2026 年 30 巻 p. 17-27
For toothed whales, the Early Miocene was a time of transition between archaic and modern clades. In Japan, there are horizons that include whale fossils from the Early to early Middle Miocene, such as the Ichishi Group in Mie, the Mizunami and Iwamura groups in Gifu, the Morozaki Group in Aichi, and some formations in Akita, Iwate and Hokkaido. The Bihoku Group in Hiroshima has abundant baleen whale (Mysticeti) fossils, but only one possible toothed whale (Odontoceti) fossil exists. Here, we report the first unambiguous fossil record of Odontoceti from the Korematsu Formation of the Bihoku Group (latest Early to earliest Middle Miocene), a pair of fused middle parts of mandibles with two teeth. Although this specimen is fragmentary, it is evident that odontocetes lived in this region during the time of deposition of the Korematsu Formation. However, questions remain as to why there are so few odontocete specimens relative to mysticetes.

The suborders Odontoceti (toothed whales) and Mysticeti (baleen whales) comprise the Neoceti or crown Cetacea (Fordyce and de Muizon, 2001). Early odontocetes from the Oligocene have heterodont teeth and poorly telescoped skulls (Fordyce, 2002; Sanders and Geisler, 2015). Like the Platanistidae and Ziphiidae, early members of modern groups appeared in the Early Miocene (Marx et al., 2016). Thus, the Early Miocene was a time of transition from archaic odontocetes to modern ones (Bianucci and Landini, 2007).
Many Early Miocene odontocetes have been reported since the 2010s from Italy (Bisconti et al., 2020), Malta (Bianucci et al., 2011), Argentina (Viglino et al., 2018, 2019, 2020, 2022; Gaetán et al., 2019, 2025), Peru (Lambert et al., 2015, 2017; Bianucci et al., 2018, 2020), Washington, Oregon, Maryland and Virginia in the USA (Boersma et al., 2017; Lambert et al., 2018; Nelson and Uhen, 2018; Peredo et al., 2018; Godfrey and Lambert, 2023), New Zealand (Aguirre-Fernández and Fordyce, 2014; Tanaka and Fordyce, 2015, 2016; Tanaka et al., 2023) and Japan (see next).
In Japan, there are horizons that preserve Early to early Middle Miocene odontocete fossils, such as the Ichishi Group in Mie, the Mizunami and Iwamura groups in Gifu, the Morozaki Group in Aichi, and some formations in Akita, Iwate and Hokkaido (Table 1) (Oishi and Hasegawa, 1995; Ichishima, 2005). Several nominal species have been established based on specimens derived from these areas (Kimura and Barnes, 2016; Guo and Kohno, 2021, 2023; Kimura and Hasegawa, 2022; Tanaka and Nakagawa, 2024).
| Horizon | Specimen | Identification | Parts | Age | Localities | Reference |
|---|---|---|---|---|---|---|
| Korematsu Fm., Bihoku Gr. | HMN-F30103 | Odontoceti indet. | mandibles | 16.1 to 15.6 Ma, late Early to early Middle Miocene | Miyoshi City, Hiroshima | This study |
| Korematsu Fm., Bihoku Gr. | HMN-F30102 | cf. Odontoceti | right humerus | 16.1 to 15.6 Ma, late Erly to early Middle Miocene | Shobara City, Hiroshima | Tanaka et al., 2020 |
| Hiramatsu Fm., Ichishi Gr. | GMNH-PV-2570, Holotype | Ninjadelphis ujiharai | partial skeleton including skull, periotics, tympanic bullae, mandibles and forelimb elements | 17 Ma, late Early Miocene | Iga City, Mie | Kimura and Barnes, 2016 |
| Haze Fm., Ichishi Gr. | MPM-Fo1058, Holotype | Miodelphinus miensis | Skull, right and left periotics and tym- panic bullae, right incus and malleus, four isolated teeth, three possible hyoid bones and two ribs | 18.7 to 18.5 Ma, Early Miocene | Tsu City, Mie | Tanaka and Nakagawa, 2024 |
| Oi Fm., Ichishi Gr. | MFM 53701 | Odontoceti | forelimb | Early Miocene | Tsu City, Mie | Kimura and Kaede, 2016 |
| Oi Fm., Ichishi Gr. | private specimens | cf. Stenella kabatensis (now Eodelphinus kabatensis) | three teeth | Early Miocene | Tsu City, Mie | Matsuhashi and Ooyagi, 2013 |
| Oi Fm., Ichishi Gr. | private specimens | Delphinidae indet. | periotic and two teeth | Early Miocene | Tsu City, Mie | Matsuhashi and Ooyagi, 2013 |
