Difference between revisions of "Nature"

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== Life ==  
 
== Life ==  
  
Although there is no universal agreement on the definition of life, scientists generally accept that the biological manifestation of life is characterized by [[Organism|organization]], [[metabolism]], [[cell growth|growth]], [[adaptation]], response to [[stimulus (physiology)|stimuli]] and [[reproduction]].<ref>{{cite web | year = 2006 | url = http://www.calacademy.org/exhibits/xtremelife/what_is_life.php | title = Definition of Life | publisher = California Academy of Sciences | accessdate = 2007-01-07 }}</ref> Life may also be said to be simply the characteristic state of [[organism]]s.
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Although there is no universal agreement on the definition of life, scientists generally accept that the biological manifestation of life is characterized by [[Organism|organization]], [[metabolism]], [[cell growth|growth]], [[adaptation]], response to [[stimulus (physiology)|stimuli]] and [[reproduction]].[http://www.calacademy.org/exhibits/xtremelife/what_is_life.php] Life may also be said to be simply the characteristic state of [[organism]]s.
  
 
Properties common to terrestrial organisms ([[plant]]s, [[animal]]s, [[fungi]], [[protist]]s, [[archaea]] and [[bacteria]]) are that they are cellular, carbon-and-water-based with complex organization, having a metabolism, a capacity to grow, respond to stimuli, and reproduce. An entity with these properties is generally considered life. However, not every definition of life considers all of these properties to be essential. Human-made [[Artificial life|analogs of life]] may also be considered to be life.
 
Properties common to terrestrial organisms ([[plant]]s, [[animal]]s, [[fungi]], [[protist]]s, [[archaea]] and [[bacteria]]) are that they are cellular, carbon-and-water-based with complex organization, having a metabolism, a capacity to grow, respond to stimuli, and reproduce. An entity with these properties is generally considered life. However, not every definition of life considers all of these properties to be essential. Human-made [[Artificial life|analogs of life]] may also be considered to be life.
  
The [[biosphere]] is the part of Earth's outer shell — including air, land, surface rocks and water — within which life occurs, and which [[biotic]] processes in turn alter or transform. From the broadest [[Geophysiology|geophysiological]] point of view, the biosphere is the global ecological system integrating all living beings and their relationships, including their interaction with the elements of the [[lithosphere]] (rocks), [[hydrosphere]] (water), and [[atmosphere]] (air).  Currently the entire Earth contains over 75 billion tons (150 ''trillion'' pounds or about 6.8&nbsp;x&nbsp;10<sup>13</sup>&nbsp;[[kilogram]]s) of [[biomass (ecology)|biomass]] (life), which lives within various environments within the biosphere.<ref>The figure "about one-half of one percent" takes into account the following (See, e.g., {{cite book |last=Leckie |first=Stephen |year=1999 |chapter=How Meat-centred Eating Patterns Affect Food Security and the Environment |chapterurl=http://www.idrc.ca/en/ev-30610-201-1-DO_TOPIC.html |title=For hunger-proof cities : sustainable urban food systems |publisher=International Development Research Centre |location=Ottawa |id=ISBN 0-88936-882-1}}, which takes global average weight as 60 kg.), the total human biomass is the average weight multiplied by the current human population of approximately 6.5 billion (see, ''e.g.'', {{cite web |title=World Population Information |url=http://www.census.gov/ipc/www/world.html |accessmonthday=September 28 |accessyear=2006 |publisher=U.S. Census Bureau}}): Assuming 60–70 kg to be the average human mass (approximately 130–150&nbsp;[[pound (mass)|lb]] on the average), an approximation of total global human mass of between 390 billion (390×10<sup>9</sup>) and 455 billion kg (between 845 billion and 975 billion lb, or about 423 million-488 million [[short ton]]s). The total biomass of all kinds on earth is estimated to be in excess of 6.8&nbsp;x&nbsp;10<sup>13</sup>&nbsp;kg (75 billion short tons). By these calculations, the portion of total biomass accounted for by humans would be very roughly 0.6%.</ref>
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The [[biosphere]] is the part of Earth's outer shell — including air, land, surface rocks and water — within which life occurs, and which [[biotic]] processes in turn alter or transform. From the broadest [[Geophysiology|geophysiological]] point of view, the biosphere is the global ecological system integrating all living beings and their relationships, including their interaction with the elements of the [[lithosphere]] (rocks), [[hydrosphere]] (water), and [[atmosphere]] (air).  Currently the entire Earth contains over 75 billion tons (150 ''trillion'' pounds or about 6.8&nbsp;x&nbsp;10<sup>13</sup>&nbsp;[[kilogram]]s) of [[biomass (ecology)|biomass]] (life), which lives within various environments within the biosphere. The figure "about one-half of one percent" takes into account the following (See, e.g., [http://www.idrc.ca/en/ev-30610-201-1-DO_TOPIC.html] ISBN 0-88936-882-1), which takes global average weight as 60 kg.), the total human biomass is the average weight multiplied by the current human population of approximately 6.5 billion (see, ''e.g.'', [http://www.census.gov/ipc/www/world.html] Assuming 60–70 kg to be the average human mass (approximately 130–150&nbsp;[[pound (mass)|lb]] on the average), an approximation of total global human mass of between 390 billion (390×10<sup>9</sup>) and 455 billion kg (between 845 billion and 975 billion lb, or about 423 million-488 million [[short ton]]s). The total biomass of all kinds on earth is estimated to be in excess of 6.8&nbsp;x&nbsp;10<sup>13</sup>&nbsp;kg (75 billion short tons). By these calculations, the portion of total biomass accounted for by humans would be very roughly 0.6%.
  
