<?xml version="1.0"?><rdf:RDF xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:edm="http://www.europeana.eu/schemas/edm/" xmlns:wgs84_pos="http://www.w3.org/2003/01/geo/wgs84_pos" xmlns:foaf="http://xmlns.com/foaf/0.1/" xmlns:rdaGr2="http://rdvocab.info/ElementsGr2" xmlns:oai="http://www.openarchives.org/OAI/2.0/" xmlns:owl="http://www.w3.org/2002/07/owl#" xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#" xmlns:ore="http://www.openarchives.org/ore/terms/" xmlns:skos="http://www.w3.org/2004/02/skos/core#" xmlns:dcterms="http://purl.org/dc/terms/"><edm:WebResource rdf:about="http://www.dlib.si/stream/URN:NBN:SI:doc-YIXQG0F0/ffd897d6-36fa-4939-bc14-12b3e9f6c66f/PDF"><dcterms:extent>5519 KB</dcterms:extent></edm:WebResource><edm:WebResource rdf:about="http://www.dlib.si/stream/URN:NBN:SI:doc-YIXQG0F0/1cad8ae6-9f0a-45b9-b6a1-6c55a85cc34c/TEXT"><dcterms:extent>0 KB</dcterms:extent></edm:WebResource><edm:TimeSpan rdf:about="1953-2025"><edm:begin xml:lang="en">1953</edm:begin><edm:end xml:lang="en">2025</edm:end></edm:TimeSpan><edm:ProvidedCHO rdf:about="URN:NBN:SI:doc-YIXQG0F0"><dcterms:isPartOf rdf:resource="https://www.dlib.si/details/URN:NBN:SI:spr-Y5SOGFOQ" /><dcterms:issued>2020</dcterms:issued><dc:creator>Bricman, Andrej</dc:creator><dc:creator>Križnar, Matija</dc:creator><dc:creator>Ocepek, Ivan</dc:creator><dc:format xml:lang="sl">številka:2</dc:format><dc:format xml:lang="sl">letnik:63</dc:format><dc:format xml:lang="sl">str. 311-321</dc:format><dc:identifier>ISSN:0016-7789</dc:identifier><dc:identifier>COBISSID_HOST:41484035</dc:identifier><dc:identifier>URN:URN:NBN:SI:doc-YIXQG0F0</dc:identifier><dc:language>sl</dc:language><dc:publisher xml:lang="sl">Geološki zavod Slovenije</dc:publisher><dcterms:isPartOf xml:lang="sl">Geologija</dcterms:isPartOf><dc:subject xml:lang="en">ammonites</dc:subject><dc:subject xml:lang="sl">amoniti</dc:subject><dc:subject xml:lang="">Ancyloceratina</dc:subject><dc:subject xml:lang="en">Cretaceous, lower</dc:subject><dc:subject xml:lang="">Crioceratites</dc:subject><dc:subject xml:lang="sl">fosili</dc:subject><dc:subject xml:lang="en">fossils</dc:subject><dc:subject xml:lang="sl">Glavonožci</dc:subject><dc:subject xml:lang="">Himantoceras</dc:subject><dc:subject xml:lang="sl">Karavanke, severne</dc:subject><dc:subject xml:lang="sl">kreda, spodnja</dc:subject><dc:subject xml:lang="sl">Leše</dc:subject><dc:subject xml:lang="en">North Karavanke Mts.</dc:subject><dc:subject xml:lang="sl">Paleontologija</dc:subject><dc:subject xml:lang="sl">Prevalje</dc:subject><dc:subject xml:lang="en">Slovenia</dc:subject><dc:subject xml:lang="sl">Slovenija</dc:subject><dcterms:temporal rdf:resource="1953-2025" /><dc:title xml:lang="sl">Spodnjekredni heteromorfni amoniti (Ancyloceratina) z Leš pri Prevaljah (Severne Karavanke, SV Slovenija)| Lower Cretaceous heteromorph ammonites (Ancyloceratina) from Leše near Prevalje (North Karavanke Mts. NE Slovenia)|</dc:title><dc:description xml:lang="sl">The paper deals with newly discovered Valanginian-Hauterivian fauna of heteromorphic ammonites (Ancyloceratina) from locality south of the village of Leše above the Meža River valley (North Karavanke Mountains). Fossils were recovered fro m the pelagic limestone. Among the studied heteromorphic ammonites are Lower Cretacaoeus species Himantoceras trinodosum (Upper Valanginian) and Crioceratites cf. nolani(Hauterivian). Based on the accompanied ammonites (Ammonitina) from the outcrop, we biostratigraficaly confirm the presence of Lower Cretaceous ammonites fauna in the Northern Karavanke Mountains. This is also the first report on heteromorphic ammonites in Slovenia</dc:description><dc:description xml:lang="sl">Predstavljamo in opisujemo valanginijsko-hauterivijsko združbo heteromorfnih amonitov (Ancyloceratina) iz najdišča južno od Leš nad dolino reke Meže (Severne Karavanke). Amoniti so bili najdeni v apnencu tipa pelagični mudstone. Preiskave heteromorfnih amonitov so pokazale prisotnost značilnih spodnjekrednih vrst Himantoceras trinodosum (zgornji valanginij) in Crioceratites cf. nolani (hauterivij). S prisotnost jo še drugi z amonitov z Leškega najdišča smo biostratigrafsko potrdili spodnje kredno starost zbrane favne v Severnih Karavankah. Enako pa tudi prvič potrdili prisotnost heteromorfnih amonitov v Sloveniji</dc:description><edm:type>TEXT</edm:type><dc:type xml:lang="sl">znanstveno časopisje</dc:type><dc:type xml:lang="en">journals</dc:type><dc:type rdf:resource="http://www.wikidata.org/entity/Q361785" /></edm:ProvidedCHO><ore:Aggregation rdf:about="http://www.dlib.si/?URN=URN:NBN:SI:doc-YIXQG0F0"><edm:aggregatedCHO rdf:resource="URN:NBN:SI:doc-YIXQG0F0" /><edm:isShownBy rdf:resource="http://www.dlib.si/stream/URN:NBN:SI:doc-YIXQG0F0/ffd897d6-36fa-4939-bc14-12b3e9f6c66f/PDF" /><edm:rights rdf:resource="http://creativecommons.org/licenses/by/4.0/" /><edm:provider>Slovenian National E-content Aggregator</edm:provider><edm:intermediateProvider xml:lang="en">National and University Library of Slovenia</edm:intermediateProvider><edm:dataProvider xml:lang="sl">Geološki zavod Slovenije</edm:dataProvider><edm:object rdf:resource="http://www.dlib.si/streamdb/URN:NBN:SI:doc-YIXQG0F0/maxi/edm" /><edm:isShownAt rdf:resource="http://www.dlib.si/details/URN:NBN:SI:doc-YIXQG0F0" /></ore:Aggregation></rdf:RDF>