NATURE | VOL 409 | 4 JANUARY 2001 | www.nature.com 53
articles
Dual origin of tribosphenic mammals
Zhe-Xi Luo*, Richard L. Cifelli² & Zo®a Kielan-Jaworowska³
*Section of Vertebrate Paleontology, Carnegie Museum of Natural History, Pittsburgh, Pennsylvania 15213, USA
² Oklahoma Museum of Natural History, 2401 Chautauqua, Norman, Oklahoma 73072, USA
³ Institute of Paleobiology, Polish Academy of Sciences, ulica Twarda 51/55, PL-00-818 Warszawa, Poland
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Marsupials, placentals and their close therian relatives possess complex (tribosphenic) molars that are capable of versatile
occlusal functions. This functional complex is widely thought to be a key to the early diversi®cation and evolutionary success of
extant therians and their close relatives (tribosphenidans). Long thought to have arisen on northern continents, tribosphenic
mammals have recently been reported from southern landmasses. The great age and advanced morphology of these new
mammals has led to the alternative suggestion of a Gondwanan origin for the group. Implicit in both biogeographic hypotheses is
the assumption that tribosphenic molars evolved only once in mammalian evolutionary history. Phylogenetic and morphometric
analyses including these newly discovered taxa suggest a different interpretation: that mammals with tribosphenic molars are not
monophyletic. Tribosphenic molars evolved independently in two ancient (holotherian) mammalian groups with different
geographic distributions during the Jurassic/Early Cretaceous: an australosphenidan clade endemic to Gondwanan landmasses,
survived by extant monotremes; and a boreosphenidan clade of Laurasian continents, including extant marsupials, placentals and
their relatives.
Because most mammals are only represented in the fossil record by
their teeth, dental evidence has prominently ®gured in interpreting
the relationships of early mammals. The highly distinctive tribo-
sphenic molars, capable of both shearing (sphen) and grinding
(tribein) occlusal functions, are the most important dental feature of
marsupials and placentals (extant therians) and their close fossil
relatives, collectively known as tribosphenidans
1
. The tribosphenic
molar has been used to distinguish these therians from other
Mesozoic mammals
1±4
, including stem holotherians such as ``sym-
metrodonts'' and ``eupantotheres''
3,4
, and from living monotremes.
The traditional view that tribosphenic molars arose in the Early
Cretaceous, and that the early diversi®cation of therians took place
on northern continents
5
, has been challenged by recent discoveries
on Gondwanan landmasses. Ambondro, from Madagascar, has fully
tribosphenic molars
6
yet is of Middle Jurassic age, and is therefore
some 25 Myr older than the earliest northern therians.
Ausktribosphenos, a tribosphenic mammal from the Early Creta-
ceous of Australia, is thought to have been a placental, possibly even
a member of the living hedgehog family
7,8
. Thus, these new fossils
have important implications for reconstructing the paleobiogeo-
graphy and timing of divergence of the main extant mammalian
groups. Here we re-evaluate the phylogenetic relationships of these
newly discovered mammals, with respect to other Mesozoic and
extant mammal groups.
Phylogenetic relationships
Parsimony analysis of the available evidence from the dentition and
mandible (Fig. 1; also see Methods) places the tribosphenic mam-
mals Ambondro
6
and Ausktribosphenos
7,8
, together with the earliest
known monotreme Steropodon
6
(Australia, Early Cretaceous), in a
monophyletic group, which we term the Australosphenida (concept
modi®ed from Ausktribosphenida
7
; see `Systematic Palaeontol-
ogy'). This group is characterized by a well-developed, continuous
mesial cingulid that wraps around and extends to the lingual side of
the trigonid (Fig. 2); a mesiodistally short, buccolingually broad
talonid; and reduced height of the trigonidÐat least when com-
pared with other Jurassic/Early Cretaceous holotherians. Notably,
Ausktribosphenos retains plesiomorphies of the jaw as seen in stem
mammals
9
, and we provisionally recognize some of these primitive
characters to be preserved also in Steropodon. By contrast, the
Boreosphenida, a clade of northern mammals with tribosphenic
molars
10±12
(Fig. 1), have distinctive cingulid cuspules (cuspule e,
cuspule f, or both) but lack a continuous mesial cingulid. The mesial
cingulid does not wrap around or extend to the lingual side of the
molars. Furthermore, boreosphenidans and proximal relatives, such
as Henkelotherium, are more derived in that they have a mandibular
angle far more posteriorly positioned than australosphenidans,
Kuehneotherium, morganucodontids and Sinoconodon.
Further dental apomorphies are consistent with the monophyly
of australosphenidans. For example, Steropodon
13
and
Ausktribosphenos
7
both have the `twinned' paraconid and metaco-
nid, and a well-developed lingual cusp on the talonid (Fig. 2).
Ambondro
6
and Ausktribosphenos
7,8
share an unusual feature in
which the premolars seem to be molariform, with a distinctive
triangulation of the three main cusps and a prominent lingual
cingulid. The posterior part of the premolar is buccolingually wide.
This derived feature is shared by Obdurodon dicksoni
14
(Australia,
Miocene), an ornithorhynchid monotreme
14,15
widely accepted to
be a relative of Steropodon (in which the premolar is not pre-
served
13
). None of these derived premolar features of fossil ornitho-
rhynchids, Ambondro and Ausktribosphenos is present in the earliest
known eutherians
10,11
, metatherians
12
, nor stem taxa of the
northern tribosphenidans
16±18
. They are also absent in a wide variety
of non-tribosphenic (eupantothere) mammals including Peramus
17
and Henkelotherium
18
.
Australosphenidans may have af®nities with the northern holo-
there Shuotherium
19±21
(Fig. 1), some unknown early ``symmetro-
donts''
9
, or the holotherian Dryolestidae
14
. However, by any
previous interpretation they are independent from boreospheni-
dans and their proximal relatives, including Henkelotherium
19
and
pre-tribosphenic Peramus
17,22
. The clade of Ausktribosphenos,
Ambondro and the monotreme Steropodon (Fig. 1), as inferred
from mandibular and postcanine tooth morphology, is consistent
with the phylogenies established by independent studies of
basicranial
23,24
and postcranial
25±27
features of the main Mesozoic
mammal groups documented by well-preserved fossils. In our
expanded analysis (Fig. 1b), we added the cranial and postcranial
features for those better-preserved taxa (for example,
Morganucodon, Jeholodens and Henkelotherium). The simultaneous
analysis (Fig. 1b) of cranial and postcranial data, together with the
dental and mandibular characters, corroborates the australosphe-
nidan clade and the boreosphenidan clade. Hence, the hypothesis of
a diphyletic origin for tribosphenic mammals is supported by
morphological characteristics other than teeth and mandibles.
Independent multivariate analysis of the shape of the lower molar
shows that Ausktribosphenos and Steropodon are grouped together
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