News and Views
The smallest primates
Daniel L. Gebo
Department of Anthropology, Northern Illinois University, DeKalb,
IL 60115, U.S.A. E-mail: dgebo@niu.edu
Marian Dagosto
Department of Cell and Molecular Biology, Northwestern University
Medical School, Chicago, IL 60611, U.S.A. E-mail:
m-dagosto@nwu.edu
K. Christopher
Beard
Section of Vertebrate Paleontology, Carnegie Museum of Natural
History, Pittsburgh, PA 15213, U.S.A. E-mail:
Eosimias@alphaclp.clpgh.org
Tao Qi
Institute of Vertebrate Paleontology and Paleoanthropology,
Chinese Academy of Sciences, P.O. Box 643, Beijing, 100044,
People’s Republic of China
Journal of Human Evolution (2000) 38, 585–594
doi:10.1006/jhev.2000.0395
Available online at http://www.idealibrary.com on
Among living members of the Order Primates, taxa weighing less than 50 g are
extremely rare (Jungers, 1985; Atsalis et al.,
1996). Moreover, all living species of primates in this small size range are members
of the Malagasy radiation of strepsirhines
(Genus: Microcebus; Atsalis et al., 1996).
This was not the case, however, for the
diverse primate fauna from the middle
Eocene Shanghuang fissure-fillings of southern Jiangsu Province, China (Beard et al.,
1994). Primate postcranial elements
from the Shanghuang fissure-fillings show
that a diversity of tiny haplorhine primates
(about six species) inhabited eastern
China during the middle Eocene. Among
these diminutive Chinese taxa are two
species that considerably extend the known
size range of primates. The distribution of
body mass for the entire Shanghuang
primate fauna is distinct from that of
other known primate faunas, both living
and extinct. The earliest phases of haplorhine phylogeny, including the initial
diversification of tarsiiform and anthropoid
primates, probably occurred at or below the
0047–2484/00/040585+10$35.00/0
lower limits of body mass found in living
primates.
The smallest living mammals are species
of the Insectivora, Chiroptera, Rodentia,
and Dasyuridae (Nowak & Paradiso, 1983;
Churchfield, 1996). Sorex minutissimus (1·5–
3 g), Suncus etruscus (1·5–2 g), Rynchonycteris naso (2·1–4·3 g), Salpingotulus (3 g),
Micromys (5–9 g), and Mus (2·5–12 g) are
among the tiniest living mammals (Nowak &
Paradiso, 1983; Churchfield, 1996). Within
an estimated body mass of only 1·3 g, the
early Eocene insectivore Batodonoides vanhouteni may actually have exceeded the
lower limits of body mass found in living
mammals (Bloch et al., 1998). No living
primates approach this small size. Microcebus
myoxinus, the smallest living primate, weighs
26–37 g, and other species of this genus
range from 32–77 g (Atsalis et al., 1996). At
125 g Cebuella is the tiniest living anthropoid. Tarsiers are the smallest extant haplorhines, ranging from 90–150 g. The body
mass of the smallest species, Tarsius pumilus
is unknown, although it is unlikely to be less
than 50 g.
2000 Academic Press
586
. .
ET AL.
Figure 1. Shanghuang calcanei IVPP V 11848 (center) and IVPP V 11847 (right) compared to Microcebus
murinus (Left, NIU specimen), one of the smallest living species of primates (60 g). Scale in millimeters.
See Table 1 for measurements.
Known fossil primates do not significantly
exceed the range in body mass shown by
living primates. Altanius orlovi, estimated at
21–23 g based on molar size (Conroy,
1987), is possibly the smallest fossil primate,
but opinions are varied as to whether this
species is a primate or a plesiadapiform
(Rose et al., 1994). The omomyids Pseudoloris, Teilhardina, Tetonius, Uintanius, Trogolemur, Uintalacus, Utahia, Washakius and
Anemorhysis are the smallest undoubted fossil primates described to date. If all primate,
prosimian only, or strepsirhine only regression models are used to estimate body mass
from molar size, these species are approximately the size of living Microcebus, but not
smaller (Gingerich, 1981; Conroy, 1987;
Dagosto & Terranova, 1992). However, if a
tarsier only regression model is used, some
of these species may have been as small as
15 g (Gingerich, 1981). The smallest fossil
anthropoids are Eosimias [67–179 g (Beard
et al., 1994, 1996)], Algeripithecus [150–
300 g (Godinot & Mahboubi, 1992)] and
Qatrania wingi [160–278 g (Conroy, 1987)].
