Radioactive Decay: Life beyond the Sunlight’s Reach

radioactive decay

Scientists have been gazing at the hems of habitability in the quest to discern life’s limits. They have tunnelled kilometres underneath Earth’s exterior, digging out from the base of excavation shafts and fading boreholes long into ocean sediments. Life is present in staggering quantities, according to estimates, the occupied subsurface region has double the capacity of the oceans and holds on the order of 10^30 cells, making it one of the most consequential habitats on Earth, as well as one of the earliest and most distinct.

“Life was everywhere that we looked”

Tori Hoehler- Scientist at NASA

Researchers are furthermore working to comprehend how most of the life down there perseveres. Sunlight for photosynthesis fail to reach such bottoms, and the insufficient amount of organic carbon nutrients that does is usually soon consumed. Unlike populations of organisms that inhabit near hydrothermal vents on the seafloor or within continental areas warmed by volcanic action, ecosystems here ordinarily can’t depend on the high-temperature means that hold some subsurface life free of photosynthesis; these microorganisms are seen hanging on in pitch-black darkness and cold water.

Radioactive decay is supporting life that exists in various layers of the Earth.
Various Layers in the Earth’s Interior are known, however, life forms at such depths are rare and mysterious. Image: IE

Research published by two individual groups seem to have answered some of part of the strange question, which goes like this: How can a place with no sunlight support life?

No Sunlight, Not a Problem. Radioactive Decay is Here to Support Life.

These separate research were published in February 2021 and presented the evidence, considering the analogy with the Sun’s nuclear-fusion reaction as an energy source, likewise, here on Earth, there has to be some life-supporting energy source. As the research claims, a complex kind of nuclear process called radioactive decay sustains life deep beneath the surface.

This research has been backed with a lot of data and evidence that radiations from unstable atoms of certain elements present in rocks can divide water units into hydrogen and chemically reactive peroxides. Some living cells have the ability to directly use hydrogen to meet energy needs, while the peroxides turn neighbouring compounds into supplementary energy resources.

WaterWords–Hydrothermal Vent
A hydro thermal vent has been depicted here in. A lot minerals being added from the vent into the oceans make it a place suitable for life to sustain but the sun light hardly reaches here. Such vents have gained significance in the research fields these days. Image: USGS

However, these radiolytic reactions yield energy at a very slow pace when compared to the sun and some thermal processes. Through the research, it was clear that they are fast enough to drive microbial activity in a particular setting found in depths and that they are accountable for a varied pool of organic moieties and other molecules important to life. Now this research has a lot more to tell us about how life must have started and the environmental setting led to the same, it has opened up new vistas for astrobiologists, nuclear scientists and chemists.

Again, the opinion that exploring space for extra-terrestrial life is not worth it until we have known completely about the life forms on Earth. But then, what also holds true is such research help in understanding the setting of any place that leads to the evolution of such life forms, to our surprise, that depends on the energy released in radioactive decay.

Radiolytic Hydrogen is the New Sunlight!

Sunlight hours — Australian Antarctic Program
Sunlight is the life-giving radiation for most living entities. This image displays the surface of frozen oceans illuminated with sunlight, however, deep down in it thrive life forms that live near drastic hydrothermal vents. Image: Antarctica

In 2010, Japanese scientists-geomicrobiologists conducted drilling and excavation to collect samples of sub-seafloor deposits from various oceans. Meanwhile, the sample from the expedition and suspended in water, later on exposing this water to different radiations, they found the amount of hydrogen produced was in significantly larger amounts than when pure water gets exposed to such radiations. This is clear evidence that sediments were responsible for the amplification of hydrogen yields in the radiolytic splitting. The production of hydrogen was seen to be increased by a factor of 30 in some cases, and this can not fail to ridicule any scientist.

Well, then why is the hydrogen gas not detected during the expedition?

Scientists claimed that water, irradiating with various radiations in the lab was split into hydrogen very efficiently, but was not detected in even the slightest amounts during the drilling of sediments.

Hydrogen was mysteriously absent as it was being consumed by the microbes present in the sediments. According to their model, sediments that are a few million years old and are at depth are producing radiolytic hydrogen which is being consumed more swiftly than organic matter.

As a result, the radiolysis of water is the dominant source of energy in older sediments. Sadly, this hydrogen is just 2 per cent of the total energy available in oceans and the rest 98 per cent comes from the carbon of organic molecules suspended in the waters of the oceans. Planetary scientists perceive this as a relatively slow process, but from a geologic perspective, it holds due significance.

A Project that could ‘Complexify’ Chemistry

The Earth 4D Project has seen multiple collaborations from scientists from around the globe to study organic molecules present in the waters around Canada and the chemistry involved that governs the factors of life’s origin. In a nutshell, this team aims to complex organic molecules’ role in the metabolism of the earliest microbes. The study sounds difficult but the team has members who are renowned in the field of research. The results of this project have been of interests to various people and awaited with excitement.

Astrobiologists are also recognising how critical it might be to analyse radiolysis when necessitating the habitability of planetoids and moons everywhere in the solar system and the rest of the universe. Sunshine, soaring temperatures, and other circumstances might not be rigorously required to favour extraterrestrial life. Radiolysis should be almost universal on any hard planet that has water in its subsurface.

Take Mars. In a pair of studies, one published a couple of years ago and the other last month, Tarnas, Mustard, Sherwood Lollar, and other researchers translated quantitative work being done on radiolysis on Earth to the Martian subsurface. They found that based on the planet’s mineral composition and other parameters, Mars today might be able to sustain microbial ecosystems akin to those on Earth—with radiolysis alone. The scientists identified regions of the planet where the microbial concentration would likely be greatest, which could guide where future missions should be targeted.

Mars has been a Planet under Study for Years now.

The research and quantitative work done with respect to the subsurface of Earth are now being translated for Martian lands. Based on such comparison and mineral composition of the planet it is not wrong to assume that life might exist. Certain regions have been identified where microbial concentrations might be greatest.

Mars is just one planetary body that we might have explored among millions of others. Amid all such research, the question of utmost importance is

WHY DOES LIFE EXIST?

IF AT ALL IT EXISTS, WHAT IS THE ULTIMATE GOAL OF LIFE, SPECIFICALLY, HUMAN LIFE?

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Umakant Bohara
Umakant Bohara
Pursuing M.S. with Chemistry as a major Learning how to learn

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