Facies

, 61:17 | Cite as

The first sphinctozoan-bearing reef from an Ordovician back-arc basin

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Abstract

Although sphinctozoans, multi-chambered hypercalcified sponges, can be traced from the Cambrian, their reef-building capacity in the Early Paleozoic appears limited. The oldest sphinctozoan-coral-microbial reef‏ is documented here, from the Upper Sanqushan Formation (Late Katian) of southeast China. This is also the first report of Ordovician sphinctozoans from South China. The sponges occur in a >120-m-thick reef that is mainly constructed by calcimicrobes (Kordephyton, Renalcis, and Epiphyton) with a low abundance of in situ metazoans, predominantly sphinctozoan sponges (Corymbospongia) and rugose corals (mostly Palaeophyllum and Streptelasma). Tetradium is the only tabulate coral preserved in growth position. Crinoids and brachiopods are common reef dwellers. Dasycladacean algae are rare and probably transported and stromatactis is abundant. Bio- and litho-facies in this area as well as the characteristics of the microbialite suggest that the reef developed in a deeper subtidal setting that was unfavorable for most metazoan reef builders. In contrast to the high-energy stromatolite-sphinctozoan reefs from the Late Silurian, this case represents a low-energy community, indicating that the first reef-building sphinctozoans might have originated in a relatively deep-water environment on seamounts of a back-arc basin during the Late Ordovician.

Keywords

Sphinctozoans Microbialites Stromatactis Late Katian Back-arc basin South China 
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Notes

Acknowledgments

Financial support from the National Natural Science Foundation of China (41072002 and 41221001), China Scholarship Council (File No. 201204910171) and Postgraduate Grant Scheme from the International Association of Sedimentologists (1st session in 2014) is acknowledged. We are grateful to Prof. Baba Senowbari-Daryan (University of Erlangen-Nürnberg) and Dr. Guangxu Wang (Nanjing Institute of Geology and Palaeontology) for assistance in identifying the sphinctozoans and corals, respectively. We thank Birgit Leipner-Mata (University of Erlangen-Nürnberg) for the help with thin-sections and polished slabs, and Christian Schulbert (University of Erlangen-Nürnberg) and Kristoffer Uhl (University of Erlangen-Nürnberg) for the help with photographing. Constructive reviews by Marcelo Carrera and Maurice Tucker are greatly acknowledged.

