160° ~g=r v^ I— I I — t i=r 15«' k-J i-ui u-i L— I I— I i—i 140° 130* 120 Ftyolc£>n I •<*CProf Walfs ALASKA I— I' i-*i ^ (INTERNATIONAL NORTH PACIFIC fJSHERIEf' COMMISSIONS^ • 1)«W»<7J> N MEETING ' UhMtED STATES DEPARTMENT OF THE INTERIOR FISH AND WILDLIFE SERVICE BUREAU OF COMMERCIAL FISHERIES WASHINGTON, D. C. S /. A jv n CIRCULAR 85 UNITED STATES DEPARTMENT OF THE INTERIOR Fred A. Seaton, Secretary FISH AND WILDLIFE SERVICE Amie J. Suomela, Commissioner BUREAU OF COMMERCIAL FISHERIES Donald L. McKeman, Director INTERNATIONAL NORTH PACIFIC FISHERIES COMMISSION UNITED STATES SECTION MEETING, MARCH I960 PAPERS Presented before a Joint Session of the Alaska Legislature Juneau, Alaska March 4, I960 Circular 85 Washington, D. C. May I960 UNITED STATES SECTION INTERNATIONAL NORTH PACIFIC FISHERIES COMMISSION Commissioners Milton E, Brooding, Chairnaan Edward W. Allen John H, Clawson Arnie J. Suomela Advisors Clinton E. Atkinson Stuart Blow Fred C. Cleaver Reynold A. Fredin John T. Gharrett George Y. Harry William C. Herrington Walter Kirkness Donald P. Loker J. L. McHugh Donald L. McKernan William F. Royce Williann Smoker William M. Terry Wo F. Thompson W, G. Van Campen Advisory Committee C. Lj, Anderson W. C. Arnold Harold F. Cary Richard S. Croker Albert M. Day Haakon Friele DeWitt Gilbert Milton C. James George Johansen Robert C. Kallenberg Harold E. Lokken Milo Moore Alfred Owen T. F. Sandoz John W. Smith Peter Tanstad Lowell Wakefield James Waugh 11 CONTENTS Page The International North Pacific Fisheries Commission and its work 1 Statement of the United States Section, International North Pacific Fisheries Commission, by Milton E. Brooding, Chairman 3 Scientific research by the United States, by J, L. McHugh 11 Research related to the case for abstention, by R. A, Fredin • 13 Distribution and racial composition of salmon on the high seas, by Clinton E, Atkinson 19 Pacific salmon in international waters, by Allan C. Hartt (presented by William F. Royce) •>•• 25 111 % fS -. r^ % V? f "o;?.' AIIIO 1. . r^ V f\ ^ .' ^ > [ Pr( vison ol Ltn t \ 1 1 1 1 1 1 1 1 Figure l.--North Pacific Ocean and Bering Sea, showing position of Provisional Abstention Line. 18 At the time the treaty was signed, almost no information was available on distribution of Asian or North American salmon on the high seas. It is true that the Japanese in the 1930*s had vmdertaken a detailed survey of the Bering Sea west of 180°, but the main purpose of their survey was to determine where Scdmon were most abundant for purposes of establishing a commercial fishery, and no attention was given to whether the fish taken were of Asian or North American origin. The limited research of the United States in 1937 and 1938 in eastern Bering Sea indicated that salmon were probably confined to the continental shelf. After entry into force of the Treaty on June 12, 1953, the Commission was organized in February of 1954 and its pro- gram of research was approved in the fall of that same year. The first explorations to determine distribution of salmon were made in the spring of 1955 when the U. S. Fish and Wildlife Service vessel John N. Cobb was sent out along the west coast of North America, across the Gulf of Alaska, and along the Alaskan Peninsula. Wherever the Cobb set its nets, salmon were taken. Based upon this information, two halibut schooners were chartered in July 1955 to investigate the critical waters between 175° E. and 165° W, lying on both sides of the pro- visional line. Again, they took salmon all along the Aleutian Islands north of about 48° N, But when the boats passed into more southern waters, salmon disappeared from their catches and instead, quantities of edbacore were taken. It was now obvious that two separate environments had been found. This was most important to us because it meant that we had found the southern range of salmon distribution (fig. 2), 170» 180 40° I30» Figure 2.- -North Pacific Ocean and Bering Sea showing area inhabited by salmon in May - June. 19 However, further evidence was required on distribution of salmon in spring (winter in the sea) when the colder water of the North Pacific extends as far south as about 40° N. Arrangements, therefore, were made for vessels from the laboratory of the Bureau of Commercial Fisheries at Hono- lulu to extend their spring cruise for tuna into waters north of 40° N. and, as predicted, salmon were found in these waters. It was evident that the distribution of salmon was intimately associated with conditions in the ocean, varying from season to season and, of course, from year to year. Coupled with this knowledge of the southern limit of sal- mon distribution, subsequent studies have shown that the northern limit lies at a temperature of about 3° C, and here again the temperature pattern varies markedly between seasons and years. Yearly changes in abundance of