Evaluation from otolith Sr stable isotope ratios of possible juvenile growth areas of Japanese eels collected from the West Mariana Ridge spawning area

Abstract

The widely distributed East Asian Japanese eel Anguilla japonica constitutes a single genetically homogeneous population with a single spawning area near the West Mariana Ridge. Otolith ⁸⁷Sr/⁸⁶Sr ratios of adults (categorized as “river“, “estuarine” or “sea” eels, according to their habitat use history determined from otolith Sr:Ca ratio analysis) collected from the spawning area in 2008 and 2009 were examined in an attempt to determine their juvenile growth areas. In addition, ⁸⁷Sr/⁸⁶Sr ratios of water samples from rivers in China, Taiwan, Korea, and Japan were determined. Otolith ⁸⁷Sr/⁸⁶Sr ratios of the “river”, “estuarine” and “sea” eels were 0.707793, 0.708580-0.709944 and 0.709068, respectively, and water sample ratios from China, Korea, Taiwan, and Japan were 0.7104320-0.7141010, 0.7190826-0.7227976, 0.7115523-0.7146914 and 0.706191-0.712484, respectively. “River” and “estuarine” eels, which had otolith ⁸⁷Sr/⁸⁶Sr ratios less than 0.7092 (seawater ratio), appeared to have inhabited Japanese rivers and/or estuaries because similarly low isotope ratios were recorded only from Japan. However, the juvenile growth areas of other eels were unknown, as their origins could not be determined from otolith ⁸⁷Sr/⁸⁶Sr ratios alone, and required further information regarding otolith elemental and isotope compositions.

Introduction

The Japanese eel Anguilla japonica is a catadromous temperate species and a high value commercial fisheries target in East Asia. However, stock levels of Japanese eels associated with glass eel recruitment have shown serious declines throughout the distribution range in recent decades, as have those of two other Northern Hemisphere temperate eel species, the European eel A. anguilla and American eel A. rostrata. The 2010 catch of exploitable stock of Japanese eels and glass eels in Japan has been estimated as only 8% of maximum post-World War II catch levels (Tanaka 2014), with continued the downward trend thereafter. The European eel is listed as critically endangered on the IUCN Red List (2011 Version), and both Japanese and American eels were considered as “threatened” in 2014 by the IUCN (Japanese eel: Jacoby and Gollock 2014; American eel: Jacoby et al. 2014). Such a remarkable decline of eel stocks in the Northern Hemisphere is thought to have been caused by various anthropogenic factors, including overexploitation of stock, habitat loss due to construction of dams, weirs, sluices and culverts, pollution and disease, as well as by environmental factors, such as changes in climatic and oceanic current conditions, that are detrimental to larval recruitment (Feunteun 2002; Tatsukawa 2003; Dekker 2003; Kimura and Tsukamoto 2006; Kim et al. 2007; Friedland et al. 2007; Bonhommeau et al. 2008; Miller et al. 2009; Tsukamoto et al. 2009; Itakura et al. 2014; Yokouchi et al. 2014; Chang et al. 2015). The critical status of those eel populations has accelerated attempts to manage and restore them, involving studies on life history, including spawning and oceanic migration of larvae and maturing adults, habitat use and behavior (“yellow eel” stage) (Feunteun 2002), as well as artificial seedling production.

Spawning-condition adults and fertilized eggs of Japanese eels were first collected from waters along the seamount chain near the Mariana Trench in 2008 and 2009 (Chow et al. 2009; Tsukamoto et al. 2011; Kurogi et al. 2011), additional eggs being collected a few years later (Aoyama et al. 2014). This spawning location discovery provided definitive evidence for a single spawning area for the species, otherwise occurring over a broad area of East Asia, including northern Luzon (Philippines), Taiwan, eastern China, Korea, and Japan. It was also confirmed that Japanese eels constitute a single panmictic population, as indicated by mitochondrial and microsatellite DNA studies (Ishikawa et al. 2001; Tseng et al. 2001; Han et al. 2010a, Minegishi et al. 2012; Gong et al. 2014). However, even though the geographically broad range is supported by a single spawning area well distant from juvenile growth areas, it is possible that some East Asian regions may be more important than others in contributing adult fish to the reproduction pool year by year. If so, intensive management and restoration activities targeting such juvenile growth areas would be the most effective means of working towards restoration of the species. However, to date nothing is known regarding which juvenile growth areas contribute adult fish to the spawning population.

