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The Largest Asiatic Amphechinus (Erinaceidae, Insectivora, Mammalia) from the Oligocene of Mongolia

Authors:
  • Borissiak Paleontological Institute of the Russian Academy of Sciences

Abstract

A lower jaw fragment of a new hedgehog species, Amphechinus gigas sp. nov., from the Oligocene Shand-Gol Formation of Mongolia is described. This species is substantially larger than A. rectus, A. akespensis and other known Amphechinus species from Asia and comparable in size to the European species A. robustus, A. ginsburgi, and A. intermedius. Regarding the length of the lower cheek tooth row, A. gigas is comparable to Recent Erinaceus europaeus; however, the much deeper and more massive horizontal ramus of the dentary shows that A. gigas is larger than the latter.
302
Paleontological Journal, Vol. 36, No. 3, 2002, pp. 302–306. Translated from Paleontologicheskii Zhurnal, No. 3, 2002, pp. 75–80.
Original Russian Text Copyright © 2002 by Lopatin.
English Translation Copyright © 2002 by
åÄIä “Nauka
/Interperiodica” (Russia).
INTRODUCTION
Amphechinus
belongs to the earliest genera of the
subfamily Erinaceinae. This genus was widespread in
the Oligocene and Miocene of Eurasia and occurred in
the Miocene of North America and Africa (Gureev,
1979; Gould, 1995). The following six species were
described from Asia: Oligocene
A. rectus
(Matthew et
Granger, 1924),
A. kansuensis
(Bohlin, 1942), and
A. minimus
(Bohlin, 1942) from China and Mongolia;
Early Miocene
A. akespensis
Lopatin, 1999 and
A. microdus
Lopatin, 1999 from Kazakhstan; and Early
Miocene
A. bohlini
Bi, 2000 from China (Matthew and
Granger, 1924; Bohlin, 1942; Trofimov, 1960; Mellett,
1968; Sulimski, 1970; Huang, 1984; Lopatin, 1999; Bi,
2000).
A. minimus
and
A. microdus
are small, i.e., com-
parable in size to living
Sorex araneus
L.
A. kansuensis
and
A. bohlini
are somewhat larger.
A. rectus
and
A. akespensis
are only slightly smaller than
Erinaceus
europaeus
L. Late Oligocene
A. arvernensis
(Blain-
ville, 1839) and Early Miocene
A. edvardsi
(Filhol,
1879) from Europe are of approximately the same size.
Certain European species of
Amphechinus
, i.e., Oli-
gocene
A. robustus
(Lavocat, 1951); Middle Miocene
A. ginsburgi
Baudelot, 1972; and
A. intermedius
(Gail-
lard, 1899) are as large as Recent
Erinaceus europaeus.
Postpalerinaceus vireti
(Crusafont Pairo et Villalta, 1947)
from the Pliocene of Spain is larger than all the above-
listed species. Crusafont Pairo and Villalta (1947) and
Gould (1995) assigned
P. vireti
to the genus
Amphechi-
nus
(=
Palaeoerinaceus, Palerinaceus
), whereas Gureev
(1979) assigned it to a particular subgenus of the genus
Erinaceus
.
The present study describes a new species of the
genus
Amphechinus
from the Lower Oligocene of
Mongolia. Regarding the tooth measurements, the new
species is comparable to
A. robustus, A. ginsburgi,
A. intermedius, Postpalerinaceus vireti
, and
Erinaceus
europaeus
; at the same time, its lower jaw is substan-
tially larger and more massive than those of the listed
species. The fragmentary lower jaw of the new species
was found together with
A. rectus
and
A.
cf.
kansuensis.
The Largest Asiatic
Amphechinus
(Erinaceidae, Insectivora,
Mammalia) from the Oligocene of Mongolia
A. V. Lopatin
Paleontological Institute, Russian Academy of Sciences, Profsoyuznaya ul. 123, Moscow, 117997 Russia
e-mail: alopat@paleo.ru
Received October 26, 2000
Abstract
—A lower jaw fragment of a new hedgehog species,
Amphechinus gigas
sp. nov., from the Oligocene
Shand-Gol Formation of Mongolia is described. This species is substantially larger than
A. rectus, A. akespensis
,
and other known
Amphechinus
species from Asia and comparable in size to the European species
A. robustus,
A. ginsburgi
, and
A. intermedius.
Regarding the length of the lower cheek tooth row,
A. gigas
is comparable to
Recent
Erinaceus europaeus
; however, the much deeper and more massive horizontal ramus of the dentary
shows that
A. gigas
is larger than the latter.
