Earth:Duho Formation
| Duho Formation Stratigraphic range: Mid-Miocene ~15–12 Ma | |
|---|---|
| Type | Geological formation |
| Unit of | Yeonil Group |
| Underlies | Alluvium |
| Overlies | Hagjeon Formation |
| Thickness | 150–250 m (490–820 ft)[1] |
| Lithology | |
| Primary | Mudstone |
| Other | Sandstone, Shale |
| Location | |
| Coordinates | [ ⚑ ] : 36°00′N 129°12′E / 36.0°N 129.2°E |
| Region | North Gyeongsang Province |
| Country | South Korea |
| Extent | Pohang Basin (:ko:포항 분지) |
| Type section | |
| Named for | Duho-dong, Pohang |
| Named by | Um et al., 1964[2] |
| File:250px Geological map and stratigraphy of the Pohang Basin | |
The Duho Formation (Korean: 두호층; Hanja: 斗湖層; RR: Duho-cheung) is a Middle Miocene geological formation in Pohang, South Korea. This formation is deposited in a deep marine environment and is roughly dated to around 15 to 12 million years ago based on various analyses. It is the uppermost unit of the Yeonil Group of Pohang Basin and mainly composed of yellow-brown to dark gray mudstones.[3]
Geology

The deposition of the Pohang Basin began some time after 21.89 to 21.68 million years ago, corresponding to the Early Miocene, based on zircon U-Pb dating.[4] This deep-marine basin was probably produced by rapid subsidence around 17 million years ago, following the abrupt ending of the strike-slip deformation and volcanic activity, and experienced tectonic inactivity for 5 to 7 million years until the crustal uplift in southeastern Korea around 10 million years ago which caused the sedimentation to cease.[5] The basin was likely a pelagic zone around 17.6 to 11.5 million years ago based on biostratigraphy analysis.[6]
The intrusive basalt of the Yeonil Group from the southern part of the basin is dated to the lower Middle Miocene around 15.16 to 14.82 million years ago based on K-Ar dating,[7] which implies the evolution of back-arc basin in the seas of southeastern Korea, followed by the tectonic inversion which changed the geodynamic setting and basaltic magma composition.[8] Paleomagnetic dating (analysis of the sediments' ancient magnetic fields) of the Duho Formation yielded the age estimate ranging from 14.7 to 11.6 million years ago.[9] The age estimate of the Yeonil Group based on the same technique is around 17.3 to 11.3 million years ago for the lower and upper part respectively with a reliable pole position of 15 million years ago, while biostratigraphy analysis indicated that the age of the Duho Formation likely ranged from 14 to 12 million years ago.[10] It is probably not younger than 11.95 million years ago based on the radiolarians recovered from the formation.[11]
Paleoecology
Notable fossils from the Duho Formation include a variety of aquatic invertebrates such as ophiuroids, bivalves and mantis shrimps, numerous extant genera of plants, indeterminate remains of toothed whales with some diagnostic to the genus level, and diverse ichthyofauna ranging from small bony fish to large cartilaginous fish like the giant lamniform shark Otodus megalodon which would have been the apex predator of the Miocene seas of Korea. While the fauna consists of species ranging from the shallow coastal waters (neritic and epipelagic zone) to the depths of over 1,000 metres (3,300 ft) (bathypelagic zone), the sediments were probably deposited in a pelagic deep-water setting as evidenced by the paleoecological and bathymetric features of the fossil assemblage.[1]
Fossil content
Crustaceans
| Crustaceans of the Duho Formation[12] | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Region | Member | Material | Notes | Image |
| Leesquilla |
|
