天津科技大学学报
天津科技大學學報
천진과기대학학보
JOURNAL OF TIANJIN UNIVERSITY OF SCIENCE & TECHNOLOGY
2013年
1期
22-29
,共8页
郭术津%孙军%张辉%翟惟东
郭術津%孫軍%張輝%翟惟東
곽술진%손군%장휘%적유동
浮游植物%北黄海%秋季%具槽帕拉藻
浮遊植物%北黃海%鞦季%具槽帕拉藻
부유식물%북황해%추계%구조파랍조
phytoplankton%northern Yellow Sea%autumn%Paralia sulcata
2011年11月21—25日在北黄海海域对32个站位进行了生物采样,应用Uterm?hl方法对调查海域的浮游植物群落进行了研究.经115个样品的分析,共发现浮游植物3门31属64种.调查区浮游植物群落主要由硅藻和甲藻组成,还有少量的金藻,物种以暖温性和广布性物种为主,主要优势种为:具槽帕拉藻、虹彩圆筛藻、三角角藻、斯氏几内亚藻、梭形角藻和旋链角毛藻等.本次调查浮游植物细胞丰度平均值为4.2×103,个/L;硅藻占浮游植物细胞丰度的比例最大,平均值为3.6×103个/L;其次为甲藻,平均值为0.95×103个/L.调查海域浮游植物细胞丰度分布不均匀,辽宁南岸海域最高,山东近岸海域其次,北黄海中部海域最低.细胞丰度在水体中的垂直分布趋势为先降低后升高,其中底层的细胞丰度主要由具槽帕拉藻和虹彩圆筛藻贡献.从断面分布上看,细胞丰度高值多集中在受陆源输入影响明显的近岸海域.调查区浮游植物群落多样性指数和均匀度指数均在北黄海北部海域较高,在近岸海域较低.与历史资料的对比发现,近30年来北黄海浮游植物群落结构比较稳定.
2011年11月21—25日在北黃海海域對32箇站位進行瞭生物採樣,應用Uterm?hl方法對調查海域的浮遊植物群落進行瞭研究.經115箇樣品的分析,共髮現浮遊植物3門31屬64種.調查區浮遊植物群落主要由硅藻和甲藻組成,還有少量的金藻,物種以暖溫性和廣佈性物種為主,主要優勢種為:具槽帕拉藻、虹綵圓篩藻、三角角藻、斯氏幾內亞藻、梭形角藻和鏇鏈角毛藻等.本次調查浮遊植物細胞豐度平均值為4.2×103,箇/L;硅藻佔浮遊植物細胞豐度的比例最大,平均值為3.6×103箇/L;其次為甲藻,平均值為0.95×103箇/L.調查海域浮遊植物細胞豐度分佈不均勻,遼寧南岸海域最高,山東近岸海域其次,北黃海中部海域最低.細胞豐度在水體中的垂直分佈趨勢為先降低後升高,其中底層的細胞豐度主要由具槽帕拉藻和虹綵圓篩藻貢獻.從斷麵分佈上看,細胞豐度高值多集中在受陸源輸入影響明顯的近岸海域.調查區浮遊植物群落多樣性指數和均勻度指數均在北黃海北部海域較高,在近岸海域較低.與歷史資料的對比髮現,近30年來北黃海浮遊植物群落結構比較穩定.
2011년11월21—25일재북황해해역대32개참위진행료생물채양,응용Uterm?hl방법대조사해역적부유식물군락진행료연구.경115개양품적분석,공발현부유식물3문31속64충.조사구부유식물군락주요유규조화갑조조성,환유소량적금조,물충이난온성화엄포성물충위주,주요우세충위:구조파랍조、홍채원사조、삼각각조、사씨궤내아조、사형각조화선련각모조등.본차조사부유식물세포봉도평균치위4.2×103,개/L;규조점부유식물세포봉도적비례최대,평균치위3.6×103개/L;기차위갑조,평균치위0.95×103개/L.조사해역부유식물세포봉도분포불균균,료녕남안해역최고,산동근안해역기차,북황해중부해역최저.세포봉도재수체중적수직분포추세위선강저후승고,기중저층적세포봉도주요유구조파랍조화홍채원사조공헌.종단면분포상간,세포봉도고치다집중재수륙원수입영향명현적근안해역.조사구부유식물군락다양성지수화균균도지수균재북황해북부해역교고,재근안해역교저.여역사자료적대비발현,근30년래북황해부유식물군락결구비교은정.
Totally 115 phytoplankton water samples were collected from 32 stations in northern Yellow Sea from November 21 to 25 in 2011. The composition and abundance of the phytoplankton species were studied with Uterm?hl method. A total of 64 taxa which belong to 31 genera of 3 phyla were identified. The phytoplankton community was mainly composed of Bacillariophyta and Pyrrophyta,and there were also a few species belonging to Chrysophyta. Most of the ecotype of the phy-toplankton species was neritic or cosmopolitan. The dominant species were Paralia sulcata Cleve,Coscinodiscus oculus-iridis Ehrenberg,Ceratium tripos Nitzsch,Guinardia striata Hasle,Ceratium fusus Dujardin and Chaetoceros curvisetus Cleve,etc. The average of phytoplankton cell abundance was 4.2×103 cells/L,with cell abundance of Bacillariophyta aver-aging at 3.6×103 cells/L and Pyrrophyta averaging at 0.95×103 cells/L. Horizontally,cell abundance distributed unevenly in the surveyed area,with Liaoning coastal water ranking first,followed by Shandong coastal water,and the central part of northern YS ranking last. Vertically,phytoplankton cell abundance first decreased in the upper water,and then increased with the increase of depth. Near the bottom water,Par. sulcata and Cos. iridis were the dominant species. Sectionally, phytoplankton mainly concentrated in the coastal area under anthropogenic influences. Both Shannon-Wiener diversity index and Pielou’s evenness index appeared higher in the northern part of northern YS. Compared with historical data, phytoplankton communities in northern YS didn’t show significant alteration during the past 30 years.