(a)
(b)
(c)
10 mm0
Fig. 1.
Amphechinus gigas
sp. nov., holotype PIN,
no. 4567/14, fragmentary right dentary containing P
4
–M
2
:
(a) labial, (b) occlusal, and (c) lingual views.
PALEONTOLOGICAL JOURNAL
Vol. 36
No. 3
2002
THE LARGEST ASIATIC
AMPHECHINUS
(ERINACEIDAE, INSECTIVORA, MAMMALIA) 303
The material comes from the Shand-Gol Formation.
The specimens were found in a bed located 10–15 m
above a basalt layer in the eastern slope of the Khunuk
Valley, opposite to the Menkhen-Teg locality in the Val-
ley of Lakes (collected by E.V. Devyatkin and I.G. Liskun,
1972). The material on
A. rectus
from several Shand-
Gol localities (Ulan-Khurekh 1, collected by V.Yu. Reshe-
tov in 1979; Tsagan-Obo 3 and Elste-Turamne-Ar, col-
lected by E.K. Sytchevskaya in 1993 and 1995) and
specimen PIN, no. 475/1200 from the Tatal-Gol local-
ity, described by Trofimov (1960), were used for com-
parison.
The following abbreviations are used in this paper:
(PIN) Paleontological Institute of the Russian Academy
of Sciences, Moscow, and (IVPP) Institute of Verte-
brate Paleontology and Paleoanthropology, Beijing.
SYSTEMATIC PALEONTOLOGY
Family Erinaceidae Fischer, 1817
Subfamily Erinaceinae Fischer, 1817
Tribe Amphechinini Gureev, 1979
Genus
Amphechinus
Aymard, 1850
Amphechinus gigas
Lopatin, sp. nov.
Amphechinus
cf.
rectus
: Huang, 1984, p. 308, pl. I, fig. 12.
Etymology. From the Greek
gigas
(giant).
Holotype. PIN, no. 4567/14, fragmentary right
dentary containing P
4
–M
2
; Mongolia, Khunuk locality;
Lower Oligocene, Shand-Gol Formation.
Description (Figs. 1, 2, and 3a). A large hedge-
hog, P
4
–M
3
is approximately 15 mm long, and M
1
–M
3
is approximately 12 mm long. The horizontal ramus of
the lower jaw is deep and massive. The large mental
foramen is on a level with the posterior root of P
4
. The
I
2
is stout. Judging by the preserved alveoli, the canine
was larger than the anterior premolar.
P
4
has a weakly developed posterior cingulid. The
paraconid is somewhat higher than the protoconid. The
protoconid is noticeably posteriorly inclined. Meta-
conid is absent, the lingual wall of the protoconid is
almost straight, flat, and only slightly inflated at the
base. The talonid is very short but broad, broader than
the trigonid.
M
1
is large and long, the trigonid is more than two-
thirds as long as the entire M
1
. The labial cingulid is
well developed and broad, the postcingulid is
extremely weak. The paraconid is large and massive.
The paralophid is long and has a weak notch. The pro-
toconid is substantially more massive and higher than
the metaconid. The metalophid notch looks like a small
depression between the apices of the protoconid and the
metaconid. The metastylid is undeveloped. The talonid
is substantially shorter than the trigonid, but it is of the
same width. The entoconid is higher than the hypo-
conid, strongly longitudinally compressed, and extends
anteriorly to form a relatively high and straight entoc-
ristid, which encloses lingually the talonid basin. The
cristid oblique connects the hypoconid to the middle of
the posterior base of the protoconid. The metalophid
and the posterolophid curve posteriorly; the entocristid
and the cristid oblique extend almost in parallel to the
longitudinal tooth axis.
M
2
is almost 1.5 times shorter than M
1
. The trigonid
is slightly broader and 1.7 times longer than the talonid.
M
2
is similar to M
1
in structural pattern, but differs in
certain features, i.e., the paralophid is shortened, the
metaconid is reduced to a lesser extent, and the meta-
stylid looks like a weak projection.
M
3
is represented by the anterior root located in the
alveolus and by the anterior wall of the alveolus of the
posterior root. Judging from the arrangement and mea-
surements of these structures, M
3
was at most half as
long as M
2
.
