Sugar-grain sized meteorites rocked the climates of early Earth and Mars

Bombardments of 'micro-meteorites' on Earth and Mars four billion years ago may have caused the planets' climates to cool dramatically, hampering their ability to support life, according to research published today in the journal Geochimica et Cosmochimica Acta.

Scientists from Imperial College London studied the effects of the Late Heavy Bombardment (LHB), a period of time in the early Solar System when showers lasting around 100 million years barraged and Mars. This bombardment discharged into the upper atmospheres of both planets and the researchers' analysis suggests that this may have had a catastrophic impact on their environments.

Micro-meteorites come from the rocky between Mars and Jupiter. These space rocks, which are the size of sugar grains, get dragged by gravity towards Earth and Mars. As they enter the planets' upper atmospheres, they heat up to temperatures of approximately 1000 degrees Celsius, releasing gases including sulphur dioxide. Sulphur dioxide in the atmosphere forms aerosols, consisting of solid and liquid particles, which deflect sunlight away from the surface, making planets cooler.

The authors of the new study have calculated that showers of micro-meteorites delivered approximately 20 million tonnes of sulphur dioxide each year into the of Earth during the LHB. The team deduced that on Mars, these micro-meteorites delivered up to half a million tonnes of sulphur dioxide each year for the same period of time.

Professor Mark Sephton, an author of the study from the Department of Earth Science and Engineering at Imperial College London, says:

"Far less of the Sun's energy was reaching Earth 4 billion years ago, which would have made it hard for early life to emerge. Recently denied of its protective magnetic field and constantly subjected to large meteorite impacts, Mars was also starting to lose its at this time, causing global cooling. The influx of sulphur dioxide into the Mars's atmosphere would have dealt a further blow to a planet already on the ropes, making conditions for life even more of a challenge."

The team say that such a large influx of sulphur dioxide into early Earth's atmosphere had the same cooling effect on the climate as if there was an eruption of the size of the 1991 Mount Pinatubo eruption every year for 100 million years. The 1991 Mount Pinatubo eruption released 17 million tonnes of gases, including sulphur dioxide, into the atmosphere, preventing 10 percent of sunlight from reaching Earth and cooling the planet by half a degree Celsius.

On Mars during the LHB, the scientists predict that the cooling effects of sulphur dioxide on the red planet's atmosphere would have been the equivalent of an eruption 1/34th the size of Mount Pinatubo occurring every year for 100 million years.

The scientists say that the environmental consequences of sulphur dioxide in Earth's atmosphere could have been disastrous. At this time, the Sun's energy was 30 percent weaker than it is today, meaning less energy was reaching the surface. The team believe that a weaker Sun, combined with increasing levels of sulphur dioxide from micro-meteorites, could have plunged Earth into an Arctic winter, lasting millions of years and making conditions for primitive microbial life extremely difficult.

On Mars, being further away from the Sun, the scientists suggest the environmental consequences would have been even more dramatic. High levels of sulphur dioxide would cause temperatures to plunge and water on the surface, in the form of lakes and rivers, to disappear, turning a warm wet world into a cold arid one.

Dr Richard Court, who is lead author of the study from the Department of Earth Science and Engineering at Imperial College London, adds:

"These sugar-grain sized meteorites are left over material from the construction of our early Solar System, helping to build rocky planets such as Earth and Mars. Our study is helping us to see how these tiny space rocks could also bring environmental devastation on a global scale to early Earth and Mars."

The researchers came to their conclusions by simulating what happens to micro-meteorites as they entered the atmosphere, using a technique called flash pyrolysis to heat rock fragments that were identical to micro-meteorites to 1000 degrees Celsius. They then used infrared spectroscopy to measure the amount of sulphur dioxide released from these rocks. The team then used their results and calculations of meteorite in-fall rates during the LHB to determine how much sulphur dioxide was delivered to Earth and Mars from micro-meteorites.

This study is a continuation of earlier work by the team who have discovered that meteorites are not the source of the present-day methane in the atmosphere of , raising hopes that the methane is being generated by life on the red planet. Their work has also shown that meteorites delivered other important gases to Earth during its early history that would have made it more habitable. In the future, the team will assess the contributions gases from meteorites on planets outside of the Solar System.


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Meteorite bombardment may have made Earth more habitable

More information: "The contribution of sulphur dioxide from ablating micro-meteorites to the atmospheres of Earth and Mars", 1 April 2011, Geochimica et Cosmochimica Acta
Citation: Sugar-grain sized meteorites rocked the climates of early Earth and Mars (2011, April 2) retrieved 21 April 2019 from https://phys.org/news/2011-04-sugar-grain-sized-meteorites-climates-early.html
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Apr 02, 2011
What's a little SO2 amongst bacteria and lichen when rocks the size of Texas are falling at the same time?

Apr 02, 2011
Lucky - IF the LB rate had continued a lot would indeed have accumulated.
But the current best estimate of what the earth receives now is 50-100 tons of space dust per day (based on tudies of space dust on antarctic and greenland ice sheets).
This space dust has a sulfer content averaging around 3%.
The LHB dust should have had comparable sulfer content so 20M tons of sulfer implies 600M tons of dust per year, or ~1.5M tons per day.

Thus what you see at night is a mere 1/30,000 to 1/15,000 of what you would have seen in the LHB. The rate dropped dramatically after the 100M year LHB, so the accumulation is on the order of 1/40 of what it appears that you were calculating.

Just imagine ~20,000 times the 'shooting stars' we have now - that would be glorious!


Apr 02, 2011
Shootist - bacteria possibly (and plenty of chemical energy available and geothermal heat, so cooling would not be a problem; those Texas-sized rocks, however, would be).

But lichens? Lichens are eukaryotic, and current estimates are that even the first eukaroyotes only evolved almost 2 billion years after the LHB.

Apr 02, 2011
Shootist - bacteria possibly (and plenty of chemical energy available and geothermal heat, so cooling would not be a problem; those Texas-sized rocks, however, would be).

But lichens? Lichens are eukaryotic, and current estimates are that even the first eukaroyotes only evolved almost 2 billion years after the LHB.


Lichen living today certainly didn't descend from anything lichen-like living then, that is certain. Neither did much of anything else. The LHB was certainly a sterilizing event.

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