Recent studies using pop-up archival tags on “silver eel” stage individuals have accumulated useful information on spawning migration routes and behaviors of several anguillid eel species (Jellyman and Tsukamoto 2002, 2005, 2010; Manabe et al. 2011; Aarestrup et al. 2009; Chow et al. 2015; Righton et al. 2016; Schabetsberger et al. 2015). Beguer-Pon et al. (2015) successfully tracked the movements of one maturing American eel, equipped with pop-up satellite archival tags, from the Scotian Shelf into the northern limit of the Sargasso Sea spawning area, although most other tracked eels have not reached close to their spawning areas. The aforementioned study demonstrated that rivers and/or estuaries around the Scotian Shelf represented a juvenile growth area of American eel that contributed to spawning area stock. Although Manabe et al. (2011) tracked “silver eel” stage A. japonica individuals released near Japan using pop-up tags, the eels neither reached the spawning area nor showed evidence of spawning related behaviors. A modelling simulation study by Chang et al. (2016) suggested that ocean circulation significantly affected the spawning migration route and duration of Japanese eels after their departure from the south coast of Japan.

Isotopic and elemental compositions of fish otoliths are also known to be useful as a natural fingerprint of historical environments in studies of movement ecology (Thorrold et al. 2001; Rooker et al. 2008, 2014; Walther et al. 2011; Walther and Limburg 2012; Molly et al. 2015). In particular, otolith strontium stable isotopic ratios (⁸⁷Sr/⁸⁶Sr ratio) of freshwater fishes have been clearly shown to indicate the water characteristics of habitats occupied by the fishes. Otolith ⁸⁷Sr/⁸⁶Sr ratios vary in direct proportion to the ratio of ambient water, which reflects the ratio of the watershed geology, such as age and composition of rock formations (Kennedy et al. 1997, 2000, 2002; Barnett-Johnson et al. 2005; Sano et al. 2008; Hobbs et al. 2010; Amakawa et al. 2012; Garcez et al. 2015). Therefore, a marked geological diversity across a study area, being reflected in otolith ⁸⁷Sr/⁸⁶Sr ratios of fishes distributed in the area, can be expected to vary significantly among habitat tributaries. Previously inhabited tributaries of each fish can be reconstructed from the otolith ⁸⁷Sr/⁸⁶Sr ratio and bedrock geology.

In the present study, we attempted to identify the juvenile growth areas of spawning-condition Japanese eels collected from the spawning area along the seamount chain of the West Mariana Ridge in 2008 and 2009, based on their otolith ⁸⁷Sr/⁸⁶Sr ratios. Thirty-three water samples from representative rivers within the distribution range of the species (six rivers in China, five in Korea, four in Taiwan, and 18 in Japan) were also used for ⁸⁷Sr/⁸⁶Sr ratio analysis, to provide insight into the underlying lithology of juvenile Japanese eel growth areas in combination with literature values. This should provide some initial information on the contribution of adult Japanese eels from East Asian regions to the spawning population and aid the establishment of more effective management and restoration strategies for this commercially important fish.

