Introduction
The Korean Peninsula, located in the marginal sea of the northwest Pacific, is surrounded by unique waters on three sides, each of which shows quite different oceanographic features. The Korean Peninsula exhibits a variety of environmental characteristics, with noticeable climatic differences in all cardinal directions (Lee et al., Reference Lee, Heo, Lee and Kwon2005). Additionally, complex ocean currents and water masses influence the Korean Peninsula, as it is situated between subtropical and subarctic waters (Rebstock & Kang, Reference Rebstock and Kang2003). Each sea surrounding Korean Peninsula has formed independent marine ecosystems because of their heterogeneous characteristics (Figure 1). The East Sea, also called Japan Sea, has a monotonous coastline with few Islands and bays and has developed a deep-sea ecosystem due to its average depth of about 1700 m and the maximum depth of 4049 m (Barnes & Mann, Reference Barnes and Mann1991; Kang et al., Reference Kang, Kim, Park, Kim, Ryu, Kang and Park2014). In the East Sea, the East Korea Warm Current (EKWC) and North Korean Cold Current (NKCC) meet, forming a subpolar front (Gong & Son, Reference Gong and Son1982; Cho et al., Reference Cho, Kim, Kang, Lee, Kim, Choi and Choi2004; Kang et al., Reference Kang, Kim, Park, Kim, Ryu, Kang and Park2014). The Jeju Warm Current (JWC), which splits from the Tsushima Warm Current (TWC), flows clockwise around Jeju-do Island and transports warm and saline water to the Korea Strait through the Jeju Strait, while the Yellow Sea Bottom Cold Water (YSBCW) expands to the east from the southern Yellow Sea by baroclinic conditions and southerly monsoon winds (Wang et al., Reference Wang, Hirose, Kang and Takayama2014; Yang et al., Reference Yang, Cho, Seo, You and Seo2014; Kim et al., Reference Kim, Choi, Kim and Sun2022). Since the southern part of Jeju-do Island is directly affected by the high-temperature and -salinity water of the TWC, subtropical fish are highly abundant and diverse (Kim & Rho, Reference Kim and Rho1994; Ko et al., Reference Ko, Kim, Kim and Rho2003; Kim, Reference Kim2009). Marine biodiversity serves as an indicator of a healthy marine ecosystem and plays a crucial role in supporting the structure and function of ecosystems (Costanza & Mageau, Reference Costanza and Mageau1999; Worm & Lotze, Reference Worm, Lotze and Letcher2009; Johnson et al., Reference Johnson, Runge, Alexandra Curtis, Durbin, Hare, Incze, Link, Melvin, O'Brien and Guelpen2011). Therefore, considerable efforts need to be made to monitor changes in marine biodiversity and biological responses to global warming in these areas.
Figure 1. Schematic diagram showing diverse oceanic currents and water masses affecting the seas around the Korean peninsula cited from Yu & Kim (Reference Yu and Kim2018) and Nakayama (Reference Nakayama2022).
During our field survey monitoring fish species around Jeju-do Island and Busan, we discovered three previously unrecorded fish species, Diplogrammus xenicus (Callionymidae), Erilepis zonifer (Anoplopomatidae), Pseudojuloides paradiseus (Labridae). E. zonifer, North Pacific boreal species, inhabits the sea surface at juvenile stages but it descends deeper as it grows (Orlov et al., Reference Orlov, Tokranov and Megrey2012). Although D. xenicus and P. paradiseus are subtropical species, they tend to avoid high-temperature water around the equator (Briggs, Reference Briggs1999; Tea et al., Reference Tea, Greene, Earle and Gill2020). Furthermore, both of them show sexual dimorphism, males are splendid and females are relatively monotonous.
Their first records in Korean waters suggest an expansion of their habitat range, which might be related to climate change. The purpose of this study is to describe morphological and molecular characteristics of the species, confirm their taxonomic status, and discuss the implications of these findings in Korean waters.
