ArticlePDF Available

Semiaquatic adaptations in a giant predatory dinosaur

Authors:
  • Museo di Storia Naturale di Milano
  • Museo di Storia Naturale di Milano

Abstract

We describe adaptations for a semiaquatic lifestyle in the dinosaur Spinosaurus aegyptiacus. These adaptations include retraction of the fleshy nostrils to a position near the mid-region of the skull and an elongate neck and trunk that shift the center of body mass anterior to the knee joint. Unlike terrestrial theropods, the pelvic girdle is downsized, the hindlimbs are short, and all of the limb bones are solid without an open medullary cavity, for buoyancy control in water. The short, robust femur with hypertrophied flexor attachment and the low, flat-bottomed pedal claws are consistent with aquatic foot-propelled locomotion. Surface striations and bone microstructure suggest that the dorsal “sail” may have been enveloped in skin that functioned primarily for display on land and in water.
DOI: 10.1126/science.1258750
, 1613 (2014);345 Science et al.Nizar Ibrahim
Semiaquatic adaptations in a giant predatory dinosaur
This copy is for your personal, non-commercial use only.
clicking here.colleagues, clients, or customers by , you can order high-quality copies for yourIf you wish to distribute this article to others
here.following the guidelines can be obtained byPermission to republish or repurpose articles or portions of articles
): September 25, 2014 www.sciencemag.org (this information is current as of
The following resources related to this article are available online at
http://www.sciencemag.org/content/345/6204/1613.full.html
version of this article at: including high-resolution figures, can be found in the onlineUpdated information and services,
http://www.sciencemag.org/content/suppl/2014/09/10/science.1258750.DC1.html
can be found at: Supporting Online Material
http://www.sciencemag.org/content/345/6204/1613.full.html#related
found at: can berelated to this article A list of selected additional articles on the Science Web sites
http://www.sciencemag.org/content/345/6204/1613.full.html#ref-list-1
, 15 of which can be accessed free:cites 40 articlesThis article
http://www.sciencemag.org/cgi/collection/paleo
Paleontology subject collections:This article appears in the following
registered trademark of AAAS. is aScience2014 by the American Association for the Advancement of Science; all rights reserved. The title CopyrightAmerican Association for the Advancement of Science, 1200 New York Avenue NW, Washington, DC 20005.
(print ISSN 0036-8075; online ISSN 1095-9203) is published weekly, except the last week in December, by theScience
on September 25, 2014www.sciencemag.orgDownloaded from on September 25, 2014www.sciencemag.orgDownloaded from on September 25, 2014www.sciencemag.orgDownloaded from on September 25, 2014www.sciencemag.orgDownloaded from on September 25, 2014www.sciencemag.orgDownloaded from
7. M. White, N. Ashton, Curr. Anthropol. 44, 598609 (2003).
8. F. Fontana et al., J. Anthropol. Archaeol. 32, 478498
(2013).
9. A. Picin, M. Peresani, C. Falguères, G. Gruppioni, J.-J. Bahain,
PLOS ONE 8, e76182 (2013).
10. R. Barkai, A. Gopher, S. E. Lauritzen, A. Frumkin, Nature 423,
977979 (2003).
11. R. Shimelmitz, R. Barkai, A. Gopher, J. Hum. Evol. 61, 458479
(2011).
12. S. L. Kuhn, Curr. Anthropol. 54, S255S268 (2013).
13. V. B. Doronichev, PaleoAnthropol. 2008, 107 (2008).
14. E. Boëda, in The Definition and Interpretation of Levallois
Technology, H. L. Dibble, O. Bar-Yosef, Eds. (Prehistory Press,
Madison, WI, 1995), pp. 4169.
15. E. Boëda, Le Concept Levallois: Variabilité des Méthodes (CNRS
Éditions, Paris, 1994).
16. P. J. Brantingham, S. L. Kuhn, J. Archaeol. Sci. 28, 747761
(2001).
17. S. J. Lycett, M. I. Eren, J. Archaeol. Sci. 40, 23842392
(2013).
18. S. J. Lycett, M. I. Eren, World Archaeol. 45, 519538 (2013).
19. M. I. Eren, S. J. Lycett, PLOS ONE 7, e29273 (2012).
20. R. Foley, M. M. Lahr, Camb. Archaeol. J. 7, 3 (1997).
21. S. J. Armitage et al., Science 331, 453456 (2011).
22. H. Valladas et al., J. Hum. Evol. 65, 585593 (2013).
23. M. Meyer et al., Nature 505, 403406 (2014).
24. K. Prüfer et al., Nature 505,4349 (2014).
25. Materials and methods are available as supporting material on
Science Online.
26. R. Badalian et al., Radiat. Meas. 34, 373378 (2001).
27. E. V. Arutyunyan, V. A. Lebedev, I. V. Chernyshev,
A. K. Sagatelyan, Dokl. Earth Sci. 416, 10421046 (2007).
28. V. A. Lebedev, I. V. Chernyshev, K. N. Shatagin, S. N. Bubnov,
A. I. Yakushev, J. Volcanol. Seismol. 7, 204229 (2013).
29. S. Joannin et al., Earth Planet. Sci. Lett. 291,149158
(2010).
30. V. Ollivier et al., Quat. Int. 223-224, 312326 (2010).
31. E. Frahm et al., J. Archaeol. Sci. 41, 333348 (2014).
32. A. J. Jelinek, Science 216, 13691375 (1982).
33. S. McBrearty, J. Archaeol. Res. 69, 7 (2013).
34. J. J. Shea, Curr. Anthropol. 52,135 (2011).
35. T. Hopkinson, A. Nowell, M. White, PaleoAnthropology 2013,61
(2013).
36. S. Lycett, J. Anthropol. Archaeol. 26, 541575 (2007).
37. R. Stöckli, E. Vermote, N. Saleous, R. Simmon, D. Herring,
The Blue Marble Next Generation - A true color earth dataset
including seasonal dynamics from MODIS (NASA Earth
Observatory, 2005); http://earthobservatory.nasa.gov/
Features/BlueMarble/bmng.pdf.
38. L. Augustin et al., Nature 429, 623628 (2004).
ACKNO WLEDGM ENTS
Data discussed in this paper can be found in the supplementary
materials. All artifacts are stored at the Institute of Archeology
and Ethnography, Yerevan, Armenia. We thank the following
organizations for their financial support: the University of
Connecticut [20082014: Norian Armenian Programs Committee,
College of Liberal Arts and Sciences (CLAS), Office of Global
Affairs, Study Abroad; and CLAS Book Committee]; the UK
Natural Environment Research Council (grant IP-1186-0510), the
L. S. B. Leakey Foundation (2010 and 2011), the Irish Research
Council (2008 and 2009), and the University of Winchester.
We also thank P. Avetisyan and B. Yeritsyan, Institute of Archeology
and Ethnography, Republic of Armenia, for their collaboration.
