Geoncheonri Formation
| Geoncheonri Formation | |
|---|---|
| Stratigraphic range: Albian ~ | |
 | |
| Type | Geological formation |
| Unit of | Hayang Group |
| Underlies | Yucheon Group Jusasan Formation (volcanics) |
| Overlies | Chaeyaksan Formation (volcanics) |
| Thickness | Up to 800 m (2,600 ft) |
| Lithology | |
| Primary | Mudstone |
| Other | Siltstone |
| Location | |
| Coordinates | 35°54′N 128°36′E / 35.9°N 128.6°E |
| Approximate paleocoordinates | 45°12′N 122°42′E / 45.2°N 122.7°E |
| Region | Daegu, Gyeongsangbuk-do, Gyeongsangnam-do |
| Country |  South Korea |
| Extent | Gyeongsang Basin |
   Geoncheonri Formation (South Korea) | |
The Geoncheonri Formation (Korean: 건천리층; Hanja: 乾川里層; RR: Geoncheonli-cheung) is an Early Cretaceous (Aptian-Albian) geologic formation of the Hayang Group in the Gyeongsang Basin of southeast South Korea.[1] Fossil ornithopod tracks,[2] as well as fossils of Kirgizemys have been reported from the lacustrine siltstones and mudstones of the formation.[3]
Description[edit]
The Geoncheonri Formation (ca. 800 metres (2,600 ft) thick) is the uppermost formation of the Hayang Group, belonging to the Gyeongsang Supergroup. The Gyeongsang Supergroup is widely distributed in the southeastern part of the Korean Peninsula, mainly within the Gyeongsang Basin, which is the largest sedimentary basin of South Korea. It is divided into the Shindong and Hayang Groups, consisting mainly of thick siliciclastic sequences of alluvial, fluvial and lacustrine sediments, and the Yucheon Group, characterized by the dominance of volcanic rocks.[4]
The Hayang Group consists of Chilgok, Silla, Hakbong, Haman, Banyawol, Songnaedong, Chaeyaksan and Geoncheonri Formations in ascending order. The Geoncheonri Formation is conformably underlain by the Chaeyaksan Formation and overlain by the Jusasan Formation, the lowermost of the Yucheon Group.[4]
Since plant fossils were first reported in the Geoncheonri Formation in 1925, a series of paleontological studies has been made with molluscs, spores and pollen, charophytes, and dinosaur footprints. Plant fossils from the Geoncheonri Formation were correlated with the Monobegawa Group and the Gyliak Series (Lower to "Middle" Cretaceous) in Japan. Yang (1978) noted that the co-occurrence of a pelecypod Trigonioides paucisulcatus in the Geonchonri Formation and in the Gyliakian Goshonoura Group (Cenomanian to Turonian) of Japan. However, primitive angiosperm pollen (Retimonocolpites peroreticulatus and Tricolpites sp.) and other palynological features suggest that the age of the Geoncheonri Formation is Aptian to Albian. The charophytes from the Geoncheonri Formation also indicate an Aptian to Albian age.[4]
Fossil content[edit]
The following fossils were reported from the formation:[1]
See also[edit]
- List of dinosaur-bearing rock formations
- Gugyedong Formation
- Haman Formation
- Hasandong Formation
- Jinju Formation
- Sagog Formation
References[edit]
- ^ a b Geoncheonri Formation in the Paleobiology Database
- ^ Weishampel et al., 2004, pp.517-607
- ^ a b Lee et al., 2009
- ^ a b c Gyeongsan City in the Paleobiology Database
- ^ a b Lee et al., 2001
Bibliography[edit]
- Lee, Y.-N.; J. H. Hutchison, and K.-H. Chang. 2009. The first Mesozoic turtle from South Korea. Cretaceous Research 30. 1287–1292. .
- Weishampel, David B.; Peter Dodson, and Halszka (eds.) Osmólska. 2004. The Dinosauria, 2nd edition, 1–880. Berkeley: University of California Press. Accessed 2019-02-21. ISBN 0-520-24209-2
- Lee, Y.-N.; K.-M. Yu, and C. B. Wood. 2001. A review of vertebrate faunas from the Gyeongsang Supergroup (Cretaceous) in South Korea. Palaeogeography, Palaeoclimatology, Palaeoecology 165. 357–373. .