| Oi Fm., Ichishi Gr. | private specimen | Delphinoidea indet. | tooth | Early Miocene | Tsu City, Mie | Matsuhashi and Ooyagi, 2013 |
| Oi Fm., Ichishi Gr. | private specimens | cf. Scaldicetus sp. | two teeth | Early Miocene | Tsu City, Mie | Matsuhashi and Ooyagi, 2013 |
| Oi Fm., Ichishi Gr. | private specimens | Odontoceti indet. | two teeth | Early Miocene | Tsu City, Mie | Matsuhashi and Ooyagi, 2013 |
| Oi Fm., Ichishi Gr. | WMNH-Ge-1121340002 | Odontoceti indet. | mandibles | 17.2 to 16.3 Ma, Early Miocene | Tsu City, Mie | Tanaka et al., 2021 |
| Yamanouchi Fm., Mizunami Gr. | MFM | Aulophyseter sp. | skull, mandible, teeth and atlas | Early Miocene | Mizunami City, Gifu | Okazaki, 1992 |
| Akeyo Fm., Mizunami Gr. | MFM | Platanistoidea? | right scapula, humerus, ulna, radius and carpals | Early Miocene | Mizunami City, Gifu | Kamei and Okazaki, 1974; Ichishima, 2005 |
| Akeyo Fm., Mizunami Gr. | MFM 18002, Holotype | “Eurhinodelphis” minoensis re-identified as an odontoceti | mandibles, vertebrae, ribs, teeth | Early Miocene | Mizunami City, Gifu | Okazaki, 1976; Ichishima, 2005 |
| Akeyo Fm., Mizunami Gr. | MFM 18003 | “Eurhinodelphis” minoensis re-identified as an odontoceti | mandibles and teeth | Early Miocene | Mizunami City, Gifu | Okazaki, 1976; Ichishima, 2005 |
| Akeyo Fm., Mizunami Gr. | MFM | Eurhinodelphis sp. A. re-identified as a kentriodontid | skull and ear bones | Early Miocene | Mizunami City, Gifu | Okazaki, 1976; Ichishima, 2005 |
| Toyama Fm., Iwamura Gr. | MFM 18190 | Squalodelphinidae indet. | left periotic, right tympanic bulla and right malleus | 17 to 16 Ma, Early Miocene | Mizunami City, Gifu | Kimura, 2019 |
| Morozaki Gr. | TMNH 10785, Holotype | Miophyseter chitaensis | skull, periotic, tympanic bulla and skeleton | Early Miocene | Minamichita, Aichi | Chita−kujira Excavation Research Group, 1993; Kimura and Hasegawa, 2022, 2023 |
| Bessho Fm. | SFM-00001, Holotype | Brygmophyseter shigensis | skeleton | early Middle Miocene | Matsumoto, Nagano | Hirota and Barnes, 1995; Kimura et al., 2006 |
| Bessho Fm. | MCM-56221 | Ziphiidae indet. | skull | early Middle Miocene | Matsumoto, Nagano | Hasegawa and Kimura, 2003 |
| Bessho Fm. | KIM-1, Holotype | Sinanodelphis izumidaensis | skull, vertebrae and forelimb | early Middle Miocene | Aoki, Nagano | Makiyama, 1936; Kohno et al., 2007 |
| Bessho Fm. | MCM-56211 | Delphinoidea indet. | skull | early Middle Miocene | Matsumoto, Nagano | Kohno et al., 2007 |
| Kadonosawa Fm. | IGPS 59740 | Scaldicetus indet. | tooth | late Early to early Middle Miocene | Ninohe City, Iwate | Matsumoto, 1926; Kohno and Ray, 2008 |
| Sugota Fm. | UTHFM 00034, Holotype | Platysvercus ugonis | skull | 16.7 to 16.29 Ma, Early Miocene | Ugo Town, Akita | Guo and Kohno, 2023 |
| Kadonosawa Fm. | NMHF 999, Holotype | Kentriodon sugawarai | skull, one tooth, the right tympanoperiotic, malleus, mandibles and atlas | late Early to early Middle Miocene | Ninohe City, Iwate | Guo and Kohno, 2021 |
| Takinoue Fm. | HMG 387, Holotype | Kentriodon hobetsu | skull | early Middle Miocene | Mukawa, Hokkaido | Ichishima, 1995 |
Abundant fossils of baleen whales are known from the Bihoku Group in Hiroshima (Kimura et al., 2007, 2010, 2011; Ohzawa et al., 2007; Otsuka and Ota, 2008; Tsai, 2017). In contrast, only one possible toothed whale fossil identified as cf. Odontoceti has been reported from this unit (Tanaka et al., 2020). The specimen is a 9 cm long right humerus, which shows an unusual shape, including a flat shaft and a proximally well projected common tubercle. It is similar to the humerus of odontocetes in that it has a deep fossa for the infraspinatus. However, the attribution to Odontoceti remains tentative. Here, we report the first unambiguous record of Odontoceti from the Bihoku Group (latest Early to earliest Middle Miocene) in Miyoshi, Hiroshima, Japan.
