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US ISSN 0006-9698

CAMBRIDGE, MaAss. 8 May 2012 NUMBER 529

A NEW AMBER-EMBEDDED SPHAERODACTYL GECKO FROM HISPANIOLA,
WITH COMMENTS ON MORPHOLOGICAL SYNAPOMORPHIES OF
THE SPHAERODACTYLIDAE

JUAN D. DAZA! AND AARON M. BAUER!-2

AsstrRAct. A new species of Sphaerodactylus (Squamata: Gekkota: Sphaerodactylidae) is described from an
amber inclusion from the late Early Miocene or early Middle Miocene (15 to 20 million years ago) of the Dominican
Republic. Unlike earlier amber-embedded specimens assigned to this genus, the new specimen is largely skeletal, with
some integument remaining. A combination of 258 (of 674) osteological and external characters could be scored for
the new species in a cladistic analysis of 21 gekkotan species, including representatives of all sphaerodactylid genera.

The most parsimonious trees obtained confirm the placement of the amber gecko within the genus Sphaerodactylus
and a comparison with extant Hispaniolan and Puerto Rican congeners suggests phenetic similarity both with
members of S. difficilis complex and the S. shrevei species group. Character mapping on the basis of the phylogenetic
analysis permits the preliminary identification of morphological characters diagnostic of the Sphaerodactylidae,
Sphaerodactylini, and Sphaerodactylus. Osteological features of the new species are discussed in the broader context
of sphaerodactyl, sphaerodactylid, and gekkotan variation. Extant Hispaniolan Sphaerodactylus display significant
ecomorphological variation and it is likely that the many known, though not yet described, amber-embedded
specimens will eventually reveal similar patterns in their Miocene congeners.

Key worps: Sphaerodactylus; Sphaerodactylidae; gecko; osteology; Hispaniola; new species; phylogeny

INTRODUCTION

Amber-embedded fossils provide unique
insights into extinct vertebrate taxa as they

' Department of Biology, Villanova University, 800 Lancaster
Avenue, Villanova, Pennsylvania 19085, U.S.A.; e-mail:
juan.daza@villanova.edu, aaron.bauer@villanova.edu.

> Department of Herpetology, Museum of Comparative
Zoology, Harvard University, 26 Oxford Street, Cam-
bridge, Massachusetts 02138, U.S.A. ~

frequently preserve the integument and
thus give an impression of what the intact
animal looked like in life. The mode of
amber preservation, however, limits verte-
brate inclusions to taxa small enough to be
trapped in the viscous resin. Thus, aside
from isolated bird feathers (e.g., Grimaldi
and Case, 1995; Alonso et al, 2000;
Perrichot et al, 2008) and mammal hairs
and bones (MacPhee and Grimaldi, 1996;

© The President and Fellows of Harvard College 2012.

i)

Sontag, 2008), known vertebrate inclusions
are limited to several minute frogs (Poinar
and Cannatella, 1987; Poinar, 1992; Grimaldi,
1996), unidentified (but probably squamate)
skin pieces (Poinar and Poinar, 1999; Grimaldi
et al., 2002; Perrichot and Néraudeau, 2005),
and to a fairly large number of small
lizards. At least four areas of the world
have yielded such lizard fossils. The oldest
inclusion is Baabdasaurus xenurus, an au-
tarchoglossan of indeterminate affinities
described from a partial specimen in amber
from the Lower Cretaceous (120 million
years ago [MYA]) of Lebanon (Arnold
et al., 2002). A 100-million-year-old gekko-
tan in amber, Cretaceogekko burmae, 1s
known from deposits in Myanmar (Arnold
and Poinar, 2008). Amber deposits of the
Baltic, dating from the early Eocene (Lars-
son, 1978; Ritzkowski, 1997; Weitschat and
Wichard, 2002), have yielded a minimum
of three different species in the extinct
lacertid genus Succinilacerta (Katinas, 1983;
Kosmowska-Ceranowicz et al., 1997a, 1997b;
Krumbiegel, 1998; Bohme & Weitschat, 1998,
2002; Borsuk-Bialynicka et al, 1999) and a
single gekkotan, Yantarogekko balticus (Bauer
et al., 2005).

The greatest number of amber lizards,
however, are known from the Miocene of the
Dominican Republic. These fossils include
several specimens referred to the dactyloid
genus Anolis (Lazell, 1965; Rieppel, 1980; de
Queiroz et al., 1998; Polcyn et al., 2002), and
several geckos referable to the extant genus
Sphaerodactylus (Bohme, 1984; Kluge, 1995).
Although a very limited number of lizards in
Dominican amber have been formally de-
scribed, many more specimens are known to
exist in the holdings of private collectors
(Poinar and Poinar, 1999; D. A. Grimaldi,
personal communication).

Biostratigraphic and paleogeographic data
indicate that the amberiferous deposits 1n the
Dominican Republic were formed in a single

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No. 529

sedimentary basin during the late Early
Miocene through early Middle Miocene,
about 15 to 20 MYA (Grimaldi, 1995;
Iturralde-Vinent and MacPhee, 1996). Am-
ber fossils from tropical America originate
mainly from the resin of the extinct legumi-
nous tree Hymenaea protera (Poinar and
Cannatella, 1987; Poinar, 1992; Iturralde-
Vinent, 2001), and on the basis of inference
from historical forest distribution in Hispa-
niola, these trees were mainly distributed in
the evergreen forests of the southeast area,
surrounding the depositional basin (Itur-
ralde-Vinent and MacPhee, 1996). Today,
Dominican amber is commercially exploited
in three geological formations: La Toca
(North), Yanigua (Eastern), and Sombrerito
(south of the Cordillera Central in the area
of Plateau Central-San Juan).

We here report on a new amber-embedded
gecko from La Toca mine, in the Cordillera
Septentrional, Santiago Province, north of
Municipio Santiago de los Caballeros
(Fig. 1). We further review osteological data
for the Sphaerodactylidae and identify puta-
tive synapomorphies that support the mono-
phyly of this recently recognized clade of
gekkotans. To date only two nonmolecular
characters, neither found in all members of
the clade, have been identified as possible
evidence of affinities:

1. presence of parafrontal bones (present
in Aristelliger and Teratoscincus and pre-
sumably lost in all miniaturized sphaerodac-
tylids) and

2. single-egg clutch (except in Teratoscincus
and Euleptes, which retain: two-egg clutches;
Gamble et al, 2008a).

MATERIALS AND METHODS

Anatomical Observations. Faked lizard
inclusions in amber are common, so the
authenticity of the specimen was confirmed
on the basis of several criteria intrinsic to both

2012

Figure 1.

A NEW AMBER GECKO FROM HISPANIOLA 3

La Toca Formation
Northern mining district

&

\
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< .
> Santiago de
«<< los Caballeros

pang Domingo

—)

DOMINICAN REPUBLIC

0 100 km
hott —

Left, black areas indicate the distribution of Sphaerodactylus geckos in the Americas. Right, map of

Hispaniola showing the type locality of Sphaerodactylus ciguapa sp. nov. (modified from Iturralde-Vinent, 2001).

the amber itself and the lizard it contained
(Bauer and Branch, 1995). The amber specimen
and comparative ethanol-preserved, cleared
and stained, and dry skeletal material were
examined using a Nikon SMZ1000 dissecting
microscope equiped with a digital camera
(Nikon DS-Fil) and the image acquisition
software NIS Elements D v. 3.1, and a Leica
MZ6 dissecting microscope equipped with a
camera lucida. Digital radiographs were ob-
tained using a Kevex™ PXS10-16W X-ray
source and Varian Amorphous Silicon Digital
X-Ray Detector PaxScan® 4030R set to 130 kV
at 81 uA. For each X-ray linear and pseudofilm
filters were used. Drawings were traced directly
over digital images using Adobe® Illustrator®
CS3 13.0.2 and complemented with illustra-
tions made with the camera lucida. Measure-
ments were made from the X-ray images to
avoid measurement error caused by the refrac-
tive index of amber (n = 1.55). Anatomical
terminology follows Daza et al. (2008).
_ Phylogenetic Analysis. To objectively iden-
tify characters uniting the new species with its
congeners and other members of the Spha-
erodactylidae, a cladistic analysis of selected
taxa was performed. A morphological data

set of 674 characters scored for 21 taxa
(Appendix 1; data available at www.morpho-
bank.org; project number p532, accession
number X1201) was analyzed in the computer
program T.N.T. (Goloboff et al, 2003a,
2008) using maximum parsimony. All char-
acters were treated as unordered, and equally
weighted. In addition to representatives of 12
sphaerodactylid genera, including all six
genera of “sphaerodactyls,” seven outgroup
gekkotan species were included: Hemidactylus
brookii, Narudasia festiva, and Pseudogekko
smaragdinus (Gekkonidae), and Phyllodac-
tylus_ wirshingi, Gymnodactylus_ geckoides,
Thecadactylus rapicauda, and Tarentola maur-
itanica (Phyllodactylidae). Our sampling out-
side sphaerodactylids is minimal considering
the diversity of the Gekkota as a whole and
we recognize that taxon sampling may
significantly affect tree topology. However,
as our focus is on the characters that define
Sphaerodactylidae, sphaerodactyls, and Spha-
erodactylus we believe that this limitation will
not materially affect our results. Twenty
independent searches were done using de-
faults of “xmult” plus 10 cycles of tree drifting
(Goloboff, 1999). Support was estimated

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No. 529

amma

Figure 2.

through Bremer support indices (BS; Bremer,
1994), relative Bremer support indices (rela-
tive fit difference [RFD]; Goloboff and Farris,
2001), bootstraps, and symmetric resampling
(SR) expressed as GC values (difference in fre-
quencies for groups supported—contradicted;
Goloboff et al, 2003b).

