Morphological and genetic evidence for a new karst specialist lizard from New Guinea (Cyrtodactylus: Gekkonidae)

Exposed limestone karst landscapes, especially in the tropics, are often home to distinctive and specialized biotas. Among vertebrates, a particularly large number of karst-associated lizard taxa have been described, but for the vast majority, evidence of specific adaptions to karst is lacking. A number of studies, however, have provided evidence of consistent morphological trends in lizards that use complex, three-dimensional, saxicoline habitats such as those that typify karst areas. Here we combine morphological and genetic data to test whether a newly discovered gecko from an extremely rugged karst area in New Guinea shows morphological trends matching those observed in other lizards associated with complex rock habitats such as karst and caves. Consistent with predictions, the new species' head is flatter and narrower than similar-sized relatives, and it has proportionally larger eyes and longer limbs. These trends indicate this taxon represents the second documented instance of karst specialization in a New Guinean vertebrate, and suggest morphological traits to test for evidence of specialized ecological associations in the many karst-associated Cyrtodactylus taxa from Southeast Asia.

1. Introduction

Large areas of exposed limestone karst in tropical regions present spectacular landscapes, and are home to unique, endemic and putatively specialized local biotas in Madagascar [1], Southeast Asia [2] and Australia [3,4]. Lizards often show a particularly close association with karst landforms, including numerous taxa that have only been described recently [5–10]. Two broad, and by no means mutually exclusive, hypotheses can be advanced to explain this association. First, refugial evolutionary dynamics, such as persistence through climatic change in microrefugia, was the driver of localized distributions [4]. Or second, adaptive processes led formerly more generalist lineages to become ecological specialists, restricted to the topographically complex, nutrient-poor and biologically distinctive habitats provided by karst [2,11].

Understanding patterns of morphological differentiation is one element of teasing apart the relative roles of these two processes. Morphological studies have suggested a suite of specializations occur in many lizards that use complex, three-dimensional rock structures, including, but not exclusive to karst [12]. These include relatively long limbs, a more gracile body, and often a flatter head [12–15]. Other studies have also suggested a tendency for highly specialized rock-dwelling lizards to have proportionally larger eyes [16], but this has not been tested systematically. In contrast, if taxa endemic to karst show little evidence of morphological differentiation, and are allopatric isolates separated from relatives by climatically unsuitable regions, it suggests that karst endemism may be more strongly linked to refugial than adaptive processes.

The bent-toed geckos (Gekkonidae: Cyrtodactylus) are the most speciose genus of geckos, occurring across India, Indochina, Southeast Asia and Australia [17]. Over 60 species from Indochina, Peninsular Malaysia and Borneo appear to be restricted to isolated karst regions, surrounded by unsuitable habitat for Cyrtodactylus or forest areas occupied by other congeners [10,18–21]. Despite this diversity and probable ecological specialization, there has been relatively little work on patterns of ecomorphological evolution in Cyrtodactylus. Recent work, however, that compared some ‘cave’ taxa (not exclusive to limestone) to more generalized relatives found them to have a gracile build, longer limbs and a dorsal colour pattern consisting of well-defined, narrow transverse bands [15,17,22].

Although most Cyrtodactylus diversity is concentrated in Asia, New Guinea, northeastern Australia and the surrounding islands of western Melanesia are also home to a monophyletic radiation of around 30 species, notable for the apparently parallel evolution of giant species [23]. While five Australian taxa within this radiation seem to be closely associated with saxicoline habitats [19], karst-associated Cyrtodactylus have not been reported from New Guinea. This is despite the presence of large areas of exposed limestone karst landforms [24,25]. Among other taxa, two widespread but patchily distributed bird and mammal species may be linked with New Guinea karst [26,27], and recent surveys note a distinctive plant fauna (characterized by the absence of some typically common taxa, some specialist forms and some elevational depression) [28]. However, compared to nearby regions in Southeast Asia, there has been little investigation into patterns of biotic endemism and specialization in the New Guinea karsts.

