Biological Aspects of Large Whitespotted Conger (Conger Myriaster) in the Akashi Strait, Eastern Seto Inland Sea, Japan

Total Page:16

File Type:pdf, Size:1020Kb

Biological Aspects of Large Whitespotted Conger (Conger Myriaster) in the Akashi Strait, Eastern Seto Inland Sea, Japan Aquaculture Sci. 60(3),341-348(2012) Biological Aspects of Large Whitespotted Conger (Conger myriaster) in the Akashi Strait, Eastern Seto Inland Sea, Japan 1, 2,* 2 Shigeaki GORIE and Kazuya NAGASAWA Abstract: This paper reports on various biological aspects of whitespotted conger (Conger myriaster) on the basis of a long-term pot survey conducted in the Akashi Strait from 1982 to 2009. The fish caught consisted of one or two major size groups, and large females (>500 mm total length) were predominant. Both the gonadosomatic index and condition factor of large females were higher in winter (January and February) than those in other seasons. Females appear to spend for up to four years in this strait and then begin a spawning migration by age-5 to other waters. While catch per unit effort (CPUE) in the pot survey showed considerably large annual and seasonal fluctuations, it was high from May to August and from November to January when bottom water temperature ranged from 10–25℃ but low from September to October (>25℃) and from February to April (<10℃). The Akashi Strait is likely to be an important habitat of large whitespot- ted conger for their early maturation. Key words: Conger myriaster; Length frequency distribution; Seto Inland Sea; Pot survey The whitespotted conger (Conger myriaster) This strait is small (only 4 km between the two is a benthic, commercially important marine fish islands) but has a strong tidal current (Kunishi and is usually caught by the small trawl fishery 1976), and the maximum water depth is about in the eastern Seto Inland Sea. They migrate 120 m (Kaseno 1976). While various fisheries to this region as leptocephali and recruit to the have been conducted there using different types fishery at about 250 mm in total length (TL) of fishing gear, such as small trawls, longlines, in October (Gorie and Ohtani 1998). The male- boat seines, gillnets, and angling, a pot fishery biased occurrence is known for young fish is not commonly operated because of the strong (<45 cm TL) (Takemori et al. 2004) and a sex- current (Uchihashi 1976). Furthermore, the pot biased migratory habit has been suggested fishery to catch whitespotted conger is strictly (Okamura et al. 2000). Large fish caught in this prohibited from December to May under the region are mostly females, some of which move Hyogo Prefectural Fishery Adjustment Rules from the Harima Nada Sea to both Osaka Bay outside the common fishery areas off Hyogo and the Kii Channel from January to August: Prefecture, and only a few fisheries cooperative this movement appears to be the onset of their associations are permitted to operate the fishery. spawning migration (Gorie et al. 2010). It is generally known that large whitespotted The Akashi Strait is part of the eastern Seto conger are commercially caught with longlines Inland Sea and located between Honshu (the in the Akashi Strait, but we have little informa- main island of Japan) and Awaji Island (Fig. 1). tion on them. As those large fish have been Received 2 December 2011; Accepted 12 March 2012. 1 Fisheries Technology Institute, Hyogo Prefectural Technology Center for Agriculture, Forestry and Fisheries, Akashi, Hyogo 674-0093, Japan. 2 Graduate School of Biosphere Science, Hiroshima University, Higashi-Hiroshima, Hiroshima 739-8528, Japan. *Corresponding author: Tel, (+81) 78-941-8601; Fax, (+81) 78-941-8604; E-mail, [email protected] (S. Gorie). 342 S. Gorie and K. Nagasawa thought to be a spawning stock (Gorie et al. 15.9 mm, respectively) (Nabeshima et al. 1995). 2010), it is important to collected their biologi- Sampling was done from evening to night. Deeply cal data for stock management and spawning frozen sardines were thawed, cut in pieces, and stock conservation. then put as bait in the pots. Pots were usually Since 1982, a monitoring survey of whites- put down to the sea before one hour of sunset potted conger has been conducted using pots and allowed the fish to trap for four hours. The in the Akashi Strait in order to clarify annual effective number of pots in each fishing survey changes in their length frequency distribution ranged from 60–110. The CPUE was expressed and catch per unit effort (CPUE). Although this as a number of the fish caught per pot for four survey must be operated during the neap tide, dipping hours. it can be done regardless of fishing grounds Oceanographic data, such as bottom water tem- and appears to be appropriate to examine the perature (WT), salinity, and depth, were taken with stock assessment in the Akashi Strait. In this STD ( JFE Advantech Co., Ltd., Nishinomiya, paper, biological aspects of whitespotted conger Japan) before fishing. caught through the pot survey are presented. Seasonal changes in gonadosomatic index, con- Fish examination dition factor, and age composition are also dis- The fish caught were transferred to the cussed on the assumption that large females in laboratory, where they were measured for total the eastern Seto Inland Sea including this strait length (TL, mm) and body weight (BW, g). In conduct a spawning migration. 