SUPPLEMENTARY MATERIALS
www.sciencemag.org/content/345/6204/1609/suppl/DC1
Materials and Methods
Supplementary Text
Figs. S1 to S16
Tables S1 to S7
References (39192)
Databases S1 and S2
27 May 2014; accepted 19 August 2014
10.1126/science.1256484
PALEONTOLOGY
Semiaquatic adaptations in a giant
predatory dinosaur
Nizar Ibrahim,
1
*Paul C. Sereno,
1
Cristiano Dal Sasso,
2
Simone Maganuco,
2
Matteo Fabbri,
3
David M. Martill,
4
Samir Zouhri,
5
Nathan Myhrvold,
6
Dawid A. Iurino
7
We describe adaptations for a semiaquatic lifestyle in the dinosaur Spinosaurus
aegyptiacus. These adaptations include retraction of the fleshy nostrils to a position
near the mid-region of the skull and an elongate neck and trunk that shift the center of
body mass anterior to the knee joint. Unlike terrestrial theropods, the pelvic girdle is
downsized, the hindlimbs are short, and all of the limb bones are solid without an open
medullary cavity, for buoyancy control in water. The short, robust femur with hypertrophied
flexor attachment and the low, flat-bottomed pedal claws are consistent with aquatic
foot-propelled locomotion. Surface striations and bone microstructure suggest that
the dorsal sailmay have been enveloped in skin that functioned primarily for display
on land and in water.
Bones of the predatory dinosaur Spinosaurus
aegyptiacus first came to light over a cen-
tury ago from Upper Cretaceous rocks in
Egypt (13) but were destroyed in World
War II (4). More recently, isolated teeth
and bones (5) and the anterior half of an adult
skull (6) have been discovered in the Kem Kem
beds of eastern Morocco (Fig. 1A) and equiv-
alent horizons in Algeria, but are insufficiently
complete to estimate the size, proportions, and
functional adaptations of this species. Here
we report the discovery of a partial skeleton of
S. aegyptiacus fromthemiddleoftheKemKem
sequence(Fig.1B),whichisprobablyCenomanian
in age (~97 million years ago) (7).
The subadult skeleton, here designated the neo-
type of S. aegyptiacus (8), preserves portions of the
skull, axial column, pelvic girdle, and limbs. It was
discovered in fluvial sandstone that has yielded re-
mains of the sauropod Rebbachisaurus (9)andthree
other medium-to-large theropods (an abelisaurid,
Deltadromeus,andCarcharodontosaurus)(7,10).
We regard two additional Kem Kem theropods,
Sigilmassasaurus brevicollis and S. maroccanus
(11,12), to be referable to S. aegyptiacus (8).
The neotype skeleton and isolated bones refer-
able to S. aegyptiacus were scanned with com-
puted tomography, size-adjusted, and combined
with a digital recreation of the original Egyptian
fossils (Fig. 2A, red). Missing bones were extrap-
olated between known bones or estimated from
those of other spinosaurids (6,13,14). The digi-
tal model of the adult skeleton of Spinosaurus
(Fig. 2A), when printed and mounted, measures
over 15 m in length, longer than Tyrannosaurus
specimens (~12.5 m) (15).
A concentrated array of neurovascular foramina
open on the anterior end of the snout and ap-
pear similar to foramina in crocodilians that
house pressure receptors that detect water move-
ment (8,16)(Fig.2Bandfig.S6).Theenlarged,
procumbent, interlocking anterior teeth are well
adapted for snaring fish (5,6)(Fig.2Bandfig.S4).
The fossa for the fleshy nostril is small and, unlike
any other nonavian dinosaur, is retracted to a
posterior position to inhibit the intake of water
(Fig. 2C and figs. S4 and S6) (8).
Most cervical and dorsal centra are elongate
compared to the sacral centra, resulting in a pro-
portionately long neck and trunk (Figs. 2A and 3
and tables S1 and S2). The anteriormost dorsal
centra, however, are proportionately short, ex-
ceptionally broad, and concavoconvex (Fig. 2D).
These characteristic vertebrae, the affinity of which
has been controversial (7,11,12), are referred
here to S. aegyptiacus, based on their association
with spinosaurid skeletons in Niger (8)andEgypt
(2).Thehorizontalcervicodorsalhingecreated
by these broad centra would facilitate dorsoven-
tral excursion of the neck and skull in the pur-
suit of prey underwater.
Thedistaltwo-thirdsofthetailcomprisesver-
tebrae with relatively short centra, diminutive
zygapophyses, and anteroposteriorly compressed
neural spines (Fig. 2G). The affinity of these
caudal elements has been uncertain (17), but
comparisons with associated remains from Egypt
(2) and more proximal caudals in the neotype
(Fig. 2A) allow referral to Spinosaurus. Short
centra and reduced neural arch articulations
enhance lateral bending during tail propulsion
in bony fish (18).
The forelimb has hypertrophied deltopectoral
and olecranon processes for powerful flexion and
extension (Fig. 2A). Elongate manual phalanges
(Fig. 2H) and less recurved, manual unguals that
SCIENCE sciencemag.org 26 SEPTEMBER 2014 VOL 345 ISSUE 6204 1613
1
Department of Organismal Biology and Anatomy, University
of Chicago, Chicago, IL 60637, USA.
2
Museo di Storia
Naturale di Milano, Corso Venezia 55, 20121 Milan, Italy.
3
School of Earth Sciences, University of Bristol, Queens
Road, Bristol, BS8 1RJ, UK.
4
School of Earth and
Environmental Sciences, University of Portsmouth, Burnaby
Road, Portsmouth, PO1 3QL, UK.
5
Laboratoire de
Géosciences, Faculté des Sciences Aïn Chock, Université
Hassan II, Casablanca, Morocco.
6
Intellectual Ventures, 3150
139th Avenue Southeast, Bellevue, WA 98005, USA.
7
Dipartimento di Scienze della Terra, Sapienza Università di
Roma, Piazzale Aldo Moro 5, 00185 Rome, Italy.
*Corresponding author. E-mail: nibrahim@uchicago.edu
RESEARCH |REPORTS
areprobablyreferabletoSpinosaurus (11)and
were possibly used in gaffing and slicing aquatic
prey suggest that the manus is proportionately
longer than in earlier spinosaurids (13,14).
Thepelvicgirdleandhindlimbareconsiderably
reduced in Spinosaurus (Fig. 2A). The surface
area of the iliac blade is approximately one-half
that in most other theropods (table S1), and the
supraacetabular crest that supports the hindlimb
is low (Fig. 2F). Hindlimb length is just over 25%
of body length (table S1). In a plot of forelimb,
hindlimb, and body length (Fig. 3), Spinosaurus
and other large theropods maintain fairly similar
forelimb lengths. Relative hindlimb length, however,
is noticeably less in the spinosaurid Suchomimus
(25%) and especially in Spinosaurus (19%) than
in other large tetanuran theropods.
Unlike other mid- or large-sized dinosaurs, the
femur in Spinosaurus is substantially shorter
than the tibia (Fig. 2, I and J, and table S1). In
smaller-bodied bipedal dinosaurs, short femoral
proportions indicate increased stride length and
enhanced speed. In Spinosaurus this is clearly
not the case, given the short hindlimb. The femur
in Spinosaurus has an unusually robust attach-
ment for the caudofemoral musculature, which
is anchored along nearly one-third of the femoral
shaft (Fig. 2I), suggesting powerful posterior
flexionofthehindlimb.Thearticulationatthe
knee joint for vertical limb support, in contrast,
is reduced. The distal condyles of the femur are
narrow, and the cnemial crest of the tibia is only
moderatelyexpanded(Fig.2,IandJ).Together
these features recall the shortened condition of
the femur in early cetaceans (19,20) and in extant
semiaquatic mammals that use their hindlimbs
in foot-propelled paddling (21).
Pedal digit I is unusually robust and long in
Spinosaurus:UnlikeAllosaurus or Tyrannosaurus,
1614 26 SEPTEMBER 2014 VOL 345 ISSUE 6204 sciencemag.org SCIENCE
Fig. 1. Geographic location and stratigraphic
position of the neotype skeleton of S. aegyptiacus.