Materials and methods

Fish sample collection

Twelve spawning-condition adult A. japonica were collected from the spawning area during R/V Kaiyo Maru (Fisheries Agency, Japan) and Hokko Maru (Fisheries Agency, Japan) cruises conducted from May to August (2008) and in May and June (2009) (Chow et al. 2009; Tsukamoto et al. 2011; Kurogi et al. 2011), captured in a large midwater trawl net [maximum mouth opening 60 m wide and 50 m high, with 7 mm mesh cod end and a graded series of mesh sizes (60–2010 mm) in the main body of the net] towed along the southern part of the West Mariana Ridge. Collection details and biological data for each fish were given by Chow et al. (2009), Kurogi et al. (2011) and Tsukamoto et al. (2011). Juvenile stage (“yellow eel”) Japanese eels, known to reside not only in freshwater, but also in brackish estuarine and coastal marine habitats, can be divided into three categories based on their otolith Sr:Ca ratios according to their history of freshwater, estuarine and seawater habitat use (Tsukamoto et al. 1998; Tzeng et al. 2000; Tsukamoto and Arai 2001), viz “river” eels—individuals that entered and remained in freshwater river habitats after arrival of the glass eel stage in an estuary; “estuarine” eels—individuals inhabiting estuaries or moving between different habitats; and “sea” eels—individuals that at no time entered freshwater. The 12 spawning-condition adult eels comprised one “river” eel, six “estuarine” eels and five “sea” eels based on otolith Sr:Ca ratio analysis by Mochioka et al. (2010). Since the ⁸⁷Sr/⁸⁶Sr ratio of seawater is consistently 0.7092 (Goldstein and Jacobsen 1987; McArthur 1994), with the ratios of “sea” eel otoliths expected to be of similar value and unchangeable among different seawater habitats, four of the five “sea” eels were excluded from the otolith ⁸⁷Sr/⁸⁶Sr ratio analysis. Thus, seven of the 12 spawning-condition adult eels (one “river”, five “estuarine”, and one “sea” eel, Table 1) were used for the analysis in the present study.

Table 1 Sex and total length of spawning-condition adult eels, collection data and location, and otolith ⁸⁷Sr/⁸⁶Sr ratios

River water sample collection

River water samples were taken during 2008 and 2011 from 33 rivers—in mainland China (6), South-Korea (5), Taiwan (4) and Japan (18) (Fig. 1, Table 2), all known habitats of Japanese eel. One-liter water samples from the lowest freshwater reach of each river were filtered through a 0.45-µm membrane filter (ADVANTEC, Tokyo, Japan) soon after sampling, and then acidified (1%) using concentrated ultrapure HCl (Tamapure-AA-100, Tama Chemicals, Tokyo, Japan) and stored in acid-washed polypropylene bottles. All glass filtration materials and sampling bottles were acid-washed prior to use.

Fig. 1

Map of East Asia showing the rivers from which water samples were taken. River numbers correspond to those listed in Table 2. Bold gray coastlines indicate recruitment areas of Japanese eel

Table 2 ⁸⁷Sr/⁸⁶Sr ratios of water samples from Chinese, Korean, Taiwanese and Japanese rivers, including data from previous studies

⁸⁷Sr/⁸⁶Sr ratio analysis of otolith

Otoliths removed from each fish were embedded in epoxy resin (Epofix; Struers, Denmark), mounted on a glass slide, and ground using a grinding machine equipped with 70 μm and 13 μm diamond cup-wheels (Diskoplan-TS; Struers, Denmark), so as to expose the elver mark (a marked ring formed at the time of completion of metamorphosis from the leptocephalus to glass eel stage). A sample of otolith material for analysis was taken from outside a 150 μm radius from the otolith core using a micromilling technique using a MicroMill (New Wave Research Inc., USA) (Fig. 2). The otolith central portion (less than 150 μm from the core), which corresponded to the sea-going leptocephalus stage, had been previously removed by drilling to avoid contamination. Micromilled samples were not taken from the outermost portion of the otolith (corresponding to the oceanic migration period during the silver eel stage), the otolith portion representing that developmental period likely being narrow since no feeding (and hence no body growth) would have occurred during oceanic migration (Chow et al. 2010; Kurogi et al. 2011).