Institutional abbreviations.—GMNH, Gunma Museum of Natural History, Gunma, Japan; HMG, Hobetsu Museum, Mukawa, Hokkaido, Japan; HMN, Hiwa Museum for Natural History, Hiroshima, Japan; HUM, Hiroshima University Museum, Hiroshima, Japan; IGPS, Institute of Geology and Paleontology, Tohoku University, Sendai, Miyagi, Japan; KIM, Kohsenji Izumida Museum, Ueda, Nagano, Japan; MCM, Matsumoto City Museum, Matsumoto, Nagano, Japan; MFM, Mizunami Fossil Museum, Mizunami, Gifu, Japan; MPM, Mie Prefectural Museum, Tsu, Mie, Japan; NMHF, Ninohe Museum of History and Folklore, Ninohe, Iwate, Japan; MSFM, Matsumoto City Shiga Fossil Museum, Matsumoto, Nagano, Japan; SFM, Shobara Kaseki Shudankai Fossil Museum, Shobara, Hiroshima, Japan; TMNH, Toyohashi Museum of Natural History, Toyohashi, Aichi, Japan; UTHFM, Ugo Town History and Folklore Museum, Ogachi, Akita, Japan; WMNH, Wakayama Prefectural Museum of Natural History, Kainan, Wakayama, Japan.
The new specimen (HMN-F30103) was discovered in August 1979 by Noriko Ochi from the Bihoku Group in Nishisakeyamachi, Miyoshi, Hiroshima, Japan. In this area, the Bihoku Group is divided into the lower Korematsu Formation, which comprises sandstones, and the upper Itabashi Formation, which comprises shales (Seto and Yamauchi, 2009). Based on the matrix of the specimen, HMN-F30103 was derived from the Korematsu Formation. The paleoenvironment of the Korematsu Formation was a bay characterized by a mangrove community (Seto and Yamauchi, 2009). The age of the Korematsu Formation in this area was estimated as 16.1 to 15.6 Ma (latest Burdigalian to earliest Langhian; latest Early to earliest Middle Miocene) based on microfossils (Yamamoto, 1999). Preparation of the fossil was completed by Toshiyuki Kimura and one of the authors (YT) using pneumatic scribes and immersion of a block in dilute 4% acetic acid.
Order Cetacea Brisson, 1762
Unranked clade Neoceti Fordyce & de Muizon, 2001
Suborder Odontoceti Flower, 1867
Odontoceti indet.

Referred specimen.—HMN-F30103, the middle part of a fused and narrow mandibular symphysis with two single-rooted teeth in life position.
Locality.—Nishisakeyamachi, Miyoshi, Hiroshima, Japan: Latitude 34°47′08″N, longitude 132°50′47″E (Figure 1).

Horizon and age.—Korematsu Formation, Bihoku Group. Latest Burdigalian to earliest Langhian; latest Early to earliest Middle Miocene (16.1 to 15.6 Ma: Yamamoto, 1999).
Terminology for mandibular osteology follows Mead and Fordyce (2009).
Ontogeny.—HMN-F30103 shows individualized and ossified alveoli. This indicates that the animal was probably not a juvenile. For example, juveniles of Pontoporia blainvillei have an open alveolar groove instead of individualized and ossified alveoli (Gutstein et al., 2009).
