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Geological History of Earth

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Geological History of Earth Geological history of Earth 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). Earth formed about 4.54 billion years ago by accretion from the solar nebula, a disk-shaped mass of dust and gas left over from the formation of the Sun, which also created the rest of the Solar System. Earth was initially molten due to extreme volcanism and frequent collisions with other bodies. Eventually, the outer layer of the planet cooled to form a solid crust when water began accumulating in the atmosphere. The Moon formed soon afterwards, possibly as a result of the impact of a planetoid with the Earth. Geologic time represented in a diagram called a geological clock, showing the relative lengths of the Outgassing and volcanic activity produced the eons of Earth's history and noting major events primordial atmosphere. Condensing water vapor, augmented by ice delivered from comets, produced the oceans. As the surface continually reshaped itself over hundreds of millions of years, continents formed and broke apart. They migrated across the surface, occasionally combining to form a supercontinent. Roughly 750 million years ago, the earliest-known supercontinent Rodinia, began to break apart. The continents later recombined to form Pannotia, 600 to 540 million years ago, then finally Pangaea, which broke apart 200 million years ago. The present pattern of ice ages began about 40 million years ago, then intensified at the end of the Pliocene. The polar regions have since undergone repeated cycles of glaciation and thaw, repeating every 40,000–100,000 years. The last glacial period of the current ice age ended about 10,000 years ago. Contents Precambrian Hadean Eon Archean Eon Proterozoic Eon Phanerozoic Eon Paleozoic Era Mesozoic Era Cenozoic Era See also References Further reading External links Precambrian The Precambrian includes approximately 90% of geologic time. It extends from 4.6 Life timeline Ice Ages billion years ago to the beginning of the 0 — Primates Quater nary Flowers ←Earliest apes Cambrian Period (about 541 Ma). It includes P Birds h Mammals – Plants Dinosaurs three eons, the Hadean, Archean, and Karo o a n ← Andean Tetrapoda Proterozoic. -50 0 — e Arthropods Molluscs r ←Cambrian explosion o ← Cryoge nian Ediacara biota Major volcanic events altering the Earth's – z ←Earliest animals o ←Earliest plants environment and causing extinctions may i Multicellular -1000 — c have occurred 10 times in the past 3 billion life [1] ←Sexual reproduction years. – P r -1500 — o Hadean Eon t – e r Eukaryotes o -2000 — z o i Huron ian – c ←Oxygen crisis -2500 — ←Atmospheric oxygen – Photosynthesis Pong ola Artist's conception of a protoplanetary disc -3000 — A r c – h e During Hadean time (4.6–4 Ga), the Solar a -3500 — n ←Earliest oxygen System was forming, probably within a large Single-celled cloud of gas and dust around the sun, called – life an accretion disc from which Earth formed -4000 — ←Earliest life 4,500 million years ago.[2] The Hadean Eon H a water is not formally recognized, but it essentially – d e marks the era before we have adequate a ←Earliest water -4500 — record of significant solid rocks. The oldest n ←Earth (−4540) (million years ago) Clickable dated zircons date from about ( 4,400 million years ago.[3][4][5] Earth was initially molten due to extreme volcanism and frequent collisions with other bodies. Eventually, the outer layer of the planet cooled to form a solid crust when water began accumulating in the atmosphere. The Moon formed soon afterwards, possibly as a result of the impact of a large planetoid with the Earth.[6][7] Some of this object's mass merged with the Earth, significantly altering its internal composition, and a portion was ejected into space. Some of the material survived to form an orbiting moon. More recent potassium isotopic studies suggest that the Moon was formed by a smaller, high- energy, high-angular-momentum giant impact cleaving off a significant portion of the Earth.[8] Outgassing and volcanic activity produced the primordial atmosphere. Condensing water vapor, augmented by ice delivered from comets, produced the oceans.