References

  1. Adachi N, Liu J, Ezaki Y (2012) Early Ordovician stromatoporoid Pulchrilamina spinosa from South China: geobiological significance and implications for the early development of skeletal-dominated reefs. Paleontol Res 16:59–69CrossRefGoogle Scholar
  2. Adachi N, Liu J, Ezaki Y (2013) Early Ordovician reefs in South China (Chenjiahe section, Hubei Province): deciphering the early evolution of skeletal-dominated reefs. Facies 59:451–466CrossRefGoogle Scholar
  3. Aoki K, Isozaki Y, Yamamoto A, Sakata S, Hirata T (2014) Mid-Paleozoic arc granitoids in SW Japan with Neoproterozoic xenocrysts from South China: new zircon U–Pb ages by LA-ICP-MS. J Asian Earth Sci 97 (Part A):125–135Google Scholar
  4. Bian LZ, Zhou XP (1990) Calcareous algae from the Sanqushan Formation (Upper Ordovician) at the border area between Zhejiang Province and Jiangxi Province. J Nanjing Univ (Earth Sci) 2:1–23 (in Chinese with English abstract) Google Scholar
  5. Bian LZ, Fang YT, Huang ZC (1996) On the types of Late Ordovician reefs and their characteristics in the neighbouring regions of Zhejiang and Jiangxi Provinces, South China. In: Fan JS (ed) The ancient organic reefs of China and their relations to oil and gas. Marine Press, China, pp 54–75 (in Chinese) Google Scholar
  6. Carrera MG, Botting JR (2008) Evolutionary history of Cambrian spiculate sponges: implications for the Cambrian evolutionary fauna. Palaios 23:124–138CrossRefGoogle Scholar
  7. Carrera MG, Rigby JK (1999) Biogeography of Ordovician sponges. J Paleontol 73:26–37Google Scholar
  8. Carrera MG, Rigby JK (2004) Sponges. In: Webby BD, Paris F, Droser ML, Percival IG (eds) The great Ordovician biodiversification event. Columbia University Press, New York, pp 102–111Google Scholar
  9. Charvet J (2013) The Neoproterozoic–Early Paleozoic tectonic evolution of the South China Block: an overview. J Asian Earth Sci 74:198–209CrossRefGoogle Scholar
  10. Chen X, Rong JY (1992) Ordovician plate tectonics of China and its neighbouring regions. In: Webby BD, Laurie L (eds) Global Perspectives on Ordovician Geology. Balkema, Rotterdam, pp 177–291Google Scholar
  11. Chen X, Rong JY, Wang XF, Wang ZH, Zhang YD, Zhan RB (1995) Correlation of the Ordovician rocks of China: charts and explanatory notes. International Union of Geological Sciences, TrondheimGoogle Scholar
  12. Chen H, Hou MC, Xu X, Tian JC (2006) Tectonic evolution and sequence stratigraphic framework in South China during Caledonian. J Chengdu Univ Technol 33:1–8 (in Chinese with English abstract) Google Scholar
  13. Cherns L, Wheeley JR (2007) A pre-Hirnantian (Late Ordovician) interval of global cooling–The Boda event re-assessed. Palaeogeogr Palaeoclim Palaeoecol 251:449–460CrossRefGoogle Scholar
  14. Choh SJ, Hong J, Sun N, Kwon SW, Park TY, Woo J, Kwon Y, Lee DC, Lee DJ (2013) Early Ordovician reefs from the Taebaek Group, Korea: constituents, types, and geological implications. Geosci J 17:139–149CrossRefGoogle Scholar
  15. Debrenne F, Reitner J (2001) Sponges, cnidarians, and ctenophores. In: Zhuravlev A, Riding R (eds) The ecology of the Cambrian radiation. Columbia University Press, New York, pp 301–325Google Scholar
  16. Debrenne F, Wood R (1990) A new Cambrian sphinctozoan sponge from North America, its relationship to Archaeocyaths and the nature of early sphinctozoans. Geol Mag 127:435–443CrossRefGoogle Scholar
  17. Elicki O (1999) Palaeoecological significance of calcimicrobial communities during ramp evolution: an example from the Lower Cambrian of Germany. Facies 41:27–39CrossRefGoogle Scholar
  18. Fagerstrom J (1984) The ecology and paleoecology of the Sclerospongiae and Sphinctozoa (sensu stricto): a review. Palaeontogr Am 54:370–381Google Scholar
  19. Finks R, Rigby J (2004) Heteractinida. In: Kaesler RL (ed) Treatise on invertebrate paleontology Part E (Revised), Porifera, vol. 3. The Geological Society of America & The University of Kansas, Lawrence, pp 557–584Google Scholar
  20. Flügel E (2004) Microfacies of Carbonate Rocks, Analysis. Springer, Berlin Heidelberg New YorkGoogle Scholar
  21. Guo LZ, Shi YS, Lu HF, Ma RS, Dong HG, Yang SF (1989) The pre-Devonian tectonic patterns and evolution of South China. J Southeast Asian Earth Sci 3:87–93CrossRefGoogle Scholar
