PL EN


Preferencje help
Widoczny [Schowaj] Abstrakt
Liczba wyników
2016 | 61 | 3 |

Tytuł artykułu

Possible polychaete tubeworms from the Late Emsian (Early Devonian) of the Parana Basin, Brazil

Autorzy

Treść / Zawartość

Warianty tytułu

Języki publikacji

EN

Abstrakty

EN
Plastically deformed and silicified worm tubes from the Late Emsian (Early Devonian) of the Parana Basin are described herein as a new species and genus of annelid worms Annulitubus mutveii gen. et sp. nov. The tubes are straight and ornamented by smooth rings. Their microstructure is homogenous, which most likely is a diagenetic alteration. The characteristic early diagenetic compression of the tubes may point out to their original elastic organic tube wall. We cannot state it with full confidence but the most likely tube producers were tube-dwelling polychaete annelids, which were otherwise uncommon in the Paleozoic times.

Słowa kluczowe

Wydawca

-

Rocznik

Tom

61

Numer

3

Opis fizyczny

p.627-632,fig.,ref.

Twórcy

Bibliografia

  • Berke, S.K. and Woodin, S.A. 2008. Tube decoration may not be cryptic for Diopatracuprea (Polychaeta: Onuphidae). Biology Bulletin 214: 50–56.
  • Bosetti, E.P. Grahn, Y., Horodyski, R.S., and Mauller, M. P. 2012. The first recorded decline of the Malvinokaffric Devonian fauna in the Paraná Basin (southern Brazil) and its cause; taphonomic and fossil evidences. Journal of South American Earth Sciences 37: 228–241.
  • Boyce, A.J., Little, C.T.S., and Russel, M.J. 2003. A new fossil vent biota in the Ballynoe barite deposit, Silvermines, Ireland: evidence for intracratonic sea-floor hydrothermal activity about 352 Ma. Economic Geology 98: 649–656.
  • Clarke, J.M. 1913. Fósseis devonianos do Paraná. Monographia do Serviço Geológico e Mineralógico do Brazil 1: 1−353.
  • Clayton, C.J. 1986. The chemical environment of flint formation in Upper Cretaceous chalk. In: G.D.G. Sieveking and M.B. Hart (eds.), The Scientific Study of Flint and Chert, 43–54. Cambridge University Press, Cambridge.
  • Conway Morris, S. and Peel, J.S. 2008. The earliest annelids: lower Cambrian polychaetes from the Sirius Passet Lagerstätte, Peary Land, North Greenland. Acta Palaeontologica Polonica 53: 137–148.
  • Cortijo, I., Cai, Y., Hua, H., Schiffbauer, J.D., and Xiao, S. 2015a. Life history and autecology of an Ediacaran index fossil: Development and dispersal of Cloudina. Gondwana Research 28: 419–424.
  • Cortijo, I., Martí Mus, M., Jensen, S., and Palacios, T. 2015b. Late Ediacaran skeletal body fossil assemblage from the Navalpinoanticline, central Spain. Precambrian Research 267: 186–195.
  • Day, J.H. 1967. A monograph on the Polychaeta of Southern Africa. British Museum (Natural History) 656: 1–878.
  • Dill, H.G. 2001. The geology of aluminium phosphates and sulphates of the alunite group minerals: a review. Earth-Science Reviews 53: 35–93.
  • Fauchald, K. 1977. The polychaete worms. Definitions and keys to the orders, families and genera. Natural History Museum of Los Angeles County, Science Series 28: 1–188.
  • Georgieva, M.N., Little, C.T.S., Ball, A.D., and Glover, A.G. 2015. Mineralization of Alvinella polychaete tubes at hydrothermal vents. Geobiology 13: 152–169.
  • Goedert, J.L., Peckmann, J., and Reitner, J. 2000. Worm tubes in an allochthonous cold-seep carbonate from Lower Oligocene rocks of Western Washington. Journal of Paleontology 74: 992–999.
  • Grube, A.E. 1850. Die Familien der Anneliden. Archiv für Naturgeschichte, Berlin 16: 249–364.
  • Hall, J. 1847. Palaeontology of New York. Volume 1. Containing Descriptions of the Organic Remains of the Lower Division of the New York System. 339 pp. C. Van Benthuysen, Albany.
  • Horowitz, D. 1967. Diagenetic replacement and solution of biogenic phosphate by silica. Journal of Sedimentary Petrology 37: 1238–1240.
  • Ippolitov, A.P., Vinn, O., Kupriyanova, E.K., and Jäger M. 2014. Written in stone: history of serpulid polychaetes through time. Memoirs of Museum Victoria 71: 123–159.
  • Lamarck, J.-B. 1809. Memoires sur les fossiles des environs de Paris. Annales du Museum d’Histoire Naturelle 1: 299–312.
  • Lange, F.W. and Petri, S. 1967. The Devonian of the Paraná Basin. Boletim Paranaense de Geociências 21−22: 5–55.
  • Little, C.T.S., Herrington, R.J., Maslennikov, V.V., and Zaykov, V.V. 1998. The fossil record of hydrothermal vent communities. Geological Society of London, Special Publications 148: 259–270.
  • Little, C.T.S., Herrington, R.J., Maslennikov, V.V., Morris, N.J., and Zaykov, V.V. 1997. Silurian hydrothermal vent community from the southern Urals, Russia. Nature 385: 146–148.
  • Little, C.T.S., Maslennikov, V.V., Morris, N.J., and Gubanov, A.P. 1999. Two Palaeozoic hydrothermal vent communities from the southern Ural mountains, Russia. Palaeontology 42: 1043–1078.
