miocene mollusks from the n agashino formation of the ... · manuscript rec eived dec. 13,2005...
TRANSCRIPT
豊橋市自然史博物館研報 Sci. Rep . Toyohashi Mus. Na t. Hist. , No. 16,ト14, 2006
Miocene Mollusks from the N agashino Formation of the Shitara Group in Shinshiro City, Aichi Prefecture, central J apan
Hiroshi Shibata * and Takashi Ichihara **
愛知県新城市の設楽層群長篠層産中新世貝類化石
柴田博*市原俊**
(Abstract)
The present pap巴r d巴scribes and illustrat巴s a molluscan fauna coll巴ct巴d from the N aga shino Fo rmation of th e Shita ra Group at Arumi,
Shinshiro City, Aichi Prefecture. The collect ion loc ality of mollu sks is identical with or very clos巴 to th e localit y from which Haya shi
and Koshimizu (1992) reported mollusks ide ntifi ed by them w ith middle Eoce ne speci巴s. The molluscan faun a cons ists 01' nine spec ie s;
Modiolus sp. , Crassostrea gravit esta (Yokoyama), Laeνicardium sp. , Phaco soma kωνagensis (Araki), M ere tr ix aru gai Otuka, H iat ula
minoensis (Yokoyama), Solen sp. , Na ticidae ge n. et sp. inde t. and C hicoreus sp. The Nagashino Forrnation is referr巴d to ea rl y Mioc巴n巴 age
on th巴 basis of their geo lo gic ranges
for the Nagas hin o Format ion of the Hok usetsu Subgroup
Introduction from associated mollusks. After the publi shm ent of
Hayashi and Koshimizu (1992) , Ma tsuoka (1996) report ed
Miura (1890) was the first to mak e r巴ferenc巴 to the ag巴 Miocene mollu sks from th巴 Hokusetsu Subgroup, and
of the Shitara Group in th巴 Shitara ar巴a, Aichi Pr巴fecture, Aoyama (1996) assigned th e Shitara Group to Miocene
ass igning it to Miocene ag巴 on the basis of th巴 molluscan age on the stratigraphica l basis. More recently Hoshi and
fauna . Ther eafter many workers referred it to early or others (2000) suggested the 巴arly Miocene as the age for
ear ly to middle Mioc巴ne age on th巴 paleontological or the Hokus巴tsu Subgroup from correlatio n of radiolarians
stratigra phic basis for abou t a hundred yea rs. Th巴y includ巴 from its middle to upper par t. Thus it is h巴lpful to 巴xamme
Is hikawa (1900; 1901), Notomi (1 929), Tsuboya (1 936), the molluscan fauna from th e Naga shin o Formation for
Hayashi (1973) , Yoshida (1953) , K ato (1 962) , Shibata carrying forward th巴 age assignment of this formation
and oth巴rs (1977), Shibata (1 978), Collaborative Resear ch and the Shit ara Group . Conc巴rning th巴 molluscan fauna
Group for th巴 Shidara Basin (1979) and Shib ata and Ina from th e Na gashino Formation seve ral works hav巳 been
(1983). pl巴viously pub lis hed besides Ha yashi and Koshimizu
Hayashi and Koshimizu (1 992), how巴ver, gave fission (1992) . They are occurre nc e records of Miocen巴 species by
track dates of Paleogen巴 ag巴 for the Hokus巴tsu Subgroup Hayash i (1973) , Shibata and others (1977) and Yokoyama
of the Shitara Group , and suggested middle Eocene ag巴(1987) , description of M iocene sp巴cies by Shibata and In a
*豊橋市自然史博物館. Toyoha shi Mus eum of Natura l History , ト238 Oana, Oiwa-cho, To yohashi 441-3147, Japa n.
**名古屋大学大学院環境学研究科. Gr adu ate School of Environm ent al Studies, Nago ya University, Furo-cho, Chikusa-ku, Nago ya 464-8601 , Jap an
Manuscript rec eived Dec. 13, 2005 原稿受付 2005年 12 月 13 日.
Manuscript ac cepted Jan. 18, 2006 原稿受理 2006年 l 月 1 8 日
Key words : Mol lusks,巴arly Miocene, N aga shino Formation, Shi tar a Group, Shin shiro City, Aichi Prefectur巴キーワード:貝類, 前期中新世, 長篠層, 設楽層郡.新城市, 愛知県.
Hiroshi Shibata and Takashi Ichihara 2
(1983) and a taxonomic revision of th巴 previously r巴ported
mollusks (Hayashi , 1973) by Hayashi (1988) .
