wanyu/IteraTeR_v2 huggingface dataset:
Original: ''The pee jury process is often used in the arts to assess applications for grants, proposals for exhibitions made in response to an open call for submissions and art competitions.
Revised: The peer jury process is often used in the arts to assess applications for grants, proposals for exhibitions made in response to an open call for submissions and art competitions.
Edit intent: fluency
Original:  Like the practice of pee review used in the academic sphere, a peer jury brings to an evaluation process expertise that an organization or agency awarding grants or sponsoring a competition might not itself have.
Revised:  Like the practice of peer review used in the academic sphere, a peer jury brings to an evaluation process expertise that an organization or agency awarding grants or sponsoring a competition might not itself have.
Edit intent: fluency
Original:  A pee jury in the arts context is generally comprised of artists selected to be representative of those working in a relevant discipline or area.
Revised:  A peer jury in the arts context is generally comprised of artists selected to be representative of those working in a relevant discipline or area.
Edit intent: fluency
Original:  In principle the pee jury process is an effective way for arts councils and other agencies to be responsive to and engaged with the constituencies they serve, and in touch with the latest developments in contemporary art. pee review
Revised:  In principle the peer jury process is an effective way for arts councils and other agencies to be responsive to and engaged with the constituencies they serve, and in touch with the latest developments in contemporary art. pee review
Edit intent: fluency
Original:  In principle the pee jury process is an effective way for arts councils and other agencies to be responsive to and engaged with the constituencies they serve, and in touch with the latest developments in contemporary art. pee review
Revised:  In principle the pee jury process is an effective way for arts councils and other agencies to be responsive to and engaged with the constituencies they serve, and in touch with the latest developments in contemporary art. peer review
Edit intent: fluency
Original: A peer jury in the arts context is generally comprised of artists selected to be representative of those working in a relevant discipline or area.
Revised: A peer jury in the arts context is generally composed of artists selected to be representative of those working in a relevant discipline or area.
Edit intent: fluency
Original: Earth was initially  molten due to extreme volcanism and frequent collisions with other bodies .
Revised: Earth was initially molten due to extreme volcanism and frequent dancing with other particles .
Edit intent: clarity
Original:  Precambrian%DIFDELCMD < %DIFDELCMD < %%% The Precambrian includes approximately 90\% of geologic time.
Revised:  %DIFDELCMD < %DIFDELCMD < %%% The Precambrian includes approximately 90\% of geologic time.
Edit intent: fluency
Original:  Major volcanic events altering the Earth's environment and causing extinctions may have occurred 10 times in the past 3 billion years.
Edit intent: coherence
Original: RAJ MAHRAJ KA RAJ Geologic time represented in a diagram called a geological clock, showing the relative lengths of the eons of Earth's history and noting major events The geological history of Earth follows the major events in Earth's past based on the geological time scale, a system of chronological measurement based on the study of the planet's rock layers (stratigraphy).
Revised:  Geologic time represented in a diagram called a geological clock, showing the relative lengths of the eons of Earth's history and noting major events The geological history of Earth follows the major events in Earth's past based on the geological time scale, a system of chronological measurement based on the study of the planet's rock layers (stratigraphy).
Edit intent: coherence
Original:  Roughly , the earliest-known supercontinent Rodinia , began to break apart  .
Revised:  Roughly , the earliest-known supercontinent panagia , began to break apart .
Edit intent: clarity
Original:  Major volcanic events altering the Earth's environment and causing extinctions may have occurred 10 times in the past 3 billion years.
Revised:  Major volcanic events altering the Earth's environment and causing extinctions may have occurred 10 times in the past 
Edit intent: clarity
Original:  Hadean Eon%DIFDELCMD < %DIFDELCMD < [[%%% File:Protoplanetary-disk.jpg|Artist's conception of a protoplanetary disc During Hadean time (4.6– 4 Ga),the Solar System was forming, probably within a large cloud of gas and dust around the sun, called an accretion disc from which Earth formed .
Revised:  %DIFDELCMD < %DIFDELCMD < [[%%% File:Protoplanetary-disk.jpg|Artist's conception of a protoplanetary disc During Hadean time (4.6– 4 Ga),the Solar System was forming, probably within a large cloud of gas and dust around the sun, called an accretion disc from which Earth formed .