External and osteological features of addi-
tional taxa of Sphaerodactylus and other
sphaerodactylids (Appendix 2) were also
compared in the course of diagnosing the
new species, but were not incorporated into
the phylogenetic analysis. Original descrip-
tions and other references (Schwartz and
Graham, 1980; Schwartz and Thomas, 1983;
Schwartz and Henderson, 1991) were consult-
ed for further information about body size
and scalation features of Sphaerodactylus spp.

Institutional Abbreviations. Material exam-
ined was obtained from the following collec-
tions: Aaron M. Bauer personal collection,
Villanova University, Villanova; (AMB);
American Museum of Natural History, New
York (AMNH); The Natural History Muse-
um, London (BMNH); California Academy
of Sciences, San Francisco (CAS); Field

Right lateral view of Sphaerodactylus ciguapa sp. nov. Scale bar = 5 cm.

Museum of Natural History, Chicago
(FMNH); James Ford Bell Museum, Univer-
sity of Minnesota, Saint Paul (JFBM):
Museum of Comparative Zoology, Harvard
University, Cambridge (MCZ); Museum of
Vertebrate Zoology, University of California,
Berkeley (MVZ), Museu de Zoologia, Uni-
versidade de Sao Paulo, Sao Paulo (MZUSP):
Sam Noble Oklahoma Museum of Natural
History, University of Oklahoma, Norman
(OMNH); Richard Thomas personal collec-
tion, Universidad de Puerto Rico, Rio Pie-
dras, Puerto Rico (RT); Museo de Zoologia,
Universidad de Puerto Rico, Rio Piedras
(UPRRP); United States National Museum,
Washington (USNM; USNMFH—Field Se-
ries); Coleccidn de Herpetologia de la Uni-
versidad del Valle, Cali, Colombia (UV-C).
Description of new species
Sphaerodactylus ciguapa Daza and Bauer,
new species
Figures 2—7

Holotype. MCZR-186380, amber-embedded,
nearly complete skeleton with patches of
integument. Collected from the late Early
Miocene to early Middle Miocene (15 to

A NEW AMBER GECKO FROM HISPANIOLA

9
sacrum “a

pelvic girdle right pes

pygial
vertebrae

pelvic girdle
left pes
pelvic girdle

sacrum

? —

. oo as

Figure 3.

left radius —

jaw

ON

basicranium

right humerus

B

quadrate

left humerus
left ulna
left manus

right humerus C
f

basicranium
Be

jaw

left arm

(A) Dorsal, (B) lateral, and (C) ventral X-rays of Sphaerodactylus ciguapa sp. nov. Scale bar = 5 cm.

The partially radiopaque “V”’-shaped element in the caudal area labeled with a question mark may represent a
portion of the regenerated tail or an artifact unrelated to the specimen itself.

20 MYA) amber deposits of La Toca mine,
in the Cordillera Septentrional, Santiago
Province, north of Municipio Santiago de
los Caballeros, Dominican Republic. -
Diagnosis. A medium-sized Sphaerodacty-
lus with an estimated snout—vent length
(SVL) of 33 mm. Basicranium with narrow

clinoid process; rounded crista alaris;
straight crista prootica; squarish paroccipital
process; knoblike sphenoccipital tubercle;
fenestra ovalis completely visible in ventral
view; foramen magnum roughly oval. Clav-
icles each with a single enlarged fenestra;
interclavicle with broad lateral arms; 26

6 BREVIORA

No. 529

cob

hhy

Figure 4. Dorsal view of basicranium, jaw, hyoid apparatus, and atlas of Sphaerodactylus ciguapa sp. nov. Gray
areas with white zig-zags indicate portions of the specimen worn. during polishing. Abbreviations: Icb, first
ceratobranchial; 2cb, second ceratobranchial; at, atlas; bhy, basihyal; bo, basioccipital; bp, basipterygoid process;
cal, crista alaris; clp, clinoid process; cob, compound bone (angular, articular, prearticular); cor, coronoid; crs, crista
sellae; ept, epipterygoid; fco, fossa columellae, hhy, hypohyal; mf, mandibular fossa; occ, occipital condyle; oto,
otooccipital; pop, paroccipital process; ppp, postparietal process; pro, prootic; pt, pterygoid; q, quadrate; sa,
surangular; set, sella turcica; pbsph, parabasisphenoid; sq, squamosal; tbr, trabeculae. Scale bar = 5 mm.

presacral vertebrae; pelvis with large and
ventrally directed pectineal process; digits
short, with manual metacarpals twice the
length of the phalanges; fourth phalangeal
element of the fourth manual digit short.
Gular and body laterodorsal scales small,
rounded posteriorly, and juxtaposed to weak-
ly imbricate; some lateral scales distinctly
keeled; forelimb scales smooth and strongly
imbricate; claw enclosed by three scales.
Ninety-nine extant and one fossil species
of Sphaerodactylus are currently recognized
as valid (BOhme, 1984; Kluge, 2001; Uetz,
2011). In general, Sphaerodactylus are
known as endemics of small areas (Schwartz
and Henderson, 1991; Henderson and
Powell, 2009); because of this it 1s reason-

able to compare this fossil with the 35
extant species from Hispaniola, as well as
the other fossil species. However, because
the age of the Dominican amber deposits
is older than, or contemporaneous with,
estimations of the formation of the Mona
Passage and the separation of Hispaniola
and Puerto Rico (~16—11 MYA; Iturralde-
Vinent and MacPhee, 1996; MacPhee et al.,
2003) we also compared the. new species
with 10 extant species from the “Puerto
Rico Area” (sensu Thomas, 1999), an area
that includes the islands of Mona, Monito,
and Desecheo as well as Greater Puerto
Rico (sensu Thomas and Schwartz, 1966)
(Appendix 2; species endemic to St. Croix,
U.S. Virgin Islands were not included as

2012

A NEW AMBER GECKO FROM HISPANIOLA 7

Sco

scofo

Figure 5.

Right lateral view of Sphaerodactylus ciguapa sp. nov. showing skull, cervical vertebrae, and pectoral

girdle. Gray areas with white zig-zags indicate portions of the specimen worn during polishing. Abbreviations: Icb,
first ceratobranchial; at, atlas; ax, axis; clv, clavicle; cob, compound bone; cor, coronoid; cv#, cervical vertebrae #:
epi, epipterygoid; h, humerus; hvc, groove for the course of the lateral head vein; hy, hypapophyses; mf, mandibular
fossa; ocr, occipital recess; ppp, postparietal process; pt, pterygoid; rap, retroarticular process; rib, rib; sco,
scapulocoracoid; scofo, scapulocoracoid foramen; sq, squamosal; V, incisura prootica for the course of the trigeminal

nerve. Scale bar = 5 mm.

this island is not part of the Puerto Rican
Bank).

The specimen of S. ciguapa is skeletally
mature (see Discussion), and is comparable
in size (here we have considered 29-36-mm
SVE to be in the same size range of S.
ciguapa) to 17 extant species from Hispaniola
(S. altavelensis, S. armstrongi, S. asterulus, S.
cinereus, S. clenchi, S. darlingtoni, S. diffici-

Wiss» vlazelli. (SS. leucastera Ss. randi-as:
rhabdotus, S. samanensis, S. savagei, S.
schuberti, S. shrevei, S. thompsoni, and

S. zygaena), four from the Puerto Rico Area
(S. monensis, S. klauberi, S. macrolepis, S.
micropithecus), and to the amber-preserved
species S. dommeli (BOhme, 1984). Of these
22 species, S. ciguapa may be distinguished
from S. monensis, S. macrolepis, and S.
thompsoni by its much smaller dorsal scales,
from S. samanensis by its larger and more
swollen scales, from S. cinereus by its
heterogeneous dorsal scalation including
imbricating, keeled scales (versus granular
dorsal scalation), and from all others except

S. asterulus, S. difficilis, S. dommeli, S.
rhabdotus, and S. shrevei by its swollen,
weakly keeled to keelless dorsal scales
(versus flat scales with strongly to very
strongly keeled scales, see Fig. 8 for exam-
ples of scale features discussed). The new
species may be distinguished from S. rhab-
dotus by its more weakly keeled and
subimbricate (versus strongly keeled and
strongly imbricate) dorsal scales, and from
S. asterulus, S. difficilis, and S. shrevei by the
presence of an extremely large clavicular
fenestra (versus a small fenestra). The amber-
embedded S. dommeli, which comes from the
same mine area as S. ciguapa, may be
differentiated on the basis of its smaller,
more granular dorsal scales (see Bohme,
1984, fig. 3). Additionally, we were unable
to identify enlarged clavicular fenestrae in
X-rays of S. dommeli.

