Difference between revisions of "Greenhouse gas regulation"
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− | {{Definition|title= Greenhouse gas regulation|definition = The balance and maintenance of the chemical composition of the atmosphere and oceans by maine living organisms | + | |
+ | {{Definition|title= Greenhouse gas regulation|definition = The balance and maintenance of the chemical composition of the atmosphere and oceans by maine living organisms<ref name=B>Beaumont, N.J.; Austen, M.C.; Atkins, J.P.; Burdon, D.; Degraer, S.; Dentinho, T.P.; Derous, S.; Holm, P.; Horton, T.; van Ierland, E.; Marboe, A.H.; Starkey, D.J.; Townsend, M.; Zarzycki, T. (2007). Identification, definition and quantification of goods and services provided by marine biodiversity: implications for the ecosystem approach. Mar. Pollut. Bull. 54(3): 253-265 </ref>.}} | ||
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+ | Marine ecosystems are an important regulator of the global CO<sub>2</sub>/O<sub>2</sub> (carbon dioxide/oxygen) balance. The biogeochemical cycling of these gases is greatly controlled by the living biota existing on earth of which the marine realm is extremely important. For example, marine plants and animals aid in controlling carbon dioxide in the ocean, as phytoplankton remove it from the surface waters while releasing oxygen. When phytoplankton die, they sink and add to the supersaturation of carbon dioxide in the deep sea. This results in a vertical gradient of CO<sub>2</sub> in the ocean, which has been termed the 'Biological Pump'. See [[Algal bloom dynamics]] for further details. | ||
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+ | Greenhouse gas regulation is vital in regulating the climate of our planet. The seabed has a significant role in this process through its ability to sequester CO<sub>2</sub>. Gases such as CO<sub>2</sub> in the atmosphere traps heat from the sun, heating the planet. This process occurs naturally and has kept the Earth's temperature about 60 degrees Fahrenheit warmer than it would otherwise be. Excessive amounts of gases such as atmospheric CO<sub>2</sub>, however, can have a significant contribution to global warming and is thus a factor in regulating climate<ref name=B/>. | ||
==References== | ==References== | ||
<references/> | <references/> | ||
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+ | [[Category:Climate change, impacts and adaptation]] |
Revision as of 11:35, 31 July 2020
Definition of Greenhouse gas regulation:
The balance and maintenance of the chemical composition of the atmosphere and oceans by maine living organisms[1].
This is the common definition for Greenhouse gas regulation, other definitions can be discussed in the article
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Marine ecosystems are an important regulator of the global CO2/O2 (carbon dioxide/oxygen) balance. The biogeochemical cycling of these gases is greatly controlled by the living biota existing on earth of which the marine realm is extremely important. For example, marine plants and animals aid in controlling carbon dioxide in the ocean, as phytoplankton remove it from the surface waters while releasing oxygen. When phytoplankton die, they sink and add to the supersaturation of carbon dioxide in the deep sea. This results in a vertical gradient of CO2 in the ocean, which has been termed the 'Biological Pump'. See Algal bloom dynamics for further details.
Greenhouse gas regulation is vital in regulating the climate of our planet. The seabed has a significant role in this process through its ability to sequester CO2. Gases such as CO2 in the atmosphere traps heat from the sun, heating the planet. This process occurs naturally and has kept the Earth's temperature about 60 degrees Fahrenheit warmer than it would otherwise be. Excessive amounts of gases such as atmospheric CO2, however, can have a significant contribution to global warming and is thus a factor in regulating climate[1].
References
- ↑ 1.0 1.1 Beaumont, N.J.; Austen, M.C.; Atkins, J.P.; Burdon, D.; Degraer, S.; Dentinho, T.P.; Derous, S.; Holm, P.; Horton, T.; van Ierland, E.; Marboe, A.H.; Starkey, D.J.; Townsend, M.; Zarzycki, T. (2007). Identification, definition and quantification of goods and services provided by marine biodiversity: implications for the ecosystem approach. Mar. Pollut. Bull. 54(3): 253-265