Fig. 2

Otolith section of a spawning-condition adult eel (no. U8-1) used for micromilling sampling and ⁸⁷Sr/⁸⁶Sr analysis. Solid and dashed circles indicate the portion sampled for analysis and the central portion drilled out so as to avoid contamination by the oceanic leptocephalus stage, respectively

Micromilling, chemical separation and thermal-ionization mass spectrometry (TIMS) for ⁸⁷Sr/⁸⁶Sr analysis were performed following Takahashi et al. (2006, 2009). Each otolith was placed on the stage of the micromilling machine, and a single drop of Milli-Q water put on the subsequently drilled sampling point. The diameter and depth of each drill hole were approximately 270 μm and 45 μm, respectively, two points sampled on each otolith (Fig. 2). The drilled sample slurry was then pipetted from the otolith surface and transferred to a cleaned PFA screw-cap vial. The PFA vial was heated to evaporate water, and 7 M HNO₃ (Tamapure-AA-100, Tama Chemicals, Tokyo, Japan) added to dissolve the otolith sample. Sr was subsequently extracted and purified from the resulting solution by ion chromatography using Sr Spec resin (Eichrom Technologies Inc., USA). ⁸⁷Sr/⁸⁶Sr analysis was conducted on a TIMS (TRITON TI, Thermo Finnegan, USA), installed at the Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Japan. Each ⁸⁷Sr/⁸⁶Sr ratio datum was normalized for isotopic fractionation using a correction value for ⁸⁸Sr/⁸⁶Sr of 8.375209. The NIST SRM 987 standard value of 0.710253 ± 0.000011 (2σ, n = 16) was corrected for instrumental drift and bias using a correction to the NIST SRM 987 standard of 0.710245 for each daily data set.

⁸⁷Sr/⁸⁶Sr ratio analysis of river water

From each water sample, 980 ml was evaporated in a Teflon bottle on a hot plate at 90 °C, and the residue then dissolved with 0.5 mL of 7 M HNO₃ (Tamapure-AA-100, Tama Chemicals, Tokyo, Japan). Chemical separation and mass spectrometry for Sr were performed using the same protocols as for the otolith samples. During water sample measurement, the NIST SRM 987 value was 0.710245 ± 0.000014 (2σ, n = 16).

Results

The otolith ⁸⁷Sr/⁸⁶Sr ratio of the “river” eel (no. E16-2) from the spawning area was 0.707793, those of five “estuarine” eels (no. E18-1, U8-1, M-1, EH13-1, M-3) ranging from 0.708580 to 0.709944 (mean ± SD: 0.709416 ± 0.000562) (Table 1, Fig. 3). The “sea” eel (no. U8-2) otolith showed a ratio of 0.709068, a little lower than the sea water ratio (0.7092, Goldstein and Jacobsen 1987; McArthur 1994). Table 2 shows water ⁸⁷Sr/⁸⁶Sr ratios of East Asian rivers, including ratios of 14 Japanese rivers given by Yamanaka et al. (2005), Amakawa et al. (2012) and Amano et al. (2013). Water ⁸⁷Sr/⁸⁶Sr ratios of rivers in China, Korea, and Taiwan ranged between 0.710432 and 0.714101 (mean ± SD: 0.711875 ± 0.000848), 0.713083–0.722798 (0.716990 ± 0.004290), and 0.711552–0.714691 (0.713191 ± 0.001425), respectively (Table 2). Whereas the aforementioned ratios were all > 0.71, 22 out of 32 Japanese rivers had ⁸⁷Sr/⁸⁶Sr ratios < 0.71, the overall range was between 0.705469 and 0.713091 (0.708449 ± 0.001999) (seven rivers in central Honshu Island, one in Shikoku Island, and two in Kyushu Island were characterized by ratios > 0.71).