General Description. The fossil is enclosed
in an oval piece of polished amber measuring
48.5 mm in its maximum dimension. The
specimen lies close to one of the margins of

8 BREVIORA

Figure 6.

bar 2 mm.

the piece and in some spots it is exposed as a

result of the polishing process. The amber
has a partial fracture plane at the posterior

end of the specimen, but the two portions
remain together. The amber matrix embed-

cf
clv

Sphaerodactylus ciguapa sp. nov. in dorsolateral view showing portions of the pectoral girdle. Scale

ding the specimen is semitransparent yellow
and the bone color is dark brown, providing
a contrast that facilitates observation of the
whole specimen (Fig. 2). The specimen is
mainly skeletonized (Figs. 2, 3), with a few

2012

Figure 7.

scattered patches of skin. The skeleton
preserves the posterior half of the left
pterygoid, a portion of the left epipterygoid,
a tiny fragment of the left parietal, left
squamosal, left quadrate, and some portions
of the brain case (including left prootic, left
otooccipital, parabasisphenoid, and basioc-
cipital), the posterior part of the right
mandibular ramus, parts of the hyoid appa-
ratus, all of the cervical, thoracolumbar,
sacral, pygal, and some postpygal caudal
vertebrae, the left arm and the proximal
portion of the right humerus, both suprasca-
pulas, scapulocoracoids, and clavicles, the

A NEW AMBER GECKO FROM HISPANIOLA 9

Sphaerodactylus ciguapa sp. nov. showing (A) left laterodorsal scapular integument, (B) mid-trunk
dorsal scales adjacent to the vertebral line, (C) left hand showing the typical Sphaerodactylus scalation pattern
around the claw, and (D) dorsal scales of S. difficilis (USNM 328965), an extant species from Hispaniola with similar
scalation to S. ciguapa. Scale bar = 0.5 mm.

complete sternum, the pelvis, left femur and
tibia, and both feet. All elements, except the
right pes, are articulated.

Holotype Measurements (unless otherwise
stated, measurements were made along the
long axis of each element; for paired
elements, left side measurement is provided):
braincase from the tip of the basipterygoid
process to the occipital condyle: 3.66 mm;
quadrate length from the cephalic condyle to
the mandibular condyles: 1.9 mm; squamosal:
0.71 mm; jaw fragment: 3.28 mm; cervical +
thoracolumbar vertebrae: 24.91 mm; sacrum
length: 0.88 mm; sacrum width: 2.31 mm; tail

10 BREVIORA No. 529

Figure 8.
swollen, juxtaposed), (B) S. rosaurae (USNM 570205, medium, rounded, swollen, juxtaposed, with a middorsal zone
of granular scales), (C) S. parkeri (USNM 328281, large, rounded, not swollen, imbricate), (D) S. argus (USNM
251978, small, acute, not swollen, imbricated), (E) S. richardsoni (USNM 252126, large, acute, swollen, imbricate),

Dorsal scale variation in Sphaerodactylus geckos. (A) S. pacificus (USNM 157531, small, rounded,

(F) S. thompsoni (USNM 328977, large, rounded, swollen, juxtaposed).

(proximal segment only preserved): 3.77 mm;
scapulocoracoid from the fossa glenoidea
to the dorsal margin: 2.28 mm; humerus:
4.46 mm; ulna: 3.23 mm; radius: 2.79 mm;
third manual digit + metacarpal: 2.43 mm;
pelvic girdle from the epipubic cartilage to the
posterior edge of illtum: 3.31 mm; metischial
process: 0.35 mm; tibia: 2.77 mm; third pedal
digit + metatarsal: 3.31 mm.
Dermatocranium. The parietal is only
represented by the tip of the posterior end
of the left postparietal process (ppp, Figs. 4,
5); the postparietal process 1s very narrow
and contacts the squamosal laterally at the

-midpoint of this bone, as in other sphaero-

dactyls. The squamosal (sq, Figs. 4, 5) is
small, slightly curved, and rounded in cross-
section. Its distal end contacts the braincase
and the top of the quadrate. A fragment of
the left pterygoid (pt, Figs. 4, 5) extends
from a point anterior to the fossa columellae
(fco, Fig. 4) to the end of the quadrate pro-
cess. Basispterygoid—pterygoid, epipterygoid—
pterygoid, quadrate—pterygoid, and cranio-
mandibular skull joints are preserved. The
former two are synovial and the latter a
syndesmosis (Frazzetta, 1962; Payne et al,
2011). In lateral view the pterygoid is mostly

2012

straight; it possesses a large facet for the basis-
pterygoid joint that is visible in medial view.

Splanchnocranium. A nearly complete left
epipterygoid (ept, Figs. 4, 5) is preserved,
although the dorsal portion of this bone is
broken and is disarticulated from the pro-
otic. Only the left quadrate bone (q, Figs. 3,
4) is preserved. The bone is completely
convex and the dorsal margin is rounded
with no lateral indentation. Although the
craniomandibular joint is in situ, it can be
seen that the distal articular surface bears
two condyles, and that the lateral is slightly
larger than the medial one. The presence and
position of the quadrate foramen cannot be
established in the specimen. The left auditory
meatus 1s nearly intact, and includes portions
of the tympanic membrane, implying that the
left stapes is preserved within the middle ear,
although it is not visible.

Neurocranium. The parabasisphenoid com-
plex (pbsph, Fig. 4) is fused posteriorly
to the basiocciptal. The left basipterygoid
process (bp, Fig. 4) is short but expanded
distally and anterolaterally oriented. It is
partially covered by a long, narrow clinoid
process (clp, Fig. 4) that roofs the notch on
the basipterygoid process and marks the
course of the lateral head vein (hvc, Fig. 5).
The right basipterygoid process is missing.
The paired trabeculae (tbr, Fig. 4) are
clearly distinguishable; they are round in
cross-section and parallel to one another.
Posterior to the trabeculae, the sella turcica
(set, Fig. 4) 1s bounded posteriorly by an
anteriorly curved crista sellae (crs, Fig. 4).
The anterior opening of the Vidian canal is
located ventral to the crista sellae. Most of
the basioccipital (bo, Fig. 4) is preserved; it
is concave dorsally and forms part of the
double occipital condyle (occ, Fig. 4) and
the ventral border of the foramen magnum.
The sphenoccipital tubercle epiphysis is
small and knoblike and is located anteriorly,
causing the crista tuberalis to be inclined

A NEW AMBER GECKO FROM HISPANIOLA 1]

posterodorsally. The left prootic (pro,
Fig. 4) is preserved but its medial surface
is partly worn down because of the polishing
process. The crista alaris is rounded and
small, and does not overhang the inferior
process of the prootic. The inferior process
bears the incisura prootica, which in geckos
is closed, forming an oval foramen that
surrounds a portion the mandibular branch
of the trigeminal nerve, CN5 (V, Fig. 5). A
portion of the left otooccipital (oto, Fig. 4)
is present, but none of the foramina in the
occiput (1.e., vagus and hypoglossal foram-
ina) are discernable.

Mandible (Figs. 3-5). The posterior por-

tion of the left jaw comprises the posterior

process of the coronoid (cor), the surangular
(sa), compound bone (cob; angular, prear-
ticular and articular), and, on the labial side,
the posterior portion of the dentary. A wide
mandibular fossa is formed by the suran-
gular and the compound bone. This fossa
opens laterally through a small slit (external
mandibular fenestrae) that marks the sepa-
ration between the partially fused surangu-
lar and the compound bone (Daza et al,
2008).

Hyoid Apparatus (Figs. 4, 5). A portion of
the basihyal (without the glossohyal process)
is preserved. The second epibranchials are
articulated to the basihyal and oriented
almost parallel to one another, as in S.
macrolepis (Noble, 1921). Both first epibran-
chials are preserved and curve upward
toward the posterior portion of the brain-
case. Anterior to the right second cerato-
branchial there is an elongated bony struc-
ture that could be a portion of the mght
hypohyal.

