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<datestamp>2018-01-11</datestamp>
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<title lang=en>Marine carbonate systems in the Sarmatian (Middle Miocene) of the Central Paratethys: the Zsambek Basin of Hungary</title>
<creator>Cornee, Jean-Jacques</creator>
<creator>Moissette, Pierre</creator>
<creator>Saint Martin, Jean-Paul</creator>
<creator>Kazmers, Miklos</creator>
<creator>Toth, Emoke</creator>
<creator>Gorog, Agnes</creator>
<creator>Dulai, Alfred</creator>
<creator>Muller, Pal</creator>
<contributor>Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Paléoenvironnement et paléobiosphère (PP) ; Université Claude Bernard Lyon 1 (UCBL) - Institut national des sciences de l'Univers (INSU - CNRS) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Paléobiodiversité et paléoenvironnements ; Université Pierre et Marie Curie - Paris 6 (UPMC) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<description>International audience</description>
<source>ISSN: 1469-3496</source>
<source>EISSN: 1365-3091</source>
<source>Sedimentology</source>
<publisher>Blackwell Publishing</publisher>
<identifier>hal-00429337</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00429337</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00429337</source>
<source>Sedimentology, Blackwell Publishing, 2009, 56 (6), pp.1728-1750. 〈10.1111/j.1365-3091.2009.01055.x〉</source>
<identifier>DOI : 10.1111/j.1365-3091.2009.01055.x</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1111/j.1365-3091.2009.01055.x</relation>
<language>en</language>
<subject lang=en>Buildups</subject>
<subject lang=en>carbonates</subject>
<subject lang=en>Hungary</subject>
<subject lang=en>Miocene</subject>
<subject lang=en>oolites</subject>
<subject lang=en>Paratethys</subject>
<subject>[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces, environment</subject>
<subject>[SDE.MCG] Environmental Sciences/Global Changes</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>The study of eight stratigraphic sections at the margin of the semi-enclosed Zsambek Basin (Hungary) allows the sedimentary anatomy of oolitic-bioclastic systems in the Sarmatian of the Central Paratethys to be reconstructed. The mollusc, foraminiferal and ostracod associations indicate that the carbonate systems are Latest Badenian to Late Sarmatian in age. The Lower-Upper Sarmatian deposits are organized in superimposed subaqueous dunes prograding towards the basin on a low-angle ramp. During the Late Sarmatian, the ramp underwent subaerial erosion linked to a moderate relative fall in sea-level. Lagoonal deposits were later formed and microbial-nubeculariid-bryozoan-serpulid buildups were emplaced. The 'abnormal' marine conditions of the Sarmatian, conducive to the development of a poorly diversified flora and fauna and dominant non-skeletal grains, are linked to fluctuating salinities, mesotrophic to eutrophic conditions and perhaps high alkalinity.</description>
<date>2009</date>
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