Astronomy: Nature of Life on Other Planets

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Introduction

Earth is a unique planet in many geophysical, biological, and astronomical aspects. It possesses the perfect conditions for life. Although it is hard to find a planet similar to Earth anywhere near us, it is possible for life to exist in much harsher environments. Some planets and moons in the Solar system, such as Mars, Venus, Titan, and even Uranus, have the potential for life to exist on or under their surfaces. Out of all potential candidates, Titan seems the most likely one due to the presence of an atmosphere, water, and various organic chemicals on its surface (King 4466). Although the conditions on the planet would be too harsh for most Earth-based organisms, some have the potential of surviving even on Titan, providing us with a blueprint for the potential development of life. The purpose of this paper is to speculate about the existence of halophilic organisms in the salty oceans underneath the surface of Titan.

The Conditions for Life on Titan

Titan provides various conditions that could potentially sustain life. It has an atmosphere that shields the surface from excess radiation, it has water on and underneath the surface, and it possesses a wide range of organic chemicals that can be potentially used by organisms to form cell membranes and facilitate metabolism (Dyches and Bauer). One of the most likely places for halophilic organisms to exist is Titan’s vast underground ocean (Dickerson). Although the surface of Titan is frozen, its underground layers are warmed up by the moon’s core, which is evidenced by cryovolcanoes erupting water and methane. The ocean itself is hypersaline, meaning that any organisms other than halophilic microbes are unlikely to be able to live there. Dyches and Bauer state that methane and CO come from inside the moon, rather from the outside.

Halophilic Organisms as Residents of Titan

Halophilic organisms are extremely resilient lifeforms that could be found on Earth. They typically live in hypersaline environments such as the Dead Sea and various surface-based or underground salt lakes. They are resistant to radiation, high temperatures, and various other hazards. According to King (4465), extremely halophilic biota can utilize CO as an energy source in order to facilitate cellular metabolism. Since Titan possesses natural sources of CO and methane coming from inside the planet, it is possible for pockets of these gases to exist above the hypersaline oceans, thus providing solvents and energy sources for Titan-based halophilic organisms.

Similarities and Differences to Earth Organisms

Some of the similarities to Earth-based halophilic organisms would include utilizing CO as a source of energy for metabolism processes and possessing extreme degrees of halotolerance (King 4465). These are the qualities that Earth organisms possess and utilize to survive in the harshest environments on our planet. Some of the unique qualities that Titan-based halophilic organisms might possess would likely revolve around existing in complete darkness, enduring high temperatures, and surviving contact with any unknown salts and chemical elements that may be found on Titan’s surface. In addition, they are likely to be more agile than Earth-based organisms due to gravity, which is very low on Titan (14 percent of Earth’s gravity) meaning that they would not be required to spend as much energy to move (Tate).

Conclusions

Hypersaline underground oceans of Titan are the most likely places for life to exist due to possessing harsh, but survivable environments, water, CO, and protection from very low surface temperatures. Extremely halophilic bacteria have the potential to live and survive in these environments, possessing qualities similar to organisms inhabiting Earth.

Works Cited

Dickerson, Kelly.Space.com. 2014, Web.

Dyches, Preston, and Markus Bauer. “Cassini Explores a Methane Sea on Titan.” NASA. 2016, Web.

King, Gary M. “Carbon Monoxide as a Metabolic Energy Source for Extremely Halophilic Microbes: Implications for Microbial Activity in Mars Regolith.” PNAS, vol. 112, no. 14, 2015, pp. 4465-4470.

Tate, Karl. Space.com. 2015, Web.

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