Vertebral Column. All the presacral verte-
brae are preserved. The total number is 26,
as 1S typical for most geckos. There are eight
cervical vertebrae (Fig. 5), which follows the
commonest formula for lizards: 3 (ribless) +
3 (short distal widened ribs) + 2 (long slender

12 BREVIORA

ribs) = 8 (Hoffstetter and Gasc, 1969). The
intercentra of the atlas, axis, and third—sixth
cervicals bear ventral hypapophyses and are
positioned intervertebrally, remaining un-
fused from the vertebrae centra (type A,
Hoffstetter and Gasc, 1969). The hypapo-
physes are double in the atlas and axis and
single in the remaining cervicals. The orien-
tation of the hypapophyses varies ventrally
(atlas), posteriorly (axis), and anteriorly
(remaining cervicals). The height of the
seventh and eighth cervicals is 25% greater
than that of the anterior cervicals, having
taller and squarer neural arches when viewed
laterally. These last two cervical vertebrae
are more similar to the thoracolumbar series.
All vertebrae bearing ribs have synapophyses
(parapophysis + diapophysis; Hoffstetter and
Gasc, 1969) that project laterally from the
anteroventral part of the centrum (Fig. 5).
The short ribs of cervical vertebrae 4-6 are
not bifurcated distally (cv4-cv5, Fig. 5), but
in sphaerodactyls, these ribs have a cartilagi-
nous terminus that is not preserved in the
fossil. Ribs from the fourth and fifth
cervicals are free, and the sixth and seventh
contact the medial surface of the scapulocor-
acoid. The dorsal process of the clavicle
contacts the dorsal surface of the sixth
vertebral rib. Four or five vertebrae are
connected to the sternum via sternal ribs
(Fig. 3). The remaining thoracic vertebrae
have long ribs that decrease in length
posteriorly, each bearing small postxiphi-
sternal inscriptional ribs. There is one ribless
lumbar vertebra. The sacrum has fused
transverse processes; the first sacral has an
expanded transverse process that overlaps
the second sacral. The exact number of pygal
vertebrae (i.e., caudals lacking chevrons;
Russell, 1967; Hoffstetter and Gasc, 1969)
could not be determined, but there are at
least five caudal vertebrae with elongated
transverse processes. The tail seems to be
regenerated, appearing as a poorly defined

No. 529

cartilaginous rod that is broken and bent and
is situated along the posterior portion of the
body (?, Fig. 3).

Pectoral Girdle and Forelimbs (Fig. 6). The
two clavicles are expanded medially, rotated
forward, and articulated medially, contact-
ing the anteroventral end of the interclavicle.
The clavicles each have a single fenestra,
which is among the largest seen in any
sphaerodactyl examined.

Pelvic Girdle and Hind Limbs (Fig. 3). The
pelvic girdle and hind limbs are mainly
covered by integument and are only visible
in the X-rays. The ischium, pubis, and ilium—
which is articulated with the sacrum—are
fused. The two inominate bones are still
articulated at the pubic (epipubic cartilage
preserved) and ischial symphyses, forming a
large ischiopubic fenestra (Figs. 3A, C). The
pectineal process of the pubis is large and
ventrally directed, as in all sphaerodactyls
(Noble, 1921; Gamble et al, 201la). The
posterior flange of the ischium is more or less
straight. The left acetabulofemoral joint is
preserved; the left leg retains all of its
elements. Of the right hind limb, only the
pes, which is twisted and facing the front of
the pelvis, is preserved. An exact phalangeal
formula cannot be determined from the X-
rays because of the superposition of the
vertebrae, but all Sphaerodactylus known have
manual and pedal formulae of 2:3:4:5:3
and 2:3:4:5:4, respectively, with phalanges 2
and 3 of digit 4 of both manus and pes
shortened (Russell and Bauer, 2008).

Integument. There are scales present in the
gular, dorsolateral trunk, and apendicular
regions. Gular scales are small, flattened,
rounded posteriorly, not swollen, and juxta-
posed; lateral scales covering the scapular
blade and the body flanks are small, moder-
ately keeled, rounded to subacute posterior-
ly, slightly swollen, and juxtaposed with little
or no imbrication (Fig. 7A); dorsal scales on
the mid-trunk are slighty larger, unkeeled to

2012

weakly keeled, oval, slightly swollen, and
subimbricate to weakly imbricate (Fig. 7B).
The scales covering the forelimbs are round-
ed posteriorly, smooth and strongly imbri-
cated; the claw is enclosed by three scales,
which are arranged in the typical asymmet-
rical pattern of Sphaerodactylus (Fig. 7C): an
enlarged outer inferolateral, a terminal +
median dorsal, and an inner inferolateral
(sensu Parker, 1926), or ventral, dorsal, and
ventrolateral (sensu Kluge, 1995).
Etymology. “La Ciguapa” is a Spanish
name for a mythical humanoid of Domini-
can folklore. It is described as a woman with
brown or dark blue skin, whose feet face

backward, and who has a very long mane of .

smooth, glossy hair that covers her naked
body (Angulo Guridi, 1866; Pérez, 1972;
Ubinas Renville, 2000, 2003). It 1s supposed
to inhabit the high mountains of the
Dominican Republic. The name, treated here
aS a noun in apposition, recalls the dark
brown bones and twisted feet in the holotype
specimen and the source of the specimen in
the Cordillera Septentrional of the Domini-
can Republic. The Ciguapa legend has been
proposed to be derived from the “opias”
(spirits of the dead) of the indigenous
Caribbean Taino people (Bosch Gavino,
D353):

RESULTS

Phylogenetic Analysis. Rooting with any
of the outgroup taxa resulted in the same
ingroup topology and measures of support,
so Hemidactylus brookii was~ arbitrarily
chosen to root all trees presented herein.
_ Tree searches found four most parsimonious

trees (MPT) of 1,135 steps (Consistency
index [Ci] = 0.379. Retention index [Ri] =
0.404). Two of these trees recovered a
monophyletic Sphaerodactylidae, as strongly
supported by molecular data (Gamble et al.,
2008a, 2008b, 2011b); therefore we used one

A NEW AMBER GECKO FROM HISPANIOLA 13

of these trees as working hypothesis for
mapping characters. Nine internal nodes are
well supported, with absolute BS values
greater than or equal to 3, and relative BS
values above 11. Five of these nine nodes
also had bootstrap values above 82 and GC
values above 77 (Fig. 9).

In the selected topology Aristelliger lar +
Teratoscincus scincus are sister to remaining
sphaerodactylids, with Quedenfeldtia, Eu-
leptes, and Saurodactylus as sequential sister
taxa to the clade formed by sphaerodactyls +
Pristurus. Among the most parsimonious
trees the positions of Lepidoblepharis and
Sphaerodactylus are interchangeable within
the sphaerodactyls.

Character Mapping. As previously noted,
there are only two nonmolecular characters
that currently serve to diagnose the family
Sphaerodactylidae, and neither of these is
expressed in all members of the group or is
exclusive to the clade. Thus, the monophyly
of this family has not yet been tested using
morphological data. Here we present all the
characters that apply to each of three nested
clades on the basis of their mapping on the
preferred most parsimonious tree. For each
one of named clades we emphasize those
characters that exhibit less homoplasy and
may therefore be useful for the morpholog-
ical diagnosis of these groups. Characters
that could be scored on S. ciguapa are
indicated in bold numbers.

Sphaerodactylidae: This clade inludes all
the genera listed in Gamble et al. (2008a) and
is supported by seven characters: 10) convex
snout; 136) dagger-shaped anterolateral pro-
cess of frontal; 308) anterior inferior alveolar
foramen surrounded by dentary, splenial,
and angular; 334) anterior tip of splenial
narrow and pointed; 439) branched xiphi-
sternum; 506) metatarsal V greatly hooked
(see Discussion); 560) two pygial vertebrae.
Of these characters, 506 was not present in
any other sampled gekkotan, whereas char-

14 BREVIORA

Hemidactylus brookii
Phyllodactylus wirshingi
Gymnodactylus geckoides
Q ,~ Thecadactylus rapicauda
Tarentola mauritanica
Narudasia festiva
Pseudogekko smaragdinus

Aristelliger lar

Teratoscincus scincus
Quedenfeldtia trachyblepharus
Euleptes europaea
Saurodactylus mauritanicus
Pristurus carteri

Gonatodes albogularis

——__—_—
% Lepidoblepharis xanthostigma
x
Oy ° Sphaerodactylus roosevelt
Se ome Sphaerodactylus klauberi
% © Sphaerodactylus ciguapa
% Coleodactylus brachystoma
Ly Chatogekko amazonicus

Pseudogonatodes guinanensis

No. 529

Figure 9. One of four most parsimonious trees of gekkonoid geckos. Circles at nodes denote BS/RFD equal to
or higher than 3/11, filled circles further indicate boostrap/GC values higher than 82/78. X-rays of representative
sphaerodactylid geckos from the tree are shown at right (not to same scale). Initials next to each X-ray correspond to
the the genus and specific epithet of taxa represented on the tree.

acters 136 and 334, although present in all
sphaerodactylids, are also found in some
phyllodactylids.

Sphaerodactylini + Pristurus: This clade is
supported by 11 characters: 19) fenestra
vomeronasalis continuous within the fenes-
tra exochoanalis; 37) ascending nasal process
of the premaxilla separates nasals through-
out approximately half their length; 93)
postorbitofrontal large, with no reduction
of processes; 97) postorbitofrontal ventrolat-
erally curved; 140) brief contact between the
frontal and the maxilla; 266) fusion of
parabasisphenoid and_ basioccipital; 332)

splenial fused to the coronoid; 352) suran-
gular contacts dentary posterior to the
coronoid—dentary suture; 440) mesosternal
extension absent; 454) humeral ectepicondyle
continuous, consolidated .with the bone
shaft; 601) nostril in contact with rostral
scale. The least homoplasic character was
601, which is present only in Aristelliger
outside sphaerodactyls. Although there were
no exclusive characters for this clade, char-
acters 93, 352, 440, and 454 were also
invariably present among sphaerodactyls,
but these character states occur in other
sampled genera.