Measurements, mm. Holotype: length of P
4
–M
2
is 12.6; length of M
1
–M
2
, 9.7; length
×
width: (P
4
) 3.2
×
2.1; (M
1
) 5.8
×
3.1 (trigonid, 4.0
×
3.1; talonid, 1.8
×
3.1); and (M
2
) 4.0
×
2.75 (trigonid, 2.5
×
2.75; talonid,
1.5
×
2.45); dentary depth at P
4
and M
1
, 8.0; at M
2
, 8.2;
and at M
3
, 7.7; dentary thickness at P
4
, 4.9; at M
1
, 4.3;
and at M
2
, 4.2.
Comparison.
A. gigas
sp. nov. differs from all
known species of the genus by very large measure-
ments (table) and extremely massive lower jaw. In
(a)
(b)
05 mm
Fig. 2.
Amphechinus gigas
sp. nov., holotype PIN,
no. 4567/14, fragmentary right dentary containing P
4
–M
2
:
(a) labial, (b) occlusal, and (c) lingual views.
(c)
304
PALEONTOLOGICAL JOURNAL
Vol. 36
No. 3
2002
LOPATIN
addition, it differs from the majority of species by the
structure of P
4
(in which the paraconid is higher than
the protoconid and metaconid is absent) and by the
presence of double-rooted M
3
. The new species differs
from the most similar species from Asia (
A. rectus
and
A. akespensis) by the absence of metaconid on P4 and
certain structural details of the lower molars, in partic-
ular, weak postcingulids of M1 and M2 and the absence
of metastylid on M1.
Remarks. Judging from the measurements
(5.9 mm long and 3.3 mm wide) and structure, the
large M1 (specimen IVPP, no. V7340) from the Ulan-
tatal locality of China, which was initially determined
as A. cf. rectus (Huang, 1984), actually belongs to
A. gigas.
Occurrence. Lower Oligocene of Mongolia and
China.
Material. Holotype.
DISCUSSION
The Recent Erinaceidae are divisible into three
groups by measurements: small, in which the body is
10–15 cm long and the skull is 30–40 mm long;
medium-sized, the body is 15–30 cm long, the skull is
41–63 mm long; and large forms, the body is 31–45 cm
long and the skull is 60–87 mm long. The first group
comprises the shrew-hedgehogs Hylomys (including
Neotetracus and Neohylomys) and Podogymnura, the
second comprises the true hedgehogs Hemiechinus,
Paraechinus, and Erinaceus (including Atelerix and
Mesechinus), and the third includes the gymnura Echi-
nosorex gymnurus. The largest member of true hedge-
hogs (Erinaceinae) is the European hedgehog Erina-
ceus europaeus (Gureev, 1979), the body of which is
19.5–30 cm long, and the skull is 43–63 mm long.
Extinct hedgehogs include certain giant insecti-
vores. In particular, the skull of Deinogalerix koenig-
swaldi Freudenthal, 1972 from the Late Miocene of
Italy (Gargano) is 210–223 mm long (Freudenthal, 1972).
Judging from the reconstructed skeleton, the body of
this shrew-hedgehog was approximately 60–70 cm
long. Quite apparently, this is an exception accounted
for by the insular giantism (Guérin, 1997); in general,
extinct hedgehogs that are comparable in size to Erina-
ceus europaeus should be regarded as large erinaceids.
Only a small number of such forms occurred in the Oli-
gocene and Miocene of Eurasia; these were mainly the
Measurements of teeth and lower jaws of large-sized hedgehog species (Amphechinus, Postpalerinaceus, and Erinaceus)
Species Reference P4–M3P4–M2M1–M3M1–M2P4M1M2M2/M1
Jaw depth
under
P4–M1
A. rectus Huang, 1984 7.5–8.1 – 1.4–2.5 3.7–4.4 2.4–3.2 0.62–0.74 3.9–5.1
PIN,
no. 475/1200 11.5 9.9 9.0 7.3 2.6 4.4 3.3 0.75 6.6
PIN,
no. 4567/12 about
12.0 about
10.0 9.7 7.5 4.7 3.3 0.70 6.6
A. akes-
pensis Lopatin, 1999 10.5 2.8 4.7–4.8 3.5 0.73 6.5
A. arver-
nensis Baudelot, 1972 11.2 9.0 – 2.4 4.4 3.4 0.79 6.03
Ziegler, 1998 ––––2.62–2.98 3.93–4.38 2.9–3.54 0.74–0.81 4.05–5.25
A. edwardsi Baudelot, 1972 11.2 9.0 – 2.8 4.4 3.2 0.75 5.7–6.0
Ziegler, 1990 – – –2.6–3.15 4.01–5.0 3.32–3.61 – –
A. gigas holotype about
15.0 12.6 about
12.0 9.7 3.2 5.8 4.0 0.69 8.0
Huang, 1984 – – – – – 5.9 – –
A. robustus Lavocat, 1951 12.0 10.0–11.0 9.0 2.7 4.95 3.9 0.79 6.1
Ziegler, 1990 2.75 – 3.53
Ziegler, 1998 4.11–4.35 5.4–6.2 4.17–4.8 0.77 6.0–6.9
A. gins-
burgi Baudelot, 1972 14.6–14.9 11.3–11.5 3.2–3.47 5.2–5.34 4.38 0.82 6.2–7.0
A. inter-
medius Baudelot, 1972 15.0 11.5 – 3.8 5.5 4.5 0.86 7.0
P. vireti Baudelot, 1972 3.52–3.84 5.52–6.04 4.6–5.3 0.85 7.2
E. europaeus collection PIN 15.0–15.3 12.7–13.5 12.3–12.4 10.0–10.3 3.5 5.5–5.9 4.5–4.9 0.81–0.83 5.4–5.9
PALEONTOLOGICAL JOURNAL Vol. 36 No. 3 2002
THE LARGEST ASIATIC AMPHECHINUS (ERINACEIDAE, INSECTIVORA, MAMMALIA) 305
above-mentioned species of the genus Amphechinus.