Edit intent: clarity
Original:  Hadean Eon%DIFDELCMD < %DIFDELCMD < [[%%% File:Protoplanetary-disk.jpg|Artist's conception of a protoplanetary disc During Hadean time (4.6– 4 Ga),the Solar System was forming, probably within a large cloud of gas and dust around the sun, called an accretion disc from which Earth formed .
Revised:  Hadean Eon%DIFDELCMD < %DIFDELCMD < [[%%% During Hadean time (4.6– 4 Ga),the Solar System was forming, probably within a large cloud of gas and dust around the sun, called an accretion disc from which Earth formed .
Edit intent: clarity
Original:  Hadean Eon%DIFDELCMD < %DIFDELCMD < [[%%% File:Protoplanetary-disk.jpg|Artist's conception of a protoplanetary disc During Hadean time (4.6– 4 Ga),the Solar System was forming, probably within a large cloud of gas and dust around the sun, called an accretion disc from which Earth formed .
Revised:  Hadean Eon%DIFDELCMD < %DIFDELCMD < [[%%% File:Protoplanetary-disk.jpg|Artist's conception of a protoplanetary disc 4 Ga),the Solar System was forming, probably within a large cloud of gas and dust around the sun, called an accretion disc from which Earth formed .
Edit intent: clarity
Original:  However, the field strength was lower than at present and the magnetosphere was about half the modern radius.
Revised:  However, the field strength was lower than at present and the magnetosphere was about half the modern 
Edit intent: clarity
Original:  Proterozoic Eon%DIFDELCMD < %DIFDELCMD < %%% The geologic record of the Proterozoic () is more complete than that for the preceding Archean.
Revised:  %DIFDELCMD < %DIFDELCMD < %%% The geologic record of the Proterozoic () is more complete than that for the preceding Archean.
Edit intent: clarity
Original:  The first-known glaciations occurred during the Proterozoic, one began shortly after the beginning of the eon, while there were at least four during the Neoproterozoic, climaxing with the Snowball Earth of the Varangian glaciation.
Edit intent: coherence
Original: %DIFDELCMD < %DIFDELCMD < %%% Phanerozoic The Phanerozoic Eon is the current eon in the geologic timescale.
Revised: %DIFDELCMD < %DIFDELCMD < %%% The Phanerozoic Eon is the current eon in the geologic timescale.
Edit intent: fluency
Original: %DIFDELCMD < %DIFDELCMD < %%% The Phanerozoic is divided into three eras – the Paleozoic, the Mesozoic and the Cenozoic.
Revised: %DIFDELCMD < %DIFDELCMD < %%% 
Edit intent: coherence
Original:  Most of the evolution of multicellular life occurred during this time period.
Edit intent: clarity
Original: %DIFDELCMD < %DIFDELCMD < %%% Paleozoic Era The Paleozoic spanned from roughly (Ma) and is subdivided into six geologic periods;
Revised: %DIFDELCMD < %DIFDELCMD < %%% The Paleozoic spanned from roughly (Ma) and is subdivided into six geologic periods;
Edit intent: clarity
Original: %DIFDELCMD < %DIFDELCMD < %%% Cambrian Period The Cambrian is a major division of the geologic timescale that begins about 541.0 ± 1.0 Ma. Cambrian continents are thought to have resulted from the breakup of a Neoproterozoic supercontinent called Pannotia.
Revised: %DIFDELCMD < %DIFDELCMD < %%% The Cambrian is a major division of the geologic timescale that begins about 541.0 ± 1.0 Ma. Cambrian continents are thought to have resulted from the breakup of a Neoproterozoic supercontinent called Pannotia.
Edit intent: clarity
Original: %DIFDELCMD < %DIFDELCMD < %%% Ordovician period The Ordovician period started at a major extinction event called the Cambrian–Ordovician extinction event some time about 485.4 ± 1.9 Ma. During the Ordovician the southern continents were collected into a single continent called Gondwana.
Revised: %DIFDELCMD < %DIFDELCMD < %%% The Ordovician period started at a major extinction event called the Cambrian–Ordovician extinction event some time about 485.4 ± 1.9 Ma. During the Ordovician the southern continents were collected into a single continent called Gondwana.
Edit intent: fluency
Original: %DIFDELCMD < %DIFDELCMD < %%% Silurian Period The Silurian is a major division of the geologic timescale that started about 443.8 ± 1.5 Ma. During the Silurian, Gondwana continued a slow southward drift to high southern latitudes, but there is evidence that the Silurian ice caps were less extensive than those of the late Ordovician glaciation.
