海洋科学
海洋科學
해양과학
MARINE SCIENCES
2015年
7期
13-21
,共9页
乔芮%栾青杉%王俊%袁伟%崔毅%孙坚强
喬芮%欒青杉%王俊%袁偉%崔毅%孫堅彊
교예%란청삼%왕준%원위%최의%손견강
浮游植物%群落%崂山湾%冗余分析
浮遊植物%群落%嶗山灣%冗餘分析
부유식물%군락%로산만%용여분석
phytoplankton%community%Laoshan Bay%redundancy analysis
2013年春季(3、4、5月)对崂山湾海域浮游植物群落及其理化环境进行了3个航次的调查研究。共鉴定浮游植物40属75种,硅藻是调查区主要的浮游植物类群;浮游植物细胞丰度平均为1.27×106个/m3,3月份的平均丰度显著高于4、5月份(P<0.01);优势种主要为冰河拟星杆藻(Asterionopsis glacialis)、加拉星平藻(Asteroplanus karianus)、密联角毛藻(Chaetoceros densus)和夜光藻(Noctiluca scintillans),浮游植物群落演替明显,由3月份硅藻控制逐步过渡到4、5月份硅/甲藻共同控制;相对较低的硝酸盐水平是导致4、5月份浮游植物丰度显著低于3月份的主要原因;物种–环境数据的冗余分析(RDA)结果显示,温度、硝酸盐含量是控制崂山湾春季浮游植物分布的重要环境因子。
2013年春季(3、4、5月)對嶗山灣海域浮遊植物群落及其理化環境進行瞭3箇航次的調查研究。共鑒定浮遊植物40屬75種,硅藻是調查區主要的浮遊植物類群;浮遊植物細胞豐度平均為1.27×106箇/m3,3月份的平均豐度顯著高于4、5月份(P<0.01);優勢種主要為冰河擬星桿藻(Asterionopsis glacialis)、加拉星平藻(Asteroplanus karianus)、密聯角毛藻(Chaetoceros densus)和夜光藻(Noctiluca scintillans),浮遊植物群落縯替明顯,由3月份硅藻控製逐步過渡到4、5月份硅/甲藻共同控製;相對較低的硝痠鹽水平是導緻4、5月份浮遊植物豐度顯著低于3月份的主要原因;物種–環境數據的冗餘分析(RDA)結果顯示,溫度、硝痠鹽含量是控製嶗山灣春季浮遊植物分佈的重要環境因子。
2013년춘계(3、4、5월)대로산만해역부유식물군락급기이화배경진행료3개항차적조사연구。공감정부유식물40속75충,규조시조사구주요적부유식물류군;부유식물세포봉도평균위1.27×106개/m3,3월빈적평균봉도현저고우4、5월빈(P<0.01);우세충주요위빙하의성간조(Asterionopsis glacialis)、가랍성평조(Asteroplanus karianus)、밀련각모조(Chaetoceros densus)화야광조(Noctiluca scintillans),부유식물군락연체명현,유3월빈규조공제축보과도도4、5월빈규/갑조공동공제;상대교저적초산염수평시도치4、5월빈부유식물봉도현저저우3월빈적주요원인;물충–배경수거적용여분석(RDA)결과현시,온도、초산염함량시공제로산만춘계부유식물분포적중요배경인자。
Based on the surveys carried out in the Laoshan Bay during spring (March, April and May) of 2013, we studied the phytoplankton community in association with the ambient environment in this area. The results indi-cated that a total of 75 species (40 genera) were found from the samples collected, and diatoms were the predomi-nant forms in the community. The averaged phytoplankton cell abundance was 1.27×106 cells/m3, with the mean value in March was significantly higher than those in April and May (P<0.01). The dominant species wereAste-rionopsis glacialis,Asteroplanus karianus,Chaetoceros densus andNoctiluca scintillans. The succession of the phytoplankton community was obvious, from the diatom-control in March to the co-control of diatom and dinoflagellate in April and May. The decrease of phytoplankton abundance in April and May was related to the rela-tive low concentration of nitrate in the seawater. Redundancy analysis (RDA) of the species and environment cor-relation showed that temperature and nitrate were the main environmental factors in controlling the phytoplankton distribution in spring of 2013.