W巴巴xamm巴d a larg巴 molluscan collection by Y oshiaki
Y okoyama and an additional on巴 by K巴iji Matsuoka both
1'rom the Nagashino Formation at Arumi , Shinshiro City
for this study . Collecting of them was mad巴 separately
at the same n巴w exposure mad巴 by roadworks in 1987
Their collections consist 01' nine species including thre巴
sp巴cies previously not reported from th巴 Nagashino
Formation. The purpos巴 of this paper is to describ巴 and
illustrate them and to discuss th巳 age 01' that 1'ormation . We
1'ollow Hayashi and Koshimizu (1992) 1'or the stratigraphic
classi 1'ication of the Shitara Group .
All specim巴ns d巴 scribed her 巴 in are deposited in
Toyohashi Mus巴um 01' Natural History.
Fig. 1. Map showing th巴 collection locality in Shinshiro City, Aichi Pr巴fecture.
We are ind巴bted to M r. Yoshiaki Yokoyama of (Yokoyama) , Phacosoma kawagensis (Araki) , Meretrix
Horaijisan Natural History Museum and Dr. Keiji Matsuoka arugai Otuka, Solen sp . and Hiatula minoensis (Yokoyama)
of Toyohashi Museum 01' Natural History 1'or allowing us to have b巳en known to occur outside the Shitara ar巴a .
examm巴 th巴ir molluscan collections from Arumi . Phacosoma kawagensis (Araki) and Solen sp. hav巴 been
known from the 巴arly Mioc巴n巴, and Meretrix αrugai Otuka
Locality and Hiatula minoensis (Yokoyama) have been r巴corded
from the early to middle Mioc巴ne . Crassostrea gravitesta
The two molluscan collections 巴xamined were obtain巴d (Yokoyama) has a g巴ologic range 01' the early Miocene to
S巴parately by Yoshiaki Yokoyama and by Keiji Matsuoka th巴 Pliocen巴 The geologic ranges of thes巴 species indicat巴
1'rom the same exposure of the Nagashino Formation the 巴arly Mioc巴ne is most probable as the age for the
at Arumi (Fig. 1) in 1987. Enclosing sedim巴nts 01' Nagashino Formation.
mollusks consist of coarse-grained sandstone and granule Shibata and others (1977) r巳port巴d a total 01' nin巴 species
conglomerate. That exposure was made by roadworks in of mollusks from the Nagashino Formation at their localiti巴8
1987 , and is now los t. A detail巴d description 01' its location 1 and 2, which are n巴ar to the present coll巴cting locality.
and the stratigraphy at it can b巴 found in Yokoyama Among them are Trapezium modiolaeforme Oyama and
(1987) . Hayashi and Koshimizu (1992) gav巴 no detailed Saka and Cyclina japonica Kamada. These species hav巴
description 1'or the 10cality at which they collected mollusks a geologic range 01' the early Miocen巴 and that of the 巴arly
regarded by th巴m as middl巴 Eoc巴ne ones , only showing it to middle Mioc巳n巴, resp巴ctively. There is , how巴ver, no
on th巴ir geologic map. The present collection locality is speci巴 s of which geologic range 巴xtends to th巴 Paleog巴ne
considered to b巴 id巴ntical with or very close to that locality in th巴 nm巴 species . These facts support the ag巴 asslgnment
by referenc巳 to its location on their geologic map . mentioned abov巴. All thos巴 S巴ven species are found in th巴
molluscan 1'auna (Itoigawa and others, 1974, Itoigawa and
Age oth巴rs , 1981) 1'rom the Mizunami Group in Gifu Pre1',巴cture ,
and their occurrence in the group is r巴strict巳d to th巴 lower
Th巴 molluscan collections 1'rom Arumi consist 01' nin巴 part 01' th巳巴arly Mioc巴ne Akeyo Formation. Thus the
sp巴cies , which ar巴 Modiolus sp., Crassostrea gravitesta Nagashino Formation is correlated with it.
(Yokoyama) , Laevicardium sp. , Phαcosoma kawagensis
(Araki) , Meretrix arugai Otuka , Hiatula minoensis
(Yokoyama) , Solen sp. , Naticidae g巳n. et sp. inde t. and
Chicoreus sp . Fiv 巳 of them , Crassostreα grα v z testα
Descriptions
Phylum Mollusca
Miocene Mollusks from the Nagashino Formation
Class Bivalvia
Subclass Pteriomorphia
Order Mytiloida
Superfamily Mytilacea
Family Mytilidae
Subfamily Modiolinae
Genus Modiolus Lamarck, J 799
Modiolus sp.
