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A new species of agglutinated tube, Cryptosiphon oboloides sp. nov., is described from the Furongian of Estonia. The agglutinated tubes are composed of pieces of lingulate shells that are placed to form an overall pattern. The studied agglutinated tube strongly resembles cases of modern caddisfly larvae, though we do not suggest any phylogenetic affinity to caddisflies. The tubes originally contained an organic inner lining with a sticky external surface that enabled worms to glue on shell fragments and sand grains. The relatively well-arranged grains in the tube wall suggest that the animal actively assisted in gluing the shell fragments, orienting, and finding the right place for them. It is possible that worms capable of building agglutinated tubes from shell material originated in Baltica and later dispersed to the Armorican Terrane Assemblage and other regions in the Early to Middle Ordovician.
Czasopismo
Rocznik
Tom
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art. no. e41
Opis fizyczny
Bibliogr. 27 poz., rys.
Twórcy
autor
- Department of Geology, University of Tartu, Estonia
autor
- Natural History Museum, University of Tartu, Estonia
autor
- Geology Department, Faculty of Science, Alexandria University, Egypt
autor
- College of Science, King Saud University, Riyadh, Kingdom of Saudi Arabia
autor
- College of Science, King Saud University, Riyadh, Kingdom of Saudi Arabia
Bibliografia
- 1. Becker-Kerber, B., Horodyski R.S., del Mouro, L., Sedorko, D., Lehn, I., Sanchez, D.F., Fournier, J., Mazurier, A. and El Albani, A. 2021. Devonian agglutinated polychaete tubes: all in all it’s just another grain in the wall. Proceedings of the Royal Society, B 288, 20211143.
- 2. Cocks, L.R.M. and Torsvik, T.H. 2021. Ordovician palaeogeography and climate change. Gondwana Research, 100, 53–72.
- 3. Ettensohn, F.R. 1981. Crininicaminus haneyensis, a new agglutinated worm tube from the Chesterian of east-central Kentucky. Journal of Paleontology, 55, 479–482.
- 4. Fischer, D.W. 1962. Small conoidal shells of uncertain affinities. In: Moore, R.C. (Ed.), Treatise on Invertebrate paleontology. Part W, 130–143. Geological Society of America and University of Kansas Press; Lawrence.
- 5. Fournier, J., Etienne, S. and Le Cam, J.-B. 2010. Inter- and intraspecific variability in the chemical composition of the mineral phase of cements from several tube-building polychaetes. Geobios, 43, 191–200.
- 6. Grube, A. 1850. Die Familien der Anneliden. Archiv für Naturgeschichte, 16, 249–364.
- 7. Kirjanov, V.V. 1968. Palaeontological remains and stratigraphy of the Baltic Group deposits in Volhynia-Podolia, 24 pp. Naukova Dumka; Kiev. [In Russian]
- 8. Lamarck, J.B.P.A. 1809. Philosophie zoologique, vol. 1, 442 pp. + vol. 2, 450 pp. Dentu; Paris.
- 9. Linnæus, C. 1767. Systema naturae, per regna tria naturae, secundum classes, ordines, genera, species, cum caracteribus, differentiis, synonymis, locis. Tomus I. Pars 2. Editio duodecima, reformata, 533–1327. L. Salvii; Holmiae.
- 10. Lipps, J.H. and Sylvester, A.G. 1968. The enigmatic Cambrian fossil Volborthella and its occurrence in California. Journal of Paleontology, 42, 329–336.
- 11. Mancin, N., dell’Acqua, F., Riccardi, M.P., Lo Bue, G. and Marchini, A. 2022. Fractal analysis highlights analogies in arenaceous tubes of Sabellaria alveolata (Metazoa, Polychaeta) and agglutinated tests of foraminifera (Protista). PLoS ONE, 17 (8), e0273096.
- 12. Mens, K. and Pirrus, E. 1997. Cambrian. In: Rauaks,A. and Teedumäe, A. (Eds), Geology and Mineral Resources of Estonia, 39–51. Estonian Academy Publishers; Tallinn.