2012

Sphaerodactyls: This clade is equivalent
to Sphaerodactylini (Gamble et al, 2008a).
Althought this clade was not recovered in
any of our MPTs, we performed a con-
strained search forcing this New World
clade, which receives strong molecular sup-
port, to be monophyletic. We obtained a
single MPT three steps longer than the
shortest trees from the unconstrained analy-
sis (L138 sisose Ci = 0.3532 IRI = 0333),
Eleven characters support this clade in the
constrained analysis: 19) fenestra vomerona-
salis continuous within the fenestra exochoa-
nalis; 110) lacrimal foramen bounded by
prefrontal and maxilla; 165) parietal nuchal
fossa present and extending substantially
onto the skull table; 184) posterior end of
squamosal not in contact with dorsum of
quadrate; 201) secondary palate formed
around choanal groove of palatine, ventro-
medial fold partly hides or hides most of the
the choanal groove; 220) anterior point of
the ectopterygoid relatively wide, abruptly
tapering to point; 281) crista prootica of
prootic with straight margin (except in
Chatogekko, which has a triangular crista
prootica); 340) coronoid low, hardly elevated
above jaw outline; 486) pectineal process of
pubis large and ventrally directed; 601) nostril
in contact with rostral scale; 612) supraciliary
spine present. Of these characters 201 and 340
were not present in any other sampled
gekkotan. Other characters that show low
homoplasy are 165 and 601 (also in Aristelli-
ger), 184 (also in Teratoscincus), and 486 (also
in Thecadactylus). Character 612 is also
present in Aristelliger but lost in Chatogekko,
Coleodactylus, and Pseudogonatodes.

Sphaerodactylus: Sixteen characters sup-
port this genus: 8) anterorbital portion of the
skull equals 30% or less of the total skull
length; 10) flat snout; 19) fenestra vomerona-
salis and incisura jacobsoni separated; 28)
foramen magnum roughly oval; 98) postorbi-
tofrontal, with large lateral process; 179)

A NEW AMBER GECKO FROM HISPANIOLA 15

postparietal process length less than half the
length anterior to the parietal notch; 330)
presence of angular and surangular processes
of dentary; 347) the anterolingual process of
the coronoid separates the dentary and
splenial anteriorly; 368) 12-13 premaxillary
teeth; 586) body with keeled scales; 600) two
to four loreal scales; 605) tympanic edge not
smooth; 638) digits with the distal-most
superolateral scales in contact; 651) dorsal

color pattern of head and nape with light

stripes; 652) dorsal color pattern of body with
ocelli; 671) ear partially occluded by flaps of
skin. Of the characters listed, 330, 638, 651
were not found in any other sampled gekko-

. tan. Sphaerodactylus geckos differ from other

sphaerodactyls by characters 19 and 605.
Other characters that were less homoplastic
were 179 (also present in Teratoscincus and
Chatogekko), 368 (also present in Pseudogo-
natodes), 586 and 600 (also present in Chato-
gekko), and 671 (also present in Pristurus).

DISCUSSION

Phylogeny. Four main hypotheses exist for
the relationships of sphaerodactylid geckos
(Fig. 10), two of them morphologically de-
rived (Kluge, 1995; Arnold, 2009) and the
others based on multigene analyses (Gamble
et al., 2008a, 2011b). There are discrepancies
in the branching pattern between the mor-
phological and molecular topologies, mainly
with respect to the basal relationships within
Sphaerodactylidae. Whereas the molecular
phylogenies (Gamble et al, 2008a, 2011b;
Figs. 1OC, D) include a clade comprising
Pristurus, Euleptes, Teratoscinus, Aristelliger,
and Quedenfeldtia, in the morphological hy-
potheses Pristurus was found to be either the
sister taxon of all sphaerodactyls (Kluge, 1995;
Daza, 2008) or Pristurus + Quedenfeldtia
were sister to sphaerodactyls (Arnold, 2009).
The sister group relationship between Aris-
telliger and Quedenfeldtia as suggested by

16 BREVIORA

Cnemaspis
Narudasia
Saurodactylus
Quedenfeldtia
Pristurus
Gonatodes
Lepidoblepharis
Sphaerodactylus
Coleodactylus
Pseudogonatodes

©

Pristurus
Euleptes
Teratoscincus
Aristelliger
Quedenfeldtia
Saurodactylus

Gonatodes
Lepidoblepharis
Sphaerodactylus
Coleodactylus
Pseudogonatodes

No. 529
B OG

Euleptes
Teratoscincus
Aristelliger
Saurodactylus
sphaerodactyls
Pristurus

Quedenfeldtia

0

Pristurus
Euleptes
Teratoscincus
Aristelliger
Quedenfeldtia
Saurodactylus
Chatogekko
Gonatodes
Lepidoeblepharis
Sphaerodactylus
Coleodactylus
Pseudogonatodes

Figure 10. Phylogenetic relationships of sphaerodactylid geckos on the basis of previously published analyses.
(A) Reanalysis of Kluge’s (1995) morphological data set, (B) Arnold (2009), (C) Gamble ef al. (2008a), and (D)
Gamble et al. (2011b). “Sphaerodactyls” in Figure 10B includes all the miniaturized New World sphaerodactylids (1.e.,
Coleodactylus, Gonatodes, Lepidoblepharis, Pseudogonatodes, Sphaerodactylus, and the newly recognized Chatogekko).

multigene phylogenies is not congruent with
our morphological results, in which an
Aristelliger + Teratoscinus clade is supported
by 14 morphological characters, one of them
being the parafrontal bones, which are unique
osteological structures in the circumorbital
series only known in these two genera (Bauer
and Russell, 1989; Daza and Bauer, 2010).
The two molecular hypotheses differ mainly
in the degree of resolution outside Sphaer-
odactylinae and in the placement of the
extremely modified Coleodactylus amazonicus
group (Figs. 10C—D), which has recently been
recognized as a new sphaerodactyl genus,
Chatogekko (Gamble et al., 201 1a).

The branching pattern we obtained for the
sphaerodactyl clade is consistent with a

previous morphological hypothesis (Kluge,
1995; Fig. 10A), but there is also a degree of
taxonomic congruence between our hypothe-
sis and recent multigene phylogenies (Gamble
et al., 2008a, 2011b). For instance, both
molecular and morphological data provide
strong support for the Sphaerodactylinae (1.e.,
sphaerodactyls + Saurodactylus), although
they differ in the position of Pristurus.
Previous morphological analyses have not
indentified synapomorphies that support
Sphaerodactylidae; for instance, a reanalysis
of Kluge’s (1995) data set using the gekkonid
genus Cnemaspis to root the tree results in a
MPT in which Narudasia (another gekkonid)
is nested within Sphaerodactylidae (Fig. 10A).
Our new analysis including a superior number

2012

of characters (approximately 27 and 55 times
the number of morphological characters of
Kluge [1995] and Arnold [2009], respectively)
provides provisional empirical morphological
evidence for the monophyly of Sphaerodacty-
lidae and two clades nested within it. Although
characters or combinations of characters
support the monophyly of less inclusive clades
like Sphaerodactylus and sphaerodactyls, rela-
tively homoplasy-free characters supporting
the Sphaerodactylidae remain elusive. The
reduction of clutch size from two to one (see
Gamble et al, 2008a) remains a_ possible
synapomorphy for the family, although on
the basis of our topology (Fig. 9) it is equivocal

if this character applies at the level of the .

Sphaerodactylidae as a whole, or to this clade
exclusive of Teratoscincus + Aristelliger.

A strongly hooked metatarsal V was
the least homoplastic trait supporting the
Sphaerodactylidae in our analysis. Although
this was not seen in any of the outgroup taxa
in our phylogenetic analysis, this character is
not exclusive to the Sphaerodactylidae, as
both straight (Figs. 11A—C) and hooked
(e.g., Ailuronyx seychellensis, Fig. 11D) mor-
phologies occur in other gekkonoids. Among
the Sphaerodactylidae this bone is variable
but 1s always bent, being strongly hooked in
some genera (e.g., Aristelliger, Quedenfeldtia,
Teratoscincus; Figs. 11E-G) or more gently
curved (e.g., sphaerodactyls, Fig. 11H).

Despite the fragmentary nature of S.
ciguapa it was possible to score it for 258

characters (38.2% of the complete list). The.

analysis of these data unambiguously sup-
ports its placement within the genus Sphaer-
odactylus. Unfortunately in our phylogenetic
_analysis Sphaerodactylus was represented by
only a few species from the argus series from
Puerto Rico; hence this hypothesis is not
useful for establishing the intrageneric rela-
tionships of S. ciguapa. Our comparisons
with living taxa from Hispaniola and Greater
Puerto Rico (see Diagnosis) suggest at least

A NEW AMBER GECKO FROM HISPANIOLA 7

phenetic similarity with S. difficilis, a mem-
ber of a widespread and diverse species
complex (Thomas and Schwartz, 1983) in
the notatus species group of the argus series,
and with members (S. shrevei, S. asterulus,
S. rhabdotus) of the shrevei species group
(Schwartz and Graham, 1980) in the cinereus
series. However, as these two groups span
most of the phylogenetic diversity within
West Indian Sphaerodactylus (Hass, 1991,
1996), the more specific affinities of S.
ciguapa remain uncertain.