Primate postcranial elements from the
middle Eocene Shanghuang fissure-fillings
of southeastern China (Beard et al., 1994)
place new limits on the range of body mass
in this order, and suggest that major primate
clades may have originated below the limits
of body mass in living primates. IVPP V
11847 and IVPP V 11848 (IVPP=Institute
of Vertebrate Paleontology and Paleoanthropology) are calcanei from Shanghuang
Fissures A and D, respectively (Figure 1).
The vertebrate faunas from these fissures
have been estimated to date to approximately 45 ma on purely biostratigraphic
evidence (Wang & Dawson, 1992; Beard
et al., 1994). Both calcanei are complete,
and exhibit all of the features typical of
primates (Gebo, 1988), allowing them to be
securely assigned to this order. The epiphysis of the heel is fused to the rest of the
bone in both specimens, indicating that
these bones are from adults. These specimens pertain to new, and as yet unnamed,
species.
The Shanghuang calcanei are attributed
to Haplorhini on the basis of the morphology of the posterior calcaneal facet,
which is relatively short and broad, unlike in
adapiforms where it is long and narrow.
Both of these calcanei are also far outside
the size range represented by Shanghuang
adapids. IVPP V 11847 is morphologically
similar to calcanei of North American
omomyids. However, IVPP V 11847 probably pertains to a different haplorhine taxon
because the only omomyid currently known
from Shanghuang is Macrotarsius [900–
1221 g (MacPhee et al., 1995)], a taxon
likely to have been larger than that represented by IVPP V 11847 by roughly two
orders of magnitude. IVPP V 11848 differs
morphologically from IVPP V 11847 in
having a much broader distal segment, and
a calcaneocuboid joint in which the pivot is
shifted medially. These morphological differences exceed those found in living and
fossil primate families, suggesting that IVPP
V 11848 and IVPP V 11847 represent distinctly different haplorhine clades. The anatomical distinctions of the IVPP V 11848
specimen are shared with anthropoids, suggesting attribution to Anthropoidea, probably the Eosimiidae. Dental remains have
not yet been allocated to either of these
small taxa.
Compared with other primates, the most
remarkable aspect of these bones is their
small size. IVPP V 11847 is only 4·0 mm in
length, while IVPP V 11848 measures
4·25 mm (Table 1, Figure 1). Both Shanghuang calcanei are considerably smaller than
those of any extant or fossil primate for
which the relevant anatomy is known (Table
1). The entire length of the IVPP V 11847
and IVPP V 11848 calcanei is only as long as
the combined heel and posterior facet
lengths of calcanei belonging to Microcebus
murinus, a 60 g primate (Figure 1). Comparisons of total calcaneal length are complicated by the variable degree to which the
distal part of the calcaneus is elongated in
primates. Microcebus, for example, has a
particularly long distal calcaneus (about
65% of total length). The Shanghuang
specimens exhibit more moderate distal
elongation (52–53%), comparable to that of
omomyids. However, all other dimensions
of the calcaneus are also considerably
smaller than in other known primates
(Table 1).
587
Several measurements of the calcaneus
prove to be reasonable estimators of body
mass in prosimian primates (Dagosto &
Terranova, 1992). Using these equations,
the body mass of IVPP V 11847 is predicted
to be 9·5–16·4 g (Table 2). Similar estimates for IVPP V 11848 range from 13·3–
23·6 g. The Chinese fossils are beyond the
size range of the extant primates used to
construct the model. Therefore, classical
calibration may be more appropriate in this
instance (Hens et al., 1998). Estimates from
this technique are slightly lower than those
derived from inverse calibration (Table 2).
The factor score from a first principal component analysis of all calcaneal variables was
also used to predict body mass (Payseur
et al., 1999). This method yields estimates of
10·6 g for IVPP V 11847 and 17·2 g for
IVPP V 11848 (or 8·1 g and 12·5 g,
respectively, using classical calibration).
