A crater as an abode for life

Nov 04, 2013 by Amanda Doyle
Pingaluit crater in Canada is a geologically-young impact crater with a lake. Credit: NASA

A new study shows how the heat generated from an asteroid impact could lead to a crater becoming a refuge for life, or even a potential birthplace for life's origin.

An asteroid or comet smashing into the surface of a planet can spell doom for living creatures, but if the isn't large enough to completely decimate a planet's inhabitants, then the impact can ultimately provide a habitat for life. This is the finding of a new study reported at the European Planetary Science Congress in September by Iain Gilmour of the Open University in the UK.

If an ice or water-rich target is the victim of an impact, the combination of heat and groundwater will create what is known as a hydrothermal system. In addition, many complex organic compounds, which could be precursor molecules for life, are created at high temperatures such as those in a collision. This combination could create the ingredients needed for life as we know it, making impact-induced habitats a potential candidate for the birthplace of life on Earth.

For a habitat within a crater to remain "home sweet home," there must be a constant supply of water and nutrients. The lifetime of the hydrothermal system is also crucial, as the heat from the impact will eventually fade away into its surroundings.

Measuring the cooling time of an ancient crater can shed light on the importance of such an abode in the origins of life, and also probe how a crater can provide a habitable niche for microbial life on other planets.

The Boltysh crater in the Ukraine makes the perfect target for such an investigation, so Gilmour and his colleagues investigated the heating timescale of the crater.

The 24 kilometer diameter crater was created around 65 million years ago, and predates the Chicxulub crater - the smoking gun from the that wiped out the dinosaurs - by a few thousand years. Shortly after the impact that formed the Boltysh crater, a lake formed within it, laying down layers of sediments over time.

In 2008, Gilmour and his team drilled a 596 meter borehole to sample these sediments, and found that the post-impact sedimentary record at this crater is well preserved, enabling the scientists to reconstruct the thermal history of the crater.

A cross section of the Tswaing crater in South Africa shows how the layers of sediments that have been deposited over time can be sampled by drilling a borehole. Credit: Brandt, D., (1994), Brandt & Reimold (1999), Partridge & Reimold (1990)

Taking the temperature of the crater

Different techniques can be used to persuade the sediments to reveal their past. One of the methods used by the scientists utilized molecules known as , which have the same chemical formula but different structures.

Certain types of isomers are sensitive to heat, and the level of isomers will deplete at a certain rate when they are in the vicinity of a heat source. At the bottom of the Boltysh crater core, which samples the layers of sediments laid down directly above the impact site, the levels of two different isomers drop significantly. The thermal degradation of the isomers can be measured experimentally, so it is known that the temperature of the lake was between 75 and 250 degrees Celsius for a time after the impact.

As the isomers are only depleted in a few meters of the core above the impact site, it is possible to place a limit on the heating duration. However, the isomers cannot reveal the source of the , which is why another experimental technique was used to characterize the post-impact heating.

This technique involved measuring the composition of certain within carbonates in the sediments. Isotopes of the same element have the same number of protons and electrons, but different numbers of neutrons. While such isotopes can undergo the same chemical reactions, the rate of reactions will be quicker for some isotopes. For instance, evaporation will deplete heavier isotopes while enriching lighter ones, leaving different levels of the isotopes.

Evaporation of a lake is strongly dependent on the amount of time that it takes for water to flow into and out of the lake, and this "flushing time" is recorded by the isotopes in the lake sediments. The flushing time will be altered by groundwater, heated from the impact, bubbling up through fissures into the lake. The isotope compositions of the Boltysh crater can thus be used to estimate the heating time by seeing how long the water in the lake interacted with the hydrothermal groundwater.

The sediments also contain minute traces of vegetation, and changes in the vegetation over time can be linked to changes in the environment. The flora at the bottom of the core reveal that vegetation had been recovering for a few thousand years after the Boltysh impact, until the Cretaceous–Paleogene impact decimated the vegetation, along with the dinosaurs.

The sediments also record changes in carbon which coincide with a period of warming during the first few hundred thousand years of the early Paleogene. These events act as bookends, making it easier to date the sediments and thus the heating timescale of the lake.

The results show that the hydrothermal system at Boltysh persisted for somewhere between 30,000 and 40,000 years, and it seems that the presence of the lake significantly extended the heating time.

A crater as an abode for life
The Boltysh crater in the Ukraine has well preserved sediments, allowing an estimation of the post-impact heating timescale. Credit: Jolley et al. (2010)

Haughton crater, which is of a similar size to Boltysh, should have a comparable timescale for its hydrothermal system. However, Haughton crater did not fill up with a lake until millions of years after the impact, long after the had cooled, and subsequently its heating timescale was only 5,000 years.

The formation of a and its longevity could be key factors in a crater being a home for life.

Craters as habitats in the Solar System

"The cooling timescale, at 30,000 to 40,000 years, is not that long when one considers that after it's cold then it may not remain a viable habitat," said Gilmour. "The question then becomes one of cratering flux on early planets and whether that flux is enough to create interlinked habitats, but not so great as to potentially wipe out life."

Such a heating timescale suggests that in moderately sized craters, the heating may not have been significant enough to destroy all existing life, so microbial life might have survived.

Many craters on Mars are of a similar size, so there could still be a record of organic matter if the sediments that carry this information are preserved. This is why NASA's Curiosity rover is currently rummaging around in the Gale crater on Mars searching for any signs of a past habitat.

A crater etched into the landscape of a planet is not only the fingerprint of the rogue Solar System body that caused the collision, it also provides clues to the impact on life after such an event. Knowledge of the heating duration of the Boltysh crater therefore is a step forward in understanding how collisions influence , both on Earth and on other planets.

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5 / 5 (1) Nov 04, 2013
This combination could create the ingredients needed for life as we know it, making impact-induced habitats a potential candidate for the birthplace of life on Earth

Since we don't know the origin of life, there are quite a few potential candidates. I personally think this one is one of the least plausible I've seen seriously considered, but that's just my opinion.

For instance, evaporation will deplete heavier isotopes while enriching lighter ones, leaving different levels of the isotopes

Don't they have that backward? I thought lighter isotopes evaporate more easily, so there should be more of the heavy ones left behind in the sediments.