Endolith

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Endolith lifeform found inside an Antarctic rock

An endolith or endolithic is an

animal shells, or in the pores between mineral grains of a rock. Many are extremophiles, living in places long considered inhospitable to life. The distribution, biomass, and diversity of endolith microorganisms are determined by the physical and chemical properties of the rock substrate, including the mineral composition, permeability, the presence of organic compounds, the structure and distribution of pores, water retention capacity, and the pH.[2][3][4][5] Normally, the endoliths colonize the areas within lithic substrates to withstand intense solar radiation, temperature fluctuations, wind, and desiccation.[6]
They are of particular interest to astrobiologists, who theorize that endolithic environments on Mars and other planets constitute potential refugia for extraterrestrial microbial communities.[7][8]

Subdefinitions

The term "endolith", which defines an organism that colonizes the interior of any kind of rock, has been further classified into five subclasses:[9]

Chasmoendolith
Colonizes fissures and cracks in the rock connected to the surface (chasm = cleft)
Cryptoendolith
Colonizes structural cavities within natural pore spaces within the rocks. These pores are usually indirectly connected to the rock surface; (crypto = hidden)
Euendolith
Penetrates actively into the interior of rocks forming channels and grooves that conform with the shape of its body, rock boring organism (eu = true)
Hypoendolith
Colonizes the pore spaces located on the underside of the rock and that make contact with the soil (hypo = under)
Autoendolith
Capable of rocks formation by mineral depositation (auto = self)

Environment

Endolithic microorganisms have been reported in many areas around the globe. There are reports in warm hyper-arid and arid deserts such as Mojave and Sonora (USA), Atacama (Chile), Gobi (China, Mongolia), Negev (Israel), Namib (Namibia Angola), Al-Jafr basin (Jordan) and the Depression of Turpan (China),

Dry Valleys and permafrost of Antarctica,[30] the Alps,[31] and the Rocky Mountains.[32][33]

Metabolism and survival

The metabolism of endolithic microorganisms is versatile, in many of those communities have been found genes involved in

Pacific oceans that contain DNA.[35][36] Photosynthetic endoliths have also been discovered.[37]

As water and nutrients are rather sparse in the environment of the endolith, water limitation is a key factor in the capacity of survival of many endolithic microorganisms, many of those microorganisms have adaptations to survive in low concentrations of water.[38] Besides, the presence of pigments, especially in cyanobacteria and some algae, such as; beta carotenes and chlorophyll help them in the protection against dangerous radiation and is a way to obtain energy.[39] Another characteristic is the presence of a very slow reproduction cycle. Early data suggest some only engage in cell division once every hundred years. In August 2013 researchers reported evidence of endoliths in the ocean floor, perhaps millions of years old and reproducing only once every 10,000 years.[40] Most of their energy is spent repairing cell damage caused by cosmic rays or racemization, and very little is available for reproduction or growth. It is thought that they weather long ice ages in this fashion, emerging when the temperature in the area warms.[29]

Ecology

As most endoliths are

subsurface lithoautotrophic microbial ecosystem (SLiME),[41] or endolithic systems within the subterranean lithic biome
.

Endolithic systems are still at an early stage of exploration. In some cases its biota can support simple invertebrates, most organisms are unicellular. Near-surface layers of rock may contain blue-green algae but most energy comes from chemical synthesis of minerals. The limited supply of energy limits the rates of growth and reproduction. In deeper rock layers microbes are exposed to high pressures and temperatures.[42]

Endolithic fungi and algae in marine ecosystems

Only limited research has been done concerning the distribution of marine endolithic fungi and its diversity even though there is a probability that endolithic fungi could perhaps play an important role in the health of coral reefs.