1996 to 2009, they were sexed by the observation of the gonad (Gorie et al. 2004) and the gonad was Materials and Methods weighed (GW, g). For age determination, otoliths were removed, Fish collection cleaned, dried, and stored in small sealable plas- The study area is located in the western Akashi tic bags until otolith structure analysis. They were Strait (Fig. 1). Water depth of the survey area heated at 200℃ for several minutes on a hot ranged from 20–50 m. The bottom consisted of plate until the color turned light brown. Burnt gravel and cobbles. A fishing survey was con- otoliths were embedded in polyester resin ducted almost every month from 1982 to 1999 (Marumoto Struers K. K., Tokyo, Japan) and sec- and 2–5 times a year (usually twice: June and tioned into 0.3 mm thick intervals using a dia- November) from 2000 to 2009, using commer- mond saw (Leica SP1600; Leica Microsystems cially available pots (nominal mesh size, 18 setsu; GmbH, Wetzlar, Germany). Serial transverse sec- mesh size of the upper and bottom parts, 18 and tions were mounted on glass slides with sticky Fig. 1. The study area (hatched) for the pot survey in the Akashi Strait, eastern Seto Inland Sea, Japan. Conger myriaster in the Akashi Strait 343 wax (Maruto Instrument Co., Ltd., Tokyo, Japan). observation, sections were covered with clear Their surfaces were ground using abrasive- nail polish and then microscopically observed coated papers (Presi, Grenoble, France), etched under transmitted light or UV light (Katayama with 0.2N HCl for several tens of seconds. Before et al. 2002, 2010). Fig. 2. Monthly changes in length frequency distribution of whitespotted conger caught in the Akashi Strait based on the pot survey. Monthly data taken from 1982 to 2009 are combined. Vertical lines indicate 500 mm TL. Numerical values represent MTL±SD mm and percentage proportion of large fish (>500 mm TL). n, sample size. 344 S. Gorie and K. Nagasawa Since the spawning season was estimated to TL (MTL) gradually increased from winter be from August through February (Tanaka et (Jan.–Mar.) to fall (Oct.–Dec.) and showed al. 1987; Lee and Byun 1996; Mochioka 2001; over 500 mm MTL during summer (July–Sep.) Kurogi et al. 2002), age is chronologically and fall. The fall MTL value was the biggest expressed, assuming that the fish hatch every (Fig. 3). There was a significant difference in January. Gonadosomatic index (GSI) and condi- MTL between four seasons (ANOVA, P<0.001): tion factor (CF) were calculated as follows: GSI P-value between winter and spring (Apr.-June) (%)=GW・ BW –1 ・ 100 and CF= BW・ TL–3 ・ 106, was 0.023, and others were less than 0.001 respectively. In this paper, individuals of whites- (Tukey-Kramer test). potted conger are categorized into two groups: large fish (>500 mm TL) and small fish (≤500 mm Gonadosomatic index (GSI) TL). As stated above, the majority of the fish examined for sex were females. The overall GSI Statistical analysis ranged from 0.02–5.06 (mean=1.59, n=245) In this paper, results are presented as mean and 0.14–0.44 (0.25, 6) in females and males, and standard deviation (SD). Overall significant respectively. Also, GSI ranged from 0.18–5.06 differences in TL, GSI, and CF between four (1.65, 233) in large females, while it from 0.02 seasons were determined by one-way analysis –0.86 (0.46, 12) in small ones. In most of large of variance (ANOVA). If the one-way ANOVA females, GSI was less than 4, and mean monthly was significant, differences between each GSI values were 1.5 in April to December and season were estimated using Tukey-Kramer 2.7 in January to February (Fig. 4). Although method. The GSI of fish between the Akashi only a small number (n=4) of large females Strait and other region (Osaka Bay and the Kii were examined in February, their GSI values Channel combined) was examined by Mann- were clearly separated into two (high and low) Whitney’s U test. groups. In large females, there was a significant dif- Results ference in GSI between four seasons (ANOVA, P<0.001): GSI was the highest in winter (Jan.– Total length distribution Feb.) (Tukey-Kramer test, P<0.001), decreased A total of 14,370 whitespotted conger were markedly in spring (Apr.–June), but increased caught during this survey from 1982 to 2009, and 7,829 fish (54%) were larger than 500 mm TL. The overall TL and BW ranged from 217– 953 (mean=519, n=14,370) mm and from 12– 2,028 (283, 14,354) g.
