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UK scientists claim they now know how Earth recovered on its own from a sudden episode of severe global warming at the time of the dinosaurs.
http://news.bbc.co.uk/2/hi/science/nature/3451787.stm
UK scientists claim they now know how Earth recovered on its own from a sudden episode of severe global warming at the time of the dinosaurs.
From this quote from the storyOriginally posted by Ivan Seeking
http://news.bbc.co.uk/2/hi/science/nature/3451787.stm
Sounds like the Earth created it's own widescale version of TUMS to get rid of the gas.Calcium combined with CO2, for instance, would have caused the precipitation of calcium carbonate. This process of CO2 consumption would have lowered levels of the greenhouse gas on a global scale.
Andre, I looked it over last year, and concluded it'd take me quite some time to come to grips with it sufficiently to post half-way decent questions and challenges. Then I got more interested in other things ... and never got back to it (maybe Nereid is a kind of butterfly?)Originally posted by Andre
Nereid,
Your hints to the mysterous deitic planet suggest that you endorse the wet greenhouse thermal runaway hypothesis for Venus. You're probably also familiar with the hypothesis of the spinning stop of Venus due to atmospheric drag (Correia et al). However, both hypotheses have their weaknesses. One of them being a lack of integration.
Familiar with/interested in Andre's hypothesis of all Venus enigmatic features?
Posted it here about over half a year ago.
Maybe we should give some to that whale of Ivans! Ivan! Where's the picture of that whale? Show us again!Originally posted by Evo
From this quote from the story Sounds like the Earth created it's own widescale version of TUMS to get rid of the gas.
"Earth 'shook off' ancient warming" refers to a period of time in Earth's history, known as the Paleocene-Eocene Thermal Maximum (PETM), where the planet experienced a rapid and extreme warming event. This warming was caused by a massive release of greenhouse gases, primarily carbon dioxide, into the atmosphere. However, the Earth eventually returned to a cooler state, or "shook off" the warming, as natural processes balanced out the amount of greenhouse gases in the atmosphere.
The exact cause of the PETM is still debated among scientists, but it is believed that the release of greenhouse gases was triggered by a combination of factors, including volcanic activity, changes in ocean circulation, and the release of methane from frozen deposits in the Earth's crust. It is also possible that a meteor impact or a sudden release of methane from the ocean could have contributed to the warming event.
The Earth "shook off" the ancient warming through a process called negative feedback. As the planet warmed, certain natural processes were triggered that helped to remove excess carbon dioxide from the atmosphere. For example, increased plant growth and ocean uptake of carbon dioxide helped to reduce the amount of this greenhouse gas in the atmosphere, leading to a cooling effect.
The PETM is considered a relatively short-lived event in Earth's history, lasting for about 150,000 years. However, the warming did have long-term effects on the planet. It is estimated that the event caused a global temperature increase of 5-8 degrees Celsius, which had significant impacts on the Earth's ecosystems. It also led to changes in ocean chemistry and circulation, and may have contributed to the extinction of some species.
While there are some similarities between the PETM and current climate change, such as the release of greenhouse gases into the atmosphere, there are also significant differences. The rapid and extreme warming during the PETM was caused by natural processes, whereas current climate change is primarily driven by human activities, such as burning fossil fuels. Additionally, the rate of warming during the PETM was much faster than the current rate of warming, making it difficult to directly compare the two events.