Corresponding author: Surya Narayanan ( surya.ornata@gmail.com ) Academic editor: Uwe Fritz
© 2022 Sandeep Das, Saunak Pal, Sasidharan Siddharth, Muhamed Jafer Palot, Veerappan Deepak, Surya Narayanan.
This is an open access article distributed under the terms of the Creative Commons Attribution License (CC BY 4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Citation:
Das S, Pal S, Siddharth S, Palot MJ, Deepak V, Narayanan S (2022) A new species of large-bodied Hemidactylus Goldfuss, 1820 (Squamata: Gekkonidae) from the Western Ghats of India. Vertebrate Zoology 72: 81-94. https://doi.org/10.3897/vz.72.e76046
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Abstract
A new large (94–107mm SVL) species of gecko of the genus Hemidactylus is described from the drier parts of the Western Ghats of India. The new species is closely related to H. graniticolus, from which it can be distinguished based on dorsal pholidosis at mid-body, the structure of tubercles on the dorsum, dorsal pholidosis on the tail. The new species is also 6.6–7.2% divergent from H. graniticolus in the ND2 mitochondrial gene.
Gecko, Kerala, morphology, ND2, new species, phylogeny, taxonomy
The gekkonid genus Hemidactylus Goldfuss, 1820 is one of the most specious groups of geckos with 180 known species distributed across the globe (
Among these larger geckos (SVL >100 mm), seven species are restricted to the Western Ghats, namely: Hemidactylus aaronbaueri Giri, 2008; H. maculatus Duméril & Bibron, 1836; H. prashadi Smith 1935; H. paaragowli Srikanthan, Swamy, Mohan & Pal, 2018; H. acanthopholis Mirza & Zanap, 2014; H. vanam Chaitanya, Lajmi & Giri, 2018; and H. tamhiniensis Khandekar, Thackeray & Agarwal, 2021. Three species, H. graniticolus Agarwal, Giri & Bauer 2011; H. triedrus Daudin,1802; and H. whitakeri Mirza, Gowande, Patil, Ambekar & Patel 2018 seems to be widespread and are reported from the Western Ghats, the Eastern Ghats and the Mysore plateau (
We collected four specimens of Hemidactylus sp. and generated DNA sequence for two specimens of Hemidactylus sp. (ZSI/WGRC/IR.V/3471 &
Bidirectional sequences were manually checked using the CHROMAS 2.6.6 software (http://technelysium.com.au/wp/chromas) and aligned using ClustalW (
A Maximum Likelihood (ML) analysis was carried out with RAxML GUI version 2.0 (
All the morphological characters examined (mensural and meristic) follow
Comparative data for the Hemidactylus graniticolus were obtained from
Museum abbreviations are as follows:
In both ML and BI analyses, the new species is recovered as a sister to the Hemidactylus graniticolus sensu stricto clade with strong support (ML 88, BI 1.0) and are together forming a strongly supported (ML 100, BI 1.0) monophyletic group with three other putative species identified as H. cf. graniticolus (see,
ML phylogeny showing the phylogenetic relationships of Hemidactylus easai sp. nov. Numbers at internal branches are posterior probability and ML bootstrap support values, respectively. Sample marked in blue is generated in this study and sample from the type locality of H. graniticolus is marked in red.
Uncorrected pairwise distances for mitochondrial ND2 gene among the graniticolus clade.