Morphology. The skeletal anatomy of at
least some representative Sphaerodactylus
geckos has been studied in detail (Noble,
1ODI= Parkered926= Daza er al. 2008)s In
conjunction with the new data derived from
S. ciguapa it is possible to reevaluate certain
aspects of the osteology of the genus, and
sphaerodactyls more broadly, within the
more inclusive framework of the Gekkota.

The clinoid process of the parabasisphe-
noid is variable. In this fossil it is narrower
than that described in S. roosevelti (Daza
et al., 2008), or observed in S. difficilis; it is
unknown how variable this structure is
across Sphaerodactylus species, but it might
be a diagnostic character at some level. The
paired (unfused) trabeculae in Sphaerodacty-
lus are connected by a bony lamina in adults,
including the type of S. ciguapa, whereas in
juveniles these are discrete (Daza ef al,
2008). The sphenoccipital tubercle is reduced
in small sphaerodactyls (excluding Gona-
todes) and a similar reduction is present in
miniaturized lizards from all gekkotan fam-
ilies (e.g., Aprasia [Pygopodidae], Coleonyx
[Eublepharidae], Narudasia [Gekkonidae],
Homonota [Phyllodactylidae]). The reduction
of the apophysis that caps the sphenoccipital
tubercle suggests modifications to the tendi-
nous attachment of the fourth division of the
m. longissimus capitis, which extends back
into the ventral neck region along the fourth
cervical in lepidosaurs (Al Hassawi, 2007)

18 BREVIORA No. 529

Figure 11. Left pes of some gekkonoid lizards showing variation on the shape of metatarsal V (shaded in gray)
in phyllodactylids (A, B), gekkonids (C, D), and sphaerodactylids (EI). (A) Phyllodactylus wirshingi (CAS 175498),
(B) Tarentola mauritanica (UC MVZ 178184), (C) Pseudogekko brevipes (CAS 128978), (D) Ailuronyx seychellensis
(CAS 8421, (E) Aristelliger lar (USNM_ 260003), (F) Quedenfeldtia trachyblepharus (USNM_ 196417), (G)
Teratoscincus scincus (CAS 101437), (H) Lepidoblepharis xantostigma (USNM 313791), and (1) Sphaerodactylus
klauberi (UPRRP 006416).

2012

and whose fibers are attached to the ventral
hypapophyses of the cervical vertebrae. Since
reduction of this tubercle seems to be present
only in small species, it 1s possible this is
a character linked to miniaturization and
might be related to a reduction of the neck
muscle fibers.

In S. ciguapa, as in the rest of sphaer-
odactyls, the basicranial elements are fused,
obscuring the sutures between the braincase
bones. Observations of juveniles and newly
hatched Sphaerodactylus indicate that the
fenestra ovalis is bounded anteriorly by the
prootic and posteriorly by the otooccipital
(Daza et al., 2008); hence this fenestra serves
to estimate the limit between these two
elements. In gekkotans the otooccipital has
a synchondrosis articulation with the quad-
rate (Payne eft al/., 2011), although this joint
also has been described as syndesmosis
(Webb, 1951). In geckos the articulation of
the quadrate has been described as “parocci-
pital abutting” where this bone forms a well-
defined articular process, which is applied
against the anteroventral aspect of the
paroccipital process (Rieppel, 1984). The
paroccipital process of geckos has been
described as thick or thin (Jollie, 1960), and
this variation seems to be related to skull
size, being generally elongated in larger
species and reduced in small species. Similar
variation has been seen in size series of
amphisbaenians (Montero and Gans, 2008).
Sphaerodactylus spp. have a small, thick

paroccipital process that in posterior view -

is square (1.e., width and height subequal).
Shape and size of the paroccipital process
define its participation in the quadrate
‘suspension in gekkotans. In Pristurus, Gona-
todes, and Lepidoblepharis this process forms
a true paroccipital abuttment, but in Sphaer-
odactylus, Chatogekko, Coleodactylus, “and
Pseudogonatodes, the quadrate is suspended
from the lateral surface of the braincase, in
front of the paroccipital process (pop,

A NEW AMBER GECKO FROM HISPANIOLA 19

Fig. 4), with no participation of the squa-
mosal. In very small forms (e.g., Chatogekko)
the paroccipital process is so small that it has
minimal or no participation in the suspen-
sion of the quadrate (Gamble et al, 201 1a).

Ventral to the paroccipital process is
located the rounded occipital recess, which
in adult lizards represents the recessus scale
tympani (Oelrich, 1956; Rieppel, 1985) and
which in Sphaerodactylus is exclusively sur-
rounded by the otooccipital (Daza et al.,
2008). In other gekkonomorphs participa-
tion of the basioccipital in the margin of the
occipital recess has been reported (Kluge,
1962; Grismer, 1988; Conrad and Norell,

_ 2006). This participation is due to an out-

growth of the sphenooccipital tubercle; there-
fore the medial margin of the occipital recess
is a good indication of the boundary between
the otooccipital and the basiooccipital in
forms with a fused braincase.

The perforated stapes, commonly present
among sphaerodactylids, is uncommon among
squamates; this feature has only been reported
in some gekkotans, some amphisbaenians, and
dibamids (Greer, 1976; Kluge, 1983; Rieppel.,
1984; Gauthier et al, 1988, Bauer, 1990;
Conrad, 2008; McDowell, 2008). The only
sphaerodactylid where the stapes is unperfo-
rated is Saurodactylus, where this bone is short
and has a thick shaft and large footplate
(Evans, 2008). Although in S. ciguapa this
bone is not visible, it is very likely that it has a
stapedial foramen like its congeners.

The number of presacral vertebrae among
sphaerodactylids is variable; most of the
genera have the most common gekkotan
number of 26 (Hoffstetter and Gasc, 1969),
Whereas in Quedenfeldtia and Pristurus this
number is reduced to 24 and 23, respectively.
Arnold (2009) related the reduction of verte-
brae in Pristurus species to a shift from active
foragers to ambush predators. He also scored a
reduction of presacral vertebrae in Saurodac-
tylus mauritanicus, which was not corroborat-

20 BREVIORA

No. 529

Figure 12. Ventral view of the pectoral girdles of sphaerodactyl geckos. (A) Sphaerodactylus glaucus (MVZ
Herps 149093), (B) Gonatodes albogularis (MVZ Herps 83369), (C) Lepidoblepharis xantostigma (USNM 313791),
(D) Coleodactylus brachystoma (MZUSP. uncatalogued), (D) Chatogekko amazonicus (AMNH R_ 132039), (E)
Pseudogonatodes guinanensis (MZUSP 94826). Abbreviations: ace, anterior coracoid emargination; cf, clavicular
fenestra; clv, clavicle; eco, epicoracoid; fg, fossa glenoidea; h, humerus; iclv, interclavicle; me, mesosternal extension;
sco, scapulocoracoid; scof, scapulocoracoid fenestra; scofo, scapulocoracoid foramen; stn, sternum; stnr, sternal rib;

xy, xiphisternum. Scale bar = 1 mm.

ed by the specimens we reviewed. Reduction of
presacral vertebrae explains the development
of stocky bodies in Quedenfeltia and Pristurus,
a process that according to the current
morphological hypothesis and the molecular
topologies would have been independently
acquired (but see Arnold, 2009).

Centrum morphology of presacral verte-
brae is procoelic in most sphaerodactyls,

whereas Gonatodes has amphicoelous verte-
brae (Hoffstetter and Gasc, 1969; Kluge,
1967, 1995). The formation of procoelous
vertebrae in Sphaerodactylus proceeds differ-
ently from that in the rest of squamates. In
these geckos the intervertebral tissue does
not form a condyle but persists (Werner,
1971), suggesting that the procoelous verte-
brae in these geckos might be derived from

2012

amphicoelous ancestors (Hoffstetter and
Gasc, 1969: Werner, 1971) with vertebrae
resembling those of Gonatodes. Caudal ver-
tebrae in sphaerodactyls have the first
autotomy plane within the sixth or seventh
caudal, as is consistent with S. ciguapa. It
appears as if the type may have rebroken its
tail at the proximal-most autotomy plane in
an effort to escape when trapped in the resin.

