in Bedford , while the Kier Group and Kingspan Timber Solutions are based in Sandy , and Jordans Cereals are based in Biggleswade . EasyJet , Impellam , TUI Airways and Vauxhall Motors are all based in Luton , Whitbread

2475-707: Is the setting of the world's largest oil reserves, including the Ghawar Field , the world's largest oil field. The Jurassic-aged Sargelu and Naokelekan formations are major source rocks for oil in Iraq . Over 1500 gigatons of Jurassic coal reserves are found in north-west China, primarily in the Turpan-Hami Basin and the Ordos Basin . Major impact structures include the Morokweng impact structure ,

2574-622: Is used to mark the beginnings of stages, as well as smaller timespans within stages, referred to as "ammonite zones"; these, in turn, are also sometimes subdivided further into subzones. Global stratigraphy is based on standard European ammonite zones, with other regions being calibrated to the European successions. The oldest part of the Jurassic Period has historically been referred to as the Lias or Liassic, roughly equivalent in extent to

2673-473: The 2009 structural changes to local government in England , Bedfordshire County Council was abolished, and its responsibilities for education were passed to Bedford Borough Council and Central Bedfordshire Council . Bedford Borough Council voted in November 2009 to change to the two-tier model in its area. The change was due to be introduced over a five-year period and be completed in 2015. However, with

2772-585: The France–Switzerland border . The name "Jura" is derived from the Celtic root * jor via Gaulish *iuris "wooded mountain", which was borrowed into Latin as a name of a place and evolved into Juria and finally Jura . During a tour of the region in 1795, German naturalist Alexander von Humboldt recognized carbonate deposits within the Jura Mountains as geologically distinct from

2871-529: The Greensand Way , the greensand ridge that can be found in Surrey , Sussex and Kent ). The waymarker for the route employs a silhouette of the muntjac , a common sight in the vicinity of the village of Woburn , through which the walk passes. 51°54′59″N 0°40′13″W  /  51.916373°N 0.670391°W  / 51.916373; -0.670391 This Bedfordshire location article

2970-513: The International Commission on Stratigraphy (ICS) ratify global stages based on a Global Boundary Stratotype Section and Point (GSSP) from a single formation (a stratotype ) identifying the lower boundary of the stage. The ages of the Jurassic from youngest to oldest are as follows: Jurassic stratigraphy is primarily based on the use of ammonites as index fossils . The first appearance datum of specific ammonite taxa

3069-529: The Jurassic and Cretaceous periods, with some limestone . Local clay has been used for brick-making of Fletton-style bricks in the Marston Vale . Glacial erosion of chalk has left hard flint nodules deposited as gravel—these have been commercially extracted in the past at pits which are now lakes: at Priory Country Park , Wyboston and Felmersham . The Greensand Ridge is an escarpment across

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3168-841: The Marston Vale Line . The River Great Ouse links Bedfordshire to the Fenland waterways. As of 2004 there are plans by the Bedford & Milton Keynes Waterway Trust to construct a canal linking the Great Ouse at Bedford to the Grand Union Canal at Milton Keynes, 14 miles (23 km) distant. Luton Airport (the fifth busiest in the United Kingdom) has flights to many UK, European, Middle Eastern and North African destinations, operated largely (but not exclusively) by low-cost airlines. Local news

3267-728: The Redcar Mudstone Formation , and was ratified in 2005. The beginning of the Pliensbachian is defined by the first appearance of the ammonite Bifericeras donovani . The village Thouars (Latin: Toarcium ), just south of Saumur in the Loire Valley of France , lends its name to the Toarcian Stage. The Toarcian was named by Alcide d'Orbigny in 1842, with the original locality being Vrines quarry around 2 km northwest of Thouars. The GSSP for

3366-800: The Triassic aged Muschelkalk of southern Germany , but he erroneously concluded that they were older. He then named them Jura-Kalkstein ('Jura limestone') in 1799. In 1829, the French naturalist Alexandre Brongniart published a book entitled Description of the Terrains that Constitute the Crust of the Earth or Essay on the Structure of the Known Lands of the Earth. In this book, Brongniart used

