Hekou Formation | |
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Stratigraphic range: Late Cretaceous, | |
Type | Geological formation |
Unit of | Guifeng Group |
Underlies | Tangbian Formation |
Overlies | Unconformity: Zhoutian Formation |
Lithology | |
Primary | Conglomerate, glutenite |
Other | Sandstone, siltstone, tuff |
Location | |
Region | Jiangxi Province, Asia |
Country | China |
The Hekou Formation is a Cretaceous geologic formation in China. Pterosaur fossils have been recovered from the formation. It is a unit of the Guifeng Group and dates to the Late Cretaceous. [2] Dinosaur fossils from the formation include a nearly perfect oviraptorid embryo nicknamed Baby Yingliang, an unnamed large hadrosaurid, and hadrosauroid eggs with embryos. [3] [4] [5] Mammal fossils include Erythrobaatar and Yubaatar qianzhouensis . [6] [7] The polyglyphanodontian lizard Yechilacerta has also been described from the formation. [8]
The Hekou Formation is a constituent of the Guifeng Group; a sequence of formations that were deposited in the Xinjiang Basin including the Hekou, Tangbian, and Lianhe formation which record aeolian-alluvial interactions in a palaeoplateau desert. Both a successional and coeval model of the deposition of these units have been proposed, with estimated ages of the Hekou formation ranging from Coniacian-Santonian to Maastrichtian. [9] [10] The associated facies include alluvial fans and adjacent wadi river channels, with mudcracks indicating subaerial exposure of the deposits. Oxygen-18 isotope values recorded in Dinosaur eggshells indicated low annual precipitation and humidity, suggesting an arid to semi-arid environment. The occurrence of striated cobbles in the alluvial facies suggests glacial activity in the catchment areas of the Cretaceous plateau. [11] [12]