- 13. Mens, K., Viira, V., Paalits, I. and Puura, I. 1993. Upper Cambrian biostratigraphy of Estonia. Proceedings of the Estonian Academy of Sciences, Geology, 42, 148–159.
- 14. Mouro, L.D., Zatoń, M., Fernandes, A.C.S. and Waichel, B.L. 2016. Larval cases of caddisfly (Insecta: Trichoptera) affinity in Early Permian marine environments of Gondwana. Scientific Reports, 6, 19215.
- 15. Muir, L.A., Botting, J.P., Lefebvre, B., Upton, C. and Zhang, Y. 2019. Agglutinated tubes as a feature of Early Ordovician ecosystems. Palaeoworld, 28, 96–109.
- 16. Muir, L.A., Botting, J.P., Walker, S.N.A., Schiffbauer, J.D. and MacGabhann, B.A. 2022. Onuphionella corusca sp. nov.: an early Cambrian-type agglutinated tube from Upper Ordovician strata of Morocco. In: Hunter, A.W., Álvaro, J.J., Lefebvre, B., Van Roy, P. and Zamora, S. (Eds), The Great Ordovician Biodiversification Event: Insights from the Tafilalt Biota, Morocco. Geological Society Special Publications, 485, 297–309.
- 17. Popov, L.E. and Khazanovich, K.K. 1985. New data on the strati graphy of the Cambrian–Ordovician phosphorite deposits in the northwest of the Russian Plate. In: Khazanovich, K.K. (Ed.), Problems of development and rational use of the resources of the Baltic Basin phosphorite, 38–47.
- 18. Trudy Geologicheskogo Instituta; Moscow. Prantl, F. 1948. Some terebelloid remains from the Ordovician of Bohemia. Věstník Královské české Společnosti Nauk, Třída matematicko-přírodovědná, 8, 1–8.
- 19. Schmidt, F. 1888. Über eine neuentdeckte untercambrische Fauna in Estland. Académie Impériale des Sciences de St.-Pétersbourg Mémoires, VIIe Série, 36, 1–27.
- 20. 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.
- 21. Vinn, O. and Luque, J. 2013. First record of a pectinariid-like (Polychaeta, Annelida) agglutinated worm tube from the Late Cretaceous of Columbia. Cretaceous Research, 41, 107–110.
- 22. Vinn, O. and Mutvei, H. 2009. Calcareous tubeworms of the Phanerozoic. Estonian Journal of Earth Sciences, 58, 286–296.
- 23. Vinn, O., Zabini, C., Sene-Silva, G., Kirsimäe, K. and SusanMarcos, L. 2016. Possible polychaete tube worms from the Late Emsian (Early Devonian) of the Parana Basin, Brazil. Acta Palaeontologica Polonica, 61, 627–632.
- 24. Wiggins, G.B. 2015. Caddisflies: The Underwater Architects, 300 pp. University of Toronto Press; Toronto.
- 25. Wilson, M.A. and Taylor, P.D. 2001. Palaeoecology of hard substrate faunas from the Cretaceous Qahlah Formation of the Oman Mountains. Palaeontology, 44, 21–41.
- 26. Zatoń, M. and Bond, D.P.G. 2016. Insight into tube-building behaviour and palaeoecology of some agglutinating worms from the Upper Devonian of Nevada, USA. Palaeogeography, Palaeoclimatology, Palaeoecology, 445, 138–146.
- 27. Zatoń, M., Kano, Y., Wilson, M.A. and Filipiak, P. 2012. Unusual tubular fossil associated with microbial crusts from the middle Jurassic of Poland: agglutinated polychaete worm tubes. Palaios, 27, 550–559
Uwagi
Opracowanie rekordu ze środków MNiSW, umowa nr POPUL/SP/0154/2024/02 w ramach programu "Społeczna odpowiedzialność nauki II" - moduł: Popularyzacja nauki (2026).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-d8288231-ba03-4258-935f-1d9d43bd4dd5
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