Materials and methods
P. paradiseus specimen was collected with a lift net in Seogwipo-si, southern Jeju-do Island on 25 May 2022. D. xenicus specimen was collected with a scoop net in Seogwipo-si, southern Jeju-do Island on 14 August 2022. E. zonifer specimen was collected with a gill net in Busan, which is located at the boundary between the Korea Strait and the East Sea, on 18 July 2022. The specimens were transported to the Ichthyology laboratory at Pukyong National University (PKU) and identified following Nakabo (Reference Nakabo1983, Reference Nakabo2013) and Tea et al. (Reference Tea, Greene, Earle and Gill2020). They were fixed in 10–15% formalin, and preserved in 70% ethanol after washing. Three specimens were deposited in National Marine Biodiversity Institute of Korea (MABIK). Meristic characters were conducted following Lockington (Reference Lockington1880), Fricke & Zaiser (Reference Fricke and Zaiser1982), Orlov et al. (Reference Orlov, Tokranov and Megrey2012), and Tea et al. (Reference Tea, Greene, Earle and Gill2020). The specimens were measured using a tapeline and vernier callipers, and measurements were converted into ratios (%) relative to total length (TL) or SL (Figure 2). Molecular analysis was performed to confirm morphology-based species identifications. Total genomic DNA was extracted from muscle tissue using 10% Chelex 100 resin (Bio-Rad, Hercules, CA, USA). The mitochondrial DNA (mtDNA) cytochrome c oxidase subunit I (COI) was amplified using the universal primer set developed by Ward et al. (Reference Ward, Zemlak, Innes, Last and Hebert2005). We used the PCR conditions sas follows: predenaturation at 95 ℃ for 5 min; 35 cycles of denaturation at 95 ℃ for 30 s, annealing at 52 ℃ for 45 s, extension at 72 ℃ for 45 s; final extension at 72 ℃ for 7 min. The amplified sequences were deposited in the National Center for Biotechnology Information (NCBI) database. Sequence alignments were conducted using CLUSTALW (Thompson et al., Reference Thompson, Higgins and Gibson1994) within BioEdit version 7 (Hall, Reference Hall1999). Subsequently, genetic divergence was calculated using the Kimura two-parameter model (Kimura, Reference Kimura1980), and a neighbour-joining tree was constructed to infer the phylogenetic relationships among specimens.
Figure 2. Diagrams of the measurements: A. D. xenicus; B. E. zonifer; C. P. paradiseus (1, total length; 2, standard length; 3, head length; 4, head depth; 5, snout length; 6, orbital diameter; 7, postorbital length; 8, upper jaw length; 9, lower jaw length; 10, prepectoral length; 11, pectoral length; 12, prepelvic length; 13, pelvic length; 14, pelvic spine length; 15, predorsal length; 16, dorsal fin base length; 17, first dorsal spine length; 18, second dorsal spine length; 19, last dorsal spine length; 20, longest dorsal ray length; 21, first dorsal fin base length; 22, second dorsal fin base length; 23, body depth; 24, greatest body depth; 25, anal fin base length; 26, first anal spine length; 27, second anal spine length; 28, third anal spine length; 29, longest anal ray length; 30, preanal length; 31, caudal peduncle length; 32, caudal peduncle depth; 33, caudal length).
Results
Diplogrammus xenicus (Jordan & Thompson, Reference Jordan and Thompson1914) (Perciformes: Callionymidae) (×Figure 3A)
Material examined. MABIK PI00061773 (PKU 62992), 1 specimen, male, 123.8 mm TL, Seogwipo-si, Jeju-do Island, Korea (33°13’21.1”N 126°14’30.9”E)
Figure 3. Photographs of unrecorded fish species collected from Korea: A, D. xenicus, MABIK PI00061773 (PKU 62992), 94.5 mm SL, collected from Jeju-do Island; B, E. zonifer, MABIK PI00061776 (PKU 63131), 116 cm SL, collected from Busan; C, P. paradiseus, MABIK PI00061777 (PKU 63132), 144.4 mm SL, collected from Jeju-do Island. The scale bars of A and C indicate 1 cm, and a bar of B indicates 10 cm.
Diagnosis. D. IV-8; A. 7; P1. ii+15~17; mouth small; infraorbital canals branched; preopercle not barbed; body with dermal fold; opercle with flap; caudal fin not protruding; diagonal patterns on anal fin (no pattern in female).
Description (in males). Body compressed and elongated. Head and mouth small in proportion to body length. Lower lip with few fleshy papillae. Infraorbital canals branched. Posterior tip of preopercle not barbed. Opercle with flap. Both lateral lower sides of body with a dermal fold-like ridge. First dorsal spine elongated. All caudal fin rays branched. Lateral line reaching to caudal fin rays. Head and body brownish. Eye yellowish. Posterior preopercle with dark blue speckle. Blue blotches and spots on head to caudal fin. Upper of pectoral fin whitish and lower part blackish with blue spots. Dorsal fin dark yellowish with translucent oblique patterns. Anal fin black with light lines and spots. Upper half of caudal fin yellow and lower part blackish.
