Essential Concepts & Key Facts
High-yield conceptual summaries for competitive exams and rapid revision.
- A carbon sink is any reservoir, natural or artificial, that absorbs more carbon dioxide from the atmosphere than it releases.
- The global carbon cycle maintains dynamic equilibrium across four spheres: atmosphere, biosphere, hydrosphere, and lithosphere.
- Earth's oceans are the largest active natural carbon sink, absorbing roughly 25 to 30 percent of anthropogenic CO2 emissions.
- The oceanic solubility pump dissolves atmospheric carbon dioxide in cold, dense polar waters that sink into deep abyssal layers.
- The oceanic biological pump relies on photosynthetic marine phytoplankton to convert dissolved inorganic carbon into organic matter.
- When marine organisms with calcium carbonate shells die, their remains settle on the seabed, forming deep carbonate sediments.
- Ocean carbon absorption forms carbonic acid, driving ocean acidification and lowering the pH of marine surface waters.
- Terrestrial forests act as major biological carbon sinks by converting atmospheric CO2 into plant biomass via photosynthesis.
- Carbon is stored long-term in aboveground tree trunks, branches, root systems, and underground soil organic matter.
- Boreal forests (taiga) store vast quantities of carbon in cold, slow-decaying forest floor humus and underlying permafrost soils.
- Peatlands cover only 3 percent of Earth's land surface but store roughly 30 percent of all soil carbon, surpassing global forest biomass.
- Waterlogged, anaerobic conditions in peatlands prevent microbial decomposition, locking undecayed plant carbon for millennia.
- Blue carbon refers to carbon sequestered and stored by marine and coastal ecosystems, including mangroves, seagrasses, and salt marshes.
- Mangrove forests can sequester carbon up to 10 times faster per unit area than mature terrestrial tropical rainforests.
- Soil organic carbon (SOC) represents the largest terrestrial organic carbon pool, holding three times more carbon than the atmosphere.
- Agricultural practices such as conservation tillage, cover cropping, and agroforestry increase soil carbon sequestration capacity.
- A carbon sink becomes a net carbon source when disturbances such as deforestation, draining of wetlands, or wildfires release stored carbon.
- Thawing Arctic permafrost risks releasing gigatons of trapped methane and carbon dioxide into the atmosphere, creating a feedback loop.
- Article 5 of the UNFCCC Paris Agreement explicitly obligates signatory nations to conserve and enhance carbon sinks and reservoirs.
- Artificial carbon sinks include Carbon Capture and Storage (CCS) systems that inject captured CO2 into deep geological rock formations.
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