salmon have be en followed closely since 1955 by fishing the sajiae stations on the high seas. In this work we discovered that the numbers, kinds, and sizes of salmon on the high seas vary from time to time and place to place. For example, we have found the ocean near the central Aleutian area to be heavily poptilated with pink salmon {Oncorhynchus gorbuscha) during odd-numbered years, and we have found that these are Asian fish. In marked contrast, very few pink salmon are present in the even- numbered years, and these fish are predominantly of North American origin. Pink salmon invariably return to spawn at the end of their second year of life, hence these patterns are not surprising. The distribution of salmon within this area varies as the season progresses. In 1959 pink salmon were first observed in large numbers about 200 miles south of the Aleutian chain. As the summer progressed, pink salmon became more and more abundant near and north of the Aleutian chain in the Bering Sea, but by mid-Jxily they co\ild be found only in the westernmost part of the ocean, near the Asian continent. Similar changes have been foundfor red salmon (0. nerka). In May and Jxine of 1959, the central area just north of the Aleutians was heavily populated with adult red salmon almost certainly of Bristol Bay origin, and red salmon remained abundant here until about the end of June, In July, the larger, more mature red salmon became scarce but we began to catch large numbers of immature red salmon. In 1959 these immature red salmon were about 10 times more abundant than in previous years and were certainly part of the very large outmigration of small fish from Bristol Bay in 1958. These initial explorations were sufficient to give us an answer to the first question posed by the Protocol, that is, did Asian and North American salmon intermingle on the hign seas? There is no question but that large numbers of salmon from Asia and North America intermingle in the mid- Pacific and the Bering Sea. We also found that the amount of mixing and the actual distribution of the salmon was related to the abundance of fish from certain mainland 20 rearing areas and to the configuration of the hydrography of the sea. Our next problem was to define this area of mixing for the three important species of salmon: red, pink and chum {0. keta) salmon. Tagging experiments provided the best way to define these areas, and such investigations were arranged by contract with the Fisheries Research Institute of the University of Washington, Finally, to answer the problem set forth in the Protocol, we must know not only where salmon are, but also the rela- tive abundance of North American salmon at any point on the high seas. The answer to this question required the develop- ment of new methods for identifying Asian and North Ameri- can fish. In effect, we must examine a salmon, and by certain differences, such as variations in size, shape, or numbers of parts in various sections of the body, be able to say that this fish is from Asia or from North America, Three suc- cessfxil methods for identifying stocks of salmon are now being used. These areas of the North Pacific Ocean mentioned above were all fished by our research vessels for the purpose of securing samples to determine where fish in the high seas originated. In studying these fish samples, examination of the structure of scales of individual fish was the first approach followed. It has been found that salmon tend to deposit rings (or circvili) on their scales in patterns charac- teristic for each area, A careful study of these characters of red salmon scales demonstrated by 1957 that Bristol Bay red salmon were fovind far to the west in the central Pacific, Subsequently, we have devised means of making quantitative separations into continent of origin of scale ssmnples taken on the high seas. Similarly, we have experienced considerable success in the study of the coxints of body structures of salmon. This different approach makes use of variations in the number of scales on the fish, bones in the backbone, bones in the gill arches, and fin rays, as well as a number of other readily- examined portions of the fish which tend to show differences. This method has been particularly useful to us in developing quantitative separation of red salmon on the high seas. We have been able to determine with reasonable precision what portion of the salmon in a sample taken in the middle of the ocean came from North America and what portion Ceime from Asia, One of the newer and more fascinating approaches, or techniques, applied is that of serological or blood chemistry differences between Asian and North American fish. It has been necessary to develop this research from a rather scanty basis of knowledge of blood types in fish. However, it has been found that salmon and other fishes do indeed have