(Fig. 2-1)
Modiolus sp. Hayashi , 1973, pl. 2, fig. 3
Mytilus sp. Hayashi, 1988, pl. 2, fig. 3
Material -. One specimen.
Crassostrea gravitesta (Y okoyama, J 926)
(Fig. 2-4 )
3
1926 Ostrea gravitesta Yokoyama, Jour. Fac. Sci. , Imp. Uni v
Tokyo, Sec . 2, vo l. 1, pt. 9, p. 388, pl. 45, figs. 1, 2
Ostrea gravite sta Yokoyama. Nomura, 1938, p. 248, pl. 33, fig
15 ; Makiyama, 1958, pl. 57, figs . la-c, 2a-c ; Ogasawara,
1973, pl. 13, fig. 28 ; Hayashi, 1973, pl. 2, fig. 5.
Ostrea (Crassostreα) gravitesta Yokoyama. Kaseno, 1956, p. 7, pl
1, figs. 5a-c
Crassostrea gra vitest a (Yokoyama). Itoi gaw a and oth巴rs , 1974,
p. 72, pl. 17, fig. 1; Yoon, 1976, p. 9, pl. 1, figs. 24, 25 , pl.
3, fig s. 17, 18; ltoi gawa and Nishikawa, 1976 , pl. 33, fig
11 ; Ogasawara and Noda, 1978 , p. 32, pl. 3, fig. 23 ; Taguchi
and others, 1979, pl. 1, fig. 15 ; Yoon, 1979 , p. 10, pl. 3,
fig. 1; Amano, 1980, p. 106, pl. 13, figs. 29a, b; Takayasu,
Description -. Shell small , ovate , expanded posteriorly, 1981 , p. 99, pl. 2, fig. 15; Itoiga wa and others, 1981 , 1982,
bulged along an oblique medial line running from beak p. 53, pl. 10, fig. 3; Shibata and lna, 1983 , p. 43 , pl. 4, fig. 9;
to postenor 巴nd. Beak low, situated close to anterior end. Naka ga wa and Takeyama, 1985, pl. 2 1 ,行gs. la, b; Okumu ra
Anterior and post巴rior ends rounded. Post巴ro-dorsal margin and others , 1985 , pl. 49, fig s. 2a, b; Itoigawa and Shibata,
slightly arched, passing into posterior margin with a blunt 1986, pl. 16, fig . 11; Hayashi, 1988, pl. 2, fig. 5; Kanno and
angle . Postero-ventral corn巴r produced post巴ro-ventrally. others, 1988 , pl. 2, fig . 12; Okamoto and others, 1989, pl. 5,
Surface smooth. Dimensions; length 19.5 mm , height 17 .0 fig s. 14a, b; Muramatsu, 1992, pl. 49, fig . 14
mm. Crassost rea gravitesta eoli ensis Kim, Noda and Yoon , 1974, p.
274, pl. 38, fig . 15, pl. 39, fig s. la -c; Lee, 1992, p. 79, fig s.
Discussion - The sp巴clm巴n at hand is a d巴form巴d 28-10a, b.
inner cas t. It bears a similarity in shape and siz巴 to
Modiolus nakamurai Itoigawa an d Shibata from the ear ly Material -. Two right vaJves .
Miocen巴 Akeyo Formation of the Mizunami Group in
Gifu Prefecture, but it is impossibl巴 to mak巴 a detailed 0巴scription - Right valve large , v巴ry thick , ovate,
comparison of the specim巴n with that speci巴s owing to flatt巴n巴d. 8eak pointed , with a triangular ligamenta l
the ill stat巴 of its preservation . The specimen res巴mbles groove b巴low it. Surface with rudel y co rrugated growth
Modiolus yasuhiroi Kamada describ ed from the middle lin巴s
Mioc ene Taga Group in the Joban Coal-Fi巴ld and Modiolus
arakaw ensis (Kanno) from the middle Miocen e Nagura
Formation of th巴 Chichibu-machi Group in Saitama
Pre1'ecture, but the shell is smaller
Ord er Pt巴rioida
Subord er Ostr巴ma
Sup巴rfamily Ostl巴acea
Family Ostreidae
Subfamily Ostr巴mae
G巴nus Crassostrea Sacco, 1897
Dim ensions (in mm) 一
Length
82.3
Height
188. 7
88.5 125 .3
Discus sion -. The lar ge and thick shell is a di ag nos tic
charact巴r 0 1' C ra ssostrea graν ites ta (Yokoyama).
Crassostrea graνltestα(Yokoyama) clos巴ly resemble s
Crassostr ea gigas (Thunberg), a li ving species of Japan, but
th巴 shell is thi cker.