3465-636: The Aalenian, precessionally forced climatic changes dictated peatland wildfire magnitude and frequency. The European climate appears to have become noticeably more humid at the Aalenian-Bajocian boundary but then became more arid during the middle Bajocian. A transient ice age possibly occurred in the late Bajocian. The Callovian-Oxfordian boundary at the end of the MJCI witnessed particularly notable global cooling, potentially even an ice age. This

3564-748: The Bajocian Stage after the town of Bayeux (Latin: Bajoce ) in Normandy, France. The GSSP for the base of the Bajocian is located in the Murtinheira section at Cabo Mondego , Portugal; it was ratified in 1997. The base of the Bajocian is defined by the first appearance of the ammonite Hyperlioceras mundum . The Bathonian is named after the city of Bath , England, introduced by Belgian geologist d'Omalius d'Halloy in 1843, after an incomplete section of oolitic limestones in several quarries in

3663-593: The Black Jurassic and the overlying clayey sandstone and ferruginous oolite of the Brown Jurassic sequences of southwestern Germany. The GSSP for the base of the Aalenian is located at Fuentelsaz in the Iberian range near Guadalajara, Spain , and was ratified in 2000. The base of the Aalenian is defined by the first appearance of the ammonite Leioceras opalinum . Alcide d'Orbigny in 1842 named

3762-560: The Black Jurassic in England by William Conybeare and William Phillips in 1822. William Phillips, the geologist, worked with William Conybeare to find out more about the Black Jurassic in England. The French palaeontologist Alcide d'Orbigny in papers between 1842 and 1852 divided the Jurassic into ten stages based on ammonite and other fossil assemblages in England and France, of which seven are still used, but none has retained its original definition. The German geologist and palaeontologist Friedrich August von Quenstedt in 1858 divided

3861-655: The Callovian–Oxfordian boundary, peaking possibly as high as 140 metres above present sea level at the Kimmeridgian–Tithonian boundary. The sea levels falls in the late Tithonian, perhaps to around 100 metres, before rebounding to around 110 metres at the Tithonian–Berriasian boundary. The sea level within the long-term trends across the Jurassic was cyclical, with 64 fluctuations, 15 of which were over 75 metres. The most noted cyclicity in Jurassic rocks

3960-649: The Chocolate Factory' and 'Batman Begins' and as a rehearsal space for Take That , with the other having been extensively refurbished and now accommodating Hybrid Air Vehicles, a British modern airship design and manufacturing company. St Paul's Church, Bedford is a Church of England parish church and the Civic Church of the Borough of Bedford and the County of Bedfordshire. Located on St Paul's Square,

4059-464: The Early Jurassic, but also including part of the preceding Rhaetian . The Hettangian Stage was named by Swiss palaeontologist Eugène Renevier in 1864 after Hettange-Grande in north-eastern France. The GSSP for the base of the Hettangian is located at the Kuhjoch Pass, Karwendel Mountains , Northern Calcareous Alps , Austria; it was ratified in 2010. The beginning of the Hettangian, and thus

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4158-519: The Greek goddess of dawn . His name was chosen by Albert Oppel for this stratigraphical stage because the Tithonian finds itself hand in hand with the dawn of the Cretaceous. The base of the Tithonian currently lacks a GSSP. The working definition for the base of the Tithonian is the first appearance of the ammonite genus Gravesia . The upper boundary of the Jurassic is currently undefined, and

4257-483: The Jurassic as a whole, is marked by the first appearance of the ammonite Psiloceras spelae tirolicum in the Kendlbach Formation exposed at Kuhjoch. The base of the Jurassic was previously defined as the first appearance of Psiloceras planorbis by Albert Oppel in 1856–58, but this was changed as the appearance was seen as too localised an event for an international boundary. The Sinemurian Stage

4356-797: The Jurassic, both the North and South Pole were covered by oceans. Beginning in the Early Jurassic, the Boreal Ocean was connected to the proto-Atlantic by the "Viking corridor" or Transcontinental Laurasian Seaway, a passage between the Baltic Shield and Greenland several hundred kilometers wide. During the Callovian, the Turgai Epicontinental Sea formed, creating a marine barrier between Europe and Asia. Madagascar and Antarctica began to rift away from Africa during

4455-428: The Jurassic, however, has no clear, definitive boundary with the Cretaceous and is the only boundary between geological periods to remain formally undefined. By the beginning of the Jurassic, the supercontinent Pangaea had begun rifting into two landmasses: Laurasia to the north and Gondwana to the south. The climate of the Jurassic was warmer than the present, and there were no ice caps . Forests grew close to

