| dbo:abstract |
The Fremouw Formation is a Triassic-age rock formation in the Transantarctic Mountains of Antarctica. It contains the oldest known fossils of tetrapods from Antarctica, including synapsids, reptiles and amphibians. Fossilized trees have also been found. The formation's beds were deposited along the banks of rivers and on floodplains. During the Triassic, the area would have been a riparian forest at 70–75°S latitude. (en) La formation de Fremouw est une formation géologique du Trias, située dans la chaîne Transantarctique de l'Antarctique. Des fossiles de reptiles et d'amphibiens préhistoriques ont été découverts dans cette formation ainsi que des arbres fossilisés. Les couches géologiques de la formation se sont déposées le long des berges de rivières et de plaines inondables. Au cours du Trias, la région aurait été une zone riparienne (forêt galerie) à 70-75° de latitude sud. (fr) De Fremouw-formatie is een geologische formatie op Antarctica. De formatie is beroemd omdat uit de gevonden fossielen blijkt dat Antarctica niet altijd een ijskoud, ontoegankelijk continent was. De Fremouw-formatie stamt uit het tijdvak Trias (periodes Induan tot Anisian - 251 tot 237 miljoen jaar geleden). De eerste fossielen werden in 1969 gevonden. Naast de Fremouw-formatie zijn ook in de Lashly-formatie en de Hanson-formatie fossielen van dieren uit het Mesozoïcum gevonden. (nl) La Formazione Fremouw è una formazione geologica risalente al Triassico che si trova nei Monti Transantartici, nell'Antartide. In questa formazione sono stati trovati fossili di rettili e anfibi, oltre a alberi fossilizzati. Gli strati della formazione si sono depositati lungo le rive di antichi fiumi e pianure alluvionali. Durante il Triassico, l'area era probabilmente una zona di foreste ripariali situate alla latitudine 70–75°S. (it) |
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| dbp:age |
latest Permian-early Late Triassic (en) |
| dbp:name |
Fremouw Formation (en) |
| dbp:overlies |
dbr:Buckley_Formation |
| dbp:period |
Triassic (en) |
| dbp:prilithology |
dbr:Siltstone dbr:Sandstone dbr:Mudstone |
| dbp:region |
Transantarctic Mountains of Antarctica (en) |
| dbp:subunits |
Lower, middle, upper (en) |
| dbp:thickness |
up to (en) |
| dbp:type |
dbr:Geological_formation |
| dbp:underlies |
dbr:Falla_Formation |
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dbr:Beacon_Supergroup |
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| gold:hypernym |
dbr:Formation |
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-84.0 165.0 |
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| rdfs:comment |
The Fremouw Formation is a Triassic-age rock formation in the Transantarctic Mountains of Antarctica. It contains the oldest known fossils of tetrapods from Antarctica, including synapsids, reptiles and amphibians. Fossilized trees have also been found. The formation's beds were deposited along the banks of rivers and on floodplains. During the Triassic, the area would have been a riparian forest at 70–75°S latitude. (en) La formation de Fremouw est une formation géologique du Trias, située dans la chaîne Transantarctique de l'Antarctique. Des fossiles de reptiles et d'amphibiens préhistoriques ont été découverts dans cette formation ainsi que des arbres fossilisés. Les couches géologiques de la formation se sont déposées le long des berges de rivières et de plaines inondables. Au cours du Trias, la région aurait été une zone riparienne (forêt galerie) à 70-75° de latitude sud. (fr) De Fremouw-formatie is een geologische formatie op Antarctica. De formatie is beroemd omdat uit de gevonden fossielen blijkt dat Antarctica niet altijd een ijskoud, ontoegankelijk continent was. De Fremouw-formatie stamt uit het tijdvak Trias (periodes Induan tot Anisian - 251 tot 237 miljoen jaar geleden). De eerste fossielen werden in 1969 gevonden. Naast de Fremouw-formatie zijn ook in de Lashly-formatie en de Hanson-formatie fossielen van dieren uit het Mesozoïcum gevonden. (nl) La Formazione Fremouw è una formazione geologica risalente al Triassico che si trova nei Monti Transantartici, nell'Antartide. In questa formazione sono stati trovati fossili di rettili e anfibi, oltre a alberi fossilizzati. Gli strati della formazione si sono depositati lungo le rive di antichi fiumi e pianure alluvionali. Durante il Triassico, l'area era probabilmente una zona di foreste ripariali situate alla latitudine 70–75°S. (it) |
| rdfs:label |
Fremouw Formation (en) Formation de Fremouw (fr) Formazione Fremouw (it) Fremouw-formatie (nl) |
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freebase:Fremouw Formation yago-res:Fremouw Formation wikidata:Fremouw Formation dbpedia-fr:Fremouw Formation dbpedia-it:Fremouw Formation dbpedia-nl:Fremouw Formation https://global.dbpedia.org/id/4jevB |
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POINT(165 -84) |
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-84.000000 (xsd:float) |
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165.000000 (xsd:float) |
| prov:wasDerivedFrom |
wikipedia-en:Fremouw_Formation?oldid=1078893922&ns=0 |
| foaf:depiction |
wiki-commons:Special:FilePath/Bowenia_Spectabilis_in_Prague_Botanical_Garden_DSC_0083.jpg wiki-commons:Special:FilePath/Cryobatrachus_kitchingi.jpg wiki-commons:Special:FilePath/KryostegaDB16.jpg wiki-commons:Special:FilePath/Parotosuchus_BW.jpg wiki-commons:Special:FilePath/Prolacerta_broomi.jpg wiki-commons:Special:FilePath/Cynognathus_NT_small.jpg wiki-commons:Special:FilePath/Thrinaxodon_BW.jpg wiki-commons:Special:FilePath/Myosaurus.jpg wiki-commons:Special:FilePath/Lystrosaurus_BW.jpg wiki-commons:Special:FilePath/Procolophon_BW.jpg wiki-commons:Special:FilePath/Ericiolacerta_BW.jpg |
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