Late Wuchiapingian (Late Dzhulfian, early Late Permian) limestone olistolites within the Tertiary flysch of Glypia Unit (Mount Parnon, central–eastern Peloponnesus, Greece)
Some olistolites reworked in a Tertiary flysch of Mount Parnon (Peloponnesus, Greece) exhibit a Late Permian assemblage, dominated by Paradunbarula (Shindella) shindensis, Hemigordiopsis cf . luquensis and Colaniella aff . minima. This association corresponds to the Late Wuchiapingian (=Late Dzhulfi...
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| creator | Skourtsos, Emmanuel Vachard, Daniel Zambetakis-Lekkas, Alexandra Martini, Rossana Zaninetti, Louisette |
| description | Some olistolites reworked in a Tertiary flysch of Mount Parnon (Peloponnesus, Greece) exhibit a Late Permian assemblage, dominated by
Paradunbarula (Shindella) shindensis,
Hemigordiopsis cf
. luquensis and
Colaniella aff
. minima. This association corresponds to the Late Wuchiapingian (=Late Dzhulfian), a substage whose algae and foraminifera are generally little known. Contemporaneous limestones crop out in the middle part of the Episkopi Formation in Hydra, but they are rather commonly reworked in Mesozoic and Cainozoic sequences. The palaeobiogeographical affinities shared by the foraminiferal markers of Greece, southeastern Pamir, and southern China, are very strong (up to the specific level), and are congruent with the Pangea B reconstructions.
To cite this article: E. Skourtsos et al., C. R. Geoscience 334 (2002) 925–931.
Les olistolithes calcaires d'un flysch tertiaire du mont Parnon (Péloponnèse, Grèce) révèlent des associations du Wuchiapingien supérieur (=Djoulfien supérieur ; Permien supérieur). L'une d'elles, caractérisée par
Paradunbarula (Shindella) shindensis, Hemigordiopsis cf.
luquensis et
Colaniella aff.
minima, permet d'aborder une discussion biostratigraphique sur les algues et foraminifères de ce sous-étage. Ces calcaires, généralement remaniés dans les diverses séries du Cénozoı̈que et du Mésozoı̈que, sont l'équivalent d'une partie de la formation d'Episcopi à Hydra. L'association confirme la grande identité des microfossiles de la Grèce, du Pamir du Sud-Est et de la Chine du Sud, au cours du Permien supérieur. Elle renforce les reconstitutions de type Pangée B.
Pour citer cet article : E. Skourtsos et al., C. R. Geoscience 334 (2002) 925–931. |
| doi_str_mv | 10.1016/S1631-0713(02)01830-8 |
| format | Article |
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Paradunbarula (Shindella) shindensis,
Hemigordiopsis cf
. luquensis and
Colaniella aff
. minima. This association corresponds to the Late Wuchiapingian (=Late Dzhulfian), a substage whose algae and foraminifera are generally little known. Contemporaneous limestones crop out in the middle part of the Episkopi Formation in Hydra, but they are rather commonly reworked in Mesozoic and Cainozoic sequences. The palaeobiogeographical affinities shared by the foraminiferal markers of Greece, southeastern Pamir, and southern China, are very strong (up to the specific level), and are congruent with the Pangea B reconstructions.
To cite this article: E. Skourtsos et al., C. R. Geoscience 334 (2002) 925–931.
Les olistolithes calcaires d'un flysch tertiaire du mont Parnon (Péloponnèse, Grèce) révèlent des associations du Wuchiapingien supérieur (=Djoulfien supérieur ; Permien supérieur). L'une d'elles, caractérisée par
Paradunbarula (Shindella) shindensis, Hemigordiopsis cf.
luquensis et
Colaniella aff.
minima, permet d'aborder une discussion biostratigraphique sur les algues et foraminifères de ce sous-étage. Ces calcaires, généralement remaniés dans les diverses séries du Cénozoı̈que et du Mésozoı̈que, sont l'équivalent d'une partie de la formation d'Episcopi à Hydra. L'association confirme la grande identité des microfossiles de la Grèce, du Pamir du Sud-Est et de la Chine du Sud, au cours du Permien supérieur. Elle renforce les reconstitutions de type Pangée B.