Mantis shrimp belonging to the family Squillidae | ||||
| Pohsquilla |
|
Mantis shrimp belonging to the family Squillidae | ||||
| Squilla | S. sp. | Mantis shrimp belonging to the family Squillidae | ||||
Insects
The probable ant fossil named as Aphaenogaster "koreana" in a 2018 conference abstracts is a nomen nudum.[13]
| Insects of the Duho Formation | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Region | Member | Material | Notes | Image |
| Scarites | S. sp.[14] | A single individual known with part and counterpart | First officially described terrestrial animal (ground beetle) from the deep marine Duho Formation | |||
Echinoderms
| Echinoderms of the Duho Formation | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Region | Member | Material | Notes | Image |
| Ophiura | O. pohangensis[15] | Brittle star fossils previously described from the same formation are probably conspecific with O. pohangensis | ||||
| Brissopsis | B. pohangensis[16] | Sea urchin | ||||
Molluscs
| Molluscs of the Duho Formation[17] | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Region | Member | Material | Notes | Image |
| Acharax | A. tokunagai | |||||
| Conchocele | C. bisecta | |||||
| Delectopecten | D. peckhami | |||||
| Lucinoma |
|
|||||
| Macoma | M. incongrua | |||||
| Mizuhopecten | M. kimurai ugoensis | Reported as Patinopecten kimurai ugoensis,[18] but this species was already moved to a different genus Mizuhopecten by Mausda (1963)[19] | ||||
| Nuculana | N. pennula | |||||
| Panomya | P. simotomensis | |||||
| Patinopecten | P. sp. | |||||
| Phos | P. cf. minoensis | |||||
| Portlandia | P. cf. gratiosa | |||||
| Propeamussium | P. tateiwai | |||||
| Squiresica[20] | S. yooni | Vesicomyid bivalve mollusc fossil originally assigned to as Calyptogena cf. elongata | ||||
| Yoldia | Y. sagittaria | |||||
Mammals
| Mammals of the Duho Formation | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Region | Member | Material | Notes | Image |
| Kentriodontidae[21] | Indeterminate | Partial maxilla (DWFM 10001) | Extinct family of toothed whales | |||
| Pomatodelphininae[22] | Indeterminate | Partial rostrum and mandible (KIGAM VP 201101) | River dolphin found in marine deposits and related to Pomatodelphis | |||
| Tursiops[23] | T. sp. | Partial skeleton measuring 70 cm (2.3 ft) long, with a nearly complete skull | Only described in thesis, not officially published. Resembles the modern bottlenose dolphin with the estimated complete length of the specimen around 1.5–2 m (4.9–6.6 ft) | |||
| Kogia[23] | K. sp. | Partial skull measuring 40 cm (1.3 ft) long, associated with the tooth of an adult tiger shark | Only described in thesis, not officially published. Resembles the modern pygmy sperm whale and dwarf sperm whale | |||
Bony fish
| Bony fish of the Duho Formation | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Region | Member | Material | Notes | Image |
| Auxis |
|
First and second fossil record of the genus Auxis in Korea | ||||
| Cyclothone[26] | C. duhoensis | Single complete specimen | The oldest nominal species of Cyclothone | |||
| Pleuronectiformes[27] | Indeterminate | 4 individuals | First record of flatfish from this formation, at least 2 individuals might be distinct from Pleuronichthys[28] | |||
| Pleuronichthys[28] | P. sp. | 2 individuals, both juvenile | Species unknown, due to both specimens being juvenile | |||
| Stenobrachius[29] | S. sangsunii | Single specimen, complete articulated skeleton with counterpart | Lanternfish | |||
| Vinciguerria[30] | V. orientalis | 61 specimens, from articulated to disarticulated skeletons | Distinct from modern species of Vinciguerria in terms of caudal skeleton structure | |||