Fig. 3

Plots of the ⁸⁷Sr/⁸⁶Sr values of water samples from four regions of East Asia and of reproductive stage Japanese eels Anguilla japonica caught within the spawning area along the West Mariana Ridge in the western North Pacific. Samples are ordered in the same direction (left to right) as in Tables 1 and 2 (top to bottom). Shading indicates the general range of the eel values for comparison with the water samples. Bold line indicates the ⁸⁷Sr/⁸⁶Sr value of seawater. Japanese rivers are shown by six regions [north–eastern region (open triangle), central region (dark gray triangle), and western region (gray triangle) of Honshu Island, Shikoku Island (dark gray triangle), and Kyushu Island (filled triangle)]. White (circle), gray (circle) and black (circle) circles indicate “river”, “estuarine”, and “sea” eels, respectively

Discussion

The geology of East Asia is characterized by a greater age of bedrock formation in the continental region; the Chinese mainland (including the Korean Peninsula) comprising Precambrian continental block older than the Pacific Ocean margin and oceanic plate subduction-related orogenic belt, including the Japan archipelago and Taiwan Island (Teraoka and Okumura 2003, 2011). Figure 4 shows the East Asian framework, including Japan, Taiwan, China and the Korean Peninsula. Bedrocks of the main landmasses of Japan are primarily composed of Paleozoic to modern (543 million years ago–present) sedimentary, metamorphic and igneous rocks (Wakita 2013), where Northeastern Japan is characterized by post-Miocene volcanic and sedimentary rocks mostly covering a Paleozoic–Mesozoic basement of metamorphic/igneous rocks. Southwestern Japan is further divided into inner and outer zones by the Median Tectonic Line running through Kii Peninsula and Shikoku Island. The distribution of bedrock parallels the elongated direction of the archipelagic arc, with younger rock trending to the outer zone (Pacific side). The inner zone is composed of Paleozoic–Mesozoic granitic intrusive rocks with minor sedimentary rocks, whereas the outer zone comprises sedimentary/metamorphic rocks of Mesozoic to Cenozoic age. Taiwan Island is characterized by three geological zones running approximately north–south: (1) Western foothills mostly comprising clastic rocks (Miocene–Quaternary), which originated from the Chinese mainland; (2) Central Range with clastic rocks (Eocene–Miocene) in the western region and metamorphic rock (Cretaceous) in the eastern region; and (3) Eastern Coastal Range, comprising post-Miocene clastic and volcanic rocks (Sibuet and Hsu 2004, Fig. 4). The Chinese mainland, as a whole, is covered by older bedrock (formed 2.4 billion–230 million years ago), primarily comprising three blocks: (1) Sino-Korean and Yangtze blocks, which are bordered by (2) the Qinling zone, running east–west in the central region; and (3) the Cathaysia block, expanding southeast of the Yangtze (Wang and Mo 1995; Zhao and Cawood 2012) (Fig. 4). The Sino-Korean block, including the middle-lower reaches of the Yellow River and North Korea, is composed of bedrocks dominated by Archean–early Proterozoic igneous and metamorphic rocks, and middle to later Proterozoic continental sedimentary rock. The Yangtze block, including the Yangtze valley and upper reaches, is composed of bedrocks dominated by Late Archean–Early Protrozoic igneous and metamorphic rocks, and Late Proterozoic–Triassic oceanic sedimentary rock. The Cathaysia block bedrock is dominated by Archean igneous and metamorphic rocks, and Proterozoic–Silurian sedimentary rock (Li et al. 2014). Bedrock of the Korean Peninsula is primarily composed of metamorphic rocks, dominated by Precambrian gneiss, with Cretaceous–Cainozoic sedimentary rocks covering the southernmost part of the peninsula (Lee 1987), which are an eastward extension of the Sino-Korean block and Qinling zone. Detailed geological maps of East Asia, including Japan, are provided by Geological Survey of Japan, Advanced Institute of Science and Technology (https://gbank.gs.jp/geonavi/?lang=en).

Fig. 4

Modified from Teraoka and Okumura (2003) and Li et al. (2014). NE Japan and SE Japan indicate Northeastern Japan and Southwestern Japan, respectively

Geological frameworks of Japan, Taiwan, China and the Korean Peninsula.

