Wikipedia

Endolith

For the dental term, seePulp stone.

Anendolithorendolithicis anorganism(archaeon,bacterium,fungus,lichen,algaeoramoeba) that is able to acquire the necessary resources for growth in the inner part of arock,[1]mineral,coral,animal shells,or in theporesbetweenmineralgrains of a rock. Many areextremophiles,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]Normally, the endoliths colonize the areas within lithic substrates to withstand intense solar radiation, temperature fluctuations, wind, and desiccation.[3] They are of particular interest toastrobiologists,who theorize that endolithic environments onMarsand other planets constitute potentialrefugiafor extraterrestrial microbial communities.[4][5]

Endolith lifeform found inside an Antarctic rock

Subdefinitions

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The term "endolith", which defines an organism that colonizes the interior of any kind of rock, has been further classified into five subclasses:[6]

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

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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),[7][8]also in cold deserts as Arctic and Antarctic,[9]and deepsubsoiland ocean trenches rocks.[10]However, there are reports of endolithic microorganisms in inter-tropical zones,[11]where humidity and solar radiation are significantly different from the above-mentioned biomes. Endoliths have been found in the rock down to a depth of 3 km (1.9 mi), though it is unknown if that is their limit (due to the cost involved in drilling to such depths).[12][13]The main threat to their survival seems not to result from the pressure at such depth, but from the increased temperature. Judging fromhyperthermophileorganisms, the temperature limit is at about 120 °C (Strain 121can reproduce at 121 °C), which limits the possible depth to 4-4.5 km below thecontinentalcrust, and 7 or 7.5 km below theoceanfloor. Endolithic organisms have also been found in surface rocks in regions of low humidity (hypolith) and low temperature (psychrophile), including theDry ValleysandpermafrostofAntarctica,[14]theAlps,[15]and theRocky Mountains.[16][17]

Metabolism and survival

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The metabolism of endolithic microorganisms is versatile, in many of those communities have been found genes involved insulphur metabolism,iron metabolismandcarbon fixation.In addition, whether they metabolize these directly from the surrounding rock, or rather excrete an acid to dissolve them first is yet undetermined. According to Meslier & DiRuggiero[18]there are found genes in the endolithic community involved innitrogen fixation.TheOcean Drilling Programfound microscopic trails inbasaltfrom theAtlantic,Indian,andPacificoceans that containDNA.[19][20]Photosynthetic endoliths have also been discovered.[21]

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.[18]Besides, the presence of pigments, especially incyanobacteriaand somealgae,such as;beta carotenesandchlorophyllhelp them in the protection against dangerous radiation and is a way to obtain energy.[22]Another characteristic is the presence of a very slowreproductioncycle. Early data suggest some only engage incell divisiononce 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.[23]Most of their energy is spent repairingcell damagecaused bycosmic raysorracemization,and very little is available for reproduction or growth. It is thought that they weather longice agesin this fashion, emerging when the temperature in the area warms.[13]

Ecology

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As most endoliths areautotrophs,they can generate organic compounds essential for their survival on their own from inorganic matter. Some endoliths have specialized in feeding on their autotroph relatives. The micro-biotopewhere these different endolithic species live together has been called asubsurface lithoautotrophic microbial ecosystem(SLiME),[24]orendolithic systemswithin the subterranean lithicbiome.

Endolithic systemsare 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.[25]

Endolithic fungi and algae in marine ecosystems

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Only limited research has been done concerning the distribution ofmarine endolithic fungiand its diversity even though there is a probability that endolithic fungi could perhaps play an important role in the health ofcoral 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 implexisandLithopythium gangliiforme.Discovery of endolithic fungi, such asDodgella priscusandConchyliastrum,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.[26]

In the wake of worldwidecoral bleaching,studies have suggested that the endolithic algae located in the skeleton of the coral may be aiding the survival of coral species by providing an alternative source of energy. Although the role that endolithic fungi play is important in coral reefs, it is often overlooked because much research is focused on the effects of coral bleaching as well as the relationships betweenCoelenterateandendosymbioticSymbiodinia.[27]

According to a study done by Astrid Gunther endoliths were also found in the island ofCozumel(Mexico). The endoliths found there not only included algae and fungi but also includedcyanobacteria,spongesas well as many other microborers.[28]

Endolithic parasitism

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Until the 1990sphototrophicendoliths were thought of as somewhat benign, but evidence has since surfaced that phototrophic endoliths (primarilycyanobacteria) have infested 50 to 80% of midshore populations of the mussel speciesPerna pernalocated inSouth 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.[29]

Endolithic fungi found in the eggs of Cretaceous dinosaurs

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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.".[30]

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.[30]

Relationship with astrobiology

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Endolithic microorganisms have been considered a model for the search for life on other planets by inquiring about what sort of microorganisms onEarthinhabit specificminerals,which helps to propose those lithologies as life detection targets on an extra-terrestrial surface such asMars.Several studies have been carried out in extreme places that serve as analogs for Mars's surface and subsurface, and many studies ingeomicrobiologyon Earth's hot and cold deserts have been developed.[31]In theseextreme environments,microorganisms find protection against thermal buffering, UV radiation, and desiccation while living inside pores and fissures of minerals and rocks.[8][4]Life in these endolithic habitats might face similar stress due to the scarcity of water and high UV radiation that rule on modern Mars.[18]

