Stromatolite

Stromatolites at Strelley Pool chert (SPC) (Pilbara Craton) - Western Australia
Modern stromatolites in Shark Bay, Western Australia

Stromatolites (/stroʊˈmætəlaɪts, strə-/[1][2]) or stromatoliths (from Greek στρώμα, strōma, mattress, bed, stratum, and λίθος, lithos, rock) are layered bio-chemical accretionary structures formed in shallow water by the trapping, binding and cementation of sedimentary grains by biofilms (microbial mats) of microorganisms, especially cyanobacteria.[3] Fossilized stromatolites provide ancient records of life on Earth by these remains, some of which may date from 3.7 billion years ago.[4][5] Lichen stromatolites are a proposed mechanism of formation of some kinds of layered rock structure that are formed above water, where rock meets air, by repeated colonization of the rock by endolithic lichens.[6][7]

Morphology

Stromatolites in the Soeginina Beds (Paadla Formation, Ludlow, Silurian) near Kübassaare, Saaremaa, Estonia

Stromatolites exhibit a variety of forms and structures, or morphologies, including conical, stratiform, branching, domal,[8] and columnar types. Stromatolites occur widely in the fossil record of the Precambrian, but are rare today. Very few ancient stromatolites contain fossilized microbes. While features of some stromatolites are suggestive of biological activity, others possess features that are more consistent with abiotic (non-biological) precipitation.[9] Finding reliable ways to distinguish between biologically formed and abiotic stromatolites is an active area of research in geology.[10]

Formation

Time lapse photography of modern microbial mat formation in a laboratory setting gives some revealing clues to the behavior of cyanobacteria in stromatolites. Biddanda et al. (2015) found that cyanobacteria exposed to localized beams of light moved towards the light, or expressed phototaxis, and increased their photosynthetic yield, which is necessary for survival.[11] In a novel experiment, the scientists projected a school logo onto a petri dish containing the organisms, which accreted beneath the lighted region, forming the logo in bacteria.[11] The authors speculate that such motility allows the cyanobacteria to seek light sources to support the colony.[11] In both light and dark conditions, the cyanobacteria form clumps that then expand outwards, with individual members remaining connected to the colony via long tendrils. This may be a protective mechanism that affords evolutionary benefit to the colony in harsh environments where mechanical forces act to tear apart the microbial mats. Thus these sometimes elaborate structures, constructed by microscopic organisms working somewhat in unison, are a means of providing shelter and protection from a harsh environment.

Fossil record

Some Archean rock formations show macroscopic similarity to modern microbial structures, leading to the inference that these structures represent evidence of ancient life, namely stromatolites. However, others regard these patterns as being due to natural material deposition or some other abiogenic mechanism. Scientists have argued for a biological origin of stromatolites due to the presence of organic globule clusters within the thin layers of the stromatolites, of aragonite nanocrystals (both features of current stromatolites),[10] and because of the persistence of an inferred biological signal through changing environmental circumstances.[12][13]

Stromatolites in the Hoyt Limestone (Cambrian) exposed at Lester Park, near Saratoga Springs, New York.
Pre-Cambrian stromatolites in the Siyeh Formation, Glacier National Park
Stromatolites (Pika Formation, Middle Cambrian) near Helen Lake, Banff National Park, Canada

Stromatolites are a major constituent of the fossil record of the first forms of life on earth.[14] The earliest fossils date to 3.7 billion years ago.[5] They peaked about 1.25 billion years ago[12] and subsequently declined in abundance and diversity,[15] so that by the start of the Cambrian they had fallen to 20% of their peak. The most widely supported explanation is that stromatolite builders fell victim to grazing creatures (the Cambrian substrate revolution); this theory implies that sufficiently complex organisms were common over 1 billion years ago.[16][17][18]

Proterozoic stromatolite microfossils (preserved by permineralization in silica) include cyanobacteria and possibly some forms of the eukaryote chlorophytes (that is, green algae). One genus of stromatolite very common in the geologic record is Collenia.