blood types. It has been possible to produce antisera which will react with the blood of North American red salmon but will not react with the blood of Asian red salmon. By this means it is possible to collect samples of blood on the high 21 seas and, subsequently to determine whether the blood was from Asian or North American fish, although the fish may have been taken thousands of miles from its point of origin. To siommarize briefly the results and progress at this point, we have worked out, for the years during which research has been possible, a picture of the distribution of North American red, pink, and chum salmon on the high seas. For red salmon it has been found that Bristol Bay fish are dominant in the Aleutian area as far west as 175° E. longitude; that is, a matter of about three-fourths of the distance from Bristol Bay to Kamchatka (fig, 3). Asian fish in smadler numbers are found as far east as the eastern Aleutian Islands, Figure 3.- -Distribution of western Alaska red salmon in 1957. In the shaded areas, western Alaska-type red salmon were dominant, and their relative abundance was proportional to the depth of the shading. Pink sailmon from the Bering Sea coast of North America were found very nearly as far west as Bristol Bay red salmon; however, not nearly so abundantly. Conversely, Asian pink salmon in 1957, and apparently also in 1959i were found as far east as the tip of the Alaska Peninsula in very considerable numbers. It seems that in these odd-numbered years Kamchatka fish overwhelmingly dominated the entire mid-Aleutian pink salmon population, Chxim salmon were distributed in approximately the same manner as pink salmon. Asian chums have been caught near the Shumagin Islands, and North American chums, while they go far to the west, do not appear actually to reach the Asian mainland. Again, the numbers of Asian chum Scdmon in mid-ocean appear to far outnumber those from North America. 22 The resiilts of racial studies provide two important answers related to problems of the Protocol. First, infor- mation on the extent of mixing of the salmon on the high seas is further strengthened. The east-west extent of the mixing area is shown in figure 4, North American red salmon, the species of greatest concern, have been recognized by the Commission to predominate in catches as far west as 175° E; these red salmon originated in the Bristol Bay region. Figure 4.--East-west extent of high seas mixing between American and Asian salmon. The area observed was near the Aleutians. The bars indicate for each species the range of latitude over which American and Asian fish are commonly found in the same waters. But the most important problem at this time is raised by the information on proportions of Bristol Bay red Seilmon found in various areas of the high seas (fig. 1), Even though the data presented here are only of the most general nature, the chart does show the extent of the Bristol Bay red salmion runs which migrate beyond the provisional line and are subject to capture by the Japanese fishery. This is the problem of the Protocol now before the Commission. 23 PACIFIC SALMON IN INTERNATIONAL WATERS^ Presented by William F. Royce Director, Fisheries Research Institute University of Washington Seattle, Washington Intensive research in the past several years has shown that the five species of Pacific salmon (genus Oncorhynchus) and steelhead trout {Salmo gairdneri ) travel tremendous distances in their ocean migrations. American salmon travel so far west, and Asian salmon so far east, that stocks from both continents are found mixed throughout a large part of the central North Pacific Ocean and Bering Sea. Some king or Chinook salmon {0. t skawytscka) born in the gravels of the Salmon River in the State of Idaho range at least as far as the central Aleutian Islands before maturing and returning again 2,500 miles to ascend the Columbia River enroute home. Occasional red or sockeye salmon {0. nerka) from lakes in British Columbia swim westward at least to 177° E. longitude, well over halfway to Asia, in their ocean travels. Chum salmon (0. keta) from southeastern Alaska naay make a round trip of 3,500 miles to the central Aleutians in their quest for food at sea, Steelhead trout from rivers of the State of Washington and Oregon also may wander at least to the central Aleutians in their seaward journeys. Likewise chum salmon and pink salmon (0. gorhuscha) from many Asian spawning areas are found feeding along the Aleutian chain as far eastward as the Alaska Peninsula, a distance of 1,000 to 1,500 miles from their nated streams. Ch\ims in the rich ocean feeding areas at the base of the Alaska Peninsula often are a mixture originating from such diverse spawning grounds as the Anadyr River in the Siberian Arctic, various rivers tributary to the Sea of Okhotsk, streams on the island of