检索规则说明:AND代表“并且”;OR代表“或者”;NOT代表“不包含”;(注意必须大写,运算符两边需空一格)
检 索 范 例 :范例一: (K=图书馆学 OR K=情报学) AND A=范并思 范例二:J=计算机应用与软件 AND (U=C++ OR U=Basic) NOT M=Visual
作 者:何剑锋[1,2] 王桂忠[2] 李少菁[2] Tushling K 郑淑娴[1,2]
机构地区:[1]中国极地研究中心,国家海洋局极地科学重点实验室 [2]厦门大学海洋学系,亚热带海洋研究所,厦门大学海洋环境科学教育部重点实验室,厦门361005 [3]Institute for Polar Ecology,241498 Kiel,Germany
出 处:《极地研究》2005年第1期1-10,共10页Chinese Journal of Polar Research
基 金:国家自然科学基金(40006010;30270112);科技部科技基础性工作专项项目 (2003DEB5J057);国家海洋局青年海洋科学基金(2003122)项目资助
摘 要:对1999年春季采集于北极拉普捷夫海东南部的冰藻和冰下浮游植物群落的种类组成进行了分析,并对丰度和生物量进行了统计和对比。藻种以硅藻占绝对优势,其中又以羽纹硅藻为主。优势种集中,主要包括海洋拟脆杆藻(Fragilariopsisoceanica)、圆柱拟脆杆藻(F.cylindrus)、寒冷菱形藻(Nitzschiafrigida)、普罗马勒菱形藻(N. promare)、带纹曲壳藻(Ach nanthestaeniata)、新寒冷菱形藻(Nitzschianeofrigida)、大洋舟形藻(Naviculapelagica)、范氏舟形藻(N. vanhoeffenii)、北极直链藻(Melosiraarctica)、北方舟形藻(N. septentrionalis)、新月细柱藻(Clindrothecaclosterium)和绿藻门的塔形藻(Pyramimonassp. )。微藻主要集中在冰底10cm,丰度为14. 6—1562. 2×104 cells·L-1,平均为639. 0×104 cells·L-1;生物量为7. 89—2093. 5μgC·L-1,平均为886. 9μgC·L-1,总体上比次冰底高1个数量级,比冰下表层水柱高2个数量级。冰底20cm冰柱的累计丰度和生物量平均分别为冰下20m水柱累计量的7. 7和12. 2倍,显示冰藻在春季海冰融化前在近岸生态系统中的重要作用。尽管各站位冰底和冰下表层水柱藻类群落的相似性普遍不高,但整个调查海域冰底和冰下水柱优势种极为相似,春季期间冰藻对冰下浮游植物群落的影响明显。由于?Species composition, abundance and biomass of ice algal and underlying phytoplankton communities were investigated in southeastern Laptev Sea in spring 1999. Diatoms were predominant in algal species and pennate diatoms were dominant in diatom species. 12 dominant algal species occurred in ice and underlying water column, which included Fragilariopsis oceanica, F. cylindrus, Nitzschia frigida, N. promare, Achnanthes taeniata, Nitzschia neofrigida, Navicula pelagica, N. vanhoeffenii, N. septentrionalis, Melosira arctica, Clindrotheca closterium and Pyramimonas sp. The algal abundance within bottom 10cm sea ice were between 14.6 and 1562.2 ×10 4 cells·L -1 with an average of 639.0 ×10 4 cells·L -1 , and the algal biomass were between 7.89 and 2093.5 μg C·L -1 with an average of 886.9 μg C·L -1 , which were about one magnitude higher than those of sub-bottom and two magnitude higher than those of underlying surface water. The integrated algal abundance and biomass within bottom 20cm ice column were averagely 7.7 and 12.2 times as those in underlying 20m water column, respectively, suggesting that the ice algae might play an important role in maintaining the coastal marine ecosystem before the melting of sea ice. The influence of ice algae to the phytoplankton community was obvious although the similarities of algal community in ice bottom and water surface were not high in many sites. But the “seeding” of ice algae to phytoplankton was low because the abundance and biomass in water column were much lower than those in bottom ice and no rapid growth occurred within phytoplankton community.
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在链接到云南高校图书馆文献保障联盟下载...
云南高校图书馆联盟文献共享服务平台 版权所有©
您的IP:216.73.216.229