Current estimations of the carbon cycle allude to an unbalanced model of the exchange of carbon throughout observed reservoirs. Since the industrial revolution, we have been unable to compensate for anthropogenic emissions and changes in land use which have impacted the carbon cycle. Throughout the past few decades, scientists observed an increase in the net flux of carbon into atmosphere, but cannot identify a definite sink that would balance the carbon budget as portrayed by most models.
What is the Carbon Cycle?
The carbon cycle refers to the fluxing of the element carbon throughout the carbon-containing reservoirs existing at or near the surface of the earth. The largest reservoir by far is the solid lithosphere, which contains carbon-rich deposits that also share the longest residence time. The next two largest reservoirs are the ocean and the atmosphere. When combined with the lithosphere, they would account for most of the carbon existing on Earth. The biosphere is also an important reservoir, but has been excluded from most fundamental models of the carbon cycle as it can be accounted for by fluxes of carbon to the oceanic and terrestrial reservoirs.
Carbon Flux: Natural and Anthropogenic
There are fluxes of carbon that occur naturally, and then there are also fluxes that originate from human involvement which are called anthropogenic sources. From models based on the carbon cycle, we have agreement up until the time that anthropogenic sources were introduced into the system. This new flux has entered the carbon cycle through the atmosphere, but can not be accounted for.
References
Chester, Roy. Marine Geochemistry Second Edition. Malden, MA: Blackwell Science Ltd. 2000, 2003
Richard Houghton, Senior Scientist, Carbon Research. Understanding the Global Carbon Cycle. Woods Hole Research Center, http://www.whrc.org/carbon/
Hesshaimer, Vago, Heimann, Martin, Levin, Ingeborg. Radiocarbon evidence for a smaller oceanic carbon dioxide sink than previously believed. Nature (London). 370 (6486), p. 201-203, 1994.
Frankignoulle, Michel , Borges, Alberto V. European Continental shelf as a significant sink for atmospheric carbon dioxide. Global Biochemical Cycles. Pages 569-576, September 1, 2001
Houghton, R. A. , Davidson, E. A. , Woodwell, G.M. Missing sinks, feedbacks, and understanding the role of terrestrial ecosystems in the global carbon balance, Global Biochemical Cycles. Vol. 12, No. 1, Pages 25-34, March 1998
Tsunogia, Shizuo , Ono, Tsuneo , Watanabe, Shuichi. Increase in total carbonate in the western North Pacific water and a hypothesis on the missing sink of anthropogenic carbon, Journal of Oceanography, Vol. 49, Pages 305-315, 1993
Burdige, David J. , Alperin, Marc J., Homstead, Juliana, Martens, Christopher S., The role of benthic fluxes of dissolved organic carbon in oceanic and sedimentary carbon cycling. Geophysical Research Letters, Vol.19, Pages 1851-1854, 1992
http://en.wikipedia.org/wiki/Carbon_cycle
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