title: 10cc

text: Frictions mounted between the group's two creative teams during the recording of "How Dare You", with each pair realising how far apart their ideas had become. At the beginning of the sessions for band's fifth album further creative differences occurred and Godley and Creme left 10cc to work on a project that eventually evolved into the triple LP set "Consequences" (1977), a sprawling concept album that featured contributions from satirist Peter Cook and jazz vocalist Sarah Vaughan.


title: 10cc

text: The first of a series of albums by Godley & Creme, "Consequences" began as a demonstration record for the "Gizmotron", an electric guitar effect they had invented. The device, which fitted over the bridge of an electric guitar, contained six small motor-driven wheels attached to small keys (four wheels for electric basses); when the key was depressed, the Gizmotron wheels bowed the guitar strings, producing notes and chords with endless sustain. First used during the recording of the "Sheet Music" track "Old Wild Men", the device was designed to further cut their recording costs: by using it on an electric guitar with studio effects, they could effectively simulate strings and other sounds, enabling them to dispense with expensive orchestral overdubs.


title: 10cc

text: In a 2007 interview with the ProGGnosis—Progressive Rock & Fusion website, Godley explained: "We left because we no longer liked what Gouldman and Stewart were writing. We left because 10cc was becoming safe and predictable and we felt trapped."


title: 10cc

text: But speaking to "Uncut" magazine 10 years earlier, he expressed regret about the band breaking up as they embarked on the "Consequences" project:


title: 10cc

text: Stewart said there were immediate benefits in the absence of Godley and Creme. "It became clear things went much smoother and the atmosphere was much more pleasant than with Lol and Kevin," he said.


title: 10cc

text: Godley & Creme went on to achieve cult success as a songwriting and recording duo, scoring several hits and releasing a string of innovative LPs and singles. Having honed their skills on the equally innovative clips that they made to promote their own singles (e.g. their 1985 single "Cry") they returned to their visual arts roots and became better-known as directors of music videos in the 1980s, creating acclaimed videos for chart-topping acts including George Harrison ("When We Was Fab"), Asia ("Heat of the Moment", "Only Time Will Tell") The Police ("Every Breath You Take"), Duran Duran ("Girls on Film"), Frankie Goes to Hollywood ("Two Tribes"), Peter Gabriel's duet with Kate Bush ("Don't Give Up"), and Herbie Hancock ("Rockit"). They also directed a video for Stewart and Gouldman's "Feel the Love".


title: 10cc

text: After the departure of Godley and Creme, Stewart and Gouldman opted to continue as 10cc, working with drummer Paul Burgess, who had up to that point been their tour backup drummer. Their first album as a three piece band was "Deceptive Bends" (1977), named after a sign on the Mickleham bends on the A24 between Leatherhead and Dorking in Surrey. The album, recorded at the newly completed Strawberry South Studio in Dorking, Surrey, reached No. 3 in Britain and No. 31 in the US and also yielded three hit singles, "The Things We Do for Love" (UK No. 6, US No. 5), "Good Morning Judge" (UK No. 5, US No. 69) and "People in Love" (US No. 40). Stewart later said he and Gouldman felt vindicated by its success: "I was out to prove also that we could write a hit album without Kevin and Lol ... we did!"


title: 10cc

text: In 1977, 10cc embarked on an international tour with guitarist Rick Fenn, keyboardist Tony O'Malley (Kokomo) and an additional drummer Stuart Tosh (ex-Pilot) and recorded a live album, "Live and Let Live" (1977), which mixed the hits with material by Stewart and Gouldman from 10cc's career (alongside two songs written with Godley and Creme).


title: 10cc

text: Fenn, Tosh, Burgess and keyboardist Duncan Mackay, who replaced Tony O'Malley after the tour, were now full members of the band and performed on 1978's "Bloody Tourists", which provided the band with their international No. 1 single, the reggae-styled "Dreadlock Holiday", also their third UK No. 1. Both "Bloody Tourists" and "Dreadlock Holiday" performed very successful around the world, however additional songs released as singles became only minor hits with the second UK single "Reds in My Bed", featuring lead vocals by Stuart Tosh, failing to chart.


title: 10cc

text: The band suffered a major setback in January 1979 when Stewart was seriously injured in a car crash. Due to his injuries, Stewart was unable to work on music and 10cc had to be put on hold. This led to cancellation of 1979 legs of tour with other band members working on solo projects. Stewart later told the BBC:


title: 10cc

text: Gouldman, too, considered the aftermath of Stewart's accident to be a turning point. In a 1995 BBC interview he said:


title: 10cc

text: While Stewart recovered, Gouldman recorded the title track to the film "Sunburn" with the help of some of the 10cc band members, which became a minor UK hit in 1979. Gouldman also recorded the soundtrack to the animated film "Animalympics", which was originally intended as 10cc project. Rick Fenn went onto large success touring with Mike Oldfield and recording with Nick Mason after being introduced by Eric Stewart while Duncan Mackay took part in recording of Kate Bush album "Never for Ever".


title: 10cc

text: To fill the gap between 10cc releases, a greatest hits compilation was issued in late 1979 "Greatest Hits 1972–1978", and released a single, coupling "I'm Not in Love" with "For You and I", which failed to chart.


title: 10cc

text: As Stewart recovered, he recorded the soundtrack to the film "Girls", mainly working with Duncan Mackay with other 10cc band members making guest appearances.


title: 10cc

text: The band signed with Warner Bros. Records, producing a new 10cc offering entitled "Look Hear?". The lead single "One-Two-Five" failed to chart in the native UK and the album proved to be less successful than previous 10cc albums. In the aftermath of the tour in support Eric Stewart, Graham Gouldman and the rest of the band members again embarked on a number of side projects.


title: 10cc

text: Gouldman and Stewart subsequently decided to continue 10cc as a duo with other members becoming session and touring musicians. The band returned to the Mercury label to record "Ten Out of 10" (1981) featuring Fenn and Burgess on a number of tracks. The UK release of the album (and its associated singles "Les Nouveaux Riches" and "Don't Turn Me Away") failed to chart.


title: 10cc

text: In a bid to inject an American flavour to the album and bolster its commercial appeal, Warner Bros. invited singer-songwriter Andrew Gold to contribute to a revised North American version of the LP. Gold wound up co-writing and playing on three new tracks which appeared on the North American release of "Ten Out of 10". This ultimately led to an offer from Gouldman and Stewart to officially join 10cc; an offer Gold declined because of other commitments. Gouldman later admitted greater involvement by Gold might have lifted the band's early 1980s output from its mediocrity:


title: 10cc

text: Despite the revisions to the album made for the North American market, "Ten Out of 10" did not chart in US, nor did any singles pulled from the LP. However, the single "Don't Turn Me Away" was a surprise minor hit in Canada, reaching No. 38. Ironically, this track was one that appeared on the original "less commercial" UK version of the LP, and was "not" one of the tracks that had been specially added to the North American release.


title: 10cc

text: The band embarked on their 10th anniversary tour in early 1982, with Fenn, Burgess and Tosh joining Stewart and Gouldman, along with new keyboardist Vic Emerson of Sad Café. They released "The Power of Love", co-written with Andrew Gold, as a single, which did not chart. "Run Away", released as a single in June 1982, reached No.50 in the UK; "We've Heard it all Before" (October 1982) did not chart. All three of these singles were tracks from the revised North American version of "Ten Out of 10", and had not previously been issued in the UK.


title: 10cc

text: Stewart also released a 1982 solo album, "Frooty Rooties", with Burgess as a drummer and participation from Gouldman and Fenn on one track.


title: 10cc

text: 10cc began a UK tour in March 1983, coinciding with the release of the single "24 Hours". The song was made available both as a 7" and 10" single, with live versions of "Dreadlock Holiday" and "I'm Not in Love" on the b-sides. It failed to chart, as did a further single, "Feel The Love (Oomachasaooma)"/"She Gives Me Pain", issued in July 1983. "Feel The Love (Oomachasaooma)" was promoted by a tennis-themed video clip, directed by none other than former 10cc members Godley and Creme, by now well into their joint careers as noted music video pioneers.


title: 10cc

text: The next 10cc LP, "Windows in the Jungle", (October 1983) used session heavyweights including drummer Steve Gadd, but the album was dominated by Stewart; Gouldman only performed partial lead vocals on one song. It reached No.70 on the UK charts. The band toured the UK in October, with drummer Jamie Lane in place of Paul Burgess (who was working with Jethro Tull). This turned out to be their last tour until they reformed eight years later.


title: 10cc

text: After 1983, the band went into recess as Stewart produced recordings for Sad Café and Gouldman produced tracks for the Ramones. Stewart continued his association with Paul McCartney; he had already appeared on "Tug of War" in 1982 and "Pipes of Peace" in 1983. During 1984 he appeared in the video for the US single "So Bad" which also featured Ringo Starr and the feature film/soundtrack for "Give My Regards to Broad Street". He then co-wrote much of the "Press to Play" album (1986), though he was critical of the album's production. He also produced the album "Eyes of a Woman" (1985) by Agnetha Fältskog of ABBA.


title: 10cc

text: Gouldman, meanwhile, teamed with Andrew Gold to form the duo Common Knowledge, which, after two unsuccessful singles changed their name to Wax. The duo's albums included "Magnetic Heaven" (1986), "American English" (1987) and "A Hundred Thousand in Fresh Notes" (1989). The duo scored some success including a Spanish No.1 single and their only British hit, "Bridge to Your Heart" (1987) which reached No. 12. Gouldman also assembled and produced the charity single "You'll Never Walk Alone" by The Crowd in aid of the Bradford City stadium fire. Released in 1985, the single reached No.1 in the UK charts.


title: 10cc

text: A compilation album, "Changing Faces – The Very Best of 10cc and Godley & Creme", was released in 1987 and gave the band their biggest hit album since 1978.


title: 10cc

text: A four CD box set, "Greatest Songs and More", was issued in Japan in 1991, which included many b-sides available on CD for the first time.


title: 10cc

text: In 1991, the original four members reunited to record "...Meanwhile" (1992), an album produced by Gary Katz of Steely Dan fame. Katz was suggested by the record label Polydor who wanted 10cc to enjoy success in America, and because of his links to Steely Dan—a similar-sounding 1970s band. However, the album was not a "reunion" in the strict sense of the word. All the album's songs were written by Stewart and Gouldman (with the exception of one track which was co-written by Stewart and Paul McCartney in the late 1980s with additional writing from Gouldman). Creme and Godley agreed to guest on the album to fulfil their obligation to Polydor—both had owed Polydor one album when they split in the late 1980s. Godley and Creme sang background vocals on several tracks on the album. Godley also sang the lead on one song, "The Stars Didn't Show". The record label did everything it could to make it appear that it was a genuine reunion album to generate publicity, but to little effect.


