热带海洋学报
熱帶海洋學報
열대해양학보
JOURNAL OF TROPICAL OCEANOGRAPHY
2013年
3期
40-46
,共7页
马艳娥%柯志新%黄良民%谭烨辉
馬豔娥%柯誌新%黃良民%譚燁輝
마염아%가지신%황량민%담엽휘
浮游植物%细胞体积%粒级结构%生物量%大亚湾
浮遊植物%細胞體積%粒級結構%生物量%大亞灣
부유식물%세포체적%립급결구%생물량%대아만
phytoplankton%cell size%size structure%biomass%Daya Bay
于2010年8月和2011年1月对大亚湾6个典型站位的浮游植物进行采样调查,估算了浮游植物细胞体积,分析了各区域浮游植物的粒级组成,比较了大亚湾各典型站位浮游植物生物量的粒级结构差异。大亚湾浮游植物的细胞体积范围为64-496757μm3,以1600-3200μm3粒级的浮游植物种类最多,分布在粒级谱两端的浮游植物的种类较少。夏季大亚湾浮游植物细胞丰度和由细胞体积转换的湿重生物量高于冬季,夏季平均为76.5×104个·L?1和1.6mg·L?1,冬季平均为22.52×104个·L?1和0.45mg·L?1。夏冬两季均以营养盐水平高且水交换能力差的 S8站位生物量最高,且该站夏冬两季均以甲藻为主。夏季大亚湾湾内站位和冬季大部分站位顶端粒级的种类对浮游植物初级生产力和碳库的贡献很重要,但因为丰度小,在细胞丰度表示的浮游植物现存量和优势种中没有体现,细胞体积转换生物量则能更为客观合理地表征浮游植物现存量和作为优势种的判断依据。
于2010年8月和2011年1月對大亞灣6箇典型站位的浮遊植物進行採樣調查,估算瞭浮遊植物細胞體積,分析瞭各區域浮遊植物的粒級組成,比較瞭大亞灣各典型站位浮遊植物生物量的粒級結構差異。大亞灣浮遊植物的細胞體積範圍為64-496757μm3,以1600-3200μm3粒級的浮遊植物種類最多,分佈在粒級譜兩耑的浮遊植物的種類較少。夏季大亞灣浮遊植物細胞豐度和由細胞體積轉換的濕重生物量高于鼕季,夏季平均為76.5×104箇·L?1和1.6mg·L?1,鼕季平均為22.52×104箇·L?1和0.45mg·L?1。夏鼕兩季均以營養鹽水平高且水交換能力差的 S8站位生物量最高,且該站夏鼕兩季均以甲藻為主。夏季大亞灣灣內站位和鼕季大部分站位頂耑粒級的種類對浮遊植物初級生產力和碳庫的貢獻很重要,但因為豐度小,在細胞豐度錶示的浮遊植物現存量和優勢種中沒有體現,細胞體積轉換生物量則能更為客觀閤理地錶徵浮遊植物現存量和作為優勢種的判斷依據。
우2010년8월화2011년1월대대아만6개전형참위적부유식물진행채양조사,고산료부유식물세포체적,분석료각구역부유식물적립급조성,비교료대아만각전형참위부유식물생물량적립급결구차이。대아만부유식물적세포체적범위위64-496757μm3,이1600-3200μm3립급적부유식물충류최다,분포재립급보량단적부유식물적충류교소。하계대아만부유식물세포봉도화유세포체적전환적습중생물량고우동계,하계평균위76.5×104개·L?1화1.6mg·L?1,동계평균위22.52×104개·L?1화0.45mg·L?1。하동량계균이영양염수평고차수교환능력차적 S8참위생물량최고,차해참하동량계균이갑조위주。하계대아만만내참위화동계대부분참위정단립급적충류대부유식물초급생산력화탄고적공헌흔중요,단인위봉도소,재세포봉도표시적부유식물현존량화우세충중몰유체현,세포체적전환생물량칙능경위객관합리지표정부유식물현존량화작위우세충적판단의거。
Based on samples collected at six typical sites of Daya Bay in August 2010 and January of 2011, phytoplankton cell volume was estimated, phytoplankton size structure was analyzed, and phytoplankton biomass size structure was investigated. Cell volume of phytoplankton in Daya Bay was in the range of 64 to 496757 μm3, though only a few species distributed at the two ends of the range;the species distributed in the range of 1600?3200 μm3 were the richest. Phytoplankton cell abundance and cell volume converted biomass were 76.5×104 cell·L?1 and 1.6 mg·L?1 in summer, and 22.52×104 cell·L?1 and 0.45 mg·L?1 in winter, respectively, which were both obviously lower than those in summer. S8 that was labeled by highest nutrient and lowest water exchange capability showed the highest biomass and was dominated by dinoflagellates in both summer and winter. At most sites in winter and those sites inside the bay in summer, the species with the largest cell size made significant contribution to biomass and carbon stock. However, the contribution of large species with low abundance could not be seen through cell abundance represented biomass and key species. Biomass converted by cell volume was comparatively a more reasonable way to represent phytoplankton stock and to identify key species than cell abundance.