Movement and Growth of Whitespotted Conger Conger Myriaster in the Eastern Seto Inland Sea, Japan
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Intrinsic Vulnerability in the Global Fish Catch
The following appendix accompanies the article Intrinsic vulnerability in the global fish catch William W. L. Cheung1,*, Reg Watson1, Telmo Morato1,2, Tony J. Pitcher1, Daniel Pauly1 1Fisheries Centre, The University of British Columbia, Aquatic Ecosystems Research Laboratory (AERL), 2202 Main Mall, Vancouver, British Columbia V6T 1Z4, Canada 2Departamento de Oceanografia e Pescas, Universidade dos Açores, 9901-862 Horta, Portugal *Email: [email protected] Marine Ecology Progress Series 333:1–12 (2007) Appendix 1. Intrinsic vulnerability index of fish taxa represented in the global catch, based on the Sea Around Us database (www.seaaroundus.org) Taxonomic Intrinsic level Taxon Common name vulnerability Family Pristidae Sawfishes 88 Squatinidae Angel sharks 80 Anarhichadidae Wolffishes 78 Carcharhinidae Requiem sharks 77 Sphyrnidae Hammerhead, bonnethead, scoophead shark 77 Macrouridae Grenadiers or rattails 75 Rajidae Skates 72 Alepocephalidae Slickheads 71 Lophiidae Goosefishes 70 Torpedinidae Electric rays 68 Belonidae Needlefishes 67 Emmelichthyidae Rovers 66 Nototheniidae Cod icefishes 65 Ophidiidae Cusk-eels 65 Trachichthyidae Slimeheads 64 Channichthyidae Crocodile icefishes 63 Myliobatidae Eagle and manta rays 63 Squalidae Dogfish sharks 62 Congridae Conger and garden eels 60 Serranidae Sea basses: groupers and fairy basslets 60 Exocoetidae Flyingfishes 59 Malacanthidae Tilefishes 58 Scorpaenidae Scorpionfishes or rockfishes 58 Polynemidae Threadfins 56 Triakidae Houndsharks 56 Istiophoridae Billfishes 55 Petromyzontidae -
Marine Ecology Progress Series 530:223
The following supplement accompanies the article Economic incentives and overfishing: a bioeconomic vulnerability index William W. L. Cheung*, U. Rashid Sumaila *Corresponding author: [email protected] Marine Ecology Progress Series 530: 223–232 (2015) Supplement Table S1. Country level discount rate used in the analysis Country/Territory Discount rate (%) Albania 13.4 Algeria 8.0 Amer Samoa 11.9 Andaman Is 10.0 Angola 35.0 Anguilla 10.0 Antigua Barb 10.9 Argentina 8.6 Aruba 11.3 Ascension Is 10.0 Australia 6.5 Azores Is 7.0 Bahamas 5.3 Bahrain 8.1 Baker Howland Is 7.0 Bangladesh 15.1 Barbados 9.7 Belgium 3.8 Belize 14.3 Benin 10.0 Bermuda 7.0 Bosnia Herzg 10.0 Bouvet Is 7.0 Br Ind Oc Tr 7.0 Br Virgin Is 10.0 Brazil 50.0 Brunei Darsm 10.0 Country/Territory Discount rate (%) Bulgaria 9.2 Cambodia 16.9 Cameroon 16.0 Canada 8.0 Canary Is 7.0 Cape Verde 12.3 Cayman Is 7.0 Channel Is 7.0 Chile 7.8 China Main 5.9 Christmas I. 10.0 Clipperton Is 7.0 Cocos Is 10.0 Colombia 14.3 Comoros 10.8 Congo Dem Rep 16.0 Congo Rep 16.0 Cook Is. 10.0 Costa Rica 19.9 Cote d'Ivoire 10.0 Croatia 10.0 Crozet Is 7.0 Cuba 10.0 Cyprus 6.8 Denmark 7.0 Desventuradas Is 10.0 Djibouti 11.2 Dominica 9.5 Dominican Rp 19.8 East Timor 10.0 Easter Is 10.0 Ecuador 9.4 Egypt 12.8 El Salvador 10.0 Eq Guinea 16.0 Eritrea 10.0 Estonia 10.0 Faeroe Is 7.0 Falkland Is 7.0 Fiji 6.2 Finland 7.0 Fr Guiana 10.0 Fr Moz Ch Is 10.0 Country/Territory Discount rate (%) Fr Polynesia 10.0 France 4.0 Gabon 16.0 Galapagos Is 10.0 Gambia 30.9 Gaza Strip 10.0 Georgia 20.3 Germany (Baltic) 7.0 Germany (North Sea) 7.0 Ghana 10.0 Gibraltar 7.0 Greece 7.0 Greenland 7.0 Grenada 9.9 Guadeloupe 10.0 Guam 7.0 Guatemala 12.9 Guinea 10.0 GuineaBissau 10.0 Guyana 14.6 Haiti 43.8 Heard Is 7.0 Honduras 17.6 Hong Kong 7.4 Iceland 17.3 India 11.7 Indonesia 16.0 Iran 15.0 Iraq 14.1 Ireland 2.7 Isle of Man 7.0 Israel 6.9 Italy 5.8 Jamaica 17.5 Jan Mayen 7.0 Japan (Pacific Coast) 10.0 Japan (Sea of Japan) 10.0 Jarvis Is 10.0 Johnston I. -