1 | 2 | 3 | 4 | 5 | 6 | 7 | 8 | 9 | 10 | 11 | 12 | 13 | 14 | ||
1 | Hemidactylus graniticolus AK348 | ||||||||||||||
2 | Hemidactylus graniticolus AK347 | 1.4 | |||||||||||||
3 | Hemidactylus graniticolus CES15213 | 1.2 | 1.4 | ||||||||||||
4 | Hemidactylus graniticolus CES15236 | 0.7 | 1.4 | 1.0 | |||||||||||
5 | Hemidactylus graniticolus AK117 | 1.2 | 2.0 | 1.6 | 1.5 | ||||||||||
6 | Hemidactylus graniticolus CESG380 | 3.9 | 4.0 | 3.9 | 3.9 | 4.4 | |||||||||
7 | Hemidactylus graniticolus CES15257 | 1.6 | 1.8 | 1.9 | 1.6 | 1.8 | 3.1 | ||||||||
8 | Hemidactylus easai sp. nov. ZSI/WGRC/IR.V/3471 | 7.0 | 7.2 | 7.1 | 7.2 | 6.6 | 7.1 | 6.6 | |||||||
9 |
Hemidactylus easai sp. nov. |
7.0 | 7.2 | 7.1 | 7.2 | 6.6 | 7.1 | 6.6 | 0.0 | ||||||
10 | Hemidactylus cf. graniticolus CESG146 | 10.6 | 10.4 | 10.4 | 10.7 | 10.6 | 10.1 | 10.0 | 8.8 | 8.8 | |||||
11 | Hemidactylus cf. graniticolus CESG139 | 10.1 | 9.9 | 9.8 | 10.1 | 10.1 | 10.0 | 9.5 | 8.5 | 8.5 | 1.1 | ||||
12 | Hemidactylus cf. graniticolus CESG122 | 9.8 | 9.7 | 9.7 | 10.0 | 9.4 | 9.2 | 9.2 | 9.3 | 9.3 | 8.2 | 7.9 | |||
13 | Hemidactylus cf. graniticolus CESG123 | 9.8 | 9.7 | 9.7 | 10.0 | 9.4 | 9.2 | 9.2 | 9.3 | 9.3 | 8.2 | 7.9 | 0.0 | ||
14 | Hemidactylus cf. graniticolus CES15265 | 10.4 | 9.6 | 9.7 | 10.0 | 9.6 | 9.3 | 9.7 | 8.7 | 8.7 | 6.0 | 5.7 | 7.8 | 7.8 | |
15 | Hemidactylus kolliensis BNHS2537 | 17.2 | 17.0 | 16.3 | 16.2 | 16.0 | 14.9 | 17.0 | 16.9 | 16.9 | 17.6 | 17.2 | 18.0 | 18.0 | 18.3 |
ZSI/WGRC/IR.V/3471 (Figs
ZSI/WGRC/IR.V/3472 (adult male),
The specific epithet is a patronym honouring Dr P. S. Easa, former director of Kerala Forest Research Institute, Thrissur, Kerala for his contributions towards wildlife research, conservation and management, primarily in the Western Ghats over the last four decades and for mentoring SD. We suggest Easa’s rock gecko as common name.
A large-sized gecko of the genus Hemidactylus, snout-vent length up to SVL 107 mm (n=4). Dorsal pholidosis heterogeneous, composed of roughly circular, granular scales intermixed with much enlarged, fairly regularly arranged longitudinal rows of 17 or 18 striated subtrihedral tubercles at midbody (Fig.
The holotype, an adult male, (SVL 105.8 mm) well preserved and is in good condition. Head short (HL/SVL 0.30), slightly elongate (HW/HL 0.76), not strongly depressed (HH/HL 0.41), distinct from neck. Loreal region slightly inflated, canthus rostralis indistinct (Fig.
Dorsal pholidosis heterogeneous, composed of subcircular granular scales intermixed with enlarged, fairly regularly arranged strongly keeled, pointed tubercles in 18 longitudinal rows, extending from occiput to tail, that are heterogeneous in shape and size; enlarged tubercles on the two most medial parasagittal rows slightly smaller than rest on dorsum and the rows most broadly spaced from one another, gradually increasing in size and becoming conical towards flanks, last two rows on flanks slightly smaller than medial parasagittal rows and strongly conical; each enlarged tubercle surrounded by a rosette of 12–15 small granules with 2–5 granules between two longitudinally adjacent enlarged tubercles (3–6 between parasagittal rows at midbody); enlarged tubercles on nape and shoulder smaller and conical, those on occiput and the temporal region still smaller, conical.