  22. Isozaki Y (2011) Ordovician rocks in Japan. In: Gutiérrez-Marco JC, Rábano I, García-Bellido D (eds), Ordovician of the World. Cuadernos del Museo Geominero 14, Instituto Geológico y Minero de España, Madrid, pp 251–252Google Scholar
  23. Isozaki Y, Kase T (2014) The occurrence of the oarge oastropod “Pleurotomaria” Yokoyamai Hayasaka from the Capitanian (Permian) Iwaizaki Limestone in northeast Japan. Paleontol Res 18:250–257CrossRefGoogle Scholar
  24. Jiang BY, Sinclair HD, Niu YZ, Yu JH (2014) Late Neoproterozoic–Early Paleozoic evolution of the South China Block as a retroarc thrust wedge/foreland basin system. Int J Earth Sci 103:23–40CrossRefGoogle Scholar
  25. Johns RA (1998) Sponge diversity patterns in the Middle Capitan Reef of the Guadalupe Mountains, Texas, and their environmental implications. In: Armstrong FA, KellerLynn K (eds) Guadalupe Mountains Symposium proceedings. National Park Service, Guadalupe Mountains National Park, Texas, pp 279–295Google Scholar
  26. Kruse PD (1987) Further Australian Cambrian sphinctozoans. Geol Mag 124:543–553CrossRefGoogle Scholar
  27. Kruse PD (1996) Update on the northern Australian Cambrian sponges Rankenella, Jawonya and Wagima. Alcheringa 20:161–178CrossRefGoogle Scholar
  28. Kruse PD, Reitner JR (2014) Northern Australian microbial-metazoan reefs after the mid-Cambrian mass extinction. Mem Assos Australas Palaeontol 45:124–138Google Scholar
  29. Kwon SW, Park J, Choh SJ, Lee DC, Lee DJ (2012) Tetradiid-siliceous sponge patch reefs from the Xiazhen Formation (late Katian), southeast China: a new Late Ordovician reef association. Sediment Geol 267–268:15–24CrossRefGoogle Scholar
  30. Lee JH, Lee HS, Chen J, Woo J, Chough SK (2014) Calcified microbial reefs in Cambrian Series 2, North China Platform: implications for the evolution of Cambrian calcified microbes. Palaeogeogr Palaeoclim Palaeoecol 403:30–42CrossRefGoogle Scholar
  31. Li Y, Kershaw S, Mu X (2004) Ordovician reef systems and settings in South China before the Late Ordovician mass extinction. Palaeogeogr Palaeoclim Palaeoecol 205:235–254CrossRefGoogle Scholar
  32. Li ZX, Wang RC, Jahn BM (2013) Tectonic evolution, magmatism and metallogeny of the South China Craton—an introduction. J Asian Earth Sci 74:195–197CrossRefGoogle Scholar
  33. Li QJ, Li Y, Kiessling W (2015) Allogenic succession in Late Ordovician reefs from southeast China: a response to the Cathaysian orogeny. Estonian J Earth Sci 64:68–73CrossRefGoogle Scholar
  34. Liu J, Ezaki Y, Adachi N, Zhan RB (2010) Evidence for decoupling of relative abundance and biodiversity of marine organisms in the initial stage of the GOBE: a preliminary study on shellbeds of the Lower Ordovician in South China. J Earth Sci Spe Issue 21:44–48CrossRefGoogle Scholar
  35. Newton A, Soja CM (2002) Paleoenviromental implications of Silurian sponge-microbe associations from the northern Urals, Russia. Colgate Univ J Sci 34:25–44Google Scholar
  36. Pratt BR, James NP (1982) Cryptalgal-metazoan bioherms of early Ordovician age in the St George Group, western Newfoundland. Sedimentology 29:543–569CrossRefGoogle Scholar
  37. Radugin KZ, Stepanova MV (1964) Onitchatykh vodoroslyakh dokembriya severo-zapadnoy chasti Vostochnovo Sayana. 60-64 in Materialy po geologii i poleznym iskopaemym Zapadnoy Sibiri. Tomskiy Gosudarstvenniy Universitet, Tomsk (in Russian) Google Scholar
  38. Ran B, Liu S, Jansa L, Sun W, Yang D, Ye Y, Wang S, Luo C, Zhang X, Zhang C (2015) Origin of the Upper Ordovician–lower Silurian cherts of the Yangtze block, South China, and their palaeogeographic significance. J Asian Earth Sci 108:1–17CrossRefGoogle Scholar
  39. Riding R (2011) Microbialites, stromatolites, and thrombolites. In: Reitner J, Thiel V (eds) Encyclopedia of Geobiology. Springer, Berlin Heidelberg New York, pp 635–654CrossRefGoogle Scholar
  40. Rigby JK, Potter AW (1986) Ordovician Sphinctozoan sponges from the Eastern Klamath Mountains, northern California. Mem Paleontol Soc 20:1–47Google Scholar
  41. Rigby JK, Blodgett RB, Britt BB (2008a) Ordovician sponges from west-central and east-central Alaska and western Yukon Territory, Canada. Bull Geosci 83:153–168CrossRefGoogle Scholar