Distribution. Korea (Present study), Southern Japan, Philippines, Indonesia, and Western Australia (Sonoyama et al., Reference Sonoyama, Ogimoto, Hori, Uchida and Kawano2020; GBIF Secretariat, 2023).
Remarks. D. xenicus can be distinguished from closely related species, such as D. goramensis, by the shape of the infraorbital canal. D. goramensis has no branched infraorbital canal, unlike D. xenicus (Nakabo, Reference Nakabo2013). These species exhibit sexual dimorphism, so species identification based on morphological traits can be challenging (Fricke & Zaiser, Reference Fricke and Zaiser1982). In adult males, the colouration of the lower anal fin rays differs. D. xenicus has short oblique black lines on the anal fin, while D. goramensis has many small dark spots. The counts and measurements are well-matched with previous studies (Jordan & Thompson, Reference Jordan and Thompson1914; Fricke & Zaiser, Reference Fricke and Zaiser1982) (Table 1). Also, molecular identification based on mtDNA COI sequences supported the morphology-based results of D. xenicus (Figure 4). As this is the first record in Korea, we suggest the new Korean name of the genus and species, ‘Ju-reum-dot-yang-tae-sok’ and ‘Ju-reum-dot-yang-tae’.
Table 1. Comparison of the morphometrics and meristic characters of D. xenicus
Figure 4. Neighbor-Joining tree based on mtDNA COI sequences. Each mark indicates the family of species and the colour indicates distinct species: circle (
), Labridae; Square (
), Anoplopomatidae; Diamond (
), Callionymidae; Triangle (
), outgroups.
Erilepis zonifer (Lockington, Reference Lockington1880) (Perciformes: Anoplopomatidae) (Figure 3B)
Material examined. MABIK PI00061776 (PKU 63131), 1 specimen, 1310 mm TL, Busan, Korea (35°09’02.6”N 129°09’10.6”E)
Diagnosis. D. XII~XIV-I~II, 16~21; A. II~III, 11~14; P1. 16~19; LL. 120~130; body deep and short; the first and second dorsal fins proximal; white spots on side of body (uniformly dark as they grow).
Description. Body slightly deep and stout-like. Head and mouth large. Lips thick. Eyes small. Nostrils below midline of eye. Upper jaw not reaching to eye. No spine on preopercle and opercle. Pectoral fin ahead of pelvic fin. Pectoral fin reaching to between the 6th and 7th spine of the first dorsal fin. The first and second dorsal fins proximal. Anal fin base short. Caudal fin truncated. Lateral line reaching to caudal peduncle. Scales small and ctenoid. Head and body deep dark. Large dark spots and blots on the lateral side of body. All fin ray black.
Distribution. Korea (Present study), Japan, Russia, USA (East of around 138° E) (Mecklenburg, Reference Mecklenburg2003; Nakabo, Reference Nakabo2013; GBIF Secretariat, 2023).
Remarks. The family Anoplopomatidae comprises only two genera and two species worldwide (Froese & Pauly, Reference Froese and Pauly2023): Anoplopoma fimbria (Pallas, Reference Pallas1814) and E. zonifer. Anoplopomatidae species can be distinguished by their body shape and the distance between the first and second dorsal fins. A. fimbria has a slender and slightly compressed body with well-separated first and second dorsal fins. Our specimen of the first dorsal fin base length is 22.1% in TL (25.0% SL), other specimens are 17.7% in TL by Jordan & Thompson (Reference Jordan and Thompson1914) and 13.2–15.7% in SL by Lockington (Reference Lockington1880) and Orlov et al. (Reference Orlov, Tokranov and Megrey2012) (Table 2). Because we investigated only one specimen, it seems to be an individual variation. Molecular identification based on mtDNA COI sequences supported morphology-based results of E. zonifer with a high degree of confidence (Figure 4). As this species was named as ‘Keun-eun-dae-gu’ by NIFS (2010) previously, we followed the name, and suggest the new Korean name for the family and genus, ‘Eun-dae-gu-gwa’, ‘Keun-eun-dae-gu-sok’, respectively.
Table 2. Comparison of the morphometrics and meristic characters of E. zonifer
Please align it to the center.