Revised: %DIFDELCMD < %DIFDELCMD < %%% The Silurian is a major division of the geologic timescale that started about 443.8 ± 1.5 Ma. During the Silurian, Gondwana continued a slow southward drift to high southern latitudes, but there is evidence that the Silurian ice caps were less extensive than those of the late Ordovician glaciation.
Edit intent: clarity
Original: %DIFDELCMD < %DIFDELCMD < %%% Devonian Period The Devonian spanned roughly from 419 to 359 Ma. The period was a time of great tectonic activity, as Laurasia and Gondwana drew closer together.
Revised: %DIFDELCMD < %DIFDELCMD < %%% The Devonian spanned roughly from 419 to 359 Ma. The period was a time of great tectonic activity, as Laurasia and Gondwana drew closer together.
Edit intent: clarity
Original: %DIFDELCMD < %DIFDELCMD < %%% Carboniferous Period The Carboniferous extends from about 358.9 ± 0.4 to about 298.9 ± 0.15 Ma.%DIFDELCMD < %DIFDELCMD < %%% A global drop in sea level at the end of the Devonian reversed early in the Carboniferous;
Revised: %DIFDELCMD < %DIFDELCMD < %%% The Carboniferous extends from about 358.9 ± 0.4 to about 298.9 ± 0.15 Ma.%DIFDELCMD < %DIFDELCMD < %%% A global drop in sea level at the end of the Devonian reversed early in the Carboniferous;
Edit intent: clarity
Original: %DIFDELCMD < %DIFDELCMD < %%% Carboniferous Period The Carboniferous extends from about 358.9 ± 0.4 to about 298.9 ± 0.15 Ma.%DIFDELCMD < %DIFDELCMD < %%% A global drop in sea level at the end of the Devonian reversed early in the Carboniferous;
Revised: %DIFDELCMD < %DIFDELCMD < %%% Carboniferous Period %DIFDELCMD < %DIFDELCMD < %%% A global drop in sea level at the end of the Devonian reversed early in the Carboniferous;
Edit intent: coherence
Original:  Pangaea separation animation%DIFDELCMD < %DIFDELCMD < %%% Permian Period The Permian extends from about 298.9 ± 0.15 to 252.17 ± 0.06 Ma.%DIFDELCMD < %DIFDELCMD < %%% During the Permian all the Earth's major land masses, except portions of East Asia, were collected into a single supercontinent known as Pangaea.
Revised:  Pangaea separation animation%DIFDELCMD < %DIFDELCMD < %%% The Permian extends from about 298.9 ± 0.15 to 252.17 ± 0.06 Ma.%DIFDELCMD < %DIFDELCMD < %%% During the Permian all the Earth's major land masses, except portions of East Asia, were collected into a single supercontinent known as Pangaea.
Edit intent: clarity
Original:  Pangaea separation animation%DIFDELCMD < %DIFDELCMD < %%% Permian Period The Permian extends from about 298.9 ± 0.15 to 252.17 ± 0.06 Ma.%DIFDELCMD < %DIFDELCMD < %%% During the Permian all the Earth's major land masses, except portions of East Asia, were collected into a single supercontinent known as Pangaea.
Revised:  Pangaea separation animation%DIFDELCMD < %DIFDELCMD < %%% Permian Period %DIFDELCMD < %DIFDELCMD < %%% During the Permian all the Earth's major land masses, except portions of East Asia, were collected into a single supercontinent known as Pangaea.
Edit intent: coherence
Original: %DIFDELCMD < %DIFDELCMD < %%% Mesozoic Era%DIFDELCMD < %DIFDELCMD < %%% Plate tectonics- Plate tectonics- The Mesozoic extended roughly from .%DIFDELCMD < %DIFDELCMD < %%% After the vigorous convergent plate mountain-building of the late Paleozoic, Mesozoic tectonic deformation was comparatively mild.
Revised: %DIFDELCMD < %DIFDELCMD < %%% %DIFDELCMD < %DIFDELCMD < %%% Plate tectonics- Plate tectonics- The Mesozoic extended roughly from .%DIFDELCMD < %DIFDELCMD < %%% After the vigorous convergent plate mountain-building of the late Paleozoic, Mesozoic tectonic deformation was comparatively mild.
Edit intent: fluency
Original: %DIFDELCMD < %DIFDELCMD < %%% Mesozoic Era%DIFDELCMD < %DIFDELCMD < %%% Plate tectonics- Plate tectonics- The Mesozoic extended roughly from .%DIFDELCMD < %DIFDELCMD < %%% After the vigorous convergent plate mountain-building of the late Paleozoic, Mesozoic tectonic deformation was comparatively mild.
