Ancient Oxygen Levels Correlate With Animal Evolution
A paper in this week's Science correlates rise in atmospheric oxygen with the evolution of large placental animals.
The concluding paragraph of the paper states:
Continue ReadingThe data presented here provide evidence of a secular increase in atmospheric oxygen over the past 205 My that broadly corresponds with three main aspects of vertebrate evolution, namely endothermy, placentation, and size. Particularly notable are high stable O2 levels during the time of placental mammal origins and diversification and a close correspondence between marked increases in both atmospheric oxygen levels and mammalian body size during the early to middle Eocene. Although increases in mammalian body size, morphological disparity, and inferred ecological heterogeneity during this interval may have been influenced as well by other environmental factors such as warm global temperatures and the spread of tropical and subtropical habitats, the correlation between evolutionary changes in mammalian body size and increased atmospheric O2 has a physiological basis related to placental mammal reproduction. The changes in oxygen appear to have been driven by tectonics and increased burial efficiency of organic matter on continental margins.
The correlations are represented in this accompanying figure (click to enlarge):
Here are a few more details from news@nature.com:They have found that the amount of oxygen in the Earth's atmosphere 200 million years ago was only about half what it is today. And the appearance of large placental mammals, around 50 million years ago, happened at the same time as the oxygen level more or less doubled.
This is also about the same time that the Atlantic Ocean opened up: a supercontinent split into the Americas, Africa and Eurasia, creating the ocean between them.
This continental movement created thousands of kilometres of coastline that helped to wash organic carbon into the sea, locking it away from the process of decay. Because such carbon escapes chemical processes that would turn it into carbon dioxide, the more carbon is washed away, the more oxygen remains in the atmosphere...
Placental mammals began to appear at the end of the Cretaceous, but they were small, rodent-sized creatures. "We don't really see large mammals until the Eocene," says Falkowski.
This, he suggests, was made possible by the sudden oxygen rise at that time. Large mammals have a lower density of capillaries than small mammals, so they can only distribute oxygen around their bodies efficiently if there is a lot of oxygen in the air. Placental reproduction also needs a lot of ambient oxygen, because only a small proportion of that in the mother's blood reaches the fetus.