title: 10cc

text: "...Meanwhile" did not spawn any major hits, but was relatively well received in Japan and in Europe. It prominently featured session musicians Jeff Porcaro of Toto on drums, Freddie Washington on bass, Michael Landau on lead and rhythm guitar, and Bashiri Johnson on percussion. Also appearing on the album were Dr. John (Mac Rebennack) on piano, David Paich (also of Toto fame) on keyboards, longtime 10cc collaborator Andrew Gold on guitar and many other renowned session musicians and singers. "...Meanwhile" is believed to be Porcaro's last session work before he died of a heart attack. Dr. John was recommended by producer Gary Katz and invited along to the sessions.


title: 10cc

text: Gouldman, in a 1995 interview, was philosophical about the album: "When we finally did come back to record again, it was based on market research that our record company had done, that said a new 10cc album would do really, really well. And, ah, history has proved that wrong." Yet according to Stewart, both he and Gouldman had approached the album positively. "We wrote in a three-month period, 22 songs. Every day we were coming up with new ideas, and they were getting better and better, as far as we were concerned. And they sounded like 10cc songs again."


title: 10cc

text: The album was followed by a tour in 1993, with former members Rick Fenn and Stuart Tosh returning alongside new players Steve Piggot (keyboards, synthesisers) and Gary Wallis (drum, percussion). This tour was captured on the live album and DVD "Alive".


title: 10cc

text: In 1995 the band released "Mirror Mirror", produced by Gouldman, Stewart and Adrian Lee of Mike + The Mechanics, and without participation from Godley or Creme. Despite initial objections by Gouldman, "Mirror Mirror" included an acoustic version of "I'm Not in Love" which became a No. 29 UK hit single, but overall the album did not fare very well. Gouldman has described "Mirror Mirror" as "almost like two-halves of an album", largely a result of the fact that he and Stewart recorded in separate countries. "I don't like to say we hoodwinked the people, but you could say it's not quite what it appears to be, and anyone with any sense, who reads the credits, could see that," he told "Goldmine" magazine. Their recording arrangement also provided further evidence of a fractured relationship between Stewart and Gouldman: aside from "I'm Not in Love", Stewart did not appear on any of the tracks Gouldman played or sang on, while Gouldman did not appear on any of Stewart's tracks.


title: 10cc

text: In the spring of 1995, the band toured Europe and Japan with a line-up of Stewart, Gouldman, Fenn, Tosh, Alan Park (keyboards, synthesisers) and Geoff Dunn (drums, percussion).


title: 10cc

text: Stewart left the band after this tour, and has since commented: "10cc is well and truly finished as far as I am concerned." Married to a pair of sisters, Stewart and Creme have kept in touch.


title: 10cc

text: In 1999 Gouldman convened a 10cc line-up comprising himself, Fenn, Paul Burgess, and new recruits Mick Wilson (vocals, guitar) and Mike Stevens (vocals, keyboards, sax, guitar). This version of the band played their first gig at Ronnie Scott's Jazz Club in Birmingham and then began touring regularly in 2002. The same five members have been associated with the group ever since. A new member, Keith Hayman (keyboards), switched with Mike Stevens in 2006 and continued to do so until 2011. This iteration of the group also featured occasional guest appearances by Kevin Godley, and toured both the UK and overseas, playing 10cc hits plus a section of Gouldman's hits written for others. Wilson handled the majority of the lead vocals, taking over from Eric Stewart on that front. Although popular with audiences, Stewart is critical of the band continuing without him. Founding guitarist Lol Creme, discussing his newest live act in 2012, opined:


title: 10cc

text: In 2006 offered a six-track EP to download credited to GG/06: "The Same Road", "Johnny Hurts", "Beautifulloser.com", "Hooligan Crane", "Son of Man" and "Barry's Shoes", described as the first of a group of songs they had worked on for three years. A few of these songs were added to the rotation of songs that 10cc played in their live set, while the song "Son of Man" later became the opening theme for 10cc shows with Godley providing the video.


title: 10cc

text: The band released a live album and DVD titled "Clever Clogs" in 2008 featuring Kevin Godley on several songs, including GG/06's "BeautifulLoser.com".


title: 10cc

text: In early 2009, Gouldman's 10cc launched its official website, 10ccworld.com (now 10cc.world). Since the release, the website offered various live recordings of the shows through its online store. Regarding new 10cc studio release Gouldman has said that without Stewart, Creme or Godley, there will never be another 10cc album, though he is happy to play past albums in concert.


title: 10cc

text: To celebrate the 40th anniversary of the band's formation 10cc performed a concert at the Royal Albert Hall on 10 May 2012 with Kevin Godley performing several songs with the band. Universal Music also issued two box sets for this occasion. The first one titled "Tenology", a four-CD/one-DVD retrospective, was released on 19 November 2012. All four original members helped choose the track listing and gave interviews to Paul Lester as part of the project. The second box set titled "Classic Album Selection" featured albums from "The Original Soundtrack" to "Live and Let Live" along with bonus tracks.


title: 10cc

text: In 2016, Godley recorded a video performance of "Somewhere in Hollywood" for 10cc's live performance of the album Sheet Music during that year. The same year Keith Hayman again replaced Mike Stevens on keyboards.


title: 10cc

text: In December 2015, BBC Four released the hour-long documentary titled "I'm Not in Love: The Story of 10cc."


title: 10cc

text: In July 2017, a box set titled "Before, During and After: The Story of 10cc" was released. The four-disc set contains 10cc material as well as material from the late 60s and early 70s that the band recorded under various names and material from various projects that band members were involved in after leaving the band. Eric Stewart also released a solo boxset through Cherry Records while promoting his autobiography


title: 10cc

text: In 2018 the 10cc concert line up changed with Iain Hornal taking Wilson's place as vocalist. Mick Wilson now sings and tours with 'Go Now - The Music of the Moody Blues' and also as part of 'Frontm3n' with Pete Lincoln (ex The Sweet) and Peter Howarth (The Hollies).


title: Lactic acid

text: Lactic acid is an organic acid. It has a molecular formula . It is white in the solid state and it is miscible with water. When in the dissolved state, it forms a colorless solution. Production includes both artificial synthesis as well as natural sources. Lactic acid is an alpha-hydroxy acid (AHA) due to the presence of a hydroxyl group adjacent to the carboxyl group. It is used as a synthetic intermediate in many organic synthesis industries and in various biochemical industries. The conjugate base of lactic acid is called lactate (or the lactate anion). The name of the derived acyl group is lactoyl.


title: Lactic acid

text: In solution, it can ionize by loss of a proton to produce the lactate ion . Compared to acetic acid, its p"K" is 1 unit less, meaning lactic acid is ten times more acidic than acetic acid. This higher acidity is the consequence of the intramolecular hydrogen bonding between the α-hydroxyl and the carboxylate group.


title: Lactic acid

text: Lactic acid is chiral, consisting of two enantiomers. One is known as -lactic acid, ("S")-lactic acid, or (+)-lactic acid, and the other, its mirror image, is -lactic acid, ("R")-lactic acid, or (−)-lactic acid. A mixture of the two in equal amounts is called -lactic acid, or racemic lactic acid. Lactic acid is hygroscopic. -Lactic acid is miscible with water and with ethanol above its melting point, which is about . -Lactic acid and -lactic acid have a higher melting point. Lactic acid produced by fermentation of milk is often racemic, although certain species of bacteria produce solely -lactic acid. On the other hand, lactic acid produced by anaerobic respiration in animal muscles has the () enantiomer and is sometimes called "sarcolactic" acid, from the Greek , meaning "flesh".


title: Lactic acid

text: In animals, -lactate is constantly produced from pyruvate via the enzyme lactate dehydrogenase (LDH) in a process of fermentation during normal metabolism and exercise. It does not increase in concentration until the rate of lactate production exceeds the rate of lactate removal, which is governed by a number of factors, including monocarboxylate transporters, concentration and isoform of LDH, and oxidative capacity of tissues. The concentration of blood lactate is usually at rest, but can rise to over 20mM during intense exertion and as high as 25mM afterward. In addition to other biological roles, -lactic acid is the primary endogenous agonist of hydroxycarboxylic acid receptor 1 (HCA), which is a G protein-coupled receptor (GPCR).


title: Lactic acid

text: In industry, lactic acid fermentation is performed by lactic acid bacteria, which convert simple carbohydrates such as glucose, sucrose, or galactose to lactic acid. These bacteria can also grow in the mouth; the acid they produce is responsible for the tooth decay known as caries. In medicine, lactate is one of the main components of lactated Ringer's solution and Hartmann's solution. These intravenous fluids consist of sodium and potassium cations along with lactate and chloride anions in solution with distilled water, generally in concentrations isotonic with human blood. It is most commonly used for fluid resuscitation after blood loss due to trauma, surgery, or burns.


title: Lactic acid

text: Swedish chemist Carl Wilhelm Scheele was the first person to isolate lactic acid in 1780 from sour milk. The name reflects the "lact-" combining form derived from the Latin word , meaning "milk". In 1808, Jöns Jacob Berzelius discovered that lactic acid (actually -lactate) also is produced in muscles during exertion. Its structure was established by Johannes Wislicenus in 1873.


title: Lactic acid

text: In 1856, the role of "Lactobacillus" in the synthesis of lactic acid was discovered by Louis Pasteur. This pathway was used commercially by the German pharmacy Boehringer Ingelheim in 1895.


title: Lactic acid

text: In 2006, global production of lactic acid reached 275,000 tonnes with an average annual growth of 10%.


title: Lactic acid

text: Lactic acid is produced industrially by bacterial fermentation of carbohydrates, or by chemical synthesis from acetaldehyde. , lactic acid was produced predominantly (70–90%) by fermentation. Production of racemic lactic acid consisting of a 1:1 mixture of and stereoisomers, or of mixtures with up to 99.9% -lactic acid, is possible by microbial fermentation. Industrial scale production of -lactic acid by fermentation is possible, but much more challenging.


title: Lactic acid

text: Fermented milk products are obtained industrially by fermentation of milk or whey by "Lactobacillus" bacteria: "Lactobacillus acidophilus", "Lacticaseibacillus casei" ("Lactobacillus casei"), "Lactobacillus delbrueckii" subsp. "bulgaricus" ("Lactobacillus bulgaricus"), "Lactobacillus helveticus", "Lactococcus lactis" ," Bacillus amyloliquofaciens", and "Streptococcus salivarius" subsp. "thermophilus" ("Streptococcus thermophilus").