Certain members of the Brachyericinae also reach rela-
tively large sizes; in particular, the skull of Late Oli-
gocene Metexallerix gaolanshanensis Qiu et Gu, 1988
from China is approximately 50 mm long (Qiu and Gu,
1988).
The table shows the tooth measurements of large-
sized species of Amphechinus and proper hedgehogs.
The teeth of Amphechinus are relatively small and the
horizontal ramus of the lower jaw is relatively deeper
and more massive than those of Erinaceus (Fig. 3);
therefore, it is impossible to perform direct compari-
sons of sizes between the members of these genera.
Based on the ratios between the lengths of the lower
tooth row (table), lower jaw, and skull in certain
European species of the genus Amphechinus (the skulls
of A. arvernensis and A. edwardsi are approximately
35 mm long), it is possible to estimate the measure-
ments of the species from Asia as follows: the skulls of
A. minimus and A. microdus are approximately 20 mm
long, those of A. kansuensis and A. bohlini are about
25 mm long, those of A. rectus and A. akespensis are
about 30–45 mm long, and those of A. gigas are about
55–60 mm long.
To date, the following species of the family Erina-
ceidae have been found in the Shand-Gol Fauna of
Mongolia and northern China: Tupaiodon morrisi and
Zaraalestes minutus (Tupaiodontinae); Exallerix hsan-
dagolensis (Brachyericinae); and Palaeoscaptor acri-
dens, Amphechinus rectus, and A. cf. minimus (Erinace-
inae) (Matthew and Granger, 1924; Trofimov, 1960;
McKenna and Holton, 1967; Mellett, 1968; Sulimski,
1970; Huang, 1984). Taking into account the prelimi-
nary study of the Oligocene Erinaceidae from Mongo-
lia stored at the PIN, the number of Amphechinus spe-
cies recorded in the Shand-Gol Fauna increases by
four; these are A. cf. minimus, A. cf. kansuensis, A. rec-
tus, and A. gigas. These species are well distinguished
from each other not only by the dental structure but also
by the measurements. This fact is evidence of adaptive
radiation of Oligocene Amphechinus and explains the
presence of a large number of sympatric species of the
same genus in Central Asia. As far as is known (Bohlin,
1942; Bendukidze, 1993; Lopatin, 1999; Meng et al.,
1999; Bi, 2000), the differentiation in size of the
Amphechinus species remained in Asia at the end of the
Late Oligocene (A. minimus, A. kansuensis, and A. cf.
rectus) and early in the Miocene (A. microdus, A. bohlini,
and A. akespensis); however, the species comparable in
size to A. gigas have not been recorded in the deposits
of this age.
ACKNOWLEDGMENTS
This study was supported by the Russian Founda-
tion for Basic Research, project nos. 98-04-49089,
99-04-48636, and 00-15-97754.