4 Hiroshi Shibata and Takashi Ichihara
G巴ologic rang巴ー. Early Miocene to Pliocene
Subclass Heterodonta
Order Veneroida
Superfamily Cardiacea
Family Cardiidae
Subfamily Laevicardiina巴
Genus Laevicardium Swainson, 1840
Laevicardium sp.
(Figs. 2-2, 3a, b)
Phacosoma kawagensis (Araki, 1960)
(Figs. 2-5a-c, 6; Fig . 3-1)
1960 Dosinia japonica kωνagensis Araki , Bul l. Lib. Arts Dept.,
Mie Univ. , Spec. Vo l., (1), p. 95 , pl. 7, fig. 3
Dosinia (Phacosoma) kawagensis Araki. Masuda, 1963, p. 22 ,
pl. 4, figs. 1-8; Yoon , 1979 , p. 15 , pl. 2, figs. 7, 9, 10;
Matsubara , 1995 , p. 330, figs. 4-9-11 ; Honda and others ,
1998, p. 20, fig. 5-16
Dosinia anguloides Nomura (non Nomura). Hata, 1967, pl. 4, figs.
2, 3
Dosinia kawagensis Araki. Hayashi and Miura, 1973 , pl. 2, fig. 12;
Glycymeris cisshuensis Makiyama (non Makiyama). Hayashi , Hayashi , 1973, pl. 1, figs. 2, 3; Ishida and others , 1980, pl. 3,
1973 , pl. 1, fig. 6. fig.12
Glycymeris cf. altoumbonata Nagao. Hayashi , 1988, pl. 1, fig. 6. Dosinia nomurai Otuka (non Otuka). Hayashi , 1973 , pl. 1, fig. 1
Dosinorbis kawagensis (Araki). Itoigawa and others , 1974, p. 87 ,
Mat巴rial -. Two specimens. pl. 23 , fig s. 1-6.
Phacosoma kawagensis (Araki). Itoigawa and others , 1981 ,
Description -. Shell small , thin , ovate in outlin巴, slightly 1982, p. 80, pl. 14, figs. 6a, b; Shibata and Ina, 1983 , p. 48 ,
longer than high , moderately intlated . Beaks small , situated pl. 5, fig. 12; ltoigawa and Shibata, 1986, pl. 16 , fig. 13;
at a little ant巴rior of the middle of th巴 shelll巴ngth. Ant巴rior Muramatsu, 1992, pl. 49 , fig. 10
end rounded , v巴ntral margin arched , postero-ventral corn巴r Dosinia (Phacosoma) chikuzenensis nomurai Otuka (non Otuka)
roundlyangulate . Surface with many radiating rib s. Hayashi , 1988 , p. 5, pl. 1, fig s. 2, 3
Dimensions (in mm)
Length H巴ight Thickn巴ss
32.6
26.1
30.0
2l.8
13.0
Dosinia (Phacosoma) chikuzenens is Nagao (non Nagao)ー Hayashi ,
1988 , pl. 1, fig. 1
Material -. More than 160 specimens in th巴 Yokoyama's
collection and 22 sp巴cimens in the Matsuoka's collection .
About 2/5 of them are with their both valves conjoined,
Discussion -. Laevicardium sp. r巴sembles Laevicardium and the others are with their both valves disarticulated. All
undatopictum (Pilsbry) living in the West Pacific in shap巴 specimens are more or less lat巴rally compressed.
but the sh巴11 is larg巴r , and radial ribs in the posterior part
of th巴 shell are less prominen t. Laevicardium sp. is also 0巴scription -. Shell of medium size, suborbicular, longer
analogous to Laevicardium yoshidense Kanno from the than high , slightly intlated. Beaks pointed , turned forward ,
early Miocene Nenokami Sandstone of the Ogano-machi a little ant巴riorly situated. Ant巴ro-dorsal margin short,
Group in Saitama Pr巴fecture , but it has a larger number n巴arly straigh t. Post巴ro-dorsal margin gently arcuate ,
of radial ribs. It somewhat res巴mbles Nemocardium sp. pa ssing into anterior margin with an obtuse angle . Ventral
reported by Shibata (1970) from th巴巴arly Miocen巴Ichishi margin round巴d. Pallial sin us deep , angulat巴 Surface
Group in Mie Prefecture , but the shell is mor巴巴longate. with regular concentric lines. Lunul巴 W巴11 mark巴d , small ,
cordate, depressed. Escutcheon long, naηow.