Over nine-tenths of the total biomass on Earth is plant life, on which animal life depends very heavily for its existence.<ref>{{cite web |first=Peter V. |last=Sengbusch |title=The Flow of Energy in Ecosystems - Productivity, Food Chain, and Trophic Level |work=Botany online |publisher=University of Hamburg Department of Biology |url=http://www.biologie.uni-hamburg.de/b-online/e54/54c.htm |accessmonthday=September 23|accessyear=2006}}</ref> More than 2 million species of plant and animal life have been identified to date,<ref>{{cite web |last=Pidwirny |first=Michael |year=2006 |work=Fundamentals of Physical Geography (2nd Edition) |title=Introduction to the Biosphere: Species Diversity and Biodiversity |url=http://www.physicalgeography.net/fundamentals/9h.html |accessmonthday=September 23|accessyear=2006}}</ref> and estimates of the actual number of existing species range from several million to well over 50 million.<ref>{{cite web |url=http://faculty.plattsburgh.edu/thomas.wolosz/howmanysp.htm |title=How Many Species are There? |work=Extinction Web Page Class Notes |accessmonthday=September 23|accessyear=2006}}</ref><ref>"Animal." World Book Encyclopedia. 16 vols. Chicago: World Book, 2003. This source gives an estimate of from 2-50 million.</ref><ref>{{cite web |url=http://www.sciencedaily.com/releases/2003/05/030526103731.htm |title=Just How Many  Species Are There, Anyway? |publisher=Science Daily |year=2003 |month=May |accessmonthday=September 26|accessyear=2006 }}</ref> The number of individual species of life is constantly in some degree of flux, with new species appearing and others ceasing to exist on a continual basis.<ref>{{cite web |last=Withers |first=Mark A. |coauthors=et al. |title=Changing Patterns in the Number of Species in North American Floras |work=Land Use History of North America |url=http://biology.usgs.gov/luhna/chap4.html |year=1998 |accessmonthday=September 26|accessyear=2006 }} Website based on the contents of the book: {{cite book |editor=Sisk, T.D., ed. |year=1998 |title=Perspectives on the land use history of North America: a context for understanding our changing environment |publisher=U.S. Geological Survey, Biological Resources Division |id=USGS/BRD/BSR-1998-0003 |edition=Revised September 1999 }}</ref><ref>{{cite web |title=Tropical Scientists Find Fewer Species Than Expected |url=http://www.sciencedaily.com/releases/2002/04/020425072847.htm |year=2002 |month=April |publisher=Science Daily |accessmonthday=September 27|accessyear=2006 }}</ref> The total number of species is presently in rapid decline.<ref>{{cite journal |last=Bunker |first=Daniel E. |coauthors=et al. |title=Species Loss and Aboveground Carbon Storage in a Tropical Forest |url=http://www.sciencemag.org/cgi/content/abstract/310/5750/1029 |journal=Science |year=2005 |month=November |volume=310 |issue=5750 |pages=pp. 1029-31 |id={{doi|10.1126/science.1117682}} }}</ref><ref>{{cite journal |last=Wilcox |first=Bruce A. |title=Amphibian Decline: More Support for Biocomplexity as a Research Paradigm |journal=EcoHealth |year=2006 |month=March |volume=3 |issue=1  |url=http://www.ecohealth.net/pdfs/Vol3/ECH_Editorial_3_1.pdf |id={{doi|10.1007/s10393-005-0013-5}} |pages=pp.1-2 }}</ref><ref>{{cite book |editor=Clarke, Robin, Robert Lamb, Dilys Roe Ward eds. |year=2002 |title= Global environment outlook 3 : past, present and future perspectives |chapter=Decline and loss of species |chapterurl=http://www.grida.no/geo/geo3/english/221.htm |publisher=Nairobi, Kenya : UNEP |location=London; Sterling, VA |id=ISBN 92-807-2087-2}}</ref>
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Over nine-tenths of the total biomass on Earth is plant life, on which animal life depends very heavily for its existence.[http://www.biologie.uni-hamburg.de/b-online/e54/54c.htm] More than 2 million species of plant and animal life have been identified to date, [http://www.physicalgeography.net/fundamentals/9h.html] and estimates of the actual number of existing species range from several million to well over 50 million.[http://faculty.plattsburgh.edu/thomas.wolosz/howmanysp.htm] [http://www.sciencedaily.com/releases/2003/05/030526103731.htm] The number of individual species of life is constantly in some degree of flux, with new species appearing and others ceasing to exist on a continual basis.[http://biology.usgs.gov/luhna/chap4.html] Website based on the contents of the book: Perspectives on the land use history of North America: a context for understanding our changing environment [http://www.sciencedaily.com/releases/2002/04/020425072847.htmThe total number of species is presently in rapid decline. [http://www.sciencemag.org/cgi/content/abstract/310/5750/1029] [http://www.ecohealth.net/pdfs/Vol3/ECH_Editorial_3_1.pdf] [http://www.grida.no/geo/geo3/english/221.htm] ISBN 92-807-2087-2)
  