(A) Locality (X), situated 18 km northeast of Erfoud
in southeastern Morocco. (B) Stratigraphic position
at the base of the upper unit of the Kem Kem beds,
with correlative positions of associated remains
of contemporary dinosaurs. Abbreviations: c, clay;
CT, Cenomanian-Turonian limestone; p, pebbles; P,
Paleozoic; sd, sandstone; st, siltstone.
Fig. 2. Semiaquatic skeletal adaptations in S. aegyptiacus.(A) Skeletal reconstruction in swimming
pose showing known bones (red) based on size-adjusted, computed tomographic scans of the neotype
(FSAC-KK 11888), referred specimens, and drawings of original bones (1). (B) Rostral neurovascular
foramina in lateral view (MSNM V4047 and a digital restoration of the holotypic lower jaw). (C)Narial
fossa in lateral view (MSNM V4047). (D) Anterior dorsal vertebra (~D1) in lateral, anterior, and posterior
views (UCRC PV601). (E) Dorsal neural spine (D8) in left lateral view (FSAC-KK 11888). (F) Left ilium in
lateral view (FSAC-KK 11888). (G) Mid-caudal vertebra (~CA30, reversed) in anterior and left lateral
views (UCRC PV5). (H) Right manual II-1 phalanx in proximal, lateral, and dorsal views (FSAC-KK 11888).
(I) Left femur in lateral view (FSAC-KK 11888). (J) Right tibia (reversed) in lateral view (FSAC-KK 11888).
(K) Right pedal digit III ungual in dorsal, lateral, and proximal views (FSAC-KK 11888). Abbreviations: af,
articular facet; ag, attachment groove; at, anterior trochanter; C2, 10, cervical vertebra 2, 10; CA1, caudal
vertebra 1; cc, cnemial crest; ce, centrum; clp, collateral ligament pit; D13, dorsal vertebra 13; ded, dorsal
extensor depression; dip, dorsal intercondylar process; fl, flange; ft, fourth trochanter; ftu, flexor tubercle;
lco, lateral condyle; nf, narial fossa; ns, neural spine; nvfo, neurovascular foramina; poz, postzygapophysis;
prz, prezygapophysis; S1, 5, sacral vertebra 1, 5; sac, supraacetabular crest; tp, transverse process.
Institutional abbreviations: FSAC, Faculté des Sciences Aïn Chock, Casablanca; MSNM, Museo di
Storia Naturale di Milano; UCRC, University of Chicago Research Collection, Chicago. Scale bars, 10 cm
in(B)to(D),(G),(H),and(K);and20cmin(E),(F),(I),and(J).
RESEARCH |REPORTS
the first phalanx of digit I in Spinosaurus is
the longest nonungual phalanx in the pes (fig.
S1) and would have been in contact with the
substrate in a stationary pose. The pedal un-
guals are proportionally large, long, low, and
flat-bottomed (Fig. 2K and figs. S1 and S2),
features that differ markedly from the deeper
recurved unguals in other large theropods.
The unguals in Spinosaurus are reminiscent of
the flattened pedal unguals of shorebirds that
do not perch (22). In addition, the toes of some
shorebirds have fleshy lobes and interdigital
webbing that enhance foot-propelled propulsion.
The lengthened digit I and flattened pedal un-
guals in Spinosaurus suggestthatthefootmay
have been adapted to traversing soft substrates
or webbed for paddling.
Increasesinbonemassanddensityarecom-
mon skeletal modifications in terrestrial verte-
brates transitioning to a semiaquatic existence (23).
In Spinosaurus, this was achieved by enlarging
midline display structures, eliminating open med-
ullary cavities in the long bones, and increasing
bone density. In subadult Spinosaurus,thedorsal
neural spines are composed primarily of dense
bone with only a narrow central zone of cancel-
lous bone (Fig. 4D), and long bones have solid
shafts (Fig. 4, A and C) with no development of
the open medullary cavity that is present in other
theropods, including early spinosaurids (Fig. 4B).
Bone density within the long bones, in addition,
is 30 to 40% greater in Spinosaurus than in other
theropods (8).
We estimated a center-of-body mass for a
flesh rendering of Spinosaurus created over
the digital skeleton (8). Center-of-mass estimates
for several theropods have been expressed as
a percentage of femoral length measured an-
teriorly from the hip joint (24). The center of
massinabipedmustbelocatedoverthemid-
dle one-third of the pes to generate a plausible
mid-stance pose (25). In our flesh rendering of
Spinosaurus, the center of body mass is po-
sitioned in front of both the hip and knee joints
at a distance greater than femur length (fig. S3),
suggesting that forelimb support was required
during terrestrial locomotion. Spinosaurus ap-
pears to have been poorly adapted to bipedal
terrestrial locomotion. The forward position of
the center of mass within the ribcage may have
enhanced balance during foot-propelled locomo-
tion in water.
These adaptations suggest that Spinosaurus
was primarily a piscivore, subsisting on sharks,
sawfish, coelacanths, lungfish, and actinopterygian s
that were common in the Kem Kem river system
(5,7,11). A long narrow skull and powerful fore-
limbs are also present in earlier spinosaurids, which
like Spinosaurus (26) have been interpreted as
predominantly piscivorous (13,14,27,28).
The locomotor adaptations outlined above,
however, mark a profound departure in form and
function from early spinosaurids. Prominent
among these are the reduced pelvic girdle; short
hindlimb; short femur; and long, low, flat-bottomed
pedal unguals, all of which can be verified in
the second partial skeleton described by Stromer
as Spinosaurus B(2,8). We note here that Spino-
saurus must have been an obligate quadruped
on land, the first discovered among theropod
dinosaurs, given the usual horizontal sacroiliac
joint and the anterior location of the estimated
center of body mass (8). Baryonyx was interpreted
as a facultative quadruped, based on its long skull
and neck and robust humerus (27), but this was
not confirmed by the discovery of more complete
hindlimb remains of the related Suchomimus (13).
In Spinosaurus we infer foot-powered paddling
from the relatively short femur with hypertro-
phied flexor attachment and strong pedal digit
I, as occurs in semiaquatic mammals such as early
cetaceans (1921). Low, flat-bottomed pedal unguals
are coincident with digital lobes or webbing in
SCIENCE sciencemag.org 26 SEPTEMBER 2014 VOL 345 ISSUE 6204 1615
Fig. 3. Ternary morphospace plot comparing
forelimb, hindlimb, and body length. Fore li mb
(humerus + radius + metacarpal II), hindlimb (femur +
tibia + metatarsal III), and body length (from snout
tip to posterior extremity of pelvic girdle) are plotted
as percentages of the sum of forelimb, hindlimb,
and body lengths in S. aegyptiacus and other large
tetanuran theropods (data from Table 1). Blue zone
shows the range of forelimb length, from 7% (Tyran-
nosaurus) to 12% (Allosaurus). Hindlimb length
(red zone) ranges from 34% (Allosaurus)to19%
(Spinosaurus). Abbreviations: Ac, Acrocanthosaurus;
Al, Allosaurus;Sp,Spinosaurus;Su,Suchomimus;Ty,
Tyrannosaurus.
hind limb
forelimb
body
Ty
Ac
Al
10
60
20
Sp
Su
70
80
40
30
Fig. 4. Bone microstructure and dorsal spine form. (A) Mid-shaft thin section of the right femur of
S. aegyptiacus (FSAC-KK 11888). (B) Mid-shaft thin section of the right femur of Suchomimus tenerensis
(MNN GAD608). (C) Cross-sectional view of right manual II-1 phalanx of S. aegyptiacus (FSAC-KK 11888).
