Aptian oor Spaans

Aptian

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A subdivision of the Early (Lower) Cretaceous epoch.

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Aptiense

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en
subdivision of the Early Cretaceous epoch
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Aptiano

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aptiense

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Aptian stage
Aptiense

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Descriptions of new plant macrofossils from the Lower Cretaceous (Aptian-Albian) of Colombia are presented.
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In these areas, Psittacosaurus mongoliensis fossils are found in most sedimentary strata dating to the Aptian to Albian stages of the Early Cretaceous Period, or approximately 125 to 100 mya.
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Sapeornis is a type of avialan which lived during the early Cretaceous period (late Aptian to early Albian, roughly 125-120 mya).
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All specimens of Changchunsaurus were collected from the Quantou Formation of the Songliao Basin, dating to the Aptian–Cenomanian stages.
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Based on changes in ammonite taxa, the boundary between the Aptian and Albian stages of the Early Cretaceous has been located within the Glen Rose Formation of Texas, which may contain Acrocanthosaurus footprints and lies just above the Twin Mountains Formation.
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The holotype, USNM 540686, was found in the Patuxent Formation, dating from the late Aptian.
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It is of Aptian stage (Early Cretaceous), and is notable for its fossils of dinosaurs.
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Amargasaurus was discovered in sedimentary rocks of the La Amarga Formation, which dates back to the Barremian and late Aptian stages of the Early Cretaceous.
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Mystiornis is an extinct genus of bird which existed in what is now western Siberia, Russia during the early Cretaceous period (Barremian/Aptian age).
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Fossils have been found from the Nova Olinda Member of the Aptian-age Crato Formation in the Araripe and Lima Campos Basins of northeastern Brazil.
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Maaradactylus is based on Museu Paleontologico de Santana do Cariri specimen MPSC R 2357, a skull, atlas, and axis discovered in 2010 in the Aptian—Albian-age Romualdo Formation of Sítio São Gonçalo, Santana do Cariri, Ceará, in the Araripe Basin of Brazil.
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Both specimens come from the Aptian-age Lower Cretaceous Jiufotang Formation of Liaoning, with an estimated date of 120 million years ago.
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The Sabaletas greenchists (Arquía complex) yields 39Ar-40Ar plateau age of 127±5 Ma and integrated ages between 102-115 Ma eventually recording the initial accommodation of the Albian-Aptian volcano-sedimentary sequence of the Quebradagrande Complex to the continental margin.
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Ultrasaurus lived 100 to 110 million years ago, during the Aptian and Albian stages of the early Cretaceous.
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Jeholosaurids were herbivorous neornithischian dinosaurs from the Cretaceous Period (Aptian - Santonian, with a possible Campanian record) of Asia.
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This indicates that the Twin Mountains Formation lies entirely within the Aptian stage, which lasted from 125 to 112 million years ago.
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It contains a single species, Liaoningosaurus paradoxus, and is represented by two fossil specimens collected from the Yixian Formation (Aptian age) of Liaoning Province.
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The Paja Formation is a Mesozoic geologic formation from the Aptian epochs of the Early Cretaceous of central Colombia, extending on the Altiplano Cundiboyacense in the Eastern Ranges of the Colombian Andes in the departments of Cundinamarca, Santander and Boyacá.
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Ankylosaurians attained large sizes at the Aptian-Albian boundary; both Peloroplites and Cedarpelta are comparable in size to Sauropelta, a nodosaurid from about the same time but known from the Cloverly Formation of Wyoming and Montana.
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These allow postulating the same age for both units within the Albian-Aptian range. The petrographic, lithologic, litogeoquímica, radiometric information and estratigrágicas relations suggest that both units may have been generated in the same magmatic arc and were subsequently dismembered by Romeral Fault System The magmatic arc that led to the Barroso Formation, Quebradagrande Complex and associated plutons, got emplaced along the weaker zone, or convergence zone of oceanic and continental crust, which were next to each other, or very close together. This is based to the composition of the clusters associated with Quebradagrande Complex, with input from both cortices and the intrusion of plutons as Sabanalarga Batholith, Buritica tonalite and Diorite of Altavista.
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Based on correlation with the Trinity Group of Texas, the Antlers Formation is estimated to be late Aptian-early Albian.
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It contains the single species Corriebaatar marywaltersae and represents the first evidence of Australian multituberculates Fossils date back to the Aptian stage of the Early Cretaceous.
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The Lower Greensand (known as the Woburn Sand north of the London Basin) is of Aptian age.
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Two nearly complete, articulated skeletons and a variety of disarticulated material from other individuals of all ages are known from the Ilek Formation of Siberia, which ranges from the Aptian to Albian stages of the Early Cretaceous.
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Barbosania is an extinct genus of crestless ornithocheirid pterosaur from the Cretaceous Romualdo Member of the Santana Formation of northeastern Brazil, dating to the Aptian to Albian.
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