 
===Evolution===
 
===Evolution===
Life, as we understand it, is currently only known to exist on the planet Earth. The [[origin of life]] is still a poorly understood process, but it is thought to have occurred about 3.9 to 3.5 billion years ago during the [[hadean]] or [[archean]] eons on a primordial earth that had a substantially different environment than is found at present.<ref name=Line>{{cite journal | author = Line M | title = The enigma of the origin of life and its timing | url=http://mic.sgmjournals.org/cgi/content/full/148/1/21?view=long&pmid=11782495 | journal = Microbiology | volume = 148 | issue = Pt 1 | pages = 21-7 | year = 2002 | id = PMID 11782495}}</ref> These life forms possessed the basic traits of self-replication and inheritable traits. Once life had appeared, the process of [[evolution]] by [[natural selection]] resulted in the formation of ever-more diverse life forms.
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Life, as we understand it, is currently only known to exist on the planet Earth. The [[origin of life]] is still a poorly understood process, but it is thought to have occurred about 3.9 to 3.5 billion years ago during the [[hadean]] or [[archean]] eons on a primordial earth that had a substantially different environment than is found at present.[http://mic.sgmjournals.org/cgi/content/full/148/1/21?view=long&pmid=11782495] These life forms possessed the basic traits of self-replication and inheritable traits. Once life had appeared, the process of [[evolution]] by [[natural selection]] resulted in the formation of ever-more diverse life forms.
  
Species that were unable to adapt to the changing environment and competition from other life forms became extinct. However, the [[fossil]] record retains evidence of many of these older species. Current fossil and [[DNA]] evidence shows that all existing species can trace a continual ancestry back to the first primitive life forms.<ref name=Line/>
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Species that were unable to adapt to the changing environment and competition from other life forms became extinct. However, the [[fossil]] record retains evidence of many of these older species. Current fossil and [[DNA]] evidence shows that all existing species can trace a continual ancestry back to the first primitive life forms.
  
The advent of [[photosynthesis]] in very basic forms of plant life worldwide allowed the sun's energy to be harvested to create conditions allowing for more complex life. The resultant [[oxygen]] accumulated in the atmosphere and gave rise to the [[ozone layer]]. The incorporation of smaller cells within larger ones resulted in the [[endosymbiotic theory|development of yet more complex cells]] called [[eukaryotes]].<ref>{{cite journal |first=L. V. |last=Berkner |coauthors=L. C. Marshall |year=1965 |month=May |title=On the Origin and Rise of Oxygen Concentration in the Earth's Atmosphere |journal=Journal of the Atmospheric Sciences |volume=22 |issue=3 |pages=pp. 225–261 |url=http://ams.allenpress.com/perlserv/?request=get-abstract&doi=10.1175%2F1520-0469(1965)022%3C0225:OTOARO%3E2.0.CO%3B2 }}</ref> Cells within colonies became increasingly specialized, resulting in true multicellular organisms. With the ozone layer absorbing harmful [[ultraviolet radiation]], life colonized the surface of Earth.
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The advent of [[photosynthesis]] in very basic forms of plant life worldwide allowed the sun's energy to be harvested to create conditions allowing for more complex life. The resultant [[oxygen]] accumulated in the atmosphere and gave rise to the [[ozone layer]]. The incorporation of smaller cells within larger ones resulted in the [[endosymbiotic theory|development of yet more complex cells]] called [[eukaryotes]].[http://ams.allenpress.com/perlserv/?request=get-abstract&doi=10.1175%2F1520-0469(1965)022%3C0225:OTOARO%3E2.0.CO%3B2Cells within colonies became increasingly specialized, resulting in true multicellular organisms. With the ozone layer absorbing harmful [[ultraviolet radiation]], life colonized the surface of Earth.
  
