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<metadata xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:dc="http://purl.org/dc/elements/1.1/"><dc:title>Upper Triassic foraminifera from the Northern Calcareous Alps, Austria</dc:title><dc:creator>Gale,	Luka	(Avtor)
	</dc:creator><dc:creator>Mette,	Wolfgang	(Avtor)
	</dc:creator><dc:subject>Upper Triassic</dc:subject><dc:subject>Pötschenkalk</dc:subject><dc:subject>Zlambach Formation</dc:subject><dc:subject>Kössen Formation</dc:subject><dc:subject>Kendlbach Formation</dc:subject><dc:subject>morphogroup</dc:subject><dc:description>Foraminiferal assemblages and   proportions of  foraminiferal morphogroups were    determined from   Upper Triassic deposits of  the   Eiberg Basin and   the   Hallstatt Zone    of  the   Northern Calcareous Alps    in  Austria (Eastern Alps). Foraminifera were hand-picked from the residue of marl samples taken from the upper Norian Pötschenkalk Formation, the middle–upper Rhaetian Zlambach Formation, and the uppermost Rhaetian Tiefengraben Member of the Kendlbach Formation. In  total,    72  species from   31  genera were    determined. Foraminiferal assemblages from   the   Pötschenkalk Formation at the   Thälerergraben section are   relatively diverse.Dentalina, Ammodiscus, Nodosaria,  and  Glomospirella  dominate.  Foraminiferal assemblages from the Zlambach Formation at the Rossmoos-/Stambachgraben section are also abundant and diverse. The most common foraminifera are Reophax, Dentalina, and Annulina. The uppermost Kössen Formation at the Schlossgraben section is dominated by hyaline taxa. The most common genera are Ichthyolaria, Lenticulina,  and  Nodosaria. At the Fonsjoch section, the uppermost Kössen Formation contains Lenticulina, Astacolus, and Trochammina. An increase in opportunists suggests variations in oxygen levels during the deposition of the uppermost Kössen Formation. The   Kendlbach Formation at  the   Schlossgraben section is  dominated by  Lagenida over   agglutinated taxa.    Astacolus, Lenticulina, and Trochammina are the most common genera. At the Fonsjoch section, the Kendlbach Formation contains mostly Ast acolus, followed by Trochammina, Ammobaculites, Reophax, and Lenticulina. Increases in opportunists point to increased stressful conditions. An increase in nodosariid foraminifera higher up the section indicates a return to better oxygenated conditions.</dc:description><dc:date>2026</dc:date><dc:date>2026-07-06 11:02:54</dc:date><dc:type>Neznano</dc:type><dc:identifier>30808</dc:identifier><dc:identifier>UDK: 56</dc:identifier><dc:identifier>ISSN pri članku: 0016-7789</dc:identifier><dc:identifier>DOI: 10.5474/geologija.2026.005</dc:identifier><dc:identifier>COBISS_ID: 283533315</dc:identifier><dc:language>sl</dc:language></metadata>
