Abstract
Recent molecular clock studies place the origin of phylum Cnidaria within the Cryogenian Period (ca. 850–635 Ma), with the split between the two subphyla (Anthozoaria and Medusozoa) likewise occurring during this time interval. However, the oldest cnidarian macrofossils, all medusozoans, occur in rocks of the late Ediacaran Period (ca. 560–541 Ma). Lightly skeletonized Corumbella werneri, currently known from late Ediacaran strata of Brazil, Paraguay and Nevada (USA), has been allied with coronate and conulariid scyphozoans, but it also shares gross morphological similarities with Carinachites spinatus, a possible conulariid from Cambrian Stage 1 (China), and it may be compared with Sinotubulites and Wutubus annularis from the late Ediacaran Dengying Formation (China). The strongest evidence of affinity with coronate scyphozoans is exhibited by Paraconularia sp. from a Corumbella-bearing shale interval in the latest Ediacaran Tamengo Formation of central Brazil. Furthermore, Paraconularia sp. from this rock unit establishes conulariids as a cnidarian clade that crossed the Proterozoic-Phanerozoic boundary. Finally, Haootia quadriformis from the late Ediacaran lower Fermeuse and Trepassy formations (southeastern Newfoundland, Canada) exhibits intriguing gross morphological similarities to extant staurozoans and may represent the earliest record of metazoan musculature. Together, C. werneri and latest Ediacaran Paraconularia sp. fix the split between the medusozoan classes Cubozoa and Scyphozoa at no later than ca. 543 Ma. If H. quadriformis was indeed a staurozoan or stem staurozoan, then this fossil taxon fixes the split between the class Staurozoa and all other medusozoan cnidarians at no later than ca. 560 Ma.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
References
Antcliffe JB, Brasier MD (2007) Charnia and sea pens are poles apart. J Geol Soc 164:49–51
Babcock LE, Feldmann RM (1986) Devonian and Mississippian conulariids of North America. Part B. Paraconularia, Reticulaconularia, new genus and organisms rejected from Conulariida. Ann Carnegie Mus 55:411–479
Babcock LE, Grunow AM, Sadowski AR, Leslie SA (2005) Corumbella, an Ediacaran-grade organism from the Late Neoproterozoic of Brazil. Palaeogeogr Palaeoclimatol Palaeoecol 220:7–18
Cai Y, Xiao S, Hong H, Yuan X (2015) New material of the biomineralizing tubular fossil Sinotubulites from the late Ediacaran Dengying formation, South China. Precambrian Res 261:12–24
Chen J-Y, Oliveri P, Gao F et al (2002) Precambrian animal life: probable developmental and adult cnidarian forms from southwest China. Dev Biol 248:182–196. doi:10.1006/dbio.2002.0714
Chen Z, Zhou C, Xiao S et al (2014) New Ediacara fossils preserved in limestone and their ecological implications. Sci Rep. doi:10.1038/srep04180
Conway Morris S, Chen M (1992) Carinachitiids, hexangulaconulariids, and Punctatus: problematic metazoans from the Early Cambrian of South China. J Paleontol 66:384–385
Cortijo I, Cai Y, Hong H et al (2015) Life history and autecology of an Ediacaran index fossil: development and dispersal of Cloudina. Gondwana Res 28:419–424
Fairchild TR, Sanchez EAM, Pacheco MLAF, Leme JM (2012) Evolution of Precambrian life in the Brazilian geological record. Int J Astrobiology 11:309–323
Fedonkin M, Gehling JG, Grey K et al (2007) The rise of animals. Johns Hopkins University Press, Baltimore
Ford RC, Van Iten H, Clark GR III (2016) Microstructure and composition of the periderm of conulariids. J Paleontol (in press)
