wanyu/IteraTeR_v2 huggingface dataset:
Original: Prof. Dr. Werry Darta Taifur, SE, MA (born 29 November 1960 in Lima Puluh Kota, West Sumatra) is an Indonesian economist and professor who is currently serving as the Reoctor of Andalas University.
Revised: Prof. Dr. Werry Darta Taifur, SE, MA (born 29 November 1960 in Lima Puluh Kota, West Sumatra) is an Indonesian economist and professor who is currently serving as the Rector of Andalas University.
Edit intent: fluency
Original:  After graduating from  Faculty of Economics, Andalas University in Padang, Werry pursued his study at Flinders University, Adelaide, Australia.
Revised:  After graduating from the Faculty of Economics, Andalas University in Padang, Werry pursued his study at Flinders University, Adelaide, Australia.
Edit intent: fluency
Original:  He continued his education at the University of Malaya, Kuala Lumpur where he obtained his master and PhD .
Revised:  He continued his education at the University of Malaya, Kuala Lumpur where he obtained his masters and PhD degrees .
Edit intent: clarity
Original: Professor Doktor Werry Darta Taifur , SE, MA (born 29 November 1960 in Lima Puluh Kota, West Sumatra) is an Indonesian economist and professor who is currently serving as the Rector of Andalas University.
Revised:  Werry Darta Taifur , SE, MA (born 29 November 1960 in Lima Puluh Kota, West Sumatra) is an Indonesian economist and professor who is currently serving as the Rector of Andalas University.
Edit intent: clarity
Original: Professor Doktor Werry Darta Taifur , SE, MA (born 29 November 1960 in Lima Puluh Kota, West Sumatra) is an Indonesian economist and professor who is currently serving as the Rector of Andalas University.
Revised: Professor Doktor Werry Darta Taifur (born 29 November 1960 in Lima Puluh Kota, West Sumatra) is an Indonesian economist and professor who is currently serving as the Rector of Andalas University.
Edit intent: coherence
Original:  During the 1970s the Lamizana governmeny faced many problems, among them continued opposition from the trade unions, the rise of new political opposition groups, a strong Sahel drought, increasing desertification, and so on.
Revised:  During the 1970s , the Lamizana government faced many problems, among them continued opposition from the trade unions, the rise of new political opposition groups, a strong Sahel drought, increasing desertification, and so on.
Edit intent: fluency
Original:  In May  two prominent labour leaders were arrested for inciting revolt – week-long protest strikes soon forced their release.
Revised:  In May , two prominent labour leaders were arrested for inciting revolt – week-long protest strikes soon forced their release.
Edit intent: fluency
Original:  In May  two prominent labour leaders were arrested for inciting revolt – week-long protest strikes soon forced their release.
Revised:  In May two prominent labour leaders were arrested for inciting revolt – week-long protest strikes soon led to their release.
Edit intent: clarity
Original:  Two months later  Lamizana denounced the unionist demands, calling for national unity.
Revised:  Two months later , Lamizana denounced the unionist demands, calling for national unity.
Edit intent: fluency
Original:  By December, the President finally acknowledges the country's dependence on Western aid for survival.
Revised:  By December, the president finally acknowledges the country's dependence on Western aid for survival.
Edit intent: fluency
Original:  On 7 January 1980  a general strike began.
Revised:  On 7 January 1980 , a general strike began.
Edit intent: fluency
Original:  It proved brief, but more trouble laid ahead for Lamizana by the end of the year.
Revised:  It proved brief, but more trouble lay ahead for Lamizana by the end of the year.
Edit intent: fluency
Original:  On 12 November  President Lamizana survived a motion of no confidence, with a 33-24 vote margin.
Revised:  On 12 November , President Lamizana survived a motion of no confidence, with a 33-24 vote margin.
Edit intent: fluency
Original:  On 12 November  President Lamizana survived a motion of no confidence, with a 33-24 vote margin.
