Vertical distribution of oceanic tintinnid (Ciliophora: Tintinnida) assemblages from the Bering Sea to Arctic Ocean through Bering Strait

Vertical distribution of oceanic tintinnid (Ciliophora: Tintinnida) assemblages from the Bering Sea to Arctic Ocean through Bering Strait
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DOI:
10.1007/s00300-019-02585-2
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发表时间:
2019-09
期刊:
影响因子:
1.7
通讯作者:
Chaofeng Wang;Zhiqiang Xu;Cheng-gang Liu;Haibo Li;Chen Liang;Yuan Zhao;Guangtao Zhang;Wuchang Zhang;T. Xiao
Chaofeng Wang;Zhiqiang Xu;Cheng-gang Liu;Haibo Li;Chen Liang;Yuan Zhao;Guangtao Zhang;Wuchang Zhang;T. Xiao
中科院分区:
环境科学与生态学3区
文献类型:
--
作者:
Chaofeng Wang;Zhiqiang Xu;Cheng-gang Liu;Haibo Li;Chen Liang;Yuan Zhao;Guangtao Zhang;Wuchang Zhang;T. Xiao

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有关浮游生物种类分布的知识是了解浮游生态系统结构和功能的基础。为了了解白令海和北冰洋丁虫垂直分布模式的差异及其通过白令海峡的联系,我们报道了从白令海到北冰洋的丁虫组合的垂直分布。白令海优势种(冷叶党参、钝顶叶党参、副甲藻、褐棘孔藻)的丰度高峰出现在50m以上,北冰洋优势种(P.urnula)的丰度峰出现在表层和深层。白令海和北冰洋海域的降雪发生在50到80米之间。白令海峡优势种(尖吻对虾、对虾、褐家对虾)从表层到底层均有分布。两个都是。尖端和尖端。白令海峡在120微米以下的海区没有浮游植物,白令海区优势种(冷藻、钝顶梭子藻、副甲藻、褐藻)陆续向北消失,白令海峡北部超过50微米的海区出现乌氏松毛虫。Auta(仅发生在白令海峡)介于OFP之间。乌鲁拉和P。钝顶牛。白令海优势种的温度范围宽,盐度范围窄(32.7-33.3),它们连续向北消失可能反映了北冰洋耐盐性的差异。北冰洋轮虫的盐度范围宽,温度范围窄。它通过白令海峡的分布可能受到温度(− 1.8至1.2摄氏度)的限制。Fs的垂直分布。尖端和尖端。光芒与深度相关。我们的结果有助于更好地了解微生物食物网的垂直分布,并为今后研究北极中上层群落的变化提供了基线。
Knowledge on the distribution of plankton species is fundamental to understand planktonic ecosystem structure and function. To understand the difference of tintinnid vertical distribution pattern in the Bering Sea and the Arctic Ocean and their connection through the Bering Strait, we reported the vertical distribution of tintinnid assemblages from the Bering Sea to the Arctic Ocean. Bering Sea-dominant species (Codonellopsis frigida,Ptychocylis obtusa,Parafavellaspp.,Acanthostomella norvegica) had abundance peak in the upper 50 m. In the Arctic Ocean, abundance peak of dominant species (P. urnula) occurred in surface and deep chlorophyllamaximum layers.Salpingella acuminataandS. faureioccurred from 50 to 80 m in Bering Sea and Arctic Ocean oceanic waters. Bering Strait-dominant species (P. acuta,Parafavellaspp.,A. norvegica) occurred from the surface to the bottom. BothS. acuminataandS. faureiwere absent in Bering Strait at depths shallower than 120 m. Bering Sea-dominant species (C. frigida,P. obtusa,Parafavellaspp.,A. norvegica) disappeared successively northward.Ptychocylis urnulaoccurred in the northern part of Bering Strait at depths exceeding 50 m. The size ofP. acuta(only occurring in Bering Strait) was between that ofP. urnulaandP. obtusa. Bering Sea-dominant species had wide temperature but narrow salinity ranges (32.7–33.3); their successive northward disappearance might reflect difference in the salinity tolerance.Ptychocylis urnulahad a wide salinity but narrow temperature range in the Arctic Ocean. Its distribution through Bering Strait is likely limited by temperature (− 1.8 to 1.2 °C). The vertical distribution ofS. acuminataandS. faureimight correlate with depth. Our results contribute to a better understanding of the vertical distribution of the microbial food web and serve as a baseline for future studies on the pelagic community change in the Arctic.