Recommended publications
  • Akashi Kaikyo Suspension Bridge
    Held on (21 st Aug-27 th Aug ) 2011 Report on JSCE Study Tour Grant Sushma Chaudhary Representing Nepal Engineer’s Association (NEA) Department of Civil Engineering Nepal Engineering College Pokhara University Changunarayan V. D. C. – 9 Bhaktapur, Nepal 2011 Japan Society of Civil Engineers Study Tour Grant Report Sushma Chaudhary Representing Nepal Engineer’s Association (NEA) Department of Civil Engineering Nepal Engineering College, Pokhara University Changunarayan V.D.C.-9, Bhaktapur, Nepal 1. Introduction In commemoration of the 75 th Anniversary of the JSCE, a fund was established in the name of “International Scientific Exchange Fund” to promote international exchange and cooperation among the civil engineers from different part of the world. The study tour Grant is offered to undergraduate students who are enrolled in the civil engineering program and pursue a civil engineering career to provide them an opportunity to learn the latest civil engineering technologies and projects. The STG program covers the travel and other necessary expenses during the stay in Japan since 1992. I am second Nepalese to be chosen for this STG and it is a big honour for me. I am deeply thankful for this opportunity to Japan Society of Civil Engineers and Nepal Engineer’s Association. This report includes my day-to-day activities from the time I flew to Japan to the very last day of my stay. It also includes acknowledgment and conclusion at the end. The duration of the study tour was seven days starting from 21 st august to 27 th august 2011.The ISEF committee has designed a perfect study tour schedule considering our research interests.
    [Show full text]
  • Deep Groundwater Discharge and Ground Surface Phe- Nomena
    ῕῔ῒῑΐ Bull. Earthq. Res. Inst. Univ. Tokyo Vol. 2* ῍,**/῎ pp. +*/ῌ+-+ Deep Groundwater Discharge and Ground Surface Phe- nomena Tameshige Tsukuda+῎, *, Keinosuke Gotoh,῎ and Osamu Sato-῎ +῎ Earthquake Research Institute, University of Tokyo ,῎ Division of Environmental System Science, Department of Systems Science, Graduate School of Science and Technology, Nagasaki University -῎ Research Center for Hazards in Snowy Areas, Niigata Univerisityῐ Abstract Stress changes associated with crustal deformations may induce migration of fluid within the crust. It is hypothetically expected that a volume of pore water, being suddenly pressured in response to an elevated stress level in some seismogenic zone, will tend to intrude up into a crack network, and incidentally emerge at the ground surface. Groundwater changes in temperature and concentrations of chemical constituents should be observed at the spot where the upwelling fluid comes out. This paper reports the following . transient events recently found in Japan as evidence of the near surface discharge of hot and pressured water of a deep origin: +) Frequent rises in well water temperature were observed at Iwakuni,Yamaguchi Prefecture, southwest Japan. The largest rise occurred just before the ,**+ Geiyo earthquake of M 0.1, which indicated a possible precursor for the shock. A chemical analysis of ion concentrations of the hot water suggested that the temperature anomalies arise from contamination by intruding external deep water; ,) Gushing of groundwater at the sea bottom was considered to have occurred at the Akashi Strait , days before the +33/ Kobe earthquake of M 1.-, based on an interpretation of the appearance of brownish-black seawater found by the captain of a passenger boat; -) Upwelling of deep hot groundwater was occurred at Inagawa Town, Hyogo Prefecture, southwest Japan, which was associated with the +33/ Kobe earthquake.