Mandible.—HMN-F30103 is a pair of fused mandibles with two teeth missing their crowns. No indications could be found for a mesorostral groove or for sutures of the premaxilla, maxilla, and vomer, so this fragment can be confidently identified as a part of a mandible. The mandibular fragment is 37.7 mm long, 25.7 mm wide and 17.1 mm in height excluding the teeth. The right and left mandibles are completely fused. The surface of the mandibles is smooth. The mandibles exhibit dorsally swollen lateral parts and the mandibular symphysis as a weak groove on the dorsal surface (Figure 2A).
The minimum distances between right and left alveoli is 14.9 and 17.4 mm for the two preserved pairs of alveoli. This difference may be explained by the anterior narrowing of the mandible, as seen in many odontocetes, the anterior side being this the narrowest. Thus, the two preserved teeth are probably from the right side (Figure 2).
Two open alveoli are preserved on the presumed left side, which are circular openings (the anterior alveolus is 6.6 mm long and 6.1 mm wide, and the posterior alveolus is 6.3 mm long and 5.8 mm wide). Around the alveoli, the lateral borders of the mandibles are nearly rectilinear in dorsal and lateral views (Figure 2A, C and F). The alveoli are shallow (about 5 mm deep) with smooth walls.
On the ventrolateral surfaces of the right and left mandibles (Figure 2B, C and F), there are a couple of long, shallow grooves running anteroposteriorly. Between the grooves, there is a ventrally swollen ventromedial part. In anteroposterior view (Figure 2D and E), the mandible is heart-shaped. The cross-sections show a foramen filled by the matrix at the center of the bone, which is surrounded by dense bone.
Teeth.—Two single-rooted teeth are preserved in life position. The crowns are broken away. In cross section, the roots are transversely flattened and elliptical in cross section (anterior tooth: 5.4 mm long and 4.4 mm wide; posterior tooth: 4.8 mm long and 3.9 mm wide).
HMN-F30103 is an odontocete because it has single rooted teeth, which is not a feature in true or toothless baleen whales (Chaeomysticeti). Early mysticetes had teeth and originated before the Early Miocene (Marx et al., 2024). Some have both double- and single-rooted teeth (e.g. Mammalodon: Fitzgerald, 2010; Coronodon: Boessenecker et al., 2023), whereas others have only single rooted teeth (e.g. Aetiocetus: Emlong, 1966). However, toothed baleen whales differ from HMN-F30103 in having anteroposteriorly long posterior teeth with wide robust roots and in lacking mandibles with parallel sided lateral surfaces and long mandibular symphysis. Crocodiles also have a similar mandibular morphology but have cranial ornamentation (Clarac et al., 2015). Thus, HMN-F30103 is different from crocodiles with smooth surface of the bone and walls of the alveoli.
More precise identification of HMN-F30103 is challenging, as several different odontocete lineages share narrow mandibles with an anteroposteriorly long mandibular symphysis (e.g. Allodelphinidae, Squalodelphinidae, Platanistidae, Eoplatanistidae and Kentriodontidae). See Table 2 for a detailed comparison of these families. Although HMN-F30103 preserves only partial mandibles, it possesses shallow anteroposteriorly long grooves on the ventrolateral side, circular alveoli, cross sections being transversely wider than high, and more or less the same length of the alveoli and interalveolar spaces. Among the odontocetes used for comparison, only WMNH-Ge-11121340002, Odontoceti indet. shows the same combination of these four features. However, these four features are not diagnostic, even at the family level (Table 2). For example, among squalodelphinids, Squalodelphis fabianii has shallow longitudinal grooves on the ventrolateral surface of the mandible, whereas Notocetus vanbenedeni lacks such grooves.