Discovery of a Spawning Area of the Common Japanese Conger Conger Myriaster Along the Kyushu-Palau Ridge in the Western North Pacific
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Springer - Publisher Connector Fish Sci (2012) 78:525–532 DOI 10.1007/s12562-012-0468-6 ORIGINAL ARTICLE Biology Discovery of a spawning area of the common Japanese conger Conger myriaster along the Kyushu-Palau Ridge in the western North Pacific Hiroaki Kurogi • Noritaka Mochioka • Makoto Okazaki • Masanori Takahashi • Michael J. Miller • Katsumi Tsukamoto • Daisuke Ambe • Satoshi Katayama • Seinen Chow Received: 21 November 2011 / Accepted: 4 January 2012 / Published online: 23 February 2012 Ó The Author(s) 2012. This article is published with open access at Springerlink.com Abstract The common Japanese conger Conger myrias- larvae (preleptocephali) 5.8 and 7.8 mm in total length ter is an important commercial coastal fisheries species in (TL), which were caught at 17°N. The 5.8 mm TL larva East Asia, but its spawning area has not been determined. was estimated to be 3–4 days after hatching, the youngest A larval sampling survey was conducted in September preleptocephalus (i.e., the earliest stage) of this species 2008 along 136°E between 13°N and 22°N, which roughly ever collected. Eighteen other leptocephali were caught at followed the Kyushu-Palau Ridge in the western North 18°N and 21°N, and these ranged from 18.6 to 40.0 mm Pacific. Twenty larval specimens were confirmed to be TL. Based on these collections, we discerned that there is a C. myriaster using DNA analysis. Two were newly hatched spawning area of C. myriaster in the area along the Kyu- shu-Palau Ridge approximately 380 km south of Okino- torishima Island. -
Supplementary Information Doi: 10.1038/Nclimate1691
SUPPLEMENTARY INFORMATION DOI: 10.1038/NCLIMATE1691 Shrinking of fishes exacerbates impacts of global ocean changes on marine ecosystems Supplementary information Method Dynamic Bioclimate Envelope Model (DBEM) As a first step, we predicted the current (19702000) distribution map of each species an algorithm described in [1,2]. This algorithm estimates the relative abundance of a species on a 30’ latitude x 30’ longitude grid of the world ocean. Input parameters for DBEM include the species’ maximum and minimum depth limits, northern and southern latitudinal range limits, an index of association to major habitat types (seamounts, estuaries, inshore, offshore, continental shelf, continental slope and the abyssal) and known occurrence boundaries. The parameter values of each species, which are posted on the Sea Around Us Project website (http://www.seaaroundus.org/distribution/search.aspx), were derived from data in online databases, mainly FishBase (www.fishbase.org). Jones et al. 3 compared the predicted species distribution from this algorithm with empirically observed occurrence records and found that the algorithm has high predictive power, and that its skills are comparable with other commonly used species distribution modelling approach for marine species such as Maxent4 and Aquamap5. As a second step, we used DBEM to identify the ‘environmental preference profiles’ of the studied species, defined by outputs from the Earth System Models, including sea water temperature (bottom and surface), depth, salinity, distance from seaice and habitat types. Preference profiles are defined as the suitability of each of these environmental conditions to each species, with suitability calculated by overlaying environmental data (19702000) with maps of relative abundance of the species 6. -
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. -
Research Report on China's Trash Fish Fisheries Greenpeace East-Asia 2017
