1985
DOI: 10.2113/gssgfbull.i.5.637
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Presentation de 9 cartes paleogeographiques au 1/20000000000eme s'etendant de l'Atlantique au Pamir pour la periode du Lias a l'Actuel

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Cited by 247 publications
(58 citation statements)
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“…The marine influences were most frequent in Italy (at the Tortonian, Aquitanian, Oligocene, Paleocene and Campanian-Santonian periods) and less important for the Jura (Tortonian) and Spain (Campanian-Santonian, Paleocene). The Krim region was inundated Sampling strategy to assess groundwater biodiversity 787 during the Campanian-Santonian, Paleocene and Oligocene periods; the Roussillon at the Campanian-Santonian, Paleocene and Pliocene periods (Debrand-Passard & Courbouleix, 1984;Dercourt et al, 1985). Concomitantly, many thalassoid species, including syncarids (Guil & Camacho, 2001), some amphipods (Notenboom, 1991) and isopods (Coineau, 1994), were observed in those regions most influenced by Tethys belts.…”
Section: Groundwater Species Richnessmentioning
confidence: 99%
“…The marine influences were most frequent in Italy (at the Tortonian, Aquitanian, Oligocene, Paleocene and Campanian-Santonian periods) and less important for the Jura (Tortonian) and Spain (Campanian-Santonian, Paleocene). The Krim region was inundated Sampling strategy to assess groundwater biodiversity 787 during the Campanian-Santonian, Paleocene and Oligocene periods; the Roussillon at the Campanian-Santonian, Paleocene and Pliocene periods (Debrand-Passard & Courbouleix, 1984;Dercourt et al, 1985). Concomitantly, many thalassoid species, including syncarids (Guil & Camacho, 2001), some amphipods (Notenboom, 1991) and isopods (Coineau, 1994), were observed in those regions most influenced by Tethys belts.…”
Section: Groundwater Species Richnessmentioning
confidence: 99%
“…During the Permian to Early Jurassic, South Tethys began to widen with the formation of oceanic crust, as the result of the northward drift of Central Iran; while a Palaeo-Tethys Ocean, which existed during the Palaeozoic at the present northern margin of the Elburz Range, progressively narrowed and was closed by the end of the Lias (Stöcklin, 1974). After the suture of Palaeo-Tethys, the African-Arabian plate continued to move northwards (Dercourt et al, 1985;Scotese and Golenka, 1993).…”
Section: The First Period Of Stability Of the Arabian Platformmentioning
confidence: 99%
“…Biogenic phosphates were selected from the western (Normandy, Boulonnais, south England) and the eastern (Burgundy, Jura, and southeast basin) parts of the Anglo-Paris Basin. The paleogeographic map (modified after Dercourt et al [1985] and Ziegler [1988]) shows that Western Europe occupied a tropical position during the Middle-Late Jurassic; a latitude is shown and labelled 20°-30°to give an estimate of uncertainties. Since the Bathonian, the Anglo-Paris basin, located at the occidental extremity of the Tethys, was connected northward to boreal realms.…”
Section: Sample Collectionmentioning
confidence: 99%