Superfamily Veneracea
Family Veneridae
Subfamily Dosiniinae
Genus Phacosoma Jukes-Brown , 1912
Dim巴nsions (in mm) ー.
Length
47.2
42.6
Height Thickness
4l.4 18.5
39.2 12.5
Miocene Mollusks from the Nagashino Formation
41.8
40.5
46.2
36 .2
36.7
43 .1
16.1
11.7
5
Mactra squalida (Yokoyama) (non Yokoyama). Hayashi, 1988, pl.
2, fig. 2
Eomeretrix sp. Hayashi and Koshimizu, 1992, figs. 3-4, 5
Discussion -. Phacosoma kawagensis (Araki) res巴mbles Mat巴rial -. Twenty-s巴ven specimens in the collection by
Phacosoma japonicum (Reeve) living in th巴 adjacent Yokoyama and 2 specim巴ns in the co Jlection by Matsuoka .
seas of Japan , but th巴 shell is smaller, and the proportion Most of th巴m are well preserved , and 7 sp巴cimens in th巴
of th巴 shell I巴ngth to the sh巴llh巴ight is small巴r. 1t also former are with their both valv巴s articulated.
r巴sembles Phacosoma nomurai (Otuka) described from
the early Mioc巴ne Lower Kadonosawa Formation in Iwate
Pref,巴cture , but the shell is slight ly depr巴ssed in th巴 antenor
and posterior parts , and the post巴ro-dorsal margin less
slopes ventrally .
This species is the most ab undant speci 巴 s at the
collection locality . Specimens occur in a clust巴r , mostly
with the convex sides of their valves parallel to the bedding
planes of th巴Ir 巴nclosing sedimen t.
Geologic range -. Early Mioc巴n巴.
Subfamily Meretricinae
G巴nus Meretrix Lamarck, 1799
Meretrix arugai Otuka, 1938
(Figs. 3-2-5a, b)
1938 Meretrix arugai Otuka, Jour. Fac . Sci. , Imp. Univ. Tokyo ,
Description -. Shell medium in size , thick , subtrigonal ,
longer than high , inflated. Beaks swollen , high , turned
inward , locat巴d at a little front of the cent巴r of the sh巴 11
Antero-dorsal margin straight , post巴ro-dorsal margin
sligh tly arcuate , ventral margin broadly rounded. Anterior
end round巴d , post巴rior end more narrowly rounded. Lunule
and escutcheon absen t. Three cardinal t巴eth on cardinal
plate . Pallial sinus moderat巴Iy deep , angulat巴. Surfac巴
smooth with fine growth lines .
Dimensions (in mm) ー.
Length Height Thickness
71.0 59.0 30.2
59.4 51.2 34 .4
79 .5 65.2
79 .3 65.1
79.1 61.8
S巴c . 2, p. 30, pl. 2, figs. 11 , 12. Discussion -. Meretrix arugai Otuka is charact巴rized by
Meretrix arugai Otuka. Hatai , 1940, p. 129; Araki , 1960, p. 93 , pl. the well swollen beak. It resembles Meretrix lusoria
7, fig. 5; Itoigawa and others , 1974, p. 86 , pl. 22 , figs. 5-8; (Rりding) and Meretrix lamarcki (Deshayes) , both living
Itoigawa and Nishikawa, 1976, pl. 34, fig. 8; Taguchi and species of Japan , but the beak is more swollen
others , 1979, pl. 3, fig. 8; Ishida and others , 1980, pl. 3, fig.
5; Itoigawa and others , 198 1, 1982, p. 89 , pl. 17, figs. 4a, b,
5a, b; Takahashi , 1984, pl. 1, fig. 2; Itoigawa and Shibata,
1986, pl. 17 , fig. 5; Sasaki and Ogasawara, 1986, pl. 5, figs.
7a, b; Nakagawa, 1989, pl. 1, fig . 8; Noda and oth巴rs , 1989,
pl. 25 , figs. 5a, b; Okamoto and others , 1989 , pl. 6, fig. 12;
Okamoto and others , 1990, pl. 9, fig. 6; Noda and others ,
1994, figs . 6-10 , 14a, b, 18; Matsubara, 1995 , p. 333 , figs.
5-8.9. 11
Meretrix cf. arugai Otuka. Hayashi , 1973 , pl. 2, figs. 1, 2
?Meretrix arugai Otuka. Oga sawara and Noda, 1978, p. 35 , pl. 3,
figs. 17, 20, 22a, b
Pitar? sp. Shibata and Ina, 1983 , p. 48 , pl. 5, fig . 15.