title: Lactic acid

text: As a starting material for industrial production of lactic acid, almost any carbohydrate source containing (Pentose sugar) and (Hexose sugar) can be used. Pure sucrose, glucose from starch, raw sugar, and beet juice are frequently used. Lactic acid producing bacteria can be divided in two classes: homofermentative bacteria like "Lactobacillus casei" and "Lactococcus lactis", producing two moles of lactate from one mole of glucose, and heterofermentative species producing one mole of lactate from one mole of glucose as well as carbon dioxide and acetic acid/ethanol.


title: Lactic acid

text: Racemic lactic acid is synthesized industrially by reacting acetaldehyde with hydrogen cyanide and hydrolysing the resultant lactonitrile. When hydrolysis is performed by hydrochloric acid, ammonium chloride forms as a by-product; the Japanese company Musashino is one of the last big manufacturers of lactic acid by this route. Synthesis of both racemic and enantiopure lactic acids is also possible from other starting materials (vinyl acetate, glycerol, etc.) by application of catalytic procedures.


title: Lactic acid

text: -Lactic acid is the primary endogenous agonist of hydroxycarboxylic acid receptor 1 (HCA), a G protein-coupled receptor (GPCR).


title: Lactic acid

text: During power exercises such as sprinting, when the rate of demand for energy is high, glucose is broken down and oxidized to pyruvate, and lactate is then produced from the pyruvate faster than the body can process it, causing lactate concentrations to rise. The production of lactate is beneficial for NAD regeneration (pyruvate is reduced to lactate while NADH is oxidized to NAD), which is used up in oxidation of glyceraldehyde 3-phosphate during production of pyruvate from glucose, and this ensures that energy production is maintained and exercise can continue. During intense exercise, the respiratory chain cannot keep up with the amount of hydrogen ions that join to form NADH, and cannot regenerate NAD quickly enough.


title: Lactic acid

text: However, lactate is continually formed at rest and during all exercise intensities. Lactate serves as a metabolic fuel being produced and oxidatively disposed in resting and exercising muscle. Some causes of this are metabolism in red blood cells that lack mitochondria, and limitations resulting from the enzyme activity that occurs in muscle fibers having high glycolytic capacity. Lactic acidosis is a physiological condition characterized by accumulation of lactate (especially -lactate), with formation of an excessively low pH in the tissues a form of metabolic acidosis.


title: Lactic acid

text: Lactic acidosis during exercise may occur due to the H from ATP hydrolysis (ATP + HO → ADP + + H), and that reducing pyruvate to lactate (pyruvate + NADH + H → lactate + NAD) actually consumes H. The causative factors of the increase in [H] result from the production of lactate from a neutral molecule, increasing [H] to maintain electroneutrality. A contrary view is that lactate is produced from pyruvate, which has the same charge. It is pyruvate production from neutral glucose that generates H:


title: Lactic acid

text: Although the reaction glucose → 2 lactate + 2 H releases two H when viewed on its own, the H are absorbed in the production of ATP. On the other hand, the absorbed acidity is released during subsequent hydrolysis of ATP: ATP + HO → ADP + + H. So once the use of ATP is included, the overall reaction is


title: Lactic acid

text: Although glucose is usually assumed to be the main energy source for living tissues, there are a few reports that indicate that it is lactate, and not glucose, that is preferentially metabolized by neurons in the brain of several mammalian species (the notable ones being mice, rats, and humans). According to the lactate-shuttle hypothesis, glial cells are responsible for transforming glucose into lactate, and for providing lactate to the neurons. Because of this local metabolic activity of glial cells, the extracellular fluid immediately surrounding neurons strongly differs in composition from the blood or cerebrospinal fluid, being much richer with lactate, as was found in microdialysis studies.


title: Lactic acid

text: Some evidence suggests that lactate is important at early stages of development for brain metabolism in prenatal and early postnatal subjects, with lactate at these stages having higher concentrations in body liquids, and being utilized by the brain preferentially over glucose. It was also hypothesized that lactate may exert a strong action over GABAergic networks in the developing brain, making them more inhibitory than it was previously assumed, acting either through better support of metabolites, or alterations in base intracellular pH levels, or both.


title: Lactic acid

text: Studies of brain slices of mice show that β-hydroxybutyrate, lactate, and pyruvate act as oxidative energy substrates, causing an increase in the NAD(P)H oxidation phase, that glucose was insufficient as an energy carrier during intense synaptic activity and, finally, that lactate can be an efficient energy substrate capable of sustaining and enhancing brain aerobic energy metabolism "in vitro". The study "provides novel data on biphasic NAD(P)H fluorescence transients, an important physiological response to neural activation that has been reproduced in many studies and that is believed to originate predominantly from activity-induced concentration changes to the cellular NADH pools."


title: Lactic acid

text: Lactate can also serve as an important source of energy for other organs, including the heart and liver. During physical activity, up to 60% of the heart muscle's energy turnover rate derives from lactate oxidation.


title: Lactic acid

text: Blood tests for lactate are performed to determine the status of the acid base homeostasis in the body. Blood sampling for this purpose is often arterial (even if it is more difficult than venipuncture), because lactate levels differ substantially between arterial and venous, and the arterial level is more representative for this purpose.


title: Lactic acid

text: Two molecules of lactic acid can be dehydrated to the lactone lactide. In the presence of catalysts lactide polymerize to either atactic or syndiotactic polylactide (PLA), which are biodegradable polyesters. PLA is an example of a plastic that is not derived from petrochemicals.


title: Lactic acid

text: Lactic acid is also employed in pharmaceutical technology to produce water-soluble lactates from otherwise-insoluble active ingredients. It finds further use in topical preparations and cosmetics to adjust acidity and for its disinfectant and keratolytic properties.


title: Lactic acid

text: Lactic acid containing bacteria have shown promise in reducing Oxaluria (Kidney Stones) with its descaling properties on calcium compounds. 54


title: Lactic acid

text: Lactic acid is found primarily in sour milk products, such as kumis, laban, yogurt, kefir, and some cottage cheeses. The casein in fermented milk is coagulated (curdled) by lactic acid. Lactic acid is also responsible for the sour flavor of sourdough bread.


title: Lactic acid

text: In lists of nutritional information lactic acid might be included under the term "carbohydrate" (or "carbohydrate by difference") because this often includes everything other than water, protein, fat, ash, and ethanol. If this is the case then the calculated food energy may use the standard per gram that is often used for all carbohydrates. But in some cases lactic acid is ignored in the calculation. The energy density of lactic acid is per 100 g.


title: Lactic acid

text: Some beers (sour beer) purposely contain lactic acid, one such type being Belgian lambics. Most commonly, this is produced naturally by various strains of bacteria. These bacteria ferment sugars into acids, unlike the yeast that ferment sugar into ethanol. After cooling the wort, yeast and bacteria are allowed to “fall” into the open fermenters. Brewers of more common beer styles would ensure that no such bacteria are allowed to enter the fermenter. Other sour styles of beer include Berliner weisse, Flanders red and American wild ale.


title: Lactic acid

text: In winemaking, a bacterial process, natural or controlled, is often used to convert the naturally present malic acid to lactic acid, to reduce the sharpness and for other flavor-related reasons. This malolactic fermentation is undertaken by lactic acid bacteria.


title: Lactic acid

text: While not normally found in significant quantities in fruit, lactic acid is the primary organic acid in akebia fruit, making up 2.12% of the juice.


title: Lactic acid

text: As a food additive it is approved for use in the EU, USA and Australia and New Zealand; it is listed by its INS number 270 or as E number E270. Lactic acid is used as a food preservative, curing agent, and flavoring agent. It is an ingredient in processed foods and is used as a decontaminant during meat processing. Lactic acid is produced commercially by fermentation of carbohydrates such as glucose, sucrose, or lactose, or by chemical synthesis. Carbohydrate sources include corn, beets, and cane sugar.


title: Lactic acid

text: Lactic acid has historically been used to assist with the erasure of inks from official papers to be modified during forgery.


title: Lactic acid

text: Lactic acid is used in some liquid cleaners as a descaling agent for removing hard water deposits such as calcium carbonate, forming the lactate, calcium lactate. Owing to its high acidity, such deposits are eliminated very quickly, especially where boiling water is used, as in kettles. It also is gaining popularity in antibacterial dish detergents and hand soaps replacing Triclosan.


title: Gondwana

text: Gondwana () was a large landmass, often referred to as a supercontinent, that formed during the late Neoproterozoic (about 550 million years ago) and began to break up during the Jurassic period (about 180 million years ago). The final stages of break-up, involving the separation of Antarctica from South America (forming the Drake Passage) and Australia, occurred during the Paleogene. Gondwana was not considered a supercontinent by the earliest definition, since the landmasses of Baltica, Laurentia, and Siberia were separated from it. To differentiate it from the Indian region of the same name (see ), it is also commonly called Gondwanaland.


title: Gondwana

text: Gondwana was formed by the accretion of several cratons. Eventually, Gondwana became the largest piece of continental crust of the Palaeozoic Era, covering an area of about , about one-fifth of the Earth's surface. During the Carboniferous Period, it merged with Laurasia to form a larger supercontinent called Pangaea. Gondwana (and Pangaea) gradually broke up during the Mesozoic Era. The remnants of Gondwana make up around two-thirds of today's continental area, including South America, Africa, Antarctica, Australia, Zealandia, Arabia, and the Indian Subcontinent.


title: Gondwana

text: The formation of Gondwana began   with the East African Orogeny, the collision of India and Madagascar with East Africa, and was completed with the overlapping Brasiliano and Kuunga orogenies, the collision of South America with Africa, and the addition of Australia and Antarctica, respectively.


title: Gondwana

text: Regions that were part of Gondwana shared floral and zoological elements that persist to the present day.


title: Gondwana

text: The continent of Gondwana was named by the Austrian scientist Eduard Suess, after the region in central India of the same name, which is derived from Sanskrit for "forest of the Gonds". The name had been previously used in a geological context, first by H.B. Medlicott in 1872, from which the Gondwana sedimentary sequences (Permian-Triassic) are also described.


title: Gondwana

text: Some scientists prefer the term "Gondwanaland" to make a clear distinction between the region and the supercontinent.


