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Revision of the trace fossil Megagrapton Książkiewicz, 1968 with focus on Megagrapton aequale Seilacher, 1977 from the lower Eocene of the Lesser Caucasus in Georgia

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Abstrakty
EN
Megagrapton Książkiewicz, 1968 is a characteristic deep-sea trace fossil belonging to the group of graphoglyptids and mostly preserved as a network of irregular meshes in hypichnial semirelief. So far, eleven ichnospecies have been distinguished under this ichnogenus, though commonly on weak evidence. The so-far poorly known ichnospecies Megagrapton aequale Seilacher, 1977 is described here on the basis of the numerous, newly discovered specimens from deep-sea siliciclastic deposits of the Bolevani Subsuite (lower Eocene) in the Lesser Caucasus of Georgia, together with other collections and published examples. A neotype of this ichnospecies is designated and the diagnosis emended. M. aequale occurs in lower Cambrian to upper Miocene deep-sea turbiditic deposits, mostly in the Paleogene. It is characterized by relatively small, variable meshes, which have mostly irregular sub-pentagonal, sub-hexagonal or sub-heptagonal shapes that are variable in size and are bordered by curved or straight semicircular ridges. It has been mistaken for Paleodictyon, which forms regular hexagonal nets. Paleodictyon imperfectum Seilacher, 1977 is included in M. aequale as the ichnosubspecies M. a. imperfectum, which is characterized by relatively thin bordering ridges. After critical analysis of all ichnospecies, only M. irregulare Książkiewicz, 1968, M. submontanum (Azpeitia Moros, 1933), and M. aequale are recommended for further use. These are distinguished on the basis of the prevailing morphology of the meshes, irrespective of large differences in morphometric parameters within the ichnospecies. Irredictyon chaos Vialov, 1972 is included in M. irregulare as the ichnosubspecies M. i. chaos, which is characterized by relatively thick bordering ridges. Megagrapton is interpreted as a cast of a subsurface open burrow network with a few connections to the sea floor. The burrows probably functioned as a trap for small organisms (ethological subcategory irretichnia).
Słowa kluczowe
Rocznik
Strony
art. no. 8
Opis fizyczny
Bibliogr. 97 poz.,map., rys., tab., wykr.
Twórcy
  • Jagiellonian University, Institute of Geological Sciences, Gronostajowa 3a, 30-387 Kraków, Poland
  • Iv. Javakhishvili Tbilisi State University, Faculty of Exact and Natural Sciences, University 13, 0186 Tbilisi, Georgia
  • Iv. Javakhishvili Tbilisi State University, Alexander Janelidze Institute of Geology, Politkovskaia 31, 0186 Tbilisi, Georgia
  • Iv. Javakhishvili Tbilisi State University, Alexander Janelidze Institute of Geology, Politkovskaia 31, 0186 Tbilisi, Georgia
  • Iv. Javakhishvili Tbilisi State University, Alexander Janelidze Institute of Geology, Politkovskaia 31, 0186 Tbilisi, Georgia
  • Iv. Javakhishvili Tbilisi State University, Alexander Janelidze Institute of Geology, Politkovskaia 31, 0186 Tbilisi, Georgia
  • Department of Geology and Paleontology, Georgian National Museum, 3, Purtseladze, 0105 Tbilisi, Georgia
autor
  • Iv. Javakhishvili Tbilisi State University, Faculty of Exact and Natural Sciences, University 13, 0186 Tbilisi, Georgia
  • Department of Geology and Paleontology, Georgian National Museum, 3, Purtseladze, 0105 Tbilisi, Georgia
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Uwagi
Opracowanie rekordu ze środków MEiN, umowa nr SONP/SP/546092/2022 w ramach programu "Społeczna odpowiedzialność nauki" - moduł: Popularyzacja nauki i promocja sportu (2022-2023).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-6b2b856e-28da-418a-aff3-f97e022cbe95
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