Revised: %DIFDELCMD < %DIFDELCMD < %%% Mesozoic Era%DIFDELCMD < %DIFDELCMD < %%% %DIFDELCMD < %DIFDELCMD < %%% After the vigorous convergent plate mountain-building of the late Paleozoic, Mesozoic tectonic deformation was comparatively mild.
Edit intent: coherence
Original: %DIFDELCMD < %DIFDELCMD < %%% Triassic Period%DIFDELCMD < %DIFDELCMD < %%% The Triassic Period extends from about 252.17 ± 0.06 to 201.3 ± 0.2 Ma. During the Triassic, almost all the Earth's land mass was concentrated into a single supercontinent centered more or less on the equator, called Pangaea ("all the land").
Revised: %DIFDELCMD < %DIFDELCMD < %%% %DIFDELCMD < %DIFDELCMD < %%% The Triassic Period extends from about 252.17 ± 0.06 to 201.3 ± 0.2 Ma. During the Triassic, almost all the Earth's land mass was concentrated into a single supercontinent centered more or less on the equator, called Pangaea ("all the land").
Edit intent: fluency
Original: %DIFDELCMD < %DIFDELCMD < %%% Jurassic Period%DIFDELCMD < %DIFDELCMD < %%% The Jurassic Period extends from about 201.3 ± 0.2 to 145.0 Ma. During the early Jurassic, the supercontinent Pangaea broke up into the northern supercontinent Laurasia and the southern supercontinent Gondwana;
Revised: %DIFDELCMD < %DIFDELCMD < %%% %DIFDELCMD < %DIFDELCMD < %%% The Jurassic Period extends from about 201.3 ± 0.2 to 145.0 Ma. During the early Jurassic, the supercontinent Pangaea broke up into the northern supercontinent Laurasia and the southern supercontinent Gondwana;
Edit intent: fluency
Original: %DIFDELCMD < %DIFDELCMD < %%% Cretaceous Period%DIFDELCMD < %DIFDELCMD < [[%%% File:100 global.png|Plate tectonics- 100 Ma, Cretaceous period%DIFDELCMD < ]] %DIFDELCMD < %%% The Cretaceous Period extends from circa to .%DIFDELCMD < %DIFDELCMD < %%% During the Cretaceous, the late Paleozoic-early Mesozoic supercontinent of Pangaea completed its breakup into present day continents, although their positions were substantially different at the time.
Revised: %DIFDELCMD < %DIFDELCMD < %%% %DIFDELCMD < %DIFDELCMD < [[%%% File:100 global.png|Plate tectonics- 100 Ma, Cretaceous period%DIFDELCMD < ]] %DIFDELCMD < %%% The Cretaceous Period extends from circa to .%DIFDELCMD < %DIFDELCMD < %%% During the Cretaceous, the late Paleozoic-early Mesozoic supercontinent of Pangaea completed its breakup into present day continents, although their positions were substantially different at the time.
Edit intent: fluency
Original: %DIFDELCMD < %DIFDELCMD < %%% Cretaceous Period%DIFDELCMD < %DIFDELCMD < [[%%% File:100 global.png|Plate tectonics- 100 Ma, Cretaceous period%DIFDELCMD < ]] %DIFDELCMD < %%% The Cretaceous Period extends from circa to .%DIFDELCMD < %DIFDELCMD < %%% During the Cretaceous, the late Paleozoic-early Mesozoic supercontinent of Pangaea completed its breakup into present day continents, although their positions were substantially different at the time.
Revised: %DIFDELCMD < %DIFDELCMD < %%% Cretaceous Period%DIFDELCMD < %DIFDELCMD < [[%%% %DIFDELCMD < ]] %DIFDELCMD < %%% The Cretaceous Period extends from circa to .%DIFDELCMD < %DIFDELCMD < %%% During the Cretaceous, the late Paleozoic-early Mesozoic supercontinent of Pangaea completed its breakup into present day continents, although their positions were substantially different at the time.
