Unusual distribution of floating seaweeds in the East China Sea in the early spring of 2012

被引:47
|
作者
Komatsu, Teruhisa
Mizuno, Shizuha
Natheer, Alabsi
Kantachumpoo, Attachai
Tanaka, Kiyoshi
Morimoto, Akihiko [1 ]
Hsiao, Sheng-Tai [2 ]
Rothausler, Eva A.
Shishidou, Hirotoshi [3 ]
Aoki, Masakazu [4 ]
Ajisaka, Tetsuro [5 ]
机构
[1] Nagoya Univ, Hydrospher Atmospher Res Ctr, Chikusa Ku, Nagoya, Aichi 4648601, Japan
[2] Taiwan Fisheries Res Inst, Marine Fisheries Div, Keelung 20246, Taiwan
[3] Kagoshima Prefectural Fisheries Technol & Dev Ctr, Ibusuki, Kagoshima 8910315, Japan
[4] Tohoku Univ, Grad Sch Agr Sci, Div Appl Aquat Biosci, Aoba Ku, Sendai, Miyagi 9818555, Japan
[5] Kyoto Univ, Div Appl Biosci, Grad Sch Agr, Sakyo Ku, Kyoto 6068502, Japan
基金
日本学术振兴会;
关键词
Floating seaweed; Sargassum horneri; Phaeophyta; East China Sea; Kuroshio; Transport; Ekman drift current; SSH; PHAEOPHYCEAE; TEMPERATURE; DISPERSAL; LONGEVITY; PACIFIC; OBJECTS; CLUMPS;
D O I
10.1007/s10811-013-0152-y
中图分类号
Q81 [生物工程学(生物技术)]; Q93 [微生物学];
学科分类号
071005 ; 0836 ; 090102 ; 100705 ;
摘要
Floating seaweeds play important ecological roles in offshore waters. Recently, large amounts of rafting seaweed have been observed in the East China Sea. In early spring, juveniles of commercially important fish such as yellowtail accompany these seaweed rafts. Because the spatial distributions of seaweed rafts in the spring are poorly understood, research cruises were undertaken to investigate them in 2010, 2011, and 2012. Floating seaweed samples collected from the East China Sea during the three surveys contained only Sargassum horneri. In 2010 and 2011, seaweed rafts were distributed only in the continental shelf and the Kuroshio Front because they had become trapped in the convergence zone of the Kuroshio Front. However, in 2012, seaweed was also distributed in the Kuroshio Current and its outer waters, and massive strandings of seaweed rafts were observed on the northern coast of Taiwan and on Tarama Island in the Ryukyu Archipelago. Environmental data (wind, currents, and sea surface height) were compared among the surveys of 2010, 2011, and 2012. Two factors are speculated to have caused the unusual distribution in 2012. First, a continuous strong north wind produced an Ekman drift current that transported seaweed southwestward to the continental shelf and eventually stranded seaweed rafts on the coast of Taiwan. Second, an anticyclonic eddy covering northeast Taiwan and the Kuroshio Current west of Taiwan generated a geostrophic current that crossed the Kuroshio Current and transported the rafts to the Kuroshio Current and its outer waters. Such unusual seaweed distributions may influence the distribution of fauna accompanying the rafts.
引用
收藏
页码:1169 / 1179
页数:11
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