 
===Microbes===
 
===Microbes===
{{main|Microbe}}
 
The first form of life to develop on the Earth were microbes, and they remained the only form of life on the planet until about a billion years ago when multi-cellular organisms began to appear.<ref>{{cite journal |
 
author = Schopf J | title = Disparate rates, differing fates: tempo and mode of evolution changed from the Precambrian to the Phanerozoic. | url=http://www.pubmedcentral.nih.gov/picrender.fcgi?artid=44277&blobtype=pdf | journal = Proc Natl Acad Sci U S A | volume = 91 | issue = 15 | format=PDF | pages = 6735-42 | year = 1994 | id = PMID 8041691}}</ref> Microorganisms are single-celled organisms that are generally smaller than the human eye can see. They include Bacteria, Fungi, Archaea and Protista.
 
  
These life forms are found in almost every location on the Earth where there is liquid water, including the interior of rocks within the planet.<ref>{{cite journal | author = Szewzyk U, Szewzyk R, Stenström T | title = Thermophilic, anaerobic bacteria isolated from a deep borehole in granite in Sweden. | url=http://www.pnas.org/cgi/reprint/91/5/1810 | journal = Proc Natl Acad Sci U S A | volume = 91 | issue = 5 | pages = 1810-3 | year = 1994 | id = PMID 11607462}}</ref>
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The first form of life to develop on the Earth were microbes, and they remained the only form of life on the planet until about a billion years ago when multi-cellular organisms began to appear.[http://www.pubmedcentral.nih.gov/picrender.fcgi?artid=44277&blobtype=pdf] Microorganisms are single-celled organisms that are generally smaller than the human eye can see. They include Bacteria, Fungi, Archaea and Protista.
Their reproduction is both rapid and profuse. The combination of a high mutation rate and a [[horizontal gene transfer]]<ref>{{cite journal | author = Wolska K | title = Horizontal DNA transfer between bacteria in the environment. | journal = Acta Microbiol Pol | volume = 52 | issue = 3 | pages = 233-43 | year = 2003 | id = PMID 14743976}}</ref> ability makes them highly adaptable, and able to survive in new environments, including [[outer space]].<ref>{{cite journal | author = Horneck G | title = Survival of microorganisms in space: a review. | journal = Adv Space Res | volume = 1 | issue = 14 | pages = 39-48 | year = 1981 | id = PMID 11541716}}</ref>  They form an essential part of the planetary ecosystem. However some microorganisms are [[pathogenic]] and can post health risk to other organisms.
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These life forms are found in almost every location on the Earth where there is liquid water, including the interior of rocks within the planet.[http://www.pnas.org/cgi/reprint/91/5/1810]
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Their reproduction is both rapid and profuse. The combination of a high mutation rate and a [[horizontal gene transfer]] They form an essential part of the planetary ecosystem. However some microorganisms are [[pathogenic]] and can post health risk to other organisms.
  
 
===Plants and animals===
 
===Plants and animals===
  
The distinction between plant and animal life is not sharply drawn, with some categories of life that stand between or across the two. Originally [[Aristotle]] divided all living things between plants, which generally do not move, and animals. In [[Carolus Linnaeus|Linnaeus]]' system, these became the [[kingdom (biology)|Kingdoms]] [[Vegetabilia]] (later [[Plantae]]) and [[Animal]]ia. Since then, it has become clear that the Plantae as originally defined included several unrelated groups, and the [[fungus|fungi]] and several groups of [[alga]]e were removed to new kingdoms. However, these are still often considered plants in many contexts. Bacterial life is sometimes included in flora,<ref>{{cite web |title=flora |url=http://webster.com/cgi-bin/dictionary?va=flora |work=Merriam-Webster Online Dictionary |publisher=Merriam-Webster |accessmonthday=September 27|accessyear=2006 }}</ref><ref>{{cite book |year=1998 |title=Status and Trends of the Nation's Biological Resources |chapter=Glossary |chapterurl=http://biology.usgs.gov/s+t/SNT/noframe/zy198.htm#F |publisher=Department of the Interior, Geological Survey |location=Reston, VA |id=SuDocs No. I 19.202:ST 1/V.1-2}}</ref> and some classifications use the term ''bacterial flora'' separately from ''plant flora''.
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The distinction between plant and animal life is not sharply drawn, with some categories of life that stand between or across the two. Originally [[Aristotle]] divided all living things between plants, which generally do not move, and animals. In [[Carolus Linnaeus|Linnaeus]]' system, these became the [[kingdom (biology)|Kingdoms]] [[Vegetabilia]] (later [[Plantae]]) and [[Animal]]ia. Since then, it has become clear that the Plantae as originally defined included several unrelated groups, and the [[fungus|fungi]] and several groups of [[alga]]e were removed to new kingdoms. However, these are still often considered plants in many contexts. Bacterial life is sometimes included in flora,[http://webster.com/cgi-bin/dictionary?va=flora] [http://biology.usgs.gov/s+t/SNT/noframe/zy198.htm#F] and some classifications use the term ''bacterial flora'' separately from ''plant flora''.
  