| Zaprora[31] | Z. koreana | Single specimen in part and counterpart, representing the caudal body region | Second fossil record of the family Zaproridae | |||
Cartilaginous fish
The record of Otodus obliquus from this formation is most likely a misidentification of other otodontid or lamniform shark.[32]
| Cartilaginous fish of the Duho Formation[1] | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Region | Member | Material | Notes | Image |
| Carcharhinus |
|
Teeth | ||||
| Cetorhinus | C. huddlestoni[33] | Gill rakers and oral tooth mold | ||||
| Cosmopolitodus |
|
Teeth | Uncertain whether it is a distinct genus or a junior synonym of Carcharodon | |||
| Dalatias | D. orientalis | Teeth | Two teeth originally assigned to as D. licha (CNUNHM-F279) and D. cf. licha (CNUNHM-F392) respectively are now the paratypes of D. orientalis | |||
| Galeocerdo | G. aduncus | Teeth | ||||
| Hexanchus | H. griseus | Tooth | Miocene record of the modern bluntnose sixgill shark | |||
| Isurus |
|
Teeth | ||||
| Mitsukurina | M. owstoni | Teeth | Among the oldest known record of the modern goblin shark; one tooth (CNUNHM-F268) was originally assigned to as M. cf. lineata | |||
| Otodus | O. megalodon | Teeth | Largest known macropredatory shark that ever lived | |||
| Parotodus | P. benedenii | Tooth | ||||
Plants
| Plants of the Duho Formation | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Region | Member | Material | Notes | Image |
| Acer[34][35] |
|
|||||
| Alangium[36] | A. aequalifolium | |||||
| Albizia[37] | A. miokalkora | |||||
| Castanea[36] | C. tanaii | |||||
| Castanopsis[36] | C. pohangensis | |||||
| Carpinus[38][36] |
|
|||||
| Cinnamomum[36] | C. lanceolatum | |||||
| Cryptocarya[36] | C. ennichiensis | |||||
| Cunninghamia[39] | C. protokonishii | |||||
| Cyclobalanopsis[36] |
|
|||||
| Dipteronia[40] | D. brownii | |||||
| Entada[36] | E. mioformosana | |||||
| Fagus[36] | F. cf. hayate | |||||
| Firmiana[41] | F. sinomiocenica | |||||
| Fraxinus[42][36] |
|
|||||
| Ilex[43] | I. protocornuta | frameless | ||||
| Keteleeria[44] | K. ezoana | |||||
| Hemitrapa[36] | H. yokoyamae | Extinct genus of aquatic plants related to water caltrop | ||||
| Lindera[36] | L. gaudini | |||||
| Liriodendron[42] | L. meisenense | |||||
| Liquidambar[36] | L. miosinica | |||||
| Paliurus[36] | P. koreanus | |||||
| Pasania[36] |
|
|||||
| Parrotia[36] | P. fagifolia | |||||
| Phoebe[36] | P. mioformosana | |||||
| Picea[44] | P. kaneharai | |||||
| Pinus[44] |
|
|||||
| Platanus[36] | P. guillelmae | |||||
| Pseudolarix[45] |
|
|||||
| Pterocarya[36] | P. asymmetrosa | |||||
| Rhododendron[36] | R. tatewakii | |||||
| Tilia[41] | T. asiatica | |||||
| Zelcova[36] | Z. ungeri | |||||
Ichnofossils
| Ichnofossils of the Duho Formation[46] | ||||||
|---|---|---|---|---|---|---|
| Genus | Species | Region | Member | Material | Notes | Image |
| Chondrites |
|
Three deep-water ichnofossils | C. isp. 1 and C. isp. 2 are deposited under oxygen-depleted and oxygenated conditions respectively | |||
| Palaeophycus | P. isp. | |||||
| Planolites | P. isp. | |||||
| Taenidium | T. isp. | |||||
References
- ↑ 1.0 1.1 1.2 Malyshkina, T.P.; Ward, D.J.; Nazarkin, M.V.; Nam, G.-S.; Kwon, S.-H.; Lee, J.-H.; Kim, T.-W.; Kim, D.-K. et al. (2023). "Miocene Elasmobranchii from the Duho Formation, South Korea". Historical Biology 35 (9): 1726–1741. doi:10.1080/08912963.2022.2110870. Bibcode: 2023HBio...35.1726M.
- ↑ Um, S.H.; Lee, D.W.; Bak, B.S. (1964). "Explanatory text of the geological map of Pohang sheet". Geological Survey of Korea: 1–38.
