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Life is a characteristic distinguishing physical entities having biological processes (such as signaling and self-sustaining processes) from those that do not, [1] [2] either because such functions have ceased (death ), or because they lack such functions and are classified as inanimate . [3] [4] [5] Various forms of life exist such as plants , animals , fungi , protists , archaea , and bacteria . The criteria can at times be ambiguous and may or may not define viruses , viroids or potential artificial life as living. Biology is the primary science concerned with the study of life, although many other sciences are involved. The smallest contiguous unit of life is called an organism . Organisms are composed of one or more cells , undergo metabolism , maintain homeostasis , can grow , respond to stimuli , reproduce (either sexually or asexuall y ) and, through evolution , adapt to their environment in successive generations . [1] A diverse array of living organisms can be found in the biosphere of Earth , and the properties common to these organisms— plants , animals , fungi , protists , archaea , and bacteria —are a carbon - and water -

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Life is a characteristic distinguishing physical entities having biological processes (such as signaling and self-sustaining processes) from those that do not,[1][2] either because suchfunctions have ceased (death), or because they lack such functions and are classified as inanimate.[][!]["] #arious forms of life e$ist such as plants, animals, fungi, protists, archaea, and bacteria. %he criteria can at times be ambiguous and may or may not define viruses, viroids or potential artificial life as living. &iology is the primary science concerned 'ith the study of life, although many other sciences are involved.%he smallest contiguous unit of life is called an organism. (rganisms are composed of one or more cells, undergo metabolism, maintain homeostasis, can gro', respond to stimuli, reproduce (either se$ually or ase$ually) and, through evolution, adapt to their environment in successive generations.[1] ) diverse array of living organisms can befound in the biosphere of *arth, and the properties common to these organisms+plants, animals, fungi, protists, archaea, and bacteria+are a carbon- and 'ater-basedcellular form 'ith comple$ organi,ation and heritable genetic information.)biogenesis is the natural process of life arising from non-living matter, such as simple organic compounds. %he age of the *arth is about !."! billion years old.[-][.][/] %he earliest life on *arth arose at least ." billion years ago,[0][11][11] during the *oarchean *ra 'hen sufficient crust had solidified follo'ing the molten 2adean *on. %he earliest physical evidence of life on *arth is biogenic graphite from .. billion-year-old metasedimentary rocks found in 3estern 4reenland [12] and microbial mat fossils in .!/ billion-year-old sandstonefrom in 3estern )ustralia.[1][1!] 5ome theories, such as the 6ate 2eavy &ombardment theory, suggest that life on *arth mayhave started even earlier,[1"] and may have begun as early as !.2" billion years ago according to one study,[1-] and even earlier yet, !.! billion years ago, according to another.[1.] %he mechanism by 'hich life began on *arth is unkno'n, although many hypotheses have been formulated. 5ince emerging, life has evolved into a variety of forms, 'hich have been classified into a hierarchy of ta$a. 6ife can survive and thrive in a 'ide range of conditions. 7onetheless, more than 00 percent of all species, amounting to over five billion species,[1/] that ever lived on *arth are estimated to be e$tinct.[10][21] *stimates on the number of *arth8s current species range from 11 million to 1!million,[21] of 'hich about 1.2 million have been documented and over /- percent have not yet been described.[22]%he chemistry leading to life may have begun shortly after the &ig &ang, 1./ billion years ago, during a habitable epoch 'hen the9niverse 'as only 11:1. million years old.[2][2!][2"] )ccording to the panspermia hypothesis, microscopic life+distributed bymeteoroids, asteroids and other small 5olar 5ystem bodies+maye$ist throughout the universe.[2-] %hough life is confirmed only on the*arth, many think that e$traterrestrial life is not only plausible, but probable or inevitable.