Early Sarmatian paleoenvironments in the easternmost Pannonian Basin (Borod Depression, Romania) revealed by the micropaleontological data
The Sarmatian sedimentary record of the Borod Depression (eastern Pannonian Basin) consists of a marine sequence with continental influence. The investigated section, located near Vârciorog, was biostratigraphically and paleoenvironmentally analysed. The micro- and macrofossil assemblages include da...
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| Veröffentlicht in: | Geologica Carpathica 2014-02, Vol.65 (1), p.67-81 |
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| creator | Filipescu, Sorin Miclea, Angela Gross, Martin Harzhauser, Mathias Zágoršek, Kamil Jipa, Cătălin |
| description | The Sarmatian sedimentary record of the Borod Depression (eastern Pannonian Basin) consists of a marine sequence with continental influence. The investigated section, located near Vârciorog, was biostratigraphically and paleoenvironmentally analysed. The micro- and macrofossil assemblages include dasycladaceans, characeans, foraminifera, molluscs, polychaetes, ostracods, crabs, bryozoans, fish and vertebrate remains, which are characteristic for a shallow marine setting with local transitions to continental facies. The microfossil assemblages are characteristic for the Elphidium reginum Zone and Mohrensternia Zone of the early Sarmatian (Serravallian). The succession of populations correlates with the sedimentological trend, allowing the separation of several genetic units. The relative sea-level changes and the progradational trend from the top of the section suggest active tectonics in the hinterland (Apuseni Mountains). The shallow seas surrounding the emerging islands (Apuseni Mountains) provided the connections between the Pannonian and Transylvanian basins during the early Sarmatian |
| doi_str_mv | 10.2478/geoca-2014-0005 |
| format | Article |
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The investigated section, located near Vârciorog, was biostratigraphically and paleoenvironmentally analysed. The micro- and macrofossil assemblages include dasycladaceans, characeans, foraminifera, molluscs, polychaetes, ostracods, crabs, bryozoans, fish and vertebrate remains, which are characteristic for a shallow marine setting with local transitions to continental facies. The microfossil assemblages are characteristic for the Elphidium reginum Zone and Mohrensternia Zone of the early Sarmatian (Serravallian). The succession of populations correlates with the sedimentological trend, allowing the separation of several genetic units. The relative sea-level changes and the progradational trend from the top of the section suggest active tectonics in the hinterland (Apuseni Mountains). 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The shallow seas surrounding the emerging islands (Apuseni Mountains) provided the connections between the Pannonian and Transylvanian basins during the early Sarmatian</description><subject>Borod Depression (NW-Romania)</subject><subject>bryozoans</subject><subject>Decapoda</subject><subject>Elphidium</subject><subject>Foraminifera</subject><subject>Marine</subject><subject>Mollusca</subject><subject>molluscs</subject><subject>Ostracoda</subject><subject>ostracods</subject><subject>paleoenvironments</subject><subject>paleogeography</subject><subject>Sarmatian (late Middle Miocene)</subject><subject>sequence stratigraphy</subject><issn>1335-0552</issn><issn>1336-8052</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2014</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><recordid>eNptkV1LIzEUhgdxQaleexvYGwVHk8nHTMAb66q7UFhZ9TqcSU-7U2aSmqQu_Qv-6k1bL0S8yoE873s-3qI4YfSiEnVzOUdvoawoEyWlVO4Vh4xzVTZUVvvbWpZUyuqgOI5xkQnKmWwEPSzebiH0a_IIYYDUgSNL6NGje-2CdwO6FEnnSPqLBCEmDG7wMZEHcM67DT6GmP9Pxz74KfmBy4Axdt6dkz9-gEyckYCvmD2npF1vfYbOBr_t4pLv_byz0JMpJDgqvs2gj3j8_o6K57vbp5uf5eT3_a-b60kJgulUNsBmrZK25Y2U7cwKlddGqZjWuqUNaiWh0kCtZWip0iC0FlxSW2FLleR8VJzufJfBv6wwJjN00WLfg0O_iobVVa20kKLK6PdP6MKvgsvTGSZpIzhTus7U5Y7Ki8UYcGaWoRsgrA2jZhOP2cZjNvGYTTxZcbVT_IM-H3WK87Ba5-KD_ddKJZmq-X_4GZjM</recordid><startdate>20140201</startdate><enddate>20140201</enddate><creator>Filipescu, Sorin</creator><creator>Miclea, Angela</creator><creator>Gross, Martin</creator><creator>Harzhauser, Mathias</creator><creator>Zágoršek, Kamil</creator><creator>Jipa, Cătălin</creator><general>De Gruyter Open</general><general>Earth Science Institute, Slovak Academy of Sciences</general><scope>AAYXX</scope><scope>CITATION</scope><scope>7UA</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>H96</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>PCBAR</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>H95</scope></search><sort><creationdate>20140201</creationdate><title>Early Sarmatian paleoenvironments in the easternmost Pannonian Basin (Borod Depression, Romania) revealed by the micropaleontological data</title><author>Filipescu, Sorin ; 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The investigated section, located near Vârciorog, was biostratigraphically and paleoenvironmentally analysed. The micro- and macrofossil assemblages include dasycladaceans, characeans, foraminifera, molluscs, polychaetes, ostracods, crabs, bryozoans, fish and vertebrate remains, which are characteristic for a shallow marine setting with local transitions to continental facies. The microfossil assemblages are characteristic for the Elphidium reginum Zone and Mohrensternia Zone of the early Sarmatian (Serravallian). The succession of populations correlates with the sedimentological trend, allowing the separation of several genetic units. The relative sea-level changes and the progradational trend from the top of the section suggest active tectonics in the hinterland (Apuseni Mountains). The shallow seas surrounding the emerging islands (Apuseni Mountains) provided the connections between the Pannonian and Transylvanian basins during the early Sarmatian</abstract><cop>Bratislava</cop><pub>De Gruyter Open</pub><doi>10.2478/geoca-2014-0005</doi><tpages>15</tpages><oa>free_for_read</oa></addata></record> |
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| subjects | Borod Depression (NW-Romania) bryozoans Decapoda Elphidium Foraminifera Marine Mollusca molluscs Ostracoda ostracods paleoenvironments paleogeography Sarmatian (late Middle Miocene) sequence stratigraphy |
| title | Early Sarmatian paleoenvironments in the easternmost Pannonian Basin (Borod Depression, Romania) revealed by the micropaleontological data |
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