Similarly, head and body length can be
predicted from calcaneal size. For IVPP V
11847, the first principal component yields
an estimate for head and body length of
60–70 mm. The same estimate for IVPP V
11848 is 70–80 mm. These values are less
than half those for the smallest living primate, Microcebus myoxinus (Atsalis et al.,
1996), but are similar to those of shrews and
mice weighing about 15 g (Churchfield,
1996). All of the preceding models are based
on extant strepsirhines. Because neither of
these fossils belongs to this clade, they may
not follow the same scaling trends. In other
fossil primates, especially omomyids, body
mass estimates based on postcrania do not
always agree with estimates based on teeth
(Dagosto & Terranova, 1992). Table 2 provides body mass estimates for other small
primates based on calcaneal variables. It is
clear from both the body size estimates and
from the absolute measurements (Table 1)
that, by any standard, the Shanghuang
primates are the smallest known.
Mammals of very small size face a variety
of physiological constraints (Calder, 1984;
588
Table 1 Measurements of the calcaneus (in mm) for the Shanghuang fossils, extant Microcebus, and some small omomyids*
Microcebus
?rufus
Microcebus
murinus
Teilhardina
belgica
Arapahovius
gazini
Absarokius
abbotti
Shoshonius
cooperi
Tetonius
sp.
Washakius
insignis
8·58
2·33
5·27
1·77
1·58
1·67
1·57
2·48
7·10
2·46
3·63
1·64
1·86
4·81
9·80
2·87
5·58
1·95
2·28
3·38
9·79
3·25
5·20
2·23
2·22
2·32
1·55
4·95
4·25
1·80
2·20
1·20
0·85
1·25
0·90
2·22
10·09
2·55
6·20
1·87
1·97
1·73
1·69
4·95
4·00
1·55
2·10
1·15
0·75
1·00
0·80
3·56
10·00
3·35
2·56
1·80
1·54
3·34
2·61
2·18
2·45
2·51
2·12
1·90
*For the extant species and omomyids, the mean is given. Designations C1–C7 refer to the illustration of measurements in Dagosto & Terranova (1992), Figure
1. The mean body mass of Microcebus rufus is 42 g and 59 g for Microcebus murinus (Atsalis et al., 1996). A single calcaneus of Microcebus ?myoxinus from Kirindy
(uncatalogued specimen from the Field Museum, Chicago) measures 8·93 mm in length. The mean body mass of this species is 30 g (Atsalis et al., 1996).
ET AL.
IVPP V
11848
. .
Area of lower first molar
Calcaneal length (C1)
Calcaneal width (C2)
Distal length
Posterior calcaneal facet length (C3)
Posterior length (C7)
Calcaneocuboid width (C6)
Calcaneocuboid height (C5)
IVPP V
11847
Table 2 Body size estimates (g) from the strepsirhine regression equations in (Dagosto & Terranova, 1992)*
Measurement
Area of lower first
molar
Calcaneal width (C2)
PCA (C2–C6, index 6)
Average of calcaneal
estimates from inverse
calibration
Average of calcaneal
estimates from classical
calibration
IVPP V 11848
15·4 (12·0–19·8)
10·9
16·4 (12·2–22·0)
11·1
9·5 (5·9–14·9)
4·9
9·7 (7·2–13·0)
9·3
13·1 (7·2–26·9)
7·0
10·6 (6·6–17·1)
8·1
12·5
23·6 (18·3–30·4)
17·2
18·5 (13·8–24·7)
13·8
13·3 (8·5–21·1)
7·2
22·2 (17·8–27·8)
17·6
15·9 (11·9–21·4)
11·8
17·2 (10·6–24·8)
12·6
18·5
8·6
13·4
Microcebus
murinus
Teilhardina
belgica
Absarokius
abbotti
65·9 (50–86)
78·0 (62–99)
222·0 (170–291)
60·4 (47–78)
54·5 (42–70)
84·7 (66–109)
131·9 (102–170)
131·9 (102–170)
58·2 (43–78)
40·6 (30–54)
65·3 (49–88)
122
145
58·6 (37–93)
108·5 (69–171)
77·0 (49–122)
Washakius
insignis
138
(113–169)
(91–164)
51·3 (41–64)
88·9 (71–111)
59·8 (45–80)
94·2 (70–127)
61·3
47·6
69·5
109·1
Tetonius
homunculus
232
(194–277)
(108–194)
95·8 (77–120)
124·2
Length of posterior calcaneal facet (C3)
Calcaneocuboid Ht
(C5)
Calcaneocuboid facet
width (C6)
Index 6 (=C5C6)
IVPP V 11847
*The prediction and the 95% confidence interval is given. For each calcaneal variable, the top line gives the estimate from inverse calibration, the second line
gives the estimate from classical calibration. All raw values are multiplied by the appropriate correction factor following (Sprugel, 1983). All correction factors are
less than 5%.