[2.][2/] (ther planets and moons[20] in the5olar 5ystem and other planetary systems are being e$amined for evidence of having once supported simple life, and pro;ects such as5*%< are trying to detect radio transmissions from possible alien civili,ations.%he meaning of life+its significance, origin, purpose, and ultimate fate+is a central concept and =uestion in philosophy and religion. &oth philosophy and religion have offered interpretations as to ho' life relates to e$istence and consciousness, and on related issues such as life stance, purpose, conception of a god or gods, a soul or an afterlife. >ifferent cultures throughout history have had 'idely varying approaches to these issues.Contents[hide] 1*arly theorieso 1.1?aterialismo 1.22ylomorphismo 1.#italism 2>efinitionso 2.1&iologyo 2.26iving systems theories (rigin !*nvironmental conditionso !.1@ange of tolerance "Aorm and function -Blassification .*$traterrestrial lifeo ..1@esearch />eath 0)rtificial life 11Chanero,oic *ono 11.1Caleo,oic *rao 11.2?eso,oic *rao 11.Beno,oic *ra 115ee also 127otes 1@eferences 1!Aurther reading 1"*$ternal linksEarly theoriesMaterialismClant gro'th in the 2oh @ainforest2erds of ,ebra and impala gathering on the ?aasai ?ara plain)n aerial photo of microbial mats around the 4rand Crismatic 5pring ofDello'stone 7ational Cark5ome of the earliest theories of life 'ere materialist, holding that all that e$ists is matter, and that life is merely a comple$ form or arrangement of matter. *mpedocles (!1 &B) argued that every thing in the universe is made up of a combination of four eternal EelementsE or Eroots of allEF earth, 'ater, air, and fire. )ll change is e$plained by the arrangement and rearrangement of these four elements. %he various forms of life are caused by an appropriate mi$ture of elements.[1]>emocritus (!-1 &B) thought that the essential characteristic of life is having a soul (psyche). 6ike other ancient 'riters, he 'as attempting to e$plain 'hat makes something a living thing. 2is e$planation 'as that fiery atoms make a soul in e$actly the same 'ay atoms and void account for any other thing. 2e elaborates on fire because of the apparent connection bet'een life and heat, and because fire moves.[1]Clato8s 'orld of eternal and unchanging Aorms, imperfectly represented in matter by a divine )rtisan, contrasts sharply 'ith the various mechanistic 3eltanschauungen, of 'hich atomism 'as, by the fourth century at least, the most prominent... %his debate persisted throughout the ancient 'orld. )tomistic mechanism got a shot in the arm from *picurus... 'hile the 5toics adopted a divine teleology... %he choice seems simpleF either sho' ho' a structured, regular 'orld could arise out of undirected processes, or in;ect intelligence into the system.[2]+@. G. 2ankinson, Cause and Explanation in Ancient Greek Thought%he mechanistic materialism that originated in ancient 4reece 'as revived and revised by the Arench philosopher @enH >escartes, 'ho held that animals and humans 'ere assemblages of parts that together functioned as a machine. ar'inian evolution.[-"](thers take a systemic vie'point that does not necessarily depend on molecular chemistry. (ne systemic definition of life is that living things are self-organi,ing and autopoietic(self-producing). #ariationsof this definition include 5tuart Kauffman8s definition as an autonomous agent or a multi-agent system capable of reproducing itself or themselves, and of completing at least one thermodynamic 'ork cycle.[--]Viruses*lectron micrograph of adenovirus'ith a cartoon to demonstrate its icosahedral structure#iruses are most often considered replicators rather than forms of life. %hey have been described as Eorganisms at the edge of life,E[-.]since they possess genes, evolve by natural selection,[-/][-0] andreplicate by creating multiple copies of themselves through self-assembly. 2o'ever, viruses do not metaboli,e and they re=uire a host cell to make ne' products. #irus self-assembly 'ithin host cells has implications for the study of the origin of life, as it may support the hypothesis that life could have started as self-assembling organic molecules.[.1][.1][.2]Li!ing systems theories%he idea that the *arth is alive is found in philosophy and religion, but the first scientific discussion of it 'as by the 5cottish scientist Games 2utton. 7), the e$ception being sulfur. %he latter is a component of the amino acids cysteine and methionine. %he most biologically abundant of these elements is carbon, 'hich has the desirable attribute of forming multiple, stable covalent bonds. %his allo's carbon-based (organic) molecules to form an immense variety of chemical arrangements.