[9] During the Hadean the Late Heavy Bombardment occurred (approximately 4,100 to 3,800 million years ago) during which a large number of impact craters are believed to have formed on the Moon, and by inference on Earth, Mercury, Venus and Mars as well. Archean Eon The Earth of the early Archean (4,000 to 2,500 million years ago) may have had a different tectonic style. During this time, the Earth's crust cooled enough that rocks and continental plates began to form. Some scientists think because the Earth was hotter, that plate tectonic activity was more vigorous than it is today, resulting in a much greater rate of recycling of crustal material. This may have prevented cratonisation and continent formation until the mantle cooled and convection slowed down. Others argue that the subcontinental lithospheric mantle is too buoyant to subduct and that the lack of Archean rocks is a function of erosion and subsequent tectonic events. In contrast to the Proterozoic, Archean rocks are often heavily metamorphized deep-water sediments, such as graywackes, mudstones, volcanic sediments and banded iron formations. Greenstone belts are typical Archean formations, consisting of alternating high- and low-grade metamorphic rocks. The high- grade rocks were derived from volcanic island arcs, while the low-grade metamorphic rocks represent deep-sea sediments eroded from the neighboring island rocks and deposited in a forearc basin. In short, greenstone belts represent sutured protocontinents.[10] The Earth's magnetic field was established 3.5 billion years ago. The solar wind flux was about 100 times the value of the modern Sun, so the presence of the magnetic field helped prevent the planet's atmosphere from being stripped away, which is what probably happened to the atmosphere of Mars. However, the field strength was lower than at present and the magnetosphere was about half the modern radius.[11] Proterozoic Eon The geologic record of the Proterozoic (2,500 to 541 million years ago) is more complete than that for the preceding Archean. In contrast to the deep-water deposits of the Archean, the Proterozoic features many strata that were laid down in extensive shallow epicontinental seas; furthermore, many of these rocks are less metamorphosed than Archean-age ones, and plenty are unaltered.[12] Study of these rocks show that the eon featured massive, rapid continental accretion (unique to the Proterozoic), supercontinent cycles, and wholly modern orogenic activity.[13] Roughly 750 million years ago,[14] the earliest-known supercontinent Rodinia, began to break apart. The continents later recombined to form Pannotia, 600–540 Ma.[4][15] 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.[16] Phanerozoic Eon The Phanerozoic Eon is the current eon in the geologic timescale. It covers roughly 541 million years. During this period continents drifted about, eventually collected into a single landmass known as Pangea and then split up into the current continental landmasses. The Phanerozoic is divided into three eras – the Paleozoic, the Mesozoic and the Cenozoic. Most of biological evolution occurred during this time period. Paleozoic Era The Paleozoic spanned from roughly 542 to 251 million years ago (Ma)[4] and is subdivided into six geologic periods; from oldest to youngest they are the Cambrian, Ordovician, Silurian, Devonian, Carboniferous and Permian. Geologically, the Paleozoic starts shortly after the breakup of a supercontinent called Pannotia and at the end of a global ice age. Throughout the early Paleozoic, the Earth's landmass was broken up into a substantial number of relatively small continents. Toward the end of the era the continents gathered together into a supercontinent called Pangaea, which included most of the Earth's land area. Cambrian Period The Cambrian is a major division of the geologic timescale that begins about 541.0 ± 1.0 Ma.[4] Cambrian continents are thought to have resulted from the breakup of a Neoproterozoic supercontinent called Pannotia. The waters of the Cambrian period appear to have been widespread and shallow. Continental drift rates may have been anomalously high. Laurentia, Baltica and Siberia remained independent continents following the break-up of the supercontinent of Pannotia. Gondwana started to drift toward the South Pole. Panthalassa covered most of the southern hemisphere, and minor oceans included the Proto-Tethys Ocean, Iapetus Ocean and Khanty Ocean. 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.[4] During the Ordovician the southern continents were collected into a single continent called Gondwana. Gondwana started the period in the equatorial latitudes and, as the period progressed, drifted toward the South Pole. Early in the Ordovician the continents Laurentia, Siberia and Baltica were still independent continents (since the break-up of the supercontinent Pannotia earlier), but Baltica began to move toward Laurentia later in the period, causing the Iapetus Ocean to shrink between them. Also, Avalonia broke free from Gondwana and began to head north toward Laurentia. The Rheic Ocean was formed as a result of this. By the end of the period, Gondwana had neared or approached the pole and was largely glaciated. The Ordovician came to a close in a series of extinction events that, taken together, comprise the second- largest of the five major extinction events in Earth's history in terms of percentage of genera that became extinct.
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