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Review key Carbon Sinks: Natural Reservoirs, Carbon Cycle and Climate Mitigation exam facts and rate your mastery to track revision.
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#1
A carbon sink is any reservoir, natural or artificial, that absorbs more carbon dioxide from the atmosphere than it releases.
#2
The global carbon cycle maintains dynamic equilibrium across four spheres: atmosphere, biosphere, hydrosphere, and lithosphere.
#3
Earth's oceans are the largest active natural carbon sink, absorbing roughly 25 to 30 percent of anthropogenic CO2 emissions.
#4
The oceanic solubility pump dissolves atmospheric carbon dioxide in cold, dense polar waters that sink into deep abyssal layers.
#5
The oceanic biological pump relies on photosynthetic marine phytoplankton to convert dissolved inorganic carbon into organic matter.
#6
When marine organisms with calcium carbonate shells die, their remains settle on the seabed, forming deep carbonate sediments.
#7
Ocean carbon absorption forms carbonic acid, driving ocean acidification and lowering the pH of marine surface waters.
#8
Terrestrial forests act as major biological carbon sinks by converting atmospheric CO2 into plant biomass via photosynthesis.
#9
Carbon is stored long-term in aboveground tree trunks, branches, root systems, and underground soil organic matter.
#10
Boreal forests (taiga) store vast quantities of carbon in cold, slow-decaying forest floor humus and underlying permafrost soils.
#11
Peatlands cover only 3 percent of Earth's land surface but store roughly 30 percent of all soil carbon, surpassing global forest biomass.
#12
Waterlogged, anaerobic conditions in peatlands prevent microbial decomposition, locking undecayed plant carbon for millennia.
#13
Blue carbon refers to carbon sequestered and stored by marine and coastal ecosystems, including mangroves, seagrasses, and salt marshes.
#14
Mangrove forests can sequester carbon up to 10 times faster per unit area than mature terrestrial tropical rainforests.
#15
Soil organic carbon (SOC) represents the largest terrestrial organic carbon pool, holding three times more carbon than the atmosphere.
#16
Agricultural practices such as conservation tillage, cover cropping, and agroforestry increase soil carbon sequestration capacity.
#17
A carbon sink becomes a net carbon source when disturbances such as deforestation, draining of wetlands, or wildfires release stored carbon.
#18
Thawing Arctic permafrost risks releasing gigatons of trapped methane and carbon dioxide into the atmosphere, creating a feedback loop.
#19
Article 5 of the UNFCCC Paris Agreement explicitly obligates signatory nations to conserve and enhance carbon sinks and reservoirs.
#20
Artificial carbon sinks include Carbon Capture and Storage (CCS) systems that inject captured CO2 into deep geological rock formations.
Subject Specialist Commentary
Analytical perspective & practical exam advice from the Master10 academic board
A carbon sink is any natural or artificial system that absorbs and stores more carbon dioxide from the atmosphere than it emits. Oceans represent the planet's largest active sink, soaking up vast amounts of carbon through chemical dissolution and marine phytoplankton. On land, growing forests, healthy soils, and coastal wetlands act as vital biological storehouses. By trapping atmospheric greenhouse gases for decades or millennia, these ecosystems slow down global warming and help stabilize Earth's climate system.
For UPSC Prelims and environmental studies exams, focus on the ecological distinction between green and blue carbon. Blue carbon refers to coastal marine ecosystems like mangroves, seagrasses, and salt marshes, which can sequester carbon up to ten times faster per hectare than terrestrial tropical rainforests. A favorite exam trap overlooks peatlands: despite covering only three percent of global land, waterlogged peatlands store thirty percent of all soil carbon. Remember that degraded sinks can flip into carbon sources through wildfires and deforestation.
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