Carbon Dioxide: Importance, Uses, and Sources


Carbon dioxide (CO2) is one of the very few carbon containing inorganic compounds found in nature. It is the most ubiquitous greenhouse trace gas. Photoautotrophs fix CO2, in a process called photosynthesis, into organic energy forms essential to the c hemoheterotrophs on this planet. However, there may be disadvantages in releasing large quantities of CO2 into the atmosphere, due to its ability to absorb infrared radiation emitted from the Earth.

It has been estimated that 50% to 60% of the anthropogenic greenhouse effect is attributed to this gas. In order to conceptualize our place in the life series of Earth, ice core data from Antarctica indicates CO2 levels ranged from 200 to 300 ppm over the last 160,000 yrs. prior to the industrial revolution. Since 1860 the concentration of CO2 has grow exponentially (Botkin and Keller, 1995).

Continuous measurements of atmospheric CO2 have been made at the Mauna Loa Observatory since 1958 by Scripps Institution of Oceanography. This data demonstrates an upward trend in CO2 levels with seasonal decreases during summer months and increases dur ing winter months (Boden, Kanciruk, and Farrell, 1990).

Questions:

Some additional resources: