Corresponding author: Joo Myun Park ( joomyun@gmail.com ) Academic editor: Ronald Fricke
© 2021 Se Hun Myoung, Laith A. Jawad, Joo Myun Park.
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:
Myoung SH, Jawad LA, Park JM (2021) New record of Neoclinus lacunicola (Actinopterygii: Perciformes: Chaenopsidae) from Ulleung Island, Korea revealed by body morphometry and mitochondrial DNA barcoding. Acta Ichthyologica et Piscatoria 51(4): 339-344. https://doi.org/10.3897/aiep.51.67056
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One specimen (38.3 mm SL) of Neoclinus lacunicola Fukao, 1980, belonging to the family Chaenopsidae, was first recorded from Ulleung Island, Korea (East Sea, otherwise known as the Sea of Japan) on 5 January 2021. This species was characterized by paired external pores of incomplete lateral line running from the upper margin of the opercle, seven pairs of supraorbital cirri arranged in two rows, occipital region with a pair of cirri, and 13 rays of pectoral fin. This species is morphologically similar to the Neoclinus toshimaensis Fukao, 1980, but differs in the number of cirri on the supraorbital (6–7 versus 9–11 cirri). This study documents the first report of N. lacunicola in Korean waters and proposes the new Korean name of ‘eol-lug-bi-neul-be-do-la-chi’ for the species. For the confirmation of the identity of the species, a partial gene sequence of the mt COI (570 bp) of N. lacunicola was obtained for the first time.
Neoclinus species, tube blenny, new record, rocky shore, East Sea, Sea of Japan
The family Chaenopsidae comprises 96 species belonging to 14 genera distributed worldwide, with one genus and eight species occurring in Japanese waters (
Neoclinus lacunicola Fukao, 1980 was firstly reported as a new species in 1980 (
To date, one species of tube blennies, i.e., Neoclinus bryope (Jordan et Snyder, 1902) has firstly been reported in Korean waters (
One specimen of N. lacunicola was collected from Tonggumi (37°27′33.50′′N, 130°51′28.84′′E) in the coastal waters of Ulleung Island, Gyeongsangbuk-do, Korea (East Sea, otherwise known as the Sea of Japan), by a SCUBA diver on 5 January 2021 (Fig.
To compare molecular data, total genomic DNA was extracted from the muscle tissue using 10% Chelex resin (Bio-Rad, Hercules, CA). A portion of the mitochondrial COI gene was amplified using universal primers (
MABIK PI00049728, 1 specimen, 38.3 mm SL, Tonggumi, Ulleung Island, Gyeongsangbuk-do, Korea (37°27′33.50′′N, 130°51′28.84′′E).
Description.
The body counts, measurements, and proportions of body parts are shown in Table
Morphometric measurements of the Neoclinus lacunicola in comparison with previous records.
Morphological characters | Presently reported specimen |
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Sex (number of specimens) | Female (1) | Male (1) | Female (2) | Male (2) |
Counts | ||||
Dorsal rays | XXII, 18 | XXIII, 19 | XXII–XXIII, 17–19 | |
Anal rays | II, 27 | II, 27 | II, 27 | |
Pectoral rays | 13 | 13 | 12 or 13 | |
Pelvic rays | I, 3 | I, 3 | — | |
Principal caudal rays | 7 + 6 = 13 | 7 + 6 = 13 | 7 + 6 = 13 | |
Measurements | ||||
Standard length [mm] | 38.3 | 48.8 | 38.9–49.4 | 38.0–42.8 |
% of standard length | ||||
Total length | 113.8 | 112.9 | 113.8–114.7 | 114.7–115.5 |
Body depth | 12.3 | 14.5 | 12.6–13.6 | 12.9 |
Head length | 20.4 | 20.5 | 21.5–24.2 | 23.1 |
Head width | 13.8 | 14.1 | — | — |
Head depth | 13.3 | — | 13.6–15.4 | 14.5 |
Orbit diameter | 4.3 | 4.3 | 5.9–6.9 | 6.1 |
Postorbital length | 13.1 | 13.3 | — | — |
Interorbital width | 1.3 | — | 1.0 | 0.9 |
Snout length | 4.0 | 3.9 | 4.4–4.5 | 5.1 |
Upper jaw length | 9.9 | 10.2 | 10.3–11.1 | 11.2 |
Pre-dorsal length | 15.9 | 15.6 | 15.4–17.5 | 17.3 |
Pre-anal length | 40.9 | 41.0 | 38.7–42.7 | 40.4 |
Length of dorsal fin base | 82.0 | 83.8 | 81.7–87.0 | 82.9 |
Length of soft dorsal fin base | 34.5 | 34.8 | — | — |
Length of anal fin base | 53.5 | 56.1 | 54.0–56.7 | 55.4 |
Anal origin to pelvic insertion | 20.1 | 23.3 | — | — |
Depth of caudal peduncle | 6.1 | 6.4 | 5.1–5.4 | 5.3–5.6 |
Length of caudal peduncle | 5.0 | 5.7 | 6.1–6.9 | 6.3–7.1 |
Length of 1st dorsal-fin spine | 5.5 | 6.4 | 5.9 | 7.0 |
Longest dorsal spine length | 9.0 (13th) | 8.4 (13th) | — | — |
Longest dorsal soft ray length | 11.8 (11th) | 10.2 (11th) | — | — |
Longest anal ray length | 9.1 (24th) | 8.2 (24th) | — | — |
Length of last dorsal-fin spine | 8.1 | — | 6.5–8.2 | 7.7 |
Length of 1st dorsal-fin soft ray | 9.7 | — | 8.7–10.5 | 9.3 |
Length of 1st anal-fin spine | 5.0 | 3.9 | 2.6–4.4 | 4.0 |
Length of 1st anal-fin soft ray | 7.6 | 6.4 | 5.7–6.9 | 7.9 |
Longest pectoral ray length | 16.4 (9th) | 12.5 (9th) | — | — |
Longest pelvic ray length | 9.4 (2nd) | 9.1 (2nd) | — | — |
Head red and body uniformly white with black patterns (Fig.
Based on an analysis of the mitochondrial cytochrome oxidase subunit I gene (COI) sequence (570 bp), the presently reported specimen was different from other six species of the genus Neoclinus with genetic distances of 0.141–0.220 (Fig.
A neighbor-joining tree, based on partial mtDNA COI region using Neoclinus lacunicola (MABIK PI00049728) and other species of Neoclinus. Numbers at branches indicate bootstrap probabilities in 10 000 bootstrap replications. Scale bar equals 0.02 of Tamura and Nei’s distance (1993) with K2 parameter model.
In this study, one specimen of chaenopsid fishes has been collected from Ulleung Island with body elongated and compressed, no scales, supraorbital and nasal cirri present (
Chaenopsid fishes, occurring in Korean waters, have previously been known only as two species (N. bryope and N. chihiroe), but an additional species has now been reported through this study. The ecological characteristics of chaenopsid fishes are known that they do not have large movements and inhabit small caves between rocks or in empty gastropod tubes (
We are grateful to Mr. Min-Su Woo and Mr. Jin Young Shin, Korea Institute of Ocean Science and Technology for their assistance with sampling. This research was funded by the Korea Institute of Ocean Science and Technology (grant numbers PE99913, PN90190). This work was also supported by the National Research Foundation of Korea (NRF) grant funded by the Korean government (MSIT) (No. 2020R1F1A1051773).