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Poster abstracts and manuscripts from the Third International ...

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Fishing debris accounted for 18.3% of <strong>the</strong> petrochemical debris;<br />

gillnet floats alone comprised 15.0% of <strong>the</strong> total petrochemical<br />

debris. Fishing net fragments (35 trawl net fragments, 27<br />

gillnet<br />

of <strong>the</strong> total petrochemical debris observed (Fig. 5).<br />

fragments, 3 unknown net fragments) were minor components<br />

As <strong>the</strong><br />

results of collecting <strong>the</strong> fishing net fragments, weight of two<br />

fishing net fragments were more than several hundred kilograms.<br />

They consisted of many kinds of trawl nets, gillnet, ropes, <strong>and</strong><br />

o<strong>the</strong>r strings, <strong>and</strong> those fragments were bound (Photo 1).<br />

net fragments were mainly observed <strong>from</strong> June 24 to 30 in 1989<br />

while cruising in <strong>the</strong> central North Pacific (Fig. 6).<br />

79<br />

Density of marine debris<br />

Fishing<br />

Density (number/km 2 ) of marine debris was high in <strong>the</strong> center of<br />

North Pacific (about 160°W line <strong>from</strong> 40°N to Hawaii, l.0/km 2 )<br />

<strong>and</strong> off North America (0.6/km 2 ). It was low in <strong>the</strong> Bering Sea.<br />

offshore area off Alaska, Kamchatka <strong>and</strong> Kurile Isl<strong>and</strong>s (under<br />

0.2/km2). The highest densities of marine debris occurred in <strong>the</strong><br />

nor<strong>the</strong>astern area off Hawaii (1.4/km 2 ) <strong>and</strong> <strong>the</strong> coastal area off<br />

nor<strong>the</strong>rn Japan (1.3/km 2 ). Distribution of plastic debris density<br />

were similar to that of total debris density except off California<br />

(Table 2).<br />

Distribution characteristics of marine debris<br />

Percentages of marine debris observed in <strong>the</strong> North Pacific <strong>and</strong><br />

Bering Sea are shown in Table 3. Percentage of wood <strong>and</strong> natural<br />

log were higher than 14.4% in <strong>the</strong> Bering Sea, offshore area off<br />

Alaska, Aleutian Isl<strong>and</strong>s, Kamchatka, <strong>and</strong> Kurile Isl<strong>and</strong>s except<br />

high latitude (47°N line) of western North Pacific (53.1%). On<br />

<strong>the</strong> o<strong>the</strong>r h<strong>and</strong>, percentage of petrochemical products were higher<br />

than 82.1% off nor<strong>the</strong>rn Japan, central North Pacific, <strong>and</strong> in <strong>the</strong><br />

north eastern area off Hawaii <strong>and</strong> low, less than 46.7%, off<br />

California, Alaska Bay, Aleutian Isl<strong>and</strong>s, Bering Sea, off<br />

Kamchatka, <strong>and</strong> Kurile Isl<strong>and</strong>s.<br />

Discussion<br />

Distribution of total density of marine debris in this study was<br />

similar to results of Mio et al. <strong>and</strong> Day et al. Density of wood<br />

<strong>and</strong> natural log were higher in <strong>the</strong> north area <strong>and</strong> lower in <strong>the</strong><br />

middle area of North Pacific. On <strong>the</strong> contrary, density of<br />

petrochemical products was higher in <strong>the</strong> middle area <strong>and</strong> lower in<br />

<strong>the</strong> north area of North Pacific. This result may be related to<br />

human population <strong>and</strong> number of towns.<br />

Matsumura et al. reported that marine debris in <strong>the</strong> North Pacific<br />

may accumulate in <strong>the</strong> nor<strong>the</strong>astern area off Hawaii. Density of<br />

marine debris was highest off nor<strong>the</strong>rn Japan <strong>and</strong> in <strong>the</strong> nor<strong>the</strong>astern<br />

area off Hawaii. This tendency was shown on change of<br />

daily number of Styrofoam, vinyl, polyethylene, plastic observed<br />

in 1989's survey (Fig. 7) <strong>and</strong> 1990's survey (Fig. 8).<br />

Fur<strong>the</strong>rmore, many fishing net fragments were observed in <strong>the</strong><br />

nor<strong>the</strong>astern area off Hawaii. Kuroshio extension flows to <strong>the</strong><br />

central North Pacific (Favorite et al. 1976) Matsumura et al.<br />

indicated that a large gyre current exists in nor<strong>the</strong>ast area off<br />

Hawaii. The nor<strong>the</strong>astern area off Hawaii is recognized as an

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