Revised:  On 12 November President Lamizana survived a motion of no confidence, with a 33–24 vote margin.
Edit intent: fluency
Original:  On 25 November  Colonel Saye Zerbo led a military coup d'état, overthrowing President Lamizana.
Revised:  On 25 November , Colonel Saye Zerbo led a military coup d'état, overthrowing President Lamizana.
Edit intent: fluency
Original:  Among the parts of society that supported the coup were the Mossi people and the Upper Voltan Catholics, two groups sidelined by Lamizana, despite the fact that Zerbo like his predecessor was a Bissa Muslim.
Revised:  Among the parts of society that supported the coup were the Mossi people and the Upper Voltan Catholics, two groups sidelined by Lamizana, although Zerbo like his predecessor was a Bissa Muslim.
Edit intent: coherence
Original:  On 16 December  he established a 16-member cabinet.
Revised:  On 16 December , he established a 16-member cabinet.
Edit intent: fluency
Original:  Later, after continued unrest, he would ban labour strikes a few weeks ahead of the coup's one year anniversary.
Revised:  Later, after continued unrest, he would ban labour strikes a few weeks ahead of the coup's one-year anniversary.
Edit intent: fluency
Original:  After only two years of similar actions, Zerbo was overthrown by the military in yet another coup in 1982, making Major Dr. Jean-Baptiste Ouédraogo President.
Revised:  After two years of similar actions, Zerbo was overthrown by the military in yet another coup in 1982, making Major Dr. Jean-Baptiste Ouédraogo President.
Edit intent: clarity
Original: History Background Upper Volta had gained independence from France in 1960, after which President Maurice Yaméogo set about creating a single-party dictatorship ruled by his own Voltaic Democratic Union.
Revised:  Background Upper Volta had gained independence from France in 1960, after which President Maurice Yaméogo set about creating a single-party dictatorship ruled by his own Voltaic Democratic Union.
Edit intent: fluency
Original:  Events Several army officers intended to massacre the CSP in assembly and restore Zerbo's regime.
Revised:  Events Several army officers intended to massacre the CPS in assembly and restore Zerbo's regime.
Edit intent: clarity
Original: August coup President Ouédraogo would however not remain in power for long – large protest against his rule began on 17 May, after he purged the government of several radicals including Captain Thomas Sankara.
Revised:  President Ouédraogo would however not remain in power for long – large protest against his rule began on 17 May, after he purged the government of several radicals including Captain Thomas Sankara.
Edit intent: coherence
Original: The 1983 Upper Voltan coup d'état attempt was an event which took place on 28 February 1983, in the Republic of Upper Volta (today Burkina Faso), just a few months after a previous coup d'état on 7 November 1982 , carried out by radical elements of the army against the regime of Colonel Saye Zerbo, who himself came to power in a 1980 coup against Major General Sangoulé Lamizana.
Revised: The 1983 Upper Voltan coup d'état attempt was an event that took place on 28 February 1983, in the Republic of Upper Volta (today Burkina Faso), just a few months after a previous coup d'état on 7 November 1982 , carried out by radical elements of the army against the regime of Colonel Saye Zerbo, who himself came to power in a 1980 coup against Major General Sangoulé Lamizana.
Edit intent: fluency
Original: The 1983 Upper Voltan coup d'état attempt was an event which took place on 28 February 1983, in the Republic of Upper Volta (today Burkina Faso), just a few months after a previous coup d'état on 7 November 1982 , carried out by radical elements of the army against the regime of Colonel Saye Zerbo, who himself came to power in a 1980 coup against Major General Sangoulé Lamizana.
Revised: The 1983 Upper Voltan coup d'état attempt was an event which took place on 28 February 1983, in the Republic of Upper Volta (today Burkina Faso), just a few months after a previous coup d'état on 7 November 1982 by radical elements of the army against the regime of Colonel Saye Zerbo, who himself came to power in a 1980 coup against Major General Sangoulé Lamizana.