A clavicular fenestra seems to be a constant
_ character for Sphaerodactylus (Noble, 1921;
Gamble et al, 201la), and this opening is
huge in S. ciguapa. In Gonatodes, Lepidoble-
pharis, and Chatogekko the clavicles are
unperforated (Figs. 12B, C, E; Noble, 1921;
Parker, 1926; Gamble et a/,, 2011a), where-
as in Coleodactylus and Pseudogonatodes
these may be closed or open, and the pres-
ence of a fenestra may be asymmetrical
(Clee ic. 121) = They laterale arms ‘of =the
interclavicle are another variable feature
within sphaerodactyls (Kluge, 1995). In some
Sphaerodactylus, including S. ciguapa, and in
Chatogekko the arms are almost indistin-
guishable, producing an almost rhomboid
interclavicle (Figs. 6, 12A, E); in Gonatodes
the interclavicle is cruciform with elongated
arms (Fig. 12B; Rivero-Blanco, 1976, 1979);
Lepidoblepharis have short, squarish arms
(Fig. 12C); Coleodactylus has broad, rounded
arms (Fig. 12D); and in Pseudogonatodes
interclavicle shape is variable—P. barbouri
has an interclavicle with rounded lateral arms
(Noble 192IE= Ranker 1926) and) im. .2.
guinanensis the interclavicles have no lateral
arms (Fig. 12F). Variation in the develop-
ment of the lateral arms of the interclavicle is
likely to be correlated with differences in the
posterior insertion of the sternohyoid muscle.
_ Although the appendicular skeleton pre-
sents no obviously phylogenetically informa-
tive characters, the epiphyses of the long
bones are fused to the diaphyses, confirming
that the type of S. ciguapa is skeletally
mature.

A NEW AMBER GECKO FROM HISPANIOLA 21

Unfortunately scale descriptors have not
been used consistently by different authors
and variation, both between individuals and
across the dorsum of single animals, can be
extreme, rendering both the characterization
and comparison of scalation difficult at best.
Dorsal scale shape in Sphaerodactylus spp.
varies from granular to elongate and strong-
ly keeled (Fig. 8). When the scales are
elongate they are typically extremely flat-
tened and imbricate (Barbour, 1921). AI-
though granular scales are common in
related genera, truly granular scales cover-
ing the body dorsum are rarely present in
Sphaerodactylus (Thomas, 1975). Among
the only exceptions are S. scapularis from

Gorgona Island in Colombia (Harris, 1982;

J.D.D., personal observation) and Hispan-
jolan -species ‘such as S. cinereus, 5S.
elasmorhynchus, and the extinct S. dommeli.
Sphaerodactylus copei, another Hispaniolan
species, has very large, swollen dorsals with
a region of middorsal granular scales. The
scalation of S. ciguapa may have been
similar to this, but the fragmentary nature
of the integument in the type makes it
difficult to determine the actual distribution
of scale types across the body and precise
meristic comparisons with other congeners
are precluded.

Ecology. Amber inclusions have revealed a
good deal about the floral and faunal
composition of the Miocene biota of the
Dominican Republic (Poinar and Poinar,
1994, 1999). To the extent that available
fossils permit the reconstruction of herpeto-
faunal communities of the period, they
appear to be similar to those predominating
today. Species of Anolis, Sphaerodactylus,
Typhlops, and Eleutherodactylus, the four
genera recorded as Dominican inclusions,
today comprise 171 of 243 species of
amphibians and reptiles found on Hispaniola
(Hedges, 2011). Extant Anolis lizards are
known for their distinctive ecomorphs and

22 BREVIORA

have served as the basis for fruitful research
programs in both ecology and evolution
(Williams, 1976; Losos et al, 1998; Losos,
2009). Hispaniolan Sphaerodactylus likewise
seem to reflect morphological adaptation to
particular lifestyles and substrates. Thomas
(1975) and Thomas et al. (1992) proposed that
head shape and coloration might be adaptive
traits, an argument supported by replicated
evolution of dark brown cryptic colored
species in the montane species dwelling in the
leaf litter from the Greater Antilles (Schwartz
and Garrido, 1985). The study of this varia-
tion has the potential to provide a rich system
for the study of comparative biology (D.
Scantlebury, personal communication).

To date the only specimens of amber-
preserved Sphaerodactylus that have been
reported are S. ciguapa, two specimens of S.
dommeli (Bohme, 1984), and an undescribed
small (14 mm SVL + 16.6 mm tail length)
specimen with slightly imbricated dorsal scales
(Kluge, 1995). Kluge concluded that the last of
these was possibly a juvenile on the basis of its
small size, but S. ariasae, the smallest Sphaer-
odactylus, has an adult SVL range of 14.1—
17.9 mm (Hedges and Thomas, 2001), so the
possibility exists that this animal represents a
very different ecomorph from the larger S.
ciguapa and S. dommeli.

Although it may never be _ possi-
ble to fully reconstruct the Sphaerodactylus
fauna of the Miocene, the study of the
relatively large number of as yet undescribed
amber geckos from the Dominican Republic
(Poinar and Poinar 1999: D. A. Grimaldi,
personal communication) may result in the
description of additional new taxa and pro-
vide a clearer picture of the paleodiversity of
this important group of Caribbean geckos.

ACKNOWLEDGMENTS

We thank James Hanken, Director of the
Museum of Comparative Zoology, for pur-

No. 529

chasing the specimen described herein and
making it available for our study. Yale
Goldman provided locality data for the
specimen and David Grimaldi (AMNH)
provided advice on Dominican amber. Kyle
Luckenbill and Ned Gilmore (Academy of
Natural Sciences in Philadelphia) and San-
dra Rareron and Kenneth Tighe (National
Museum of Natural History, Smithsonian
Institution) kindly helped with the X-rays.
For access to comparative material we thank
Richard Thomas (RT, UPRRP), Colin
McCarthy (BMNH), Kevin de Queiroz,
Roy McDiarmid, Ron Heyer, George Zug,
Jeremy Jacobs, and Steve Gotte (USNM),
Jonathan Losos and José Rosado (MCZ),
Fernando Castro-H (UV-C), Hussam Zaher
(MZUSP), Laurie Vitt (OMNH), Tony
Gamble (JFBM), Darell Frost and David
Kizirian (AMNH), Jens Vindum, Robert
Drewes, and Alan Leviton (CAS), Alan
Resetar (FMNH), and Jim McGuire and
Carol Spencer (MVZ). Virginia Abdala and
Esteban Lavilla (Fundacion Miguel Lillo)
provided assistance with specimens, and Dan
Scantlebury (University of Rochester) and
Wolfgang Bohme and Philipp Wagner (Zo-
ologisches FForschungsmuseum Alexander
Koenig) kindly provided X-rays of S. shrevei
and S. dommeli, respectively. This research
was supported by the Gerald M. Lemole,
M.D. Endowed Chair in Integrative Biology
Fund, and by grant DEB 0844523 from the
National Science Foundation of the United
States.

APPENDIX 1

Specimens used in phylogenetic analyses
(Sk = dry skeleton, C&S = cleared and
stained, HRXCT = high-resolution X-ray
computed tomography, XR = X-ray, * =
ethanol-preserved specimens).

Aristelliger lar (AMNH_ R-50272_ [Sk],
USNM 259998-260007, 260009* [XR], USNM

2012

260008 [C&S]), Chatogekko amazonicus
(AMNH-R 138670 [C&S], AMNH R-138726
[C&S], AMNH R-132039 [C&S], AMNH R-
132052 [C&S], MZUSP 91394*, OMNH 36262
[C&S], OMNH 37616 [C&S], OMNH 37274
[C&S], OMNH 37110 [C&S], OMNH 36712
[C&S], USNM 302283—302284*, USNM
124173*, USNM _ 200660—200663*, USNM
200664 [C&S], USNM = 200665—200666*,
USNM_ 288763*, USNM _ 288764 [C&S],
USNM = _288765—288788*, USNM 289031
[C&S], USNM 289061—289066*, USNM
29088 1—290882*, USNM 290904 [C&S],
USNM_ § 290944-290945*, USNM _ 303472-
303473*, USNM_ 570538*, USNM 304122
304123*), Coleodactylus brachystoma (MZUSP
no data [C&S], MZUSP 87385*), Euleptes
europaea (USNM_ 014861* [XR], USNM
565911*[XR], USNM 58963 [C&S]), Gonatodes
albogularis (AMNH R-71594{Sk], MVZ 83402
[C&S], UV-C No data [Sk]), Gymnodactylus
geckoides geckoides (CAS 49397 [HRXCT)),
Hemidactylus_ brookiti (BMNH_ 1978.1472*),
Lepidoblepharis xanthostigma (RT 1875 [C&S],
USNM_ 313758*, USNM_ 313791 [C&S],
USNM_ 313834*), Narudasia festiva (AMB
8717 [C&S], CAS 186290 [C&S]), Phyllodacty-
lus wirshingi (CAS 175498 [C&S], RT 13860
[C&S]), Pristurus carteri (CAS 225349 [C&S],
BMNH_ 1971.44 [Sk], JFBM 15821 [Sk]),
Pseudogekko smaragdinus (USNM_ 197367
[C&S], USNM 198423 [C&S], USNM 198424
[C&S]), Pseudogonatodes guianensis (MZUSP
94826 [C&S], USNM 84970* [XR], USNM
166138* [XR], USNM 234574* [XR], USNM
316687* [XR], USNM 321059* [XR], USNM
333018* [XR], USNM 538260-538267* [XR],
USNM_ 566327* [XR]); Quedenfeldtia trachy-
blepharus (FMNH_ 197682 [C&S], USNM
71113* [XR], USNM 196417* [XR], MVZ
178124) [C&S], Saurodactylus mauritanicus
(BMNH _ 87.10.6.1.6 [Sk], FMNH_ 197462
[C&S], USNM 217454* [XR]), Sphaerodactylus
ciguapa (MCZ R-186380 [Sk, XR]), Sphaero-
dactylus roosevelti (UPRRP 6376-6378 [C&S],

(Gr =

~USNM_ 94980*

A NEW AMBER GECKO FROM HISPANIOLA 23

UPRRP 6380-6381 [C&S], UPRRP 6488
[C&S], USNM 326986-326987* [XR], USNM
326996* [XR], USNM 327042* [XR]), Sphaero-
dactylus klauberi (UPRRP 6409-6421 [C&S],
UPRRP 6423-6427 [C&S]), Tarentola maurita-
nica (AMNH R-71591 [Sk], AMNH R-144408
[C&S], BMNH 1913.7.3.36 [Sk], JFBM 15824
[Sk]), Teratoscincus scincus (BMNH 92.11.28.1
[Sk], CAS 101437 [C&S]), Thecadactylus rapi-
cauda (AMNH R-59722 [Sk], AMNH R-75824
[Sk], AMNH R-85312 [Sk], BMNH 59.9.6.436
[Sk], USNM 220204 [Sk]).

