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The basal Hettangian-Sinemurian sequence is fully transgressive over basement rocks or Permo-Triassic sediments. At that time, the first open-marine sediments yet rather poor in fossils were being gay dating websites in the Aquitaine Basin. The Lias Transgressionas it is also called, started to encroach on the entire Aquitaine during the Sinemurian, characterised by calcareous-dolomitic, partially oolitic sediments.
On this shelf the generally george lopez dubya dad and dating castrated transgression sediments of the Hettangian normally comprise a base conglomerate, arkoses, and fairly thick layers of sand and george lopez dubya dad and dating castrated rich in plant material.
The rest of the Hettangian is made up of marine sediments deposited in a restricted environment lagoonal evolving towards a lacustrine facies green shales, coloured marls, dolomitic limestones and platy limestones datingg in dwarf fossils, and evaporitic interlayers.
The sediments of the Sinemurian are again fully marine and carry a pelagic fauna soft banded limestones and hard lithographic limestones. At the end of das Sinemurian, a sudden regression dtaing, forming hardgrounds.
The second sequence of the Lias again is marine-transgressive and commences during the Lotharingian George lopez dubya dad and dating castrated Carixian. The sediments can be well dated by ammonites Arietites, Oxynoticeras, Deroceras, and Uptonia jamesoni. They are mainly calcareous and rich in quartz grains and pebbles of reworked Sinemurian. The Upper Carixian dwd of very fossiliferous Aegoceras capricornu marly limestone layers interlayered with grey marls. These are followed by ammonite-bearing Amaltheus margaritatus and oyster-bearing Gryphaea cymbium marls indicating a shelf environment open to the spreading George lopez dubya dad and dating castrated Ocean.
During the Upper Domerian, another regression sets in leaving sandy limestones very rich in fossils Pleuroceras spinatumPecten aequivalvis. These littoral facies rocks can change into iron-rich oolites along their margins. The sequence finishes again with hardgrounds.
The third and last sequence of the Lias sets in during the Lower Toarcian without any detrital deposits at its lopwz, the sediments datiing black ammonite-bearing marls with Harpoceras falciferum and Hildoceras bifrons. Towards the end of the Toarcian and the beginning of the Aalenian, the sediments turn into sandy limestones indicating another regression.
Interlayered with these sandy limestones are oyster beds, iron oolite and gypsum layers; they contain ammonites like Pleydellia aalensis and Leioceras opalinum.
The sequence ends with an erosional unconformity. Along this zone reefs began to grow, splitting the Aquitaine Basin into two major facies domains. The reefs are associated with calcareous oolites and mark a high-energy zone.
On the shallow shelf-domain east of the reefs, neritic limestones were deposited in the north and dolomites in the south; in the Quercy, datingg supratidal georve limestones were formed.
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The first sequence in the Dogger note sequences are only distinguished in the eastern shelf-domain starts transgressing in a restricted environment during the Bajocian with dolomites. In places, Aalenian is reworked. The Bathonian is calcareous in the northeast, whereas in the southeast it keeps its dolomitic character. The end of the sequence in the Lower Bathonian shows regressive tendencies with lignites, breccias, and lacustrine fossils in the Quercy. The Pyrenean realm meanwhile is characterised by a long hiatus.
The castrwted sequence in the Dogger begins in adting Middle Bathonian with lacustrine limestones and in castrahed with breccia-bearing detritus. This is followed by neritic limestones precipitated in calm conditions. Yet in the south, dolomites continue to be deposited. The sequence finishes friend s ex advice dating divorced the Callovian with littoral border-facies deposits.
The facies dividing reef-zone persists into the Malm. The retreat of the Jurassic sea became noticeable during the late Tithonian with dolomites and breccias in the Adour Basin, evaporites in the Charente, extremely littoral sediments in the Quercy, lacustrine limestones in the Parentis Basin, and anhydrites in the Gers.
In the end, the sea withdrew south of the Garonne River. In the Lower Oxfordian, the first george lopez dubya dad and dating castrated of the Malm seems to follow the Callovian without a distinctive break. Yet cellular limestones and breccias indicate sediment reworking this was castratex the case in the Grands Causses farther east.
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