The Southern Fold Mountains are the largest tract of karst in Melanesia, extending along the southern edge of the Central Cordillera of New Guinea from Lake Kutubu in the east to the Star Mountains in the west [25]. Rainfall in this region is extremely high (up to 8 m per year) [29]. Consequently, limestone is both highly dissected and masked by vegetation [28], making the area difficult to access and thus poorly known. One of us (P.M.O.) recently surveyed the herpetofaunal biodiversity of an extremely rugged area of limestone in these ranges. During this survey, a novel and distinctive, slender-bodied, medium-sized (snout--vent length (SVL) 97 mm) species of Cyrtodactylus was collected. This species was abundant at the type locality on both low vegetation and karst structures, but has not been detected at nearby sites which lack exposed karst. Here we test if, relative to similar-sized congeners, this species shows evidence of the morphological specializations typical of lizards associated with complex, three-dimensional saxicoline microhabitats—specifically long limbs, a flattened head and/or disproportionately large eyes [12,13,16]. We also present a formal scientific description of the new species.

2. Material and methods

2.1. Material

New specimens were collected by hand at night while spotlighting between 19 April and 8 May 2013, humanely field-euthanized using standard practices (intraperitoneal and cardiac injection of MS-222) [30], preserved in formalin, and stored in ethanol. Types have been lodged at Museum Victoria or the South Australian Museum, and two additional samples are to be repatriated to the Papua New Guinea National Museum. Liver samples for genetic analysis were taken from all samples [30]. Genetic samples and comparative material (electronic supplementary material, appendices S1 and S2) used in this study are primarily stored at the following institutions: Australian Museum (AMS)—Sydney; Museum Victoria (NMV)—Melbourne; South Australian Museum/Australian Biological Tissues Collections (SAMA/ABTC)—Adelaide; Museum of Comparative Zoology (MCZ)—Harvard University, Cambridge; and Museum Zoologicum Bogoriense (MZB)—Bogor. Additional comparative data for taxonomic descriptions were taken from published literature [31–36] while most genetic data were also taken from recent publications [17,21,23].

2.2. Genetics

To ensure maximal compatibility with published sequence data for Cyrtodactylus, we generated new sequence data from the NADH dehydrogenase subunit 2 (ND2) for four samples of the new species, in addition to two samples of Cyrtodactylus capreoloides collected sympatrically. Laboratory protocols largely followed Sistrom et al. [37] with ND2 and partial flanking tRNAs amplified using the primers M112F (5′-AAGCTTTCGGGGCCCATACC-3′) and M1123R (5′-GCTTAATTAAAGTGTYTGAGTTGC-3′) designed in the flanking methionine and alanine tRNAs.

Our final genetic dataset included 107 out of approximately 250 nominal Cyrtodactylus species globally, and 22 out of 25 recognized species from Melanesia. To initially place the putative new species within a phylogenetic framework, we analysed 987 bp of ND2 data aligned using the MUSCLE algorithm [38] using default settings as implemented in Geneious v. 6.0.5 [39], and subsequently checked for missense mutations and correct reading frames. Phylogenetic trees were estimated using standard maximum-likelihood (RAxML v.7.2.8) [40] analyses using the GTR model implemented on the CIPRES Web portal version 3.1 for online phylogenetic analysis.

We used BEAST v.1.8.0 [41] to visualize the evolution of karst-associated taxa across the radiation of Cyrtodactylus. We aligned genetic data (see above) from the new taxon with a four-gene dataset of Cyrtodactylus sequences synthesized from published literature (electronic supplementary material, appendix S1) [17,23,31,42]. This alignment included ND2 for all taxa, plus three nuclear genes (MXRA-5, RAG-1 and Phos) for a reduced number of taxa (electronic supplementary material, appendix S3). We used a three-partition strategy following previous analyses of Melanesian Cyrtodactylus [23] (mitochondrial first and second codons; mitochondrial thirds and nuclear genes) with all partitions given the GTR + G model. Topology and timeframes of divergence were estimated using the uncorrelated lognormal model, birth–death speciation prior for 20 million generations, sampling every 20 000 with the first 20% of trees discarded as burn-in, giving a total of 800 trees from which to estimate topological support. Dating calibrations followed those used elsewhere [23], with the addition of a broad normally distributed prior at the base of sampled Cyrtodactylus (mean 32, s.d. 5.0) derived from an analysis of multi-locus nuclear data containing the majority of recognized gecko genera and major lineages [4,43]. Habitat was coded as a simple binary state (karst versus not karst) and transition patterns were estimated using a simple all rates equal model (electronic supplementary material, appendices S4 and S5).