The ⁸⁷Sr/⁸⁶Sr ratios of water samples from rivers examined in both the present and previous studies seemed to reflect some of the geological characteristics of each region of East Asia, as described above (Table 2). All of the river water samples from the Chinese mainland and Korean peninsula presented relatively high values (> 0.71), clearly higher than samples from most Japanese rivers (exceptions being rivers situated in central Honshu Island, over dominated by old Mesozoic sedimentary rocks). Although Han et al. (2010b) reported that river water from the Wujiang River, a southern Yangtze River tributary, had a ⁸⁷Sr/⁸⁶Sr ratio less than 0.71 (0.7085), the present study indicated a ratio of 0.710432 for the lower river reach, almost consistent with the ratio of the Yangtze River mainstream (0.7098–0.7108) reported by Wang et al. (2007). Rivers along the western side of Taiwan, in which recruitment of Japanese eel was more abundant than on the eastern side of the island (Kuo 1971), showed ⁸⁷Sr/⁸⁶Sr ratios greater than 0.71, although the underlying geology was characterized by relatively new Miocene–Quaternary bedrock. However, Sano (2008) reported the chemical age of Monazites of the western foothills to be 230 million to 1850 million years, which is older than Japanese bedrock, by U–Pb and Pb–Pb aging methods.

The ⁸⁷Sr/⁸⁶Sr ratios of fish otoliths have been demonstrated as consistent with the ratio of ambient water in previous studies (Kennedy et al. 1997; 2000, 2002; Barnett-Johnson et al. 2005; Hobbs et al. 2010; Amakawa et al. 2012; Garcez et al. 2015). Therefore, ⁸⁷Sr/⁸⁶Sr ratios of the otolith portion formed during the juvenile growth stage of the spawning-condition adult eels (one “river” and five “estuarine” eels) collected from the spawning area in 2008 and 2009 could be proxies for the ratios of their habitat waters. Based on a comparison of the ⁸⁷Sr/⁸⁶Sr ratios of the water samples from the four East Asian countries, the otolith ratio of the “river” eel (no. E16-2) was suggestive of a region in Japan, the closest matches being with northern, central, and southern Japanese rivers. The source of the “estuarine” eels was more complex to interpret, estuarine water being a mixture of sea water and river freshwater flowing into the estuary, such that ⁸⁷Sr/⁸⁶Sr ratio reflects the mixing rate of freshwater and seawater (e.g. Hobbs et al. 2010; Walther and Limburg 2012). Thus, when the ⁸⁷Sr/⁸⁶Sr ratio of estuarine water (= the otolith ratio of an estuarine eel) is less than the seawater ratio of 0.7092 (Goldstein and Jacobsen 1987; McArthur 1994), that of the river water flowing into the estuary must be even lower. Conversely, the river water ratio must be higher than the actual estuarine water ratio when the latter is greater than 0.7092. This suggests that the ⁸⁷Sr/⁸⁶Sr ratios of the river which eel no. U8-1(“estuarine” eel) inhabited during the juvenile growth stage was even lower than the otolith ratios (0.708580), and such lower ratio was found only from Japanese rivers. The water ratios of rivers flowing into the estuarine habitats of eel numbers E18-1, M1, EH13-1 and M3 must have been higher than their respective otolith ratios (0.709404, 0.709231, 0.709928 and 0.709935). This indicates that those eels may have been from estuarine or coastal waters, depending on the percentage contribution of river freshwater to their otolith ratio values, although the possibility of their having come from Japan cannot be excluded. However, for them to have come from Korea or Taiwan requires them to have lived in high-salinity areas. The “sea” eel (no. U8-2) with the otolith ⁸⁷Sr/⁸⁶Sr ratio (0.709068) slightly lower than the sea water ratio may have also come from Japanese coastal waters, since the ⁸⁷Sr/⁸⁶Sr ratio of the latter appears to have been strongly affected by river freshwater with even lower ratios. Because at least two spawning-condition eels (no. E16-2 and U8-1), possibly in addition to the “sea” eel with the lower ⁸⁷Sr/⁸⁶Sr ratio (no. U8-2) spent their juvenile growth phase in Japan, rivers and estuaries in Japan may be highly important for reproduction and population stability of the species. It also indicates the significance of management and restoration of Japanese eels in Japan. Growth areas of the other eels that had otolith ⁸⁷Sr/⁸⁶Sr ratios of greater than 0.71 could not be determined here; further information, including otolith elemental and isotope compositions, is necessary. A. japonica has been recorded from the northeastern region of Luzon Island (Cagayan Estuary), Philippine (Tabeta et al. 1975). Basement of Cagayan basin is of Oligocene igneous and sedimentary rocks covered with fossiliferous limestone and shale (Suzuki 1989; Florendo 1994). Basement of Ilocos region (northwestern region of Luzon Island) including Cordillera-Central mountains is characterized by late Eocene sedimentary rocks. Granite from northern region of Luzon Island was radiometrically aged in Cretaceous to Paleocene. As such, northern region of Luzon Island is composed of young bedrock, suggesting that A. japonica from there may have low otolith ⁸⁷Sr/⁸⁶Sr ratio similar to those from Japan. However, population size of A. japonica in northern region of Luzon Island is quite small because A. japonica elvers occurred in limited months (January and February) in Cagayan Estuary with constitution of only 1–2% in sympatric eel elvers (A. marmorata and A. bicolor pacifica) (Tabeta et al. 1975). This suggests a low contribution of A. japonica inhabiting northern region of Luzon Island to reproductive population in the spawning area. The possibility that they were included in the spawning-condition adults examined in the present study seemed to be low.

