Tiaojishan FormationJurassic fossilsDaohugou Bedspterosaurstheropods

Tiaojishan Formation: A Window into Jurassic Biodiversity

Tiaojishan Formation: A Window into Jurassic Biodiversity The Tiaojishan Formation is a geological treasure trove located across Hebei, Inner Mongolia, and Liaoning in China. Spanning the...

Tiaojishan Formation: A Window into Jurassic Biodiversity

The Tiaojishan Formation is a geological treasure trove located across Hebei, Inner Mongolia, and Liaoning in China. Spanning the Callovian to Kimmeridgian stages of the Middle to Late Jurassic (approximately 165 to 153 million years ago), this formation provides an extraordinary glimpse into a prehistoric world of immense biological diversity.

Reaching a thickness of 2,420 meters (7,940 ft), the formation is primarily composed of andesite, though it also contains sandstone, shale, tuff, and coal. It sits stratigraphically above the Haifanggou Formation and beneath the Tuchengzi and Houcheng Formations. The region is particularly famous for the Daohugou Beds, which have yielded exceptionally preserved fossils, including soft tissues and feathers.

Key Facts

Yanliaomyzon
Yanliaomyzon
  • Age: Middle to Late Jurassic (~165–153 Ma).
  • Location: Hebei, Inner Mongolia, and Liaoning, China.
  • Primary Rock Type: Andesite (volcanic).
  • Significance: High-quality preservation of soft tissues in pterosaurs, dinosaurs, and early mammals.
  • Key Biota: Diverse assembly of pterosaurs, theropods, cynodonts, and ancient flora.

The Fauna of the Tiaojishan Formation

Jeholopterus
Jeholopterus

The animal life preserved in the Tiaojishan Formation is remarkably varied, ranging from aquatic species to gliding mammals and feathered dinosaurs.

Pterosaurs and Flying Reptiles

The formation is renowned for its pterosaurs (flying reptiles), including the Wukongopteridae family. Notable species include Darwinopterus modularis, a key transitional form, and Jeholopterus ninchengensis, a batrachognathine anurognathid known for its preserved soft tissue anatomy.

Darwinopterus modularis
Darwinopterus modularis

Other significant pterosaurs include Sinomacrops bondei, a long-tailed anurognathid, and Kunpengopterus antipollicatus. The diversity of these creatures suggests a complex aerial ecosystem with various feeding strategies, including early filter-feeding.

Sinomacrops
Sinomacrops

Dinosaurs and Early Avialae

The theropods of this region are critical to understanding the evolution of birds. Anchiornis huxleyi and Aurornis xui provide evidence of early feather development. One of the most unusual finds is Yi qi, a scansoriopterygid theropod that possessed membranous wings for gliding, weighing roughly 380 grams (0.84 pounds).

Yi
Yi

Ornithischians (bird-hipped dinosaurs) are also present, represented by genera such as Pulaosaurus and Tianyulong.

Tianyulong
Tianyulong

Early Mammals and Cynodonts

The formation offers a detailed look at cynodonts (mammal-like reptiles) and early mammaliaforms. Juramaia sinensis is a pivotal find for understanding the divergence of marsupials and placentals. The region also reveals specialized lifestyles, such as the subterranean burrowing of Docofossor brachydactylus and the gliding capabilities of Volaticotherium antiquum, which resembled a modern flying squirrel.

Juramaia
Juramaia

Amphibians, Lizards, and Invertebrates

The aquatic and terrestrial environments supported various salamanders, such as Chunerpeton, and several species of lizards. The invertebrate record is equally rich, featuring a variety of flies (such as the tangle-veined Ahirmoneura), water boatmen, and the plectreurid spider Eoplectreurys gertschi.

Chunerpeton
Chunerpeton

Ancient Flora and Vegetation

Kunpengopterus antipollicatus
Kunpengopterus antipollicatus

The plant life of the Tiaojishan Formation indicates a lush environment. The flora is categorized into several major groups:

  • Bennettitales: Including Williamsonia and Zamites.
  • Ginkgoales: Represented by Ginkgo and Solenites.
  • Pinophyta: Various conifers including Pityocladus.
  • Pteridophyta: A wide array of ferns, such as Claytosmunda and Dicksonia.
Group Notable Genera Key Characteristics
Pterosaurs Darwinopterus, Wukongopterus Soft tissue preservation, transitional forms
Theropods Anchiornis, Yi Feathers, membranous gliding wings
Mammaliaforms Juramaia, Volaticotherium Early eutherians, gliding membranes
Flora Ginkgo, Pityocladus Diverse conifers, ferns, and ginkgophytes

Frequently Asked Questions

Wukongopterus
Wukongopterus
Pulaosaurus
Pulaosaurus
Anchiornis
Anchiornis
Aurornis
Aurornis
Caihong
Caihong
Eosinopteryx
Eosinopteryx
Epidexipteryx
Epidexipteryx
Pedopenna
Pedopenna
Scansoriopteryx
Scansoriopteryx
Serikornis
Serikornis
Xiaotingia
Xiaotingia
Agilodocodon
Agilodocodon
Docofossor
Docofossor
Maiopatagium
Maiopatagium
Megaconus
Megaconus
Volaticotherium
Volaticotherium

How old is the Tiaojishan Formation?

The formation dates back to the Middle to Late Jurassic, specifically the Callovian to Kimmeridgian stages, approximately 165 to 153 million years ago.

What makes the fossils from this region so special?

The formation is famous for its Lagerstätte quality, meaning it has exceptional preservation. This includes the preservation of soft tissues, skin impressions, and feathers, which are rarely found in the fossil record.

What was Yi qi?

Yi qi was a small, gliding dinosaur (a scansoriopterygid theropod) that developed membranous wings rather than feathered wings, weighing about 380 grams.

Which early mammal is most significant in this formation?

Juramaia sinensis is highly significant as it provides critical data on the early divergence between placental and marsupial mammals.

What was the primary geological composition of the area?

The primary lithology is andesite, a type of volcanic rock, which likely contributed to the rapid burial and excellent preservation of the organisms found there.

References

  1. Wang, Y.; Ken, S.; Zhang, W.; Zheng, S. (2006). "Biodiversity and palaeoclimate of the Middle Jurassic floras from the Tiaojishan Formation in western Liaoning, China". Progress in Natural Science. 16 (1): 222–230. doi:10.1080/10020070612330087.
  2. Xiaolin Wang; Zhonghe Zhou; Huaiyu He; Fan Jin; Yuanqing Wang; Jiangyong Zhang; Yuan Wang; Xing Xu; Fucheng Zhang (2005). "Stratigraphy and age of the Daohugou Bed in Ningcheng, Inner Mongolia". Chinese Science Bulletin. 50 (20): 2369–2376. Bibcode:2005ChSBu..50.2369W. doi:10.1007/BF03183749. S2CID 198142479.
  3. Liu, Y.; Ji, S.; Yang, Z. (2006). "U-Pb zircon age for the Daohugou Biota at Ningcheng of Inner Mongolia and comments on related issues". Chinese Science Bulletin. 51 (21): 2634–2644. Bibcode:2006ChSBu..51.2634L. doi:10.1007/s11434-006-2165-2. S2CID 96442710.
  4. Zhang, H.; Wang, M.; Liu, X. (2008). "Constraints on the upper boundary age of the Tiaojishan Formation volcanic rocks in West Liaoning-North Hebei by LA-ICP-MS dating". Chinese Science Bulletin. 53 (22): 3574–3584. Bibcode:2008SciBu..53.3574Z. doi:10.1007/s11434-008-0287-4.
  5. Notably Mongolarachne jurassica.