Rare Middle Triassic coleoids from Alpine-Carpathian system: A new records from Slovakia and their significance

Author:

Kostak Martin1ORCID,Schlögl Ján2,Fuchs Dirk3,Havrila Milan4,Kolar-Jurkovšek Tea5,Vörös Attila6,Havelcová Martina7,Šurka Juraj8,Havrila Jakub9,Holcová Katarína1

Affiliation:

1. Charles University Faculty of Science: Univerzita Karlova Prirodovedecka fakulta

2. Comenius University in Bratislava Faculty of Natural Sciences: Univerzita Komenskeho v Bratislave Prirodovedecka fakulta

3. Bayerische Staatssammlung für Paläontologie und Geologie: Bayerische Staatssammlung fur Palaontologie und Geologie

4. State Geological Institute of Dionyz Stur: Statny geologicky ustav Dionyza Stura

5. Geological Survey of Slovenia

6. Hungarian Natural History Museum: Magyar Termeszettudomanyi Muzeum

7. Institute of Rock Structure and Mechanics Czech Academy of Sciences: Ustav struktury a mechaniky hornin Akademie ved Ceske republiky

8. Earth Science Institute of the SAS: Ustav vied o Zemi Slovenskej akademie vied

9. none

Abstract

Abstract The two stratigraphically well constrained (by ammonites and conodonts) coleoid remains have been recorded in the Triassic (Anisian) dark-grey organodetritic limestones (Ráztoky Limestone) of Western Carpathians (Hronic Nappe). The facies originated between carbonate ramp and basinal development. It yields highly diversificated cephalopod fauna including nautiloids (2 taxa), ammonoids (7 taxa) and indetermined aulacoceratids. Two unusual coleoid specimens are referred to genus Mojsisovicsteuthis (M. boeckhi) and probably to a new taxon (described as Breviconoteuthis aff. breviconus herein) possessing similar morphological features of genus Breviconoteuthis (Phragmoteuthida) and/or Zugmontites. Based on index ammonites and conodonts, both records are of the uppermost Trinodosus through the lowermost Reitzi zones (Anisian – lower Illyrian). While the genus Mojsisovicsteuthis has been widely dispersed (however its records are rare), the occurrence of Breviconoteuthis and Zugmontites is strictly limited to the Alpine-Carpathian region. Compare to the holotype and additional specimens stored in the Hungarian Natural History Museum, the overal shell of Mojsisovicsteuthis and its size has been reconstructed. Its relationship to aulacoceratids and phragmoteuthids is briefly discussed. Geochemical record provided a relevant signal of the existence of algal meadows which may represent an analogy with later sea-grasses.

Publisher

Research Square Platform LLC

Reference71 articles.

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3. New genera of Anisian ammonoids from the Prezzo Limestone Southern Alps;Balini M;Atti Ticinensi di Scienze della Terra,1992

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5. The Global boundary Stratotype Section and Point (GSSP) of the Ladinian Stage (Middle Triassic) at Bagolino (Southern Alps, Northern Italy) and its implications for the Triassic time scale;Brack P;Episodes,2005

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