Pour citer cet article : E. Skourtsos et al., C. R. Geoscience 334 (2002) 925–931.</description><identifier>ISSN: 1631-0713</identifier><identifier>ISSN: 1778-7025</identifier><identifier>EISSN: 1778-7025</identifier><identifier>DOI: 10.1016/S1631-0713(02)01830-8</identifier><language>eng ; fre</language><publisher>Paris: Elsevier SAS</publisher><subject>algae ; biostratigraphie ; biostratigraphy ; Dzhulfian ; Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; foraminifera ; foraminifères ; Greece ; Grèce ; palaeogeography ; paléogéographie ; Permian ; Permien ; Petrology of sedimentary rocks except quaternary rocks ; Sedimentary rocks ; Stratigraphy ; Wuchiapingian ; Wuchiapingien</subject><ispartof>Comptes rendus. Geoscience, 2002-09, Vol.334 (12), p.925-931</ispartof><rights>2002 Académie des sciences / Éditions scientifiques et médicales Elsevier SAS</rights><rights>2002 INIST-CNRS</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a438t-84b6222e6952a61190d72a4d9bc4aa9e922920cc2c383315d09c271bc3836d6b3</citedby><cites>FETCH-LOGICAL-a438t-84b6222e6952a61190d72a4d9bc4aa9e922920cc2c383315d09c271bc3836d6b3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/S1631-0713(02)01830-8$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>314,780,784,3550,27924,27925,45995</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=14197957$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Skourtsos, Emmanuel</creatorcontrib><creatorcontrib>Vachard, Daniel</creatorcontrib><creatorcontrib>Zambetakis-Lekkas, Alexandra</creatorcontrib><creatorcontrib>Martini, Rossana</creatorcontrib><creatorcontrib>Zaninetti, Louisette</creatorcontrib><title>Late Wuchiapingian (Late Dzhulfian, early Late Permian) limestone olistolites within the Tertiary flysch of Glypia Unit (Mount Parnon, central–eastern Peloponnesus, Greece)</title><title>Comptes rendus. Geoscience</title><description>Some olistolites reworked in a Tertiary flysch of Mount Parnon (Peloponnesus, Greece) exhibit a Late Permian assemblage, dominated by
Paradunbarula (Shindella) shindensis,
Hemigordiopsis cf
. luquensis and
Colaniella aff
. minima. This association corresponds to the Late Wuchiapingian (=Late Dzhulfian), a substage whose algae and foraminifera are generally little known. Contemporaneous limestones crop out in the middle part of the Episkopi Formation in Hydra, but they are rather commonly reworked in Mesozoic and Cainozoic sequences. The palaeobiogeographical affinities shared by the foraminiferal markers of Greece, southeastern Pamir, and southern China, are very strong (up to the specific level), and are congruent with the Pangea B reconstructions.
To cite this article: E. Skourtsos et al., C. R. Geoscience 334 (2002) 925–931.
Les olistolithes calcaires d'un flysch tertiaire du mont Parnon (Péloponnèse, Grèce) révèlent des associations du Wuchiapingien supérieur (=Djoulfien supérieur ; Permien supérieur). L'une d'elles, caractérisée par
Paradunbarula (Shindella) shindensis, Hemigordiopsis cf.
luquensis et
Colaniella aff.
minima, permet d'aborder une discussion biostratigraphique sur les algues et foraminifères de ce sous-étage. Ces calcaires, généralement remaniés dans les diverses séries du Cénozoı̈que et du Mésozoı̈que, sont l'équivalent d'une partie de la formation d'Episcopi à Hydra. L'association confirme la grande identité des microfossiles de la Grèce, du Pamir du Sud-Est et de la Chine du Sud, au cours du Permien supérieur. Elle renforce les reconstitutions de type Pangée B.