(D) Thin section of a dorsal neural spine (distal section) in S. aegyptiacus (FSAC-KK 11888). (E)Dorsal
vertebrae with tall neural spines and spinal tendons in a cleared and stained specimen of Trioceros
(Chamaeleo)cristatus (FMNH 19886). Abbreviations: cb, cancellous bone; ec, erosional cavities; Hb,
Haversian bone; mc, medullary cavity; ns, neural spine; pb, primary bone; sc, scapula; st, striae; te,
tendon of multisegment spinal muscle. Institutional abbreviations: FMNH, Field Museum of Natural
History. Scale bars, 2 cm in (A) and (C), 3 cm in (B), 5 mm in (D), and 1 cm in (E).
RESEARCH |REPORTS
shore birds (22), and interdigital webbing has
been reported in theropod dinosaurs (29).
Reduction of the pelvic girdle and hindlimb and
the concomitant enhancement of axial-powered
locomotion are common among semiaquatic
vertebrates. The flexibility of the tail and the
form of the neural spines in Spinosaurus suggest
tail-assisted swimming. Like extinct and extant
semiaquatic reptiles, Spinosaurus used lateral
undulation of the tail, in contrast to the vertical
axial undulation adopted repeatedly by semi-
aquatic mammals (20,21).
The dorsal sailin Spinosaurus, the tallest
axial structure documented among dinosaurs,
has been argued to be a thermoregulatory sur-
face, a muscle- or fat-lined hump (30), or a dis-
play structure. Stromer (1) drew an analogy to
the skin-covered neural spines of the crested
chameleon, Trioceros cristatus (Fig. 4E). As in
T. cristatus,thesailofSpinosaurus is centered
over the trunk (Fig. 2A). The shape and position-
ing of the spine are also similar, and the base of
the neural spine is expanded anteroposteriorly,
with edges marked by ligament scars (Fig. 2E).
In Trioceros, a tendon of multisegmental axial
musculature attaches to the expanded base of
the neural spine (Fig. 4E). The upper portion of
the spine has sharp anterior and posterior edges,
is marked by fine vertical striae (Figs. 2E and 4D),
and is spaced away from adjacent spines, un-
lik e the broader, contiguous, paddle-shaped dorsal
spines of other spinosaurids (13). The striated
surface, sharp edges, and dense, poorly vascular-
ized internal bone of the spines suggest that they
were wrapped snugly in skin and functioned as
a display structure that would have remained
visible while swimming.
REFERENCES AND NOTES
1. E. Stromer, Ahb. Königl. Bayer. Akad. Wissen. Math-Phys. Kl.28,
132 (1915).
2. E. Stromer, Abh. Königl. Bayer. Akad. Wissen. Math-Naturwissen.
Abt.22,179 (1934).
3. J. B. Smith, M. C. Lamanna, H. Mayr, K. J. Lacovara,
J. Paleontol. 80, 400406 (2006).
4. W. Nothdurft, J. Smith, The Lost Dinosaurs of Egypt (Random
House, New York, 2002).
5. P. Taquet, D. Russell,C. R. Acad. Sci. Paris 299,347353 (1998).
6. C. Dal Sasso, S. Maganuco, E. Buffetaut, M. A. Mendez, J. Vert.
Paleontol. 25, 888896 (2005).
7. P. C. Sereno et al., Science 272, 986991 (1996).
8. See the supplementary materials on Science Online.
9. R. Lavocat, in Comptes Rendus de la 19ème Congrès
Géologique International, Alger, 1952, session XII-3, 15 (1954),
pp. 6568.
10. L. Mahler, J. Vert. Paleont. 25, 236239 (2005).
11. D. A. Russell, Bull. Mus. Hist. Nat. Paris 18, 349402 (1996).
12. B. McFeeters, M. J. Ryan, S. Hinic-Frlog, C. Schröder-Adams,
H. Sues, Can. J. Earth Sci. 50, 636649 (2013).
13. P. C. Sereno et al., Science 282, 12981302 (1998).
14. A. J. Charig, A. C. Milner, Bull. Nat. Hist. Mus 53,1170 (1997).
15. C. Brochu, J. Vert. Paleontol. Mem. 7,22 (suppl. 4), 1138
(2002).
16. D. B. Leitch, K. C. Catania, J. Exp. Biol. 215, 42174230 (2012).
17. F. E. Novas, F. Dalla Vecchia, D. F. Pais, Rev. Mus. Argent.
Cien. Nat. 7, 167175 (2005).
18. F. E. Fish, G. V. Lauder, Annu. Rev. Fluid Mech. 38, 193224
(2006).
19. S. I. Madar, Adv. Vert. Paleobiol. 1, 353378 (1998).
20. P. D. Gingerich, Paleobiology 29, 429454 (2003).
21. F. E. Fish, IEEE J. Oceanic Eng. 29, 605621 (2004).
22. A. Manegold, Acta Ornithol. 41,7982 (2006).
23. E. Amson, C. de Muizon, M. Laurin, C. Argot, V. de Buffrénil,
Proc. Biol. Sci. 281, 20140192 (2014).
24. K. T. Bates, R. B. J. Benson, P. L. Falkingham, Paleobiology 38,
486507 (2012).
25. S. M. Gatesy, M. Bäker, J. R. Hutchinson, Paleobiology 29,
535544 (2009).
26. E. Stromer, Abh. Königl. Bayer. Akad. Wissen. Math.-Naturwissen.
Abt. 33,1102 (1936).
27. A. J. Charig, A. C. Milner, Nature 324, 359361 (1986).
28. E. J. Rayfield, A. C. Milner, V. B. Xuan, P. G. Young,
J. Vert. Paleontol. 27, 892901 (2007).
29. M. L. Casanovas Cladellas et al., España Zub. Monogr. 5,
135163 (1993).
30. J. B. Bailey, J. Paleontol. 71, 11241146 (1997).
ACKNOW LEDGMENT S
We thank C. Abraczinskas for final drafts of all text figures;
M. Auditore for discussions and drawings; T. Keillor, L. Conroy,
and E. Fitzgerald for image processing and modeling; R. Masek,
T. Keillor, E. Fitzgerald, and F. Bacchia for fossil preparation;
C. Straus, N. Gruszauskas, D. Klein, and the University of Chicago
Medical Center for computed tomographic scanning; M. Zilioli,
F. Marchesini, M. Pacini, E. Lamm, and P. Vignola for preparation of
histological samples; A. Di Marzio (Siemens Milano) and P. Biondetti
(Fondazione Ospedale Maggiore Istituto di Ricovero e Cura a
Carattere Scientifico, Milan) for computed tomography scanning and
rendering of MSNM V4047; and the Island Fund of the New York
Community Trust and National Geographic Society (grant
SP-13-12) for support of this research. N.I. was also supported by
NSF grant DBI-1062542. We also thank the embassy of the
Kingdom of Morocco in Washington, DC, for their continued
interest in this project. Skeletal measurements and geologic data
are included in the supplementary materials. The neotype is going to
be deposited at the Faculté des Sciences Aïn Chock (University of
Casablanca), Casablanca, Morocco.
