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本文引用的文献

1
Ingestion and assimilation by marine protists fed on bacteria labeled with radioactive thymidine and leucine estimated without separating predator and prey.估计没有分离捕食者和猎物的情况下,用放射性胸腺嘧啶和亮氨酸标记细菌喂养的海洋原生动物的摄取和吸收。
Microb Ecol. 1995 Sep;30(2):157-70. doi: 10.1007/BF00172571.
2
Comparison of phosphate uptake rates by the smallest plastidic and aplastidic protists in the North Atlantic subtropical gyre.比较北大西洋亚热带环流区最小质体和无质体原生生物的磷酸盐摄取率。
FEMS Microbiol Ecol. 2011 Nov;78(2):327-35. doi: 10.1111/j.1574-6941.2011.01160.x. Epub 2011 Jul 14.
3
Plastid 16S rRNA gene diversity among eukaryotic picophytoplankton sorted by flow cytometry from the South Pacific Ocean.流式细胞术分选南太平洋真核微微型浮游植物的质体 16S rRNA 基因多样性。
PLoS One. 2011 Apr 28;6(4):e18979. doi: 10.1371/journal.pone.0018979.
4
Targeted metagenomics and ecology of globally important uncultured eukaryotic phytoplankton.全球重要未培养真核浮游植物的靶向宏基因组学和生态学研究。
Proc Natl Acad Sci U S A. 2010 Aug 17;107(33):14679-84. doi: 10.1073/pnas.1001665107. Epub 2010 Jul 28.
5
Significant CO2 fixation by small prymnesiophytes in the subtropical and tropical northeast Atlantic Ocean.小型颗石藻在亚热带和热带东北大西洋的显著 CO2 固定作用。
ISME J. 2010 Sep;4(9):1180-92. doi: 10.1038/ismej.2010.36. Epub 2010 Apr 15.
6
Photosynthetic picoeukaryote community structure in the South East Pacific Ocean encompassing the most oligotrophic waters on Earth.涵盖地球上最贫瘠水域的东南太平洋光合微微型真核生物群落结构。
Environ Microbiol. 2009 Dec;11(12):3105-17. doi: 10.1111/j.1462-2920.2009.02015.x. Epub 2009 Aug 5.
7
Extreme diversity in noncalcifying haptophytes explains a major pigment paradox in open oceans.非钙化定鞭藻的极端多样性解释了公海中一个主要的色素悖论。
Proc Natl Acad Sci U S A. 2009 Aug 4;106(31):12803-8. doi: 10.1073/pnas.0905841106. Epub 2009 Jul 21.
8
Use of stable isotope-labelled cells to identify active grazers of picocyanobacteria in ocean surface waters.利用稳定同位素标记细胞识别海洋表层水体中微小蓝细菌的活跃捕食者。
Environ Microbiol. 2009 Feb;11(2):512-25. doi: 10.1111/j.1462-2920.2008.01793.x.
9
High bacterivory by the smallest phytoplankton in the North Atlantic Ocean.北大西洋最小浮游植物的高噬菌率。
Nature. 2008 Sep 11;455(7210):224-6. doi: 10.1038/nature07236.
10
Microbial control of phosphate in the nutrient-depleted North Atlantic subtropical gyre.营养匮乏的北大西洋亚热带环流中磷酸盐的微生物控制
Environ Microbiol. 2007 Aug;9(8):2079-89. doi: 10.1111/j.1462-2920.2007.01324.x.

大西洋贫营养生态系统的混合营养基础。

Mixotrophic basis of Atlantic oligotrophic ecosystems.

机构信息

Ocean Biogeochemistry and Ecosystems Research Group, National Oceanography Centre, Southampton SO14 3ZH, United Kingdom.

出版信息

Proc Natl Acad Sci U S A. 2012 Apr 10;109(15):5756-60. doi: 10.1073/pnas.1118179109. Epub 2012 Mar 26.

DOI:10.1073/pnas.1118179109
PMID:22451938
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC3326507/
Abstract

Oligotrophic subtropical gyres are the largest oceanic ecosystems, covering >40% of the Earth's surface. Unicellular cyanobacteria and the smallest algae (plastidic protists) dominate CO(2) fixation in these ecosystems, competing for dissolved inorganic nutrients. Here we present direct evidence from the surface mixed layer of the subtropical gyres and adjacent equatorial and temperate regions of the Atlantic Ocean, collected on three Atlantic Meridional Transect cruises on consecutive years, that bacterioplankton are fed on by plastidic and aplastidic protists at comparable rates. Rates of bacterivory were similar in the light and dark. Furthermore, because of their higher abundance, it is the plastidic protists, rather than the aplastidic forms, that control bacterivory in these waters. These findings change our basic understanding of food web function in the open ocean, because plastidic protists should now be considered as the main bacterivores as well as the main CO(2) fixers in the oligotrophic gyres.

摘要

贫营养亚热带回旋流是最大的海洋生态系统,覆盖了地球表面的>40%。在这些生态系统中,单细胞蓝细菌和最小的藻类(质体原生生物)占主导地位,它们通过竞争溶解无机养分来固定 CO(2)。在这里,我们提供了直接证据,这些证据来自于大西洋亚热带回旋流及其相邻的赤道和温带地区的表层混合层,这些样本是在连续三年的三次大西洋子午剖面考察中收集的,表明质体和无质体原生生物以相当的速率被细菌吞噬。在有光和无光的情况下,细菌的吞噬率是相似的。此外,由于它们的丰度更高,控制这些水域中细菌吞噬的是质体原生生物,而不是无质体形式。这些发现改变了我们对开阔海洋食物网功能的基本认识,因为现在应该将质体原生生物视为贫营养回旋流中的主要细菌吞噬者和主要 CO(2)固定者。