589
590
. .
Alexander, 1996; Miller, 1996) and these
allow us to draw further paleobiological
inferences for the tiny haplorhine primates
from Shanghuang. A very high metabolic
rate (Kleiber, 1961; Alexander, 1996), and
therefore a diet rich in high caloric items
such as insects, nectar or fruit is likely (Kay,
1984; Kay & Covert, 1984; Atsalis, 1999).
The gut would probably be minimally specialized (Chivers & Hladik, 1984) with a
high surface area, allowing water and other
nutrients to be absorbed rapidly (Martin,
1990). Heat and water exchange would be a
significant problem for such tiny primates
(Porter & Gates, 1969; Alexander, 1996).
Life history factors are also influenced by
size. Small mammals have fewer but relatively larger neonates and a relatively longer
gestation time than their larger relatives
(Purvis & Harvey, 1996). Given the longer
gestations and fewer offspring reported for
living haplorhines (Martin, 1990), this
implies a small ancestral condition like that
found at Shanghuang. With small size also
comes an increased risk of predation,
especially by raptorial birds (Goodman
et al., 1993). The intermembral index (IMI)
of these species is probably low, because
IMI generally decreases with size among
primates (Jungers, 1985). A low IMI implies
frequent leaping by both IVPP V 11847 and
IVPP V 11848.
Based on available postcranial and dental
remains, we estimate that the Shanghuang
fauna contains 15–19 species of primates.
We inferred the body masses of these species
using the same techniques described above.
Figure 2 and Table 3 compare the size
distribution of the Shanghuang primate
fauna with those of other communities of
living and extinct primates. The Shanghuang fauna is apparently unique in including so many very small (<100 g) species of
primates, while lacking species of large size
(>1000 g). This distinction holds with
respect to both living and fossil primate
faunas, including one of similar age (Bridger
ET AL.
Basin, Wyoming). Being smaller allows correspondingly small home ranges, permitting
many taxa to pack into these ancient forests.
With so many small, closely related and
sympatric primates occurring in the ancient
forests at Shanghuang, competition may
have been a significant problem. Intense
competition normally promotes a diversity
of biological niches including a variety of
dietary preferences, diurnal and nocturnal
activity patterns, and levels of forest use in
primates (Charles-Dominique, 1977).
One explanation for the unique distribution of body mass shown by the Shanghuang
primate fauna is that this assemblage
samples a portion of the primate evolutionary tree that is missing from other
well-sampled fossil primate faunas (and
completely unrepresented among extant
primate diversity). Primate taxa already
described from Shanghuang include basal
tarsiids and anthropoids, in addition to the
adapiforms and omomyids that characterize
many other Eocene primate faunas (Beard
et al., 1994). It is impossible to establish the
precise phylogenetic positions of the tiny
haplorhine taxa represented by IVPP V
11847 and IVPP V 11848 on the basis of the
limited anatomical evidence. Nevertheless,
these specimens demonstrate that haplorhine primates smaller than any living primate inhabited southeastern China during
the middle Eocene. Furthermore, these tiny
haplorhines encompassed at least a moderate degree of taxonomic diversity. Because
basal tarsiids and basal anthropoids are both
represented at Shanghuang, at least part of
the radiation of tiny haplorhines known
from this site may pertain to either or both
of these clades. Indeed, based on regressions
of body mass against molar area (Gingerich,
1981), the early tarsiid Tarsius eocaenus from
Shanghuang (Beard et al., 1994) weighed
only 29 g, which is also less than any living
primate. Undoubted anthropoids of such
diminutive size have not yet been reported
from Shanghuang, although Eosimias was
Shanghuang, China
Bighorn Basin, Wyoming
12
10
10
10
8
8
8
6
6
6
4
4
4
2
2
2
0
2
3
4
5
6
7
8
9
10
Ranomafana, Madagascar
12
0
2
3
4
5
6
7
8
9
10
Manu, Peru
12
0
10
10
8
8
8
6
6
6
4
4
4
2
2
2
2
3
4
5
6
7
8
9
10
0
2
3
4
5
6
7
2
3
8
9
10
0
4
5
6
7
8
9
10
9
10
Makoukou, Gabon
12
10
0
Bridger Basin, Wyoming
12
2
3
4
5
6
7
8
Number of species
12
ln body mass (grams)
Figure 2. Body size distribution (x axis is natural log of body mass) of Shanghuang primates compared to two other Eocene fossil localities
(Bighorn and Bridger Basins, Wyoming) and three extant primate communities from South America (Manu), West Africa (Makoukou),
and Madagascar (Ranomafana). A figure of Microcebus indicates the bin for the smallest living primate (30–60 g). Body mass data for the
living primates are from Fleagle (1999), Waser (1987), and Wright (1992). Species lists for the Bighorn Basin from (Bown & Rose, 1987,
1991; Gebo et al., 1991) and the Bridger Basin from (Gunnell, 1997). Size estimates for the Wyoming fossil primates are derived from
dental dimensions using the prosimian regression equation of Conroy (1987). This may overestimate size compared to the postcranial
dimensions used for the Shanghuang primates, however, no dentally known primate from the Wyoming fossil localities is smaller than
Microcebus in the area of the first lower molar.