- ↑ Yun, C.-G. (2022). "A Tooth Of The Extinct Lamnid Shark, Cosmopolitodus planus Comb. Nov. (Chondrichthyes: Elasmobranchii) From The Miocene Of Pohang City, South Korea". Acta Palaeontologica Romaniae 18 (1): 9–16. doi:10.35463/j.apr.2022.01.02. https://actapalrom.geo-paleontologica.org/APR_v_18_1/Chan_Cosmopolidus_planus.pdf.
- ↑ Lee, T.H.; Yi, K.; Cheong, C.S.; Jeong, Y.J.; Kim, N.; Kim, M.J. (2014). "SHRIMP U-Pb Zircon Geochronology and Geochemistry of Drill Cores from the Pohang Basin". Journal of Petrological Society of Korea 23 (3): 167–185. doi:10.7854/JPSK.2014.23.3.167.
- ↑ Sohn, Y.K.; Rhee, C.W.; Shon, H. (2001). "Revised stratigraphy and reinterpretation of the Miocene Pohang basinfill, SE Korea: sequence development in response to tectonism and eustasy in a back-arc basin margin". Sedimentary Geology 143 (3–4): 265–285. doi:10.1016/S0037-0738(01)00100-2. Bibcode: 2001SedG..143..265S.
- ↑ Kim, W.H. (1990). "Significance of early to middle Miocene planktonic foraminiferal biostratigraphy of the E-core in the Pohang Basin, Korea". Journal of the Paleontological Society of Korea 6: 144–164. https://www.dbpia.co.kr/journal/articleDetail?nodeId=NODE01385604.
- ↑ Lee, H.K.; Moon, H.-S.; Min, K.D.; Kim, I.-S.; Yun, H.; Itaya, T. (1992). "Paleomagnetism, stratigraphy and geologic structure of the Tertiary Pohang and Changgi basins; K-Ar ages for the volcanic rocks". Journal of the Korean Institute of Mining Geology 25 (3): 337–349. https://koreascience.kr/article/JAKO199223034628291.pdf.
- ↑ Son, M.; Song, C.W.; Kim, M.-C.; Cheon, Y.; Cho, H.; Sohn, Y.K. (2015). "Miocene tectonic evolution of the basins and fault systems, SE Korea: dextral, simple shear during the East Sea (Sea of Japan) opening". Journal of the Geological Society 172 (5): 664–680. doi:10.1144/jgs2014-079. Bibcode: 2015JGSoc.172..664S.
- ↑ Kim, K.H.; Doh, S.J.; Hwang, C.S.; Lim, D.S. (1993). "Paleomagnetic Study of the Yeonil Group in Pohang Basin". Journal of Korean Society of Economic and Environmental Geology 26: 507–518. https://koreascience.kr/article/JAKO199323034627081.pdf.
- ↑ Lee, Y.S.; Ishikawa, N.; Kim, W.K. (1999). "Paleomagnetism of Tertiary rocks on the Korean Peninsula: tectonic implications for the opening of the East Sea (Sea of Japan)". Tectonophysics 304 (1–2): 131–149. doi:10.1016/S0040-1951(98)00270-4. Bibcode: 1999Tectp.304..131L.
- ↑ Bak, Y.; Lee, J.D.; Yun, H. (1996). "Middle Miocene Radiolarians from the Duho Formation in the Pohang Basin, Korea". Journal of the Paleontological Society of Korea 12 (2): 225–261. https://www.dbpia.co.kr/journal/articleDetail?nodeId=NODE01385644.
- ↑ Yun, H. (1985). "Some fossil Squillidae (Stomatopoda) from the Pohang Tertiary Basin, Korea". Journal of the Paleontological Society of Korea 1: 19–31. https://www.dbpia.co.kr/journal/articleDetail?nodeId=NODE01385410.
- ↑ Dong, M.; Kim, S.; Nam, K.S. (2018). "First record of gyne fossil Aphaenogaster (Hymenoptera: Formicidae: Myrmicinae) from Eastern Palaearctic Region". 2018 Spring International Conference of the Korean Society of Applied Entomology. p. 73. https://db.koreascholar.com/article/Detail/346948.