4554-437: The Jurassic, the North Atlantic Ocean remained relatively narrow, while the South Atlantic did not open until the Cretaceous. The continents were surrounded by Panthalassa , with the Tethys Ocean between Gondwana and Asia. At the end of the Triassic, there was a marine transgression in Europe, flooding most parts of central and western Europe transforming it into an archipelago of islands surrounded by shallow seas. During

4653-510: The Jurassic–Cretaceous boundary is currently the only system boundary to lack a defined GSSP. Placing a GSSP for this boundary has been difficult because of the strong regionality of most biostratigraphic markers, and lack of any chemostratigraphic events, such as isotope excursions (large sudden changes in ratios of isotopes ), that could be used to define or correlate a boundary. Calpionellids , an enigmatic group of planktonic protists with urn-shaped calcitic tests briefly abundant during

4752-407: The Late Jurassic (Kimmeridgian) of Scotland, which remains the only known unequivocal fossil of the group before the Cretaceous. Despite being the earliest known member of the Pinaceae, Eathiestrobus appears to be a member of the pinoid clade of the family, suggesting that the initial diversification of Pinaceae occurred earlier than has been found in the fossil record. The earliest record of

4851-416: The Middle Jurassic. Also abundant during the Jurassic is the extinct family Cheirolepidiaceae , often recognised through their highly distinctive Classopolis pollen. Jurassic representatives include the pollen cone Classostrobus and the seed cone Pararaucaria . Araucarian and Cheirolepidiaceae conifers often occur in association. The oldest definitive record of the cypress family ( Cupressaceae )

4950-445: The Middle to Late Jurassic, corresponding to the increasing aridity of the region. Ginkgoales , of which the sole living species is Ginkgo biloba , were more diverse during the Jurassic: they were among the most important components of Eurasian Jurassic floras and were adapted to a wide variety of climatic conditions. The earliest representatives of the genus Ginkgo , represented by ovulate and pollen organs similar to those of

5049-405: The North Atlantic Ocean with eastern Panthalassa. Palaeontological data suggest that the seaway had been open since the Early Jurassic. As part of the Nevadan orogeny , which began during the Triassic, the Cache Creek Ocean closed, and various terranes including the large Wrangellia Terrane accreted onto the western margin of North America. By the Middle Jurassic the Siberian plate and

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5148-462: The North China-Amuria block had collided, resulting in the closure of the Mongol-Okhotsk Ocean . During the Early Jurassic, around 190 million years ago, the Pacific Plate originated at the triple junction of the Farallon , Phoenix , and Izanagi tectonic plates , the three main oceanic plates of Panthalassa. The previously stable triple junction had converted to an unstable arrangement surrounded on all sides by transform faults because of

5247-403: The Roman road between London and Chester, passes through Dunstable. Until it was diverted in 2017, this was also the route of the A5 road between London and Holyhead . The Bedfordshire section of the A5 now runs from junction 11a of the M1 to rejoin Watling Street between Dunstable and Hockliffe , then continues on to cross the Buckinghamshire border at the City of Milton Keynes . To these

5346-502: The TOAE represented one of the most severe extinctions in their evolutionary history. While the event had significant impact on marine invertebrates, it had little effect on marine reptiles. During the TOAE, the Sichuan Basin was transformed into a giant lake , probably three times the size of modern-day Lake Superior , represented by the Da'anzhai Member of the Ziliujing Formation . The lake likely sequestered ~460 gigatons (Gt) of organic carbon and ~1,200 Gt of inorganic carbon during

5445-414: The Tithonian, known as the Early Tithonian Cooling Event (ETCE). The end of the Jurassic was marked by the Tithonian–early Barremian Cool Interval (TBCI), beginning 150 million years ago and continuing into the Early Cretaceous . The Toarcian Oceanic Anoxic Event (TOAE), also known as the Jenkyns Event, was an episode of widespread oceanic anoxia during the early part of the Toarcian Age, c. 183 Mya. It