SUPPLEMENTARY MATERIALS
www.sciencemag.org/content/345/6204/1613/suppl/DC1
Supplementary Text
Figs. S1 to S8
Tables S1 to S5
References (3148)
15 July 2014; accepted 3 September 2014
10.1126/science.1258750
NEUROSCIENCE
A critical time window for dopamine
actions on the structural plasticity
of dendritic spines
Sho Yagishita,
1,2
Akiko Hayashi-Takagi,
1,2,3
Graham C.R. Ellis-Davies,
4
Hidetoshi Urakubo,
5
Shin Ishii,
5
Haruo Kasai
1,2
*
Animal behaviors are reinforced by subsequent rewards following within a narrow time
window. Such reward signals are primarily coded by dopamine, which modulates the
synaptic connections of medium spiny neurons in the striatum. The mechanisms of the
narrow timing detection, however, remain unknown. Here, we optically stimulated
dopaminergic and glutamatergic inputs separately and found that dopamine promoted
spine enlargement only during a narrow time window (0.3 to 2 seconds) after the
glutamatergic inputs. The temporal contingency was detected by rapid regulation of
adenosine 3,5-cyclic monophosphate in thin distal dendrites, in which protein-kinase
A was activated only within the time window because of a high phosphodiesterase
activity. Thus, we describe a molecular basis of reinforcement plasticity at the level of
single dendritic spines.
Animal behaviors are reinforced only when
rewarded shortly after a motor or sensory
event (1,2). The neocortex, hippocampus,
and amygdala process the sensorimotor
signals and send glutamatergic synaptic out-
put to the striatum (3), where connections can
be modified by Hebbian learning mechanisms,
such as spike-timing-dependent plasticity (STDP)
(4). Animals learn to associate the sensorimotor
signals with subsequent rewards through rein-
forcement of the neuronal circuits involving do-
pamine (57). Despite its importance, this narrow
timing detection has never been demonstrated at
the cellular level and might be ascribed to neural
network properties (6,8).
Dendritic spine morphology is correlated with
spine function (9), and dendritic spines enlarge
during long-term potentiation in the cortices
(1012). We examined the effects of dopamine
on the structural plasticity in striatal medium
spiny neurons (MSNs). Results show that do-
pamine affected spine structural plasticity in a
narrow time window consistent with behav-
ioral conditioning (5). Functional imaging revealed
the molecular interrelationships between the re-
inforcement and Hebbian plasticity.
We investigated dopamine actions on glutama-
tergic synapses on MSNs using optogenetics and
1616 26 SEPTEMBER 2014 VOL 345 ISSUE 6204 sciencemag.org SCIENCE
1
Laboratory of Structural Physiology, Center for Disease
Biology and Integrative Medicine, Faculty of Medicine, The
University of Tokyo, Bunkyo-ku, Tokyo 113-0033, Japan.
2
Core Research for Evolutional Science and Technology,
Japan Science and Technology Agency, Japan Science and
Technology Agency, 4-1-8 Honcho, Kawaguchi, Saitama
332-0012, Japan.
3
Precursory Research for Embryonic
Science and Technology, Japan Science and Technology
Agency, Japan Science and Technology Agency, 4-1-8
Honcho, Kawaguchi, Saitama 332-0012, Japan.
4
Department
of Neuroscience, Mount Sinai School of Medicine, New York,
NY 10029, USA.
5
Integrated Systems Biology Laboratory,
Department of Systems Science, Graduate School of
Informatics, Kyoto University, Sakyo-ku, Kyoto 606-8501,
Japan.
*Corresponding author. E-mail: hkasai@m.u-tokyo.ac.jp
RESEARCH |REPORTS
... Any familiarity with Mesozoic dinosaur research will reveal that possible aquatic behaviour is one of the most contested issues in the field, but only as it pertains to spinosaurids (Ibrahim et al. 2014(Ibrahim et al. , 2020a(Ibrahim et al. , 2020bHenderson 2018;Hone and Holtz 2021;Fabbri et al. 2022;Sereno et al. 2022;Myhrvold et al. 2024) Halszkaraptorines appear to have superficially recalled long-tailed, short-winged geese in life, and their tooth shape, snout form, limb proportions and body shape suggest specialisation for swimming and diving; this view has been contested (Brownstein 2019), albeit via erroneous argumentation (Cau 2020). A wading, piscivorous lifestyle has also been suggested for the allied unenlagiines on the basis of tooth form and an elongated face (e.g. ...
... The real area of controversy concerns spinosaurids, and Spinosaurus specifically. The case for an aquatic Spinosaurus was made on the basis of its crocodile-like facial skeleton with retracted external nostrils and semi-conical teeth, short hindlimbs, flattened ungual phalanges, thickened bone walls and an unusually flexible tail (Ibrahim et al. 2014). This interpretation of Spinosaurus did not emerge de novo, instead representing the culmination of four decades in which spinosaurids as a whole were regarded as aquatic or amphibious (Taquet 1984;Milner 1986, 1997;Paul 1988;Buffetaut 1989;Bakker et al. 1992;Špinar and Currie 1994;Holtz 2007;Amiot et al. 2010;Bertin 2010): 'Spinosaurus and Baryonyx may . . . ...
... spent much of its life in water' (Špinar and Currie 1994, p. 96). It must also be noted that Ibrahim et al.'s (2014) interpretation of Spinosaurus as an aquatic pursuit predator has been contested and an alternative model posits it as an amphibious wader (Henderson 2018;Hone and Holtz 2021;Sereno et al. 2022;Myhrvold et al. 2024). ...
... Other studies (e.g. Ibrahim et al. 2014a, Smyth et al. 2020b) considered NHMUK PV R 16420, MSNM V4047, and MNHN SAM 124 to belong to Spinosaurus aegyptiacus. Nevertheless, as previous work has suggested (e.g. ...
... Evers et al. 2015, Malafaia et al. 2020, Isasmendi et al. 2024, and as in Spinosaurus aegyptiacus, including the neotype FSAC-KK 11888 (e.g. Carrano et al. 2012, Ibrahim et al. 2014a, Schade et al. 2023. ...
... Furthermore, the hypertrophied dorsal neural spine is much taller than that of non-spinosaurid tetanuran theropods such as Acrocanthosaurus (Stovall and Langston 1950), and other spinosaurids such as Baryonyx, Ichthyovenator, and Suchomimus (Charig and Milner 1997, Sereno et al. 1998, Allain et al. 2012. Similarly, hypertrophied neural spines occur in the spinosaurines Spinosaurus aegyptiacus and FSAC-KK 11888, which are also directed anterodorsally (Stromer 1915, Smith et al. 2006, Ibrahim et al. 2014a) as the condition noted in NHMUK PV R 16431. The neural spines of the dorsal vertebrae described here further resemble the African spinosaurines, e.g. in NHMUK PV R 16431, the neural spine widens anteroposteriorly near the base of the neural spine, then narrows dorsally, and after this constriction it widens again, but gradually in the same way as occurs in Spinosaurus aegyptiacus (Stromer 1915, Smith et al. 2006, Ibrahim et al. 2014a. ...