    [Show full text]
  • Marist Brothers International School
    MARIST BROTHERS INTERNATIONAL SCHOOL Kobe, Japan HEAD OF SCHOOL Start Date: July 2022 marist.ac.jp MISSION Marist Brothers International School will make students our utmost priority and encourage them to achieve their full potential by fostering spiritual growth, appreciating cultural diversity, and developing a life-long love of learning. We will provide the opportunity for all stakeholders to develop a sense of community, spirit, and pride in our school. VISION We educate students in a nurturing environment based on Catholic values and the traditions of the Marist Brothers. We provide a rigorous program of study that prepares our students for higher education, internationally and in Japan. Our students gain knowledge, communicate effectively, develop good character, and become responsible citizens of a global society. OVERVIEW Marist Brothers International School (MBIS) is a private, college-preparatory school serving students from Pre-Kindergarten to Grade 12. A small but diverse school, MBIS enrolls approximately 340 students who collectively represent different cultural backgrounds. MBIS maintains a strong community that nurtures a family atmosphere, and encourages warm and respectful student-teacher relationships. MBIS faculty, staff, and families are joined by their commitment to support caring and capable students in every way possible. MBIS graduates are widely celebrated for their drive to be engaged global citizens and their belief in the power of cooperation; this is—in large part—due to the fact that MBIS strives to educate the whole child and sees strong academics as one piece of what makes a complete education. At this time, Marist Brothers International School seeks a new Head of School to assume the role in July 2022 as well as an Interim Head of School to begin July 2021.
    [Show full text]
  • Failure Knowledge Database / 100 Selected Cases 1 the Hanshin Awaji Great Earthquake (Hyogo Prefecture Southward Earthquake) [O
    Failure Knowledge Database / 100 Selected Cases The Hanshin Awaji Great Earthquake (Hyogo Prefecture Southward Earthquake) [On 17th January in 1995, Hanshin and Awaji district] Masahiko Kunishima, Mariko Abe(Note1) The earthquake, which hit the city early in the morning, brought about great damage such as the burning and collapse of buildings in the Hanshin and Awaji region. A large number of casualties occurred, and the city functions were paralyzed for a long time. In particular, a large number of casualties were caused by the collapse of houses. Furthermore, the fires that broke out just after the earthquake increased the magnitude of the disaster, which became the largest earthquake disaster in the postwar era. A great number of fundamental infrastructures, such as expressways, railways, harbors and lifelines, were damaged. 1. Event Early in the morning on 17th January 1995, a M7.3 earthquake whose hypocenter was below Akashi Channel occurred and brought great damage to the Hanshin Awaji district. Over 6,400 people died and over 41,500 people were injured, and the monetary amount of the damage is estimated to have been over 9.6 trillion yen. Especially, in the region that is called the "band of the earthquake disaster" (→Figure 1, 2) located on the alluvial plain of the base of Mt. Rokkosan where a seismic intensity of 7 was registered, many old wooden houses with tiled roofs fell down, and many people who were buried under the houses died. The bridge with single pillars of Hanshin Expressway collapsed over a length of 630m (→Figure 3), and the viaduct bridges made of RC rigid frame of the Shinkansen also collapsed (→Figure 4).
    [Show full text]
  • Effect of the Southern Hyogo Earthquake on the Akashi-Kaikyo Bridge
    IV/305 EFFECT OF THE SOUTHERN HYOGO EARTHQUAKE ON THE AKASHI-KAIKYO BRIDGE Seigo Nasu, Masaaki Tatsumi Honshu-Shikoku Bridge Authority, Tokyo, Japan 1. INTRODUCTION On January 17, 1995, a huge earthquake hit Kobe city and its neighboring cities as well as Awaji island in Hyogo prefecture. This earthquake which was officially named “Southern Hyogo Earthquake” caused a devastating damage including over 5,000 death and collapse of infrastructure. The epicenter was at the northern tip of Awaji island, close to the Akashi- Kaikyo Bridge. However, the bridge survived without any sever structural damage. This report describe an effect of the quake on the Akashi-Kaikyo Bridge based on a field survey and a basic structural study. 2. SUMMARY OF TOPOGRAPHY AND GEOLOGY OF THE AKASHI STRAIT The Akashi Strait extends in a northwest-to-southeasterly direction and is about 4 km wide. At the center of the strait, the topography consists of a 400 m wide seapotshaped valley with a water depth of 100 m, the two sides of which slope steeply. The geology comprises granite of the Mesozoic era as the bedrock. This is covered roughly with the Kobe stratum of the Mesozoic epoch of Neocene, the Akashi layer of the diluvial epoch of the Quaternary period, an upper diluvial formation, and an alluvial formation (Fig.1). Results of past sonic prospecting and borehole surveys indicate that east-west system faults centering on F1, F6, and F7 are crossed perpendicularly by a north- south system fault in this part of the strait (Fig.2). Since these faults were only observable below the Kobe layer and do not reach into the Quaternary formation, it was assumed that they had not slipped for at least for 2 million years which is the definition of a nonactive fault.
