Work

Atmospheric oxygen over Phanerozoic time

Year: 1999
Type: article
Abstract: It is quite possible that the level of atmospheric oxygen has varied (roughly between 15 and 30% O2) over the past 550 million years. This variation is suggested by modeling of the carbon and sulfur cycles, by the excessive sediment burial of organic matter that accompanied the advent of large vascular land plants, and by recent physiological studies that relate to biological evolution.
Institution: Yale University
Language: English
Subfield: Paleontology
Open Access status: green
OpenAlex ID: W2131731927
FWCI: 4.709
Cites: 40
Cited by: 285
Related to: 9