 
Among the many ways of classifying [[plants]] are by regional [[flora]]s, which, depending on the purpose of study, can also include  ''fossil flora'', remnants of plant life from a previous era. People in many regions and countries take great pride in their individual arrays of characteristic flora, which can vary widely across the globe due to differences in climate and [[terrain]].
 
Among the many ways of classifying [[plants]] are by regional [[flora]]s, which, depending on the purpose of study, can also include  ''fossil flora'', remnants of plant life from a previous era. People in many regions and countries take great pride in their individual arrays of characteristic flora, which can vary widely across the globe due to differences in climate and [[terrain]].
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[[Animals]] as a category have several characteristics that generally set them apart from other living things, though not traced by scientists to having legs or wings instead of roots and leaves.  Animals are [[eukaryote|eukaryotic]] and usually [[multicellular]] (although see [[Myxozoa]]), which separates them from [[bacteria]], [[archaea]] and most [[protist]]s.  They are [[heterotroph]]ic, generally digesting food in an internal chamber, which separates them from [[plant]]s and [[alga]]e. They are also distinguished from plants, algae, and [[fungus|fungi]] by lacking [[cell wall]]s.
 
[[Animals]] as a category have several characteristics that generally set them apart from other living things, though not traced by scientists to having legs or wings instead of roots and leaves.  Animals are [[eukaryote|eukaryotic]] and usually [[multicellular]] (although see [[Myxozoa]]), which separates them from [[bacteria]], [[archaea]] and most [[protist]]s.  They are [[heterotroph]]ic, generally digesting food in an internal chamber, which separates them from [[plant]]s and [[alga]]e. They are also distinguished from plants, algae, and [[fungus|fungi]] by lacking [[cell wall]]s.
  
With a few exceptions, most notably the [[sea sponge|sponge]]s (Phylum Porifera), animals have bodies differen­tiated into separate [[biological tissue|tissues]]. These include [[muscle]]s, which are able to contract and control locomotion, and a [[nervous system]], which sends and processes signals. There is also typically an internal [[digestion|digestive]] chamber. The eukaryotic cells possessed by all animals are surrounded by a characteristic extracellular matrix composed of [[collagen]] and elastic [[glycoprotein]]s. This may be calcified to form structures like [[Animal shell|shell]]s, [[bone]]s, and [[spicule]]s, a framework upon which cells can move about and be reorganized during development and maturation, and which supports the complex anatomy required for mobility.  
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With a few exceptions, most notably the [[sea sponge|sponge]]s (Phylum Porifera), animals have bodies differen­tiated into separate [[biological tissue|tissues]]. These include [[muscle]]s, which are able to contract and control locomotion, and a [[nervous system]], which sends and processes signals. There is also typically an internal [[digestion|digestive]] chamber. The eukaryotic cells possessed by all animals are surrounded by a characteristic extracellular matrix composed of [[collagen]] and elastic [[glycoprotein]]s. This may be calcified to form structures like [[Animal shell|shell]]s, [[bone]]s, and [[spicule]]s, a framework upon which cells can move about and be reorganized during development and maturation, and which supports the complex anatomy required for mobility.
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[[Category: Biology]]
  
 
==Ecosystems==
 
==Ecosystems==

Revision as of 17:41, 31 December 2007

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Nature.jpg

Nature, in the broadest sense, is equivalent to the natural world, physical universe, material world or material universe. "Nature" refers to the phenomena of the physical world, and also to life in general. The term generally does not include manufactured objects and human interaction unless qualified in ways such as, e.g., "human nature" or "the whole of nature". Nature is also generally distinguished from the supernatural. It ranges in scale from the subatomic to the galactic.

Etymology

The word "nature" is derived from the Latin word natura, or "the course of things, natural character."[1] Natura was a Latin translation of the Greek word physis (φύσις), which originally related to the intrinsic characteristics that plants, animals, and other features of the world develop of their own accord. A useful though somewhat erratically presented account of the pre-Socratic use of the concept of φύσις may be found in Naddaf, Gerard The Greek Concept of Nature, SUNY Press, 2006. The word φύσις, while first used in connection with a plant in Homer (as we have seen), occurs very early in Greek philosophy, and in several senses. Generally, these senses match rather well the current senses in which the English word nature is used, as confirmed by Guthrie, W.K.C. Presocratic Tradition from Parmenides to Democritus (volume 2 of his History of Greek Philosophy, Cambridge UP, 1965). This is shown in the first written use of the word φύσις, in connection with a plant. The first known use of physis was by Homer in reference to the intrinsic qualities of a plant: ὣς ἄρα φωνήσας πόρε φάρμακον ἀργεϊφόντης ἐκ γαίης ἐρύσας, καί μοι φύσιν αὐτοῦ ἔδειξε. (So saying, Argeiphontes [=Hermes] gave me the herb, drawing it from the ground, and showed me its nature.) Odyssey 10.302-3 (ed. A.T. Murray). (The word is dealt with thoroughly in Liddell and Scott's Greek Lexicon.) For later but still very early Greek uses of the term, see related below. The concept of nature as a whole, the physical universe, is one of several expansions of the original notion; it began with certain core applications of the word φύσις by pre-Socratic philosophers, and has steadily gained currency ever since. This usage was confirmed during the advent of modern scientific method in the last several centuries. Isaac Newton's Philosophiae Naturalis Principia Mathematica (1687), for example, is translated "Mathematical Principles of Natural Philosophy", and reflects the then-current use of the words "natural philosophy", akin to "systematic study of nature." The etymology of the word "physical" shows its use as a synonym for "natural" in about the mid-15th century: [2]