    [Show full text]
  • Progress in Seto Inland Sea Research
    Journal of Oceanography, Vol. 58, pp. 93 to 107, 2002 Review Progress in Seto Inland Sea Research HIDETAKA TAKEOKA* Center for Marine Environmental Studies, Ehime University, Bunkyo, Matsuyama 790-8577, Japan (Received 14 May 2001; in revised form 1 September 2001; accepted 5 September 2001) The Seto Inland Sea is a representative coastal sea in Japan with a complicated geom- Keywords: etry and thus a variety of marine environments. This sea is, at the same time, one of ⋅ Seto Inland Sea, the most industrialized areas in Japan, and its marine environment has been signifi- ⋅ anthropogenic cantly affected by the anthropogenic impacts over the last four decades. The wide impacts, ⋅ range of marine environments in this sea and the serious environmental issues result- heat bypass, ⋅ nutrient trap, ing from these impacts have attracted the attention of Japanese coastal oceanogra- ⋅ tide and tidal phers. It is believed that the nature and scope of these studies might be an example of current, the progress of Japanese coastal oceanography. The historical changes in the Seto ⋅ red tide, Inland Sea environment in the last four decades are briefly summarized, and the ⋅ oxygen-deficient progress in the studies of the Seto Inland Sea is reviewed with reference to historical water mass, changes. Some recent research topics and activities are also mentioned. ⋅ fronts. 1. Introduction studies might be a good example of the progress of Japa- The Seto Inland Sea in Japan is a semi-enclosed nese coastal oceanography. This paper therefore presents coastal sea surrounded by Honshu (the main island of a review of these studies.
    [Show full text]
  • 1995 Kobe Earthquake 10-Year Retrospective
    1995 Kobe Earthquake 10-year Retrospective TM Risk Management Solutions I NTRODUCTION A Mw6.9 (Ms7.3) earthquake struck central Honshu, Japan, shortly before dawn on January 17, 1995. The earthquake was centered at the northern end of Awaji Island, on a shallow strike-slip system known as the Nojima fault. The strongest ground motions were directed at the heavily urbanized flatlands that lie between Osaka Bay and the Rokko Mountains in the southern part of Hyogo Prefecture. All urban lifeline and transportation systems, including Japan’s high-speed Shinkansen (rapid rail) system pass through this densely developed strip. Known as the Hanshin region, the cities of Kobe (1.3 million people) and Osaka (2.6 million people) dominate both the region’s politics and economy. Figure 1: The Hanshin region is located in central Honshu and is Japan’s second largest regional economy 1 1995 Kobe Earthquake 10-year Retrospective Copyright 2005 Risk Management Solutions, Inc. All Rights Reserved. January 2005 E ARTHQUAKE C HARACTERISTICS At an estimated depth of 16 km (10 miles), the Nojima fault ruptured 40 km (25 miles) from the northern end of Awaji Island northeast through the city of Kobe. Nine km (6 miles) of surface fault rupture was observed on Awaji Island, with offsets of 1.2 to 1.5 meters (0.7 to 0.9 miles). This permanent land offset is well-preserved in the construction of the Akashi Kaikyo suspension bridge that spans the 4-km (2.5-mile) Akashi strait between Awaji Island and Kobe. Bridge construction was underway at the time of the earthquake.
