By studying modern moss, researchers from the Universities of Exeter and Oxford reveal how the arrival of the first plants 470 million years ago triggered a series of ice ages by causing a dramatic reduction in atmospheric carbon. The research suggests that these plants caused the weathering of rocks and the Earth’s surface, which led to increased quantities of nutrients going into the oceans causing organic carbon burial and decreasing levels of carbon dioxide in the atmosphere.
New research reveals how the arrival of the first plants 470 million years ago triggered a series of ice ages. Led by the Universities of Exeter and Oxford, the study is published in Nature Geoscience.
The team set out to identify the effects that the first land plants had on the climate during the Ordovician Period, which ended 444 million years ago. During this period the climate gradually cooled, leading to a series of ‘ice ages’. This global cooling was caused by a dramatic reduction in atmospheric carbon, which this research now suggests was triggered by the arrival of plants.
Among the first plants to grow on land were the ancestors of mosses that grow today. This study shows that they extracted minerals such as calcium, magnesium, phosphorus, and iron from rocks in order to grow. In so doing, they caused chemical weathering of the Earth’s surface. This had a dramatic impact on the global carbon cycle and subsequently on the climate. It could also have led to a mass extinction of marine life.
The research suggests that the first plants caused the weathering of calcium and magnesium ions from silicate rocks, such as granite, in a process that removed carbon dioxide from the atmosphere, forming new carbonate rocks in the ocean. This cooled global temperatures by around five degrees Celsius.
In addition, by weathering the nutrients phosphorus and iron from rocks, the first plants increased the quantities of both these nutrients going into the oceans, fueling productivity there and causing organic carbon burial. This removed yet more carbon from the atmosphere, further cooling the climate by another two to three degrees Celsius. It could also have had a devastating impact on marine life, leading to a mass extinction that has puzzled scientists.
The team used the modern moss, Physcomitrella patens for their study. They placed a number of rocks, with or without moss growing on them, into incubators. Over three months they were able to measure the effects the moss had on the chemical weathering of the rocks.
They then used an Earth system model to establish what difference plants could have made to climate change during the Ordovician Period.
One of the lead researchers, Professor Tim Lenton of Geography at the University of Exeter said: “This study demonstrates the powerful effects that plants have on our climate. Although plants are still cooling the Earth’s climate by reducing atmospheric carbon levels, they cannot keep up with the speed of today’s human-induced climate change. In fact, it would take millions of years for plants to remove current carbon emissions from the atmosphere.”
Professor Liam Dolan of Oxford University, one of the lead researchers, said: “For me, the most important take-home message is that the invasion of the land by plants – a pivotal time in the history of the planet – brought about huge climate changes. Our discovery emphasizes that plants have a central regulatory role in the control of climate: they did yesterday, they do today and they certainly will in the future.”
Reference: “First plants cooled the Ordovician” by Timothy M. Lenton, Michael Crouch, Martin Johnson, Nuno Pires and Liam Dolan, 1 February 2012, Nature Geoscience.
The study was carried out by a team from the Universities of Exeter, Oxford and East Anglia and the John Innes Center. The research was funded by the Natural Environment Research Council.