Paleontological Research
Online ISSN : 1880-0068
Print ISSN : 1342-8144
ISSN-L : 1342-8144
RESEARCH ARTICLE
A short report of the first record of an Odontoceti (toothed whale) from the Korematsu Formation, Bihoku Group (latest Early to earliest Middle Miocene) in Japan
Yoshihiro Tanaka Takanobu YamaokaHitoshi OhzawaTomomi Kiyoshi
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2026 年 30 巻 p. 17-27

詳細
Abstract

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.

Introduction

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).

Table 1. Reported Early to early Middle Miocene odontocetes from Japan with morphological description. Abbreviations: Fr., formation; Gr., Group; cf., confer; sp., species. See also institutional abbreviation section.

HorizonSpecimenIdentificationPartsAgeLocalitiesReference
Korematsu Fm., Bihoku Gr.HMN-F30103Odontoceti indet.mandibles16.1 to 15.6 Ma, late Early to early Middle MioceneMiyoshi City, HiroshimaThis study
Korematsu Fm., Bihoku Gr.HMN-F30102cf. Odontocetiright humerus16.1 to 15.6 Ma, late Erly to early Middle MioceneShobara City, HiroshimaTanaka et al., 2020
Hiramatsu Fm., Ichishi Gr.GMNH-PV-2570, HolotypeNinjadelphis ujiharaipartial skeleton including skull, periotics, tympanic bullae, mandibles and forelimb elements17 Ma, late Early MioceneIga City, MieKimura and Barnes, 2016
Haze Fm.,
Ichishi Gr.
MPM-Fo1058, HolotypeMiodelphinus miensisSkull, right and left periotics and tym- panic bullae, right incus and malleus, four isolated teeth, three possible hyoid bones and two ribs18.7 to 18.5 Ma, Early MioceneTsu City, MieTanaka and Nakagawa, 2024
Oi Fm., Ichishi Gr.MFM 53701OdontocetiforelimbEarly MioceneTsu City, MieKimura and Kaede, 2016
Oi Fm., Ichishi Gr.private specimenscf. Stenella kabatensis (now Eodelphinus kabatensis)three teethEarly MioceneTsu City, MieMatsuhashi and Ooyagi, 2013
Oi Fm., Ichishi Gr.private specimensDelphinidae indet.periotic and two teethEarly MioceneTsu City, MieMatsuhashi and Ooyagi, 2013
Oi Fm., Ichishi Gr.private specimenDelphinoidea indet.toothEarly MioceneTsu City, MieMatsuhashi and Ooyagi, 2013
Oi Fm., Ichishi Gr.private specimenscf. Scaldicetus sp.two teethEarly MioceneTsu City, MieMatsuhashi and Ooyagi, 2013
Oi Fm., Ichishi Gr.private specimensOdontoceti indet.two teethEarly MioceneTsu City, MieMatsuhashi and Ooyagi, 2013
Oi Fm., Ichishi Gr.WMNH-Ge-1121340002Odontoceti indet.mandibles17.2 to 16.3 Ma, Early MioceneTsu City, MieTanaka et al., 2021
Yamanouchi Fm., Mizunami Gr.MFMAulophyseter sp.skull, mandible, teeth and atlasEarly MioceneMizunami City, GifuOkazaki, 1992
Akeyo Fm., Mizunami Gr.MFMPlatanistoidea?right scapula, humerus, ulna, radius and carpalsEarly MioceneMizunami City, GifuKamei and Okazaki, 1974; Ichishima, 2005
Akeyo Fm., Mizunami Gr.MFM 18002, Holotype“Eurhinodelphis” minoensis re-identified as an odontocetimandibles, vertebrae, ribs, teethEarly MioceneMizunami City, GifuOkazaki, 1976; Ichishima, 2005
Akeyo Fm., Mizunami Gr.MFM 18003“Eurhinodelphis” minoensis re-identified as an odontocetimandibles and teethEarly MioceneMizunami City, GifuOkazaki, 1976; Ichishima, 2005
Akeyo Fm., Mizunami Gr.MFMEurhinodelphis sp. A. re-identified as a kentriodontidskull and ear bonesEarly MioceneMizunami City, GifuOkazaki, 1976; Ichishima, 2005
Toyama Fm., Iwamura Gr.MFM 18190Squalodelphinidae indet.left periotic, right tympanic bulla and right malleus17 to 16 Ma, Early MioceneMizunami City, GifuKimura, 2019
Morozaki Gr.TMNH 10785, HolotypeMiophyseter chitaensisskull, periotic, tympanic bulla and skeletonEarly MioceneMinamichita, AichiChita−kujira Excavation Research Group, 1993; Kimura and Hasegawa, 2022, 2023
Bessho Fm.SFM-00001, HolotypeBrygmophyseter shigensisskeletonearly Middle MioceneMatsumoto, NaganoHirota and Barnes, 1995; Kimura et al., 2006
Bessho Fm.MCM-56221Ziphiidae indet.skullearly Middle MioceneMatsumoto, NaganoHasegawa and Kimura, 2003
Bessho Fm.KIM-1, HolotypeSinanodelphis izumidaensisskull, vertebrae and forelimbearly Middle MioceneAoki, NaganoMakiyama, 1936; Kohno et al., 2007
Bessho Fm.MCM-56211Delphinoidea indet.skullearly Middle MioceneMatsumoto, NaganoKohno et al., 2007
Kadonosawa Fm.IGPS 59740Scaldicetus indet.toothlate Early to early Middle MioceneNinohe City, IwateMatsumoto, 1926; Kohno and Ray, 2008
Sugota Fm.UTHFM 00034, HolotypePlatysvercus ugonisskull16.7 to 16.29 Ma, Early MioceneUgo Town, AkitaGuo and Kohno, 2023
Kadonosawa Fm.NMHF 999, HolotypeKentriodon sugawaraiskull, one tooth, the right tympanoperiotic, malleus, mandibles and atlaslate Early to early Middle MioceneNinohe City, IwateGuo and Kohno, 2021
Takinoue Fm.HMG 387, HolotypeKentriodon hobetsuskullearly Middle MioceneMukawa, HokkaidoIchishima, 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.