    [Show full text]
  • CHAPTER 229 Environmental Assessment of Hypothetical Large-Scale Reclamation in Osaka Bay, Japan Keiji Nakatsuji , Toshiaki Suey
    CHAPTER 229 Environmental Assessment of Hypothetical Large-Scale Reclamation in Osaka Bay, Japan Keiji Nakatsuji , Toshiaki Sueyoshi , Kohji Muraoka ABSTRACT In urban coastal areas in Japan, large-scale reclama- tion projects have recently increased, which have caused drastic changes in topographical features of the coast- line. In Osaka Bay, the sea area of 5,200 ha have been reclaimed in the past 40 years and many development projects are under construction. As a natural consequ- ence, the sea water has been polluted due to poor exchange of water with outer oceans and the load of nutritious substances discharged from rivers; hence, algal blooms occur independent of season and anoxia appears near the sea especially in summer. A 3-D baroclinic flow model is proposed to predict the tidally-interacting estuarine circulation and residual baroclinic currents in Osaka Bay and to evaluate the effects of hypothetical large-scale reclamation on the estuarine system. INTRODUCTION Osaka Bay is one of semi-enclosed urban coastal seas in Japan. High density populated and industrialized cities such as Osaka and Kobe are located at the head of Osaka Bay. The GNP (Gross National Product) of Osaka Prefec- ture approximately corresponds to that of Australia, in addition, the total amount of GNP of Osaka, Kobe and Kyoto does to that of Canada. Area of Osaka Bay is only 1400 km and its mean depth is 28 m. In the past 40 years the coastal area of 5,200 ha have been reclaimed for satisfy- ing the economical and industrial demand, and lots of development projects are under construction including a 511 ha for newly-built Kansai International Airport Island.
    [Show full text]
  • Movement and Growth of Whitespotted Conger Conger Myriaster in the Eastern Seto Inland Sea, Japan
    Aquaculture Sci. 58(2),233-242(2010) Movement and Growth of Whitespotted Conger Conger myriaster in the Eastern Seto Inland Sea, Japan 1, 2, * 1 2 Shigeaki GORIE , Minoru TANDA and Kazuya NAGASAWA Abstract: We conducted a tagging survey to study the movement and growth of whitespotted conger Conger myriaster in the eastern Seto Inland Sea and found that the fish moved to Osaka Bay and the coastal waters of the Kii Channel from the northeastern Harima Nada Sea, the release site, through the Akashi Strait from January to August. Total length and gonadsomatic index of females recaptured in the Osaka Bay-Kii Channel waters were larger and higher, respectively, than those in the Harima Nada Sea-Akashi Strait waters, suggesting that the fish conducted a pre-spawning migration. The fish were recaptured up to 420 days after release and exhibited various growth rates ranging from 0.1 to 2 mm day-1. There was no particular trend in age of recaptured females although the age ranged from 1+ to 3+. Not all the released fish passed through the Akashi Strait, nor they did always move to Osaka Bay even when they were at liberty for a long period. Some large-sized fish remained in the Akashi Strait. These results suggest that there are two types of groups (a locally resident group and a migratory group) and that whitespotted conger have a com- plicated migratory behavior. Key words: Conger myriaster; Tag and release; Growth; Spawning migration The whitespotted conger Conger myriaster target fish species. inhabits inshore waters off Japan, Korea and Whitespotted conger occur as leptocephali China (Asano 1984).
    [Show full text]
  • Awaji Island Twelve Walking Courses, from Short and Easy to Long Full-Day Treks, Featuring Many Top Attractions on Walking/ Awaji Island! Trekking Course Guide
    AWAJI SUMOTO MINAMIAWAJI Awaji Island Twelve walking courses, from short and easy to long full-day treks, featuring many top attractions on Walking/ Awaji Island! Trekking Course Guide Enjoy the best of Awaji Island — Town or mountains, walking or hiking! N To Akashi Port To Akashi↑ Kobe Awaji Jenova Line (13 min.) Awaji-shiP. 4-5 (Pearl Bridge) Awaji Island Akashi Kaikyō Bridge Panoramic fields of flowers overlooking the sea are a sight to behold! Course 1 ∴ Matsuhonoura Bay Course 1 Michi-no-Eki Hanasajiki Park/ Course 2 31 Awaji Walking/ Akashi Kaikyō Bridge Long Course Iwaya Port Distance : About 27 km Time required : About 7 hours Awaji-Kita Smart IC (For entrance only) Awaji IC/SA Road and trail, plus the Akashi Kaikyo- Bridge! Trekking Course 2 Awaji Hanasajiki(P. 4~5) 28 Ishinoneya Green Park/ Akashi Kaikyō Bridge Short Course Course Distance : About 8 km Time required : About 2 hours Higashiura IC Michi-no-Eki P. 6-7 31 71 Higashiura A peaceful course that gives you a feel for history Terminal Park Guide Course 3 Course 3 Gossa Kaito Site/Nomad Mura Long Course Murozu PA Distance : About 19km Time required : About 5 hours Hokudan IC Course 4 Hit two major power spots! Awaji Ishinoneya Green Park( P. 4~5) Gossa Kaito Higashiura 12 recommended Course 4 Site Bus Terminal Izanagi Jingu Shrine/ Parchez Kaori no Yakata courses highlight the Iwagami Jinja Shrine Short Course Kaori no Yu 28 Distance : About 10 km Time required : About 3 hours best of Awaji Island! Awaji-shi 31 Izanagi Jingu Course Difficulty Level Sumoto-shiP.