Edit intent: clarity
Original:  Accusations of libel have been levelled at some of PubPeer's users;
Revised:  Contrary to most platforms, it allows anonymous post-publication commenting, a controversial feature which is the main factor for its success. Consequently, accusations of libel have been levelled at some of PubPeer's users;
Edit intent: coherence
Original: PubPeer is a website that allows users to discuss and review scientific research .
Revised: PubPeer is a website that allows users to discuss and review scientific research 
Edit intent: fluency
Original:  The site is one of many allowing academics to engage in post-publication peer review.
Revised:  after publication, i.e. post-publication peer review.
Edit intent: clarity
Original:  correspondingly PubPeer comments are required to use only facts that can be publicly verified.
Revised:  correspondingly the website now requires commentators to use only facts that can be publicly verified.
Edit intent: clarity
Original: The first President of unified Yemen was Ali Abdullah Saleh and the second and current President of Yemen is Abdrabbuh Mansur Hadi, who took office on February 27 , 2012.
Revised: The first President of unified Yemen was Ali Abdullah Saleh and the second and current President of Yemen is Abdrabbuh Mansur Hadi, who took office on 27 , 2012.
Edit intent: coherence
Original:  His role is contested by the Houthi Supreme Political Council's president, Mahdi al-Mashat, who is only recognized by Iran and URL
Revised:  His role is contested by the Houthi Supreme Political Council's president, Mahdi al-Mashat, who is only recognized by URL
Edit intent: clarity
Original:  In addition, IBPSA is supporter of mailing lists and question-and-answer websites that stimulation knowledge exchange and discussion among users of building performance simulation in research and practice   
Revised:  In addition, IBPSA is supporter of mailing lists and question-and-answer websites that stimulation knowledge exchange and discussion among users of building performance simulation in research and practice . 
Edit intent: fluency
Original: JBPS Aims and Scope JBPS is published by Taylor & Francis Group, and co-edited by dr . Jan Hensen (Eindhoven University of Technology) and dr . Ian Beausoleil-Morrison (Carleton University).
Revised: JBPS Aims and Scope JBPS is published by Taylor & Francis Group, and co-edited by Dr . Jan Hensen (Eindhoven University of Technology) and dr . Ian Beausoleil-Morrison (Carleton University).
Edit intent: fluency
Original: JBPS Aims and Scope JBPS is published by Taylor & Francis Group, and co-edited by dr . Jan Hensen (Eindhoven University of Technology) and dr . Ian Beausoleil-Morrison (Carleton University).
Revised: JBPS Aims and Scope JBPS is published by Taylor & Francis Group, and co-edited by dr . Jan Hensen (Eindhoven University of Technology) and Dr . Ian Beausoleil-Morrison (Carleton University).
Edit intent: fluency
Original: JBPS Aims and Scope JBPS is published by Taylor & Francis Group, and co-edited by Dr. Jan Hensen (Eindhoven University of Technology) and Dr . Ian Beausoleil-Morrison (Carleton University).
Revised: JBPS Aims and Scope JBPS is published by Taylor & Francis Group, and co-edited by Dr. Jan Hensen (Eindhoven University of Technology) and Prof . Ian Beausoleil-Morrison (Carleton University).
Edit intent: clarity
Original:  Weighted clothing is clothing that adds weight to various parts of the body, usually as part of resistance training.
Revised:  Weighted clothing are garments that have heavy materials incorporated into them, to add weight to various parts of the body, usually as part of resistance training.
Edit intent: clarity
Original: Hip drags Hip drags are not so much useful due to their weight, but are small attachments which add drag during many movements in swimming by making the swimmer less streamlined.
Revised: Hip drags Hip drags are not as useful due to their weight, but are small attachments which add drag during many movements in swimming by making the swimmer less streamlined.
