Features of calcareous algae mineralization at the transition to the Phanerozoic Biosphere

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• 作者：V. A. Luchinina (1)
  A. A. Terleev (1)
  
  1. Trofimuk Institute of Petroleum Geology and Geophysics ; Siberian Branch ; Russian Academy of Siences ; pr. Akademika Koptyuga 3 ; Novosibirsk ; 630090 ; Russia
  
• 关键词：calcareous algae ; mineralization ; transition to the Phanerozoic Biosphere
• 刊名：Paleontological Journal
• 出版年：2014
• 出版时间：December 2014
• 年：2014
• 卷：48
• 期：14
• 页码：1450-1456
• 全文大小：3,997 KB
• 参考文献：1. Barattolo, F., Mesozoic and Cenozoic marine benthic calcareous algae with particular regard to Mesozoic Dasycladaleans, in / Calcareous Algae and Stromatolites, Riding, R., Ed., Berlin: Springer-Verlag, 1990, pp. 504鈥?40.
  2. Belyaeva, G.V., Luchinina, V.A., Nazarov, B.B., Retina, L.N., and Sobolev, L.P., / Kembriiskaya fauna i flora khrebta Dzhagdy (Dal鈥檔ii Vostok) (Cambrian Fauna and Flora of the Dzhagdy Range, Russian Far East), Zhuravleva, I.T., Ed., Moscow: Nauka, 1975.
  3. Cuif, J.-P., Dauphin, Y., and Sorauf, J.E., / Biominerals and Fossils through Time, Cambridge, U. K.: Cambridge Univ. Press, 2011.
  4. Golubic, S., Radoj膷i膰, R., and Lee Seong-Joo, Cyanobacteria on modern and ancient carbonate platforms, in / Scytonema-Aeolisaccus. Abstracts of the 8th Int. Symp. Fossil Algae, Granada, Spain, 18鈥?0 September, 2003, Publ. Univ. Granada, Spain, no. 21, Granada: Univ. Granada, 2003.
  5. Korde, K.B., New representatives of siphoneous algae, in / Mat-ly k Osnovam paleontologii. Vyp. 1 (Materials to / Fundamentals of Paleontology. Vol. 1), Korde, K.B., Ed., Moscow: Paleontol. Inst. Akad. Nauk SSSR, 1957, pp. 67鈥?4.
  6. Korde, K.B., / Vodorosli kembriya (Cambrian Algae), Tr. Paleontol. Inst., vol. 139, Moscow: Nauka, 1973.
  7. Krasnopeeva, P.S., Algae and archaeocyaths from the oldest formations of the Potekhino district in Khakassia, in / Mat-ly po geologii Krasnoyarskogo kraya (Materials to Geology of the Krasnoyarsk Region), Usov, M.A., Ed., Tomsk: Zap.-Sib. Geol. Trest, 1937.
  8. Luchinina, V.A., Cambrian algoflora: Association of various microorganism groups, / Paleontol. J., 2013, vol. 47, no. 9, pp. 989鈥?96. CrossRef
  9. Luchinina, V.A. and Tikhomirova, N.S., On a new preservation form of Early Cambrian algae and their ultrastructure, in / Izvestkovye vodorosli i stromatolity: sistematika, biostratigrafiya, fatsial鈥檔yi analiz: sbornik nauchnykh trudov (Calcareous Algae and Stromatolites: Systematics, Biostratigraphy, Facial Analysis: Collection of Scientific Papers), Dubatolov, V.N. and Moskalenko, T.A., Eds., Novosibirsk: Nauka, 1988, pp. 12鈥?4.
  10. Luchinina, V.A. and Terleev, A.A., Peculiarities in the development of Early Cambrian calcareous algae on the Siberian Platform, / Acta Micropalaeontol. Sin., 2003, vol. 20, no. 1, pp. 31鈥?8.
  11. Luchinina, V.A. and Terleev, A.A., The morphology of the genus / Epiphyton Bornemann, / Geol. Croatica, 2008, vol. 61, nos. 2鈥?, pp. 105鈥?11.
  12. Luchinina, V.A., A contribution to the systematics of the genus / Proaulopora Vologdin, in / Vodorosli paleozoya i mezozoya Sibiri: K III Mezhdunarodnoi palinologicheskoi konferentsii SSSR (Algae of the Paleozoic and Mesozoic of Siberia: For III International Palynological Conference of the USSR), Moscow: Nauka, 1971, pp. 5鈥?.
  13. Luchinina, V.A., Paleoalgology at the transition from the cyanobacterial (stromatolite) to algal ecosystem as exemplified by the Cambrian sediments of the Siberian platform, / Rifogennye formatsii i rify v evolyutsii biosfery, (Reef-Building Formations and Reefs in the Evolution of the Biosphere), Rozhnov, S.V., Ed., Moscow: Paleontol. Inst. Ross. Akad. Nauk, 2011, pp. 26鈥?7.
  14. Luchinina, V.A., / Renalcis and / Epiphyton as different stages in the life cycle of calcareous algae, / Paleontol. J., 2009, vol. 43, no. 4, pp. 463鈥?68. CrossRef
  15. Maslov, V.P., / Iskopaemye izvestkovye vodorosli SSSR (Fossil Calcareous Algae of the USSR), Tr. Geol. Inst. Akad. Nauk SSSR, vol. 160, Moscow: Akad. Nauk SSSR, 1956.
