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      <comment>Eötvös Loránd University, Department of Paleontology, Budapest, Hungary            
            Geological and Geophysical Institute, Department of Geological and Geophysical Collections, Budapest, Hungary            
            not available, H-1117 Budapest Pázmány P., sétány 1/C, Hungary            
            not available, H-1143 Budapest, Stefánia út. 14, Hungary            
            Export Date: 16 April 2025; Cited By: 32</comment>
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      <title>Palynomorphs of the Normapolles group and related plant mesofossils from the Iharkút vertebrate site, Bakony Mountains (Hungary)</title>
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      <abstractText>Palynological and paleobotanical investigation of bonebeds and other strata of the Csehbánya
Formation from the vertebrate locality at Iharkút (Bakony Mts, Hungary) reveals well-preserved
Santonian palynological assemblages dominated by the Normapolles group, with a minor component
consisting of other angiosperm pollen, some gymnosperm pollen, and spores. Eleven species of
Normapolles-type pollen grains belonging to seven genera and fruit remains of a new taxon,
Sphaeracostata barbackae gen. et sp. nov., are described. The new species is very abundant in the material,
represented by ca. 1000 specimens. The genus Caryanthus Friis and an unnamed form previously
reported from Hat¸eg by Lindfors et al. (2010) are also present.
Plants producing Normapolles-type pollen grains diversified during the Late Cretaceous, with a
bloom in the Santonian. The palynostratigraphy of the Upper Cretaceous terrestrial sediments in the
studied region is based on Normapolles-related species. The studied assemblage is assigned to the
Oculopollis zaklinskaiae-Tetracolporopollenites (Brecolpites) globosus Zone (or Zone C) indicating a late
Santonian age. Comparison of the Iharkút palynoflora with other known Upper Cretaceous
palynofloras of Central Europe shows diachronous occurrence of Normapolles taxa at different
geographic localities and warrants further investigation.
The ecological requirements of the amphibian fauna reflect azonal conditions controlled by the
availability of water, which is in agreement with the inferred ecological conditions based on the
paleobotanical investigations. The fauna is of entirely non-marine character, further supported by
isotope studies, in line with our data showing that the palynological samples contain no marine forms.</abstractText>
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	&lt;pre class=&quot;comment&quot; style=&quot;margin-top: 0; margin-bottom: 0;&quot;&gt;&lt;u&gt;Megjegyzés&lt;/u&gt;: Eötvös Loránd University, Department of Paleontology, Budapest, Hungary            
            Geological and Geophysical Institute, Department of Geological and Geophysical Collections, Budapest, Hungary            
            not available, H-1117 Budapest Pázmány P., sétány 1/C, Hungary            
            not available, H-1143 Budapest, Stefánia út. 14, Hungary            
           ...&lt;/pre&gt;
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