Pseudojuloides paradiseus Tea, Gill & Senou, 2020 (Perciformes: Labridae) (Figure 3C)
Material examined. MABIK PI00061777 (PKU 63132), 1 specimen, male, 162.8 mm TL, Seogwipo-si, Jeju-do Island, Korea (33°13’21.1”N 126°14’30.9”E)
Diagnosis. D. IX, 12-13; A. III, 12; median predorsal scales lack; large canine tooth on corner of mouth; colour of male: body bright yellow to orangish pink, dorsal of body black with blue dashed line; female: body reddish orange to dark red, dorsal unmarked.
Description (in males). Body compressed and elongated. Head moderately large and convex. Mouth and eyes small. Teeth well-developed. Upper jaw slightly protruded. Anal fin bases long. Caudal fin slightly round. Scales large and ctenoid. Lateral line continuous. Head with purplish wavy stripes. Body yellowish orange to pinkish orange. Blue and Black blotches under pectoral fin. Metallic blue or purplish stripes that broke into spots on upper lateral side in males. Pelvic fin pale with orange spots. Dorsal fin yellow with orange mark. Anal fin pink to orange with blue margin. Caudal fin yellow.
Distribution. Korea (Present study), Japan (Sagami Bay) (Tea et al., Reference Tea, Greene, Earle and Gill2020).
Remarks. P. paradiseus closely resembles its congeners P. elongatus and P. crux. All three species have overlapping meristic and morphometric ranges, and their genetic divergence shows an extremely close level of 0.1–1.5%. However, despite their morphological and genetic similarities, P. elongatus, P. crux, and P. paradiseus are recognized as valid species due to their distinct distribution differences. P. elongatus is found only around eastern Australia, P. crux is found only around western Australia, and P. paradiseus is found in the northwest Pacific, specifically around Japan. We identified our specimen as P. paradiseus based on morphological, molecular characteristics, and distribution (Figure 4; Table 3). This genus of species is the first record in Korea, so we suggest the new Korean name of the genus and species, ‘Pa-ra-da-i-seu-nol-rae-gi-sok’ and ‘Pa-ra-da-i-seu-nol-rae-gi’, respectively.
Table 3. Comparison of the morphological characters of P. paradiseus, P. elongatus, and P. crux
Discussion
As a result of monitoring a fish fauna around the Korean waters during the summer, we firstly found three unrecorded fish species belonging to the subtropical and boreal fishes. The two subtropical species collected from Jeju-do Island, D. xenicus and P. paradiseus, are generally known to prefer temperatures of 27–28 °C (Froese & Pauly, Reference Froese and Pauly2023). Since D. xenicus is a bottom-dwelling fish that inhabits shallow waters at depths of 9–27 m (Fricke & Zaiser, Reference Fricke and Zaiser1982), it may have a limited migratory range. P. paradiseus has been considered an endemic species of Japan, but the recent discovery of the species in Korean waters suggests the possibility of its range expansion. P. paradiseus was previously considered a synonym of P. elongatus but was recognized as a new species with a distinct distribution by Tea et al. (Reference Tea, Greene, Earle and Gill2020). In their study, Tea et al. (Reference Tea, Greene, Earle and Gill2020) divided P. elongatus into three species: P. elongatus sensu stricto from Eastern Australia, P. crux from western Australia, and P. paradiseus from Japan. They exhibit vicariance, with their distribution extending from the far northern hemisphere to the far southern hemisphere. It has also been suggested that D. xenicus belongs to a group of representative anti-tropical species, in contrast to similar species such as D. goramensis which inhabits tropical waters (Fricke, Reference Fricke1988; Briggs, Reference Briggs1999, Reference Briggs2005). In the case of anti-tropical species, allopatric speciation might have occurred due to water temperature barriers after the species migrated across the equator to the opposite hemisphere during the last glacial maximum, during which SST decreased (Burridge, Reference Burridge2002; Briggs, Reference Briggs2003; Le Port et al., Reference Le Port, Pawley and Lavery2013; Kai & Motomura, Reference Kai, Motomura, Kai, Motomura and Matsuura2022).