title: Gondwana

text: The assembly of Gondwana was a protracted process during the Neoproterozoic and Paleozoic, which remains incompletely understood because of the lack of paleo-magnetic data. Several orogenies, collectively known as the Pan-African orogeny, caused the continental fragments of a much older supercontinent, Rodinia, to amalgamate. One of those orogenic belts, the Mozambique Belt, formed and was originally interpreted as the suture between East (India, Madagascar, Antarctica, and Australia) and West Gondwana (Africa and South America). Three orogenies were recognised during the 1990s: the East African Orogeny () and Kuunga orogeny (including the Malagasy Orogeny in southern Madagascar) (), the collision between East Gondwana and East Africa in two steps, and the Brasiliano orogeny (), the successive collision between South American and African cratons.


title: Gondwana

text: The last stages of Gondwanan assembly overlapped with the opening of the Iapetus Ocean between Laurentia and western Gondwana. During this interval, the Cambrian explosion occurred. Laurentia was docked against the western shores of a united Gondwana for a brief period near the Precambrian/Cambrian boundary, forming the short-lived and still disputed supercontinent Pannotia.


title: Gondwana

text: The Mozambique Ocean separated the Congo–Tanzania–Bangweulu Block of central Africa from Neoproterozoic India (India, the Antongil Block in far eastern Madagascar, the Seychelles, and the Napier and Rayner Complexes in East Antarctica). The Azania continent (much of central Madagascar, the Horn of Africa and parts of Yemen and Arabia) was an island in the Mozambique Ocean.


title: Gondwana

text: The continent Australia/Mawson was still separated from India, eastern Africa, and Kalahari by , when most of western Gondwana had already been amalgamated. By 550 Ma, India had reached its Gondwanan position, which initiated the Kuunga orogeny (also known as the Pinjarra orogeny). Meanwhile, on the other side of the newly forming Africa, Kalahari collided with Congo and Rio de la Plata which closed the Adamastor Ocean. 540–530 Ma, the closure of the Mozambique Ocean brought India next to Australia–East Antarctica, and both North and South China were in proximity to Australia.


title: Gondwana

text: As the rest of Gondwana formed, a complex series of orogenic events assembled the eastern parts of Gondwana (eastern Africa, Arabian-Nubian Shield, Seychelles, Madagascar, India, Sri Lanka, East Antarctica, and Australia) . First the Arabian-Nubian Shield collided with eastern Africa (in the Kenya-Tanzania region) in the East African Orogeny . Then Australia and East Antarctica were merged with the remaining Gondwana in the Kuunga Orogeny.


title: Gondwana

text: The later Malagasy orogeny at about 550–515 Mya affected Madagascar, eastern East Africa and southern India. In it, Neoproterozoic India collided with the already combined Azania and Congo–Tanzania–Bangweulu Block, suturing along the Mozambique Belt.


title: Gondwana

text: The Terra Australis Orogen developed along Gondwana's western, southern, and eastern margins. Proto-Gondwanan Cambrian arc belts from this margin have been found in eastern Australia, Tasmania, New Zealand, and Antarctica. Though these belts formed a continuous arc chain, the direction of subduction was different between the Australian-Tasmanian and New Zealand-Antarctica arc segments.


title: Gondwana

text: Many terranes were accreted to Eurasia during Gondwana's existence, but the Cambrian or Precambrian origin of many of these terranes remains uncertain. For example, some Palaeozoic terranes and microcontinents that now make up Central Asia, often called the "Kazakh" and "Mongolian terranes", were progressively amalgamated into the continent Kazakhstania in the Late Silurian. Whether these blocks originated on the shores of Gondwana is not known.


title: Gondwana

text: In the Early Palaeozoic, the Armorican terrane, which today form large parts of France, was part of either Peri-Gondwana or core Gondwana; the Rheic Ocean closed in front of it and the Palaeo-Tethys Ocean opened behind it. Precambrian rocks from the Iberian Peninsula suggest that it, too, formed part of core Gondwana before its detachment as an orocline in the Variscan orogeny close to the Carboniferous–Permian boundary.


title: Gondwana

text: South-east Asia was made of Gondwanan and Cathaysian continental fragments that were assembled during the Mid-Palaeozoic and Cenozoic. This process can be divided into three phases of rifting along Gondwana's northern margin: first, in the Devonian, North and South China, together with Tarim and Quidam (north-western China) rifted, opening the Palaeo-Tethys behind them. These terranes accreted to Asia during Late Devonian and Permian. Second, in the Late Carboniferous to Early Permian, Cimmerian terranes opened Meso-Tethys Ocean; Sibumasu and Qiangtang were added to south-east Asia during Late Permian and Early Jurassic. Third, in the Late Triassic to Late Jurassic, Lhasa, West Burma, Woyla terranes opened the Neo-Tethys Ocean; Lhasa collided with Asia during the Early Cretaceous, and West Burma and Woyla during the Late Cretaceous.


title: Gondwana

text: Gondwana's long, northern margin remained a mostly passive margin throughout the Palaeozoic. The Early Permian opening of the Neo-Tethys Ocean along this margin produced a long series of terranes, many of which were and still are being deformed in the Himalaya Orogeny. These terranes are, from Turkey to north-eastern India: the Taurides in southern Turkey; the Lesser Caucasus Terrane in Georgia; the Sanand, Alborz, and Lut terranes in Iran; the Mangysglak or Kopetdag Terrane in the Caspian Sea; the Afghan Terrane; the Karakorum Terrane in northern Pakistan; and the Lhasa and Qiangtang terranes in Tibet. The Permian–Triassic widening of the Neo-Tethys pushed all these terranes across the Equator and over to Eurasia.


title: Gondwana

text: During the Neoproterozoic to Palaeozoic phase of the Terra Australis Orogen, a series of terranes were rafted from the proto-Andean margin when the Iapteus Ocean opened, to be added back to Gondwana during the closure of that ocean. During the Paleozoic, some blocks which helped to form parts of the Southern Cone of South America, include a piece transferred from Laurentia when the west edge of Gondwana scraped against southeast Laurentia in the Ordovician. This is the Cuyania or Precordillera terrane of the Famatinian orogeny in northwest Argentina which may have continued the line of the Appalachians southwards. Chilenia terrane accreted later against Cuyania. The collision of the Patagonian terrane with the southwestern Gondwanan occurred in the late Paleozoic. Subduction-related igneous rocks from beneath the North Patagonian Massif have been dated at 320–330 million years old, indicating that the subduction process initiated in the early Carboniferous. This was relatively short lived (lasting about 20 million years), and initial contact of the two landmasses occurred in the mid-Carboniferous, with broader collision during the early Permian. In the Devonian, an island arc named Chaitenia accreted to Patagonia in what is now south-central Chile.


title: Gondwana

text: Gondwana and Laurasia formed the Pangaea supercontinent during the Carboniferous. Pangaea began to break up in the Mid-Jurassic when the Central Atlantic opened.


title: Gondwana

text: In the western end of Pangaea, the collision between Gondwana and Laurasia closed the Rheic and Palaeo-Tethys oceans. The obliquity of this closure resulted in the docking of some northern terranes in the Marathon, Ouachita, Alleghanian, and Variscan orogenies, respectively. Southern terranes, such as Chortis and Oaxaca, on the other hand, remained largely unaffected by the collision along the southern shores of Laurentia. Some Peri-Gondwanan terranes, such as Yucatán and Florida, were buffered from collisions by major promontories. Other terranes, such as Carolina and Meguma, were directly involved in the collision. The final collision resulted in the Variscan-Appalachian Mountains, stretching from present-day Mexico to southern Europe. Meanwhile, Baltica collided with Siberia and Kazakhstania which resulted in the Uralian orogeny and Laurasia. Pangaea was finally amalgamated in the Late Carboniferous-Early Permian, but the oblique forces continued until Pangaea began to rift in the Triassic.


title: Gondwana

text: In the eastern end, collisions occurred slightly later. The North China, South China, and Indochina blocks rifted from Gondwana during the middle Paleozoic and opened the Proto-Tethys Ocean. North China docked with Mongolia and Siberia during the Carboniferous–Permian, followed by South China. The Cimmerian blocks then rifted from Gondwana to form the Palaeo-Thethys and Neo-Tethys oceans in the Late Carboniferous, and docked with Asia during the Triassic and Jurassic. Western Pangaea began to rift while the eastern end was still being assembled.


title: Gondwana

text: The formation of Pangaea and its mountains had a tremendous impact on global climate and sea levels, which resulted in glaciations and continent-wide sedimentation. In North America, the base of the Absaroka sequence coincides with the Alleghanian and Ouachita orogenies and are indicative of a large-scale change in the mode of deposition far away from the Pangaean orogenies. Ultimately, these changes contributed to the Permian–Triassic extinction event and left large deposits of hydrocarbons, coal, evaporite, and metals.


title: Gondwana

text: The break-up of Pangaea began with the Central Atlantic magmatic province (CAMP) between South America, Africa, North America, and Europe. CAMP covered more than seven million square kilometres over a few million years, reached its peak at , and coincided with the Triassic–Jurassic extinction event. The reformed Gondwanan continent was not precisely the same as that which had existed before Pangaea formed; for example, most of Florida and southern Georgia and Alabama is underlain by rocks that were originally part of Gondwana, but this region stayed attached to North America when the Central Atlantic opened.


title: Gondwana

text: Antarctica, the centre of the supercontinent, shared boundaries with all other Gondwana continents and the fragmentation of Gondwana propagated clockwise around it. The break-up was the result of the eruption of the Karoo-Ferrar igneous province, one of the Earth's most extensive large igneous provinces (LIP) , but the oldest magnetic anomalies between South America, Africa, and Antarctica are found in what is now the southern Weddell Sea where initial break-up occurred during the Jurassic .


title: Gondwana

text: Gondwana began to break up in the early Jurassic following the extensive and fast emplacement of the Karoo-Ferrar flood basalts . Before the Karoo plume initiated rifting between Africa and Antarctica, it separated a series of smaller continental blocks from Gondwana's southern, Proto-Pacific margin (along what is now the Transantarctic Mountains): the Antarctic Peninsula, Marie Byrd Land, Zealandia, and Thurston Island; the Falkland Islands and Ellsworth–Whitmore Mountains (in Antarctica) were rotated 90° in opposite directions; and South America south of the Gastre Fault (often referred to as Patagonia) was pushed westward. The history of the Africa-Antarctica break-up can be studied in great detail in the fracture zones and magnetic anomalies flanking the Southwest Indian Ridge.


title: Gondwana

text: The Madagascar block and the Mascarene Plateau, stretching from the Seychelles to Réunion, were broken off India, causing Madagascar and Insular India to be separate landmasses: elements of this break-up nearly coincide with the Cretaceous–Paleogene extinction event. The India–Madagascar–Seychelles separations appear to coincide with the eruption of the Deccan basalts, whose eruption site may survive as the Réunion hotspot. The Seychelles and the Maldives are now separated by the Central Indian Ridge.