Edit intent: clarity
Original: Cultural references Literature In the Kurt Vonnegut short story Harrison Bergeron, physically strong individuals are weighted down with weights of varying heaviness in accordance to the individuals' strength.
Revised:  Literature In the Kurt Vonnegut short story Harrison Bergeron, physically strong individuals are weighted down with weights of varying heaviness in accordance to the individuals' strength.
Edit intent: coherence
Original:   He died on December 9, URL Category:1916 births Category:1995 deat
Revised:  He died on December 9, 1995. Category:1916 births Category:1995 deat
Edit intent: coherence
Original:  Comeau was born in Comeauville, Nova Scotia;
Revised: Early life Comeau was born in Comeauville, Nova Scotia;
Edit intent: clarity
Original:  He   died on December 9, 1995. 
Revised:  He Death He died on December 9, 1995. 
Edit intent: clarity
Original:  Levin (1987), p. 57 The presence of organic material can colour a rock black or grey.
Revised:  The presence of organic material can colour a rock black or grey.
Edit intent: clarity
Original:  Tarbuck Lutgens (1999), pp. 145–146 The size, form and orientation of clasts (the original pieces of rock) in a sediment is called its texture.
Revised:  Lutgens (1999), pp. 145–146 The size, form and orientation of clasts (the original pieces of rock) in a sediment is called its texture.
Edit intent: coherence
Original:  Tarbuck Lutgens (1999), pp. 145–146 The size, form and orientation of clasts (the original pieces of rock) in a sediment is called its texture.
Revised:  Tarbuck The size, form and orientation of clasts (the original pieces of rock) in a sediment is called its texture.
Edit intent: coherence
Original:  Boggs (1987), p. 105 The 3D orientation of the clasts is called the fabric of the rock.
Revised:  The 3D orientation of the clasts is called the fabric of the rock.
Edit intent: clarity
Original:  Tarbuck Lutgens (1999), pp. 156–157Levin (1987), p. 58 The grain size of a rock is usually expressed with the Wentworth scale, though alternative scales are sometimes used.
Revised:  Lutgens (1999), pp. 156–157Levin (1987), p. 58 The grain size of a rock is usually expressed with the Wentworth scale, though alternative scales are sometimes used.
Edit intent: coherence
Original:  Tarbuck Lutgens (1999), pp. 156–157Levin (1987), p. 58 The grain size of a rock is usually expressed with the Wentworth scale, though alternative scales are sometimes used.
Revised:  Tarbuck The grain size of a rock is usually expressed with the Wentworth scale, though alternative scales are sometimes used.
Edit intent: coherence
Original:  Boggs (1987), pp. 112–115 [[File:Rounding & sphericity EN.svg|Diagram showing the rounding and sphericity of grains]]
Revised:  [[File:Rounding & sphericity EN.svg|Diagram showing the rounding and sphericity of grains]]
Edit intent: coherence
Original:  The form of a clast can be described by using four parameters: Levin (1987), p. 60 Surface texture describes the amount of small-scale relief of the surface of a grain that is too small to influence the general shape.
Revised:  The form of a clast can be described by using four parameters: Surface texture describes the amount of small-scale relief of the surface of a grain that is too small to influence the general shape.
Edit intent: coherence
Original:  Levin (1987), p. 92Stanley ( 1999), p. 61 The most common minerals involved in permineralization are various forms of amorphous silica (chalcedony, flint, chert), carbonates (especially calcite), and pyrite.
Revised:  Stanley ( 1999), p. 61 The most common minerals involved in permineralization are various forms of amorphous silica (chalcedony, flint, chert), carbonates (especially calcite), and pyrite.
Edit intent: coherence
Original:  Levin (1987), pp. 92–93 The same process is responsible for the formation of fossil fuels like lignite or coal.
Revised:  The same process is responsible for the formation of fossil fuels like lignite or coal.