Endolithic fungi have been discovered in shells as early as the year 1889 by Edouard Bornet and Charles Flahault. These two French phycologists specifically provided descriptions for two fungi: Ostracoblabe implexis and

Lithopythium gangliiforme. Discovery of endolithic fungi, such as Dodgella priscus and Conchyliastrum, has also been made in the beach sand of Australia by George Zembrowski. Findings have also been made in coral reefs and have been found to be, at times, beneficial to their coral hosts.[43]

In the wake of worldwide

According to a study done by Astrid Gunther endoliths were also found in the island of

sponges as well as many other microborers.[45]

Endolithic parasitism

Until the 1990s

phototrophic endoliths were thought of as somewhat benign, but evidence has since surfaced that phototrophic endoliths (primarily cyanobacteria) have infested 50 to 80% of midshore populations of the mussel species Perna perna located in South Africa. The infestation of phototrophic endoliths resulted in lethal and sub-lethal effects such as the decrease in strength of the mussel shells. Although the rate of thickening of the shells were faster in more infested areas it is not rapid enough to combat the degradation of the mussel shells.[46]

Endolithic fungi found in the eggs of Cretaceous dinosaurs

Evidence of endolithic fungi were discovered within dinosaur eggshell found in central China. They were characterized as being “needle-like, ribbon-like, and silk-like."[47].

Fungus is seldom fossilized and even when it is preserved it can be difficult to distinguish endolithic hyphae from endolithic cyanobacteria and algae. Endolithic microbes can, however, be distinguished based on their distribution, ecology, and morphology. According to a 2008 study, the endolithic fungi that formed on the eggshells would have resulted in the abnormal incubation of the eggs and may have killed the embryos in infected eggs of these dinosaurs. It may also have led to the preservation of dinosaur eggs, including some that contained embryos.[47]

Relationship with astrobiology

Endolithic microorganisms have been considered a model for the search for life on other planets by inquiring about what sort of microorganisms on Earth inhabit specific minerals, which helps to propose those lithologies as life detection targets on an extra-terrestrial surface such as Mars. Several studies have been carried out in extreme places that serve as analogs for Mars's surface and subsurface, and many studies in geomicrobiology on Earth's hot and cold deserts have been developed.[48] In these extreme environments, microorganisms find protection against thermal buffering, UV radiation, and desiccation while living inside pores and fissures of minerals and rocks.[49][7] Life in these endolithic habitats might face similar stress due to the scarcity of water and high UV radiation that rule on modern Mars.[50]

An excellent example of these adaptations is the non-hygroscopic but microporous translucent gypsum crusts, which are found as potential substrates that can mitigate exposure to UV radiation and desiccation and allow microbial colonization in hyper-arid deserts.[51][52] In the same way, the ability to grow under high water stress and oligotrophic conditions confer to endolithic microorganisms to survive in conditions similar to those found on Mars. There is evidence of the past existence of water on the red planet; perhaps, these microorganisms could develop adaptations found in current deserts on the Earth. Furthermore, The endolithic structures are a good way to find ancient or current biological activity (biosignatures) on Mars or other rocky planets.

See also

References

  1. ^ Omelon, CR (2016). "Endolithic Microorganisms and Their Habitats". In Hurst, C.J. (ed.). Advances in environmental microbiology. Their World: A Diversity of Microbial Environments. Cincinnati, USA: Springer.
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  8. ^ Chang, Kenneth (12 September 2016). "Visions of Life on Mars in Earth's Depths". The New York Times. Retrieved 12 September 2016.
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  28. ^ Schultz, Steven (13 December 1999). "Two miles underground". Princeton Weekly Bulletin. Archived from the original on 13 January 2016. — Gold mines present "ideal environment" for geologists studying subsurface microbes
  29. ^ a b Hively, Will (May 1997). "Looking for life in all the wrong places — research on cryptoendoliths". Discover. Retrieved 5 December 2019.
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  35. ^ Mullen, Leslie. "Glass Munchers Under the Sea". NASA Astrobiology Institute. Archived from the original on 20 February 2013.
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  40. ^ Yirka, Bob (29 August 2013). "Soil beneath ocean found to harbor long-lived bacteria, fungi and viruses". Phys.org. Archived from the original on 29 October 2015.
  41. ^ "Frequently Requested Information about the SLiME Hypothesis". Archived from the original on 30 September 2006.
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Notes

External links

  • Endoliths General Collection — This collection of online resources such as news articles, web sites, and reference pages provides a comprehensive array of information about endoliths.
  • Endolith Advanced Collection — Compiled for professionals and advanced learners, this endolith collection includes online resources such as journal articles, academic reviews, and surveys.