Article
The Kem Kem Group is a lowermost lithostratigraphic unit from the Upper Cretaceous that extends along the border between Algeria and Morocco, in the northern region of Africa. This geological unit has yielded several tetrapod fossils, including a well-represented assemblage of theropod dinosaurs, after more than eight decades of research. Here, we report new occurrences of spinosaurid theropods from the spinosaurine clade in the Kem Kem Group by providing anatomical descriptions and taxonomic identifications of 11 new specimens derived from the Tafilalt region of Morocco. Among the findings, we describe a cervical vertebra of Sigilmassasaurus, in addition to several cranial, axial, and appendicular elements that can safely be attributed to Spinosaurinae. Moreover, based on a unique combination of characteristics, we also describe an isolated and partial ischium belonging to an indeterminate carcharodontosaurid. We also deliver a detailed redescription of one of the most complete snouts of a spinosaurine known to date. Therefore, the theropod dinosaurs of the Kem Kem Group show considerable diversity, but many questions, especially related to the diversity of spinosaurids and the general abundance of carnivorous dinosaurs in this region, remain unclear until new materials are discovered and complete descriptions are made.
... The Cenomanian-age Kem Kem beds are a sequence of 150-200 m thick fluvial siltstones and sandstones that extend over 250 km at the southeastern border of Morocco (Ibrahim et al., 2014b;Sereno et al., 1996) (Fig. 1). The Kem Kem beds are divided into the Lower Gara Sbaa and Upper Douira Formations based on their different lithologies. ...
... Besides Spinosaurus, various aquatic and semiaquatic vertebrate species were also discovered in this group, and they formed the majority of this faunal assemblage (Ibrahim et al., 2020a;Läng et al., 2013;Smith et al., 2023). The rich assemblage of aquatic species and low-energy fluvial sediments suggests that the Lower Kem Kem beds were a palaeo-delta fed by a vast river system flowing in a south-north direction, along with abundant overbank, lacustrine and tidal-flat palaeoenvironments (Guiraud et al., 2005;Ibrahim et al., 2014bIbrahim et al., , 2020a. ...
Article
Full-text available
Oxygen isotope compositions in tooth dentine of Spinosaurus aegyptiacus were investigated as a potential proxy for high-resolution reconstructions of palaeoenvironments in Cenomanian Cretaceous Morocco. The dentine was sampled sequentially along the tooth growth direction, and the successive δ 18 O values exhibited cycles which likely tracked the oxygen isotope compositions of ingested water and inferred changes in additional palae-oenvironmental properties. A conceptual model of catchment palaeohydrology was reconstructed to explain the mechanisms of isotopic variation. Seasonally variable water balance in the catchment or changes in water sources throughout the extensive deltaic environments are the most likely explanations for the seasonal profiles. With analysis of isotopic change in the conceptual model and comparison with data of modern tropical and subtropical deltas, we found similarities between palaeoclimates and modern data, and effectively identified the wet and dry seasons represented by troughs and peaks in the δ 18 O curves. These preliminary results demonstrated that palaeoenvironmental information at sub-seasonal resolution can be well preserved in theropod tooth dentine. The methodology developed in this study can be applied to the existing abundant reserves of theropod teeth to construct a Mesozoic palaeoclimatic database.
... Vertebrate fossils from the Moroccan Kem Kem Group are often directly compared to the lost material of the Bahariya Formation, with a special focus on the theropods of both formations, which are often claimed to be conspecific (e.g. [7,155]). At first glance, these comparisons appear reasonable based on the supposed similar age (Cenomanian age for the Bahariya Formation [156,157] and Albian to Cenomanian age for the Kem Kem Group [17,18,158]) and similar faunal composition of both strata, although this is partially circular reasoning, as the similar faunal composition is used to infer the similar age. ...
... While the abelisaurid is not yet named in either formation, the theropod species Spinosaurus aegyptiacus, Sigilmassasaurus brevicollis and Carcharodontosaurus saharicus are often claimed to be present in both formations (e.g. [18,59]), with the neotypes of Spinosaurus and Carcharodontosaurus proposed from Moroccan material [8,155]. Furthermore, the enigmatic Moroccan Deltadromeus was initially compared to Bahariasaurus by Sereno et al. [7], who also referred some of the Egyptian material described by Stromer in 1934 to Deltadromeus. ...
Article
Full-text available
The first partial skeleton of a carcharodontosaurid theropod was described from the Egyptian Bahariya Oasis by Ernst Stromer in 1931. Stromer referred the specimen to the species Megalosaurus saharicus, originally described on the basis of isolated teeth from slightly older rocks in Algeria, under the new genus name Carcharodontosaurus saharicus. Unfortunately, almost all of the material from the Bahariya Oasis, including the specimen of Carcharodontosaurus was destroyed during World War II. In 1996, a relatively complete carcharodontosaurid cranium was described from similar aged rocks in Morocco and designated the neotype of the species Carcharodontosaurus saharicus in 2007. However, due to the destruction of the original material, comparisons of the neotype to the Egyptian fossils have so far only been done cursorily. A detailed reexamination of the available information on the Egyptian carcharodontosaurid, including a previously undescribed photograph of the exhibited specimen, reveals that it differs from the Moroccan neotype in numerous characters, such as the development of the emargination of the antorbital fossa on the nasals, the presence of a horn-like rugosity on the nasal, the lack of a dorsoventral expansion of the lacrimal contact on the frontals, and the relative enlargement of the cerebrum. The referability of the Egyptian specimen to the Algerian M. saharicus is found to be questionable, and the neotype designation of the Moroccan material for C. saharicus is accepted here under consideration of ICZN Atricle 75, as it both compares more favorably to M. saharicus and originates from a locality closer to the type locality. A new genus and species, Tameryraptor markgrafi gen. et sp. nov, is proposed for the Egyptian taxon. The theropods of the Bahariya Oasis and the Moroccan Kem Kem Group are thus not as closely related as previously thought, and the proposed faunal similarities between these two strata need further examination.
... During the Aptian-Turonian time span interval, abelisaurids, noasaurids, carcharodontosaurids and spinosaurids shared the environments [9]. The ecological niche of Spinosaurid could be different to abelisaurids and carcharodontosaurids [44], suggesting that niche overlap between those theropod groups was unlikely. In contrast abelisaurids and carcharodontosaurids exhibited similar mechanical advantages scores related to the leverage of the jaw systems [45] and convergent dental morphology [33]. ...
Article
Full-text available
Patterns of body size evolution in dinosaurs are relevant for understanding the evolutionary trends that have shaped the disparity of phenotypes observed in the fossil record. In this sense, previous studies have suggested that Abelisau-ridae followed Cope´s rule and Noasauridae exhibited a phylogenetic trend towards decreasing body size. However, the absence of a comprehensive analysis including ecological, phylogenetic and socio-sexual factors make it necessary to reevaluate body size evolution in Ceretatosauria under a modern phylogenetic comparative approach. Therefore, we aimed to test whether body size evolved in Ceratosauria in accordance with Cope´s rule, evaluate what factors best explain differences in body size within Ceratosauria and examine what patterns of evolution rates, selection strength and constrain explain the diversification body size in Ceratosauria. Differences in body size were found between specialized taxa (= Late Cretaceous abelisaurids) and "generalized taxa" (= Outgroups + Noasauridae). This results suggested that the presence of a specialized feeding strategy in Late Cretaceous abelisaurids was associated with differences in body size, regardless of the phylogenetic topology and evolutionary model used. Additionally, the low levels of morphological disparity, low evolutionary rates for taxa with a specialist feeding behavior in Brown-ian motion model and the fossil record suggest that the evolution of body size in Late Cretaceous abelisaurids was constrained. The cursorial abilities suggested for abelisaurids joined with the specialized predation strategy could have constrained the increase in body size in Late Cretaceous abelisaurids after the extinction of carcharodontosau-rids. On the other hand, Noasauridae exhibited a phylogenetic trend towards decreased body size, likely to avoid niche overlap with medium size theropods and minimize structural and maintenance cost while living in stressful environments and having a generalist diet. Understanding how the dynamics of dinosaur communities, such as competition and predator-prey interactions, operated in South America during the Late Cretaceous is crucial for reconstructing the evolutionary and ecological processes that shaped its unique faunal assemblage. Futures works should be focus on process-based community-evolution model and species distribution modeling to further understand the macroevolution dynamics of South America dinosaur community.