5544-529: The Toarcian around 174 million years ago. During the Toarcian Warm Interval, ocean surface temperatures likely exceeded 30 °C (86 °F), and equatorial and subtropical (30°N–30°S) regions are likely to have been extremely arid, with temperatures in the interior of Pangea likely in excess of 40 °C (104 °F).The Toarcian Warm Interval is followed by the Middle Jurassic Cool Interval (MJCI) between 174 and 164 million years ago, which may have been punctuated by brief, ephemeral icehouse intervals. During

5643-410: The United Kingdom, Bedfordshire County Council operated a three-tier education system arranged into lower, middle and upper schools, as recommended in the Plowden Report of 1967, although Luton continued to operate a two-tier system. The three-tier arrangement continued in the rest of the county, though in 2006 a vote was held with a view to moving to the two-tier model, but this was rejected. After

5742-428: The atmosphere, as well as the possible associated release of methane clathrates . This likely accelerated the hydrological cycle and increased silicate weathering , as evidenced by an increased amount of organic matter of terrestrial origin found in marine deposits during the TOAE. Groups affected include ammonites, ostracods , foraminifera , bivalves , cnidarians , and especially brachiopods , for which

5841-407: The base of the Toarcian is located at Peniche, Portugal , and was ratified in 2014. The boundary is defined by the first appearance of ammonites belonging to the subgenus Dactylioceras ( Eodactylites ) . The Aalenian is named after the city of Aalen in Germany. The Aalenian was defined by Swiss geologist Karl Mayer-Eymar in 1864. The lower boundary was originally between the dark clays of

5940-490: The cancellation of the Building Schools for the Future programme in 2010, the borough changed its proposals, and the switch proceeded on school by school basis where council funds allowed. However as of 2020 all of Bedford Borough has a two-tier education structure apart from in the Marston Vale area (one upper school remains). Most of the secondary schools in the area offer sixth form courses (such as A Levels ), though Bedford College and The Bedford Sixth Form also offer

6039-481: The county from near Leighton Buzzard to near Gamlingay in Cambridgeshire . Bedfordshire, being situated in the east of England, has a relatively dry mixed climate for the UK with regular but generally there is sometimes rainfall. Average annual rainfall is 608.6 millimetres (23.96 in) at Bedford. October is the wettest month, with 65.3 millimetres (2.57 in), and March the driest, with 37.3 millimetres (1.47 in). Although temperatures are usually moderate,

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6138-437: The county has one of the largest absolute temperature ranges in the UK – of more than 60 °C (108 °F). Average temperatures in Bedford range from a low of 1.5 °C (34.7 °F) overnight in February to a high of 22.4 °C (72.3 °F) during the day in July. The highest official temperature recorded in Bedfordshire was 39.7 °C (103.5 °F) in 2022. The lowest official temperature recorded in Bedfordshire

6237-510: The county – the University of Bedfordshire and Cranfield University . These institutions attract students from all over the UK and abroad, as well as from Bedfordshire. The enormous Cardington airship sheds are situated to the south of Bedford, near the villages of Cardington and Shortstown. They were originally built for the construction of large airships during World War I. Since falling out of their intended use, one has been used for many purposes including housing film sets for 'Charlie and

6336-419: The county, alongside the City of Milton Keynes in Buckinghamshire . Policing and fire and rescue services continue to be provided on a county-wide basis, with Bedfordshire Police governed by the Bedfordshire Police and Crime Commissioner and Bedfordshire Fire and Rescue Service governed by a Fire Authority comprising members of the three councils. For elections to the House of Commons , Bedfordshire

6435-616: The end of the Jurassic. The oldest unambiguous members of Podocarpaceae are known from the Jurassic, found across both hemispheres, including Scarburgia and Harrisiocarpus from the Middle Jurassic of England, as well as unnamed species from the Middle-Late Jurassic of Patagonia. During the Early Jurassic, the flora of the mid-latitudes of Eastern Asia were dominated by the extinct deciduous broad leafed conifer Podozamites , which appears to not be closely related to any living family of conifer. Its range extended northwards into polar latitudes of Siberia and then contracted northward in

6534-413: The end of the Triassic, the Peltaspermaceae became extinct in most parts of the world, with Lepidopteris persisting into the Early Jurassic in Patagonia. Dicroidium , a corystosperm seed fern that was a dominant part of Gondwanan floral communities during the Triassic, also declined at the Triassic–Jurassic boundary, surviving as a relict in Antarctica into the Early Jurassic. Conifers formed

