Digital repository of Slovenian research organisations

Show document
A+ | A- | Help | SLO | ENG

Title:Taxonomic and stratigraphic remarks on Placites urlichsi Bizzarini, Pompeckjiteslayeri (Hauer), Carnites floridus (Wulfen) and Sageceras haidingeri (Hauer)
Authors:ID Spatzenegger, Andreas (Author)
ID Poltnig, Walter (Author)
Files:.pdf PDF - Presentation file, download (6,67 MB)
MD5: AB794BF4CD34F889857AC92810B38C95
 
Language:English
Typology:1.01 - Original Scientific Article
Organization:Logo GeoZS - Geological Survey of Slovenia
Abstract:Investigations of an Lower Carnian Wettersteinkalk ammonoid fauna found in the Hochobir massif (Carinthia/Austria) gave rise to problems in the taxonomic relationship within the Triassic ammonoid Family Pinacoceratidae. The morphological parameters of the ammonoid genus Pompeckjites are rather unclear. Morphological variation of at least two ammonoid species as Pompeckjites layeri Hauer on one end, Placites urlichsi Bizzarini on the other end have to be take into account. Numerous field surveys, studies and excavations on upper Wettersteinkalk sites within the Karavank Mountains and Hallstatt-facies sites in the Northern Calcareous Alps were implemented and compared with the reference sites in the Dolomites. As a consequence of our investigations, the Hochobir Wettersteinkalk ammonite assemblage is thought to be equivalent in time to the ammonoid fauna of the Upper San Cassian Formation. The frequent occurrence of the Julian (Lower Carnian) ammonoid Placites urlichsi Bizzarini may be a powerful tool in field investigations for a refined correlation of the upper Wettersteinkalk reef limestone to the coeval basinal facies of the Upper San Cassian Formation (Lower Carnian/upper Trachyceras aonoides Zone). As a result of this study Placites urlichsi was included in the genus Pompeckjites. This paper could be an attempt to recognize the differences in juvenile forms of Pompeckjites layeri and Placites urlichsi and other similar disciform ammonoid genera like Carnites floridus and Sageceras sp. Based on suture lines, polished transversal-sections and morphological features.
Keywords:ammonoids, Triassic, Carnian, Wettersteinkalk, Bleiberger Sonderfazies, Upper San Cassian Formation
Publication status:Published
Publication version:Version of Record
Publication date:04.08.2023
Publisher:Geološki zavod Slovenije
Year of publishing:2023
Number of pages:str. 87-105
Numbering:vol. 66, no. 1
PID:20.500.12556/DiRROS-17794 New window
UDC:56
ISSN on article:0016-7789
DOI:10.5474/geologija.2023.003 New window
COBISS.SI-ID:164584707 New window
Publication date in DiRROS:15.01.2024
Views:579
Downloads:148
Metadata:XML DC-XML DC-RDF
:
Copy citation
  
Share:Bookmark and Share


Hover the mouse pointer over a document title to show the abstract or click on the title to get all document metadata.

Record is a part of a journal

Title:Geologija
Shortened title:Geologija
Publisher:Geološki zavod Slovenije
ISSN:0016-7789
COBISS.SI-ID:5636866 New window

Licences

License:CC BY 4.0, Creative Commons Attribution 4.0 International
Link:http://creativecommons.org/licenses/by/4.0/
Description:This is the standard Creative Commons license that gives others maximum freedom to do what they want with the work as long as they credit the author.
Licensing start date:04.08.2023

Secondary language

Language:Slovenian
Title:Taksonomija in stratigrafski razpon vrst Placites urlichsi Bizzarini, Pompeckjites layeri (Hauer), Carnites floridus (Wulfen) in Sageceras haidingeri (Hauer)
Abstract:Rezultati raziskave amonitne favne v spodnjekarnijskem wettersteinskem apnencu, ki se pojavlja na Obirju, na avstrijskem Koroškem, odpirajo problem v taksonomskem razlikovanju triasnih amonitov družine Pinacoceratidae. Razlikovanje na podlagi morfoloških parametrov amonitov rodu Pompeckjites je precej nejasno, pri čemer je treba upoštevati morfološke variacije najmanj dveh vrst, in sicer Pompeckjites layeri Hauer na eni ter Placites urlichsi Bizzarini na drugi strani. Številni ogledi nahajališč v zgornjem wettersteinskem apnencu Karavank in hallstattskem faciesu Severno apneniških Alp, njihova izkopavanja ter raziskave, poleg tega pa tudi primerjava z referenčnimi najdišči v Dolomitih kažejo, da je zbrana amonitna združba wettersteinskega apnenca najverjetneje časovni ekvivalent amonitni favni zgornje San Cassian formacije. Pogosto pojavljanje julijskega (spodnji karnij) amonita Placites urlichsi Bizzarini je na terenu lahko močno orodje za oceno korelacije med grebenskim zgornjim wettersteiskim apnencem ter ekvivalentnim bazalnim faciesom zgornje San Cassian formacije (spodnji karnij/zgornji del Trachyceras aonoides c one). Kot rezultat te raziskave je bil Placites urlichsi vključen v rod Pompeckjites. Pričujoči članek na podlagi suturnih linij, poliranih rezov in morfoloških značilnosti, pomaga prepoznati razliko med juvenilnimi oblikami Pompeckjites layeriin Placites urlichsi ter drugimi amoniti diskoidne oblike kot sta Carnites floridus in Sageceras sp.
Keywords:amoniti, trias, karnij wettersteinski apnenec, pliberški facies, Zgornja San Cassianska formacija


Collection

This document is a part of these collections:
  1. Geologija

Back