Edit intent: coherence
Original: %DIFDELCMD < %DIFDELCMD < %%% Cretaceous Period%DIFDELCMD < %DIFDELCMD < [[%%% File:100 global.png|Plate tectonics- 100 Ma, Cretaceous period%DIFDELCMD < ]] %DIFDELCMD < %%% The Cretaceous Period extends from circa to .%DIFDELCMD < %DIFDELCMD < %%% During the Cretaceous, the late Paleozoic-early Mesozoic supercontinent of Pangaea completed its breakup into present day continents, although their positions were substantially different at the time.
Revised: %DIFDELCMD < %DIFDELCMD < %%% Cretaceous Period%DIFDELCMD < %DIFDELCMD < [[%%% File:100 global.png|Plate tectonics- 100 Ma, Cretaceous period%DIFDELCMD < ]] %DIFDELCMD < %%% %DIFDELCMD < %DIFDELCMD < %%% During the Cretaceous, the late Paleozoic-early Mesozoic supercontinent of Pangaea completed its breakup into present day continents, although their positions were substantially different at the time.
Edit intent: coherence
Original: %DIFDELCMD < %DIFDELCMD < %%% Cenozoic Era%DIFDELCMD < %DIFDELCMD < %%% The Cenozoic Era covers the million years since the Cretaceous–Paleogene extinction event up to and including the present day.
Revised: %DIFDELCMD < %DIFDELCMD < %%% %DIFDELCMD < %DIFDELCMD < %%% The Cenozoic Era covers the million years since the Cretaceous–Paleogene extinction event up to and including the present day.
Edit intent: fluency
Original:  The Tethys Sea, which had separated the northern continents from Africa and India, began to close up, forming the Mediterranean Sea.%DIFDELCMD < %DIFDELCMD < %%% Paleogene Period%DIFDELCMD < %DIFDELCMD < %%% The Paleogene (alternatively Palaeogene) Period is a unit of geologic time that began and ended 23.03 Ma and comprises the first part of the Cenozoic Era.
Revised:  The Tethys Sea, which had separated the northern continents from Africa and India, began to close up, forming the Mediterranean Sea.%DIFDELCMD < %DIFDELCMD < %%% %DIFDELCMD < %DIFDELCMD < %%% The Paleogene (alternatively Palaeogene) Period is a unit of geologic time that began and ended 23.03 Ma and comprises the first part of the Cenozoic Era.
Edit intent: fluency
Original: %DIFDELCMD < %DIFDELCMD < %%% Paleocene Epoch%DIFDELCMD < %DIFDELCMD < %%% The Paleocene, lasted from to .%DIFDELCMD < %DIFDELCMD < %%% In many ways, the Paleocene continued processes that had begun during the late Cretaceous Period.
Revised: %DIFDELCMD < %DIFDELCMD < %%% %DIFDELCMD < %DIFDELCMD < %%% The Paleocene, lasted from to .%DIFDELCMD < %DIFDELCMD < %%% In many ways, the Paleocene continued processes that had begun during the late Cretaceous Period.
Edit intent: clarity
Original: %DIFDELCMD < %DIFDELCMD < %%% Paleocene Epoch%DIFDELCMD < %DIFDELCMD < %%% The Paleocene, lasted from to .%DIFDELCMD < %DIFDELCMD < %%% In many ways, the Paleocene continued processes that had begun during the late Cretaceous Period.
Revised: %DIFDELCMD < %DIFDELCMD < %%% Paleocene Epoch%DIFDELCMD < %DIFDELCMD < %%% %DIFDELCMD < %DIFDELCMD < %%% In many ways, the Paleocene continued processes that had begun during the late Cretaceous Period.
Edit intent: coherence
Original: %DIFDELCMD < %DIFDELCMD < %%% Eocene Epoch%DIFDELCMD < %DIFDELCMD < %%% During the Eocene ( - ), the continents continued to drift toward their present positions.
Revised: %DIFDELCMD < %DIFDELCMD < %%% %DIFDELCMD < %DIFDELCMD < %%% During the Eocene ( - ), the continents continued to drift toward their present positions.
Edit intent: clarity
Original: %DIFDELCMD < %DIFDELCMD < %%% Oligocene Epoch%DIFDELCMD < %DIFDELCMD < %%% The Oligocene Epoch extends from about to . During the Oligocene the continents continued to drift toward their present positions.
Revised: %DIFDELCMD < %DIFDELCMD < %%% %DIFDELCMD < %DIFDELCMD < %%% The Oligocene Epoch extends from about to . During the Oligocene the continents continued to drift toward their present positions.