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.[32][33]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

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References

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  1. ^Omelon, C.R. (2016). "Endolithic Microorganisms and Their Habitats". In Hurst, C.J. (ed.).Their World: A Diversity of Microbial Environments.Advances in environmental microbiology, vol. 1. Cincinnati, USA: Springer. pp. 171–201.doi:10.1007/978-3-319-28071-4_4.
  2. ^
  3. ^Walker, J. J.; Pace, N. R. (2007). "Endolithic microbial ecosystems".Annual Review of Microbiology.61:331–347.doi:10.1146/annurev.micro.61.080706.093302.PMID17506683.
  4. ^abWierzchos, J.; Camara, B.; De Los Rios, A.; Davila, A. F.; Sanchaz Almazo, M.; Artieda, O.; Wierzchos, K.; Gomez-Silva, B.; McKay, C.; Ascaso, C. (2011). "Microbial colonization of Ca-sulfate crusts in the hyperarid core of the Atacama Desert: Implications for the search for life on Mars".Geobiology.9(1): 44–60.doi:10.1111/j.1472-4669.2010.00254.x.PMID20726901.S2CID9458330.
  5. ^Chang, Kenneth (12 September 2016)."Visions of Life on Mars in Earth's Depths".The New York Times.Retrieved12 September2016.
  6. ^Golubic, Stjepko;Friedmann, E. Imre;Schneider, Jürgen (June 1981)."The lithobiotic ecological niche, with special reference to microorganisms".SEPM Journal of Sedimentary Research.51(2): 475–478.doi:10.1306/212F7CB6-2B24-11D7-8648000102C1865D.Archived fromthe originalon 30 December 2010.
  7. ^
  8. ^abBell, R. A. (1993). "Cryptoendolithic algae of hot semiarid lands and deserts".Journal of Phycology.29(2): 133–139.doi:10.1111/j.0022-3646.1993.00133.x.S2CID85033484.
  9. ^
  10. ^Inagaki, F.; Takai, K.; Komatsu, T.; Sakihama, Y.; Inoue, A.; Horikoshi, K. (2015). "Profile of microbial community structure and presence of endolithic microorganisms inside a deep-sea rock".Geomicrobiology Journal.19(6): 535–552.doi:10.1080/01490450290098577.S2CID84636295.
  11. ^Gaylarde, C.; Baptista-Neto, J. A.; Ogawa, A.; Kowalski, M.; Celikkol-Aydin, S.; Beech, I. (2017). "Epilithic and endolithic microorganisms and deterioration on stone church facades subject to urban pollution in a sub-tropical climate".Biofouling.33(2): 113–127.doi:10.1080/08927014.2016.1269893.PMID28054493.S2CID3295932.
  12. ^Schultz, Steven (13 December 1999)."Two miles underground".Princeton Weekly Bulletin. Archived fromthe originalon 13 January 2016.— Gold mines present "ideal environment" for geologists studying subsurface microbes
  13. ^abHively, Will (May 1997)."Looking for life in all the wrong places — research on cryptoendoliths".Discover.Retrieved5 December2019.
  14. ^de la Torre, J. R.; Goebel, B. M.;Friedmann, E. I.;Pace, N. R. (2003)."Microbial Diversity of Cryptoendolithic Communities from the McMurdo Dry Valleys, Antarctica".Applied and Environmental Microbiology.69(7): 3858–3867.Bibcode:2003ApEnM..69.3858D.doi:10.1128/AEM.69.7.3858-3867.2003.PMC165166.PMID12839754.
  15. ^Horath, Thomas; Bachofen, Reinhard (August 2009)."Molecular Characterization of an Endolithic Microbial Community in Dolomite Rock in the Central Alps (Switzerland)"(PDF).Microbial Ecology.58(2): 290–306.doi:10.1007/s00248-008-9483-7.PMID19172216.S2CID845383.
  16. ^Walker, Jeffrey J.; Spear, John R.; Pace, Norman R. (2005). "Geobiology of a microbial endolithic community in the Yellowstone geothermal environment".Nature.434(7036): 1011–1014.Bibcode:2005Natur.434.1011W.doi:10.1038/nature03447.PMID15846344.S2CID4408407.
  17. ^Walker, J. J.; Pace, N. R. (2007)."Phylogenetic Composition of Rocky Mountain Endolithic Microbial Ecosystems".Applied and Environmental Microbiology.73(11): 3497–3504.Bibcode:2007ApEnM..73.3497W.doi:10.1128/AEM.02656-06.PMC1932665.PMID17416689.
  18. ^abcMeslier, V; DiRuggiero, J (2019). "7 Endolithic microbial communities as model systems for ecology and astrobiology". In Seckbach, J.; Rampelotto, P.H. (eds.).Model Ecosystems in Extreme Environments.Academic press.ISBN978-0-1281-2742-1.
