Jayakumar Amal, Chang Bonnie X, Widner Brittany, Bernhardt Peter, Mulholland Margaret R, Ward Bess B
Department of Geosciences, Princeton University, Princeton, NJ, USA.
Joint Institute for the Study of the Atmosphere and Ocean, University of Washington, Seattle, WA, USA.
ISME J. 2017 Oct;11(10):2356-2367. doi: 10.1038/ismej.2017.97. Epub 2017 Jul 25.
Biological nitrogen fixation (BNF) was investigated above and within the oxygen-depleted waters of the oxygen-minimum zone of the Eastern Tropical North Pacific Ocean. BNF rates were estimated using an isotope tracer method that overcame the uncertainty of the conventional bubble method by directly measuring the tracer enrichment during the incubations. Highest rates of BNF (4 nM day) occurred in coastal surface waters and lowest detectable rates (0.2 nM day) were found in the anoxic region of offshore stations. BNF was not detectable in most samples from oxygen-depleted waters. The composition of the N-fixing assemblage was investigated by sequencing of nifH genes. The diazotrophic assemblage in surface waters contained mainly Proteobacterial sequences (Cluster I nifH), while both Proteobacterial sequences and sequences with high identities to those of anaerobic microbes characterized as Clusters III and IV type nifH sequences were found in the anoxic waters. Our results indicate modest input of N through BNF in oxygen-depleted zones mainly due to the activity of proteobacterial diazotrophs.
对东热带北太平洋海洋氧含量最低区域贫氧水体之上及内部的生物固氮作用(BNF)展开了研究。利用同位素示踪法估算BNF速率,该方法通过在培养过程中直接测量示踪剂富集,克服了传统气泡法的不确定性。最高的BNF速率(约4 nM/天)出现在沿海表层水体,而在近海站位的缺氧区域发现了最低可检测速率(约0.2 nM/天)。在大多数来自贫氧水体的样本中未检测到BNF。通过对nifH基因进行测序研究了固氮菌群的组成。表层水体中的固氮菌群主要包含变形菌序列(I类nifH),而在缺氧水体中发现了变形菌序列以及与被归类为III类和IV类nifH序列的厌氧微生物具有高度同源性的序列。我们的研究结果表明,在贫氧区通过BNF输入的氮量适中,这主要归因于变形菌固氮菌的活性。