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日本鄂霍次克海猿间湖和加拿大北极地区雷索卢特海峡第一年海冰及下层海水中的细菌动态:冰藻对细菌动态的抑制作用

Bacterial dynamics in first year sea ice and underlying seawater of Saroma-ko Lagoon (Sea of Okhotsk, Japan) and resolute passage (High Canadian Arctic): inhibitory effects of ice algae on bacterial dynamics.

作者信息

Monfort P, Demers S, Levasseur M

机构信息

Unité Mixte de Recherche n. 5556 "Ecosystèmes Lagunaires" CNRS-Université Montpellier II, France.

出版信息

Can J Microbiol. 2000 Jul;46(7):623-32.

Abstract

The seasonal development of bacterial abundance in first year bottom ice and underlying seawater were studied at Saroma-ko Lagoon in Hokkaido, Japan, and at Resolute Passage in the High Canadian Arctic during the algal bloom in spring 1992. The aim of this study was to evaluate whether the high algal concentrations reached during the bloom of ice algae have inhibitory effects on bacterial dynamics. Bacterial abundance (measured as total cell count and colony-forming units CFU) increased with the increase of the algal biomass up to 500 micrograms Chla.L-1 in both locations. Culturable fraction (measured as the percentage of CFU counts versus the total cell counts) was between 7% and 22% at Saroma-ko, and approximately 0.08% at Resolute Passage. When algal biomass exceeded 500 micrograms of Chla.L-1, both bacterial abundance and culturable fraction decreased significantly. There was a maximum threshold of algal biomass (between 500 and 800 micrograms of Chla.L-1) after which bacterial dynamics become negatively coupled to the algal biomass. These results suggest that bactericidal and/or bacteriostatic compounds from these extremely high algal concentrations could explain the decrease in bacterial abundance and culturability in bottom ice observed after the ice algae bloom.

摘要

1992年春季藻类大量繁殖期间,在日本北海道的佐吕间湖以及加拿大北极地区的雷索卢特海峡,对第一年海冰底部和其下海水细菌丰度的季节性变化进行了研究。本研究的目的是评估冰藻大量繁殖期间达到的高藻类浓度是否对细菌动态具有抑制作用。在这两个地点,细菌丰度(以总细胞计数和菌落形成单位CFU衡量)均随着藻类生物量增加至500微克叶绿素a/升而增加。在佐吕间湖,可培养部分(以CFU计数占总细胞计数的百分比衡量)在7%至22%之间,在雷索卢特海峡约为0.08%。当藻类生物量超过500微克叶绿素a/升时,细菌丰度和可培养部分均显著下降。藻类生物量存在一个最大阈值(在500至800微克叶绿素a/升之间),超过此阈值后细菌动态与藻类生物量呈负相关。这些结果表明,来自这些极高藻类浓度的杀菌和/或抑菌化合物可以解释冰藻大量繁殖后在海冰底部观察到的细菌丰度和可培养性的下降。

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