Paleontology and taphonomy of Kuphus polythalamius (Linnaeus 1767), Navab anticline, Central Iran

Iranian Journal of Earth Sciences

مقاله 6، دوره 15، شماره 3، مهر 2023، صفحه 195-201   

نوع مقاله: Original Research Paper

شناسه دیجیتال (DOI): 10.30495/ijes.2022.1955710.1741

نویسندگان

Keyvan Khaksar^{* 1}؛ Iraj Maghfouri Moghaddam²

¹Department of Experimental Science, Islamic Azad University, Qom branch, Qom, Iran

²Geology Department, Faculty of Science, Lorestan University, Lorestan, Iran

چکیده

The Burdigalian carbonate of the Central Iran contains very well-preserved specimens of Kuphus polythalamius. The tube of Kuphus polythalamius is a calcareous secretion that enables Pelecypoda to live in the mud of shallow seas. This research focusses on the Paleontology and taphonomy of the Kuphus polythalamius of the Member F (Qom Formation) in the southeast of Kashan located in the Central Iran. The Member F is 60 meters thick and composed of medium bedded limestone. The scattering of the larger benthic foraminifera in the study area indicates the existence of the Borelis melo curdica-Borelis melo melo assemblage zone of Burdigalian age. The presence of Kuphus polythalamius among the porcelaneous foraminiferal and green algal assemblage demonstrate that carbonate generation happened in warm tropical to subtropical marine. The surface of some samples contains distinct horizons of beekite, indicating a break in sedimentation, which is expanded as a silica crust on carbonate tubes.