title: Gondwana

text: During the initial break-up in the Early Jurassic a marine transgression swept over the Horn of Africa covering Triassic planation surfaces with sandstone, limestone, shale, marls and evaporites.


title: Gondwana

text: East Gondwana, comprising Antarctica, Madagascar, India, and Australia, began to separate from Africa. East Gondwana then began to break up when India moved northwest from Australia-Antarctica. The Indian Plate and the Australian Plate are now separated by the Capricorn Plate and its diffuse boundaries. During the opening of the Indian Ocean, the Kerguelen hotspot first formed the Kerguelen Plateau on the Antarctic Plate and then the Ninety East Ridge on the Indian Plate at . The Kerguelen Plateau and the Broken Ridge, the southern end of the Ninety East Ridge, are now separated by the Southeast Indian Ridge.


title: Gondwana

text: Separation between Australia and East Antarctica began with seafloor spreading occurring . A shallow seaway developed over the South Tasman Rise during the Early Cenozoic and as oceanic crust started to separate the continents during the Eocene global ocean temperature dropped significantly. A dramatic shift from arc- to rift magmatism separated Zealandia, including New Zealand, the Campbell Plateau, Chatham Rise, Lord Howe Rise, Norfolk Ridge, and New Caledonia, from West Antarctica .


title: Gondwana

text: The opening of the South Atlantic Ocean divided West Gondwana (South America and Africa), but there is a considerable debate over the exact timing of this break-up. Rifting propagated from south to north along Triassic–Early Jurassic lineaments, but intra-continental rifts also began to develop within both continents in Jurassic–Cretaceous sedimentary basins; subdividing each continent into three sub-plates. Rifting began at Falkland latitudes, forcing Patagonia to move relative to the still static remainder of South America and Africa, and this westward movement lasted until the Early Cretaceous . From there rifting propagated northward during the Late Jurassic or Early Cretaceous most likely forcing dextral movements between sub-plates on either side. South of the Walvis Ridge and Rio Grande Rise the Paraná and Etendeka magmatics resulted in further ocean-floor spreading and the development of rifts systems on both continents, including the Central African Rift System and the Central African Shear Zone which lasted until . At Brazilian latitudes spreading is more difficult to assess because of the lack of palaeo-magnetic data, but rifting occurred in Nigeria at the Benue Trough . North of the Equator the rifting began after and continued until .


title: Gondwana

text: The first phases of Andean orogeny in the Jurassic and Early Cretaceous were characterised by extensional tectonics, rifting, the development of back-arc basins and the emplacement of large batholiths. This development is presumed to have been linked to the subduction of cold oceanic lithosphere. During the mid to Late Cretaceous (), the Andean orogeny changed significantly in character. Warmer and younger oceanic lithosphere is believed to have started to be subducted beneath South America around this time. Such kind of subduction is held responsible not only for the intense contractional deformation that different lithologies were subject to, but also the uplift and erosion known to have occurred from the Late Cretaceous onward. Plate tectonic reorganisation since the mid-Cretaceous might also have been linked to the opening of the South Atlantic Ocean. Another change related to mid-Cretaceous plate tectonic rearrangement was the change of subduction direction of the oceanic lithosphere that went from having south-east motion to having a north-east motion at about 90 million years ago. While subduction direction changed, it remained oblique (and not perpendicular) to the coast of South America, and the direction change affected several subduction zone-parallel faults including Atacama, Domeyko and Liquiñe-Ofqui.


title: Gondwana

text: Insular India began to collide with Asia circa , forming the Indian subcontinent, since which more than of crust has been absorbed by the Himalayan-Tibetan orogen. During the Cenozoic, the orogen resulted in the construction of the Tibetan Plateau between the Tethyan Himalayas in the south and the Kunlun and Qilian mountains in the north.


title: Gondwana

text: Later, South America was connected to North America via the Isthmus of Panama, cutting off a circulation of warm water and thereby making the Arctic colder, as well as allowing the Great American Interchange.


title: Gondwana

text: The break-up of Gondwana can be said to continue in eastern Africa at the Afar Triple Junction, which separates the Arabian, Nubian, and Somali plates, resulting in rifting in the Red Sea and East African Rift.


title: Gondwana

text: In the Early Cenozoic, Australia was still connected to Antarctica 35–40° south of its current location and both continents were largely unglaciated. A rift between the two developed but remained an embayment until the Eocene-Oligocene boundary when the Circumpolar Current developed and the glaciation of Antarctica began.


title: Gondwana

text: Australia was warm and wet during the Palaeocene and dominated by rainforest. The opening of the Tasman Gateway at the Eocene-Oligocene boundary () resulted in abrupt cooling but the Oligocene became a period of high rainfall with swamps in southeast Australia. During the Miocene, a warm and humid climate developed with pockets of rainforests in central Australia, but before the end of the period, colder and drier climate severely reduced this rainforest. A brief period of increased rainfall in the Pliocene was followed by drier climate which favoured grassland. Since then, the fluctuation between wet interglacial periods and dry glacial periods has developed into the present arid regime. Australia has thus experienced various climate changes over a 15-million-year period with a gradual decrease in precipitation.


title: Gondwana

text: The Tasman Gateway between Australia and Antarctica began to open . Palaeontological evidence indicates the Antarctic Circumpolar Current (ACC) was established in the Late Oligocene with the full opening of the Drake Passage and the deepening of the Tasman Gateway. The oldest oceanic crust in the Drake Passage, however, is -old which indicates that the spreading between the Antarctic and South American plates began near the Eocene/Oligocene boundary. Deep sea environments in Tierra del Fuego and the North Scotia Ridge during the Eocene and Oligocene indicate a "Proto-ACC" opened during this period. Later, , a series of events severally restricted the Proto-ACC: change to shallow marine conditions along the North Scotia Ridge; closure of the Fuegan Seaway, the deep sea that existed in Tierra del Fuego; and uplift of the Patagonian Cordillera. This, together with the reactivated Iceland plume, contributed to global warming. During the Miocene, the Drake Passage began to widen, and as water flow between South America and the Antarctic Peninsula increased, the renewed ACC resulted in cooler global climate.


title: Gondwana

text: Since the Eocene, the northward movement of the Australian Plate has resulted in an arc-continent collision with the Philippine and Caroline plates and the uplift of the New Guinea Highlands. From the Oligocene to the late Miocene, the climate in Australia, dominated by warm and humid rainforests before this collision, began to alternate between open forest and rainforest before the continent became the arid or semiarid landscape it is today.


title: Gondwana

text: The adjective "Gondwanan" is in common use in biogeography when referring to patterns of distribution of living organisms, typically when the organisms are restricted to two or more of the now-discontinuous regions that were once part of Gondwana, including the Antarctic flora. For example, the plant family Proteaceae, known from all continents in the Southern Hemisphere, has a "Gondwanan distribution" and is often described as an archaic, or relict, lineage. The distributions in the Proteaceae is, nevertheless, the result of both Gondwanan rafting and later oceanic dispersal.


title: Gondwana

text: During the Silurian, Gondwana extended from the Equator (Australia) to the South Pole (North Africa and South America) whilst Laurasia was located on the Equator opposite to Australia. A short-lived Late Ordovician glaciation was followed by a Silurian Hot House period. The End-Ordovician extinction, which resulted in 27% of marine invertebrate families and 57% of genera going extinct, occurred during this shift from Ice House to Hot House.


title: Gondwana

text: By the end of the Ordovician, "Cooksonia", a slender, ground-covering plant, became the first vascular plant to establish itself on land. This first colonisation occurred exclusively around the Equator on landmasses then limited to Laurasia and, in Gondwana, to Australia. In the Late Silurian, two distinctive lineages, zosterophylls and rhyniophytes, had colonised the tropics. The former evolved into the lycopods that were to dominate the Gondwanan vegetation over a long period, whilst the latter evolved into horsetails and gymnosperms. Most of Gondwana was located far from the Equator during this period and remained a lifeless and barren landscape.


title: Gondwana

text: West Gondwana drifted north during the Devonian, bringing Gondwana and Laurasia close together. Global cooling contributed to the Late Devonian extinction (19% of marine families and 50% of genera went extinct) and glaciation occurred in South America. Before Pangaea had formed, terrestrial plants, such as pteridophytes, began to diversify rapidly resulting in the colonisation of Gondwana. The Baragwanathia Flora, found only in the Yea Beds of Victoria, Australia, occurs in two strata separated by or 30 Ma; the upper assemblage is more diverse and includes Baragwanathia, the first primitive herbaceous lycopod to evolve from the zosterophylls. During the Devonian, giant club mosses replaced the Baragwanathia Flora, introducing the first trees, and by the Late Devonian this first forest was accompanied by the progymnosperms, including the first large trees "Archaeopteris". The Late Devonian extinction probably also resulted in osteolepiform fishes evolving into the amphibian tetrapods, the earliest land vertebrates, in Greenland and Russia. The only traces of this evolution in Gondwana are amphibian footprints and a single jaw from Australia.


title: Gondwana

text: The closure of the Rheic Ocean and the formation of Pangaea in the Carboniferous resulted in the rerouting of ocean currents that initiated an Ice House period. As Gondwana began to rotate clockwise, Australia shifted south to more temperate latitudes. An ice cap initially covered most of southern Africa and South America but spread to eventually cover most of the supercontinent, save for northernmost Africa-South America and eastern Australia. Giant lycopod and horsetail forests continued to evolve in tropical Laurasia together with a diversified assemblage of true insects. In Gondwana, in contrast, ice and, in Australia, volcanism decimated the Devonian flora to a low-diversity seed fern flora – the pteridophytes were increasingly replaced by the gymnosperms which were to dominate until the Mid-Cretaceous. Australia, however, was still located near the Equator during the Early Carboniferous, and during this period, temnospondyl and lepospondyl amphibians and the first amniote reptilians evolved, all closely related to the Laurasian fauna, but spreading ice eventually drove these animals away from Gondwana entirely.


title: Gondwana

text: The Gondwana ice sheet melted, and sea levels dropped during the Permian and Triassic global warming. During this period, the extinct glossopterids colonised Gondwana and reached peak diversity in the Late Permian when coal-forming forests covered much of Gondwana. The period also saw the evolution of Voltziales, one of the few plant orders to survive the end-Permian extinction (57% of marine families and 83% of genera went extinct) and which came to dominate in the Late Permian and from whom true conifers evolved. Tall lycopods and horsetails dominated the wetlands of Gondwana in the Early Permian. Insects co-evolved with glossopterids across Gondwana and diversified with more than 200 species in 21 orders by the Late Permian, many known from South Africa and Australia. Beetles and cockroaches remained minor elements in this fauna. Tetrapod fossils from the Early Permian have only been found in Laurasia but they became common in Gondwana later during the Permian. The arrival of the therapsids resulted in the first plant-vertebrate-insect ecosystem.