APPENDIX 2

Specimens used for comparative purposes
dry skeleton, C&S = cleared and
stained, HRXCT = high-resolution X-ray
computed tomography, XR = X-ray, * =
ethanol-preserved specimens).

Ailuronyx seychellensis (CAS 8421 [C&S]),
Aristelliger georgeensis (CAS 176485 [HRX-
CT)), Aristelliger praesignis (AMNH R-146747
[C&S], AMNH R-71593 [Sk], AMNH R-71595
[Sk], BMNH 1964.1812 [Sk], BMNH 86.4.15.4
[Sk]), Coleodactylus guimaraesi (USNM 304122*
[XR]), Coleodactylus meridionalis (MZUSP
88673*), Coleodactylus septentrionalis (MZSP
66554*, MZUSP 66556*, USNM 302285—
302287* [XR], USNM 302337* [XR], USNM
302361* [XR], USNM 531620-531622* [XR],
USNM _ 566300* [XR]), Gonatodes annularis
(USNM 535787* [XR], USNM 535791* [XR]),
Gonatodes antillensis (AMNH_ R-72642_ [Sk],
[XR]), Gonatodes ceciliae
(USNM_ 166159* [XR]), Gonatodes humeralis
(RT 01198 [C&S], USNM 568645* [XR]),
USNM 568647* [XR]), USNM 568658* [XR]),
USNM 568663* [XR]), USNM 568677* [XR]),
USNM 568681* [XR]), USNM 568682* [XR]),
USNM 568684* [XR]), USNM 568692* [XR]),
Gonatodes taniae (UPRRP 006045 [C&S]),
Lepidoblepharis buchwaldi (USNM_ 234565*
[XR], USNM 234569* [XR]), Lepidoblepharis
festae (USNM 166140-166143* [XR]), Lepido-

24 BREVIORA

blepharis heyerorum (USNM_ 217635* [XR)),
Lepidoblepharis peraccae (UV-C 8999 [Sk)),
Pristurus crucifer (USNM 72014* [XR], USNM
217452* [XR], USNM 217453* [XR]), Pris-
turus insignis (BMNH_ 1953.1.7.73_ [Sk]),
Pseudogonatodes barbouri (AMNH_R-
144395 [C&S], AMNH R-146746 [C&S],
AMNH R-146752 [C&S], AMNH 146757
[C&S]), Pseudogonatodes peruvianus (USNM
343190* [XR], USNM 343191* [XR]), Sphaero-
dactylus altavelensis (USNM_ 328548* [XR]),
Sphaerodactylus argivus (USNM 104597* [XR]),
Sphaerodactylus argus (USNM 251977-251978*
[XR]), Sphaerodactylus ariasae (USNM 541804—
541805* [XR], USNM 541807-541810* [XR]),
Sphaerodactylus armstrongi (RT 5255 [C&S],
USNM 260053* [XR], USNM 260046* [XR],
USNM 260051—260054* [XR]), Sphaerodactylus
asterulus (USNM 328946* [XR], USNM
328949* [XR]), Sphaerodactylus beattyi (USNM
304480-304481* [XR]), Sphaerodactylus cinereus
(AMNH R-49566 [C&S]; USNM 292296*
[XR]), Sphaerodactylus copei (RT 10576 [C&S],
USNM 118881* [XR]), Sphaerodactylus corti-
cola (USNM 211428* [XR], USNM 220548—
220552* [XR]), Sphaerodactylus darlingtoni
(USNM 328962* [XR]), Sphaerodactylus diffici-
lis (AMNH R-144413-144435 [C&S], USNM
328965* [XR]), Sphaerodactylus elegans (USNM
27625* [XR], USNM 27981* [XR]), Sphaero-
dactylus gaigeae (UPRRP 6428-6432 [C&S],
UPRRP 6434-6436 [C&S]), Sphaerodactylus
goniorhynchus (BMNH 1963.841*), Sphaerodac-
tylus gossei (BMNH1964.1801-2 [Sk), Sphaero-
dactylus ladae (USNM_ 512248* [XR], USNM
512251* [KR], USNM 512253-512254* [XR]),
Sphaerodactylus leucaster (USNM_ 197338*
[XR]), Sphaerodactylus levinsi (RT 8283-8284
[Sk], USNM 220939* [XR], USNM 220921*
[XR]), Sphaerodactylus lineolatus (BMNH
OT AA 2a UPRARPS 3172) (Esso WSININ
120479* [XR], USNM 120497* [XR], USNM
12053* [XR], USNM_ 120504* [XR]), Sphaero-
dactylus macrolepis (UPRRP 6437-6445 [C&S],
USNM 221462* [XR]), Sphaerodactylus micro-

No. 529

lepis (USNM 222901* [XR]), Sphaerodactylus
micropithecus (USNM 229891* [XR]), Sphaero-
dactylus millepunctatus (AMNH_ R-16284*
[XR]), Sphaerodactylus monensis (UPRRP 6454
[C&S]), Sphaerodactylus nicholsi (UPRRP 6383-—
6386 [C&S], UPRRP 63880 [C&S]), Sphaero-
dactylus nigropunctatus (AMNH_ R-73470 [Sk];
BMNH 1946.8.24.81*), Sphaerodactylus notatus
(BMNH_ 1965.186*, USNM 494822* [XR]),
Sphaerodactylus oliveri (USNM 140431* [XR],
USNM 140435* [XR]), Sphaerodactylus oxyrhi-
nus (USNM > 292288-292289* [XR]), Sphaero-
dactylus pacificus (BMNH 1979.385—1979.386*,
USNM 157531—157532* [XR]), Sphaerodactylus
parkeri (USNM 328281* [XR]), Sphaerodactylus
parthenopion (USNM 221593* [XR]), Sphaero-
dactylus ramsdeni (USNM_ 309772* [XR)),
Sphaerodactylus randi (USNM 305427-305428*
[XR]), Sphaerodactylus rhabdotus (USNM
292328* [XR]), Sphaerodactylus richardsonii
(BMNH 1964.1801-2*, USNM 252126* [XR]),
Sphaerodactylus shrevei (USNMFH_ 194578
[XR]), Sphaerodactylus rosaurae (BMNH
1946.8.16.60*, USNM 570196-570199* [XR],
USNM 570204-570213* [XR]), Sphaerodactylus
ruibali (USNM 78921* [XR]), Sphaerodactylus
sabanus (USNM 27625* [XR], USNM 236098*
[XR]), Sphaerodactylus samanensis (USNM
319135* [XR]), Sphaerodactylus savagei (USNM
260157* [XR]; Sphaerodactylus — scapularis:
BMNH_ 1901.3.29.6*%, BMNH_ 1946.8.30.70*,
BMNH_ 1902.729.1-2*, BMNH_ 1926.1.20*),
Sphaerodactylus semasiops (BMNH_ 1968.326%*,
USNM 292294* [XR], USNM 305435* [XR]),
Sphaerodactylus sommeri (USNM_ 292313*
[XR]), Sphaerodactylus sputator (USNM
236118* [XR]), Sphaerodactylus streptophorus
(USNM 541811* [XR], USNM 541813* [XR]),
Sphaerodactylus thompsoni (USNM_= 328977*
[XR]), Sphaerodactylus townsendi (UPRRP
6389-6400 [C&S], UPRRP 6402-6407 [C&S],
USNM 291193* [XR]), Sphaerodactylus vincenti
(USNM 286941* [XR], USNM 121648* [XR]),
Sphaerodactylus millepunctatus (USNM 496644*
[XR]), Teratoscincus microlepis (AMNH_R-

2012

88524 [Sk], BMNH 1934.10.9.14 [Sk]), Teratos-
cincus przewalskii (CAS 171013 [HRXCT],
JFBM 15826 [Sk]), Teratoscincus roborowskii
(JFBM 15828 [Sk]).

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