کلیدواژه‌ها

Kuphus polythalamius؛ Beekite؛ Member F؛ Qom Formation؛ Central Iran

مراجع

1. Adams H, Adams A (1853) The genera of recent Mollusca arranged according to their organization. in-8°,  London, 661 pp.
2. Altamia MA, Shipway JR, Concepcion GP, Haygood MG, and Distel DL (2019) Thiosocius teredinicola gen. nov., sp. nov., a sulfur-oxidizing chemolithoautotrophic endosymbiont cultivated from the gills of the giant shipworm, Kuphus polythalamius, International Journal of Systematic and Evolutionary Microbiology 69(3): 638-644.
3. Amirshahkarami M, Ghabishavi A, Rahmani A (2010) Biostratigraphy and paleoenvironment of the larger benthic foraminifera in wells sections of the Asmari Formation from the Rag-e-Safid oil field, Zagros Basin, southwest Iran, Stratigraphy and Sedimentology Research 40: 63–84.
4. Bassi D, Nebelsick JH (2010) Components, facies and ramps: redefining Upper Oligocene shallow water carbonates using coralline red algae and larger foraminifera (Venetian area, northeast Italy), Palaeogeography Palaeoclimatology Palaeoecology 295:258–280.
5. Berberian M, King GCP (1981) Towards a paleogeography and tectonic evolution of Iran, Canadian Journal of Earth Sciences 18: 210–265.
6. Daneshian J, Ghanbari M (2017) Stratigraphic distribution of planktonic foraminifera from the Qom Formation: A case study from the Zanjan area (NW Central Iran), Neues Jahrbuch für Geologie und Paläontologie 283: 239–254.
7. Daneshian J, Aftabi A (2010) Foraminiferal biostratigraphy of the Qom Formation on the basis of new investigations at Navab anticline, in southeast Kashan,  Journal of Science University of Tehran 35: 137–154.
8. Daneshian J, Ramezani Dana L (2007) EarlyMiocene benthic foraminifera and biostratigraphy of the Qom Formation, Deh Namak, Central Iran, Journal of Asian Earth Sciences 29:844–858.
9. Distel D L M A, Altamia Z, Lin J R, Shipway A. Han, I. Forteza, R. Antemano, M. Limbaco, A. G. Tebo, R. Dechavez et al. (2017) Discovery of chemoautotrophic symbiosis in the giant shipworm Kuphus polythalamia (Bivalvia: Teredinidae) extends wooden-steps theory, Proceedings of the National Academy of Sciences 114: 3652–3658.
10. Douglas JA (1927) Contibutions to Oersian Paleontology: I, Faun of Fars Series: i,Kuphus arenarius: IIII, Fauna of Mio-Pliocene Series, Anglo-Persian Oil  Co؛ Holywell, Press, Oxford, 15p. 
11. GhasemShirazi B, Bakhshandeh L, Yazdi A (2014) Paleoecology of Upper Cretaceous Sediments in Central Iran, Kerman (Bondar- e Bido Section) Based on Ostracods. Marine Science 4 (2): 49-57
12. Gholamian F, Najafi M, Kim Welford J, Ghods A, BakhtiariM R (2021) Structural style of the Kashan-Ardestan syn-tectonic sedimentary basin in Central Iran, Arabian-Eurasian collision zone, the 21rd EGU General Assembly, Austria Center Vienna ,Vienna, Austria 1;57:140-1.
13. Guettard JE (1770) Memories sur differentes parties des Sciences et des Arts, 3. Paris 139-143.
14. Heydari E, Hassanzadeh J, Wade, WJ, Ghazi AM (2003) Permian– Triassic boundary interval in the Abadeh section of Iran with implications for mass extinction, Paleogeography, Paleoclimatology, Paleoecology 193(3): 405–423.
15. Holdaway H K,  Clayton C J (1982) Preservation of shell microstructure in silicifiedbrachiopods from the Upper Cretaceous WilmingtonSands of Devon, Geological Magazine 119 (4): 371-382.
16. Huber, M (2015) Compendium of Bivalves, Vol. 2, A Full-Color Guide to the Remaining Seven Families: A Systematic Listing of 8,500 Bivalve Species and 10,500 Synonyms. ConchBooks, Hackenheim, Germany.
17. Jalali M,  Sadeghi  A, Adabi MH (2017) Microfacies, sedimentary environment and sequence stratigraphy of the Qom Formation in Yort e Shah no-1 well and Morreh Kuh surface section (South of Tehran), Journal of Stratigraphy and Sedimentology Researches 33( 66): 25-48.
18. James GA, Wynd JG (1965) Stratigraphic nomenclature of Iranian oil consortium, agreement area, American Association of Petroleum Geologists Bulletin 49: 2182–2245.
19. Kamali A, Nadimi A, Farzipour A (2012) Navab anticline: a contractional structure in the transpressive bend of Qom-Zefreh fault zone, west of central Iran. The 6th International Siberian early Career Geoscientists Conference, Novosibirisk, Russia.
20. Kazanci N, Varol B (1993) "The occurrence and significance of beekite in Palaeocene alluvial-fan deposits in central Anatolia, Turkey", Terra Research 5: 36–39.
21. Khalatbari Jafari N, Alavi Mahabadi S (2021) Geological map of Natanz, scale 1:100000, Geologial Survey of Iran 321-86.
22. Lamarck JBPA (1809) Philosophie Zoologique, ou exposition des considerations relatives a` l’histoire naturelle des Animaux; ala diversite´de leur organisation et des faculte´s qu’ils en obtiennent; aux causes physiques qui maintiennent en eux la vie et donnent lieu aux mouvemens qu’ils exe´cutant; enfin a`celles qui produisent les unes le sentiment, et les autres l’intelligence de ceux qui en sont doue´s. 1: 1–428 2: 1–475. Paris.
23. Linnaeus C (1767) Systema Naturae per regna tria naturae, Secundum classes, ordines, genera, species, cum characteribus differentiis, Synonyms,Locis, Editio decima tertia, Aucta reformata, Cura J.F. Gmelin. I(5-6): 2225-3010. G.E.Beer, Lipsiae.
24. Linnaeus C (1758) Systema naturae per regna tria naturae, secundum classes, ordines, genera, species, cum characteribus, differentiis, synonymis, locis. Ed. Decima, reformata. Holmiae, 824 pp.
25. Meyer R,  Pena Dos Reis R B (1985) Paleosols and alunite silcretes in continental Cenozoic of Western Portugal, Journal Of Sedimentary Petrology 55( 1): 76-85.
26. Mohammadi E, Vaziri M R, Dastanpour M (2013)Biostratigraphy of the nummulitids and lepidocyclinids bearing Qom Formation based on larger benthic foraminifera (Sanandaj–Sirjan fore-arc basin and Central Iran back-arc basin, Iran), Arabian Journal of Geosciences 8(1):403-423.
27. Neumayr M (1884) Zur Morphologie der Bivalvenschlosses. Sitzungsberichte der Kaiserlichen Akademie der Wissenschaften Mathematisch- Naturwissenschaftliche Classe 88 (2): 385– 419.
28. Perrin C, Bosence D W J, Rosen B (1995) Quantitative approaches to palaeozonation and palaeobathymetry of corals and coralline algae in Cenozoic reefs, in Bosence D W J, Allison P. A. (eds), Marine Palaeoenvironmental Analysis from Fossils. The Geological Society of London, Special Publication 83: 181-229.
29. Pożaryska K, Pugaczewska H(1981) "Bivalve nature of Huene's dinosaur Succinodon. Acta Palaeontologica Polonica 26 (1): 27–34.
30. Rafinesque CS (1815). Analyse de la Nature, ou tableau de l'univers et des corps organisés. Italy: Aux dépens de l'auteur, 224.
31. Shipway JR, Altamia MA, Haga T, Velásquez M, Albano J, Dechavez R, Concepcion GP, Haygood MG, Distel DL (2018) Observations on the life history and geographic range of the giant chemosymbiotic shipworm Kuphus polythalamius (Bivalvia: Teredinidae ), Biology Bulletin 235: 167–177.
32. Shipway JR, Rosenberg  G, Concepcion, GP, Haygood M G, Savrda C, Distel L (2019) Shipworm bioerosion of lithic substrates in a freshwater setting, Abatan River, Philippines:Ichnologic, paleoenvironmental and biogeomorphical implications, Plos One 14: 10- 16.
33. Stoliczka F (1870) Cretaceous fauna of southern India. 3. The Pelecypoda, with a review of all known genera of this class, fossil and Recent. Geological Survey of India, Palaeontologica Indica, Series 6: 1– 537.
34. Tryon GW (1862) Monograph of the Family Teredidæ. Proceedings of the Academy of Natural Sciences of Philadelphia, 14: 453–482.
35. Turner RD (1969) Pholadacea. Treatise on Invertebrate Paleontology, Geological Society of America, University of Kansas.
36. Zammit Maempel G (1979) The Indo-Pacific affinity of someMaltese Tertiary fossils, The Central Mediterranean Naturalist 1(1): 1-12.
37. Zammit- Maempel G (1993) Kuphus melitensis, a new teredinid bivalve from the Late Oligocene Lower Coralline Limestone of Malta, Contributions to Tertiary and Quaternary Geology 30: 155-175.
38. Zhu Y, Qi Y, Zhang B, Yang H, He, C, Wang S, Zhou W, Zhu Q, Li Z (2007) Revision of the age of the Qom Formation in the Central Iran Basin, Iran, Journal of Asian Earth Sciences 29 : 715–721.