Pour citer cet article : E. Skourtsos et al., C. R. Geoscience 334 (2002) 925–931.</description><subject>algae</subject><subject>biostratigraphie</subject><subject>biostratigraphy</subject><subject>Dzhulfian</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>foraminifera</subject><subject>foraminifères</subject><subject>Greece</subject><subject>Grèce</subject><subject>palaeogeography</subject><subject>paléogéographie</subject><subject>Permian</subject><subject>Permien</subject><subject>Petrology of sedimentary rocks except quaternary rocks</subject><subject>Sedimentary rocks</subject><subject>Stratigraphy</subject><subject>Wuchiapingian</subject><subject>Wuchiapingien</subject><issn>1631-0713</issn><issn>1778-7025</issn><issn>1778-7025</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2002</creationdate><recordtype>article</recordtype><recordid>eNqFUduKFDEUbETBdfUThLwoM7CtSfqSzpPIuo7CiAvu4mM4kz5tRzJJb5JWZp_8B__Dj_JLzMys-OhTzimqTlGponjK6AtGWfvyE2srVlLBqgXlS8q6ipbdveKECdGVgvLmfp7_Uh4Wj2L8SrNOiu6k-LWGhOTzrEcDk3FfDDiyOGBvbsfZDnk_IwjB7sgBvcSwzdiSWLPFmLxD4q3JgzUJI_lu0mgcSSOSKwzJQNiRwe6iHokfyMruJgPk2plEFh_87BK5hOB8ttDoUgD7-8dPhJgwuOxk_eSdwzjHM7IKiBqXj4sHA9iIT-7e0-L67cXV-bty_XH1_vz1uoS66lLZ1ZuWc46tbDi0jEnaCw51Lze6BpAoOZecas111VUVa3oqNRdss1_bvt1Up8Xz490p-Js5B1VbEzVaCw79HFXFa9Y0UmRicyTq4GMMOKgpmG2OrRhV-3bUoR21_3pFuTq0o7qse3ZnAFGDHQI4beI_cc2kkM3-_qsjD3PabwaDitqg09ibgDqp3pv_OP0BvdSm3w</recordid><startdate>20020901</startdate><enddate>20020901</enddate><creator>Skourtsos, Emmanuel</creator><creator>Vachard, Daniel</creator><creator>Zambetakis-Lekkas, Alexandra</creator><creator>Martini, Rossana</creator><creator>Zaninetti, Louisette</creator><general>Elsevier SAS</general><general>Elsevier</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7U5</scope><scope>8FD</scope><scope>FR3</scope><scope>H8D</scope><scope>KR7</scope><scope>L7M</scope></search><sort><creationdate>20020901</creationdate><title>Late Wuchiapingian (Late Dzhulfian, early Late Permian) limestone olistolites within the Tertiary flysch of Glypia Unit (Mount Parnon, central–eastern Peloponnesus, Greece)</title><author>Skourtsos, Emmanuel ; Vachard, Daniel ; Zambetakis-Lekkas, Alexandra ; Martini, Rossana ; Zaninetti, Louisette</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a438t-84b6222e6952a61190d72a4d9bc4aa9e922920cc2c383315d09c271bc3836d6b3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng ; fre</language><creationdate>2002</creationdate><topic>algae</topic><topic>biostratigraphie</topic><topic>biostratigraphy</topic><topic>Dzhulfian</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>foraminifera</topic><topic>foraminifères</topic><topic>Greece</topic><topic>Grèce</topic><topic>palaeogeography</topic><topic>paléogéographie</topic><topic>Permian</topic><topic>Permien</topic><topic>Petrology of sedimentary rocks except quaternary rocks</topic><topic>Sedimentary rocks</topic><topic>Stratigraphy</topic><topic>Wuchiapingian</topic><topic>Wuchiapingien</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Skourtsos, Emmanuel</creatorcontrib><creatorcontrib>Vachard, Daniel</creatorcontrib><creatorcontrib>Zambetakis-Lekkas, Alexandra</creatorcontrib><creatorcontrib>Martini, Rossana</creatorcontrib><creatorcontrib>Zaninetti, Louisette</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Solid State and Superconductivity Abstracts</collection><collection>Technology