2.3. Morphology

The following morphometric measurements were taken with digital callipers to the nearest 0.1 mm, with bilateral measures recorded from the left side of the body: SVL, tail length (from the posterior edge of the vent to the tip of the tail (TL), total length of original portion of tail (OT), trunk length from posterior edge of axilla to anterior edge of groin with limbs held at right angles (TrK), maximum head width (HW), maximum head height (HH), head length from tip of snout to anterior margin of ear opening (HL), distance from posterior edge of naris to anterior edge of eye (EN) (used as a proxy for snout-length), transverse diameter of orbital (OrB), internarial distance (IN), transverse diameter of ear (EAR), forearm length from base of palm to outer edge of elbow flexed at 90° (FA), and hindlimb length from base of heel to outer edge of knee flexed at 90° (HDL).

For taxonomic comparisons the following meristic counts were also taken: left and right enlarged supralabials (SUPR), to both the midpoint of the eye and to the rictus; left and right infralabials to rictus (INFR); rows of enlarged dorsal tubercles between the ventrolateral folds (not including those on fold itself) at the midpoint of body (DTR); ventral scale rows in a transverse series between ventrolateral folds at midpoint of the body (VENT); the number of subdigital lamellae (LAM), including both the narrow (distal to the inflection of the digit; not including the ungual sheath) and wide lamellae (proximal to the inflection of the joint) under the first and fourth digits of the left manus and pes; precloacal (PREPOR) and femoral pores (FEMPOR) where present (males only); postcloacal tubercles/spurs (PCTUB); and number of dark-brown, semi-distinct dorsal bands that cross the midline between limb insertions (DB).

2.4. Multivariate and univariate statistical analyses

All statistical analyses were performed in R [44]. To test for potential morphological correlates of living on karst, we used size-corrected mensural data for the new taxon, compared against a suite of six, similarly sized (max SVL 82–109 mm) Melanesian Cyrtodactylus species, including all possible closest relatives (electronic supplementary material, appendix S6). Field observations suggest most of these taxa are arboreal and occur widely away from karst [31,36,45]. We focused on similar-sized species to reduce the potential for generalized non-allometric growth trajectories to confound analyses. In particular, many other Papuan Cyrtodactylus are very large geckos [23], raising the possibility that processes such as peramorphosis could confound analyses of relative body proportions [46].

All variables were log transformed. Probable juvenile (smaller than the smallest male with well-developed pores and/or testes) and highly contorted specimens were excluded from statistical analyses. Body, head and limb measurements were corrected for body size by regressing against principal component 1 from an initial principal components analysis (PCA), in order to account for possible non-allometric growth [47]. An initial PCA of the size-corrected body and HL data was used to determine population-level distinctiveness in multivariate space. We also visualized patterns of morphological variation across taxa in phylomorphospace [48] based on species means for size-corrected traits and a reduced ML phylogeny for the seven focal taxa.

To initially visualize patterns of univariate variation across species, we used simple boxplots of the size-corrected morphological data. Because a number of our focal taxa are only known from a small number of specimens (less than 10), we used non-parametric approaches to test for significant variation in traits. First, we used a non-parametric MANOVA (adonis function in R package vegan [49]) to test for differentiation across taxa based on a distance matrix calculated across 10 000 permutations. We then used the Kruskal–Wallis rank sum test (Kruskal.test function) to compare morphological differentiation in traits across species pairs post hoc (with the significance value set to p = 0.05).

3. Results

3.1. Genetics

Phylogenetic analyses place the novel taxon within a strongly supported radiation of Australo-Papuan Cyrtodactylus, phylogenetically distinct (mid-Miocene or earlier splits) from all other sampled Cyrtodactylus inhabiting karst areas (figure 1a,b). Based on moderate statistical support (ML bootstrap 81%, Bayesian posterior probability 1.0), it is part of a recently identified clade of medium-sized, forest-dwelling species found in the mountains/hills of central and northern New Guinea (Cyrtodactylus capreoloides, Cyrtodactylus boreoclivus and Cyrtodactylus medioclivus) [31]. The new species is most closely allied to—but deeply divergent from—the more widespread and partially sympatric taxon, C. capreoloides, although this relationship was not strongly supported (ML bootstrap 60%, PP 0.88).

Based on our sampling of just under half of the recognized species of Cyrtodactylus (109 taxa or candidate taxa), at least nine independent transitions into karst microhabitats were inferred across New Guinea, Borneo, Peninsular Malaysia and Indochina. Ancestral states estimation indicated that the new species provides the first evidence of a shift into this habitat in Melanesia. No transitions out of karst, and just one potential example of speciation within karst, were inferred.