... The facet for the ascending process of the astragalus is proximodistally tall, and is bounded proximally by a median buttress. This distinguishes it from large non-noasaurid ceratosaurs, in which the facet for the ascending process is proximodistally short and lacks a medial buttress (Chatterjee & Rudra, 1996;Kellner & Campos, 2002;Machado et al., 2013;Pol et al., 2024;Valieri et al., 2007); Noasauridae, in which the facet for the ascending process is flat (Rauhut, 2005(Rauhut, , 2011Rauhut & Carrano, 2016;Sereno, 2017); Spinosauridae, in which the ridge is absent and the facet is bounded medially by a vertical ridge (Ibrahim et al., 2014;Rauhut, 2003); and Coelurosauria, wherein the ridge is absent and the anterior surface is essentially flat (Rauhut, 2003). The median buttress emarginates the facet proximally as an oblique ridge, unlike the step-like ridge of Megalosauroidea (e.g., Megalosaurus bucklandii [Benson, 2010], Torvosaurus gurneyi [Hendrickx & Mateus, 2014]) and non-carcharodontosaurian Allosauroidea (e.g., Sinraptor dongi [Currie & Zhao, 1993] and Allosaurus fragilis [Madsen, 1976]). ...
Article
The Early Cretaceous non-avian theropod body fossil record of Victoria, Australia dominantly comprises isolated dental and postcranial remains. Numerous specimens have been collected from both the upper Strzelecki Group (upper Barremian–lower Aptian) and Eumeralla Formation (upper Aptian–lower Albian), yet theropod diversity in each unit remains poorly resolved. In both deposits, specimens pertaining to Megaraptoridae—a clade seemingly endemic to South America and Australia in the Cretaceous—are most frequently encountered. However, evidence of other typically common Gondwanan theropod groups, including Abelisauridae and Carcharodontosauria, has remained unknown. Herein, we describe five new theropod specimens: three tibiae, and two articulated caudal vertebrae with haemal arches, from the upper Strzelecki Group; and a single tibia from the Eumeralla Formation. Two of these tibiae—one each from the upper Strzelecki Group and the Eumeralla Formation—provide the first evidence for Carcharodontosauria in Australia. Two megaraptorid specimens from the upper Strzelecki Group—a tibia, and two caudal vertebrae with haemal arches—demonstrate that this clade had achieved large body size at the time of its first appearance in the fossil record. A tibia from the upper Strzelecki Group is interpreted to represent the Gondwanan dromaeosaur clade Unenlagiinae. Collectively, the new theropod remains described herein strengthen the evidence for mid-Cretaceous faunal interchange between Australia and South America across Antarctica, and highlight the presence of carcharodontosaurians and unenlagiines at high latitudes in the late Early Cretaceous.
... That period of relative silence was shattered in 2014 when Ibrahim et al. (2014) published an analysis of a remarkably complete specimen, establishing it as a neotype. They emphasized various aquatic adaptations: non-pneumatized bones, a long-neck and thin-jawed morphology often associated with fish-eating, nostrils placed midway up the skull reminiscent of the raised nostrils of crocodilians and hippopotamus, shorter hindlimbs and reduced pelvis relative to other theropods, and so forth. ...
Article
Full-text available
Paleobiology is not only a science of the deep past: it is a science of deep possibility. Drawing on recent speculative reconstructions of Spinosaurus aegyptiacus, I sketch a new account of paleobiological reconstruction. Fossils, as opposed to testing causal hypotheses, are used to characterise and evidence the ‘central subjects’ of paleobiological reconstruction, in this instance, particular dinosaur taxa. These central subjects are then situated in various ‘profiles’, representational tools which isolate particular traits across several dimensions in order to apply comparative methods which generate and test often modal hypotheses. I suggest this represents a particular phenomena-driven mode of exploring possibility, one with distinct advantages over approaches more common in theoretical evolutionary biology.
Article
Noasaurus leali is a small (~2 m) carnivorous theropod and the nominal genus of the clade Noasauridae, one of the two radiations of abelisauroid ceratosaurs predominantly present in the Southern Hemisphere during the Mesozoic. This eponymous theropod from the Maastrichtian Lecho Formation of Salta, Argentina, is known from an incomplete skeleton of which the strongly curved manual ungual is the most peculiar element. We here provide for the first time a comprehensive description of the holotypic specimens of Noasaurus, whose phylogenetic position was explored using three independent datamatrices on theropod relationships. This species is diagnosed by several apomorphies such as a dorsal ridge in the maxillary fossa, a strongly arched quadrate, a cervical neural arch with anterior epipophyseal prongs, and a manual ungual with a subtriangular flexor fossa delimited by a V-shaped ridge. Results of the phylogenetic analyses recovered Noasaurus closely related to Velocisaurus, Masiakasaurus, and Laevisuchus, which together form a Late Cretaceous radiation of small-bodied noasaurids restricted to the Southern Hemisphere. The peculiar morphology of the lateral dentition and manual unguals suggests that Noasaurus was an opportunistic carnivore feeding on small prey items and a possible piscivore gaffing fish with its specialized hand claws.
Article
Full-text available
It is often not immediately clear to museum visitors that everything they see, read, hear during their visit is the result of research and study work carried out by the management and specialists of the departments into which the museum institution is divided. Yet everything that is under the control of their senses and their perception would not exist without research work, sometimes long, always passionate: before being placed in the showcase, each specimen on display has in fact passed the scrutiny of rigorous studies, has been investigated from many points of view and finally has been deemed worthy of being brought to the admiration of the visitor. Other specimens,.... [...]
Article
Spinosaurids were common elements from dinosaur faunas during the Early Cretaceous in western Europe, with isolated teeth being the most common fossils registered in the fossil record. Here, some isolated spinosaurid teeth from the municipality of Galve (province of Teruel, Spain) are studied. They come from the lower Barremian (Lower Cretaceous) deposits of the Camarillas Formation of Western Maestrazgo Basin. These fossils are described and compared with related taxa, and analyzed with morphometric (discriminant and cluster analyses) and cladistic methods when possible. One tooth was classified as Spinosauridae indet., while the other two specimens were assigned to Baryonychinae indet. and Spinosaurinae indet., respectively. The indeterminate baryonychine tooth closely resembles a particular morphotype with an unserrated mesial carina and fluted enamel on both lingual and labial surfaces present in the Iberian Peninsula, unlike those of Baryonyx and Iberospinus. The spinosaurine tooth represents a new morphotype, which is distinguished from other teeth found in the Barremian of Teruel for having mesial and distal unserrated carinae and fluted enamel on both the lingual and labial surfaces. These teeth not only suggest the presence of at least one baryonychine and one spinosaurine taxa during the early Barremian in the eastern Iberian Peninsula, but also support their presence in fluvial systems with some marine influence where other dinosaurs have been broadly identified, such as styracosternan ornithopods.