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... Godina, I.A. Vislobokova). A series of monographs (Shevyreva, 1976;Dmitrieva, 1977;Zhegallo, 1978;Godina, 1979;Vislobokova, 1983Vislobokova, , 1990Vislobokova and Trofimov, 2002;Lopatin, 2006a;Vislobokova, 2012) and numerous articles were published (Alexeeva, 1971;Beliajeva, 1971Beliajeva, , 1974Beliajeva, , 1975Godina, 1971Godina, , 1974Godina, , 1975Godina, , 1981Godina, , 1994Dashzeveg, 1971Dashzeveg, , 1974Dashzeveg, , 1975aDashzeveg, , 1975bDashzeveg, , 1976aDashzeveg, , 1976cDashzeveg, , 1985Dmitrieva, 1971Dmitrieva, , 1974aDmitrieva, , 1974bDmitrieva, , 1975Dmitrieva, , 2002Dmitrieva, , 2007Zhegallo, 1971;Shevyreva, 1971Shevyreva, , 1972Shevyreva, , 1974Dashzeveg, 1974, 1988;Dubrovo, 1974Dubrovo, , 1976Janovskaja, 1976;Kurochkin and Dashzeveg, 1979;Vislobokova, 1979Vislobokova, , 1998Vislobokova, , 2001Sotnikova, 1979Sotnikova, , 1980Sotnikova, , 1994Sotnikova, , 2006Borissoglebskaya, 1981;Erbajeva, 1981Erbajeva, , 2013Trofimov, 1981;Zazhigin, 1989;Lange-Badré, Dashzeveg, 1989;Spassov, Lange-Badré, 1995;Lopatin, 1997Lopatin, , 2002aLopatin, , 2002bLopatin, , 2003cLopatin, , 2005aLopatin, , 2018Lavrov, 1999;Vislobokova and Trofimov, 2000;Zazhigin and Lopatin, 2000a, 2000bZazhigin, 2000, 2003;Zazhigin et al., 2002;Minjin, 2004;Wang and Dashzeveg, 2005;Baryshnikov and Lavrov, 2015;Zazhigin and Voyta, 2018). ...
... Additional taxa described from the Lower Oligocene part of the Shand-Gol Formation are the erinaceids Tupaiodon morrisi Matthew et Granger, 1924, Exallerix hsandagolensis McKenna et Holton, 1967 from Shand-Gol locality, E. manahan Lopatin et Zazhigin, 2003 from Tatal-Gol locality, Amphechinus gigas Lopatin, 2002 from Khunuk locality and Scymnerix tartareus from Ulan-Khureh locality, the talpoid Oligoscalops sp. (Proscalopidae) from Tatal-Gol locality, the didymoconid Archaeomangus ulanhureensis Lopatin, 1997 (Didymoconidae) from Ulan-Khureh locality, the giant rhinoceros Indricotherium transouralicum Pavlova, 1922(=Baluchitherium grangeri Osborn, 1923 from Shand-Gol locality, the rhinoceros Allacerops minor Beliajeva, 1954 from Ulan-Ganga locality (McKenna and Holton, 1967;Borsuk-Białynicka, 1969;Lopatin, 1997Lopatin, , 2002aLopatin, , 2003cLopatin and Zazhigin, 2003;Geisler, 2004 Kowalski, 1974), Tataromys minor longidens Schmidt-Kittler, Vianey-Liaud et Marivaux, 2007, T. plicidens Matthew et Granger, 1923, and Tsaganomys altaicus (Tsaganomyidae), the bovid Palaeohypsodontus asiaticus Trofimov, 1957(Trofimov, 1957Daxner-Hock et al., 2017;López-Guerrero et al., 2017b;Maridet et al., 2017). ...
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In Mongolia, fossil mammals are known from the Upper Jurassic, Lower and Upper Cretaceous, all series of the Paleogene and Neogene, as well as the Pleistocene. Over 335 new species and more than 185 new genera of fossil mammals (not including synonyms) were described from Mongolia up to the end of 2019. The most important results in the last hundred years of research, that most strongly influenced the development of mammal paleontology, have been: (1) the discoveries of extremely rich Paleogene and Neogene localities containing numerous fossils of various mammals by the Central Asian Expedition of the American Museum of Natural History (CAE AMNH) in 1922–1930, and subsequent expeditions; (2) the discovery and further study of the Late Cretaceous mammalian fauna by the CAE AMNH and the Mongolian Paleontological Expedition of the Academy of Sciences of the USSR (1946–1949), the Polish Mongolian Paleontological Expedition (1963–1971) and the Joint Soviet-Mongolian (Russian-Mongolian) Paleontological Expedition (JSMPE, JRMPE); (3) the discovery by the JSMPE in the late 1960s early 1970s of the Early Cretaceous Höövör mammalian fauna, at the time of its discovery the most diverse and richest in Asia; (4) the obtaining by the JSMPE of a large amount of data on the early Paleogene, the most important stage in the evolution of mammals; (5) detailed biostratigraphic study of the Oligocene and the Lower Miocene mammal fossils of the Valley of Lakes, as part of the Austrian-Mongolian project (1995–2018).
