Ishii, Ken-ichi

Nogami, Yasuo

Osaka City University Repository

]ournal of Geosciences， Osaka City University 
Vol. 9， Art. 4・I
March， 1966 
Discovery of Triassic Conodonts from the So-called 
Palaeozoic Limestone in Kedah， Malaya * 
(Notes on the Geology and Palaeontology of Malaya-I) 
Ken-ichi ISHII & Yasuo NOGAMI** 
(With 1 Plate) 
Near Kodiang rai1way station in Kedah， Northwest Malaya several limestone 
hil1s are distributed above the plain. They are cal1ed Bukit Hantu， Bt. Kechil， 
Bt. Kalong， Bt. Kodiang， Bt. Kechil， Bt. Mutong and Bt. Kepelu， respectively， from 
the southwest to the northeast. These limestones have hitherto been regarded 
as Permian in age. At the beginning of 1965， Isml collected samples of limestone 
from Bt. Kalong and Bt. Kechil (the southern one of the two simi1arly named 
hills). Triassic conodon ts were discovered from the samples. This :first discovery 
of the Triassic conodonts from the western part of Malaya is preliminarily re-
ported here. A detai1ed description will be given in the near future. 
Brief Note of Geology 
1) Bukit Kechi1 (loc. M7)， near Kodiang railway station in Kedah 
The base of the hill is composed of mudstone (2m+thick)， but the main parts 
are composed of white， intrasparitic limestone， which yields occasionally calcare-
ous algae， bivalves and foraminifera. The limestone has a strike of N 50-800 W 
and dips 10-200 towards NE. 
About 2.5 kg samples of limestone were collected at a quarry (loc. M7) on the 
hill and were dissolved in 12-13 % acetic acid. As a result， about 30 conodonts 
have been obtained. 
2) Bukit Kalong (loc. M16)， near Kodiang rai1way station in Kedah. 
The hill is composed of three parts : the lower part， of white and intrasparitic 
limestone (about 15 m thick)， the middle part， of alternation of micritic limestone 
and chert (10m+thick)， and the upper part， of brecciated intrasparitic limestone 
(20m-lthick). The limestone and chert have a general strike of N 300 W and dip 
20-300 towards NE. 
About 2.0 kg samples of limestone from the lower part were dissolved in 12-13 
ゐ aceticacid， from which about 100 conodonts have been secured. 
General Characteristics of Conodont Faunules 
Two Triassic faunules of conodonts are now obtained from Western Malaya， 
* Contribution from the OCUSEA 1964-65， No. 4. 
林 Geol.Miner. Inst.， Coll. Sci.， Univ. Kyoto. 
93 
一、
94 Ken-ichi ISHII & Yasuo NOGAMI 
Gladigondolella cf. abne.ρtis faunule from Bt. Kechi1 and Gladigondolella tethydis 
faunule from Bt. Kalong. 
、
1) Gladigondolella cf. abnelりがsfaunule 
The faunule is constituted from the following elements. 
number of specimens 
Gladigondolella cf. abne.ρtis (HUCKRIEDE)・・・・・・…・・・・・・・・・・・・・・・…...7 
Gondolella navicula HUCKRIEDE...…・・・・・・・・・・・・…・・・・・・・・・・・・・・・・・・…・・・ 2 
“Alうatognathus"ziegleri DrEBEL .......! .，.・・ m ・ 山・・・・・・・・・・山・ 3 
Dかlododellalautissima (HuCKRIEDE)・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・… 1 
D. 1neissneri (T AT'G.E) .い.川 .. .1. • • .い.. . . . . . . . . . . . . . . . …“川，μ山川E川.
D. sp. indet. .. .，.・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・ 1 
“Hindeodella " ρetrae-virz'dis HUCKRIEDE ..................…・・・・・・・・・ 3 
4H." tftassica MaLEER---------・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・ 8 
Among these elements G. cf. abne.ρtis and G. navicula are important as hori-
zon markers. G. cf. abnelうtisis closely allied to the type specimen of G. abnelうがs，
but it differs slightly from the latter in having a more weakly ornamented plat-
form. G. abneJうtiswas first described by DIEBEL (1965b) as Polygnathus n. sp. 
from the Upper Cretaceous in Kameron， Africa， and then it was named Polygna-
thus abnφtis by HUCKRIEDE (1958) who reported it from the Ca:rnian to Norian of 
the Alps. The form be]ongs， however， to the genus Gladigondolella， which is 
proposed by MULLBR (1962) with POかgnathustethydis as the type species. 
According to HUCKRIEDE (1958) Gondolella navicula shows rather wide individ・
ual variation and occurs from the upper Anisian to the Carnian. An illustrated 
specimen in Pl. 1， fig. 6a-c， isregarded as advanced type and identical with the 
type specimen (HUCKRIEDE， 1958， pl.12， fig. 18-20). 
Other elements of the faunule are characteristic of the Triassic， except for 
“AJうatognathus"ziegleri， which occurs also in the Upper Cretaceous. Therefore， 
it can be presumed， in general consideration， that the present faunule belongs to 
the Late Triassic. It cannot be certainly concluded， since not a single reference 
to the Jurassic and Lower Cretaceous conodonts has ever appeared. Anyhow the 
Mesozoic age of the faunule is conclusive. 