6633-402: The eruption of the Central Atlantic Magmatic Province (CAMP). The beginning of the Toarcian Age started around 183 million years ago and is marked by the Toarcian Oceanic Anoxic Event , a global episode of oceanic anoxia , ocean acidification , and elevated global temperatures associated with extinctions, likely caused by the eruption of the Karoo-Ferrar large igneous provinces . The end of

6732-417: The event. Seawater pH , which had already substantially decreased prior to the event, increased slightly during the early stages of the TOAE, before dropping to its lowest point around the middle of the event. This ocean acidification is the probable cause of the collapse of carbonate production. Additionally, anoxic conditions were exacerbated by enhanced recycling of phosphorus back into ocean water as

6831-449: The evidence for this is primarily European, probably controlled by changes in eustatic sea level. There is no evidence of a mass extinction of plants at the Triassic–Jurassic boundary. At the Triassic–Jurassic boundary in Greenland, the sporomorph (pollen and spores) record suggests a complete floral turnover. An analysis of macrofossil floral communities in Europe suggests that changes were mainly due to local ecological succession . At

6930-712: The far west of the county, with one station at Leighton Buzzard served by West Midlands Trains to London Euston and Northampton . The East Coast Main Line has stations at Arlesey , Biggleswade and Sandy , served by Great Northern services to King's Cross and Peterborough . The Midland Main Line serves Luton , Luton Airport (via Luton DART link from the station at Luton Airport Parkway ) and Bedford , with trains to many destinations operated by East Midlands Railway and Thameslink . Intermediate stations at Flitwick , Harlington and Leagrave are served by Thameslink. There are London North Western rural services also running between Bedford and Bletchley along

7029-472: The few cynodont lineages to survive the end of the Triassic, continued to diversify throughout the period, with the Jurassic seeing the emergence of the first crown group mammals . Crocodylomorphs made the transition from a terrestrial to an aquatic life. The oceans were inhabited by marine reptiles such as ichthyosaurs and plesiosaurs , while pterosaurs were the dominant flying vertebrates . Modern sharks and rays first appeared and diversified during

7128-686: The first appearance of Cardioceras redcliffense as the lower boundary. The village of Kimmeridge on the coast of Dorset , England, is the origin of the name of the Kimmeridgian. The stage was named by Alcide d'Orbigny in 1842 in reference to the Kimmeridge Clay . The GSSP for the base of the Kimmeridgian is the Flodigarry section at Staffin Bay on the Isle of Skye , Scotland , which

7227-465: The first appearance of the ammonite Strambergella jacobi , formerly placed in the genus Berriasella , but its use as a stratigraphic indicator has been questioned, as its first appearance does not correlate with that of C. alpina . The Kimmeridge Clay and equivalents are the major source rock for the North Sea oil . The Arabian Intrashelf Basin, deposited during the Middle and Late Jurassic,

7326-402: The genus Elatides . The Jurassic also saw the first appearances of some modern genera of cypresses, such as Sequoia . Members of the extinct genus Schizolepidopsis which likely represent a stem-group to the pine family ( Pinaceae ), were widely distributed across Eurasia during the Jurassic. The oldest unambiguous record of Pinaceae is the pine cone Eathiestrobus , known from

7425-420: The large medieval and later church of cathedral proportions and iconic spire dominates the town and area, exercises a ministry of welcome to thousands of visitors and pilgrims from far and wide each year, and is a focus for special commemorations and celebrations in the borough, county, region and wider community, as well as being a central venue for concerts, recitals and exhibitions. Historically, St Paul's played

7524-668: The late Early Jurassic in association with the eruption of the Karoo-Ferrar large igneous provinces , opening the western Indian Ocean and beginning the fragmentation of Gondwana. At the beginning of the Jurassic, North and South America remained connected, but by the beginning of the Late Jurassic they had rifted apart to form the Caribbean Seaway, also known as the Hispanic Corridor, which connected

7623-472: The late Sinemurian–Pliensbachian before regressing to near present levels by the late Pliensbachian. There seems to have been a gradual rise to a peak of ~75 m above present sea level during the Toarcian. During the latest part of the Toarcian, the sea level again dropped by several tens of metres. It progressively rose from the Aalenian onwards, aside from dips of a few tens of metres in the Bajocian and around