Article
Full-text available
Several dinosaurs, notably Ouranosaurus and Spinosaurus, have vertebral columns marked by prominent arrays of elongated neural spines. Using pelycosaurian sailbacks like Dimetrodon as analogies, popular orthodoxy holds that the tall spines served as supporting struts for dorsal sails of purported thermoregulatory function, especially heat dissipation in tropical climates. It is argued here that the neural spines of Ouranosaurus, Spinosaurus, and several other long-spined dinosaurs favor bison-like humps rather than sails: 1) in functional morphology and relative elongation they are dissimilar to pelycosaur spines but homoplastically converge on the spines of high-withered ungulates; 2) the usefulness of a sail in thermoregulation has been exaggerated—in large tetrapods it would have been fairly efficient as a thermal amplifier but ineffective as a radiator; hence large sail-bearing dinosaurs in open tropical climates are improbable; 3) the insulation properties of humps favor gigantothermy, the most likely thermobiological model for large dinosaurs. Dinosaur humps are probable adaptations for: 1) energy storage, maintenance of gigantothermy, and heat-shielding in unshaded habitats; 2) long-distance migration from feeding to nesting grounds across terrains of variable productivity; and 3) lipid conservation for production of large clutches of eggs at the nesting site. Because sacral, caudal, or dorsal humps were relatively common traits among certain groups, the fashionably anorexic image of many large dinosaurs must be emended.
Article
Full-text available
This text has been greatly enriched since its publication. There are two other books including in French (Techno-logic & Technology A Paleo-history of Sharp Lithic Objects" then later in English (Techno-logic & Technology: A Paleo-history of Knapped Lithic Objects), and Spanish "Techno-lógica & Technología Une Paleo-historia de los objetos líticos cotantes" the third and last is still in French (The technical phenomenon in prehistory: an epistemological reflection from and around Levallois). I strongly advise you to follow this trilogy resulting from a current of French technology which has been developed over more than 30 years, by exploring new voices.
Article
Full-text available
We investigate whether musculoskeletal anatomy and three-dimensional (3-D) body proportions were modified during the evolution of large (>6000 kg) body size in Allosauroidea (Dinosauria: Theropoda). Three adaptations for maintaining locomotor performance at large body size, related to muscle leverage, mass, and body proportions, are tested and all are unsupported in this analysis. Predictions form 3-D musculoskeletal models of medium-sized (Allosaurus) and large-bodied (Acrocanthosaurus) allosauroids suggest that muscle leverage scaled close to isometry, well below the positive allometry required to compensate for declining muscle cross-sectional area with increasing body size. Regression analyses on a larger allosauroid data set finds slight positive allometry in the moment arms of major hip extensors, but isometry is included within confidence limits. Contrary to other recent studies of large-bodied theropod clades, we found no compelling evidence for significant positive allometry in muscle mass between exemplar medium- and large-bodied allosauroids. Indeed, despite the uncertainty in quantitative soft tissue reconstruction, we find strong evidence for negative allometry in the caudofemoralis longus muscle, the single largest his extensor in non-avian theropods. Finally, we found significant inter-study variability in center-of-mass predictions for allosauroids, but overall observe that consistently proportioned soft tissue reconstructions produced similar predictions across the gorup, providing no support for a caudal shift in the center of mass in larger taxa that might otherwise reduce demands on hip extensor muscles during stance. Our data set provides further quantitative support to studies that argue for a significant decline in locomotor performance with increasing body size in non-avian theropods. However, although key pelvic limb synapomorphies of derived allosauroids (e.g., dorsomedially inclined femoral head)evolved at intermediate body sizes, they may nonetheless have improved mass support.
Article
The 'Gres rouges infracenomaniens' of southern Morocco, possibly of Albian age, contain evidence of one of the most diversified dinosaur assemblages known from Africa, including a relatively long-necked species of Spinosaurus and abundant but isolated bones of a peculiar theropod ('Spinosaurus B' of Stromer 1934). Also preserved are the oldest records of abelisaurids and among the oldest records of titanosaurids in Africa. Bones of infantile didnosaurs are present. The assemblage resembles that of the Bahariya Formation more than that of Gadoufaoua, possibly because of a trophic dependence upon large, freshwater fishes. It was more closely linked zoogeographically to South America than to North America.
Article
Noasauridae is a clade of ceratosaurian theropods that evolved small body size independently of other non-avian theropods. The best-preserved and most complete noasaurid is Masiakasaurus knopfleri from the Maastrichtian-aged Maevarano Formation in Madagascar. An abundance of skeletal material from several individuals spanning a wide range of ontogeny makes Masiakasaurus an ideal candidate for the analysis of growth. We histologically sampled a growth series of elements consisting of four femora and three tibiae. Bright-field and circularly polarized light microscopy were used to distinguish between slowly and rapidly growing forms of bone. To simultaneously estimate age at death and reconstruct growth trajectories, we measured the perimeters of growth lines in each specimen and fitted models to these data using a novel application of mixed-effects regression. Our histological results show an external fundamental system in the largest tibial specimen and confirm that Masiakasaurus grew determinately, matured at small body size, and is not the juvenile form of a larger-bodied theropod. Parallel-fibered bone is unusually prominent and suggests relatively slow growth. Moreover, our quantitative analysis shows that the average individual took about 8–10 years to get to the size of a large dog. Although Masiakasaurus grew 40% faster than crocodylians, it grew about 40% slower than comparably sized non-avian theropods. Slowed growth may have evolved as a means to minimize structural and maintenance costs while living in a semiarid and seasonally stressful environment. Dimorphism does not appear related to asymptotic size or growth rate but seems to reflect the degree of skeletal maturity.SUPPLEMENTAL DATA—Supplemental materials are available for this article for free at www.tandfonline.com/UJVP
Article
Pliosaurs were among the largest predators in Mesozoic seas, and yet their functional anatomy and feeding biomechanics are poorly understood. A new, well-preserved pliosaur from the Kimmeridgian of Weymouth Bay (UK) revealed cranial adaptations related to feeding. Digital modelling of computed tomography scans allowed reconstruction of missing, distorted regions of the skull and of the adductor musculature, which indicated high bite forces. Size-corrected beam theory modelling showed that the snout was poorly optimised against bending and torsional stresses compared with other aquatic and terrestrial predators, suggesting that pliosaurs did not twist or shake their prey during feeding and that seizing was better performed with post-symphyseal bites. Finite element analysis identified biting-induced stress patterns in both the rostrum and lower jaws, highlighting weak areas in the rostral maxillary-premaxillary contact and the caudal mandibular symphysis. A comparatively weak skull coupled with musculature that was able to produce high forces, is explained as a trade-off between agility, hydrodynamics and strength. In the Kimmeridgian ecosystem, we conclude that Late Jurassic pliosaurs were generalist predators at the top of the food chain, able to prey on reptiles and fishes up to half their own length.
Article
The femoral microanatomy of 155 species of extant amniotes (57 species of mammals, 15 species of turtles, 56 species of lepidosaurs, and 27 species of birds) of known lifestyle is studied to demonstrate a possible link between some basic parameters of bone structure and specific lifestyles, as well as phylogenetic relationships between taxa. Squared change parsimony with random taxon reshuffling and pairwise comparisons reveal that most compactness and size parameters exhibit both phylogenetic and ecological signals. A discriminant analysis produces several inference models, including a ternary model (aquatic, amphibious, terrestrial) that yield the correct lifestyle in 88% of the cases. These models are used to infer the lifestyle of three extinct Permian temnospondyls: Eryops megacephalus, Acheloma dunni, and Trimerorhachis insignis. © 2013 The Linnean Society of London, Biological Journal of the Linnean Society, 2013, 109, 644–655.