Research Database</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Civil Engineering Abstracts</collection><collection>Advanced Technologies Database with Aerospace</collection><jtitle>Comptes rendus. Geoscience</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Skourtsos, Emmanuel</au><au>Vachard, Daniel</au><au>Zambetakis-Lekkas, Alexandra</au><au>Martini, Rossana</au><au>Zaninetti, Louisette</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Late Wuchiapingian (Late Dzhulfian, early Late Permian) limestone olistolites within the Tertiary flysch of Glypia Unit (Mount Parnon, central–eastern Peloponnesus, Greece)</atitle><jtitle>Comptes rendus. Geoscience</jtitle><date>2002-09-01</date><risdate>2002</risdate><volume>334</volume><issue>12</issue><spage>925</spage><epage>931</epage><pages>925-931</pages><issn>1631-0713</issn><issn>1778-7025</issn><eissn>1778-7025</eissn><abstract>Some olistolites reworked in a Tertiary flysch of Mount Parnon (Peloponnesus, Greece) exhibit a Late Permian assemblage, dominated by
Paradunbarula (Shindella) shindensis,
Hemigordiopsis cf
. luquensis and
Colaniella aff
. minima. This association corresponds to the Late Wuchiapingian (=Late Dzhulfian), a substage whose algae and foraminifera are generally little known. Contemporaneous limestones crop out in the middle part of the Episkopi Formation in Hydra, but they are rather commonly reworked in Mesozoic and Cainozoic sequences. The palaeobiogeographical affinities shared by the foraminiferal markers of Greece, southeastern Pamir, and southern China, are very strong (up to the specific level), and are congruent with the Pangea B reconstructions.
To cite this article: E. Skourtsos et al., C. R. Geoscience 334 (2002) 925–931.
Les olistolithes calcaires d'un flysch tertiaire du mont Parnon (Péloponnèse, Grèce) révèlent des associations du Wuchiapingien supérieur (=Djoulfien supérieur ; Permien supérieur). L'une d'elles, caractérisée par
Paradunbarula (Shindella) shindensis, Hemigordiopsis cf.
luquensis et
Colaniella aff.
minima, permet d'aborder une discussion biostratigraphique sur les algues et foraminifères de ce sous-étage. Ces calcaires, généralement remaniés dans les diverses séries du Cénozoı̈que et du Mésozoı̈que, sont l'équivalent d'une partie de la formation d'Episcopi à Hydra. L'association confirme la grande identité des microfossiles de la Grèce, du Pamir du Sud-Est et de la Chine du Sud, au cours du Permien supérieur. Elle renforce les reconstitutions de type Pangée B.
Pour citer cet article : E. Skourtsos et al., C. R. Geoscience 334 (2002) 925–931.</abstract><cop>Paris</cop><pub>Elsevier SAS</pub><doi>10.1016/S1631-0713(02)01830-8</doi><tpages>7</tpages><oa>free_for_read</oa></addata></record> |
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| subjects | algae biostratigraphie biostratigraphy Dzhulfian Earth sciences Earth, ocean, space Exact sciences and technology foraminifera foraminifères Greece Grèce palaeogeography paléogéographie Permian Permien Petrology of sedimentary rocks except quaternary rocks Sedimentary rocks Stratigraphy Wuchiapingian Wuchiapingien |
| title | Late Wuchiapingian (Late Dzhulfian, early Late Permian) limestone olistolites within the Tertiary flysch of Glypia Unit (Mount Parnon, central–eastern Peloponnesus, Greece) |
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