Within the various uses of the word today, "nature" may refer to the general realm of various types of living plants and animals, and in some cases to the processes associated with inanimate objects; the way that particular types of things exist and change of their own accord, such as the weather and geology of the Earth, and the matter and energy of which all these things are composed. It is often taken to mean the "natural environment" or wilderness; wild animals, rocks, forest, beaches, and in general those things that have not been substantially altered by human intervention, or which persist despite human intervention. This more traditional concept of natural things which can still be found today implies a distinction between the natural and the artificial, with the latter being understood as that which has been brought into being by a human or human-like consciousness or mind.

Earth

Earth (or, "the earth") is the fifth largest planet in the solar system, third in order of distance from the Sun. It is the largest of its planetary system's terrestrial planets and the only place in the universe known to support life.

The most prominent features of the earth's climate are its two large polar regions, two relatively narrow temperate zones, and a wide equatorial tropical to subtropical region. An excellent summary description of global climate can be found at:[3] Precipitation patterns vary widely according to location, ranging from several metres of water per year to less than a millimetre. About 70 percent of the surface is covered by salt-water oceans. The remainder consists of continents and islands, with the vast majority of the inhabited land in the Northern Hemisphere.

Earth has evolved through geological and biological processes that have left traces of the original conditions. The outer surface is divided into several tectonic plates that gradually migrate across the surface over geologic time spans, which at least several times have changed relatively quickly. The interior of the planet remains active, with a thick layer of molten Earth mantle and an iron-filled core that generates a magnetic field.

The atmospheric conditions have been significantly altered from the original conditions by the presence of life forms, [4] which create an ecological balance that stabilizes the surface conditions. Despite the wide regional variations in climate by latitude and other geographic factors, the long-term average global climate is quite stable during interglacial periods,[5] and variations of a degree or two of average global temperature have historically had major effects on the ecological balance, and on the actual geography of the Earth.[6] [7]

Historical perspective

Based on the available evidence, scientists have reconstructed detailed information about the planet's past. Earth is estimated to have formed approximately 4.55 billion years ago out of the solar nebula, along with the Sun and other planets. (The Age of the Earth, ISBN 0-8047-1569-6) The moon formed relatively soon afterwards (roughly 20 million years later, or 4.53 billion years ago).

Initially molten, the outer layer of the planet cooled, resulting in the solid crust. Outgassing and volcanic activity produced the primordial atmosphere. Condensing water vapor, augmented by ice delivered by comets, produced the oceans.[8] The highly energetic chemistry is believed to have produced a self-replicating molecule around 4 billion years ago. [9]

Continents formed, then broke up and re-formed as the surface of Earth reshaped itself over the course of hundreds of millions of years, occasionally combining to make a supercontinent. Roughly 750 million years ago, the earliest known supercontinent Rodinia, began to break apart. The continents later recombined to form Pannotia which broke apart about 540 million years ago, then finally Pangaea, which broke apart about 180 million years ago.[10]

There is significant evidence, still being discussed among scientists, that a severe glacial action during the Neoproterozoic era covered much of the planet in a sheet of ice. This hypothesis has been termed the "Snowball Earth", and it is of particular interest as it precedes the Cambrian explosion in which multicellular life forms began to proliferate about 530-540 million years ago.[11] ISBN 0-521-36615-1

Since the Cambrian explosion there have been five distinctly identifiable mass extinctions. The last mass extinction occurred some 65 million years ago, when a meteorite collision probably triggered the extinction of the non-avian dinosaurs and other large reptiles, but spared small animals such as mammals, which then resembled shrews. Over the past 65 million years, mammalian life diversified. ISBN 0-684-81326-2

Several million years ago, a species of small African ape gained the ability to stand upright.Cite error: Closing </ref> missing for <ref> tag]] Template:Main All forms of life interact with the environment in which they exist, and also with other life forms. In the 20th century this premise gave rise to the concept of ecosystems, which can be defined as any situation where there is interaction between organisms and their environment.