[121] )lternative hypothetical types of biochemistryhave been proposed that eliminate one or more of these elements, s'ap out an element for one not on the list, or change re=uiredchiralities or other chemical properties.[121][122]Range of tolerane%he inert components of an ecosystem are the physical and chemical factors necessary for life + energy (sunlight or chemical energy), 'ater, temperature, atmosphere, gravity,nutrients, and ultraviolet solar radiation protection.[12] uring this time, there are four continentsF 4ond'ana ()frica, 5outh )merica, )ustralia, )ntarctica, 5iberia), 6aurentia (7orth )merica), &altica (7orthern *urope), and )valonia (3estern *urope). %he recent rise in sea levels provided many ne' species to thrive in 'ater.[10]3e!onian*ogyrinus (an amphibian) of the Barboniferous%he >evonian spans from !1" million years to -1 million years ago. )lso kno'n as E%he )ge of the AishE, the >evonian features a huge diversification of fish, including armored fish like >unkleosteus and lobe-finned fish 'hich eventually evolved intothe first tetrapods. (n land, plant groups diversified incredibly in an event kno'n as the >evonian *$plosion 'here the first trees evolved, as 'ell as seeds. %his event also diversified arthropod life. %he first amphibians also evolved, and the fish 'ere no' at the top of the food chain. 7ear the end of the >evonian, .1M of all species 'ent e$tinct in an event kno'n as the 6ate >evonian e$tinction and is the second mass e$tinction event the 'orld has seen.[10!]Carboniferous>imetrodon%he Barboniferous spans from -1 million to 11 million years ago. >uring this time, average global temperatures 'ere e$ceedingly highI the early Barboniferous averaged at about 21 degrees Belsius(but cooled do'n to 11 degrees during the ?iddle Barboniferous).[10"]%ropical s'amps dominated the earth, and the large amounts of trees created much of the carbon for the coal that is used today (hence the name EBarbon-iferousE). Cerhaps the most important evolutionary development of the time 'as the evolution of amniotic eggs, 'hich allo'ed amphibians to head farther inland and remained the dominant vertebrae throughout the duration of this period. )lso, the first reptiles and synapsids evolved in the s'amps. %hroughout the Barboniferous, there 'as a cooling pattern, 'hich eventually led to the glaciation of 4ond'ana as much of it 'as situated around the south pole in an event kno'n as the Cermo-Barboniferous glaciation or theBarboniferous @ainforest Bollapse.[10-]1ermian%he Cermian spans from 11 million to 2"1 million years ago and 'as the last period of the Caleo,oic. )t the beginning, all continents formed together to form the super-continentCangaea and had one ocean called Canthalassa. %he earth 'as very dry during this time, 'ith harsh seasons as the climate of the interior of Cangaea 'asn8t regulated by large bodies of 'ater. @eptiles and synapsids flourished in the ne' dry climate. Breatures such as >imetrodon and *daphosaurus ruled the ne' continent. %he firstconifers evolve, and dominate the terrestrial landscape. 7earing theend of the Cermian, ho'ever, Cangaea got drier and drier. %he interior 'as nothing but dry deserts, and ne' species such as5cutosaurus and 4orgonopsid filled the empty desert. *ventually,they disappeared, along 'ith 0"M of all life on earth in an event simply kno'n as Ethe 4reat >yingE, and is the third mass e$tinction event of the 'orld.[10.][10/]Mesozoi 2raMain article: Meso/oic)lso kno'n as Ethe )ge of the dinosaursE, the ?eso,oic features the rise of reptiles on their 1"1 million year con=uest to rule the earth from the seas, the land, and even in the air. %here areperiods in the ?eso,oicF the %riassic, the Gurassic, and the Bretaceous.4riassi%he %riassic ranges from 2"1 million to 211 million years ago. %he %riassic is a desolate transitional state in *arth8s history bet'een the Cermian *$tinction and the lush Gurassic Ceriod. ying. %emnospondyli evolved during this time and 'ould be the dominant predator for much of the %riassic.[211]Clateosaurus (a prosauropod)%he ?iddle %riassic spans from 2!. million to 2. million years ago.%he ?iddle %riassic featured the beginnings of the breakup ofCangaea, and the beginning of the %ethys 5ea. %he ecosystem had recovered from the devastation that 'as the 4reat >ying. Chytoplankton, coral, and crustaceans all had recovered, and the reptiles began to get bigger and bigger. 7e' a=uatic reptiles evolved such as