The connection between grazer and stromatolite abundance is well documented in the younger Ordovician evolutionary radiation; stromatolite abundance also increased after the end-Ordovician and end-Permian extinctions decimated marine animals, falling back to earlier levels as marine animals recovered.[19] Fluctuations in metazoan population and diversity may not have been the only factor in the reduction in stromatolite abundance. Factors such as the chemistry of the environment may have been responsible for changes.[20]

While prokaryotic cyanobacteria reproduce asexually through cell division, they were instrumental in priming the environment for the evolutionary development of more complex eukaryotic organisms.[14] Cyanobacteria (as well as extremophile Gammaproteobacteria) are thought to be largely responsible for increasing the amount of oxygen in the primeval earth's atmosphere through their continuing photosynthesis. Cyanobacteria use water, carbon dioxide, and sunlight to create their food. A layer of mucus often forms over mats of cyanobacterial cells. In modern microbial mats, debris from the surrounding habitat can become trapped within the mucus, which can be cemented together by the calcium carbonate to grow thin laminations of limestone. These laminations can accrete over time, resulting in the banded pattern common to stromatolites. The domal morphology of biological stromatolites is the result of the vertical growth necessary for the continued infiltration of sunlight to the organisms for photosynthesis. Layered spherical growth structures termed oncolites are similar to stromatolites and are also known from the fossil record. Thrombolites are poorly laminated or non-laminated clotted structures formed by cyanobacteria, common in the fossil record and in modern sediments.[10]

The Zebra River Canyon area of the Kubis platform in the deeply dissected Zaris Mountains of south western Namibia provides an extremely well exposed example of the thrombolite-stromatolite-metazoan reefs that developed during the Proterozoic period, the stromatolites here being better developed in updip locations under conditions of higher current velocities and greater sediment influx.[21]

Modern occurrence

Stromatolites at Lake Thetis, Western Australia
Stromatolites at Highborne Cay, in the Exumas, The Bahamas

Modern stromatolites are mostly found in hypersaline lakes and marine lagoons where extreme conditions due to high saline levels prevent animal grazing. One such location is Hamelin Pool Marine Nature Reserve, Shark Bay in Western Australia where excellent specimens are observed today, and another is Lagoa Salgada ("Salty Lake"), in the state of Rio Grande do Norte, Brazil, where modern stromatolites can be observed as bioherm (domal type) and beds. Inland stromatolites can also be found in saline waters in Cuatro Ciénegas, a unique ecosystem in the Mexican desert, and in Lake Alchichica, a maar lake in Mexico's Oriental Basin. The only open marine environment where modern stromatolites are known to prosper is the Exuma Cays in the Bahamas.[22][23]

In 2010, a fifth type of Chlorophyll, namely Chlorophyll f was discovered by Dr. Min Chen from stromatolites in Shark Bay.[24]

Modern freshwater stromatolites

Microbialite towers at Pavilion Lake, British Columbia

Laguna Bacalar in Mexico's southern Yucatán Peninsula in the state of Quintana Roo, has an extensive formation of living giant microbialites (that is, stromatolites or thrombolites). The microbialite bed is over 10 km (6.2 mi) long with a vertical rise of several meters in some areas. These may be the largest sized living freshwater microbialites, or any organism, on Earth.[25]

A little farther to the south, a 1.5 km stretch of reef-forming stromatolites (primarily of the Scytonema genus) occurs in Chetumal Bay in Belize, just south of the mouth of the Rio Hondo and the Mexican border.[26]

Freshwater stromatolites are found in Lake Salda in southern Turkey. The waters are rich in magnesium and the stromatolite structures are made of hydromagnesite.[27]

Another pair of instances of freshwater stromatolites are at Pavilion and Kelly Lakes in British Columbia, Canada. Pavilion Lake has the largest known freshwater stromatolites and has been researched by NASA as part of xenobiology research.[28] NASA, the Canadian Space Agency and numerous universities from around the world are collaborating on a project centered on studying microbialite life in the lakes. Called the "Pavilion Lake Research Project" (PLRP) its aim is to study what conditions on the lakes' bottoms are most likely to harbor life and develop a better hypothesis on how environmental factors affect microbialite life. The end goal of the project is to better understand what conditions would be more likely to harbor life on other planets.[29] There is a citizen science project online called "MAPPER" where anyone can help sort through thousands of photos of the lake bottoms and tag microbialites, algae and other lake bed features.[30]

Microbialites have been discovered in an open pit pond at an abandoned asbestos mine near Clinton Creek, Yukon, Canada.[31] These microbialites are extremely young and presumably began forming soon after the mine closed in 1978. The combination of a low sedimentation rate, high calcification rate, and low microbial growth rate appears to result in the formation of these microbialites. Microbialites at an historic mine site demonstrates that an anthropogenically constructed environment can foster microbial carbonate formation. This has implications for creating artificial environments for building modern microbialites including stromatolites.