The new species is estimated to have diverged from its putative closest relative, Cyrtodactylus capreoloides, around the late Miocene (mean age estimates in millions of years ago 6.7, highest posterior distribution 5.1–8.2). Estimated divergence times of other karst lineages varied widely, ranging from mid-Miocene to Pliocene (15–1 million years ago) (figure 1a). However, as sampling in many parts of the wide range of Cyrtodactylus was very sparse and many potential sister lineages are missing, older divergence dates in particular are likely to be overestimates and should be treated with caution.

3.2. Morphology

Multivariate analyses of size-corrected data separated the novel species from all other taxa sampled on PC axis 1, with no overlap (figure 2a). All morphological characters except trunk length (TrK) were strongly loaded onto PC axis 1 (electronic supplementary material, appendix S7). Phylomorphospace plots also indicated that the new taxon was distinct from all the other medium-sized Cyrtodactylus in our sample from New Guinea along PC axis 1, including the three most closely related species C. boreoclivus, C. capreoloides and C. medioclivus (figure 2b).

Visualization of univariate data indicated that the new species had a proportionately shallower and narrower head than all other sampled taxa, with very little overlap of values. Mean relative forelimb and hindlimb length, and orbital width were also the highest among sampled taxa, although the distribution of these values overlapped more considerably (figure 3).

Non-parametric MANOVA detected highly significant differences between taxa (p < 0.005). Subsequent post hoc non-parametric Kruskal–Wallis tests detected significant differences between taxa in all variables apart from trunk length (TrK). Of the 20 pairwise comparisons that significantly differed (with significance value set at 0.05), 18 involved the new limestone species. Transverse diameter of the orbital showed the strongest pattern, and was significantly wider in the new species than four of the six sampled taxa, including all three closest relatives. The new species also had a significantly shallower head than three other taxa (including two close relatives), and a narrower head than four other taxa (including two close relatives). While mean forelimb and hindlimb length was longer in the new species, in our statistical tests this did not differ significantly from most other species. Likewise, while head length and snout length showed some evidence of differentiation in univariate boxplots, most comparisons with other taxa were not statistically significant.

In overall appearance, the new species appeared much more gracile than the related and sympatric Cyrtodactylus capreoloides (figure 4).

3.3. Systematics

The combination of genetic and morphological data confirms that these samples represent a novel taxon that is genetically divergent and morphologically distinctive from all other Cyrtodactylus, and that occurs in sympatry with its potential sister taxon Cyrtodactylus capreoloides. We here describe it as a new species.

Cyrtodactylus Gray, 1827

Cyrtodactylus tanim n. sp. (figures 4–7).

3.3.1. Zoobank LSIDs

Original publication: urn:lsid:zoobank.org:pub:422F5175-E543-43E1-A2A1-7602C2987B48

Species combination: urn:lsid:zoobank.org:act:0E895BC0-CF6C-43EE-9BE6-39F662DE083F

3.3.2. Holotype

NMV75956 (F# SJR14640), adult male with original tail, Papua New Guinea, Western Province, limestone range approximately 9 km east of Kaiangibip Village, 1075 m.a.s.l. (5.53° S, 141.56° E) collected by P. M. Oliver (19 April 2013), with frozen tissue for genetic analysis at Museum Victoria.

3.3.3. Paratypes

Papua New Guinea, Western Province (n = 12). NMVD75957 (SJR14638), SAMA R70319 (SJR14668), SJR14637, SJR14709 (males), NMVD75958–75960 (SJR14639, SJR14669, SJR140670) (females), NMVD75961 (SJR14717) (juvenile), all with same locality and collector details as holotype and collected between 19 and 20 April 2013; NMVD75962–63 (SJR14708, SJR14743), SAMA R70320 (SJR13150) (all males) Mt Uni, approximately 6 km west of Kaiangibip Village, approximately 540 m.a.s.l. (5.48° S, 141.54° E) collected between 26 April and 3 May 2013; NMVD75964 (PMO39) (male) approximately 9 km east of Kiangibip Village, approximately 760 m.a.s.l. (−05.51°, 141.57°) collected 8 May 2013.