Hokkaido, Japan, and, as already mentioned, streams in many parts of Alaska, Silver or coho salmon (0. kisutch) from east Kamchatka range seaward to the central Aleutians (175° W.) a distance ofatleast 1,000 miles. High-seas salmon tagging has been conducted since 1955 by the Fisheries Research Institute of the College of Fish- eries of the University of Washington under contract to the United States Bureau of Commercial Fisheries. Tagging is also being done on a smaller scale by the Canadian and Japanese sections of the Commission, and the three programs have been integrated as far as practicable. Tagging salmon on the high seas has proved much more dif- ficult than tagging in coastal areas. Large specially -designed * Prepared by Allan C. Hartt, Fishery Research Institute, University of Washington for presentation at the North American Wildlife Conference. Dallas, Texas. March 7-9. 1960. 24 purse seines were developed for capturing salmon in the open sea in good condition for tagging. Brailing nets and holding tanks were designed for handling salmon with mini- mvim injury. Experiments were needed to find tags that would give maxim\am returns after 1 or 2 years on rapidly- growing fish. Identification of the several species of salmon, not normally a problem in coastal areas where fish are mature, was a problem at sea. Catches often included all five species and many age groups. Rapid identification of the younger fish sometimes only 8 to 10 inches long required practice. Sccde samples were taken from all fish tagged for later positive identification. A toted of 48,296 salmon and steelhead have been tagged over the 5 years, and 1,128 have been returned to date. The overall rate of return (2,3 percent) is based on all salmon tagged, including immatures, which of course yield fewer returns than matures. Returns of mature salmon, those destined to spawn in the year of tagging, average nearly 10 percent, Immatures may spawn 1, 2, or 3 years later, and some of those still at liberty will be recovered in I960 and 1961, Returns from centrad Pacific experiments have come from Japan, the U.S.S.R. , Alaska, Canada, Washington, Oregon, and Idaho, and from the Japa- nese high seas gill net fishery in the North Pacific Ocean and Bering Sea. Each year, results of tagging have disclosed new and valuable data on ocean habits and movements of salmon. The abxindance and migration patterns of the several species have been fovind to vary tremendously from year to year, so that continued observations are needed to answer fully the questions implicit in the North Pacific Treaty. A sximmary of resxilts to date for all species is presented in figures 5 to 8, Tagging areas are shown by circles, and recovery locations by arrowheads. The thickness of lines indicates approximate relative numbers of fish to a given destination. Liines are not intended to show exact routes, but are drawn diagrajumatically for simplicity. Fish are shown moving westward prior to going through Aleutian passes because purse- seine catches indicated a positive westward movement through tagging areas south of the Aleutians. In evaluating the four figures, it must be borne in nriind that most tagging was in the areas along the Aleutians from 160^ West to 170*^ East longitude. Mature salmon, of course, are recovered only in the year of tagging, while immatures are recovered 1 or 2 years later (except for some few immatures which were taken by the Japanese high seas gear in the year of tagging). Since tagging was conducted at numerous loca- tions each year from May to September, returns may be considered representative of summer stocks in the Aleutian area. Red salmon returns (fig. 5) indicate the overwhelming predominance of American red salmon along the entire Aleutian Chain in the North Pacific and Bering Sea. A total of 215 was returned from Bristol Bay, but only one from Asia. The destingation of a few others is uncertain. The 25 Figure 5.- -Generalized distribution pattern of tag returns from red salmon tagged at sea from 1956 to 1959. distribution of returns is in keeping with what we know about relative production in Asia and America; red salmon pro- duction in Bristol Bay alone is probably greater than that of Asia. Chum salmon (fig. 6) show quite a different picture, for those tagged in the Aleutians yielded 146 returns from Asia, and 52 frora Alaska. Nearly all Alaskan returns were from releases in the eastern Aleutians. Again results are in harmony with relative production in the pertinent recovery areas; Asian chum salmon production is much greater than that of northwest Alaska, Alaskan chiims are present at least to 177° West. The lone return to southeast Alaska indicates that few chums from this source travel as far as the central Aleutians. Pink salmon returns (fig. 7) show a still different picture. It should be noted here that pink