    [Show full text]
  • Co-Seismic Displacements of the 1995 Hyogo-Ken Nanbu Earthquake Manabu Hashimoto,* Takeshi Sagiya, Hiromichi Tsuji, Yuki Hatanak
    J. Phys. Earth, 44, 255-279, 1996 Co-seismic Displacements of the 1995 Hyogo-ken Nanbu Earthquake Manabu Hashimoto,* Takeshi Sagiya, Hiromichi Tsuji, Yuki Hatanaka, and Takashi Tada GeographicalSurvey Institute, Tsukuba 305, Japan We presentco-seismic displacements of the Hyogo-kenNanbu earthquake of January 17, 1995,detected by continuousGPS (Global Positioning System) observation, campaign type GPS survey and leveling. Continuous GPS observationgives a consistentpattern of displacementswith thoseexpected from a right lateralslip on a NE-SWtrending vertical fault in far field:stations about 50km east and west of the epicentermoved toward the epicenterby about4 cm,while stations north and south movedaway from the epicenter.By comparing with line lengthsobtained by geodoliteabout 10 yearsago, the campaigntype GPS revealed most controlpoints on AwajiIsland moved to the southwestor south,which may be attributedto the movementof the NojimaFault whichcut the surface.On the other hand, controlpoints northwest of the Rokkofault systemmoved toward the northeastand thoseon theother side moved slightly to the west,in and aroundKobe. Leveling data revealed upliftof 19cm on the northwesternside of theSuma Fault, a memberof the Rokko faultsystem, and subsidence of 7 cmjust east of this fault. Furthermore,uplift of about 5 cmwas observedin the centralpart of Kobe City, and subsidenceof 5 cm was detectedeast of Kobe. There is no significantgap in horizontaland vertical displacementsaround the northernextension of the NojimaFault, which implies a complicatedrupture process of this event.Leveling on the east coastof AwajiIsland revealed a significantuplift of about 20 cm with slight subsidenceat both edgesof this upliftregion during the past 20 years. By fittingthe abovegeodetic data, we searchedfor an optimalset of parametersof a dislocationmodel.
    [Show full text]
  • Eutrophication and Occurrences of Harmful Algal Blooms in the Seto Inland Sea, Japan
    Plankton Benthos Res 1(2): 71–84, 2006 Plankton & Benthos Research © The Plankton Society of Japan and The Japanese Association of Benthology Eutrophication and occurrences of harmful algal blooms in the Seto Inland Sea, Japan ICHIRO IMAI1*, MINEO YAMAGUCHI2 & YUTAKA HORI3 1 Laboratory of Conservation of Coastal Ecosystems, Graduate School of Global Environmental Studies (concurrent with Laboratory of Marine Environmental Microbiology, Division of Applied Biosciences, Graduate School of Agriculture) Kyoto University, Kyoto 606–8502, Japan 2 Red Tide Research Division, National Research Institute of Fisheries and Environments of Inland Sea, Maruishi, Hatsukaichi, Hiroshima 739–0452, Japan 3 Fisheries Technology Institute, Hyogo Prefectural Technology Center for Agriculture, Forestry and Fisheries, Futami, Akashi, Hyogo 674–0093, Japan Received 28 February 2006; Accepted 10 April 2006 Abstract: The Seto Inland Sea is the largest enclosed coastal sea in Japan and is also a major fishing ground includ- ing aquacultures of fish, bivalves and seaweeds. The incidents of red tides dramatically increased in frequency and scale in the Seto Inland Sea along with serious eutrophication in the 1960s and 1970s. The maximum incident of 299 was recorded in 1976, but the incident has since shown a clear decreasing trend, reaching about 100 per year in the late 1980s by virtue of regulation by law, and this level has been maintained thereafter with the level of nutrients supporting red tide occurrences. The “Law Concerning Special Measures for Conservation of the Environment of the Seto Inland Sea” was legislated in 1973 and industrial loading was decreased to half the level of 1972. The important red tide or- ganisms causing huge fishery damages by fish-kill are Chattonella antiqua, C.
    [Show full text]