3.3.4. Diagnosis

Cyrtodactylus tanim n. sp. can be distinguished from all other Melanesian and (Wallacean) Cyrtodactylus by the following unique combination of characters: moderate size (SVL to 96.7 mm) and slender, with a relatively narrow head (HW/SVL 0.17–0.19), mid-dorsal tubercles in 14–16 longitudinal rows at midpoint of body, ventrolateral fold without enlarged tubercles, subcaudal scales not transversely widened, pores in a tripartite series, precloacal pores obvious and of moderate number (15–17), femoral pores minute and numerous (31–30 per limb, 66–76 total), and dorsal colour pattern on torso consisting of six to nine semi-distinctly defined, alternating dark-brown bands or blotches, on a medium-brown background.

3.3.5. Description of the holotype

Adult male. Moderately large (SVL 96.7 mm) with slender habitus. Head large (HL/SVL 0.24), moderately slender (HW/SVL 0.17) and clearly distinct from neck (figure 5a). Snout longer than broad, rounded in dorsal profile and truncate in lateral profile (figure 5b,c). Eye to naris distance slightly greater than orbital diameter (EN/OrB 1.08), loreal region slightly inflated, interorbital region and top of snout concave, canthus rostralis rounded, weakly defined. Eyes quite large (OrB/HL 0.32), pupil vertical, supraciliaries extending from anteroventral to posterodorsal edge of orbit, longest at the anterodorsal margin. Ear opening rounded, bordered by distinct dorsal skin fold.

Rostral rectangular, wider than high, with medial suture extending ventrally approximately halfway from dorsal edge and terminating in short ventrolateral bifurcation, bordered dorsally by two flattened supranasals and one large and two small internasals. Nares bordered by first supralabial (point contact), rostral, 1 enlarged supranasal, and 5–6, granular postnasals. Supralabials generally wider than high, 11–12 total, 10 to midpoint of eye. Head, temporal and nuchal scales small and granular, interspersed with numerous enlarged weakly conical tubercles, approximately two to three times width of surrounding scales in temporal and occipital (and posterior nuchal) regions. Enlarged infralabials slightly to much wider than high, 14 on either side, bordered by rows of slightly enlarged scales that grade into small granular gular scales. Mental wider than long, broadly triangular, bearing distinct groove at contact with postmentals, in contact with first infralabials, and with a broad, lateral sulcus extending between the anterior tips of the two postmentals (figure 5d).

Body moderately gracile (TrK/SVL 0.47) with weak ventrolateral folds. Dorsum with approximately 15 rows (not including ventrolateral fold) of tubercles up to three to four times width of surrounding small, granular scales. Ventral scales much larger than dorsal scales, increasing in size medially, arranged in approximately 50 rows at midpoint of body. One semi-continuous row of enlarged, pore-bearing femoral scales per hindlimb, extending from the knee to near the groin in a series of 35–37 pores, with two additional pore-bearing scales parallel to the main row at the knee. Pore-bearing scales only slightly larger and weakly contrasting against rounded, weakly imbricate ventral femorals, but larger and distinct from granular posterior femorals. Precloacal pore row separated from femorals, in a distinct series of 16.

Limbs slender, forelimbs (FA/SVL 0.15) shorter and less robust than hindlimbs (HDL/SVL 0.19). Lateral and dorsal surfaces of crus with numerous conical tubercles, antebrachium with few and localized tubercles extending to the elbow. Digits long and well developed, inflected at basal interphalangeal joints (figure 5e,f); subdigital LAM smooth, rounded, undivided and expanded proximal to digital inflection (9–11–13–13–10 manus; 8–12–14–13–11 pes); narrow distal to digital inflection (9–10–12–13–12 manus; 9–11–13–14–13 pes) (counts excluding ungual sheath); large recurved claws sheathed by a dorsal and ventral scale.

Tail original (117 mm) and thin, scalation heterogeneous and irregular, grading from smaller dorsal scales to slightly larger scales ventrally. Hemipenile sacs swollen and prominent, each with four rounded cloacal spurs at anterolateral margin.