salmon have a very uniform 2-year life history, and in many areas throughout their range, runs have a pronounced cyclic abvmdance in odd or even years. In odd years (1957 and 1959), pinks were abiuidant in the Aleutian tagging areas, and tag returns came only from east Kamchatka or were intercepted at intermediate points on the high seas by the Japanese fleet. (In 1955, tagging consisted of small-scale preliminary experiments only as far west as Kodiak Island.) In even years (1956 and 1958), pinks were present in relatively small numbers, but all coastal returns were from Alaska. Those taken on the high seas, as shown, had an uncertain destination, but it is noteworthy that runs to east Kamchatka were large in 1957 and 1959, and smadl in 1956 and 1958. Although other Asian production areas (west Kamchatka, for example) have very large runs in even and odd years, these areas have yielded no pink scdmon returns to date. East Kamchatkan pink runs are many times larger than those to northwest Alaska, at least in odd years. The few pinks tagged in the Gxilf of Alaska 26 ^ ^ / jCk/^°'L^ / AHCT : ocean! \ \ \ \ y^iffK \ ^ :\>K ~7^^A VvV^ K/ ^^f^ j^ x^M-;VNl-,, /^ 5:^ — * ^^rp^--\ \ \ y \^'"\ / / sO "A- JL. m..v o Tagging area Recovery area 150'E I55«E I60*E I65*E ITO'E I75'E 180' I75'W I70*W reS'W I60*W I55"W I50*W 145* W I40*W 135- w Figure 6.- -Generalized distribution pattern of tag returns from chum salmon tagged at sea from 1956 to 1959. Figure 7.--Generalized distribution pattern of tag returns from pink salmon tagged at sea from 1956 to 1959, indicate that some of this species cross the Gulf from southeastern Alaska. Results of tagging king and silver salmon and steelhead trout, as mentioned previously, have demonstrated that these species travel spectacxilar distances at sea, but numbers tagged and recovered have been too small for conclusions as to relative importance of Asian and American stocks in the areas of intermingling. In figure 8 each arrow indi- cates only one tag return. To date, returns of kings and steelhead have come only from America, but silvers have come from both continents. American production of kings and steelhead is far greater than Asian. Thus, tagging to date has shown a mixture of American and Asian salmon in ocean areas fished by the Japanese 27 / / Tov y / / AHCT C oceLI \ \ \ \\jr\ \ X \ / y^ yjtt^ -A^T\^\^)^^X\\ ><\ 1 sV / /f^W Lt^ , C / 7^ ^^%UJi T^''VlA.'L^Jk^.K V^ 1 -/S WM/kNDWSKI / -4 V 5^^36o9r\5ULF OF ^S^ VVX Bf^^^0'°°'" \Z^K^\^^^^f^^' HOKKAIDO^ 4>^^N^/ /hnt ^fSi^/ / !• l^"_l/^'T°^*Jicr\*''^\ \ "iic^^?^i "X/ ^L 1* JJ*^ / \ s\ 1 7^- 1 _/2hL T^V T~~~V \-^ 1 Sl^'NO . . -^J^ \/x-^ */ •' '7 V^so-^ '^^s^H y^£j \ \-..._ \^\^^\-''''\.^ / / //M^ is:-:-xi^-r^r^ PA / ~f TsfcJ 1^J4S'">-*T \Steelhead 1 1 ISO •E 155'E I60'E I65*E TO'E I75»E 180* I75'W I70'W I65'W I60'W I55'W 150'W 145-W 140-W 135- W Figure 8.- -Generalized distribution pattern of tag returns from king and silver salmon and steelhead trout tagged at sea from 1956 to 1959. high seas fleet. Red salmon are overwhelmingly American (Bristol Bay) across the full length of the Aleutians. Chums are a mixture, and Asian fish probably predominate in areas west of 170° West longitude. Pinks are abundant and over- whelmingly Asian in odd years, whereas in even years this species is scarce, but principally American in origin. The problem of boundaries of distribution of Asian and American salmon is thus made more complex by the dis- similar distribution of the several species. These distri- butions can be expected to vary annually in accordance with relative abundance and perhaps according to varying migra- tion patterns, oceanographic conditions, and the like. Canadian and United States regulations prohibit all szilmon fishing, except some trolling, on the high seas. This permits much more effective regulation since intensity of fishing upon rtms to individual rivers may be regulated according to size of runs. Depleted stocksmay be protected, and healthy runs fished more. High seas harvesting permits no such indi- vidual controls and cilso takes many immature salmon. This paper presents a brief outline of results to date of one phase of a large research program on Pacific salmon at sea. In addition to providing data for the purposes of the International North Pacific Fisheries Conunission, the re- search is providing a wezilth of new information on the ocean biology of scdmon. The saltwater life-history of salmon and steelhead is proving no less remarkable than their much- studied yet little-understood freshwater life-history. MS. 978. 5-60 28 6P0 89 368 5 MBL WHO! Library Senal llllflilllliilll'llinilikjl 1,1 ilii'l||:'j;|j;||| 5 WHSE 00132 •^3r.-:f=i--:F-=J J— t -j^-i t— i 'y-j >— i ZL-i "u-j_^ 1»U r:.^^ y (OKHOTSK S£A j'ki/l B F R 1 X a > 1-. tski apvnski V .V ALEUTIAN isv r / A' 7' Lisiiuiatu I* : M A R I A N A H