... Palaeoscaptor gigas was originally described as a species of Amphechinus by Lopatin (2002), based on a mandible with p4-m2 from the lower Oligocene of the Shand-Gol Formation (Mongolia). Ziegler et al. (2007) reported additional material from Taatsiin Gol, and gave measurements for a P2 they assigned to this species. ...
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The Kargil Formation in the region of Ladakh (northern India) is known for its late Oligocene mammal fauna of both large mammals and rodents. New excavation in the area yielded a maxillary fragment of an insectivore with three premolars and two roots of a canine. The fossil record of the insectivores on the Indian subcontinent is as yet scanty. Based on the peculiar morphology of the last premolar, the Ladakh fossil could be identified as belonging to a new species of Erinaceinae, Ladakhechinus iugummontis n. gen. n. sp. The new find confirms the large diversity among hedgehogs in Asia during the Oligocene.
... This statement may be somewhat misleading since the Galericini apparently experienced an ecological radiation during the Miocene, resulting in eco-morphologically varied species (Van den Hoek Ostende, 2001, 2018 and locations in environments that do not correspond to tropical or sub-tropical zones (Luis and Hernando, 2000;Van den Hoek Ostende, 2003b;Van den Hoek Ostende and Doukas, 2003;Furió et al., 2011aFurió et al., , 2011b. Finally, several groups of Erinaceidae dispersed to North America in the latest Oligocene and early Miocene, viz. the Amphechinini, a group yet widespread throughout the Oligocene in Eurasia (Rich and Rasmusen, 1971;Rich, 1981;Lopatin, 2002;Ziegler, 2005b;Ziegler et al., 2007), the Brachyericinae, and the Erinaceini (Stevens, 1977;Rich, 1981;Lopatin and Zazhigin, 2003). Therefore, it is necessary to consider the possibility that Asian representatives of Lantanotherium have joined one of these waves of migration through Beringia, presumably during the early Miocene. ...
Article
The Galericinae are a group of Erinaceidae that are currently distributed in Southeast and Eastern Asia. Although galericines have an Asian origin, their fossil record in this region is scarce, which greatly limits the knowledge of the evolutionary history of this group. We describe here the first fossils of Eulipotyphla from the middle Miocene (13.4-13.2 Ma) of the Mae Moh Basin of northern Thailand, and assign the material to three taxa of Erinaceidae attributable to the Galericinae (Galerix rutlandae, Lantanotherium anthrace, sp. nov., and Lantanotherium sp.). The Mae Moh erinaceids present a Lantanotherium-Galerix association that is uncommon in the Miocene of Asia. Galerix rutlandae is a species formerly described in the Siwaliks of Pakistan and India, which reaffirms the strong affinities during the middle Miocene between the mammalian faunas of Southeast and Southern Asia. The discovery of two species of Lantanotherium in Mae Moh provides additional knowledge about the evolution in Asia of this widespread Miocene genus that had never been recorded in Southeast Asia. The presence of three Galericinae in Mae Moh Basin reinforces the hypothesis of a mainly closed and wet environment during the deposition of the K and Q lignite layers.
... Eight genera and about 15 species of the family Erinaceidae have been described from the Oligocene of Asia. They represent four subfamilies: Tupaiodontinae, Galericinae, Brachyericinae, and Erinaceinae (see Matthew and Granger, 1924;Bohlin, 1942;Trofimov, 1960;McKenna and Holton, 1967;Sulimski, 1970;Huang, 1982;Qiu and Gu, 1988;Lopatin, 1999Lopatin, , 2002Lopatin, , 2003bLopatin, , 2003cLopatin and Zazhigin, 2003). The Eocene Erinaceidae are much more poorly understood. ...
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Two members of the family Erinaceidae, Oligochenus grandis gen. et sp. nov. (Galericinae) and Amphechinus sp. (Erinaceinae) from the Ergilin Dzo locality (Mongolia; Sevkhul Member, Ergilin Dzo Formation, uppermost Eocene) are described. Oligochenus is similar in the structure of P 4 and M 1 to the Middle Eocene Eochenus and Eogalericius and differs in the absence of P 1 and the strongly reduced P 2. Amphechinus sp. from the Ergilin Dzo locality is the earliest known Erinaceinae. Remains of Tupaiodontinae indet. were found in the Lower Oligocene Ergilin Member.