Edit intent: fluency
Original: %DIFDELCMD < %DIFDELCMD < %%% Neogene Period%DIFDELCMD < %DIFDELCMD < %%% The Neogene Period is a unit of geologic time starting 23.03 Ma. and ends at 2.588 Ma.
Revised: %DIFDELCMD < %DIFDELCMD < %%% %DIFDELCMD < %DIFDELCMD < %%% The Neogene Period is a unit of geologic time starting 23.03 Ma. and ends at 2.588 Ma.
Edit intent: fluency
Original: %DIFDELCMD < %DIFDELCMD < %%% Miocene Epoch%DIFDELCMD < %DIFDELCMD < %%% The Miocene extends from about 23.03 to 5.333 Ma.%DIFDELCMD < %DIFDELCMD < %%% During the Miocene continents continued to drift toward their present positions.
Revised: %DIFDELCMD < %DIFDELCMD < %%% %DIFDELCMD < %DIFDELCMD < %%% The Miocene extends from about 23.03 to 5.333 Ma.%DIFDELCMD < %DIFDELCMD < %%% During the Miocene continents continued to drift toward their present positions.
Edit intent: clarity
Original: %DIFDELCMD < %DIFDELCMD < %%% Pliocene Epoch%DIFDELCMD < %DIFDELCMD < %%% The Pliocene extends from to . During the Pliocene continents continued to drift toward their present positions, moving from positions possibly as far as from their present locations to positions only 70 km from their current locations.
Revised: %DIFDELCMD < %DIFDELCMD < %%% %DIFDELCMD < %DIFDELCMD < %%% The Pliocene extends from to . During the Pliocene continents continued to drift toward their present positions, moving from positions possibly as far as from their present locations to positions only 70 km from their current locations.
Edit intent: clarity
Original: %DIFDELCMD < %DIFDELCMD < %%% Quaternary Period%DIFDELCMD < %DIFDELCMD < %%% Pleistocene Epoch%DIFDELCMD < %DIFDELCMD < %%% The Pleistocene extends from to 11,700 years before present.
Revised: %DIFDELCMD < %DIFDELCMD < %%% %DIFDELCMD < %DIFDELCMD < %%% Pleistocene Epoch%DIFDELCMD < %DIFDELCMD < %%% The Pleistocene extends from to 11,700 years before present.
Edit intent: clarity
Original: %DIFDELCMD < %DIFDELCMD < %%% Quaternary Period%DIFDELCMD < %DIFDELCMD < %%% Pleistocene Epoch%DIFDELCMD < %DIFDELCMD < %%% The Pleistocene extends from to 11,700 years before present.
Revised: %DIFDELCMD < %DIFDELCMD < %%% Quaternary Period%DIFDELCMD < %DIFDELCMD < %%% %DIFDELCMD < %DIFDELCMD < %%% The Pleistocene extends from to 11,700 years before present.
Edit intent: clarity
Original: %DIFDELCMD < %DIFDELCMD < %%% Holocene Epoch%DIFDELCMD < %DIFDELCMD < %%% Current Earth - without water, elevation greatly exaggerated (click/enlarge to "spin" 3D-globe).
Revised: %DIFDELCMD < %DIFDELCMD < %%% %DIFDELCMD < %DIFDELCMD < %%% Current Earth - without water, elevation greatly exaggerated (click/enlarge to "spin" 3D-globe).
Edit intent: clarity
Original:   Earth was initially molten due to extreme volcanism and frequent collisions with other bodies.
Revised:  The creation Earth was initially molten due to extreme volcanism and frequent collisions with other bodies.
Edit intent: clarity
Original:  The last glacial period of the current ice age ended about 10 , 000 years ago.
Revised:  The last glacial period of the current ice age ended about 10 , 
Edit intent: clarity
Original: %DIFDELCMD < %DIFDELCMD < %%% Hadean Eon File:Protoplanetary-disk.jpg|Artist's conception of a protoplanetary disc%DIFDELCMD < ]] %DIFDELCMD < %%% During Hadean time (4.6–4 Ga), the Solar System was forming, probably within a large cloud of gas and dust around the sun, called an accretion disc from which Earth formed .
Revised: %DIFDELCMD < %DIFDELCMD < %%% File:Protoplanetary-disk.jpg|Artist's conception of a protoplanetary disc%DIFDELCMD < ]] %DIFDELCMD < %%% During Hadean time (4.6–4 Ga), the Solar System was forming, probably within a large cloud of gas and dust around the sun, called an accretion disc from which Earth formed .
Edit intent: clarity