The boreal species E. zonifer was collected from Busan, located at the boundary between the East Sea and the Korea Strait. Except for a single immature specimen of 50 cm SL occurring in waters off Shizuoka on the Pacific side of Japan (34.9° N, 138.5° E) (Orlov et al., Reference Orlov, Tokranov and Megrey2012; Zolotov et al., Reference Zolotov, Spirin and Zudina2014), it has been almost exclusively recorded in the North Pacific Ocean above 36° N (GBIF Secretariat, 2023). The present study demonstrates that the distribution of E. zonifer extends to the southwest of the East Sea. The collected depth of E. zonifer is in relatively deep water at 100–200 m. The water temperature at 100–105 m was approximately 4.41–5.31 °C at that time. The SST of the Korea Strait, where E. zonifer was collected, is known to be highest during summer due to the TWC, while the sea bottom temperature is lowest during the same period due to the NKCC (Lim & Chang, Reference Lim and Chang1969; Cho & Kim, Reference Cho and Kim1998). The range expansion of this species might be related to the southward expansion of the NKCC, as the TWC strengthens to the north due to the compensation effect (Lim, Reference Lim1971; Mitta & Ogawa, Reference Mitta and Ogawa1984; Isobe et al., Reference Isobe, Tawara, Kaneko and Kawano1994). Global warming promotes large-scale changes in atmospheric circulation, including the strengthening of the North Pacific gyre and changes in the Hadley and Ferrell circulations or Kuroshio and Kuroshio extensions (Cheon et al., Reference Cheon, Park, Kim, Na and Kim2012; Choi et al., Reference Choi, Park and Choi2013). These changes eventually impact the strength of the TWC. Due to these complex shifts in physical processes, we carefully suggest that the southern boundary of E. zonifer might be expanding southward.
The simultaneous appearance of two subtropical species and one boreal species implies that the waters around the Korean Peninsula are exposed to quite complex marine shifts. The Intergovernmental Panel on Climate Change (IPCC) has reported that global ocean warming due to climate change has more than doubled from 1993 to 2017 in comparison to 1969 to 1993, and they predict that the trend of increasing water temperatures will be higher in the western Pacific, including Korean waters, than the global average (Shukla et al., Reference Shukla, Skea, Calvo Buendia, Masson-Delmotte, Pörtner, Roberts, Zhai, Slade, Connors, van Diemen, Ferrat, Haughey, Luz, Neogi, Pathak, Petzold, Portugal Pereira, Vyas, Huntley, Kissick, Belkacemi and Malley2019). Over the past 130 years (1880–2009), global sea temperatures increased by 0.6 °C. In comparison, the SST of Korean waters has increased by 0.9–1.5 °C, i.e. up to three times faster than the global average (Kim et al., Reference Kim, Woo, Kim and Hur2011). Recently, the number of unrecorded fish species in Korea has been increased rapidly. Korean fish diversity has increased by 37%, i.e. from 872 species (Chyung, Reference Chyung1977) to 1193 species (Jeong & Kim, Reference Jeong and Kim2023; MABIK, 2023) within 46 years, which might be related, at least in part, to the rapid increase in SST in Korea (Kang & Jeong, Reference Kang and Jeong2000; Seo & Yoon, Reference Seo and Yoon2008; Kim, Reference Kim2009; Jung et al., Reference Jung, Ha and Na2013; Yoo et al., Reference Yoo, Kim and Choi2014). These findings indicate that Korean waters are undergoing significant change.
To conserve global biodiversity in light of future climate change, fish species composition and metapopulation dynamics should be monitored continuously. Specifically, it needs to focus on the frontal area (e.g. East Sea), which is characterized by dramatic temperature and salinity changes that serves as a biogeographical barrier by the intersection of subtropical and boreal waters; this leads to adaptive responses of local populations, and finally speciation (Kim et al., Reference Kim, Choi, Chang and Kim2002, Reference Kim, Watson, Hyde, Lo, Kim, Kim and Kim2010a, Reference Kim, Kim, Han, Nam, Kim, Kong, Noh and Yoon2010b; Gwak & Nakayama, Reference Gwak and Nakayama2011; Myoung & Kim, Reference Myoung and Kim2014; Bae et al., Reference Bae, Kim, Park and Kim2020a, Reference Bae, Kim and Li2020b; Song et al., Reference Song, Bae, Kang, Park and Kim2020a, Reference Song, Myoung and Kim2020b).
Acknowledgements
The authors sincerely thank Dr Senou (Kanagawa Prefectural Museum) for borrowing the comparative specimens, and Jae-Kyung Bae, Si-Young Jeong and the fishermen for helping collect specimens. Also authors thank anonymous reviewers for their valuable comments that improved the quality of this article.
Authors’ contributions
All authors read and approved the final manuscript.
Financial support
This research was supported by the management of Marine Fishery Bio-resources Center (2024) funded by the National Marine Biodiversity Institute of Korea (MABIK). Also, this work was supported by a grant from the National Institute of Fisheries Science (R2024003).
Competing interests
The authors declare no conflict of interest, the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.
Ethical standards
Not applicable.