'Crayback' stromatolite - Nettle Cave, Jenolan Caves, NSW, Australia
'Crayback' stromatolite - Nettle Cave, Jenolan Caves, NSW, Australia

A very rare type of non-lake dwelling stromatolite lives in the Nettle Cave at Jenolan Caves, NSW, Australia.[32] The cyanobacteria live on the surface of the limestone, and are sustained by the calcium rich dripping water, which allows them to grow toward the two open ends of the cave which provide light.[33]

Stromatolites composed of calcite have been found in both the Blue Lake in the dormant volcano, Mount Gambier and at least eight cenote lakes including the Little Blue Lake in the Lower South-East of South Australia.[34]

See also

References

  1. ↑ "Stromatolite". Merriam-Webster Dictionary. Retrieved 2016-01-21.
  2. ↑ "Stromatolite". Oxford Dictionaries. Oxford University Press. Retrieved 2016-01-21.
  3. ↑ Riding, R. (2007). "The term stromatolite: towards an essential definition". Lethaia. 32 (4): 321–330. doi:10.1111/j.1502-3931.1999.tb00550.x.
  4. ↑ Nutman, Allen P.; Bennett, Vickie C.; Friend, Clark R. L.; Kranendonk, Martin J. Van; Chivas, Allan R. "Rapid emergence of life shown by discovery of 3,700-million-year-old microbial structures". Nature. doi:10.1038/nature19355.
  5. 1 2 Wade, Nicholas (31 August 2016). "World's Oldest Fossils Found in Greenland". New York Times. Retrieved 31 August 2016.
  6. ↑ Lichen Stromatolites: Criterion for Subaerial Exposure and a Mechanism for the Formation of Laminar Calcretes (Caliche), Colin F. Klappa, Journal of Sedimentary Petrology, Vol. 49 (1979)No. 2. (June), Pages 387-400,
  7. ↑ Paleobotany: The Biology and Evolution of Fossil Plants, Edith L. Taylor, Thomas N. Taylor, Michael Krings, page
  8. ↑ "Two-ton, 500 Million-year-old Fossil Of Stromatolite Discovered In Virginia, U.S.". Retrieved 2011-12-08.
  9. ↑ Grotzinger, John P.; Rothman, Daniel H. (3 October 1996). "An abiotic model for stromatolite morphogenesis". Nature. 383. doi:10.1038/383423a0. Retrieved 31 August 2016 – via Nature.
  10. 1 2 3 Lepot, Kevin; Karim Benzerara; Gordon E. Brown; Pascal Philippot (2008). "Microbially influenced formation of 2.7 billion-year-old stromatolites". Nature Geoscience. 1 (2): 118–21. Bibcode:2008NatGe...1..118L. doi:10.1038/ngeo107.
  11. 1 2 3 Biddanda, Bopaiah A.; McMillan, Adam C.; Long, Stephen A.; Snider, Michael J.; Weinke, Anthony D. (2015-01-01). "Seeking sunlight: rapid phototactic motility of filamentous mat-forming cyanobacteria optimize photosynthesis and enhance carbon burial in Lake Huron's submerged sinkholes". Aquatic Microbiology: 930. doi:10.3389/fmicb.2015.00930. PMC 4561352Freely accessible. PMID 26441867.
  12. 1 2 Allwood, Abigail; Grotzinger; Knoll; Burch; Anderson; Coleman; Kanik (2009). "Controls on development and diversity of Early Archean stromatolites". Proceedings of the National Academy of Sciences. 106 (24): 9548–9555. Bibcode:2009PNAS..106.9548A. doi:10.1073/pnas.0903323106.
  13. ↑ Cradle of life: the discovery of earth's earliest fossils. Princeton, N.J: Princeton University Press. 1999. pp. 87–89. ISBN 0-691-08864-0.
  14. 1 2 Garwood, Russell J. (2012). "Patterns In Palaeontology: The first 3 billion years of evolution". Palaeontology Online. 2 (11): 1–14. Retrieved June 25, 2015.
  15. ↑ McMenamin, M. A. S. (1982). "Precambrian conical stromatolites from California and Sonora". Bulletin of the Southern California Paleontological Society. 14 (9&10): 103–105.
  16. ↑ McNamara, K.J. (20 December 1996). "Dating the Origin of Animals". Science. 274and (5295): 1993–1997. Bibcode:1996Sci...274.1993M. doi:10.1126/science.274.5295.1993f. Retrieved 2008-06-28.
  17. ↑ Awramik, S.M. (19 November 1971). "Precambrian columnar stromatolite diversity: Reflection of metazoan appearance" (abstract). Science. 174 (4011): 825–827. Bibcode:1971Sci...174..825A. doi:10.1126/science.174.4011.825. PMID 17759393. Retrieved 2007-12-01.
