馮志萍,余 為,2,3,4,陳新軍,2,3,4
( 1.上海海洋大學 海洋科學學院,上海 201306;2.國家遠洋漁業(yè)工程技術研究中心,上海 201306;3.大洋漁業(yè)資源可持續(xù)開發(fā)教育部重點實驗室,上海 201306;4.農業(yè)農村部大洋漁業(yè)開發(fā)重點實驗室,農業(yè)農村部大洋漁業(yè)資源環(huán)境科學觀測實驗站,上海 201306 )
圖1 2000—2015年東南太平洋海域莖柔魚和智利竹魚產量Fig.1 Production of jumbo flying squid D. gigas and Chilean jack mackerel T. murphyi in the Southeast Pacific Ocean from 2000 to 2015
圖2 東太平洋海域莖柔魚和智利竹魚空間分布Fig.2 Spatial distribution of jumbo flying squid D. gigas and Chilean jack mackerel T. murphyi in the eastern Pacific Ocean
表1 不同地理區(qū)域莖柔魚胴長及種群結構類型Tab.1 The mantle length and population structure of jumbo flying squid D. gigas in different geographical regions
圖3 秘魯上升流區(qū)域表層海洋要素狀況[59]Fig.3 Oceanic conditions in the Peru upwelling surface region[59]TSW.熱帶表層水;SST.沿岸長期觀測平均水溫(C°);ESW.赤道表層水;SSW.亞熱帶表層水;PUC.秘魯智利潛流;HC.洪堡海流;SASW.亞極地表層水.TSW.tropical surface water;SST.long-term mean values of sea surface temperatures(C°);ESW.equatorial surface water;SSW.subtropical surface water;PUC.Peru-Chile undercurrent;HC.Humboldt current;SASW.sub-Antarctic surface water.