7722-465: The latest Jurassic to earliest Cretaceous, have been suggested to represent the most promising candidates for fixing the Jurassic–Cretaceous boundary In particular, the first appearance Calpionella alpina , co-inciding with the base of the eponymous Alpina subzone, has been proposed as the definition of the base of the Cretaceous. The working definition for the boundary has often been placed as

7821-605: The liberty and the ancient borough of Bedford . There have been several changes to the county boundary; for example, in 1897 Kensworth and part of Caddington were transferred from Hertfordshire to Bedfordshire. The southern end of the county is on the chalk ridge known as the Chiltern Hills . The remainder forms part of the broad drainage basin of the River Great Ouse and its tributaries. Most of Bedfordshire's rocks are clays and sandstones from

7920-428: The modern species, are known from the Middle Jurassic in the Northern Hemisphere. Several other lineages of ginkgoaleans are known from Jurassic rocks, including Yimaia , Grenana , Nagrenia and Karkenia . These lineages are associated with Ginkgo- like leaves, but are distinguished from living and fossil representatives of Ginkgo by having differently arranged reproductive structures. Umaltolepis from

8019-422: The ocean floor acting as a buffer against large CO 2 emissions. The climate of the Jurassic was generally warmer than that of present, by around 5–10 °C (9–18 °F), with atmospheric carbon dioxide likely about four times higher. Intermittent "cold snap" intervals are known to have occurred during this time period, however, interrupting the otherwise warm greenhouse climate. Forests likely grew near

8118-460: The oceans, resulting in large areas of desert and scrubland in the lower latitudes between 40° N and S of the equator. Tropical rainforest and tundra biomes are likely to have been rare or absent. The Jurassic also witnessed the decline of the Pangaean megamonsoon that had characterised the preceding Permian and Triassic periods. Variation in the frequency of wildfire activity in the Jurassic

8217-497: The period, while the first known crown-group teleost fish appeared near the end of the period. The flora was dominated by ferns and gymnosperms , including conifers , of which many modern groups made their first appearance during the period, as well as other groups like the extinct Bennettitales . The chronostratigraphic term "Jurassic" is linked to the Jura Mountains , a forested mountain range that mainly follows

8316-592: The phrase terrains jurassiques when correlating the "Jura-Kalkstein" of Humboldt with similarly aged oolitic limestones in Britain, thus coining and publishing the term "Jurassic". The German geologist Leopold von Buch in 1839 established the three-fold division of the Jurassic, originally named from oldest to the youngest: the Black Jurassic , Brown Jurassic , and White Jurassic . The term " Lias " had previously been used for strata of equivalent age to

8415-611: The poles, where they experienced warm summers and cold, sometimes snowy winters; there were unlikely to have been ice sheets given the high summer temperatures that prevented the accumulation of snow, though there may have been mountain glaciers. Dropstones and glendonites in northeastern Siberia during the Early to Middle Jurassic indicate cold winters. The ocean depths were likely 8 °C (14 °F) warmer than present, and coral reefs grew 10° of latitude further north and south. The Intertropical Convergence Zone likely existed over

8514-532: The poles, with large arid expanses in the lower latitudes. On land, the fauna transitioned from the Triassic fauna, dominated jointly by dinosauromorph and pseudosuchian archosaurs , to one dominated by dinosaurs alone. The first stem-group birds appeared during the Jurassic, evolving from a branch of theropod dinosaurs. Other major events include the appearance of the earliest crabs and modern frogs , salamanders and lizards . Mammaliaformes , one of

8613-648: The region. The GSSP for the base of the Bathonian is Ravin du Bès, Bas-Auran area, Alpes de Haute Provence , France; it was ratified in 2009. The base of the Bathonian is defined by the first appearance of the ammonite Gonolkites convergens , at the base of the Zigzagiceras zigzag ammonite zone . The Callovian is derived from the Latinized name of the village of Kellaways in Wiltshire , England, and

8712-573: The three series of von Buch in the Swabian Jura into six subdivisions defined by ammonites and other fossils. The German palaeontologist Albert Oppel in his studies between 1856 and 1858 altered d'Orbigny's original scheme and further subdivided the stages into biostratigraphic zones, based primarily on ammonites. Most of the modern stages of the Jurassic were formalized at the Colloque du Jurassique à Luxembourg in 1962. The Jurassic Period