- ↑ Lee, S.B.; Nel, A.; Nam, G.S. (2024). "The first fossil Scarites (Coleoptera: Carabidae) from the Duho Formation (middle Miocene), Korean Peninsula". Palaeoworld 33 (4): 1119–1127. doi:10.1016/j.palwor.2023.05.002. Bibcode: 2024Palae..33.1119L.
- ↑ Ishida, Y.; Thuy, B.; Nam, G.-S.; Martynov, A.; Fujita, T.; Kim, J.-H. (2022). "A New Species of Ophiura (Echinodermata, Ophiuroidea) from Miocene Deep-Sea Deposits in the Pohang Basin, Korea". Paleontological Research 26 (1): 18–30. doi:10.2517/PR200002. Bibcode: 2022PalRe..26.0002I.
- ↑ Lee, B.J.; Kong, D.-Y. (2025). "Brissopsis pohangensis sp. nov., a New Echinoid Species (Spatangoida) from the Middle Miocene Duho Formation, Pohang Basin, Korea". Economic and Environmental Geology 58 (3): 231–245. doi:10.9719/EEG.2025.58.3.231.
- ↑ 17.0 17.1 Kim, S.-H.; Park, J.-Y.; Lee, Y.-N. (2018). "A tooth of Cosmopolitodus hastalis (Elasmobranchii: Lamnidae) from the Duho Formation (Middle Miocene) of Pohang-si, Gyeongsangbuk-do, South Korea". Journal of the Geological Society of Korea 54 (2): 121–131. doi:10.14770/jgsk.2018.54.2.121. ISSN 2288-7377. https://www.dbpia.co.kr/journal/articleDetail?nodeId=NODE07425299.
- ↑ Kim, D.H.; Lee, S.J. (2011). "Fossil scallops from the Hagjeon Formation and the Duho Formation, Pohang Basin". Journal of the Geological Society of Korea 47 (3): 235–244. https://www.dbpia.co.kr/journal/articleDetail?nodeId=NODE01666167.
- ↑ Matsubara, T. (2011). "Miocene shallow marine molluscs from the Hokutan Group in the Tajima area, Hyôgo Prefecture, southwest Japan". Bulletin of the Mizunami Fossil Museum (37): 51–113. https://olivirv.myspecies.info/sites/olivirv.myspecies.info/files/Miocene%20shallow%20marine%20molluscs%20-%20Matsubara%2C%20Takashi.pdf.
- ↑ Kiel, S.; Amano, K.; Goedert, J. (2023). "New taxa, records, and data for vesicomyid bivalves from Cenozoic strata of the North Pacific region". Acta Palaeontologica Polonica 68 (2): 297–320. doi:10.4202/app.01061.2023. https://www.diva-portal.org/smash/get/diva2:1818084/FULLTEXT01.pdf.
- ↑ Lim, J.-D. (2005). "The first dolphin fossil from the Miocene of Korea". Current Science 89 (6): 939–940.
- ↑ Lee, Y.-N.; Ichishima, H.; Choi, D.K. (2012). "First record of a platanistoid cetacean from the middle Miocene of South Korea". Journal of Vertebrate Paleontology 32 (1): 231–234. doi:10.1080/02724634.2012.626005. Bibcode: 2012JVPal..32..231L.
- ↑ 23.0 23.1 Min, J.Y. (2013). A study on the Suborder Odontoceti from the Duho Formation in the Pohang Basin, Korea (MSc thesis) (in 한국어). Gwangju: Chonnam National University. pp. 1–92.
- ↑ Nam, G.S.; Nazarkin, M.V.; Bannikov, A.F. (2021). "First discovery of the genus Auxis (Actinopterygii: Scombridae) in the Neogene of South Korea". Bollettino della Società Paleontologica Italiana 60 (1): 61–67. doi:10.4435/BSPI.2021.05. https://www.paleoitalia.it/bspi-vol-601/.
- ↑ Suh, D.; Kim, S.-H.; Nam, G.-S. (2025). "A new tuna specimen (Genus Auxis) from the Duho Formation (Miocene) of South Korea". Peer Community Journal 5. doi:10.24072/pcjournal.585.