| Family | Scientific name or specimen number | Age | long groove on ventrolateral side | alveolar shape | mandibular symphysis width and height, at preserved most posterior part or anterior to diverging point of the mandibles | length of alveoli vs interalveolar spaces, at preserved most posterior part or anterior to diverging point of the mandibles | Used references for comparison |
|---|---|---|---|---|---|---|---|
| Odontoceti indet. | HMN-F30103, partly preserved mandible | late Early to early Middle Miocene | shallow | circular | wider | more or less the same | This study |
| Odontoceti indet. | WMNH-Ge-1121340002, partly preserved mandible | late Early Miocene | shallow | circular | wider | more or less the same | Tanaka et al., 2021 |
| Odontoceti indet. | “Eurhinodelphis” minoensis, holotype | Early Miocene | shallow | circular | wider | more or less the same at the level of the posterior end of the mandibular symphysis, and alveoli are longer at the anterior part of the mandibles | Okazaki, 1976 |
| Allodelphinidae | Ninjadelphis ujiharai, holotype GMNH-PV-2570 | late Early Miocene | deep | circular | more or less the same | shorter interalveolar space | Kimura and Barnes, 2016 |
| Squalodelphinidae | Squalodelphis fabianii, holotype MGP 26134 | Early Miocene | shallow | circular | wider | longer interalveolar space | Pilleri, 1985 |
| Squalodelphinidae | Notocetus vanbenedeni, MLP 5-10 | Early Miocene | absent | circular | wider | more or less the same | Lydekker, 1894; Viglino et al., 2022 |
| Platanistidae | Araeodelphis natator, holotype USNM 10478 | Early to early Middle Miocene | shallow | circular | wider | shorter interalveolar space | Kellogg, 1957 |
| Platanistidae | Pomatodelphis inaequalis, USNM 6683, partly preserved mandible | Middle to Late Miocene | shallow | anteroposteriorly longer | wider | shorter interalveolar space | Kellogg, 1959 |
| Allodelphinidae | Zarhinocetus errabundus, LACM 149588 | Middle Miocene | deep | anteroposteriorly longer | wider | shorter interalveolar space | Kellogg, 1931, Kimura and Barnes, 2016 |
| Eoplatanistidae | Eoplatanista italica holotype MGP 26150, 26151 | Early Miocene | shallow | anteroposteriorly longer | ? | shorter interalveolar space | Pilleri, 1985 |
| Eurhinodelphinidae | Xiphiacetus bossi, holotype USNM 8842 | Early to Middle Miocene | deep | circular | wider | shorter interalveolar space | Kellogg, 1925 |
| Eurhinodelphinidae | Schizodelphis sulcatus, MGP 26154 | Early to Middle Miocene | shallow | anteroposteriorly longer | ? | longer interalveolar space | Pilleri, 1985 |
| Kentriodontidae | Belonodelphis peruanus, holotype MNHN PPI 231 | Late Miocene | shallow | anteroposteriorly longer | wider | shorter interalveolar space | Muizon, 1988 |
There are several nominal Early to early Middle Miocene odontocete species from Japan (Ninjadelphis ujiharai, Miophyseter chitaensis, Brygmophyseter shigensis, Sinanodelphis izumidaensis, Platysvercus ugonis, Kentriodon sugawarai, Kentriodon hobetsu, Miodelphinus miensis and “Eurhinodelphis” minoensis. See citations in Table 1). Lambert (2004) identified the holotype of “E.” minoensis as Odontoceti incertae sedis because the specimen does not preserve diagnostic characters at the generic level. Among the odontocetes from the Early to early Middle Miocene of Japan, only N. ujiharai, B. shigensis, S. izumidaensis, K. sugawarai, and “E.” minoensis have mandibular material preserved. K. sugawarai preserves a posterior part of the mandible, and S. izumidaensis preserves an anterior part of the mandible visible only in lateral view, because the specimen is still embedded in matrix. Ninjadelphis ujiharai differs from HMN-F30103 in having deeper anteroposteriorly elongated grooves on the ventrolateral surface of the mandible and a deep groove on the median line of the dorsal surface of the mandibular symphysis. Brygmophyseter shigensis differs from HMN-F30103 in having large teeth with interalveolar spaces shorter than the anteroposterior length of teeth and a deep groove on the median line of the dorsal surface of the mandibular symphysis. “Eurhinodelphis” minoensis differs from HMN-F30103 in having deeper anteroposteriorly elongated grooves on the ventrolateral surface of the mandible, but it is similar in having a shallow groove on the median line of the dorsal surface of the mandibular symphysis. WMNH-Ge-11121340002, a Y-shaped portion of the posterior end of a long mandibular symphysis preserving several alveoli from the Oi Formation (Ichishi Group), was referred to Odontoceti indet. (Tanaka et al., 2021). WMNH-Ge-11121340002 differs from HMN-F30103 in having a deeper groove on the median line of the dorsal surface of the mandibular symphysis, but it is similar in having shallow anteroposteriorly elongated grooves on the ventrolateral surface of the mandible.