... To date, nine erinaceid species have been discovered in the Early Oligocene Shandgolian Fauna of Central Asia (Matthew and Granger, 1924;Trofimov, 1960;McKenna and Holton, 1967;Mellett, 1968;Sulimski, 1970;Huang, 1984;Storch and Dashzeveg, 1997;Lopatin, 2002;Lopatin and Zazhigin, 2003). They include two species of the subfamily Tupaiodontinae, i.e., Tupaiodon morrisi Matthew et Granger, 1924 and Zaraalestes minutus (Matthew et Granger, 1924) [= Ictopidium tatalgolensis Sulimski, 1970], and two species of the subfamily Brachyericinae, Exallerix hsandagolensis McKenna et Holton, 1967 andE. ...
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On the basis of an almost complete skull with the lower jaw from the Oligocene Shand-Gol Formation of the Ulan-Khureh locality in Mongolia, a new erinaceid genus and species, Scymnerix tartareus, is described. This is a small hedgehog whose skull is approximately 3 cm long. Scymnerix shows convergent similarity to short-faced hedgehogs (Brachyericinae) in certain cranial and dental traits, such as the shortened facial region of the skull, high and raised posterior part of the zygomatic arch, single-rooted I3, the absence of M3, the structure of P4-M2, strongly enlarged I2, and the presence of enamel sculpture on the labial surface of teeth. However, the basicranium structure of Scymnerix suggests that it should be referred to true hedgehogs (Erinaceinae). Structural cranial and dental features of Scymnerix clearly distinguish it from both Amphechinini and Erinaceini and enable one to rank this genus as a separate tribe, Scymnericini tr. nov.
... It should be pointed out that each species of the Asian Brachyericinae coexisted with true hedgehogs (from the subfamily Erinaceinae) of approximately the same size, which showed insectivorous and euryphagous feeding adaptation. For example, in addition to Exallerix hsandagolensis and E. manahan, the Shand-Gol Fauna includes four species of the genus Amphechinus, in particular, large-sized A. rectus (Matthew et Granger, 1924) and A. gigas Lopatin, 2002 (Matthew andGranger, 1924;Trofimov, 1960;Sulimski, 1970;Huang, 1984;Lopatin, 2002). In addition to Exallerix efialtes, the Erinaceidae from the Early Miocene Aral Fauna are represented by three species of Amphechinus, including relatively large A. akespensis Lopatin, 1999(Lopatin, 1999. ...
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Four new taxa of the subfamily Brachyericinae, Exallerix manahan sp. nov. (Lower Oligocene of Mongolia), Synexallerix otus gen. et sp. nov. (Lower Miocene of eastern Kazakhstan), Postexallerix securis gen. et sp. nov. (Lower Miocene of Mongolia), and P. mustelidens sp. nov. (Middle Miocene of Mongolia) are described. E. manahan is similar in size and dental structure to Late Oligocene Metexallerix gaolanshanensis Qiu et Gu, 1988 from China; therefore, the latter species is transferred to the genus Exallerix, and Metexallerix is regarded as a junior synonym of Exallerix. "Metexallerix" junggarensis Bi, 1999 from the Lower Miocene of China is considered to be the type species of Synexallerix. The genus Synexallerix is proposed to be very similar to the ancestor of Miocene North American Brachyerix and Metechinus. The genus Postexallerix comprises the latest and most specialized Asian Brachyericinae characterized by a very narrow and long trigonid of M 1 and by a strongly reduced M 2. Phylogenetic relationships and adaptations of the Brachyericinae are discussed.
... In the previous studies, the presence of two insectivore families, the Erinaceidae (Tupaiodontinae, Brachyericinae, and Erinaceinae) and the Heterosoricidae, was recorded in the Oligocene Shand Gol Fauna of Central Asia (Matthew and Granger, 1924;Trofimov, 1960;McKenna and Holton, 1967;Mellett, 1968;Sulimski, 1970;Huang, 1984;Russell and Zhai, 1987;Lopatin, 2002). In the present study, the first find of the Talpidae from the Shand Gol Formation of Mongolia is described. ...
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A new mole, Mongoloscapter zhegalloi gen. et sp. nov. (Talpinae, Scaptonychini), is described on the basis of a fragmentary lower jaw from the upper part of the Shand Gol Formation of the Tatsin Gol locality. This is the first record of the Talpidae from the Oligocene of Mongolia.
