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对从洛伊希海山暴露的海底玄武岩进行测量的细胞外酶活性和微生物多样性表明了玄武岩对全球生物地球化学循环的重要性。

Extracellular enzyme activity and microbial diversity measured on seafloor exposed basalts from Loihi seamount indicate the importance of basalts to global biogeochemical cycling.

作者信息

Jacobson Meyers Myrna E, Sylvan Jason B, Edwards Katrina J

机构信息

Department of Biological Sciences, University of Southern California, Los Angeles, California, USA

Department of Biological Sciences, University of Southern California, Los Angeles, California, USA.

出版信息

Appl Environ Microbiol. 2014 Aug;80(16):4854-64. doi: 10.1128/AEM.01038-14. Epub 2014 Jun 6.

Abstract

Seafloor basalts are widely distributed and host diverse prokaryotic communities, but no data exist concerning the metabolic rates of the resident microbial communities. We present here potential extracellular enzyme activities of leucine aminopeptidase (LAP) and alkaline phosphatase (AP) measured on basalt samples from different locations on Loihi Seamount, HI, coupled with analysis of prokaryotic biomass and pyrosequencing of the bacterial 16S rRNA gene. The community maximum potential enzyme activity (Vmax) of LAP ranged from 0.47 to 0.90 nmol (g rock)(-1) h(-1); the Vmax for AP was 28 to 60 nmol (g rock)(-1) h(-1). The Km of LAP ranged from 26 to 33 μM, while the Km for AP was 2 to 7 μM. Bacterial communities on Loihi basalts were comprised primarily of Alpha-, Delta-, andGammaproteobacteria, Bacteroidetes, and Planctomycetes. The putative ability to produce LAP is evenly distributed across the most commonly detected bacterial orders, but the ability to produce AP is likely dominated by bacteria in the orders Xanthomonadales, Flavobacteriales, and Planctomycetales. The enzyme activities on Loihi basalts were compared to those of other marine environments that have been studied and were found to be similar in magnitude to those from continental shelf sediments and orders of magnitude higher than any measured in the water column, demonstrating that the potential for exposed basalts to transform organic matter is substantial. We propose that microbial communities on basaltic rock play a significant, quantifiable role in benthic biogeochemical processes.

摘要

海底玄武岩分布广泛,承载着多样的原核生物群落,但目前尚无关于这些驻留微生物群落代谢率的数据。我们在此展示了对来自夏威夷罗伊希海山不同位置玄武岩样本测得的亮氨酸氨肽酶(LAP)和碱性磷酸酶(AP)的潜在胞外酶活性,同时结合了原核生物量分析以及细菌16S rRNA基因的焦磷酸测序。LAP的群落最大潜在酶活性(Vmax)范围为0.47至0.90 nmol(g岩石)⁻¹ h⁻¹;AP的Vmax为28至60 nmol(g岩石)⁻¹ h⁻¹。LAP的米氏常数(Km)范围为26至33 μM,而AP的Km为2至7 μM。罗伊希玄武岩上的细菌群落主要由α-、δ-和γ-变形菌纲、拟杆菌门和浮霉菌门组成。推测产生LAP的能力在最常检测到的细菌目中分布均匀,但产生AP的能力可能主要由黄单胞菌目、黄杆菌目和浮霉菌目中的细菌主导。将罗伊希玄武岩上的酶活性与其他已研究的海洋环境进行比较,发现其活性大小与大陆架沉积物相似,且比水柱中测得的任何活性高几个数量级,这表明暴露玄武岩转化有机物的潜力很大。我们认为玄武岩岩石上的微生物群落在底栖生物地球化学过程中发挥着重要且可量化的作用。

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