Final answer:
The carbon cycle is a biogeochemical process that cycles carbon through quick exchanges in living organisms and slower geological processes. The geological cycling includes the dissolution, sedimentation, and fossilization of carbon, taking millions of years. The industrial use of fossil fuels has altered the cycle's balance, increasing atmospheric CO2 levels and contributing to climate change.
Step-by-step explanation:
The carbon cycle involves various processes that recycle carbon through the biotic and abiotic components of ecosystems. There are two interconnected subcycles: a rapid carbon exchange among living organisms and a long-term cycling through geologic processes. While the former is relatively quick, it is the geological aspect of the cycle that is indeed much slower.
Processes like the dissolution of carbon from rocks by running water, which eventually ends up in the ocean, and the settling of carbon in ocean water to the bottom where it can be stores as fossil fuels or sedimentary rocks, can take millions of years. Carbon is stored in various carbon reservoirs including the atmosphere, oceans, ocean sediment, soil, and within the Earth's interior. The use of fossil fuels since the Industrial Revolution has increased atmospheric CO2 levels, contributing to climate change, thus indicating the current environmental impact of disrupting the natural carbon cycle.