Material and methods

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.

Systematic paleontology

Order Cetacea Brisson, 1762

Unranked clade Neoceti Fordyce & de Muizon, 2001

Suborder Odontoceti Flower, 1867

Odontoceti indet.

Figure 2

Figure 2. Lower jaw of HMN-F30103, Odontoceti indet. A, dorsal view; B, ventral view; C, left lateral view; D, posterior view; E, anterior view; F, right lateral view.

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).

Figure 1. Map showing the locality of HMN-F30103, Odontoceti indet. The base map was published by the Geospatial Information Authority of Japan. Abbreviations: Fr., formation; Gr., Group; Mio., Miocene.

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).

General description

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).

Discussion

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.

Table 2. Comparison of long and narrow mandibles of some Early to early Middle Miocene odontocetes, derived from Table 2 of Tanaka et al. (2021).

FamilyScientific name or specimen numberAgelong groove on ventrolateral sidealveolar shapemandibular symphysis width and height, at preserved most posterior part or anterior to diverging point of the mandibleslength of alveoli vs interalveolar spaces, at preserved most posterior part or anterior to diverging point of the mandiblesUsed references for comparison
Odontoceti indet.HMN-F30103, partly preserved mandiblelate Early to early Middle Mioceneshallowcircularwidermore or less the sameThis study
Odontoceti indet.WMNH-Ge-1121340002, partly preserved mandiblelate Early Mioceneshallowcircularwidermore or less the sameTanaka et al., 2021
Odontoceti indet.“Eurhinodelphis” minoensis, holotypeEarly Mioceneshallowcircularwidermore 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 mandiblesOkazaki, 1976
AllodelphinidaeNinjadelphis ujiharai, holotype GMNH-PV-2570late Early Miocenedeepcircularmore or less the sameshorter interalveolar spaceKimura and Barnes, 2016
SqualodelphinidaeSqualodelphis fabianii, holotype MGP 26134Early Mioceneshallowcircularwiderlonger interalveolar spacePilleri, 1985
SqualodelphinidaeNotocetus vanbenedeni, MLP 5-10Early Mioceneabsentcircularwidermore or less the sameLydekker, 1894; Viglino et al., 2022
PlatanistidaeAraeodelphis natator, holotype USNM 10478Early to early Middle Mioceneshallowcircularwidershorter interalveolar spaceKellogg, 1957
PlatanistidaePomatodelphis inaequalis, USNM 6683, partly preserved mandibleMiddle to Late Mioceneshallowanteroposteriorly longerwidershorter interalveolar spaceKellogg, 1959
AllodelphinidaeZarhinocetus errabundus, LACM 149588Middle Miocenedeepanteroposteriorly longerwidershorter interalveolar spaceKellogg, 1931, Kimura and Barnes, 2016
EoplatanistidaeEoplatanista italica holotype MGP 26150, 26151Early Mioceneshallowanteroposteriorly longer?shorter interalveolar spacePilleri, 1985
EurhinodelphinidaeXiphiacetus bossi, holotype USNM 8842Early to Middle Miocenedeepcircularwidershorter interalveolar spaceKellogg, 1925
EurhinodelphinidaeSchizodelphis sulcatus, MGP 26154Early to Middle Mioceneshallowanteroposteriorly longer?longer interalveolar spacePilleri, 1985
KentriodontidaeBelonodelphis peruanus, holotype MNHN PPI 231Late Mioceneshallowanteroposteriorly longerwidershorter interalveolar spaceMuizon, 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.