8811-478: The two-tier model in response to parent and school demand, but elsewhere in the authority the three-tier model continues. Plans for the construction of new settlements in Marston Vale have included lower, middle and upper schools. As well as sixth form departments in schools, the main further education providers in the district are Central Bedfordshire College and Shuttleworth College Luton also operates

8910-497: The world's major landmasses were coalesced into the supercontinent Pangaea , which during the Early Jurassic began to break up into northern supercontinent Laurasia and the southern supercontinent Gondwana . The rifting between North America and Africa was the first to initiate, beginning in the early Jurassic, associated with the emplacement of the Central Atlantic Magmatic Province . During

9009-585: The yew family ( Taxaceae ) is Palaeotaxus rediviva , from the Hettangian of Sweden, suggested to be closely related to the living Austrotaxus , while Marskea jurassica from the Middle Jurassic of Yorkshire, England and material from the Callovian–Oxfordian Daohugou Bed in China are thought to be closely related to Amentotaxus , with the latter material assigned to the modern genus, indicating that Taxaceae had substantially diversified by

9108-572: Was added in 1959 the M1 motorway , running from London to Leeds . Running from junctions 10 to 13 in Bedfordshire, there are two junctions serving Luton (at the southern end), with another one serving Bedford and Milton Keynes (at the northern end). Between these lies two other junctions in the county, with one connecting to the A5 and serving Dunstable , and the other serving the town of Flitwick . There

9207-474: Was first defined and introduced into scientific literature by Alcide d'Orbigny in 1842. It takes its name from the French town of Semur-en-Auxois , near Dijon . The original definition of Sinemurian included what is now the Hettangian. The GSSP of the Sinemurian is located at a cliff face north of the hamlet of East Quantoxhead , 6 kilometres east of Watchet , Somerset , England , within the Blue Lias , and

9306-629: Was governed by the 405 kyr eccentricity cycle. Thanks to the breakup of Pangaea, the hydrological cycle during the Jurassic was significantly enhanced. The beginning of the Jurassic was likely marked by a thermal spike corresponding to the Triassic–Jurassic extinction and eruption of the Central Atlantic magmatic province. The first part of the Jurassic was marked by the Early Jurassic Cool Interval between 199 and 183 million years ago. It has been proposed that glaciation

9405-582: Was named by Alcide d'Orbigny in 1852, originally the base at the contact between the Forest Marble Formation and the Cornbrash Formation . However, this boundary was later found to be within the upper part of the Bathonian. The base of the Callovian does not yet have a certified GSSP. The working definition for the base of the Callovian is the first appearance of ammonites belonging to the genus Kepplerites . The Oxfordian

9504-490: Was present in the Northern Hemisphere during both the early Pliensbachian and the latest Pliensbachian. There was a spike in global temperatures of around 4–8 °C (7–14 °F) during the early part of the Toarcian corresponding to the Toarcian Oceanic Anoxic Event and the eruption of the Karoo-Ferrar large igneous provinces in southern Gondwana, with the warm interval extending to the end of

9603-687: Was ratified in 2000. The beginning of the Sinemurian is defined by the first appearance of the ammonite Vermiceras quantoxense . Albert Oppel in 1858 named the Pliensbachian Stage after the hamlet of Pliensbach in the community of Zell unter Aichelberg in the Swabian Alb , near Stuttgart , Germany. The GSSP for the base of the Pliensbachian is found at the Wine Haven locality in Robin Hood's Bay , Yorkshire , England, in

9702-430: Was ratified in 2021. The boundary is defined by the first appearance of ammonites marking the boreal Bauhini Zone and the subboreal Baylei Zone. The Tithonian was introduced in scientific literature by Albert Oppel in 1865. The name Tithonian is unusual in geological stage names because it is derived from Greek mythology rather than a place name. Tithonus was the son of Laomedon of Troy and fell in love with Eos ,

9801-508: Was −20.6 °C (−5.1 °F) in 1947. The Bedfordshire Police and Crime Commissioner is John Tizard , a member of the Labour Party . For local government purposes, Bedfordshire is divided into three unitary authorities : the boroughs of Bedford and Luton , and the district of Central Bedfordshire . Healthcare in the county is dealt with by a single Clinical Commission Group (CCG), which serves all three local authorities in

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