  18. ↑ Bengtson, S. (2002). "Origins and early evolution of predation" (PDF). In Kowalewski, M.; Kelley, P.H. The fossil record of predation. The Paleontological Society Papers. 8. The Paleontological Society. pp. 289–317. Retrieved 29 December 2014.
  19. ↑ Sheehan, P.M. & Harris, M.T. (2004). "Microbialite resurgence after the Late Ordovician extinction". Nature. 430 (6995): 75–78. Bibcode:2004Natur.430...75S. doi:10.1038/nature02654. PMID 15229600. Retrieved 2007-12-01.
  20. ↑ Riding R (March 2006). "Microbial carbonate abundance compared with fluctuations in metazoan diversity over geological time" (pdf). Sedimentary Geology. 185 (3–4): 229–38. Bibcode:2006SedG..185..229R. doi:10.1016/j.sedgeo.2005.12.015. Retrieved 2011-12-09.
  21. ↑ Adams, E. W.; Grotzinger, J. P.; Watters, W. A.; Schröder, S.; McCormick, D. S.; Al-Siyabi, H. A. (2005). "Digital characterization of thrombolite-stromatolite reef distribution in a carbonate ramp system (terminal Proterozoic, Nama Group, Namibia)" (PDF). AAPG Bulletin. 89 (10): 1293–1318. doi:10.1306/06160505005. Retrieved 2011-12-08.
  22. ↑ "217-Stromatolites-Lee-Stocking-Exumas-Bahamas Bahamas". Retrieved 2011-12-08.
  23. ↑ Feldmann M, McKenzie JA (April 1998). "Stromatolite-thrombolite associations in a modern environment, Lee Stocking Island, Bahamas". PALAIOS. 13 (2): 201–212. doi:10.1043/0883-1351(1998)013<0201:SAIAME>2.0.CO;2.
  24. ↑ Chen, M. .; Schliep, M. .; Willows, R. D.; Cai, Z. -L.; Neilan, B. A.; Scheer, H. . (2010). "A Red-Shifted Chlorophyll". Science. 329 (5997): 1318–1319. Bibcode:2010Sci...329.1318C. doi:10.1126/science.1191127. PMID 20724585.
  25. ↑ Gischler, E.; Gibson, M. & Oschmann, W. (2008). "Giant Holocene Freshwater Microbialites, Laguna Bacalar, Quintana Roo, Mexico". Sedimentology. 55 (5): 1293–1309. Bibcode:2008Sedim..55.1293G. doi:10.1111/j.1365-3091.2007.00946.x.
  26. ↑ Rasmussen, K.A.; Macintyre, I.G. & Prufert, L (March 1993). "Modern stromatolite reefs fringing a brackish coastline, Chetumal Bay, Belize". Geology. 21 (3): 199–202. Bibcode:1993Geo....21..199R. doi:10.1130/0091-7613(1993)021<0199:MSRFAB>2.3.CO;2.
  27. ↑ Braithwaite, C. & Zedef V (November 1996). "Living hydromagnesite stromatolites from Turkey". Sedimentary Geology. 106 (3–4): 309. Bibcode:1996SedG..106..309B. doi:10.1016/S0037-0738(96)00073-5.
  28. ↑ Ferris FG, Thompson JB, Beveridge TJ (June 1997). "Modern Freshwater Microbialites from Kelly Lake, British Columbia, Canada". PALAIOS. 12 (3): 213–219. doi:10.2307/3515423. JSTOR 3515423.
  29. ↑ Brady, A.; Slater, G.F.; Omelon, C.R.; Southam, G.; Druschel, G.; Andersen, A.; Hawes, I.; Laval, B.; Lim, D.S.S. (2010). "Chemical Geology". Chemical Geology. 274: 56–67. doi:10.1016/j.chemgeo.2010.03.016.
  30. ↑ "NASA - Help NASA Find Life On Mars With MAPPER". NASA. Retrieved 2011-12-10.
  31. ↑ Power, I.M., Wilson, S.A., Dipple, G.M., and Southam, G. (2011) Modern carbonate microbialites from an asbestos open pit pond, Yukon, Canada, http://onlinelibrary.wiley.com/doi/10.1111/gbi.2011.9.issue-2/issuetoc Geobiology. 9: 180-195.
  32. ↑ Jenolan Caves Reserve Trust. "Nettle Cave Self-guided tour". Retrieved 22 May 2011.
  33. ↑ Cox G, James JM, Leggett KEA, Osborne RAL (1989). "Cyanobacterially deposited speleothems: Subaerial stromatolites". Geomicrobiology Journal. 7 (4): 245–252. doi:10.1080/01490458909377870.
  34. ↑ Thurgate, Mia E. (1996). "The Stromatolites of the Cenote Lakes of the Lower South East of South Australia" (PDF). HELICTITE, Journal of Australasian Cave Research. Speleological Research Council Limited. 34 (1): 17. ISSN 0017-9973.

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