2) Gladigondolella tethydis faunule 
The faunule is constituted from the fol1owing elements. 
number of spdcimens 
Gladigondolella tet均dis(HUCKRIEDE)・・・……ぃ・…………………… 2 
Gondolella navicula HUCKRIEDE.'.…............... .about 25 
Spathognαthodus cf. cγistagalli HUCKRIEDE .一……ぃ・ぃ・…・・・・・・… 2 
Diμododella meissneγi ('τATGE) …………………………・・・……… 5 
D. n. sp. ・・・・・・・・・・・・・・・・・・・・・…・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・ 1 
D. sp. indet. ............................. 2 
“Hz'ndeodellα" multihamata HUCKRIEDE...............…・・・……… m・3 
“H. " 
“H. " 
petrae-viridis HUCKRIEDE..................... about 15 
triassica MULLER............................... ..about 30 
Lonc hodina m:込leγiTATGE.......一…・・・……・・・……………………… 1 
Discove:η 01 T.γiassic Conodonts fiγom the so-called 
Palaeozoic Limestoγze in Kedah， Malaヲα
Neoρrioniodus cf. kochi (HUCKRIEDE)………………………・・・…… 2 
Ozarkodina saginata HUCKRIEDE ・・・….. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .・・ 2
O. Sp. indet. ・・・・・・…・・・・・・……・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・・ 4 
95 
Among these elements Gladigondolella tethydis and Gondolella navicula are 
characteristic as horizon markers. The specimen of G. tethydis illustrated in p1. 
1， fig. 1a-c， isalmost identical with the holotype from the lower Carnian. Accord-
ing to HUCKRIEDs (1958)， G. tethydis occurs from the upper Anisian to the Car-
nian. G. navicula of the present faunule is less advanced than that of Gladigondo・
lela cf. abneρtis faunule. Therefore， the faunule of conodonts from the Bt. 
Kalong is older than that from B. Kechi1 and belongs to the Middle to Late Trias-
sic period. 
References 
CLARK， D. L. (1959) : Conod0nts from the Triassic of Nevada and Utah. four. Paleont.， 33， p. 
305-312， pls. 44， 45. 
DIEBLE， K. (1956a) : Uber Trias-Conodonten. Geologie， 5， p. 9-12. 
(1956b) : Conodonten in der Oberkreide von Kameron. ibid.， 5， p. 424-450， pls. 1-4. 
HUCKRIEDE， R. (1958) : Die Conodonten der mediterranean Trias und ihr stratigraphischer 
Wert. Palaont. Z.， 32， p. 141-175， pls. 10-14. 
MULLER， K. ]. (1956) : Triassic conodonts from Nevada. four. Paleont.， 30， p.818-830， pls. 95， 
96. 
(1962) : Zur systemtischen Einteilung der Conodontphorida. Palaont. Z.， 36， p. 109-
117. 
TATGE， U. (1956) : Conodonten aus dem Germanischen Muschelkalk. Palaont. Z.， 30， p. 108-
127， 129-147， pls. 5， 6.
P.late 1 
-.98 
、
Explanation of Plate 1 
a1 specimens x about 25 
Fig. 1， 2. Gladigondolella tethydis (HUCKRIEDE) 
1. representative specimen from Bt. Kalong， loc. M16， a) upper view， b) 
oblique lateral view， c) lower view. 
2. small specimen from Bt. Kalong， loc. M16， a) oblique upper view， b) 
lateral view. 
Fig. 3-5. Gladigondolella cf. abneρtis (HUCKRIEDE) 
3. intermediate specimen between G. abneρtis and G. mungoensis， from Bt. 
Kechil， loc. M7， upper view. 
4. representative specimen from Bt. Kechil loc. M7， a) oblique upper view， 
b) lower view. 
5. smal1 specimen from Bt. Kechil loc. M7， a) lateral view， b) oblique 
lower view. 
Fig. 6-8. Gondolella navicula HUGKRIBJi)E 
6. advanced specimen from Bt. Kechi1 loc. M7， a) upper view， b) oblique 
lateral view， c) lower view. 
7. less advanced form from Bt. Kalong loc. M16， a) upper view， b) ob-
lique lateral view， c) lower view. 
8. primitive specimen from Bt. Kalong loc. M16， a) upper view， b) laterl 
view， c) oblique lower view. 
Fig. 9， 10. Sρathognathodus cf. cristagalli HUCKRIEDE 
9. from Bt. Kalong loc. M16， inner lateral view. 
10. from Bt. Kalong loc. M16， outer lateral view. 
Fig. 11. Ozarkodina saginata HUCKRIEDE 
from Bt. Kalong loc. M16， inner lateral view. 
Fig. 12. Neoρrioniodus cf. kochi (HUCKRIEDE) 
from Bt. Kalong loc. M16， inner lateral view. 
Fig. 13. "Hindeodella" triassica MULLER 
from Bt. Kalong loc. M16， inner lateral view. 
Fig. 14.“H indeodella "ρetrae-viridis HUCKRIEDE 
from Bt. Kalong loc. M16， outer lateral view. 
Fig. 15. D~ρlododella lautissima (HUCKRIEDE) 
representative form from Bt. Kechil loc. M7， a) inner view， b) lateral 
vlew. 
Fig. 16. Di，ρlododella n. sp. 
from Bt. Kalong loc. M16， a) upper view， b) oblique inner view. 
Fig. 17. Lonchodina mulleri TATGE 
from Bt. Kalong loc. M16， inner view. 
Photos NOGAMI 
K. 1 ~ 1 t 1 & Y. N ()(.Jヘ、11 : T r iassic Conodon ts f rom Mala ya Plate 1 


Discovery of Triassic Conodonts from the So-called Palaeozoic Limestone in Kedah, Malaya : Notes on the Geology and Palaeontology of Malaya-I

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Discovery of Triassic Conodonts from the So-called Palaeozoic Limestone in Kedah, Malaya : Notes on the Geology and Palaeontology of Malaya-I

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