Carbon dioxide is an important trace gas in
Earth's atmosphere currently constituting about 0.04% (400 parts per million) of the atmosphere. Despite its relatively small concentration, is a potent
greenhouse gas and plays a vital role in regulating
Earth's surface temperature through
radiative forcing and the
greenhouse effect. Reconstructions show that concentrations of in the atmosphere have varied, ranging from as high as 7,000 parts per million during the
Cambrian period about 500 million years ago to as low as 180 parts per million during the
Quaternary glaciation of the last two million years.