Gaucher C, Boggiani PC, Sprechmann P et al (2003) Integrated correlation of the Vendian to Cambrian Arroyo del Soldado and Corumbá Groups (Uruguay and Brazil): palaeogeographic, palaeoclimatic and palaeobiologic implications. Precambrian Res 120:241–278
Glaessner MF, Wade M (1966) The late Precambrian fossils from Ediacara, South Australia. Palaeontology 9:599–628
Hagadorn JW, Waggoner B (2000) Ediacaran fossils from the southwestern Great Basin, United States. J Paleontol 74:349–359
Hahn G, Hahn R, Leonardos OH et al (1982) Körporlich erhaltene Scyphozoen-Reste aus dem Jungpräkambrium Brasiliens. Geol Paläontol 16:1–18
Ivantsov AY, Fedonkin MA (2002) Conulariid-like fossil from the Vendian of Russia: a metazoan clade across the Precambrian-Cambrian boundary. Palaeontology 45:1219–1229
Laflamme M, Darroch SAF, Tweedt SM et al (2013) The end of the Ediacara biota: extinction, biotic replacement, or Cheshire Cat? Gondwana Res 23:558–573. doi:10.1016/j.gr.2012.11.004
Leme JM, Simões MG, Rodrigues SC et al (2008) Cladistic analysis of the suborder Conulariina Miller and Gurley, 1896 (Cnidaria, Scyphozoa; Vendian Triassic). Palaeontology 51:649–662
Leme JM, Van Iten H, Simões MG et al (2013) A new Ediacaran conulariid from the Tamengo Formation, Corumbá Group, Brazil, and the deep Precambrian evolutionary history of cnidarians. Corumbá Meeting 2013. The Neoproterozoic Paraguay Fold Belt (Brazil): glaciation, iron-manganese formation and biota. Universidade de Brasilia, Brasília
Liu AG, Matthews JJ, Menon LR et al (2014) Haootia quadriformis n. gen., n. sp., interpreted as a muscular cnidarian impression from the Late Ediacaran period (approx. 560 Ma). Proc R Soc B. doi:10.1098/rspb.2014.1202
Liu AG, Matthews JJ, Menon LR et al (2015) The arrangement of possible muscles fibres in the Ediacaran taxon Haootia quadriformis. Proc R Soc B. doi:10.1098/rspb.2014.2949
Miranda LS, Collins AG, Marques AC (2015) Is Haootia quadriformis related to extant Staurozoa (Cnidaria)? Evidence from the muscular system reconsidered. Proc R Soc B. doi:10.1098/rspb.2014.2396
Moczyłowska M, Westall F, Foucher F (2014) Microstructure and biogeochemistry of the organically preserved Ediacaran metazoan Sabellidites. J Paleontol 88:224–239
Muscente AD, Xiao S (2015) New occurrences of Sphenothallus in the lower Cambrian of South China: implications for its affinities and taphonomic demineralization of shelly fossils. Palaeogeogr Palaeoclimatol Palaeoecol 437:141–164
Pacheco MLAF, Leme JM, Machado AF (2011) Taphonomic analysis and geometric modeling for the reconstruction of the Ediacaran metazoan Corumbella werneri Hahn et al. 1982 (Tamengo Formation, Corumbá Group, Brazil). J Taphonomy 9:269–283
Pacheco MLAF, Galante D, Rodrigues F et al (2015) Insights into the skeletonization, lifestyle, and affinity of the unusual Ediacaran fossil Corumbella. PLoS One. doi:10.1371/journal.pone.0114219.g006
Park E, Hwang D-S, Lee S-J et al (2012) Estimation of the divergence times in cnidarian evolution based on mitochondrial proteincoding genes and the fossil record. Mol Phylogenet Evol 62:329–345
Sinclair GW (1942) The Chazy Conularida and their congeners. Ann Carnegie Mus 29:219–240
Van Iten H, Fitzke JA, Cox RS (1996) Problematical fossil cnidarians from the Upper Ordovician of the north-central USA. Palaeontology 39:1037–1064
Van Iten H, Vhylasova Z, Zhu M-Y, Zhuo E-J (2005a) Widespread occurrence of microscopic pores in conulariids. J Paleontol 79:400–407
Van Iten H, Leme JM, Rodrigues SC, Simões MG (2005b) Reinterpretation of a conulariid-like fossil from the Vendian of Russia. Palaeontology 48:619–622
