Mosses helped enrich early Earth with oxygen
Oxygen in its current form first appeared in Earth’s atmosphere some 2.4 billion years ago, in an incident known as the Great Oxidation Event. However, it was not until roughly 400 million years ago that this vital compound first approached modern levels in the atmosphere. This shift steered the trajectory of life on Earth and researchers have long debated how oxygen rose to modern concentrations.
In a study published in the journal Proceedings of the National Academy of Sciences, Professor Tim Lenton, of the University of Exeter, and his colleagues theorised that the earliest land plants, which colonised the land from 470 million years ago onwards, are responsible for the levels of oxygen that sustains our lives today. Their emergence and evolution permanently increased the flux of organic carbon into sedimentary rocks, the primary source for atmospheric oxygen, thus driving up oxygen levels in a second oxygenation event and establishing a new, stable oxygen cycle.
Earth’s early plant biosphere consisted of simple bryophytes, such as moss, which are non-vascular – meaning they do not have vein-like systems to conduct water and minerals around the plant. Using computer simulations, the researchers first estimated that these plants could have generated roughly 30% of today’s global terrestrial net primary productivity by about 445 million years ago.
When the properties of modern bryophytes were taken into account, including their elemental composition and effects on rock weathering, they found that modern levels of atmospheric oxygen were achieved by 420 to 400 million years ago, consistent with independent evidence.
These findings therefore suggest that the first land plants, such as the humble moss, created the stable oxygen-rich atmosphere that allowed large, mobile, intelligent animal life, including humans, to evolve.
Professor Tim Lenton, of the University of Exeter, said: “It’s exciting to think that without the evolution of the humble moss, none of us would be here today. Our research suggests that the earliest land plants were surprisingly productive and caused a major rise in the oxygen content of the Earth’s atmosphere.”
Article #16-04787: “Earliest land plants created modern levels of atmospheric oxygen” by Timothy M. Lenton et al.
The research was funded by the Leverhulme Trust, the Natural Environment Research Council, a Royal Society Wolfson Merit Award, and the VILLUM Foundation. It involved collaboration from the University of Leeds, the University of Copenhagen, the Georgia Institute of Technology, Ohio State University and Stockholm University.