The taxonomy of several reported specimens is uncertain (Table 1). In Japan, the Early to early Middle Miocene odontocetes are classified into the Physeteridae, Squalodelphinidae, Allodelphinidae, Ziphiidae and Kentriodontidae. The two families Squalodelphinidae and Allodelphinidae have only recently been recognized from Japanese strata in the past decade (Kimura and Barnes, 2016; Kimura et al., 2019). Those recent records suggest that various species of squalodelphinids and allodelphinids diversified and existed in the northeastern Pacific by the Early Miocene (Kimura and Barnes, 2016; Tanaka and Nakagawa, 2024).
As mentioned above, abundant baleen whale fossils have been reported from the Bihoku Group. Over 10 baleen whale specimens have been reported from the Bihoku Group in the cities of Miyoshi and Shobara, including fossils referred to Parietobalaena yamaokai, Pelocetus sp., Hibacetus hirosei, Aglaocetus sp., and Diorocetus shobarensis (Table 3) (Imamura, 1953; Yamaoka, 1995; Ohzawa et al., 2001, 2007, 2013; Kimita Village and Kimita Village Education Board, 2003; Ohzawa and Yamaoka, 2003; Furukawa et al., 2004; Kimura et al., 2007, 2010, 2011; Otsuka and Ota, 2008; Otsuka, 2008; Tsai, 2017; Kiyoshi et al., 2020). HMN-F30103 is the first unambiguous odontocete from the Bihoku Group. In short, the cetacean fossil record of the Bihoku Group comprises many mysticetes and only a few odontocetes. However, this trend is not widely seen in the world. The marine vertebrate fossil assemblage of the Lower Miocene Chilcatay Formation in Peru is dominated by odontocetes (Di Celma et al., 2018). Marx et al. (2019) reported several fossil localities of Oligocene–Miocene boundary preserving odontocetes but lacking mysticetes altogether.
| Horizon | Specimen | Identification | Age | Locality | Reference |
|---|---|---|---|---|---|
| Korematsu Fm. | HMN-F00003 | Pelocetus sp. | Early to Middle Miocene | Shobara City | Kimura et al., 2007 |
| Itabashi Fm. | HMN-F00004 | Parietobalaena cf. yamaokai | Middle Miocene | Shobara City | Kimura et al., 2010: Ohzawa et al., 2007 |
| Korematsu Fm. | HMN-F00005–9 (IDs for the same individual) | Diorocetus shobarensis, holotype | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00010, 12–19 (IDs for the same individual) | Diorocetus shobarensis, holotype | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00021 | Parietobalaena yamaokai | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00022–24 (IDs for the same individual) | Parietobalaena yamaokai, holotype | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00025 | Parietobalaena yamaokai | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00026 | Parietobalaena yamaokai | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00027 | Parietobalaena yamaokai | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00035, 36, 38, 40, 41 | Parietobalaena yamaokai | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00042–44, 54 | Parietobalaena yamaokai, paratype | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008; Ohzawa et al., 2013 |
| Korematsu Fm. | HMN-F00045–47, 49, 51, 53 | Parietobalaena yamaokai | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00060 | Parietobalaena yamaokai | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00061 | Parietobalaena yamaokai | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00062 | Parietobalaena yamaokai | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00063 | Diorocetus shobarensis, paratype | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00064–80 (seems a series belongs to an individual) | Parietobalaena yamaokai | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00081 | Parietobalaena yamaokai | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00082 | Pelocetus sp. | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00083 | Pelocetus sp. | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00084 | Hibacetus hirosei, holotype | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00085 | Parietobalaena yamaokai | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00086, 87 | Parietobalaena yamaokai | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Itabashi Fm. | HMN-F00088–92, 94–97 | cetacea | Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00098 | Parietobalaena yamaokai | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00106–115 | Pelocetus sp. | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00117 | Parietobalaena yamaokai | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00118 | Aglaocetus sp. | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00119 | Aglaocetus sp. | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00120 | Aglaocetus sp. | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00121 | Aglaocetus sp. | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00122 | Aglaocetus sp. | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00123 | Aglaocetus sp. | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00124 | Aglaocetus sp. | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00125 | Aglaocetus sp. | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008 |