- ↑ Nam, Gi-Soo; Nazarkin, Mikhail V. (2021). "A Neogene bristlemouth of the genus Cyclothone (Stomiiformes: Gonostomatidae) from South Korea". Historical Biology 33 (11): e1625911. doi:10.1080/08912963.2020.1820000. Bibcode: 2021HBio...33.2639N.
- ↑ Ko, J.Y. (2016). "The description of the flat fish (Pleuronectiformes) fossils from the Miocene Duho Formation, Pohang Yeonam-dong in Korea and its implication". Journal of the Korean Earth Science Society 37 (1): 1–10. doi:10.5467/JKESS.2016.37.1.1. https://koreascience.kr/article/JAKO201609562999181.pdf.
- ↑ 28.0 28.1 Ko, J.Y.; Nam, K.S. (2016). "Pleuronichthys sp. Fossils (Pleuronectidae) from the Duho Formation, Pohang Uhyeon-dong in Korea". Journal of the Korean Earth Science Society 37 (3): 133–142. doi:10.5467/JKESS.2016.37.3.133. https://koreascience.kr/article/JAKO201622341961685.pdf.
- ↑ Nam, Gi-Soo; Nazarkin, Mikhail V. (2022). "A new lanternfish (Myctophiformes, Myctophidae) from the Middle Miocene Duho Formation, South Korea". Journal of Vertebrate Paleontology 42 (1): e2121924. doi:10.1080/02724634.2022.2121924. Bibcode: 2022JVPal..42E1924N.
- ↑ Kye-Soo Nam; Ju-Yeong Ko; Mikhail V. Nazarkin (2019). "A new lightfish, †Vinciguerria orientalis, sp. nov. (Teleostei, Stomiiformes, Phosichthyidae), from the middle Miocene of South Korea". Journal of Vertebrate Paleontology 39 (3): e1625911. doi:10.1080/02724634.2019.1625911. Bibcode: 2019JVPal..39E5911N.
- ↑ Nam, Kye-Soo; Nazarkin, Mikhail V. (2018). "Fossil prowfish, Zaprora koreana, sp. nov. (Pisces, Zaproridae), from the Neogene of South Korea". Journal of Vertebrate Paleontology 38 (5): e1514616. doi:10.1080/02724634.2018.1514616. Bibcode: 2018JVPal..38E4616N.
- ↑ Yun, C. (2020). "New example of Cosmopolitodus hastalis (Lamniformes, Lamnidae) from the Miocene South Korea". Zoodiversity 54 (5): 433–438. doi:10.15407/zoo2020.05.433.
- ↑ Malyshinka, T.P.; Nam, G.-S.; Kwon, S.-H. (2021). "Basking Shark Remains (Lamniformes, Cetorhinidae) from the Miocene of South Korea". Journal of Vertebrate Paleontology 41 (5): 247466156. doi:10.1080/02724634.2021.2037625. Bibcode: 2021JVPal..41E7625M. https://www.tandfonline.com/doi/full/10.1080/02724634.2021.2037625.
- ↑ Kim, J.-H.; Nam, K.-S.; Jeon, Y.-S. (2017). "Diversity of Miocene fossil Acer from the Pohang Basin, Korea". Journal of the Geological Society of Korea 53 (3): 387–405. doi:10.14770/jgsk.2017.53.3.387.
- ↑ Kim, J.H. (2008). "A new species of Acer samara from the Miocene Yeonil Group in the Pohang Basin, Korea". Geosciences Journal 12 (4): 331–336. doi:10.1007/s12303-008-0033-6. Bibcode: 2008GescJ..12..331K.
- ↑ 36.00 36.01 36.02 36.03 36.04 36.05 36.06 36.07 36.08 36.09 36.10 36.11 36.12 36.13 36.14 36.15 36.16 36.17 36.18 36.19 36.20 Lim, Jong-Deock; Jeong, Eun-Kyoung; Kim, Kyungsik; Suzuki, Mitsuo; Paik, In Sung; Kim, Haang-Mook (1 March 2010). "Miocene woods of the Janggi Basin in Korea: Implications for paleofloral changes". Geosciences Journal 14 (1): 11–22. doi:10.1007/s12303-010-0002-8.
