Max Planck Institute for Marine Microbiology, Microsensor Group, Bremen, Germany ; University of Southern Denmark, Institute of Biology, NordCEE, Odense, Denmark.
PLoS One. 2013 Sep 4;8(9):e73257. doi: 10.1371/journal.pone.0073257. eCollection 2013.
Intracellular nitrate storage allows microorganisms to survive fluctuating nutrient availability and anoxic conditions in aquatic ecosystems. Here we show that diatoms, ubiquitous and highly abundant microalgae, represent major cellular reservoirs of nitrate in an intertidal flat of the German Wadden Sea and are potentially involved in anaerobic nitrate respiration. Intracellular nitrate (ICNO3) was present year-round in the sediment and was spatially and temporally correlated with fucoxanthin, the marker photopigment of diatoms. Pyrosequencing of SSU rRNA genes of all domains of life confirmed that ICNO3 storage was most likely due to diatoms rather than other known nitrate-storing microorganisms (i.e., large sulfur bacteria and the eukaryotic foraminifers and gromiids). Sedimentary ICNO3 concentrations reached up to 22.3 µmol dm(-3) at the sediment surface and decreased with sediment depth to negligible concentrations below 5 cm. Similarly, the ICNO3/fucoxanthin ratio and porewater nitrate (PWNO3) concentrations decreased with sediment depth, suggesting that ICNO3 of diatoms is in equilibrium with PWNO3, but is enriched relative to PWNO3 by 2-3 orders of magnitude. Cell-volume-specific ICNO3 concentrations in a diatom mat covering the sediment surface during spring were estimated at 9.3-46.7 mmol L(-1). Retrieval of 18S rRNA gene sequences related to known nitrate-storing and nitrate-ammonifying diatom species suggested that diatoms in dark and anoxic sediment layers might be involved in anaerobic nitrate respiration. Due to the widespread dominance of diatoms in microphytobenthos, the total nitrate pool in coastal marine sediments may generally be at least two times larger than derived from porewater measurements and partially be recycled to ammonium.
细胞内硝酸盐储存使微生物能够在水生生态系统中波动的养分供应和缺氧条件下生存。在这里,我们表明,硅藻,无处不在且高度丰富的微藻,是德国瓦登海潮间带中硝酸盐的主要细胞储存库,并且可能参与了厌氧硝酸盐呼吸。细胞内硝酸盐(ICNO3)全年存在于沉积物中,并且在空间和时间上与褐藻黄素相关联,褐藻黄素是硅藻的标记光色素。所有生命领域的 SSU rRNA 基因的 pyrosequencing 证实,ICNO3 储存最有可能是由于硅藻而不是其他已知的硝酸盐储存微生物(即大型硫细菌和真核有孔虫和 gromiids)。沉积物中的 ICNO3 浓度在沉积物表面最高可达 22.3 µmol dm(-3),并随沉积物深度的增加而降低至 5 cm 以下可忽略不计的浓度。同样,ICNO3/褐藻黄素比和孔隙水硝酸盐(PWNO3)浓度随沉积物深度的增加而降低,表明硅藻的 ICNO3 与 PWNO3 处于平衡状态,但相对于 PWNO3 富集了 2-3 个数量级。在春季覆盖沉积物表面的硅藻垫中,估计每个硅藻细胞体积的 ICNO3 浓度为 9.3-46.7 mmol L(-1)。检索与已知硝酸盐储存和硝酸盐氨化硅藻种相关的 18S rRNA 基因序列表明,黑暗和缺氧沉积物层中的硅藻可能参与了厌氧硝酸盐呼吸。由于硅藻在微藻底栖生物中广泛占主导地位,沿海海洋沉积物中的总硝酸盐库可能至少比孔隙水测量得出的大两倍,并且部分被回收为铵。