| Korematsu Fm. | HMN-F00127, 128 | Parietobalaena yamaokai | Early to Middle Miocene | Shobara City | Otsuka and Ota, 2008; Tsai, 2017 |
| Korematsu Fm. | HMN-F00640 | Parietobalaena yamaokai | Early to Middle Miocene | Shobara City | Kimura et al., 2011 |
| Itabashi Fm. | HMN-F11569 | cf.Diorocetus shobarensis | Middle Miocene | Shobara City | Kiyoshi et al., 2020 |
| Itabashi Fm. | HMN-F20256–72 (IDs for the same individual) | Cetacea indet. | Middle Miocene | Shobara City | Furukawa et al., 2004 |
| unknown | SFM-00100 | Cetotheriidae indet. | Middle Miocene | Shobara City | Ohzawa and Yamaoka, 2003 |
| Itabashi Fm. | SFM-00106 | cf. Cetotheriidae | Middle Miocene | Shobara City | Ohzawa and Yamaoka, 2003 |
| Itabashi Fm. | SFM-00107 | cf. Cetotheriidae | Middle Miocene | Shobara City | Ohzawa et al., 2001 |
| Korematsu Fm. | SFM-00111 | Cetacea indet. | Early to Middle Miocene | Shobara City | Yamaoka et al.,1995 |
| Korematsu Fm. | HUM-F-00253 | Cetacea indet. | Early to Middle Miocene | Shobara City | Imamura, 1953 |
| Korematsu Fm. | KFM-0003–23 (IDs for the same individual) | Mysticeti indet. | latest Early Miocene | Miyoshi City | Kimita Village and Kimita Village Education Board, 2003; Otsuka, 2008 |
Here we consider sampling, research, and taphonomic biases to try to explain why only one unambiguous odontocete fossil is known from the Bihoku Group when many mysticete fossils have been reported. In northern Japan, 33 odontocete fossils and 23 mysticete fossils have been reported from Hokkaido, and nine odontocete fossils and 72 mysticete fossils have been reported from Tohoku (Ichishima, 2024). Ichishima (2024) concluded that the number of reports from each of those regions is affected by research bias, noting the current data are insufficient to explain whether paleoenvironmental factors also contributed to the apparent differences. Three of the authors (TK, TY and HO) contributed to cataloguing the fossil collections from Shobara and Miyoshi at the Hiwa Museum for Natural History. Additionally, the authors have collected and prepared the majority of the cetacean fossils from these regions by ourselves, and with the exception of one isolated single rooted conical tooth, we have never seen another odontocete fossil. Having observed all known cetacean fossils from the Bihoku Group, we therefore conclude that research bias is not the cause of the low number of odontocetes relative to mysticetes. A sampling bias owing to body size is unlikely, because specimens as small as shark teeth only a few centimeters in size have been collected from the Korematsu Formation in Miyoshi and Shobara (Nakano, 1999). Although the reason for the low number of odontocetes in the Bihoku Group remains unclear, we at least reject research and sampling biases as potential factors.
Although fragmentary, the partial mandibular fossil HMN-F30103 is the first unambiguous record of Odontoceti from the Bihoku Group in Miyoshi, Hiroshima, Japan. This new specimen provides evidence that odontocetes lived in the area during the latest Early to earliest Middle Miocene (approximately 16.1 to 15.6 Ma). However, questions remain as to why so few odontocete fossils have been recovered from the Bihoku Group relative to mysticetes.
We thank Noriko Ochi for donating the studied material. Thanks also go to Toshiyuki Kimura (Gunma Museum of Natural History) for the initial preparation of the studied material and Yusuke Ando (Mizunami Fossil Museum) for providing comparative specimen photos. We thank the two reviewers Olivier Lambert (Institut royal des Sciences naturelles de Belgique) and Mariana Viglino (Instituto Patagónico de Geología y Paleontología (IPGP), CCT CONICET-CENPAT), and associate editor Hiroto Ichishima (Fukui Prefectural Dinosaur Museum) for their constructive comments that helped improve the manuscript.
Y. T. conceptualized this study and wrote the original draft. T. K. made Table 3. T. Y., H. O. and T. K. contributed discussion and revised the draft.