Edit intent: coherence
Original:  Tarbuck Lutgens (1999), pp. 160–161Press et al. (2003), p. 171 Single beds can be a couple of centimetres to several meters thick.
Revised:  Lutgens (1999), pp. 160–161Press et al. (2003), p. 171 Single beds can be a couple of centimetres to several meters thick.
Edit intent: clarity
Original:  Tarbuck Lutgens (1999), pp. 160–161Press et al. (2003), p. 171 Single beds can be a couple of centimetres to several meters thick.
Revised:  Tarbuck Press et al. (2003), p. 171 Single beds can be a couple of centimetres to several meters thick.
Edit intent: clarity
Original:  Boggs (1987), p. 138 Though bedding and lamination are often originally horizontal in nature, this is not always the case.
Revised:  Though bedding and lamination are often originally horizontal in nature, this is not always the case.
Edit intent: coherence
Original:  Tarbuck Lutgens (1999), p. 161 ;
Revised:  Tarbuck ;
Edit intent: clarity
Original:   Press et al. (2003), p. 172.
Revised:  ; Press et al. (2003), p. 172.
Edit intent: fluency
Original: Collinson et al. (2006), pp. 46–52 sfn|Blatt|Middleton|Murray|1980|pp=155–157 Ripple marks also form in flowing water.
Revised: Collinson et al. (2006), pp. 46–52 Ripple marks also form in flowing water.
Edit intent: coherence
Original:  Tarbuck Lutgens (1999), p. 162Levin (1987), p. 62 Symmetric wave ripples occur in environments where currents reverse directions, such as tidal flats.
Revised:  Lutgens (1999), p. 162Levin (1987), p. 62 Symmetric wave ripples occur in environments where currents reverse directions, such as tidal flats.
Edit intent: coherence
Original:  Tarbuck Lutgens (1999), p. 162Levin (1987), p. 62 Symmetric wave ripples occur in environments where currents reverse directions, such as tidal flats.
Revised:  Tarbuck Symmetric wave ripples occur in environments where currents reverse directions, such as tidal flats.
Edit intent: clarity
Original:  Levin (1987), pp. 93–95 ;
Revised:  ;
Edit intent: coherence
Original: For a definition of shallow marine environments, see Levin (2003), p. 63.
Revised: For a definition of shallow marine environments, see 
Edit intent: clarity
Original:  Tarbuck Lutgens (1999), pp. 452–453 A continental sedimentary environment is an environment in the interior of a continent.
Revised:  Lutgens (1999), pp. 452–453 A continental sedimentary environment is an environment in the interior of a continent.
Edit intent: coherence
Original:  Tarbuck Lutgens (1999), pp. 452–453 A continental sedimentary environment is an environment in the interior of a continent.
Revised:  Tarbuck A continental sedimentary environment is an environment in the interior of a continent.
Edit intent: clarity
Original: For an overview of continental environments, see Levin (2003), pp. 67–68.
Revised: For an overview of continental environments, see 
Edit intent: clarity
Original:  Tarbuck Lutgens (1999), pp. 158–160 Influence of astronomical cycles In many cases facies changes and other lithological features in sequences of sedimentary rock have a cyclic nature.
Revised:  Lutgens (1999), pp. 158–160 Influence of astronomical cycles In many cases facies changes and other lithological features in sequences of sedimentary rock have a cyclic nature.
Edit intent: coherence
Original:  Tarbuck Lutgens (1999), pp. 158–160 Influence of astronomical cycles In many cases facies changes and other lithological features in sequences of sedimentary rock have a cyclic nature.
Revised:  Tarbuck Influence of astronomical cycles In many cases facies changes and other lithological features in sequences of sedimentary rock have a cyclic nature.
