Austrian Journal of Earth Sciences Vienna 2019 Volume 112/2 103 - 124 DOI: 10.17738/ajes.2019.0007 Palynology, microfacies and ostracods of the Permian–Triassic boundary interval in the Rosengarten/Catinaccio Massif (Southern Alps, Italy) Hendrik NOWAK1)*, Wolfgang METTE2), Fabio M. PETTI3), Guido ROGHI4), Evelyn KUSTATSCHER1),5),6) 1) Museum of Nature South Tyrol, Bindergasse/Via Bottai 1, 39100 Bozen/Bolzano, Italy; e-mail:
[email protected]; evelyn.kustatscher@ naturmuseum.it 2) Department of Geology, Universität Innsbruck, Innrain 52f, 6020 Innsbruck, Austria; e-mail:
[email protected] 3) MUSE – Museo delle Scienze di Trento, Corso del Lavoro e della Scienza 3, Trento 38122, Italy; e-mail:
[email protected] 4) Istituto di Geoscienze e Georisorse - CNR, Via Gradenigo 6, Padova 35131, Italy; e-mail:
[email protected] 5) Department of Earth and Environmental Sciences, Paleontology & Geobiology, Ludwig-Maximilians-Universität München, Richard-Wagner-Straße 10, 80333 München, Germany 6) SNSB-Bayerische Staatssammlung für Paläontologie und Geologie, Richard-Wagner-Straße 10, 80333 München, Germany *) Corresponding author: Hendrik NOWAK KEYWORDS upper Permian, Lopingian, Lower Triassic, Dolomites, Bellerophon Formation, Werfen Formation. Abstract The Laurinswand section in the Rosengarten/Catinaccio Massif (Dolomites, Southern Alps, Italy) covers the Permian– Triassic boundary in a proximal marine setting. The section has been studied for palynology, ostracods and carbonate microfacies. Five microfacies types are defined for the carbonates of the Bellerophon Formation (Changhsingian) in this section. Ostracod assemblages from the upper Bellerophon Formation show a moderate to high diversity and mostly indi- cate normal marine conditions, with some samples from the upper Casera Razzo Member being dominated by eurytopic forms.