Callista cf. han zawa i (Nagao) . Hayashi , 1988, pl. 2, fig . 1
Geologic range -. Early to middle Miocene .
Superfamily Tellinac巴a
Family Psammobiidae
Subfamily Sanguinolariinae
Genus Hiatula Modeer, 1793
Hiatula minoensis (Yokoyama, 1926)
(Figs. 4-1 a , b, 2a, b)
1926 Soletellina minoensis Yokoyama, Jour. Fac. Sci. , Imp. Univ
Tokyo, Sec . 2, vo l. 1, pt. 7, p. 221 , pl. 28 , figs. 13 -16
Soletellina minoensis Yokoyama. Masuda , 1955 , pl. 19, fig. 9;
Hiroshi Shibata and Takashi lchihara 6
Fig. 2. Mollusks from th e Na gashino Formation at Arumi , Shinshiro City (1). 1. Modiolus sp. ( X 2). 2, 3a, b. Laevicardium sp. 3b, apical vi巴w. ( X 1.5). 4. Crassostrea gravite sta (Yokoyama ). ( X
0.8 ). 5a-c, 6. Pha cosoma kawagensis (Araki) . 5c, ap ica l view . ( X 1.5) .
.. ・・・
Miocen巴 Mollusks from the Nagashino Formation
Fig. 3. Mollusk s from th e N ag ashino Fo rm ation at Arumi , Shin shiro City (2).
6
7
1. Ph acos oma kawagensis (Ar aki ). (X 1.5 ). 2-5a, b. M eret rix ar uga i O tuk a. 5b, sho w in g th巴 cardinal te eth. ( X 1). 6, 7
Solen sp. ( X 1).
7
Hiroshi Shibata and Takashi Ichihara 8
Fig. 4. Mollusks from the Nagash ino Formation at Arumi , Shinsh iro City (3) .
la, b, 2a, b. Hiatula minoensis (Yokoyama) (X 1). 3a-c, 4a-c . Naticidae gen 巴t sp . ind巴t. ( X 2). 5. Chicoreus sp . Dorsa l view. (X 2).
Miocene Mollu sks from the Nagashino Formation 9
Araki, 1960, p. 100, pl. 8, fig. 1; Kamada, 1962, p. 126, p1. the middle of the shelllength. Antero- and post巴ro-dorsal
14, fig. 7; Mizuno, 1964, pl. 4 , figs. 3, 4; Mizuno, 1965, margins gently sloping; ant巴rior margin round ; post巴rior
p. 34, p1. 1, fig. 3; Uozumi and Fujie, 1966, pl. 12, fig. 12; margin subtruncate; ventral margin arcuate. A blunt ridge
Hayashi , 1973, pl. 1, figs. 9, 10 ; Hayashi and Miura, 1973 , running from beak to the postero-ventral corne r. Surface
p1. 1, figs. 19, 20; Kim and others, 1974, p. 278, p1. 38, fig. 4; smooth.
Okamoto and T巴rachi , 1974, p1. 47, fig. 9; Yoon, 1979, p. 14,
pl. 2, fig. 12 ; O'Hara and Nemoto, 1984, pl. 1, fig. 17; Kanno
and others, 1988, p1. 1, fig. 10.
Sanguinolaria (Soletellina) minoensis (Yokoyama). Otuka, 1934,
p. 619 , p1. 49, figs. 65a, b; Otuka, 1938, p. 34, p1. 2, fig s.
14, 18; Oyama and Saka, 1944, p. 141 , pl. 15, figs. 17, 18
(misspell巴d as Sanguinoraria)
Soletellina cf. minoensis Yokoyama. Kaseno, 1956, p. 8, p1. 3,
figs.14a-c. Discussion -. Hiatula minoensis (Yokoyama) resembles
Sanguinolaria minoensis (Yokoyama). Makiyama, 1958, pl. 39, Hiatula diphos (Linnaeus) living in th巴 West Pacific, but
figs. 13-16 . the beak is more post巴riorly located. It has some similarity
Mya cuneiformis (Bりhm) (non B�m). Hayashi, 1973, p1. 1, fig . 4. to Hiatula kobiyamae (Kanno) described from the
Latemula sp. Hayashi , 1973, p1. 1, fig. 8. Oligocene Asagai Formation in Fukushima Prefecture, but
Hiatula minoensis (Yokoyama). ltoigawa and others, 1974, p. 96, the shell is more elongat巴
pl. 28, figs. 10, 11a, b; Itoigawa and Nishikawa, 1976, p1. 34,
fig. 10 ; Ogasawara and Noda, 1978, p. 36, p1. 4, figs. 10-12,
15 , 17-19, 21, 22; Taguchi and others, 1979, pl. 3, fig. 4;
Ish ida and others, 1980, pl. 4, fig. 7; Taguchi, 1981 , p1. 2, fig
12; Itoigawa and others , 1981 , 1982, p. 102, pl. 20, figs.1 a,
b; Shibata and Ina, 1983 , p. 51 , pl. 7, fig. 4; Okamoto and
others, 1983 , p1. 23 , figs. 31 , 32; Nakagawa and Tak巴yama,
1985, pl. 17, fig. 11; Ozawa and oth巴rs , 1986, p1. 14, fig . 4;
Shibata and Kato, 1988, pl. 3, fig. 14; Nakagawa, 1989, pl.
