<?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-O0Y5O7MU/1f9aa799-218b-4f9a-b91e-a8c5184e31fb/HTML"><dcterms:extent>65 KB</dcterms:extent></edm:WebResource><edm:WebResource rdf:about="http://www.dlib.si/stream/URN:NBN:SI:doc-O0Y5O7MU/429be20d-2ced-442c-aa24-da9613b2f889/PDF"><dcterms:extent>6020 KB</dcterms:extent></edm:WebResource><edm:WebResource rdf:about="http://www.dlib.si/stream/URN:NBN:SI:doc-O0Y5O7MU/6e8a75a7-d9ef-40aa-b2ff-3fc67aac2386/TEXT"><dcterms:extent>46 KB</dcterms:extent></edm:WebResource><edm:TimeSpan rdf:about="1998-2025"><edm:begin xml:lang="en">1998</edm:begin><edm:end xml:lang="en">2025</edm:end></edm:TimeSpan><edm:ProvidedCHO rdf:about="URN:NBN:SI:doc-O0Y5O7MU"><dcterms:isPartOf rdf:resource="https://www.dlib.si/details/URN:NBN:SI:spr-MXAZXSSM" /><dcterms:issued>2008</dcterms:issued><dc:creator>Gulyás, Sándor</dc:creator><dc:creator>Jakab, Gusztáv</dc:creator><dc:creator>Sümegi, Pál</dc:creator><dc:format xml:lang="sl">številka:35</dc:format><dc:format xml:lang="sl">letnik:35</dc:format><dc:format xml:lang="sl">str. 33-43</dc:format><dc:identifier>ISSN:1408-967X</dc:identifier><dc:identifier>COBISSID:38141794</dc:identifier><dc:identifier>URN:URN:NBN:SI:doc-O0Y5O7MU</dc:identifier><dc:language>en</dc:language><dc:publisher xml:lang="sl">Oddelek za arheologijo Filozofske fakultete Univerze v Ljubljani</dc:publisher><dcterms:isPartOf xml:lang="sl">Documenta Praehistorica</dcterms:isPartOf><dc:subject xml:lang="sl">Blatno jezero</dc:subject><dc:subject xml:lang="sl">fosili</dc:subject><dc:subject xml:lang="sl">holocen</dc:subject><dc:subject xml:lang="en">Hungary</dc:subject><dc:subject xml:lang="sl">Madžarska</dc:subject><dc:subject xml:lang="sl">paleoekologija</dc:subject><dc:subject xml:lang="sl">paleontologija</dc:subject><dc:subject xml:lang="en">paleontology</dc:subject><dc:subject xml:lang="sl">pleistocen</dc:subject><dc:subject xml:lang="sl">sedimenti</dc:subject><dc:subject rdf:resource="http://www.wikidata.org/entity/Q82480" /><dcterms:temporal rdf:resource="1998-2025" /><dc:title xml:lang="sl">Holocene paleoclimatic and paleohydrological changes in Lake Balaton as inferred from a complex quantitative environmental historical study of a lacustrine sequence of the Szigliget embayment|</dc:title><dc:description xml:lang="sl">The present paper discusses the findings of a complex quantitative paleoecological investigation implemented for capturing the Upper Weichselian, Late Glacial and Postglacial development of Lake Balaton in western Hungary, in the heart of Transdanubia. The studied Late Pleistocene and Holocene lacustrine marl and peat sequence preserved the complete evolutionary history of the catchment basin of the Szigliget Embayment from the time of its birth. The inferred palaeohydrological changes, along with that of the hydroseries, were compared to those observable coevally in the terrestrial vegetation. According to the available data, the birth of the studied embayment can be put to the Late Glacial/Upper Weichselian transition.A wide array of hydrophyte vegetation and habitat types emerged in the embayment depending on the actual water supply and geomorphologic position. Based on a collective quantitative evaluation of the observed sedimentary features and fossil assemblages retrieved from the sequence, a record of paleohydrological transformations in the littoral part of the lake was drawn</dc:description><dc:description xml:lang="sl">Članek predstavlja rezultate kompleksne kvantitativne pelookoljske raziskave, katere cilj je ugotavljanje pleniglacialnega, poznoglacialnega in postglacialnega razvoja Blatnega jezera v zahodni Madžarski. V zaporedju poznopleistocenskih in holocenskih jezerskih sedimentov in šote je ohranjena celotna zgodovina porečja zaliva Szigliget od njegovega nastanka naprej. Ugotovljene paleohidrološke spremembe skupaj s premenami jezera smo primerjalis spremembami v kopenski vegetaciji. Na podlagi raziskav lahko nastanek zaliva umestimo v prehod med pleniglacialom in začetkom kasnega glaciala. Količina vode in geomorfološki položaj je pogojeval nastanku velikega spektra vodne vegetacije in habitatnih tipov. Skupna kvantitativna analiza sedimentacijskih značilnosti in fosilnih zbirov nam omogoča, da lahko opišemo zaporedje paleohidroloških premen v obalnem delu zaliva</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-O0Y5O7MU"><edm:aggregatedCHO rdf:resource="URN:NBN:SI:doc-O0Y5O7MU" /><edm:isShownBy rdf:resource="http://www.dlib.si/stream/URN:NBN:SI:doc-O0Y5O7MU/429be20d-2ced-442c-aa24-da9613b2f889/PDF" /><edm:rights rdf:resource="http://rightsstatements.org/vocab/InC/1.0/" /><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">Univerza v Ljubljani, Filozofska fakulteta</edm:dataProvider><edm:object rdf:resource="http://www.dlib.si/streamdb/URN:NBN:SI:doc-O0Y5O7MU/maxi/edm" /><edm:isShownAt rdf:resource="http://www.dlib.si/details/URN:NBN:SI:doc-O0Y5O7MU" /></ore:Aggregation></rdf:RDF>