  • Luci, L., Garberoglio, R.M., and Lazo, D.G. 2013. Serpulids and other calcareous tube-dwelling encrusting polychaetes from the Early Cretaceous Agrio Formation (Neuquén Basin, Argentina). Geobios 46: 213–224.
  • Maliva, R.G., Knoll, A.H., and Siever, R. 1989. Secular change in chert distribution: A reflection of evolving biological participation in the silica cycle. Palaios 4: 519–532.
  • Merz, R.A. 2015. Textures and traction: how tube-dwelling polychaetes get a leg up. Invertebrate Biology 134: 61–77.
  • Milani, E.J., França, A.B., and Schneider, R.L. 1994. Bacia do Paraná. Boletim Geociências da Petrobrás, Rio de Janeiro 8: 69–82.
  • Milani, E.J. and Ramos, V.A. 1998. Orogenias Paleozóicas no Domínio Sul-Ocidental do Gondwana e os ciclos de subsidência da Bacia do Paraná. Revista Brasileira de Geociências, São Paulo 28: 473–484.
  • Milani, E.J., Melo, J.H.G., Souza, P.A., Fernandes, L.A., and França, A.B. 2007. Bacia do Paraná. Boletim de Geociências da Petrobrás 15: 265–287.
  • Muscente, A.D. and Shuhai, X. 2015. New occurrences of Sphenothallus in the lower Cambrian of South China: Implications for its affinities and taphonomic demineralization of shelly fossils. Palaeogeography, Palaeoclimatology, Palaeoecology 437: 141–164.
  • Peckmann, J., Little, C.T.S., Gill, F., and Reitner, J. 2005. Worm tube fossils from the Hollard Mound hydrocarbon-seep deposit, Middle Devonian, Morocco: Palaeozoic seep-related vestimentiferans? Palaeogeography, Palaeoclimatology, Palaeoecology 227: 242–257.
  • Petri, S. and Fúlfaro, V.J. 1983. Geologia do Brasil. 631 pp. EDUSP, São Paulo.
  • Raymond, L.A. 2002. Cherts, evaporites, and other precipitated rocks. In: M.J. Kemp and R. Russian (eds.), Petrology: The Study of Igneous, Sedimentary, and Metamorphic Rocks, 436–447. McGraw-Hill, Boston.
  • Salter, J.W. 1856. Description of Palaeozoic Crustacea and Radiata from South Africa. Transactions of the Geological Society of London, Series 2 7: 215–224.
  • Scheffler, S.M. and Fernades, A.C.S. 2007.Crinoidea da Formação Ponta Grossa (Devoniano, Bacia do Paraná), Brasil. Arquivos Do Museu Nacional 65: 83–98.
  • Signor, P.W. and McMenamin, M.A.S. 1988. The early Cambrian worm tube Onuphionella from California and Nevada. Journal of Paleontology 62: 233–240.
  • Taylor, J.C. 1991. Computer programs for standardless quantitative analysis of minerals using the full powder diffraction profile. Powder Diffraction 6: 2–9.
  • Van Iten, H., Cox, R.S., and Mapes, R.H. 1992. New data on the morphology of Sphenothallus Hall: implications for its affinities. Lethaia 25: 135–144.
  • Vinn, O., Hove, H.A. ten, Mutvei, H., and Kirsimäe, K. 2008. Ultrastructure and mineral composition of serpulid tubes (Polychaeta, Annelida). Zoological Journal of the Linnean Society 154: 633–650.
  • Vinn, O. and Mutvei, H. 2009. Calcareous tubeworms of the Phanerozoic. Estonian Journal of Earth Sciences 58: 286–296.
  • Vinn, O. and Zatoń, M. 2012a. Inconsistencies in proposed annelid affinities of early biomineralized organism Cloudina (Ediacaran): structural and ontogenetic evidences. Carnets de Géologie CG2012_A03: 39−47.
  • Vinn, O. and Zatoń, M. 2012b. Phenetic phylogenetics of tentaculitoids—extinct problematic calcareous tube-forming organisms. GFF 134: 145–156.
  • Vinther, J., Eibye-Jacobsen, D., and Harper, D.A. 2011. An Early Cambrian stem polychaete with pygidial cirri. Biology Letters 7: 929–932.
  • Wilson, M.A., Vinn, O., and Yancey, T.E. 2011. A new microconchid tubeworm from the Lower Permian (Artinskian) of central Texas, USA. Acta Palaeontologica Polonica 56: 785–791.
  • Zalán, P.V., Wolff, S., Conceição, J.C., Marques, A., Astolfi, M.A., Vieira, I.S., Appi, V.T., and Zanotto, O.A. 1990. Bacia do Paraná. In: G.P. Raja Gabaglia and E.J. Milani (eds.), Origem e Evolução das Bacias Sedimentares, 135–168. Petrobras, Rio de Janeiro.
  • Zatoń, M. and Krawczyński, W. 2011. New Devonian microconchids (Tentaculita) from the Holy Cross Mountains, Poland. Journal of Paleontology 85: 757–769.
  • Zatoń, M., Zhuravlev, A.V., Rakociński, M., Filipiak, P., Borszcz, T., Krawczyński, W., Wilson, M.A., and Sokiran, E.V. 2014. Microconchid-dominated cobbles from the Upper Devonian of Russia: Opportunism and dominance in a restricted environment following the Frasnian–Famennian biotic crisis. Palaeogeography, Palaeoclimatology, Palaeoecology 401: 142–153.

Typ dokumentu

Bibliografia

Identyfikatory

Identyfikator YADDA

bwmeta1.element.agro-078bed63-d6db-48b0-a494-ba057f3039be
JavaScript jest wyłączony w Twojej przeglądarce internetowej. Włącz go, a następnie odśwież stronę, aby móc w pełni z niej korzystać.