2, figs. 3a, b; Okamoto and others, 1989, p1. 6, figs. 17, 18,
pl. 7, fig. 30; Iwamura Res巴arch Group, 1989, p1. 21 , fig. Solen (Solenarius) sp. Itoigawa and others, 1974, p. 100, pl. 31 ,
Dimensions (in mm) ー.
Length Height Thickness
71.5 40.0 21.5
69.6 40 .4 16.4
49.7 32 .5 10.8
55 .1 32.3
Geologic range -. Early to middle Mioc巴ne.
e
'
I
ML巴ー
片
山白川
d
n
a
?'en
-
-
-
r
o
u
hdSL
m
hdMJ
i
--'U
J
I
町O
白釦SP
F
s
u
u
s
n
巴G
Solen sp.
(Figs. 3-6, 7)
4; Okamoto and others, 1990, pl. 9, fig. 29; Amano, 1992, figs. 2, 3a, b.
pl. 57, fig. 14; Lee, 1992, p. 86, fig s. 31-4, 5, 14; Noda and Solen (s. s.) sp. Itoigawa and others, 1981 , 1982, p. 103, pl. 20,
others, 1994, figs. 6-8, 11 , 16; Ogasawara and Nagasawa, figs. 2a, b.
1992, p. 1241, figs. 8-1a, b, 2a, b, 5, 6a, b, 9-27 ; Matsubara, Solen sp. Shibata and Ina, 1983, p. 52, pl. 7, fig. 1
1995, p. 327, fi gs. 1-20, 21; Taguchi, 2002, pl. 5, fi g. 2.
Mya? sp. Hayashi , 1988, pl. 1, fig. 4
Hiatula sp. Hayashi, 1988, pl. 1, fig. 9.
Gobraeus つ sp. Hayashi, 1988, p1. 1, fig. 10
Material -. Three cast sp巴clmens
Description - Shell large , transversely elongate ,
compressed, ga ping at posterior 巴nd. Beaks very low ,
Mat巴rial -. Eight巴en specimens . About 1/3 of them are situated at anterior 巴nd . Anterior margin truncated ,
with their both valv巴s conjoined, and the rest are with th巴ir posterior margin round. Dor sa l and ventral margins
both valv巴s disarticulated. straight, paralle 1.
Description -. Shell medium , thin , ovat巴, compr巴ssed.
Beaks low, turned inward, situat ed at a littl e ant巴rior of
l
Hiroshi Shibata and Takashi Ichihara
Dim巴nsions (in mm) 一.
L巴ngth H巴ight Thickness
90.0
9.9
l ト4
16.2
7.0
Discussion -. Solen sp. resembles Solen strictus Gould
living in Japan , China and Kor巴a and Solen saitamensis
Kanno from the Oligocene Us hikubitoge Fo rmation in
Saitama Prefecture, but it differs from these species in
having a round posterior end. 1t has close affinity in shape
and size with Solen (Solenarius) sp. described by 1toigawa
and oth巴rs (1974) from the 巴arly Mioc巴neAk巴yo Formation
of the Mizunami Group in Gifu Prefecture,創1d it seems to
be conspecific with th巴 latter.
Geologic range -. Early Miocene
Class Gastropoda
Subclass Prosobranchia
OrderM巴sogastropoda
Family Naticidae
t
nl
ノ
p
a
t
'
e
c
l
a
g
4
.0FA
-
E
(
4EL
9u
N
Material -. Thre巴 d巴form巴d cast specimens
(Fig.4-5)
Material -. One cast of which dorsal part is covered wi th
sandstone. The apical part of the she ll is crus hed in the
sp巴CImen.
