User:Nataliaalvarez583/Terrestrial biological carbon cycle
 | This is the sandbox page where you will draft your initial Wikipedia contribution.
If you're starting a new article, you can develop it here until it's ready to go live. If you're working on improvements to an existing article, copy only one section at a time of the article to this sandbox to work on, and be sure to use an edit summary linking to the article you copied from. Do not copy over the entire article. You can find additional instructions here. Remember to save your work regularly using the "Publish page" button. (It just means 'save'; it will still be in the sandbox.) You can add bold formatting to your additions to differentiate them from existing content. |
Article Draft- Terrestrial Biological Carbon Cycle (Adding to existing article)[edit]
Atmosphere[edit]
Main article: Atmospheric carbon cycle
Most carbon leaves the terrestrial biosphere through respiration. When oxygen is present, aerobic respiration occurs, producing carbon dioxide. If oxygen is not present, e.g. as is the case in marshes or in animals' digestive tracts, anaerobic respiration can occur, which produces methane. About half of the gross primary production is respired by plants directly back into the atmosphere. Part of the net primary production, or the remaining carbon absorbed by the biosphere, is emitted back into the atmosphere through fires and heterotrophic respiration. The rest is converted into soil organic carbon, which is released more slowly, or "inert" dissolved carbon, which can remain in the biosphere for an unknown period of time.
This can be a very vital aspect to have in life as it will work to promote all kinds of living things to co-exist within an ecosystem. The role of Carbon within a Terrestrial Ecosystem consists of Carbon being stored within plants which will eventually be deposited in other forms for other organisms to absorb and consume.