  19. ^Mullen, Leslie."Glass Munchers Under the Sea".NASA Astrobiology Institute.Archived fromthe originalon 20 February 2013.
  20. ^Lysnes, Kristine; Torsvik, Terje; Thorseth, Ingunn H.; Pedersen, Rolf B. (2004)."Microbial Populations in Ocean Floor Basalt: Results from ODP Leg 187"(PDF).Proc ODP Sci Results.Proceedings of the Ocean Drilling Program.187:1–27.doi:10.2973/odp.proc.sr.187.203.2004.
  21. ^Wierzchos, Jacek; Ascaso, Carmen; McKay, Christopher P. (2006). "Endolithic Cyanobacteria in Halite Rocks from the Hyperarid Core of the Atacama Desert".Astrobiology.6(3): 415–422.Bibcode:2006AsBio...6..415W.doi:10.1089/ast.2006.6.415.hdl:10261/19099.PMID16805697.
  22. ^Osterrothová, K; Culka, A; Němečková, K; Kaftan, D; Nedbalová, L; Procházková, L; Jehlička, J (2019). "Analyzing carotenoids of snow algae by Raman microspectroscopy and high-performance liquid chromatography".Spectrochimica Acta Part A: Molecular and Biomolecular Spectroscopy.212:262–271.Bibcode:2019AcSpA.212..262O.doi:10.1016/j.saa.2019.01.013.PMID30658280.S2CID58604046.
  23. ^Yirka, Bob (29 August 2013)."Soil beneath ocean found to harbor long-lived bacteria, fungi and viruses".Phys.org.Archivedfrom the original on 29 October 2015.
  24. ^"Frequently Requested Information about the SLiME Hypothesis".Archived fromthe originalon 30 September 2006.
  25. ^Keith, DA; Iliffe, TM; Gerovasileiou, V; Gonzalez, B; Brankovits, D; Martínez García, A (2020)."S1.2 Endolithic systems".In Keith, D.A.; Ferrer-Paris, J.R.; Nicholson, E.; Kingsford, R.T. (eds.).The IUCN Global Ecosystem Typology 2.0: Descriptive profiles for biomes and ecosystem functional groups.Gland, Switzerland: IUCN.doi:10.2305/IUCN.CH.2020.13.en.ISBN978-2-8317-2077-7.S2CID241360441.
  26. ^Golubic, Stjepko; Radtke, Gudrun; Campion-Alsumard, Therese Le (2005). "Endolithic fungi in marine ecosystems".Trends in Microbiology.13(5): 229–235.doi:10.1016/j.tim.2005.03.007.PMID15866040.
  27. ^Fine, Maoz; Loya, Yossi (2002)."Endolithic algae: an alternative source of photoassimilates during coral bleaching".Proceedings of the Royal Society of London. Series B: Biological Sciences.269(1497): 1205–1210.doi:10.1098/rspb.2002.1983.PMC1691023.PMID12065035.
  28. ^Günther, Astrid (1990). "Distribution and bathymetric zonation of shell-boring endoliths in recent reef and shelf environments: Cozumel, Yucatan (Mexico)".Facies.22(1): 233–261.doi:10.1007/bf02536953.S2CID130403994.
  29. ^Kaehler, S.; McQuaid, C. D. (1999). "Lethal and sub-lethal effects of phototrophic endoliths attacking the shell of the intertidal musselPerna perna".Marine Biology.135(3): 497–503.doi:10.1007/s002270050650.S2CID84103549.
  30. ^abGong, YiMing; Xu, Ran; Hu, Bi (2008). "Endolithic fungi: A possible killer for the mass extinction of Cretaceous dinosaurs".Science in China Series D: Earth Sciences.51(6): 801–807.Bibcode:2008ScChD..51..801G.doi:10.1007/s11430-008-0052-1.S2CID126670640.
  31. ^Warren-Rhodes, K. A.; Rhodes, K. L.; Pointing, S. B.; Ewing, S. A.; Lacap, D. C.; Gomez-Silva, B.; McKay, C. P. (2006). "Hypolithic cyanobacteria, dry limit of photosynthesis, and microbial ecology in the hyperarid Atacama Desert".Microbial Ecology.52(3): 389–398.doi:10.1007/s00248-006-9055-7.PMID16865610.S2CID1914122.
  32. ^Cockell, C.; Osinski, G.; Lee, P. (2003). "The impact crater as a habitat: effects of impact processing of target materials".Astrobiology.3(1): 3181–191.Bibcode:2003AsBio...3..181C.doi:10.1089/153110703321632507.PMID12804371.
  33. ^Oren, A.; Kühl, M.; Karsten, U. (1995)."An endoevaporitic microbial mat within a gypsum crust: zonation of phototrophs, photopigments, and light penetration".Marine Ecology Progress Series.128:151–159.Bibcode:1995MEPS..128..151O.doi:10.3354/meps128151.
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  • 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.

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