Description -. Shell of medium siz巴, fusiform , w ith
conical spire . Whorls more than thre巴, separated by deep
suture, shouldered at a little above their middl巴. The last
whorl large, with contract巴d ba se. Th巴 penultimate whorl
and th巴 last whorl ornamented with two and thre巴 spiral
cords, respectively. Both whorls bearing promin ent varice s
besides spiral cords . Dimension s; height 46.2 mm, width
28.6 mm
Discussion The specim巴n is similar in shape and
surface sc ulp ture to Chicoreus (R hi zophorimu rex)
tigan ouranus (Nomura) described from the early Miocene
Chiganoura Formation in Miyagi Prefecture, but the state
of preservation of it is not good enough for a positive
identification of it with that species.
References
Amano, K. , 1980. Miocene molluscan fossi ls from the Yudoro
Formation in the east of Rumoi , Hokkaido. Prof S. Kaηno
Mem. Vol., 99120
Description -. Shell small, globula r. Whorls more than 3, Amano , K. , 1992 . Cypra ea ohi ro i and its associated mollu scan
separated by distinct sutur巴. Spire small, conica l. The last species from the Miocene Kadonosawa Formation, Northea st
whorllarge, swollen . Japan. Bu ll . Mi zun ami Fossil 凡1us . , (19): 405-4 11. (in
Japan巴s巴 with English abstrac t.)
Aoyama, M. , 1996 . Rocks and mineral s. Jn Geography of Horaiュ
cho, -Nature- , 130-224. Horai-cho , Aichi Prefectur e. (in
Japan巴se . )
Araki , Y., 1960. Geology , pa1巴ontology and s巴dim巴ntary struct ure s
(including prob lema tica ) of the Tertiary formations
Discussion -. A lI spec imen s at hand are too poor in the developed in the environs ofT su City, Mi巴 Prefecture, Japan
state of pr巴servation to d巴termine their generic and specific Bull. Lib. Art s Dep. , Mi e Uniν" Spec., 1: 1-1 18.
names . Collaborative Research Group for the Shidara Basin, 19 79. The
Dimensions (in mm) ー.
Height
82 .4
Width
13.8
14.8 12. 7
Order Neogastropoda
Family Muricidae
Genus C hi coreus Montfort, 1810
Chicoreus sp
N eogene D istr ibu ted in th巴 South District of Mt . Horaiji,
Aichi Prefecture, C巴ntral Japan. Mem. G eol. Soc. Japan ,
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Miocene Mo Jlusks from th巴 Nagashino Formation 11
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Fukui Pr巴fecture , Centra1 Jap an. Bu ll . Mi zunami Fossil Mus. , 凡1izunamiFossil Mus., (17): 35-49 . (in Japanese w ith Eng lish
(12): 27 -47. (in Japanese with English abstrac t.) abs tr ac t.)
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Shibata, R., Taguchi , K. and Fuma, M. , 1977. Miocene Yoonヲ S. , 19 76. Geology and Paleontology of the T erti ary
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assemb lages from the Katsuta Group, Okayama Prefecture Japanese.)
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(29) ・ 95-133 .
Taguchi, E. , Ono, N. and Okamoto, K. , 19 79. Fossil mollu sca n
assemblages from th巴 Miocene Bihoku Group in Niimi C it y
and Ohsa-cho, Okayama Prefecture, Japan. Bu /l. Mi zunami
Fossil Mus. , (6) : 1-15 . (in Japanese wit h English abstract.)
Takahぉhi , H. , 1984. Mollu sca n assem blag es from th e M iocene
Nakayama Formation in the Kadono district, Joban Coal-
Field, Fuku sh im a Prefecture. Fo ssils (Palaeont. So c. Japan),
(36): 1-17. (inJapanes巴 with Engli sh abstrac t.)
Takayasu , K., 198 1. Fossi l Molluscs from the Miiocene Masuda
Group at Okuda, M asuda City - Molluscan foss il s from
14 Hiroshi Shibata and Takashi Ichihara
(要旨)
柴田博・市原俊:愛知県新城市の設楽
層群長篠層産中新世貝類化石.
愛知県新城市有海の設楽層群長篠層より産出
した貝類化石を記載し,それらの写真を示した .
これらの貝類化石の採集地は,林・輿水 (1992)
が中期始新世の種に同定した有海の長篠層貝
類化石の産地と同じかそれに極めて近い地点
である . 貝類化石は , Modiolus sp. , Crassostrea
gravitesω(Yokoyama) , Laevicardium sp., Phacosomα
kωvagensis (Araki) , Meretrix arugai Otuka, Hiatula
minoensis (Yokoyama) , Solen sp. , Naticidae g巴n. et
sp. indet.そして Chicoreus sp.の9種よりなる.貝
類化石の地質時代から長篠層の時代は前期中新
世と考えられる.