3.3.6. Colour in ethanol

Dorsum consists of nine dark-brown, irregular, transverse bands or stars between shoulders and pelvis, interspersed by lighter greyish cream-coloured regions of approximately similar width. Dark-brown bands bordered by lighter, interspersed tubercles. Bands between the shoulder and occipital regions most distinct, but irregularly shaped. Nuchal band joins occipital band and extends as a stripe anterolaterally to the ventral orbital margin. Crown of head, supraorbital region and snout dark-brown, with occasionally lighter cream-coloured splotches with brown tinge. Supraciliaries dark-brown. Limbs and toes distinctly splotched to banded with dark-brown on medium-brown on upper and lateral surfaces. Ventral ground coloration cream with brownish tinge and extensive, lighter, off-white flecks throughout, generally composed of one to a few scales. Dorsal and lateral surfaces of tail darker chocolate brown with six indistinctly edged, dark-brown blotches or bands, separated by thin, creamish bands, before gradually lightening to cream again at the distal end. Subcaudal surface dark-brown with scattered lighter cream-coloured spots, becoming more immaculately dark-brown posteriorly, before gradually lightening at the tip.

3.3.7. Details of holotype

Measurements (in mm): SVL 96.7; TL 117; TrK 45.9; HW 16.9; HH 9.5; HL 23.6; EN 8.2; IN 3.4; OrB 7.6; EAR 1.6; FA 14.8; HDL 17.9. Meristic data: SUPR 12R/11 L (10 to midpoint of eyes); INFR 14; INTER 2; DTR 15, VENT 50. LAMT1 8 expanded, 10 narrow; LAMT4 13 expanded, 15 narrow; POR 90 (PREPOR 16, FEMPOR 38R/36 L).

3.3.8. Variation

Summary of meristic values for all adults (nine males, three females) in the type series are as follows (mean, with the range in parentheses): SVL 92.7 (88.0–96.7); TL 79.8 (13.0–117.0); OT 107.5 (95.0–117.0); TrK 44.8 (42.5–47.6); HW 16.6 (16.1–17.5); HL 23.6 (22.5–24.7); HH 9.3 (8.7–9.6); EN 8.3 (7.8–8.7); OrB 7.3 (6.9–7.7); EAR 1.5 (0.9–2.0); FA 15.1 (14.7–15.9); HDL 17.9 (16.9–18.5) (table 1 for a breakdown of measurements by sex).

Summary mensural data for these same individuals are as follows in mm: SUPR (to midpoint of eye) 9.9 (9–11); SUPR (rictus of mouth) 12.1 (10–14); INFR 12.9 (11–14); LAMT1 expanded 8.4 (7–9), narrow 8.4 (7–10); LAMT4 expanded 12.3 (11–14), narrow 13.2 (11–15); DTR 15.2 (14–16); VENT 49.6 (46–54); POR 89.1 (83–94); PREPOR 16.1 (15–17); FEMPOR 36.5 (31–39) per hindlimb with 0–2 pore bearing scales out of line at the knee, PCTUB 3(1–4).

Dorsal colour pattern always consists of variably defined, contrasting transverse bands of dark to chocolate-brown against an off-white to cream-coloured to light-brown ground colour (figure 6). Dark bands fairly well-defined, particularly along their posterior borders; roughly equivalent width to or slightly narrower than the intervening lighter bands, both of which are less than half the width of the trunk. Occasionally spots invade the lighter bands. Some individuals have a lighter background coloration near the temples/occiput and light band along the supralabials. Venters cream to light-brown, often punctuated with lighter-coloured spots. Subcaudal surfaces variably spotted at the dorsal end to uniformly dark-brown, before gradually lightening at the tip.

All specimens have 14–16 tubercle rows at midbody. Subcaudal scales uniformly to slightly enlarged compared to those positioned dorsolaterally.

The colour pattern and scalation of the sole juvenile paratype (NMV75961, 58.5 mm SVL) is similar to that of the adults. Faint precloacal pores are present but difficult to count.

3.3.9. Comparisons

Cyrtodactylus tanim n. sp. differs from Australasian Cyrtodactylus species in the louisiadensis, loriae, novaeguineae and tuberculatus groups in its smaller size (adult SVL <100 mm versus >100 mm), in having minute femoral pores (figure 7) much smaller than the precloacal pores (versus clearly visible and similar sized), in lacking enlarged tubercles on the ventrolateral folds (versus present), and in lacking enlarged subcaudal scales (versus present in the C. louisiadensis and C. tuberculatus groups only) [32,34,35]. Cyrtodactylus tanim n. sp. differs from C. minor and C. papuensis in its larger adult size (SVL <80 versus >80 mm), much higher total number of pores (<30 versus >60), and further differs from the latter in lacking a precloacal groove [34,50].