Southeast Environmental Research Center, OE-148, Florida International University, Miami, FL, 33199, USA.
Microb Ecol. 2014 Oct;68(3):427-40. doi: 10.1007/s00248-014-0418-1. Epub 2014 Apr 24.
Florida Bay exhibits a natural gradient of strong P limitation in the east which shifts to weak P or even N limitation at the western boundary. This nutrient gradient greatly affects seagrass abundance and productivity across the bay. We assessed the effects of N and P additions on sediment bacterial community structure in relation to the existing nutrient gradient in Florida Bay. Sediment samples from 24 permanent 0.25 m(2) plots in each of six sites across Florida Bay were fertilized with granular N and P in a factorial design for 26 months. Sediment bacterial community structure was analyzed using PCR-denaturing gradient gel electrophoresis (DGGE) analysis of 16S ribosomal RNA (rRNA) genes and a cloning strategy from DGGE bands. The phylogenetic positions of 16S rRNA sequences mostly fell into common members found in marine sediments such as sulfate-reducing Deltaproteobacteria, Gammaproteobacteria, Spirochaetes, and Bacteriodetes. Twenty-eight common DGGE bands were found in all sediment samples; however, some DGGE bands were only found or were better represented in eastern sites. Bacterial community diversity (Shannon-Weiner index) showed similar values throughout all sediment samples. The N treatment had no effect on the bacterial community structures across the bay. Conversely, the addition of P significantly influenced the bacterial community structure at all but the most western site, where P is least limiting due to inputs from the Gulf of Mexico. P additions enhanced DGGE band sequences related to Cytophagales, Ectothiorhodospiraceae, and Desulfobulbaceae, suggesting a shift toward bacterial communities with increased capability to degrade polymeric organic matter. In addition, a band related to Deferribacteres was enhanced in eastern sites. Thus, indigenous environmental conditions were the primary determining factors controlling the bacterial communities, while the addition of P was a secondary determining factor. This P-induced change in community composition tended to be proportional to the amount of P limitation obviated by the nutrient additions.
佛罗里达湾东部存在强烈的磷限制自然梯度,而在西部边界则变为弱磷甚至氮限制。这种营养梯度极大地影响了整个海湾的海草丰度和生产力。我们评估了氮和磷添加对佛罗里达湾现有养分梯度下沉积物细菌群落结构的影响。在佛罗里达湾六个地点的 24 个永久性 0.25 平方米(2)的每个永久点中,用颗粒状氮和磷以因子设计进行了 26 个月的施肥。使用聚合酶链反应-变性梯度凝胶电泳(DGGE)分析 16S 核糖体 RNA(rRNA)基因和从 DGGE 带的克隆策略分析了沉积物细菌群落结构。16S rRNA 序列的系统发育位置大多属于海洋沉积物中常见的成员,如硫酸盐还原菌 Delta 变形菌门、Gamma 变形菌门、螺旋体和拟杆菌门。在所有沉积物样品中都发现了 28 个常见的 DGGE 带;然而,一些 DGGE 带仅在东部地点发现或更好地代表。细菌群落多样性(Shannon-Weiner 指数)在所有沉积物样品中均显示出相似的值。氮处理对整个海湾的细菌群落结构没有影响。相反,除了最西部的站点外,磷的添加显著影响了细菌群落结构,而在最西部的站点,由于墨西哥湾的输入,磷的限制最小。磷的添加增强了与 Cytophagales、Ectothiorhodospiraceae 和 Desulfobulbaceae 相关的 DGGE 带序列,表明细菌群落向具有增加降解聚合物有机物能力的方向转变。此外,在东部站点中,与 Deferribacteres 相关的一个带得到了增强。因此,本土环境条件是控制细菌群落的主要决定因素,而磷的添加是次要决定因素。这种由磷引起的群落组成变化与养分添加消除的磷限制量成正比。