Van Iten H, Leme JM, Simões MG et al (2006a) Reassessment of the phylogenetic affinities of conulariids (?Ediacaran-Triassic) within the subphylum Medusozoa (phylum Cnidaria). J Syst Palaeontology 4:109–118
Van Iten H, Lichtenwalter M, Leme JM, Simões MG (2006b) Possible taphonomic bias in the preservation of phosphatic macroinvertebrates in the uppermost Maquoketa Formation (Upper Ordovician) of northeastern Iowa (north-central USA). J Taphonomy 4:207–220
Van Iten H, Moussa K, Yahaya M (2008) Conulariids of the upper Talak Formation (Mississippian, Visean) of northern Niger (West Africa). J Paleontol 82:178–182
Van Iten H, Leme JM, Marques AC, Simões MG (2013) Alternative interpretations of some earliest Ediacaran fossils from China. Acta Palaeontol Pol 58:11–113
Van Iten H, Marques AC, Leme JM et al (2014a) Origin and early evolution of the phylum Cnidaria Verrill: major developments in the analysis of the taxon’s Proterozoic-Cambrian history. Palaeontology 57:677–690
Van Iten H, Burkey MH, Leme JM, Marques AC (2014b) Cladistics and mass extinctions: the example of conulariids (Scyphozoan, Cnidaria) and the End Ordovician Extinction Event. Geol Foren Stock For 135(4):1–6. doi:10.1080/11035897.2014.880506
Vinn O, Zaton M (2012) Inconsistencies in proposed annelid affinities of early biomineralized organism Cloudina (Ediacaran): structural and ontogenetic evidences. Carnets de Géologie 2012:39–47
Wade M (1972) Hydrozoa and Scyphozoa and other medusoids from the Precambrian Ediacara fauna, South Australia. Palaeontology 15:197–225
Waggoner B (2003) The Ediacaran biotas in space and time. Integr Comp Biol 43:104–113. doi:10.1093/icb/43.1.104
Warren LV, Pacheco MLAF, Fairchild TR et al (2012) The dawn of animal skeletogenesis: ultrastructural analysis of the Ediacaran metazoan Corumbella werneri. Geology 40:691–694
Young GA, Hagadorn JW (2010) The fossil record of cnidarian medusae. Palaeoworld 19:212–221
Zapata F, Goetz FE, Smith AS et al (2015) Phylogenomic analyses support traditional relationships within Cnidaria. PLoS One 10(10), e0139068. doi:10.1371/journal.pone.0139068
Acknowledgments
HVI thanks S. Goffredo and Z. Dubinsky for inviting him to submit this contribution, and Li Guo-Xiang and Zhu Mao-Yan (Nanjing Institute of Geology and Palaeontology, China; NIGP) for reading our manuscript. This chapter was written during HVI’s sabbatical leave in the NIGP with the support of research grants from Hanover College (HVI) and the National Basic Research Program of China (Grant No. 2013CB835006) and the Natural Science Foundation of China (ZM-Y). ACM received financial support from Fundação de Amparo à Pesquisa do Estado de São Paulo – FAPESP (2011/50242-5) and CNPq (305805/2013-4; 445444/2014-2). JML received financial support from Fundação de Amparo à Pesquisa do Estado de São Paulo – FAPESP (2013/17835-8). Line drawings were prepared by W. Soares (Fig. 3.1b) and P. Busana (Figs. 3.1e, 3.3c, f, g).
Author information
Authors and Affiliations
Corresponding author
Editor information
Editors and Affiliations
Rights and permissions
Copyright information
© 2016 Springer International Publishing Switzerland
About this chapter
Cite this chapter
Van Iten, H. et al. (2016). Origin and Early Diversification of Phylum Cnidaria: Key Macrofossils from the Ediacaran System of North and South America. In: Goffredo, S., Dubinsky, Z. (eds) The Cnidaria, Past, Present and Future. Springer, Cham. https://doi.org/10.1007/978-3-319-31305-4_3
Download citation
DOI: https://doi.org/10.1007/978-3-319-31305-4_3
Published:
Publisher Name: Springer, Cham
Print ISBN: 978-3-319-31303-0
Online ISBN: 978-3-319-31305-4
eBook Packages: Biomedical and Life SciencesBiomedical and Life Sciences (R0)