The Jehol biota  includes all the living organisms – the ecosystem – of northeastern China between 133 to 120 million years ago (mya). This is the Lower Cretaceous ecosystem which left fossils in the Yixian Formation, some 125–121 mya, and the Jiufotang Formation. It is also believed to have left fossils in the Sinuiju series of North Korea.
The ecosystem in the Lower Cretaceous was dominated by wetlands and numerous lakes (not rivers, deltas, or marine habitats). Rainfall was seasonal, alternating between semi-arid, and mesic conditions. The climate was temperate. The Jehol ecosystem was interrupted at times by ash eruptions from volcanoes to the west. The word Jehol was the name given during the Japanese occupation of North-East China, 1933–1946.
Diversity[change | change source]
The Jehol biota includes many types of fossils and large numbers of individuals of each species that have been recovered. The biota includes many species that were previously known only from the Upper Jurassic or earlier. These include the dinosaur Sinosauropteryx, and the pterosaur Dendrorhynchoides. There was even a primitive protomammal – a tritylodont therapsid – from Lower Cretaceous Japan. Tritylodonts were previously thought to have gone extinct in the Middle Jurassic. The biota also has the earliest and most basal (primitive) known members of groups which spread all around the world by the Upper Cretaceous, including neoceratopsians, therizinosaurs, tyrannosaurs, and oviraptors.
The Jehol biota has produced fossils of plant mega- and microfossils, including the earliest angiosperms, charophytes and dinocysts, snails (gastropods), clams (bivalves), superabundant aquatic arthropods called conchostracans, ostracods, shrimps, insects, spiders, fish, frogs and salamanders, turtles, choristoderes, lizards (squamata), pterosaurs, and dinosaurs including dinobirds, the largest mammals known from the Mesozoic, and a great diversity of birds including the earliest advanced birds, and the smallest and largest birds known from the Mesozoic.
The forests around the lakes were dominated by conifers including members of the podocarp pine, araucaria, and cypress families. There were also ginkgos, bennettitaleans, ephedra, horsetails, ferns, and mosses. The leaves and needles of the trees show adaptations to a dry season, but some of the ferns and mosses are types that grow in very wet habitats. It is possible that the latter avoided dry conditions by growing very close to bodies of water. Archaefructus has been described as the earliest known flowering plant (Angiosperm), and it is reconstructed as a water plant.
Fossil preservation[change | change source]
The fossils have been found in several sites of exceptional preservation. The two most famous are the Yixian and Jiufotang Formations. The Yixian and Jiufotang Formations are Lagerstatten, meaning that they have exceptionally good conditions for fossil preservation. The fossils are numerous, but also very well preserved. They often have articulated skeletons (bones connected), soft tissues, colour patterns, stomach contents, and twigs with leaves and flowers still attached.
Palaeontologists deduced two things from this. The first is that the land animals and plants were washed into the lakes very gently, or were already in the lakes when they died. They do not show the damage seen in fossils formed by large floods. Second, volcanic ash is commonly interbedded with lake sediments, and ashfalls seem to have quickly buried the fossilized organisms, created anoxic conditions around them, and prevented scavenging.
Yixian Formation[change | change source]
A geological formation in Liaoning, N.E. China. Outstanding preservation in deposits of siliclastic (SiO2) sediment alternating with basalt. First recognised by the Japanese when they occupied Manchuria ('Jehol'). Dates: 125–121 million years ago. Contains the famous Confuciusornis beds.
Jiufotang Formation[change | change source]
The exact age of the Jiufotang has been debated for years, with estimates ranging from the Upper Jurassic to the Lower Cretaceous. Argon radiometry confirmed a Lower Cretaceous age for the site, 120.3 +/-0.7 million years ago. Fossils of Microraptor and Jeholornis are from the Jiufotang.
Huajiying Formation[change | change source]
Lower Cretaceous, but exact dates uncertain. This is probably the earliest of the Jehol biota lagerstätte sites. Contains sedimentary members interspersed with volcanic ash. Contains birds, dinosaurs and fish.
References[change | change source]
- Chinese: 热河群; pinyin: rè hé qún
- Swisher, Carl C. et al. 1999. "Cretaceous age for the feathered dinosaurs of Liaoning, China". Nature 400:58–61
- Li, Quanguo & Gao, Ke-qin 2007. Lower Cretaceous vertebrate fauna from the Sinuiju basin, North Korea as evidence of geographic extension of the Jehol Biota into the Korean Peninsula. Journal of Vertebrate Paleontology 27, supplement to number (3). pp106A
- Semi-arid: receives low annual precipitation. Mesic: a type of habitat with a moderate or well-balanced supply of moisture, i.e. a mesic forest, a temperate hardwood forest, or dry-mesic prairie.
- Zhonghe, Zhou; Barrett, Paul M. & Hilton, Jason. 2003. An exceptionally preserved Lower Cretaceous ecosystem Nature 421:807–811.
- Jin F. et al. 2008. On the horizon of Protopteryx and the early vertebrate fossil assemblages of the Jehol Biota. Chinese Science Bulletin, 53(18): 2820-2827.
- He H.Y. et al. 2004. Timing of the Jiufotang Formation (Jehol Group) in Liaoning, northeastern China, and its implications. Geophysical Research Letters 31(13): 1709.