Suppr超能文献

地中海深部高盐缺氧盆地氧化还原梯度沉积物中的底栖原生生物和真菌。

Benthic protists and fungi of Mediterranean deep hypsersaline anoxic basin redoxcline sediments.

机构信息

Geology and Geophysics Department, Woods Hole Oceanographic Institution Woods Hole, MA, USA.

Department of Ichthyology and Aquatic Environment, School of Agricultural Sciences, University of Thessaly Volos, Greece.

出版信息

Front Microbiol. 2014 Nov 12;5:605. doi: 10.3389/fmicb.2014.00605. eCollection 2014.

Abstract

Some of the most extreme marine habitats known are the Mediterranean deep hypersaline anoxic basins (DHABs; water depth ∼3500 m). Brines of DHABs are nearly saturated with salt, leading many to suspect they are uninhabitable for eukaryotes. While diverse bacterial and protistan communities are reported from some DHAB water-column haloclines and brines, the existence and activity of benthic DHAB protists have rarely been explored. Here, we report findings regarding protists and fungi recovered from sediments of three DHAB (Discovery, Urania, L' Atalante) haloclines, and compare these to communities from sediments underlying normoxic waters of typical Mediterranean salinity. Halocline sediments, where the redoxcline impinges the seafloor, were studied from all three DHABs. Microscopic cell counts suggested that halocline sediments supported denser protist populations than those in adjacent control sediments. Pyrosequencing analysis based on ribosomal RNA detected eukaryotic ribotypes in the halocline sediments from each of the three DHABs, most of which were fungi. Sequences affiliated with Ustilaginomycotina Basidiomycota were the most abundant eukaryotic signatures detected. Benthic communities in these DHABs appeared to differ, as expected, due to differing brine chemistries. Microscopy indicated that only a low proportion of protists appeared to bear associated putative symbionts. In a considerable number of cases, when prokaryotes were associated with a protist, DAPI staining did not reveal presence of any nuclei, suggesting that at least some protists were carcasses inhabited by prokaryotic scavengers.

摘要

已知的一些最极端的海洋栖息地是地中海深部高盐缺氧盆地(DHAB;水深约 3500 米)。DHAB 的盐水几乎饱和了盐分,这使得许多人怀疑它们对真核生物来说是无法居住的。虽然在一些 DHAB 水柱盐跃层和盐水中报告了多种多样的细菌和原生生物群落,但底栖 DHAB 原生生物的存在和活性很少被探索。在这里,我们报告了从三个 DHAB(发现、乌利亚纳、拉阿塔兰特)盐跃层沉积物中回收的原生生物和真菌的发现,并将这些与典型地中海盐度下正常含氧水域沉积物中的群落进行了比较。在所有三个 DHAB 中,都研究了与氧化还原层撞击海底的盐跃层沉积物。显微镜细胞计数表明,盐跃层沉积物中的原生生物密度高于相邻对照沉积物中的原生生物密度。基于核糖体 RNA 的焦磷酸测序分析在来自三个 DHAB 的盐跃层沉积物中检测到了真核生物核糖体型,其中大多数是真菌。与 Ustilaginomycotina Basidiomycota 相关的序列是检测到的最丰富的真核生物特征。由于盐水化学性质的不同,预计这些 DHAB 中的底栖群落会有所不同。显微镜观察表明,只有一小部分原生生物似乎带有相关的假定共生体。在相当多的情况下,当原核生物与原生生物相关联时,DAPI 染色并未显示出任何核的存在,这表明至少一些原生生物是被原核生物食腐动物占据的尸体。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/1bbc/4233946/eec628f95988/fmicb-05-00605-g001.jpg

文献AI研究员

20分钟写一篇综述,助力文献阅读效率提升50倍。

立即体验

用中文搜PubMed

大模型驱动的PubMed中文搜索引擎

马上搜索

文档翻译

学术文献翻译模型,支持多种主流文档格式。

立即体验