title: Gondwana

text: During the Mid- to Late Triassic, hot-house conditions coincided with a peak in biodiversity — the end-Permian extinction was enormous and so was the radiation that followed. Two families of conifers, Podocarpaceae and Araucariaceae, dominated Gondwana in the Early Triassic, but "Dicroidium", an extinct genus of fork-leaved seed ferns, dominated woodlands and forests of Gondwana during most of the Triassic. Conifers evolved and radiated during the period, with six of eight extant families already present before the end of it. Bennettitales and Pentoxylales, two now extinct orders of gymnospermous plants, evolved in the Late Triassic and became important in the Jurassic and Cretaceous. It is possible that gymnosperm biodiversity surpassed later angiosperm biodiversity and that the evolution of angiosperms began during the Triassic but, if so, in Laurasia rather than in Gondwana. Two Gondwanan classes, lycophytes and sphenophytes, saw a gradual decline during the Triassic while ferns, though never dominant, managed to diversify.


title: Gondwana

text: The brief period of icehouse conditions during the Triassic–Jurassic extinction event had a dramatic impact on dinosaurs but left plants largely unaffected. The Jurassic was mostly one of hot-house conditions and, while vertebrates managed to diversify in this environment, plants have left little evidence of such development, apart from Cheiroleidiacean conifers and Caytoniales and other groups of seed ferns. In terms of biomass, the Jurassic flora was dominated by conifer families and other gymnosperms that had evolved during the Triassic. The Pteridophytes that had dominated during the Palaeozoic were now marginalised, except for ferns. In contrast to Laurentia, very few insect fossils have been found in Gondwana, to a considerable extent because of widespread deserts and volcanism. While plants had a cosmopolitan distribution, dinosaurs evolved and diversified in a pattern that reflects the Jurassic break-up of Pangaea.


title: Gondwana

text: The Cretaceous saw the arrival of the angiosperms, or flowering plants, a group that probably evolved in western Gondwana (South America-Africa). From there the angiosperms diversified in two stages: the monocots and magnoliids evolved in the Early Cretaceous, followed by the hammamelid dicots. By the Mid-Cretaceous, angiosperms constituted half of the flora in northeastern Australia. There is, however, no obvious connection between this spectacular angiosperm radiation and any known extinction event nor with vertebrate/insect evolution. Insect orders associated with pollination, such as beetles, flies, butterflies and moths, and wasps, bees, and ants, radiated continuously from the Permian-Triassic, long before the arrival of the angiosperms. Well-preserved insect fossils have been found in the lake deposits of the Santana Formation in Brazil, the Koonwarra Lake fauna in Australia, and the Orapa diamond mine in Botswana.


title: Gondwana

text: Dinosaurs continued to prosper but, as the angiosperm diversified, conifers, bennettitaleans and pentoxylaleans disappeared from Gondwana 115 Ma together with the specialised herbivorous ornithischians, whilst generalist browsers, such as several families of sauropodomorph Saurischia, prevailed. The Cretaceous–Paleogene extinction event killed off all dinosaurs except birds, but plant evolution in Gondwana was hardly affected. Gondwanatheria is an extinct group of non-therian mammals with a Gondwanan distribution (South America, Africa, Madagascar, India, Zealandia and Antarctica) during the Late Cretaceous and Palaeogene. Xenarthra and Afrotheria, two placental clades, are of Gondwanan origin and probably began to evolve separately when Africa and South America separated.


title: Gondwana

text: The laurel forests of Australia, New Caledonia, and New Zealand have a number of species related to those of the laurissilva of Valdivia, through the connection of the Antarctic flora. These include gymnosperms and the deciduous species of "Nothofagus", as well as the New Zealand laurel, "Corynocarpus laevigatus", and "Laurelia novae-zelandiae". New Caledonia and New Zealand became separated from Australia by continental drift 85 million years ago. The islands still retain plants that originated in Gondwana and spread to the Southern Hemisphere continents later.


title: England cricket team

text: The England cricket team represents England and Wales in international cricket. Since 1997, it has been governed by the England and Wales Cricket Board (ECB), having been previously governed by Marylebone Cricket Club (the MCC) since 1903. England, as a founding nation, is a Full Member of the International Cricket Council (ICC) with Test, One Day International (ODI) and Twenty20 International (T20I) status. Until the 1990s, Scottish and Irish players also played for England as those countries were not yet ICC members in their own right.


title: England cricket team

text: England and Australia were the first teams to play a Test match (15–19 March 1877), and along with South Africa, these nations formed the Imperial Cricket Conference (the predecessor to today's International Cricket Council) on 15 June 1909. England and Australia also played the first ODI on 5 January 1971. England's first T20I was played on 13 June 2005, once more against Australia.


title: England cricket team

text: , England have played 1,058 Test matches, winning 387 and losing 317 (with 354 draws). In Test series against Australia, England play for The Ashes, one of the most famous trophies in all of sport, and they have won the urn on 32 occasions. England have also played 773 ODIs, winning 389. They have appeared in the final of the Cricket World Cup four times, winning once in 2019; they have also finished as runners-up in two ICC Champions Trophies (2004 and 2013). England have played 170 T20Is, winning 90. They won the ICC T20 World Cup in 2010 and 2022, and were runners-up in 2016.


title: England cricket team

text: The first recorded incidence of a team with a claim to represent England comes from 9 July 1739 when an "All-England" team, which consisted of 11 gentlemen from any part of England exclusive of Kent, played against "the Unconquerable County" of Kent and lost by a margin of "very few notches". Such matches were repeated on numerous occasions for the best part of a century.


title: England cricket team

text: In 1846 William Clarke formed the All-England Eleven. This team eventually competed against a United All-England Eleven with annual matches occurring between 1847 and 1856. These matches were arguably the most important contest of the English season if judged by the quality of the players.


title: England cricket team

text: The first overseas tour occurred in September 1859 with England touring North America. This team had six players from the All-England Eleven, six from the United All-England Eleven and was captained by George Parr.


title: England cricket team

text: With the outbreak of the American Civil War, attention turned elsewhere. English tourists visited Australia in 1861–62 with this first tour organised as a commercial venture by Messrs Spiers and Pond, restaurateurs of Melbourne. Most matches played during tours prior to 1877 were "against odds", with the opposing team fielding more than 11 players to make for a more even contest. This first Australian tour were mostly against odds of at least 18/11.


title: England cricket team

text: The tour was so successful that Parr led a second tour in 1863–64. James Lillywhite led a subsequent England team which sailed on the P&O steamship "Poonah" on 21 September 1876. They played a combined Australian XI, for once on even terms of 11-a-side. The match, starting on 15 March 1877 at the Melbourne Cricket Ground came to be regarded as the inaugural Test match. The combined Australian XI won this Test match by 45 runs with Charles Bannerman of Australia scoring the first Test century. At the time, the match was promoted as "James Lillywhite's XI v Combined Victoria and New South Wales". The teams played a return match on the same ground at Easter, 1877, when Lillywhite's team avenged their loss with a victory by four wickets. The first Test match on English soil occurred in 1880 with England victorious; this was the first time England fielded a fully representative side with W. G. Grace included in the team.


title: England cricket team

text: England lost their first home series 1–0 in 1882, with "The Sporting Times" printing an obituary on English cricket:


title: England cricket team

text: As a result of this loss, the tour of 1882–83 was dubbed by England captain Ivo Bligh as "the quest to regain the ashes". England, with a mixture of amateurs and professionals, won the series 2–1. Bligh was presented with an urn that contained some ashes, which have variously been said to be of a bail, ball or even a woman's veil, and so The Ashes was born. A fourth match was then played which Australia won by four wickets. However, the match was not considered part of the Ashes series. England dominated many of these early contests, with England winning the Ashes series 10 times between 1884 and 1898. During this period England also played their first Test match against South Africa in 1889 at Port Elizabeth.


title: England cricket team

text: England won the 1890 Ashes series 2–0, with the third match of the series being the first Test match to be abandoned. England lost 2–1 in the 1891–92 series, although England regained the urn the following year. England again won the 1894–95 series, winning 3–2 under the leadership of Andrew Stoddart. In 1895–96, England played South Africa, winning all Tests in the series. The 1899 Ashes series was the first tour where the MCC and the counties appointed a selection committee. There were three active players: Grace, Lord Hawke and Warwickshire captain Herbert Bainbridge. Prior to this, England teams for home Tests had been chosen by the club on whose ground the match was to be played. England lost the 1899 Ashes series 1–0, with Grace making his final Test appearance in the first match of the series.


title: England cricket team

text: The start of the 20th century saw mixed results for England as they lost four of the eight Ashes series between 1900 and 1914. During this period, England lost their first series against South Africa in the 1905–06 season 4–1 as their batting faltered.


title: England cricket team

text: England lost their first series of the new century to Australia in 1901–02 Ashes. Australia also won the 1902 series, which was memorable for exciting cricket, including Gilbert Jessop scoring a Test century in just 70 minutes. England regained the Ashes in 1904 under the captaincy of Pelham Warner. R. E. Foster scored 287 on his debut and Wilfred Rhodes took 15 wickets in a match. In 1905–06, England lost 4–1 against South Africa. England avenged the defeat in 1907, when they won the series 1–0 under the captaincy of Foster. However, they lost the 1909 Ashes series against Australia, suing 25 players in the process. England also lost to South Africa, with Jack Hobbs scoring his first of 15 centuries on the tour.


title: England cricket team

text: England toured Australia in 1911–12 and beat their opponents 4–1. The team included the likes of Rhodes, Hobbs, Frank Woolley and Sydney Barnes. England lost the first match of the series but bounced back and won the next four Tests. This proved to be the last Ashes series before the war.


title: England cricket team

text: The 1912 season saw England take part in a unique experiment. A nine-Test triangular tournament involving England, South Africa and Australia was set up. The series was hampered by a very wet summer and player disputes however and the tournament was considered a failure with the "Daily Telegraph" stating:


title: England cricket team

text: With Australia sending a weakened team and the South African bowlers being ineffective England dominated the tournament winning four of their six matches. The match between Australia and South Africa at Lord's was visited by King George V, the first time a reigning monarch had watched Test cricket. England went on one more tour before the outbreak of the First World War, beating South Africa 4–0, with Barnes taking 49 wickets in the series.


