Carbon-based life: Difference between revisions

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[[Carbon]] is a primary component of all known [[life]] on [[Earth]], and represents approximately 45–50% of all dry [[biomass]].<ref>{{Cite web|url=http://www.fao.org/forestry/17111/en/|title=Knowledge reference for national forest assessments - modeling for estimation and monitoring|website=www.fao.org|access-date=Feb 20, 2019|archive-date=January 13, 2020|archive-url=https://web.archive.org/web/20200113113656/http://www.fao.org/forestry/17111/en/|url-status=dead}}</ref> Carbon compounds occur naturally in great abundance on Earth. Complex biological [[molecule]]s consist of carbon atoms [[chemical bond|bonded]] with other [[chemical element|elements]], especially [[oxygen]] and [[hydrogen]] and frequently also [[nitrogen]], [[phosphorus]], and [[sulfur]] (collectively known as [[CHON|CHNOPS]]).<ref name="auto">{{Cite journal|url=https://opentextbc.ca/biology/chapter/2-3-biological-molecules/|title=2.3 Biological Molecules|first1=Charles|last1=Molnar|first2=Jane|last2=Gair|date=May 14, 2015|via=opentextbc.ca|journal=Introduction to the Chemistry of Life}}</ref><ref name=Education>{{cite web |title=CHNOPS: The Six Most Abundant Elements of Life |url=http://www.phschool.com/science/biology_place/biocoach/biokit/chnops.html |last=Education |year=2010 |work=[[Pearson Education]] |publisher=Pearson BioCoach |access-date=2010-12-10 |quote=Most biological molecules are made from covalent combinations of six important elements, whose chemical symbols are CHNOPS. ... Although more than 25 types of elements can be found in biomolecules, six elements are most common. These are called the CHNOPS elements; the letters stand for the chemical abbreviations of carbon, hydrogen, nitrogen, oxygen, phosphorus, and sulfur. |archive-date=27 July 2017 |archive-url=https://web.archive.org/web/20170727200948/http://www.phschool.com/science/biology_place/biocoach/biokit/chnops.html |url-status=live }}</ref>
 
Because it is lightweight and relatively small in size, carbon molecules are easy for [[enzyme]]s to manipulate. [[Carbonic anhydrase]] is part of this process. Carbon has an [[atomic number]] of 6 on the [[periodic table]]. The [[carbon cycle]] is a [[biogeochemical cycle]] that is important in maintaining life on Earth over a long time span. The cycle includes [[carbon sequestration]] and [[carbon sink]]s.<ref name="nasacc">{{cite web|last1=Riebeek|first1=Holli|title=The Carbon Cycle|url=http://earthobservatory.nasa.gov/Features/CarbonCycle/?src=eoa-features|website=Earth Observatory|publisher=NASA|access-date=5 April 2018|date=16 June 2011|archive-url=https://web.archive.org/web/20160305010126/http://earthobservatory.nasa.gov/Features/CarbonCycle/?src=eoa-features|archive-date=5 March 2016|url-status=live|df=dmy-all}}</ref><ref>{{cite book|last1=Archer|first1=David|title=The global carbon cycle|date=2010|publisher=Princeton University Press|location=Princeton|isbn=9781400837076}}</ref> [[Plate tectonics]] are needed for life over a long time span, and carbon-based life is important in the plate tectonics process.<ref>{{Cite web|url=https://www.sydney.edu.au/news-opinion/news/2022/05/26/how-plate-tectonics-have-maintained-earth-s--goldilocks--climate.html|title=How plate tectonics have maintained Earth's 'Goldilocks' climate|website=The University of Sydney}}</ref> An abundance of iron- and sulfur -based [[Anoxygenic photosynthesis]] life forms that lived from 3.80 to 3.85 billion years ago on Earth produces an abundance [[black shale]] deposits. These shale deposits increase heat flow and crust buoyancy, especially on the sea floor, helping to increase plate tectonics. [[Talc]] is another organic mineral that helps drive plate tectonics.<ref>{{Cite web|url=https://www.soapstonetalc.com/talc-processing/|title=Talc Processing|website=www.soapstonetalc.com}}</ref><ref>{{Cite web|url=http://eos.org/research-spotlights/talc-may-make-mexicos-subduction-zone-more-slippery|title=Talc May Make Mexico's Subduction Zone More Slippery|first=Aaron|last=Sidder|date=August 23, 2023|website=Eos}}</ref> [[Inorganic chemistry|Inorganic processes]] also help drive plate tectonics.<ref>{{Cite web|url=https://www.researchgate.net/publication/250164952|title=Geology, Age and Origin of Supracrustal Rocks at Akilia, West Greenland}}</ref> Carbon-based [[photosynthesis]] life caused a rise in [[oxygen]] on Earth. This increase of oxygen helped plate tectonics form the first continents.<ref>{{Cite web|url=https://www.forbes.com/sites/davidbressan/2023/03/07/first-continents-and-weathering-iron-minerals-helped-rise-oxygen-levels-on-early-earth/|title=Rise Of Oxygen On Early Earth Linked To The Formation Of First Continents|first=David|last=Bressan|website=Forbes}}</ref> It is frequently assumed in [[astrobiology]] that if life exists elsewhere in the [[Universe]], it will also be carbon-based.<ref name=BC>{{cite web | url = http://biocab.org/Astrobiology.html | title = Astrobiology | access-date = 2011-01-17 | date = September 26, 2006 | publisher = Biology Cabinet}}</ref><ref>{{cite web |url=http://library.thinkquest.org/C003763/index.php?page=interview07 |title=Polycyclic Aromatic Hydrocarbons: An Interview With Dr. Farid Salama |access-date=2008-10-20 |year=2000 |work=Astrobiology magazine |url-status=dead |archive-url=https://web.archive.org/web/20080620075201/http://library.thinkquest.org/C003763/index.php?page=interview07 |archive-date=2008-06-20 }}</ref> Critics, like [[Carl Sagan]] in 1973, refer to this assumption as [[carbon chauvinism]].<ref name =darling>{{cite web |url= http://www.daviddarling.info/encyclopedia/C/carbon-based_life.html |title=Carbon-based life |access-date=14 September 2007 |first=David|last=Darling |publisher=Encyclopedia of Life}}</ref>
 
==Characteristics==