Ventral scales larger than dorsal granular scales, smooth, imbricate, slightly larger on precloacal and femoral region than on chest and abdominal region; midbody scale rows across belly 42; gular region with small, granular scales, becoming slightly larger and imbricate on anterior and lateral aspect. Scales on palm and sole smooth, imbricate, subcircular; scales on the dorsal aspect of upper arm subequal last row of enlarged tubercles on dorsum, flat, weakly pointed, imbricate, keeled; dorsal aspect of forearm with smaller, granular scales, intermixed with a few enlarged, conical tubercles, those on anterior aspect are smooth, flat, imbricate; scales on dorsal part of thigh and shank granular, except those on knee flat, imbricate, intermixed with enlarged, conical tubercles, which are larger on thigh compared to shank; anterior aspect of thigh with flatter scales, posterior aspect with granular scales. Twenty-five and twenty-four pores in an enlarged row of femoral scales on left and right side respectively, separated medially by a diastema of four pore-less scales; subequal row of enlarged scales anterior to pore-bearing scales (Fig.
Tail regenerated; depressed, flat beneath, verticillate, with well-defined median furrow; scales on the dorsal aspect of tail subimbricate, larger than granules on dorsum, with a series of 4–10 much enlarged, strongly pointed, moderately keeled tubercles; ventral scales enlarged, imbricate, median row (subcaudal plates) covering almost entire base of the tail, bordered laterally by two or three rows of larger pointed, smooth, imbricate scales; those close to vent small, smooth, flat and imbricate (Fig.
Variations in the paratypes in some of the meristic and mensural characters are provided in the Table
Meristic and mensural data for the type series of Hemidactylus easai sp. nov. * denotes incomplete tail.
Voucher no. |
Holotype: ZSI/WGRC/ IR.V/3471 |
Paratype 1: ZSI/WGRC/ IR.V/3472 |
Paratype 2: |
Paratype 3: |
Sex | Male | Male | Female | Female |
SVL | 105 | 104.6 | 107 | 94.3 |
AGL | 43.3 | 39.7 | 43 | 38.3 |
BW | 30.1 | 21.8 | 21.8 | 23.4 |
TL | 101 | 102 | 87.8 | 19* |
TW | 17.6 | 14.2 | 12.1 | 12.1 |
HL | 30.5 | 30.8 | 30.1 | 26.9 |
HW | 23.3 | 22.6 | 21.5 | 19.1 |
HD | 12.8 | 12.6 | 12 | 11.3 |
FL | 14.7 | 14.1 | 13.4 | 13.5 |
CL | 17.8 | 17.4 | 17 | 15.9 |
ED | 5.9 | 6.1 | 5.6 | 4.8 |
EN | 10.1 | 9.3 | 9.5 | 8.7 |
ES | 12.9 | 12.5 | 12.5 | 10.6 |
EE | 8.3 | 8.9 | 8.1 | 8 |
EL | 2.1 | 2.4 | 2.2 | 2 |
IN | 2.7 | 2.4 | 2.6 | 2.5 |
IO | 9.6 | 10 | 9.8 | 9.3 |
Femoral pores (pore-less scales separating series) | 25&24(4) | 30&28(2) | ||
DTR | 18 | 18 | 17 | 18 |
PVT | 20 | 21 | 23 | 22 |
MVSR | 42 | 41 | 42 | 42 |
Supralabials (L&R) | 11&11 | 13&12 | 12&12 | 12&10 |
Infralabials (L&R) | 10&10 | 10&10 | 10&10 | 10&10 |
Supralabials to midorbit (L&R) | 9&9 | 9&9 | 9&9 | 9&9 |
Infralabials to midorbit (L&R) | 8&8 | 8&8 | 8&8 | 8&8 |
Manus left | 11-12-12-12-12 | 12-13-13-13-13 | 10-12-13-11-13 | 10-11-12-12-13 |
Manus right | 10-13-12-12-11 | 12-13-13-12-13 | 10-12-12-12-12 | 10-12-12-12-11 |
Pes left | 10-14-13-13-12 | 11-13-13-13-13 | 11-13-13-13-14 | 11-13-13-13-13 |
Pes right | 10-14-13-13-13 | 11-13-13-13-13 | 11-13-13-13-13 | 10-13-13-13-13 |
Dorsal aspect of the body, uniformly brownish with four indistinct transverse bands from the neck to the hind limb insertion and two on the tail, bordered by discontinuous black patches (Fig.