591
592
. .
ET AL.
Table 3 Body mass distribution for some extant and fossil primate communities*
Manu
Taxon
Makoukou
Body mass Taxon
Body mass Taxon
Extant communities
Cebuella pygmaea
Saguinus fuscicollis
Callimico goeldii
Saguinus imperator
Callicebus moloch
Aotus trivirgatus
Saimiri sciureus
Pithecia monachus
Cebus albifrons
Cebus apella
Lagothrix lagotricha
110
343
468
474
800
800
900
2110
2800
3000
7020
Galagoides demidovii
Galago alleni
Euoticus elegantulus
Arctocebus calabarensis
Perodicticus potto
Cercopithecus talapoin
Cercopithecus cephus
Cercopithecus pogonias
Cercopithecus neglectus
Cercopithecus nictitans
Cercocebus galeritus
Ateles paniscus
Alouatta seniculus
8000
8000
Cercocebus albigena
Colobus guereza
Papio sphinx
Shanghuang
Taxon
Fossil communities
NH1
E1
T1
E2
P1
NH2
P2
E3
P3
NH3
T2
E4
P4
E5
P5
Adapoides troglodytes
NH4
Adapiform
Macrotarsius macrorhysis
Ranomafana
60
269
300
306
836
1100
2900
3000
4000
4200
5260
6020
9200
11,500
Microcebus rufus
Cheirogaleus major
Eulemur fulvus
Eulemur rubriventer
Varecia variegata
Hapalemur griseus
Hapalemur simus
Hapalemur aureus
Lepilemur microdon
Avahi laniger
Propithecus diadema
Daubentonia
madagascariensis
Big Horn Basin
Body mass Taxon
12
17
26
28
28
35
53
63
71
79
81
89
107
110
123
200
353
421
800
Teilhardina tenuiculus
Teilhardina demissa
Arapahovius advena
Teilhardina crassidens
Tatmanius szalayi
Anaptomorphus wortmani
Teilhardina americana
Anemorhysis pattersoni
Teilhardina sp.
Chlorohysis
Tetonius sp.
Steinius vespertinus
Strigorhysis bridgerensis
Pseudotetonius ambiguus
Tetonius matthewi
Absarokius metoecus
Absarokius abotti
Cantius ralstoni
Cantius trigonodus
Cantius feretutus
Cantius frugivorous
Cantius abditus
Pelvcodus jarrovi
Body mass
49
362
2180
1940
3520
670
1300
1390
800
1030
5830
2490
Bridger Basin
Body mass Taxon
68
78
80
86
87
89
92
98
100
120
139
151
155
161
180
190
204
1300
2000
2000
2800
3000
4500
Trogolemur myodes
Uintanius ameghini
Sphacorhysis burntforkensis
Trogolemur amplior
Uintanius rutherfurdi
Anaptomorphus aemulus
Washakius insignis
Hemiacodon gracilis
Omomys carteri
Wyomomys bridgeri
Anaptomorphus westi
Ageitodendron matthewi
Gazinius bowni
Gazinius amplus
Smilodectes gracilis
Notharctus tenebrosus
Notharctus pugnax
Notharctus robustior
Body mass
65
70
78
85
94
133
155
300
310
320
415
493
600
875
2100
2500
3000
6900
These data are used to construct Figure 3. For the extant communities, species lists are from Waser (1987) and
Wright (1992). Species body mass is from these sources and Fleagle (1999). In cases where there is significant
sexual dimorphism, the female body weights are given. For the fossil communities, body mass estimated from tarsal
bones is given in bold, otherwise, the estimate was made from first lower molar area following Conroy (1987). If
these data were unavailable, the estimates in Fleagle (1999) were used. The number of taxa for Shanghuang is
documented in Gebo et al. (in prep) (E=eosimiid; NH=new haplorhine; P=protoanthropoid; T=tarsiid).