  42. Rigby JK, Potter AW, Anderson NK (2008b) Ordovician sponges from the Montgomery Limestone, Taylorsville area, northern Sierra Nevada, California, USA. Bull Geosci 83:299–310CrossRefGoogle Scholar
  43. Rong JY, Chen X (1987) Faunal differentiation, biofacies and lithofacies pattern of Late Ordovician (Ashgillian) in South China. Acta Palaeontol Sin 26:507–535Google Scholar
  44. Rong JY, Zhan RB, Harper DA (1999) Late Ordovician (Caradoc-Ashgill) brachiopod faunas with Foliomena based on data from China. Palaios 14:412–431CrossRefGoogle Scholar
  45. Rong JY, Zhan RB, Xu HG, Huang B, Yu GH (2010) Expansion of the Cathaysian Oldland through the Ordovician-Silurian transition: emerging evidence and possible dynamics. Sci China, Ser D Earth Sci 53:1–17CrossRefGoogle Scholar
  46. Savarese M, Mount JF, Sorauf JE, Bucklin L (1993) Paleobiologic and paleoenvironmental context of coral-bearing Early Cambrian reefs: implications for Phanerozoic reef development. Geology 21:917–920CrossRefGoogle Scholar
  47. Scrutton CT (1998) The Palaeozoic corals, II: structure, variation and palaeoecology. Proc Yorks Geol Polytech Soc 52:1–57CrossRefGoogle Scholar
  48. Senowbari-Daryan B (1991) “Sphinctozoa”: an overview Fossil and recent sponges. In: Reitner J, Keupp H (eds) Fossil and recent sponges. Springer, Berlin Heidelberg New York, pp 224–241CrossRefGoogle Scholar
  49. Senowbari-Daryan B (2005) Hypercalcified sphinctozoan sponges from Upper Triassic Norian-Rhaetian) reefs of the Nayband Formation (central and northeast Iran). Jahrb Geol Bundesanst 145:171–277Google Scholar
  50. Senowbari-Daryan B, García-Bellido DC (2002) Fossil ‘Sphinctozoa’: chambered sponges (polyphyletic). In: Hooper John NA, Van Soest Rob WM (eds) Systema porifera. Springer, Heidelberg, pp 1511–1538Google Scholar
  51. Senowbari-Daryan B, Rigby JK (2011) Part E, Revised, Volume 4, Chapter 7: Sphinctozoan and Inozoan hypercalcified sponges: an overview. Treatise Online 28:1–90Google Scholar
  52. Soja CM (1994) Significance of Silurian stromatolite–sphinctozoan reefs. Geology 22:355–358CrossRefGoogle Scholar
  53. Soja CM, Mitchell M, Newton AJ, Vendetti J, Visaggi C, Antoshkina AI, White B (2003) Paleoecology of sponge-?hydroid associations in Silurian microbial reefs. Palaios 18:225–235CrossRefGoogle Scholar
  54. Steele-Petrovich HM (2009) Biological affinity, phenotypic variation and palaeoecology of Tetradium Dana, 1846. Lethaia 42:383–392CrossRefGoogle Scholar
  55. Webby B, Rigby JK (1985) Ordovician sphinctozoan sponges from central New South Wales. Alcheringa 9:209–220CrossRefGoogle Scholar
  56. Wood R (1991) Problematic reef-building sponges. In: Simonetta AM, Morris SC (eds) The early evolution of Metazoa and the significance of problematic taxa. Cambridge University Press, Cambridge, pp 113–124Google Scholar
  57. Wood R (1995) The changing biology of reef-building. Palaios 10:517–529CrossRefGoogle Scholar
  58. Zhan RB, Rong JY, Jin J, Cocks LRM (2002) Late Ordovician brachiopod communities of southeast China. Can J Earth Sci 39:445–468CrossRefGoogle Scholar
  59. Zhang YD, Chen X, Yu GH, Dan G, Liu X (2007) Ordovician and Silurian rocks of northwest Zhejiang and northeast Jiangxi Provinces. University of Science and Technology of China Press, Hefei, SE ChinaGoogle Scholar
  60. Zhou MF, Yan DP, Kennedy AK, Li Y, Ding J (2002) SHRIMP U-Pb zircon geochronological and geochemical evidence for Neoproterozoic arc-magmatism along the western margin of the Yangtze Block, South China. Earth Planet Sci Lett 196:51–67CrossRefGoogle Scholar
  61. Zhou ZY, Yuan WW, Han NR, Zhou ZQ (2004) Trilobite faunas across the Late Ordovician mass extinction event in the Yangtze Block. In: Rong JY, Fang ZJ (eds) Mass extinction and recovery—evidences from the Palaeozoic and Triassic of South China. University of Science and Technology of China Press, Hefei, pp 127–152 (in Chinese with English abstract) Google Scholar

Copyright information

© Springer-Verlag Berlin Heidelberg 2015

Authors and Affiliations

  1. 1.GeoZentrum NordbayernUniversity of Erlangen-NürnbergErlangenGermany
  2. 2.Nanjing Institute of Geology and PaleontologyChinese Academy of SciencesNanjingChina
  3. 3.Museum für NaturkundeBerlinGermany

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