- ↑ Kim, J.-H. (2010). "Albizia miokalkora Hu and Chaney from the Duho Formation of Yeonil Group (Miocene) in the Pohang Basin, Korea". Journal of Korean Earth Science Society 31 (7): 691–697. doi:10.5467/JKESS.2010.31.7.691.
- ↑ Kim, J.-H.; Nam, K.-S. (2017). "Fossil involucres of Carpinus and their significances from the Duho Formation of Yeonil Group, Korea". Journal of the Geological Society of Korea 53 (6): 759–772. doi:10.14770/jgsk.2017.53.6.759.
- ↑ Yabe, A.; Yamakawa, C. (2017). "Revision of Cunninghamia protokonishii Tanai et Onoe (Pinopsida, Cupressaceae) from East Asia". Paleontological Research 21 (4): 309–328. doi:10.2517/2016PR032. Bibcode: 2017PalRe..21..309Y.
- ↑ Jia, L.-B.; Nam, G.-S.; Su, T.; Yang, X.; Zhou, Z.-K.; Ji, Y.-H. (2023). "Miocene Dipteronia (Sapindaceae) samaras from South Korea and their biogeographical implications". iScience 26 (4): 106515. doi:10.1016/j.isci.2023.106515. ISSN 2589-0042. PMID 37070070. Bibcode: 2023iSci...26j6515J.
- ↑ 41.0 41.1 Jia, L.B.; Nam, G.S.; Su, T.; Stull, G.W.; Li, S.F.; Huang, Y.J.; Zhou, Z.K. (2021). "Fossil fruits of Firmiana and Tilia from the middle Miocene of South Korea and the efficacy of the Bering land bridge for the migration of mesothermal plants". Plant Diversity 43 (6): 480–491. doi:10.1016/j.pld.2020.12.006. PMID 35024517. Bibcode: 2021PlDiv..43..480J.
- ↑ 42.0 42.1 Jung, S.H.; Lee, S.J. (2009). "Fossil winged fruits of Fraxinus (Oleaceae) and Liriodendron (Magnoliaceae) from the Duho Formation, Pohang Basin, Korea". Acta Geologica Sinica - English Edition 83 (5): 845–852. doi:10.1111/j.1755-6724.2009.00113.x. Bibcode: 2009AcGlS..83..845J.
- ↑ Li, X.-Y.; Nam, G.-S.; Li, S.-F.; Averyanova, A.; Yang, Y.; Yoon, M.-B.; Jia, L.-B. (2025). "Fossil evidence and ecological niche modelling reveal trait evolution and biogeography of the Ilex cornuta lineage". Journal of Palaeogeography 14 (3). doi:10.1016/j.jop.2025.02.003.
- ↑ 44.0 44.1 44.2 Kim, J.-H.; Nam, G.S.; Kim, J.-M. (2021). "Some Pinaceae from the Miocene Duho Formation (Yeonil Group) in the Pohang basin, Korea". Journal of the Geological Society of Korea 57 (1): 1–16. doi:10.14770/jgsk.2021.57.1.1. https://www.dbpia.co.kr/journal/articleDetail?nodeId=NODE10532535.
- ↑ Kim, J.H. (2009). "Occurrence of Pseudolarix (Pinaceae) from the Miocene Duho Formation of the Yeonil Group, Korea". Journal of Korean Earth Science Society 30 (5): 598–604. doi:10.5467/JKESS.2009.30.5.598.
- ↑ Kim, J.; Paik, I.S (2013). "Chondrites from the Duho Formation (Miocene) in the Yeonil Group, Pohang Basin, Korea: Occurrences and paleoenvironmental implications". Journal of the Geological Society of Korea 49 (3): 407–416. https://www.dbpia.co.kr/journal/articleDetail?nodeId=NODE02195466.

