Haifanggou Formation in the context of Lacustrine


Haifanggou Formation in the context of Lacustrine

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⭐ Core Definition: Haifanggou Formation

The Haifanggou Formation (simplified Chinese: 海房沟组; traditional Chinese: 海房溝組; pinyin: Hǎifánggōu zǔ), also known as the Jiulongshan Formation (simplified Chinese: 九龙山组; traditional Chinese: 九龍山組; pinyin: Jiǔlóngshān zǔ), is a fossil-bearing rock deposit located near Daohugou (simplified Chinese: 道虎沟; traditional Chinese: 道虎溝) village of Ningcheng County, in Inner Mongolia, northeastern China.

The formation consists of coarse conglomerates, sandstone, mudstone, and thin coal layers deposited in deltaic and lacustrine environments.

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Haifanggou Formation in the context of Tiaojishan Formation

The Tiaojishan Formation is a geological formation in Hebei and Liaoning, People's Republic of China, dating to the middle-late Jurassic period (Bathonian-Oxfordian stages). It is known for its exceptionally preserved fossils, including those of plants, insects and vertebrates. It is made up mainly of pyroclastic rock interspersed with basic volcanic and sedimentary rocks. Previously, the Tiaojishan Formation was grouped together with the underlying Haifanggou Formation (also known as the Jiulongshan Formation) as a single "Lanqi Formation." The Tiaojishan Formation forms a key part of the Yanliao Biota assemblage, alongside the Haifanggou Formation.

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Haifanggou Formation in the context of Yanliao Biota

The Yanliao Biota is the name given to an assembly of fossils preserved in northeastern China from the Middle to Late Jurassic. It includes fossils from the Tiaojishan Formation and Haifanggou Formation. This spans approximately 165 to 150 million years ago.

Like the Jehol Biota, these deposits are composed of alternating layers of volcanic tuff and sediment, and are considered Lagerstätte. These are some of the best preserved Jurassic fossils in the world, and include many important dinosaur, mammal, salamander, insect and lizard specimens, as well as plants.

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