certainly small (body size estimate:
67–158 g). Given the diversity of early haplorhines, including Tarsius eocaenus, that
were similar in size or smaller than the
smallest living mouse lemurs, it seems likely
that the earliest phases of haplorhine phylogeny, including the initial diversification of
anthropoids and tarsiers, took place at or
below the lower limits of body mass found in
living primates.
Acknowledgements
This research was supported by grants from
the L. S. B. Leakey Foundation (DLG &
MD) and the National Science Foundation
(KCB). We thank S. Goodman (Division of
Mammals, Field Museum of Natural
History) for access to uncatalogued Microcebus material, and numerous colleagues at
the IVPP for their assistance.
References
Alexander, R. M. (1996). Biophysical problems of
small size in vertebrates. In (P. J. Miller, Ed.) Miniature Vertebrates, pp. 3–14. Oxford: Clarendon Press.
Atsalis, S. (1999). Diet of the brown mouse lemur
(Microcebus rufus) in Ranomafana National Park,
Madagascar. Int. J. Primatol. 20, 193–229.
Atsalis, S., Schmid, J. & Kappeler, P. (1996). Metrical
comparisons of three species of mouse lemur. J. hum.
Evol. 31, 61–68.
Beard, K. C., Qi, T., Dawson, M. R., Wang, B. & Li,
C. (1994). A diverse new primate fauna from middle
Eocene fissure-fillings in southeastern China. Nature
368, 604–609.
Beard, K. C., Tong, Y., Dawson, M., Wang, J. &
Huang, X. (1996). Earliest complete dentition of an
anthropoid primate from the late Middle Eocene of
Shanxi Province, China. Science 272, 82–85.
Bloch, J. I., Rose, K. D. & Gingerich, P. D. (1998).
New species of Batonoides (Lipotyphla, Geolabididae) from the early Eocene of Wyoming: smallest
known mammal? J. Mamm. 79, 804–827.
Bown, T. M. & Rose, K. D. (1987). Patterns of dental
evolution in Early Eocene anaptomorphine primates
(Omomyidae) from the Bighorn Basin, Wyoming.
J. Paleont. 61, 1–162.
Bown, T. M. & Rose, K. D. (1991). Evolutionary
relationships of a new genus and three new species of
omomyid primates (Willwood Formation, Lower
Eocene, Bighorn Basin, Wyoming). J. hum. Evol. 20,
465–480.
593
Calder, W. A. (1984). Size, Function, and Life History.
Cambridge: Harvard University Press.
Charles-Dominique, P. (1977). Ecology and Behavior of
Nocturnal Primates. New York: Columbia University
Press.
Chivers, D. J. & Hladik, C. M. (1984). Diet and gut
morphology in primates. In (D. Chivers, B. Wood &
A. Bilsborough, Eds) Food Acquisition and Processing
in Primates, pp. 213–230. New York: Plenum Press.
Churchfield, S. (1996). Ecology of very small terrestrial
mammals. In (P. J. Miller, Ed.) Miniature Vertebrates,
pp. 259–276. Oxford: Clarendon Press.
Conroy, G. C. (1987). Problems of body-weight
estimation in fossil primates. Int. J. Primatol. 8,
115–137.
Dagosto, M. & Terranova, C. J. (1992). Estimating the
body size of Eocene primates: A comparison of
results from dental and postcranial variables. Int. J.
Primatol. 13, 307–344.
Fleagle, J. (1999). Primate Adaptation and Evolution.
New York: Academic Press.
Gebo, D. L. (1988). Foot morphology and locomotor
adaptation in Eocene Primates. Folia primatol. 50,
3–41.
Gebo, D. L., Dagosto, M. & Rose, K. D. (1991). Foot
morphology and evolution in early Eocene Cantius.