title: England cricket team

text: England's first match after the war was in the 1920–21 season against Australia. Still feeling the effects of the war England went down to a series of crushing defeats and suffered their first whitewash losing the series 5–0. Six Australians scored hundreds while Mailey spun out 36 English batsmen. Things were no better in the next few Ashes series losing the 1921 Ashes series 3–0 and the 1924–25 Ashes 4–1. England's fortunes were to change in 1926 as they regained the Ashes and were a formidable team during this period dispatching Australia 4–1 in the 1928–29 Ashes tour.


title: England cricket team

text: On the same year the West Indies became the fourth nation to be granted Test status and played their first game against England. England won each of these three Tests by an innings, and a view was expressed in the press that their elevation had proved a mistake although Learie Constantine did the double on the tour. In the 1929–30 season England went on two concurrent tours with one team going to New Zealand (who were granted Test status earlier that year) and the other to the West Indies. Despite sending two separate teams England won both tours beating New Zealand 1–0 and the West Indies 2–1.


title: England cricket team

text: The 1930 Ashes series saw a young Don Bradman dominate the tour, scoring 974 runs in his seven Test innings. He scored 254 at Lord's, 334 at Headingley and 232 at The Oval. Australia regained the Ashes winning the series 3–1. As a result of Bradman's prolific run-scoring the England captain Douglas Jardine chose to develop the already existing leg theory into fast leg theory, or bodyline, as a tactic to stop Bradman. Fast leg theory involved bowling fast balls directly at the batsman's body. The batsman would need to defend himself, and if he touched the ball with the bat, he risked being caught by one of a large number of fielders placed on the leg side.


title: England cricket team

text: Using Jardine's fast leg theory, England won the next Ashes series 4–1, but complaints about the Bodyline tactic caused crowd disruption on the tour, and threats of diplomatic action from the Australian Cricket Board, which during the tour sent the following cable to the MCC in London:


title: England cricket team

text: Later, Jardine was removed from the captaincy and the Laws of Cricket changed so that no more than one fast ball aimed at the body was permitted per over, and having more than two fielders behind square leg was banned.


title: England cricket team

text: England's following tour of India in the 1933–34 season was the first Test match to be staged in the subcontinent. The series was also notable for Stan Nichols and Nobby Clark bowling so many bouncers that the Indian batsman wore solar toupées instead of caps to protect themselves.


title: England cricket team

text: Australia won the 1934 Ashes series 2–1 and kept the urn for the following 19 years. Many of the wickets of the time were friendly to batsmen resulting in a large proportion of matches ending in high scoring draws and many batting records being set.


title: England cricket team

text: England drew the 1938 Ashes, meaning Australia retained the urn. England went into the final match of the series at The Oval 1–0 down, but won the final game by an innings and 579 runs. Len Hutton made the highest ever Test score by an Englishman, making 364 in England first innings to help them reach 903, their highest ever score against Australia.


title: England cricket team

text: The 1938–39 tour of South Africa saw another experiment with the deciding Test being a timeless Test that was played to a finish. England lead 1–0 going into the final timeless match at Durban. Despite the final Test being 'timeless', the game ended in a draw after 10 days as England had to catch the train to catch the boat home. A record 1,981 runs were scored, and the concept of timeless Tests was abandoned. England went on one final tour of the West Indies in 1939 before the Second World War, although a team for an MCC tour of India was selected more in hope than expectation of the matches being played.


title: England cricket team

text: Test cricket resumed after the war in 1946, and England won their first match back against India. However, they struggled in the 1946–47 Ashes series, losing 3–0 in Australia under Wally Hammond's captaincy. England beat South Africa 3–0 in 1947 with Denis Compton scoring 1,187 runs in the series.


title: England cricket team

text: The 1947–48 series against the West Indies was another disappointment for England, with the side losing 2–0 following injuries to several key players. England suffered further humiliation against Bradman's invincible side in the 1948 Ashes series. Hutton was controversially dropped for the third Test, and England were bowled out for just 52 at The Oval. The series proved to be Bradman's final Ashes series.


title: England cricket team

text: In 1948–49, England beat South Africa 2–0 under the captaincy of George Mann. The series included a record breaking stand of 359 between Hutton and Cyril Washbrook. The decade ended with England drawing the Test series against New Zealand, with every match ending in a draw.


title: England cricket team

text: Their fortunes changed on the 1953 Ashes tour as they won the series 1–0. England did not lose a series between their 1950–51 and 1958–59 tours of Australia and secured famous victory in 1954–55 under the captaincy of Len Hutton, thanks to Frank Tyson whose 6/85 at Sydney and 7/27 at Melbourne are remembered as the fastest bowling ever seen in Australia. The 1956 series was remembered for the bowling of Jim Laker who took 46 wickets at an average of 9.62, including figures of 19/90 at Old Trafford. After drawing to South Africa, England defeated the West Indies and New Zealand comfortably.


title: England cricket team

text: The England team then left for Australia in the 1958–59 season with a team that had been hailed as the strongest ever to leave on an Ashes tour but lost the series 4–0 as Richie Benaud's revitalised Australians were too strong, with England struggling with the bat throughout the series.


title: England cricket team

text: On 24 August 1959, England inflicted its only 5–0 whitewash over India. All out for 194 at The Oval, India lost the last test by an innings. England's batsman Ken Barrington and Colin Cowdrey both had an excellent series with the bat, with Barrington scoring 357 runs across the series and Cowdrey scoring 344.


title: England cricket team

text: The early and middle 1960s were poor periods for English cricket. Despite England's strength on paper, Australia held the Ashes and the West Indies dominated England in the early part of the decade. May stood down as captain in 1961 following the 1961 Ashes defeat.


title: England cricket team

text: Ted Dexter succeeded him as captain but England continued to suffer indifferent results. In 1961–62, they beat Pakistan, but also lost to India. The following year saw England and Australia tie the 1962–63 Ashes series 1–1, meaning Australia retained the urn. Despite beating New Zealand 3–0, England went on to lose to the West Indies, and again failed in the 1964 Ashes, losing the home series 1–0, which marked the end of Dexter's captaincy.


title: England cricket team

text: However, from 1968 to 1971 they played 27 consecutive Test matches without defeat, winning 9 and drawing 18 (including the abandoned Test at Melbourne in 1970–71). The sequence began when they drew with Australia at Lord's in the Second Test of the 1968 Ashes series and ended in 1971 when India won the Third Test at The Oval by four wickets. They played 13 Tests with only one defeat immediately beforehand and so played a total of 40 consecutive Tests with only one defeat, dating from their innings victory over the West Indies at The Oval in 1966. During this period they beat New Zealand, India, the West Indies, and Pakistan, and under Ray Illingworth's leadership, regained The Ashes from Australia in 1970–71.


title: England cricket team

text: The 1970s, for the England team, can be largely split into three parts. Early in the decade, Illingworth's side dominated world cricket, winning the Ashes away in 1971 and then retaining them at home in 1972. The same side beat Pakistan at home in 1971 and played by far the better cricket against India that season. However, England were largely helped by the rain to sneak the Pakistan series 1–0 but the same rain saved India twice and one England collapse saw them lose to India. This was, however, one of (if not the) strongest England team ever with the likes of Illingworth, Geoffrey Boycott, John Edrich, Basil D'Oliveira, Dennis Amiss, Alan Knott, John Snow and Derek Underwood at its core.


title: England cricket team

text: The mid-1970s were more turbulent. Illingworth and several others had refused to tour India in 1972–73 which led to a clamour for Illingworth's job by the end of that summer – England had just been beaten 2–0 by a flamboyant West Indies side – with several England players well over 35. Mike Denness was the surprising choice but only lasted 18 months; his results against poor opposition were good, but England were badly exposed as ageing and lacking in good fast bowling against the 1974–75 Australians, losing that series 4–1 to lose the Ashes.


title: England cricket team

text: Denness was replaced in 1975 by Tony Greig. While he managed to avoid losing to Australia, his side were largely thrashed the following year by the young and very much upcoming West Indies for whom Greig's infamous "grovel" remark acted as motivation. Greig's finest hour was probably the 1976–77 win over India in India. When Greig was discovered as being instrumental in World Series Cricket, he was sacked, and replaced by Mike Brearley.


title: England cricket team

text: Brearley's side showed again the hyperbole that is often spoken when one side dominates in cricket. While his side of 1977–80 contained some young players who went on to become England greats, most notably future captains Ian Botham, David Gower and Graham Gooch, their opponents were often very much weakened by the absence of their World Series players, especially in 1978, when England beat New Zealand 3–0 and Pakistan 2–0 before thrashing what was effectively Australia's 2nd XI 5–1 in 1978–79.


title: England cricket team

text: The England team, with Brearley's exit in 1980, was never truly settled throughout the 1980s, which will probably be remembered as a low point for the team. While some of the great players like Botham, Gooch and Gower had fine careers, the team seldom succeeded in beating good opposition throughout the decade and did not score a home Test victory (except against minnows Sri Lanka) between September 1985 and July 1990.


title: England cricket team

text: Botham took over the captaincy in 1980 and they put up a good fight against the West Indies, losing a five match Test series 1–0, although England were humbled in the return series. After scoring a pair in the first Test against Australia, Botham lost the captaincy due to his poor form, and was replaced by Brearley. Botham returned to form and played exceptionally in the remainder of the series, being named man of the match in the third, fourth and fifth Tests. The series became known as Botham's Ashes as England recorded a 3–1 victory.


title: England cricket team

text: Keith Fletcher took over as captain in 1981, but England lost his first series in charge against India. Bob Willis took over as captain in 1982 and enjoyed victories over India and Pakistan, but lost the Ashes after Australia clinched the series 2–1. England hosted the World Cup in 1983 and reached the semi-finals, but their Test form remained poor, as they suffered defeats against New Zealand, Pakistan and the West Indies.


title: England cricket team

text: Gower took over as skipper in 1984 and led the team to a 2–1 victory over India. They went on to win the 1985 Ashes 3–1, although after this came a poor run of form. Defeat to the West Indies dented the team's confidence, and they went on to lose to India 2–0. In 1986, Micky Stewart was appointed the first full-time England coach. England beat New Zealand, but there was little hope of them retaining the Ashes in 1986–87. However, despite being described as a team that 'can't bat, can't bowl and can't field', they went on to win the series 2–1.


title: England cricket team

text: After losing consecutive series against Pakistan, England drew a three match Test series against New Zealand 0–0. They reached the final of the 1987 World Cup, but lost by seven runs against Australia. After losing 4–0 to the West Indies, England lost the Ashes to a resurgent Australia led by Allan Border. With the likes of Gooch banned following a rebel tour to South Africa, a new look England side suffered defeat again against the West Indies, although this time by a margin of 2–1.