Table 3. Reported mysticetes from the Bihoku Group in Miyoshi and Shobara. Some fragmentary materials reported by Otsuka and Ota (2008) are omitted. Abbreviations: Fr., formation; Gr., Group; cf., confer; sp., species. See also institutional abbreviation section.

HorizonSpecimenIdentificationAgeLocalityReference
Korematsu Fm.HMN-F00003Pelocetus sp.Early to Middle MioceneShobara CityKimura et al., 2007
Itabashi Fm.HMN-F00004Parietobalaena cf. yamaokaiMiddle MioceneShobara CityKimura et al., 2010: Ohzawa et al., 2007
Korematsu Fm.HMN-F00005–9
(IDs for the same individual)
Diorocetus shobarensis, holotypeEarly to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00010, 12–19
(IDs for the same individual)
Diorocetus shobarensis, holotypeEarly to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00021Parietobalaena yamaokaiEarly to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00022–24 (IDs for the same individual)Parietobalaena yamaokai, holotypeEarly to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00025Parietobalaena yamaokaiEarly to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00026Parietobalaena yamaokaiEarly to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00027Parietobalaena yamaokaiEarly to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00035, 36, 38, 40, 41Parietobalaena yamaokaiEarly to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00042–44, 54Parietobalaena yamaokai, paratypeEarly to Middle MioceneShobara CityOtsuka and Ota, 2008; Ohzawa et al., 2013
Korematsu Fm.HMN-F00045–47, 49, 51, 53Parietobalaena yamaokaiEarly to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00060Parietobalaena yamaokaiEarly to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00061Parietobalaena yamaokaiEarly to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00062Parietobalaena yamaokaiEarly to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00063Diorocetus shobarensis, paratypeEarly to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00064–80 (seems a series belongs to an individual)Parietobalaena yamaokaiEarly to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00081Parietobalaena yamaokaiEarly to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00082Pelocetus sp.Early to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00083Pelocetus sp.Early to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00084Hibacetus hirosei, holotypeEarly to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00085Parietobalaena yamaokaiEarly to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00086, 87Parietobalaena yamaokaiEarly to Middle MioceneShobara CityOtsuka and Ota, 2008
Itabashi Fm.HMN-F00088–92, 94–97cetaceaMiddle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00098Parietobalaena yamaokaiEarly to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00106–115Pelocetus sp.Early to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00117Parietobalaena yamaokaiEarly to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00118Aglaocetus sp.Early to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00119Aglaocetus sp.Early to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00120Aglaocetus sp.Early to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00121Aglaocetus sp.Early to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00122Aglaocetus sp.Early to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00123Aglaocetus sp.Early to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00124Aglaocetus sp.Early to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00125Aglaocetus sp.Early to Middle MioceneShobara CityOtsuka and Ota, 2008
Korematsu Fm.HMN-F00127, 128Parietobalaena yamaokaiEarly to Middle MioceneShobara CityOtsuka and Ota, 2008; Tsai, 2017
Korematsu Fm.HMN-F00640Parietobalaena yamaokaiEarly to Middle MioceneShobara CityKimura et al., 2011
Itabashi Fm.HMN-F11569cf.Diorocetus shobarensisMiddle MioceneShobara CityKiyoshi et al., 2020
Itabashi Fm.HMN-F20256–72 (IDs for the same individual)Cetacea indet.Middle MioceneShobara CityFurukawa et al., 2004
unknownSFM-00100Cetotheriidae indet.Middle MioceneShobara CityOhzawa and Yamaoka, 2003
Itabashi Fm.SFM-00106cf. CetotheriidaeMiddle MioceneShobara CityOhzawa and Yamaoka, 2003
Itabashi Fm.SFM-00107cf. CetotheriidaeMiddle MioceneShobara CityOhzawa et al., 2001
Korematsu Fm.SFM-00111Cetacea indet.Early to Middle MioceneShobara CityYamaoka et al.,1995
Korematsu Fm.HUM-F-00253Cetacea indet.Early to Middle MioceneShobara CityImamura, 1953
Korematsu Fm.KFM-0003–23 (IDs for the same individual)Mysticeti indet.latest Early MioceneMiyoshi CityKimita 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.

Conclusion

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.

Acknowledgements

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.

Author contributions

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.

References
 
© 2026 The Authors.

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