Am. J. phys. Anthrop. 86, 51–73.
Gingerich, P. D. (1981). Early Cenozoic Omomyidae
and the evolutionary history of tarsiiform primates.
J. hum. Evol. 10, 345–374.
Godinot, M. & Mahboubi, M. (1992). Earliest known
simian primate found in Algeria. Nature 357, 324–
326.
Goodman, S. M., O’Connor, S. & Langrand, O.
(1993). A review of predation on lemurs: Implications for the evolution of social behavior in small,
nocturnal primates. In (P. M. Kappeler & J. U.
Ganzhorn, Eds) Lemur Social Systems and Their
Ecological Basis, pp. 51–66. New York: Plenum
Press.
Gunnell, G. (1997). Wasatchian–Bridgerian (Eocene)
paleoecology of the western interior of North
America: changing paleoenvironments and taxonomic composition of omomyid (Tarsiiformes)
primates. J. hum. Evol. 32, 105–132.
Hens, S. M., Konigsberg, L. W. & Jungers, W. L.
(1998). Estimation of African ape body length from
femur length. J. hum. Evol. 34, 401–412.
Jungers, W. L. (1985). Body size and scaling of limb
proportions in primates. In (W. L. Jungers, Ed.) Size
and Scaling in Primate Biology, pp. 345–381. New
York: Plenum Press.
Kay, R. F. (1984). On the use of anatomical features to
infer foraging behavior in extinct primates. In (P. S.
Rodman & J. G. H. Cant, Eds) Adaptations for
Foraging in Nonhuman Primates, pp. 21–53. New
York: Columbia University Press.
Kay, R. F. & Covert, H. H. (1984). Anatomy and
behavior of extinct primates. In (D. Chivers, B.
Wood & A. Bilsborough, Eds) Food Acquisition and
Processing in Primates, pp. 467–508. New York:
Plenum Press.
594
. .
Kleiber, M. (1961). The Fire of Life: An Introduction to
Animal Energetics. New York: John Wiley.
MacPhee, R. D. E., Beard, K. C. & Tao, Q. (1995).
Significance of primate petrosal from middle Eocene
fissure-fillings at Shanghuang, Jiangsu Province,
People’s Republic of China. J. hum. Evol. 29, 501–
514.
Martin, R. D. (1990). Primate Origins and Evolution—
A Phylogenetic Reconstruction. Princeton: Princeton
University Press.
Millar, P. J. (Ed.) (1996). Miniature Vertebrates.
Oxford: Clarendon Press.
Nowak, R. M. & Paradiso, R. L. (1983). Walker’s
Mammals of the World. Baltimore: Johns Hopkins
University Press.
Payseur, B. A., Covert, H. H., Vinyard, C. J. &
Dagosto, M. (1999). New body mass estimates for
Omomys carteri, a Middle Eocene primate from North
America. Am. J. phys. Anthrop. 109, 41–52.
Porter, W. P. & Gates, D. M. (1969). Thermodynamic
equilibria of animals with environment. Ecological
Monographs 39, 227–244.
Purvis, A. & Harvey, P. H. (1996). Miniature mammals: life history strategies and macroevolution. In
ET AL.
(P. J. Miller, Ed.) Miniature Vertebrates, pp. 159–174.
Oxford: Clarendon Press.
Rose, K. D., Godinot, M. & Bown, T. M. (1994). The
early radiation of euprimates and the initial diversification of Omomyidae. In (J. G. Fleagle & R. F.
Kay, Eds) Anthropoid Origins, pp. 1–27. New York:
Plenum Press.
Sprugel, D. G. (1983). Correcting for bias in logtransformed allometric equations. Ecology 64, 209–
210.
Wang, B. & Dawson, M. R. (1992). A primitive cricetid
(Mammalia: Rodentia) from the middle Eocene of
Jiangsu Province, China. Ann. Bull. Carnegie Mus.
63, 239–256.
Waser, P. M. (1987). Interactions among primate
species. In (B. B. Smuts, D. L. Cheney, R. M.
Seyfarth, R. W. Wrangham & T. T. Struhsaker, Eds)
Primate Societies, pp. 210–226. Chicago: University of
Chicago Press.
Wright, P. C. (1992). Primate ecology, rainforest conservation, and economic development: building a
National Park in Madagascar. Evol. Anthrop. 1,
25–33.