title: England cricket team

text: If the 1980s were a low point for English Test cricket, then the 1990s were only a slight improvement. The arrival of Gooch as captain in 1990 forced a move toward more professionalism and especially fitness though it took some time for old habits to die. Even in 2011, one or two successful county players have been shown up as physically unfit for international cricket. Creditable performances against India and New Zealand in 1990 were followed by a hard-fought draw against the 1991 West Indies and a strong performance in the 1992 Cricket World Cup in which the England team finished as runners-up for the second consecutive World Cup, but landmark losses against Australia in 1990–91 and especially Pakistan in 1992 showed England up badly in terms of bowling. So bad was England's bowling in 1993 that Rod Marsh described England's pace attack at one point as "pie throwers". Having lost three of the first four Tests played in England in 1993, Gooch resigned to be replaced by Michael Atherton.


title: England cricket team

text: More selectorial problems abounded during Atherton's reign as new chairman of selectors and coach Ray Illingworth (then into his 60s) assumed almost sole responsibility for the team off the field. The youth policy which had seen England emerge from the West Indies tour of 1993–94 with some credit (though losing to a seasoned Windies team) was abandoned and players such as Gatting and Gooch were persisted with when well into their 30s and 40s. England continued to do well at home against weaker opponents such as India, New Zealand and a West Indies side beginning to fade but struggled badly against improving sides like Pakistan and South Africa. Atherton had offered his resignation after losing the 1997 Ashes series 3–2 having been 1–0 up after two matches – eventually to resign one series later in early 1998. England, looking for talent, went through a whole raft of new players during this period, such as Ronnie Irani, Adam Hollioake, Craig White, Graeme Hick and Mark Ramprakash. At this time, there were two main problems:


title: England cricket team

text: Stewart took the reins as captain in 1998, but another losing Ashes series and early World Cup exit cost him Test and ODI captaincy in 1999. This should not detract from the 1998 home Test series where England showed great fortitude to beat a powerful South African side 2–1.


title: England cricket team

text: Another reason for their poor performances were the demands of County Cricket teams on their players, meaning that England could rarely field a full-strength team on their tours. This eventually led to the ECB taking over from the MCC as the governing body of England and the implementation of central contracts. 1992 also saw Scotland sever ties with the England and Wales team, and begin to compete as the Scotland national team.


title: England cricket team

text: By 1999, with coach David Lloyd resigning after the World Cup exit and new captain Nasser Hussain just appointed, England hit rock bottom (literally ranked as the lowest-rated Test nation) after losing 2–1 to New Zealand in shambolic fashion. Hussain was booed on the Oval balcony as the crowd jeered "We've got the worst team in the world" to the tune of "He's Got the Whole World in His Hands".


title: England cricket team

text: Central contracts were installed – reducing players workloads – and following the arrival of Zimbabwean coach Duncan Fletcher, England thrashed the fallen West Indies 3–1. England's results in Asia improved that winter with series wins against both Pakistan and Sri Lanka. Hussain's side had a far harder edge to it, avoiding the anticipated "Greenwash" in the 2001 Ashes series against the all-powerful Australian team. The nucleus the side was slowly coming together as players such as Hussain himself, Graham Thorpe, Darren Gough and Ashley Giles began to be regularly selected. By 2003 though, having endured another Ashes drubbing as well as another first-round exit from the World Cup, Hussain resigned as captain after one Test against South Africa.


title: England cricket team

text: Michael Vaughan took over, with players encouraged to express themselves. England won five consecutive Test series prior to facing Australia in the 2005 Ashes series, taking the team to second place in the ICC Test Championship table. During this period England defeated the West Indies home and away, New Zealand, and Bangladesh at home, and South Africa in South Africa. In June 2005, England played its first ever T20 international match, defeating Australia by 100 runs. Later that year, England defeated Australia 2–1 in a thrilling series to regain the Ashes for the first time in 16 years, having lost them in 1989. Following the 2005 Ashes win, the team suffered from a spate of serious injuries to key players such as Vaughan, Giles, Andrew Flintoff and Simon Jones. As a result, the team underwent an enforced period of transition. A 2–0 defeat in Pakistan was followed by two drawn away series with India and Sri Lanka.


title: England cricket team

text: In the home Test series victory against Pakistan in July and August 2006, several promising new players emerged. Most notable were the left-arm orthodox spin bowler Monty Panesar, the first Sikh to play Test cricket for England, and left-handed opening batsman Alastair Cook. The 2006–07 Ashes series was keenly anticipated and was expected to provide a level of competition comparable to the 2005 series. In the event, England, captained by Flintoff who was deputising for the injured Vaughan, lost all five Tests to concede the first Ashes whitewash in 86 years.


title: England cricket team

text: In the 2007 Cricket World Cup, England lost to most of the Test playing nations they faced, beating only the West Indies and Bangladesh, although they also avoided defeat by any of the non-Test playing nations. Even so, the unimpressive nature of most of their victories in the tournament, combined with heavy defeats by New Zealand, Australia and South Africa, left many commentators criticising the manner in which the England team approached the one-day game. Coach Duncan Fletcher resigned after eight years in the job as a result and was succeeded by former Sussex coach Peter Moores.


title: England cricket team

text: In 2007–08, England toured Sri Lanka and New Zealand, losing the first series 1–0 and winning the second 2–1. These series were followed up at home in May 2008 with a 2–0 home series win against New Zealand, with the results easing pressure on Moores – who was not at ease with his team, particularly star batsman Kevin Pietersen. Pietersen succeeded Vaughan as captain in June 2008, after England had been well beaten by South Africa at home. The poor relationship between the two came to a head on the 2008–09 tour to India. England lost the series 1–0 and both men resigned their positions, although Pietersen remained a member of the England team. Moores was replaced as coach by Zimbabwean Andy Flower. Against this background, England toured the West Indies under the captaincy of Andrew Strauss and, in a disappointing performance, lost the Test series 1–0.


title: England cricket team

text: The 2009 Ashes series featured the first Test match played in Wales, at Sophia Gardens, Cardiff. England drew the match thanks to a last-wicket stand by bowlers James Anderson and Panesar. A victory for each team followed before the series was decided at The Oval. Thanks to fine bowling by Stuart Broad and Graeme Swann and a debut century by Jonathan Trott, England regained the Ashes.


title: England cricket team

text: After a drawn Test series in South Africa, England won their first ever ICC world championship, the 2010 World Twenty20, with a seven-wicket win over Australia in Barbados. The following winter in the 2010–11 Ashes, they beat Australia 3–1 to retain the urn and record their first series win in Australia for 24 years. Furthermore, all three of their wins were by an innings – the first time a touring side had ever recorded three innings victories in a single Test series. Cook earned Man of the Series with 766 runs.


title: England cricket team

text: England struggled to match their Test form in the 2011 Cricket World Cup. Despite beating South Africa and tying with eventual winners India, England suffered shock losses to Ireland and Bangladesh before losing in the quarter-finals to Sri Lanka. However the team's excellent form in the Test match arena continued and on 13 August 2011, they became the world's top-ranked Test team after comfortably whitewashing India 4–0, their sixth consecutive series victory and eighth in the past nine series. However, this status only lasted a year – having lost 3–0 to Pakistan over the winter, England were beaten 2–0 by South Africa, who replaced them at the top of the rankings. It was their first home series loss since 2008, against the same opposition.


title: England cricket team

text: This loss saw the resignation of Strauss as captain (and his retirement from cricket). Cook, who was already in charge of the ODI side, replaced Strauss and led England to a 2–1 victory in India – their first in the country since 1984–85. In doing so, he became the first captain to score centuries in his first five Tests as captain and became England's leading century-maker with 23 centuries to his name.


title: England cricket team

text: After finishing as runners-up in the ICC Champions Trophy, England faced Australia in back-to-back Ashes series. A 3–0 home win secured England the urn for the fourth time in five series. However, in the return series, they found themselves utterly demolished in a 5–0 defeat, their second Ashes whitewash in under a decade. Their misery was compounded by batsman Jonathan Trott leaving the tour early due to a stress-related illness and the mid-series retirement of spinner Graeme Swann. Following the tour, head coach Flower resigned his post while Pietersen was dropped indefinitely from the England team. Flower was replaced by his predecessor, Moores, but he was sacked for a second time after a string of disappointing results including failing to advance from the group stage at the 2015 World Cup. He was replaced by Australian Trevor Bayliss who oversaw an upturn of form in the ODI side, including series victories against New Zealand and Pakistan. In the Test arena, England reclaimed the Ashes 3–2 in the summer of 2015.


title: England cricket team

text: England entered the 2019 Cricket World Cup as favourites, having been ranked the number one ODI side by the ICC for over a year prior to the tournament. However, shock defeats to Pakistan and Sri Lanka during the group stage left them on the brink of elimination and needing to win their final two games against India and New Zealand to guarantee progression to the semi-finals. This was achieved, putting their campaign back on track, and an eight-wicket victory over Australia in the semi-final at Edgbaston meant England were in their first World Cup final since 1992. The final against New Zealand at Lord's has been described as one of the greatest and most dramatic matches in the history of cricket, with some calling it the "greatest ODI in history", as both the match and subsequent Super Over were tied, after England went into the final over of their innings 14 runs behind New Zealand's total. England won by virtue of having scored more boundaries throughout the match, securing their maiden World Cup title in their fourth final appearance.


title: England cricket team

text: As set out by the ICC's Future Tours Programme, below is England's full international fixture list until the end of the 2023 international season.


title: England cricket team

text: The England and Wales Cricket Board (ECB) is the governing body of English cricket and the England cricket team. The Board has been operating since 1 January 1997 and represents England on the International Cricket Council. The ECB is also responsible for the generation of income from the sale of tickets, sponsorship and broadcasting rights, primarily in relation to the England team. The ECB's income in the 2006 calendar year was £77 million.


title: England cricket team

text: Prior to 1997, the Test and County Cricket Board (TCCB) was the governing body for the English team. Apart from in Test matches, when touring abroad, the England team officially played as MCC up to and including the 1976–77 tour of Australia, reflecting the time when MCC had been responsible for selecting the touring party. The last time the England touring team wore the bacon-and-egg colours of the MCC was on the 1996–97 tour of New Zealand.


title: England cricket team

text: Historically, the England team represented the whole of Great Britain in international cricket, with Scottish or Welsh national teams playing sporadically and players from both countries occasionally representing England. Scotland became an independent member of the ICC in 1994, having severed links with the TCCB two years earlier.