Research report on China’s trash fish fisheries Greenpeace East-Asia 2017 Definition: Trash fish: in this study, trash fish refers to those leftovers on the port, which are usually mixture of poorly preserved, small sized and low commercial valued species of fishes and invertebrates. Not directly consumed by human, trash fish are mainly used as feeds (mainly as fish feeds and also as feeds for other types of animals). Trash fish normally contains groups of species as following: ● Commercial species: comparatively high in commercial value, with larger production volume o Edible commercial species : fish and invertebrate species that could be consumed directly by humans if they were allowed to grow larger to mature or beyond mature body sizes o Non-edible commercial species: species that would not be consumed directly by humans even if they did grow to meet mature standard. Instead they are of value for processing into fish meal, fish oil and other non-food products ● Non-commercial species: low in commercial value, no scalable production volume In this research we mainly analyzed the fish samples based on the categorization above. Each fish individual can be divided into either mature or immature (=juvenile) stages : ● Juvenile fish: individuals which have not yet attained sexual maturation ● Adult fish: individuals with reproductive capability 1 Preface The 21st Century has brought with it a major challenge for mankind; one that has yet to be met. For the first time in our history we have entered a crisis of seafood supply. Our growing human populations and burgeoning demand for nutritious and plentiful seafood has exceeded what wild nature can supply in perpetuity. -
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. -
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. -
Histological and Scanning Electron Microscopic Examination of The
etics & E en vo g lu t lo i y o h n a P r f y Journal of Phylogenetics & Takiue and Akiyoshi, J Phylogen Evolution Biol 2014, 2:1 o B l i a o n l r o DOI: 10.4172/2329-9002.1000125 u g o y J Evolutionary Biology ISSN: 2329-9002 Research Article Open Access Histological and Scanning Electron Microscopic Examination of the Digestive Tract in Whitespotted Conger, Conger Myriaster (Anguilliformes) Shunpei Takiue¹,² and Hideo Akiyoshi¹* ¹Department of Biological Science, Faculty of Life and Environmental Science, Shimane University, 1060 Nishikawatsu, Matsue 690-8504, Japan ²The United Graduate School of Agricultural Sciences, Tottori University, 4-101 Koyama-Minami, Tottori 680-8553, Japan Abstract The morphology of the digestive tract of Whitespotted conger, Conger myriaster (Elopomorpha: Anguilliformes) was examined by light and scanning electron microscopy. The digestive tracts consist of esophagus, stomach, and intestine; no pyloric caeca were observed. The stomach was divided into cardiac, body, terminal and pyloric region. The esophagus was composed of two layers of striated muscularis; inner longitudinal layer and outer circular layer. The former was extended to the body region of the stomach. In contrast, the latter was terminated to the esophagus, and became coincident to the boundary of the outer longitudinal layer consisting of smooth muscle in the cardiac region of the stomach. The terminal region of the stomach was characterized by the thick longitudinal muscularis and subserosa, and the gastric glands were absent. Ciliated cells were distributed in the intestinal wall. The digestive tract secreted both acidic and neutral mucus throughout all regions. -
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. -
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). -
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.