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Cenozoic sediments of the Taatsiin Gol and TaatsiinTsagaan Nuur area are rich in fossils that provide unique evidence of mammal evolution in Mongolia. The strata are intercalated with basalt flows. ⁴⁰Ar/³⁹Ar data of the basalts frame the time of sediment deposition and mammal evolution and enable a composite age chronology for the studied area. We investigated 20 geological sections and 6 fossil localities of Oligocene and early Miocene deposits from this region. Seventy fossil beds yielded more than 19,000 mammal fossils. This huge collection encompasses 175 mammal species: 50% Rodentia, 13% Eulipotyphla and Didelphomorphia, and 12% Lagomorpha. The remaining 25% of species are distributed among herbivorous and carnivorous large mammals. The representation of lower vertebrates and gastropods is comparatively poor. Several hundred SEM images illustrate the diversity of Marsupialia, Eulipotyphla, and Rodentia dentition and give insight into small mammal evolution in Mongolia during the Oligocene and early Miocene. This dataset, the radiometric ages of basalt I (∼31.5 Ma) and basalt II (∼27 Ma), and the magnetostratigraphic data provide ages of mammal assemblages and time ranges of the Mongolian biozones: letter zone A ranges from ∼33 to ∼31.5 Ma, letter zone B from ∼31.5 to ∼28 Ma, letter zone C from ∼28 to 25.6 Ma, letter zone C1 from 25.6 to 24 Ma, letter zone C1-D from 24 to ∼23 Ma, and letter zone D from ∼23 to ∼21 Ma. Electronic supplementary material The online version of this article (doi:10.1007/s12549-016-0257-9) contains supplementary material, which is available to authorized users.
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The Aral Faunal Assemblage is rich in small mammals. Insectivores there include the hedgehogs Galerix sp., Exallerix efialtes Lopatin, Amphechinus akespensis Lopatin, A. microdus Lopatin, and Amphechinus sp.; the moles Desmanella compacta sp. nov., Pseudoparatalpa lavrovi (Bendukidze), Myxomygale asiaprima sp. nov., and Hugueneya sp.; and the soricids Gobisorex akhmetievi sp. nov., Atasorex edax gen. et sp. nov., and Aralosorex kalini Lopatin. Lagomorphs are represented by Desmatolagus simplex (Argyropulo), D. periaralicus Lopatin, D. veletus Lopatin (Desmatolagidae), and Sinolagomys pachygnathus Li et Qiu (Ochotonidae). Rodents are very diverse and include the aplodontids Prosciurus daxnerae Lopatin and Ansomys crucifer Lopatin; the beavers Steneofiber kumbulakensis (Lytschev), S. schokensis (Bendukidze), and Asiacastor sp.; the eomyids Eomyodon bolligeri Lopatin and Pseudotheridomys yanshini Lopatin; the zapodids Plesiosminthus tereskentensis Lopatin, Parasminthus debruijni Lopatin, and Bohlinosminthus cubitalus Lopatin; the cricetids Eucricetodon occasionalis Lopatin, Eumyarion tremulus Lopatin, Eumyarion sp., and Aralocricetodon schokensis Bendukidze; the primitive mole rat Argyromys aralensis (Argyropulo); the tachyoryctoidids Tachyoryctoides glikmani (Vorontzov), Tachyoryctoides sp., Aralomys gigas Argyropulo, and Eumysodon spurius Argyropulo; and the ctenodactylid Yindirtemys birgeri Bendukidze. Based on taxonomic composition, the assemblage is dated as the beginning of the Miocene (Early Aquitanian) and compared to the MN 1 European Mammal Zone. It is proposed to consider the Aral biochron as the reference level NMU 1, that is, the basal unit of the biochronological scale of the Neogene of inner Asia, which corresponds to the earliest phase of the Xiejian Asian Land Mammal Age (Earliest Xiejian or Aralian).
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Kurzfassung Die Didelphiden und Insektivoren von Herrlingen 8 (Niveau von Pech du Fraysse, MP 28) und von Herrlingen 9 (Niveau von Rickenbach, MP 29) werden vorgestellt und deren Beziehungen zu Faunen ähnlichen Alters werden diskutiert. Unter den Soriciden werden drei neue Arten beschrieben:Quercysorex ulmensis n. sp.,Srinitium caeruleum n. sp. undUlmensia antecedens n. sp. Die Didelphiden- und Insectivorenfaunen gestatten die Einstufung in das jüngere Oberoligozän. Die Fauna von Herrlingen 8 enthält mehr Formen eines bewaldeten Habitats.
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Deinogalerix koenigswaldi nov. gen., nov. spec. is the largest insectivore known so far. It is represented by an almost complete skeleton and a good number of isolated teeth and bones. These prove a considerable sexual dimorphism. It is supposed that these animals were scavengers. The time-range of Deinogalerix is within the Upper Miocene.