Ecosystems are composed of a variety of abiotic and biotic components that function in an interrelated way.[1] The structure and composition is determined by various environmental factors that are interrelated. Variations of these factors will initiate dynamic modifications to the ecosystem. Some of the more important components are: soil, atmosphere, radiation from the sun, water, and living organisms.

Each living organism has a continual relationship with every other element that makes up its environment. Within the ecosystem, species are connected and dependent upon one another in the food chain, and exchange energy and matter between themselves as well as with their environment.[2]

Every species has limits of tolerance to factors that affect its survival, reproductive success and ability to continue to thrive and interact sustainably with the rest of its environment, which in turn may have effects on these factors for many other species or even on the whole of life.[3] The concept of an ecosystem is thus an important subject of study, as such study provides information needed to make decisions about how human life may interact in a way that allows the various ecosystems to be sustained for future use rather than used up or otherwise rendered ineffective. For the purpose of such study, a unit of smaller size is called a microecosystem. For example, an ecosystem can be a stone and all the life under it. A macroecosystem might involve a whole ecoregion, with its drainage basin.[4]

The following ecosystems are examples of the kinds currently under intensive study:

Another classification can be made by reference to its communities, such as in the case of a human ecosystem. Regional groupings of distinctive plant and animals best adapted to the region's physical natural environment, latitude, altitude, and terrain are known as biomes. The broadest classification, today under wide study and analysis, and also subject to widespread arguments about its nature and validity, is that of the entire sum of life seen as analogous to a self-sustaining organism; a theory studied as earth system science (less formally known as Gaia theory).[5][6]

Human interrelationship

Although humans currently comprise only about one-half of one percent of the total living biomass on Earth,[7] the human effect on nature is disproportionately large. Because of the extent of human influence, the boundaries between what we regard as nature and "made environments" is not clear cut except at the extremes. Even at the extremes, the amount of natural environment that is free of discernible human influence is presently diminishing at an increasingly rapid pace, or, according to some, has already disappeared.

The development of technology by the human race has allowed the greater exploitation of natural resources and has helped to alleviate some of the risk from natural hazards. In spite of this progress, however, the fate of human civilization remains closely linked to changes in the environment. There exists a highly complex feedback-loop between the use of advanced technology and changes to the environment that are only slowly becoming understood.[8] Manmade threats to the Earth's natural environment include pollution, deforestation, and disasters such as oil spills. Humans have contributed to the extinction of many plants and animals.

Humans employ nature for both leisure and economic activities. The acquisition of natural resources for industrial use remains a primary component of the world's economic system. Some activities, such as hunting and fishing, are used for both sustenance and leisure, often by different people. Agriculture was first adopted around the 9th millennium BCE. Ranging from food production to energy, nature influences economic wealth.

Although early humans gathered uncultivated plant materials for food and employed the medicinal properties of vegetation for healing,[9] most modern human use of plants is through agriculture. The clearance of large tracts of land for crop growth has led to a significant reduction in the amount available of forestation and wetlands, resulting in the loss of habitat for many plant and animal species as well as increased erosion.[10]

Wilderness

Wilderness is generally defined as a natural environment on Earth that has not been directly modified by human activity. Ecologists consider wilderness areas to be an integral part of the planet's self-sustaining natural ecosystem (the biosphere).

The word, "wilderness", derives from the notion of wildness; in other words that which is not controllable by humans. The word's etymology is from the Old English wildeornes, which in turn derives from wildeor meaning wild beast (wild + deor = beast, deer).[11] From this point of view, it is the wildness of a place that makes it a wilderness. The mere presence or activity of people does not disqualify an area from being "wilderness." Many ecosystems that are, or have been, inhabited or influenced by activities of people may still be considered "wild." This way of looking at wilderness includes areas within which natural processes operate without very noticeable human interference.

Beauty in nature

Beauty in nature is has long been a common theme in life and in art, and books emphasizing beauty in nature fill large sections of libraries and bookstores. That nature has been depicted and celebrated by so much art, photography, poetry and other literature shows the strength with which many people associate nature and beauty. Why this association exists, and what the association consists of, is studied by the branch of philosophy called aesthetics. Beyond certain basic characteristics that many philosophers agree about to explain what is seen as beautiful, the opinions are virtually endless.[12]

Looked at through the lens of the visual arts, nature and wildness have been important subjects in various epochs of world history. An early tradition of landscape art began in China during the Tang Dynasty (618-907). The tradition of representing nature as it is became one of the aims of Chinese painting and was a significant influence in Asian art. Artists learned to depict mountains and rivers "from the perspective of nature as a whole and on the basis of their understanding of the laws of nature … as if seen through the eyes of a bird." In the 13th century, the Song Dynasty artist Shi Erji listed "scenes lacking any places made inaccessible by nature," as one of the 12 things to avoid in painting.[13]

In the Western world the idea of wilderness having intrinsic value emerged in the 1800s, especially in the works of the Romantic movement. British artists John Constable and JMW Turner turned their attention to capturing the beauty of the natural world in their paintings. Before that, paintings had been primarily of religious scenes or of human beings. William Wordsworth’s poetry described the wonder of the natural world, which had formerly been viewed as a threatening place. Increasingly the valuing of nature became an aspect of Western culture.[14] This artistic movement also coincided with the Transcendentalist movement in the Western world.