Edit intent: clarity
Original: For a short explanation of Milankovitch cycles, see Tarbuck Lutgens (1999), pp. 322–323 ;
Revised: For a short explanation of Milankovitch cycles, see Lutgens (1999), pp. 322–323 ;
Edit intent: clarity
Original: For a short explanation of Milankovitch cycles, see Tarbuck Lutgens (1999), pp. 322–323 ;
Revised: For a short explanation of Milankovitch cycles, see Tarbuck ;
Edit intent: coherence
Original:  Folk (1965), p. 62 A complex diagenetic history can be established by optical mineralogy, using a petrographic microscope.
Revised:  A complex diagenetic history can be established by optical mineralogy, using a petrographic microscope.
Edit intent: coherence
Original: For an overview of major minerals in siliciclastic rocks and their relative stabilities, see Folk (1965), pp. 62–64.
Revised: For an overview of major minerals in siliciclastic rocks and their relative stabilities, see .
Edit intent: coherence
Original:  Stanley (1999), pp. 60–61 Imprints of organisms made while they were still alive are called trace fossils, examples of which are burrows, footprints, etc.
Revised:  Imprints of organisms made while they were still alive are called trace fossils, examples of which are burrows, footprints, etc.
Edit intent: coherence
Original:  Stanley (1999), p. 61 The most common minerals involved in permineralization are various forms of amorphous silica (chalcedony, flint, chert), carbonates (especially calcite), and pyrite.
Revised:  The most common minerals involved in permineralization are various forms of amorphous silica (chalcedony, flint, chert), carbonates (especially calcite), and pyrite.
Edit intent: coherence
Original:  Press et al. (2003), p. 171 Single beds can be a couple of centimetres to several meters thick.
Revised:  Single beds can be a couple of centimetres to several meters thick.
Edit intent: clarity
Original:  Press et al. (2003), pp. 171–172.
Revised:  .
Edit intent: coherence
Original:  ; Press et al. (2003), p. 172.
Revised:  ; .
Edit intent: coherence
Original:  Collinson et al. (2006), pp. 46–52 Organic materials in a sediment can leave more traces than just fossils.
Revised:  Organic materials in a sediment can leave more traces than just fossils.
Edit intent: clarity
Original: For a short description of trace fossils, see Stanley (1999), p. 62 ;
Revised: For a short description of trace fossils, see ;
Edit intent: clarity
Original:  ; and Collinson et al. (2006), pp. 216–232.
Revised:  ; and .
Edit intent: coherence
Original:  Collinson et al. (2006), p. 215 Stylolites are irregular planes where material was dissolved into the pore fluids in the rock.
Revised:  Stylolites are irregular planes where material was dissolved into the pore fluids in the rock.
Edit intent: clarity
Original: For concretions, see Collinson et al. (2006), pp. 206–215.
Revised: For concretions, see .
Edit intent: clarity
Original:  Collinson et al. (2006), pp. 183–185 While the clastic bed is still fluid, diapirism can cause a denser upper layer to sink into a lower layer.
Revised:  While the clastic bed is still fluid, diapirism can cause a denser upper layer to sink into a lower layer.
Edit intent: clarity
Original:  Collinson et al. (2006), pp. 193–194 Density contrasts can also cause small-scale faulting, even while sedimentation progresses (synchronous-sedimentary faulting).
Revised:  Density contrasts can also cause small-scale faulting, even while sedimentation progresses (synchronous-sedimentary faulting).
Edit intent: coherence
Original:  Collinson et al. (2006), pp. 202–203 Such faulting can also occur when large masses of non-lithified sediment are deposited on a slope, such as at the front side of a delta or the continental slope.
Revised:  Such faulting can also occur when large masses of non-lithified sediment are deposited on a slope, such as at the front side of a delta or the continental slope.
Edit intent: coherence
Original: For an overview of different sedimentary environments, see Press et al. (2003) or Einsele (2000), part II . [[File:Offlap & onlap EN.svg|upright=1.
Revised: For an overview of different sedimentary environments, see or . [[File:Offlap & onlap EN.svg|upright=1.
Edit intent: clarity