Kimmeridgian oor Spaans

Kimmeridgian

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A subdivision of the Jurassic period.

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Kimmeridgiense

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en
subdivision of the Jurassic period
Marine conditions prevailed over most of the area during the Lower Kimmeridgian.
En el Kimmeridgiense inferior predominan en gran parte de la región condiciones marítimas.
Termium

Kimeridgiano

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kimmeridgiense

Marine conditions prevailed over most of the area during the Lower Kimmeridgian.
En el Kimmeridgiense inferior predominan en gran parte de la región condiciones marítimas.
Termium

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kimmeridgian

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kimmeridgiano

A continuous marine environment existed in the Hettangian-Tithonian span, with volcanic events in the Bajocian, Callovian, Kimmeridgian, and Tithonian.
Hay un desarrollo marino continuo entre el Hettangiano y el Titoniano y facies evaporíticas en el Oxfordiano-Kimmeridgiano.
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Bellubrunnus (meaning "the beautiful one of Brunn" in Latin) is an extinct genus of rhamphorhynchid pterosaur from the Late Jurassic (Kimmeridgian stage) of southern Germany.
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Finally, the warm summer temperatures together with the heat from the sunrays reverberating from the Kimmeridgian stones endow the wine with its typical notes of candied fruit and spices as it ages.
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The Kimmeridgian follows the Oxfordian and precedes the Tithonian.
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Nearly all zones of the Callovian, Oxfordian and Kimmeridgian are documented by fossils.
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Apatosaurus lived about 152 to 151 million years ago (mya), during the late Kimmeridgian to early Tithonian age, and are now known from fossils in the Morrison Formation of modern-day Colorado, Oklahoma, New Mexico, Wyoming, and Utah in the United States.
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Marine conditions prevailed over most of the area during the Lower Kimmeridgian.
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They were most diverse throughout the Cretaceous period, though Thrissops fossils are known from the Oxfordian-Kimmeridgian boundary in the Late Jurassic.
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The incline of the winegrowing slopes ensures optimal natural drainage, which is also guaranteed by the crack formation in the Kimmeridgian limestone.
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Tendaguripterus was a genus of dsungaripteroid pterodactyloid pterosaur from the Kimmeridgian-Tithonian-age Upper Jurassic Middle Saurian Beds of Tendaguru, Mtwara Region, Tanzania.
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It lived from 145 to 150 million years ago, during the Kimmeridgian to Tithonian ages of the Late Jurassic period.
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The Kimmeridgian, characterised by alternating marl and calcareous banks, is the source of the best soils of the vineyards, which are composed of grey clay-limestone colluviums covering the slopes and enclose a multitude of small stones that help warm the ground.
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G. acutus: Western Europe (France) of the Late Jurassic (Kimmeridgian) Lennier G. 1887.
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The soil consists of limestone dating from the middle and upper Jurassic period (Callovian to Kimmeridgian from east to west).
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A. louisae fossils are rare, known only from one site in the upper Brushy Basin Member; they date to the late Kimmeridgian stage, about 151 mya.
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The western escarpment, between the Col de l'Épine and the Col de Saint-Michel, is composed of limestones from the Kimmeridgian and Oxfordian formations, with scree at the base.
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The Kimmeridgian makes up most of the geological substrate, deeply carved in the centre by the Laignes Valley and a number of peripheral dells.
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It contains two known species: Galeamopus hayi, known from the Late Jurassic lower Morrison Formation (Kimmeridgian age, about 155 million years ago) of Wyoming, United States, and Galeamopus pabsti, known from the Late Jurassic fossils from Wyoming and Colorado.
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The coral-bearing layers are identified by ammonites as early to middle Lower Kimmeridgian.
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The holotype, CV OO722, was found in a layer of the late Upper Shaximiao Formation, probably dating from the early Kimmeridgian.
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These bones were discovered in sandstone of the late Kimmeridgian-age (late Jurassic, approximately 152 million years old) Praia da Amoreira-Porto Novo Member of the Alcobaça Formation in Porto das Barcas, Lourinhã, Portugal.
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The first part of the genus name of Kimmerosaurus comes from the location of the first Kimmerosaurus fossils, Kimmeridge Clay deposits of Dorset, England (these deposits are also the root word for the Kimmeridgian stage of the Jurassic period).
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The formation is Late Jurassic in age (Kimmeridgian/Tithonian) and is notable for containing a fauna similar to that of the Morrison Formation in the United States and the Tendaguru beds in Tanzania.
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However, several indeterminate velociraptorines have also been discovered, dating to the Kimmeridgian stage, in the Late Jurassic Period.
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Jens Zinke in 1998 assigned forty-nine teeth from the Kimmeridgian Guimarota formation of Portugal to the genus.
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