Many scientists, who study nature in more specific and organized ways, also share the conviction that nature is beautiful; the French mathematician, Jules Henri Poincaré (1854-1912) said:

The scientist does not study nature because it is useful; he studies it because he delights in it, and he delights in it because it is beautiful.
If nature were not beautiful, it would not be worth knowing, and if nature were not worth knowing, life would not be worth living. Of course I do not here speak of that beauty which strikes the senses, the beauty of qualities and of appearance; not that I undervalue such beauty, far from it, but it has nothing to do with science; I mean that profounder beauty which comes from the harmonious order of the parts and which a pure intelligence can grasp.[15]

A common classical idea of beautiful art involves the word mimesis, the imitation of nature. Also in the realm of ideas about beauty in nature is that the perfect is implied through symmetry, equal division, and other perfect mathematical forms and notions.

Matter and energy

Some fields of science see nature as matter in motion, obeying certain laws of nature which science seeks to understand. For this reason the most fundamental science is generally understood to be "physics"—the name for which is still recognizable as meaning that it is the study of nature.

Matter is commonly defined as the substance of which physical objects are composed. It constitutes the observable universe. According to the theory of special relativity, there is no unchangeable distinction between matter and energy, because matter can be converted to energy (see annihilation), and vice versa (see matter creation). The visible components of the universe are now believed to compose only 4 percent of the total mass. The remainder is believed to consist of 23 percent cold dark matter and 73 percent dark energy.[16] The exact nature of these components is still unknown and is currently under intensive investigation by physicists.

The behavior of matter and energy throughout the observable universe appears to follow well-defined physical laws. These laws have been employed to produce cosmological models that successfully explain the structure and the evolution of the universe we can observe. The mathematical expressions of the laws of physics employ a set of twenty physical constants[17] that appear to be static across the observable universe.[18] The values of these constants have been carefully measured, but the reason for their specific values remains a mystery.

Nature beyond Earth

Outer space, also simply called space, refers to the relatively empty regions of the universe outside the atmospheres of celestial bodies. Outer space is used to distinguish it from airspace (and terrestrial locations). There is no discrete boundary between the Earth's atmosphere and space, as the atmosphere gradually attenuates with increasing altitude. Outer space within the solar system is called interplanetary space, which passes over into interstellar space at what is known as the heliopause.

Outer space is certainly spacious, but it is far from empty. Outer space is sparsely filled with several dozen types of organic molecules discovered to date by microwave spectroscopy, blackbody radiation left over from the big bang and the origin of the universe, and cosmic rays, which include ionized atomic nuclei and various subatomic particles. There is also some gas, plasma and dust, and small meteors. Additionally, there are signs of human life in outer space today, such as material left over from previous manned and unmanned launches which are a potential hazard to spacecraft. Some of this debris re-enters the atmosphere periodically.

Although the planet Earth is currently the only known body within the solar system to support life, current evidence suggests that in the distant past the planet Mars possessed bodies of liquid water on the surface.[19] For a brief period in Mars' history, it may have also been capable of forming life. At present though, most of the water remaining on Mars is frozen. If life exists at all on Mars, it is most likely to be located underground where liquid water can still exist.[20]

Conditions on the other terrestrial planets, Mercury and Venus, appears to be too harsh to support life as we know it. But it has been conjectured that Europa, the fourth-largest moon of Jupiter, may possess a sub-surface ocean of liquid water and could potentially host life.[21]

Recently, the team of Stéphane Udry have discovered a new planet named Gliese 581 c, which is an extrasolar planet orbiting the red dwarf star Gliese 581. Gliese 581 c appears to lay in the habitable zone of space surrounding the star, and therefore could possibly host life as we know it.

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  1. Template:Cite web
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  3. Template:Cite web esp. section on "Abiotic Factors and Tolerance Limits."
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  7. For an example of a range of opinions, see: Template:Cite web and Ralph Waldo Emerson's analysis of the subject: Template:Cite book
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  11. "Wilderness", in The Collins English Dictionary (2000)
  12. For an example of a range of opinions, see: Template:Cite web and Ralph Waldo Emerson's analysis of the subject: Template:Cite book
  13. Chinese brush painting Asia-art.net Accessed: May 20, 2006.
  14. History of Conservation BC Spaces for Nature. Accessed: May 20, 2006.
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  21. Template:Cite web