The stock collapse of anguillid species in the Northern Hemisphere is thought to be caused at least in part, by various anthropogenic factors (Feunteun 2002; Tatsukawa 2003; Dekker 2003; Tsukamoto et al. 2009; Itakura et al. 2014, 2015; Yokouchi et al. 2008, 2014). Tatsukawa (2003) suggested dam construction as a major factor for the decline in Japanese eel distribution in Japan, as has occurred in other countries. Chen et al. (2014) also documented eel habitat loss in various areas in East Asia, which would have reduced the number of silver eels produced each year, and Itakura et al. (2014, 2015) presented data showing the negative effects of revetment shorelines in rivers on eel growth habitats. On the other hand, various attempts, such as (1) regulations of glass, yellow and silver eel fisheries, (2) management of migration obstacles (chemical or physical), in particular fish passes, and (3) restocking, have been conducted to manage and restore local stocks of Japanese eels, as has been done for European eel stocks (Moriarty and Dekker 1997; Knights and White 1998; Feunteun 2002; McCarthy et al. 2014; Brämick et al. 2016). Furthermore, monitoring of glass eel recruitment all year-round has been started on several rivers in each East Asian country (Japan, Taiwan, China and Korea) with an attempt to make those rivers sanctuaries or model rivers in near future (Kuroki et al. 2014). Because juvenile eels initially accumulate in upper estuaries and then disperse either in upstream or downstream as they grow (Kaifu et al. 2010), the growth condition in estuarine water just after recruitment appear to determine the direction of subsequent movement (Wakiya et al. 2016). It has been suggested that eels “evaluate” the alternatives of “downstream residency” or “upstream emigration” in accordance with the strategy most likely increasing individual fitness. Therefore, it is important to adequately manage the entire river system from the lower estuary to upper reaches, thus allowing eel movement in either direction (Wakiya et al. 2016). Furthermore, the demographic heterogeneity among the river systems supporting Japanese eels, pointed to the importance of conserving a variety of habitats in multiple river systems as an inclusive management target, in addition to restoration of habitat diversity of within single river systems (Yokouchi et al. 2008; 2014).

In the present study, two (“river” and “estuarine” eels) of seven spawning-condition adults collected from the spawning area near the Mariana Trench were suggested to have inhabited Japanese rivers and/or estuaries based on ⁸⁷Sr/⁸⁶Sr analyses of their otoliths and water samples from rivers of East Asian countries (China, Korea, Taiwan and Japan). This supports the likely significance of various management and restoration efforts for Japanese eel in Japanese archipelago.