Hemidactylus easai sp. nov. differs from the other large-bodied congeners by several non-overlapping morphological characters. It can be distinguished by the presence of 24–30 femoral pores (FP) separated by 2–4 pore-less scales (vs. 21 FP separated by two pore-less scales in H. kolliensis; 19–21 FP separated by 13–14 pore-less scales in H. acanthopholis; 22–24 FP separated by 3–6 pore-less scales in H. hunae; 16–18 FP separated by 13–14 pore-less scales in H. sirumalaiensis; 17–22 FP separated by 10–11 pore-less scales in H. vanam; 21–24 PF separated by four pore-less scales in H. sushilduttai; 15–19 FP separated by 3 pore-less scales in H. depressus; 17–18 FP separated by 5 pore-less scales in H. siva; 7–9 FP separated by 1–3 pore-less scales in H. triedrus; 11–15 FP separated by 1–3 pore-less scales in H. sahgali; 7–8 FP separated by 3 pore-less scales in H. whitakeri; 21–24 FP separated by 5–7 pore-less scales in H. kimbulae; 15–19 FP separated by 6 pore-less scales in H. aaronbaueri, 17–18 FP separated by 7 pore-less scales in H. tamhiniensis,18–21 FP separated by 4 pore-less scales in H. kangerensis); by the presence of 16–18 rows of moderately keeled subtrihedral tubercles (vs. 22–24 in H. paaragowli; 14–16 in H. prashadi; 15–16 in H. kolliensis and homogeneous dorsal pholidosis with no enlarged tubercles in H. scabriceps); .
From the closely related Hemidactylus graniticolus, H. easai sp. nov. can be differentiated by the presence of moderate to strongly keeled tubercles on the dorsum (vs. weakly keeled or smooth tubercles on the dorsal aspect) (Fig.
Hemidactylus easai sp. nov. is currently known only from the type locality in the Kerala parts of the Western Ghats. The type series was collected from human settlements, inside buildings on the banks of the river Bhavani, which originates from the Nilgiri Hills of Western Ghats (Fig.
The type locality of H. easai sp. nov. is in a close proximity to the Silent Valley National Park (SVNP) but not under any legal protection. It is however possible that the new species is found within the SVNP and adjacent Nilgiris mountain range, given that the habitat is contiguous.
The rate at which Hemidactylus are being described from India is high in the last decade, with 16 new descriptions of the total 48 known species (
Beyond the specimens reported here, few other specimens previously identified as H. graniticolus or H. cf. graniticolus required a closer look. One specimen (
The dry zones of peninsular India are known for its high endemism in many squamate reptiles (Hemidactylus:
With the current description and the available distributional data, it is likely that H. graniticolus may be restricted to the Mysore plateau and parts of the southern Eastern Ghats. Hemidactylus easai sp. nov. is currently known from the north of the Palghat gap and is nested within the clade containing species from the Mysore plateau and the southern Eastern Ghats, in our phylogenetic analyses (Fig.
SD would like to thank Benjamin Tapley, Jyoti Das, Rajkumar KP, Nithin Divakar, EDGE team and EDGE of Existence fellowship program for all the support and encouragement. SD would like to thank the Principal, St. Joseph’s College (Irinjalakkuda, India) for the facilities provided. SN thanks Aravind NA, ATREE (Bengaluru, India) for the support at ATREE. SP thanks the Director,
Supplementary figures and tables
Data type: .zip
Explanation note: Supplementary tables and figures for Hemidactylus easai sp. nov.