Paleobotanical evidence for near present-day levels of atmospheric CO2 during part of the Tertiary
Understanding the link between the greenhouse gas carbon dioxide (CO(2)) and Earth's temperature underpins much of paleoclimatology and our predictions of future global warming. Here, we use the inverse relationship between leaf stomatal indices and the partial pressure of CO(2) in modern Ginkg...
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Veröffentlicht in: | Science (American Association for the Advancement of Science) 2001-06, Vol.292 (5525), p.2310-2313 |
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Sprache: | eng |
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