  16. Pratt, B.R., / Epiphyton and / Renalcis-diagenetic microfossils from calcification of coccoid blue-green algae, / J. Sediment. Res., 1984, vol. 54, no. 3, pp. 948鈥?71.
  17. Pratt, B.R., The origin, biota, and evolution of deep-water mud-mounds, in / Carbonate Mud-Mounds; Their Origin and Evolution, Monty, C.L.V., Bosence, D.W., Bridges, P.H., and Pratt, B.R., Eds., Spec. Publ. Int. Assoc. Sedimentol., vol. 23, Oxford: Blackwell, 1995, pp. 49鈥?23. CrossRef
  18. Pratt, B.R., Spincer, B.R., Wood, R.A., and Zhuravlev, A.Yu., Ecology and evolution of Cambrian reefs, in / The Ecology of the Cambrian Radiation, New York: Columbia Univ. Press, 2001, pp. 254鈥?74.
  19. Pyatiletov, V.G., Luchinina, V.A., Shenfil鈥? V.Yu., and Yakshin, M.S., New data on the ancient algae of Siberia, / Dokl. Akad. Nauk SSSR, 1981, vol. 261, no. 4, pp. 982鈥?83.
  20. Riding, R., Calcified Cyanobacteria, in / Calcareous Algae and Stromatolites, Riding, R., Ed., Berlin: Springer-Verlag, 1990, pp. 55鈥?7.
  21. Riding, R., Calcified algae and bacteria, in / The Ecology of the Cambrian Radiation, Zhuravlev, A.Yu. and Riding, R., Eds., New York: Columbia Univ. Press, 2001, pp. 445鈥?73.
  22. Shkol鈥檔ik, E.L., Zhegallo, E.A., Baturin, G.N., Bogatyrev, B.A., Haber, M., Gerasimenko, L.M., Golovin, D.I., Eganov, E.A., Jelen鈥? S., Zhegallo, E.A., Yin Leimin, Kovalenker, V.A., Kruglyakov, V.V., Kukeshov, V.N., Machabeli, G.A., Melnikov, M.E., Novikov, V.M., Orleanskii, V.K., Pakhnevich, A.脗., Slukin, A.D., Khamkhadze, N.I., Sharkov, A.A., and Yubko, V.M., / Issledovanie margantsevoi, zhelezomargantsevoi mineralizatsii raznykh prirodnykh obstanovok metodami skaniruyushchei elektronnoi mikroskopii (SEM Study of Manganese, Ferro-manganese Mineralization of Different Natural Environments), Baturin, G.N., Ed., Moscow: Eslan, 2012.
  23. Taylor, T.N., Taylor, E.L., and Krings, M., / Paleobotany: The Biology and Evolution of Fossil Plants, Amsterdam: Academic Press, 2nd ed., 2009.
  24. Terleev, A.A. and Luchinina, V.A., New facts to establish the nature of the genus / Epiphyton Bornemann, 1886, / Novosti Paleontol. Stratigr., 2000, nos. 2鈥?, pp. 173鈥?77.
  25. Terleev, A.A., Tokarev, D.A., Luchinina, V.A., Simonov, V.A., and Stupakov, S.I., Cyanobacteria, algae in basalts and iron-siliceous sediments of the Lower Cambrian Tumat-Taiga Formation of the Kyzyl-Tashtyg ore deposit (eastern Tuva), in / Vodorosli v evolyutsii biosfery. Mat-ly 1 paleoal鈥檊ologicheskoi konf., 25鈥?8 fevralya 2013 g., Moskva (Algae in Biosphere Evolution: Contributions to the First Palaeoalgological Conference, Moscow, February 25鈥?8, 2013), Moscow: Paleontol. Inst. Ross. Akad. Nauk, 2013, pp. 141鈥?43.
  26. Ulitina, L.M., Bolshakova, L.N., and Kopaevich, G.V., The distribution patterns of stromatoporoids, rugose corals, and bryozoans in the Paleozoic section of the Djinset Uluu mountain ridge (Goby Altay), in / Paleontologiya i biostratigrafiya Mongolii (Paleontology and Biostratigraphy of Mongolia), Tr. Sovm. Sov.-Mongol. Paleontol. Eksp., vol. 3, Moscow: Nauka, 1976, pp. 327鈥?40.
  27. Vologdin, A.G., / Drevneishie vodorosli SSSR (The Oldest Algae of the USSR), Moscow: Akad. Nauk SSSR, 1962.
  28. Zhuravleva, I.T., Repina, L.N., Yaskovich, B.V., Khairullina, T.I., Poniklenko, I.A., and Luchinina, V.A., / K poznaniyu rannego kembriya Yuzhnogo Tyan鈥?Shanya (A Contribution to the Knowledge of the Early Cambrian of Southern Tian Shan), Tashkent: FAN, 1970.
  
• 刊物主题：Paleontology;
• 出版者：Springer US
• ISSN：1555-6174

文摘

In this paper we discuss the mineralization features of Vendian-Early Paleozoic algae, preserved in several varieties: silicified, organic-walled, calcified, and sometimes partially phosphatized. Amongst these, the calcified taxa of the Chlorophyta and Rhodophyta divisions were dominant. Calcareous algae were subjected to mineralization twice: the primary structure arose during their lifetime, while the second carbonate cover formed as a result of calcium deposition on the dead thalli by bacterial-cyanobacterial associations acting as catalysts. In cases when algal fossils are found in localities near ore deposits, their porous carbonate envelope can change color depending on the prevalent chemical elements in the solution.