铁锈色栖息地的反硝化作用对光食性生物有抑制作用

IF 15.7 1区地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY

Nature Geoscience Pub Date : 2024-10-08 DOI:10.1038/s41561-024-01561-8

引用次数: 0

摘要

实验室实验表明，在富铁系统中，反硝化过程中产生的有毒中间产物会抑制铁（II）氧化光养细菌（或称光铁嗜酸菌）的作用，而光铁嗜酸菌被认为是奥陶纪和古新生代铁地层的主要沉积物。这确定了在地球早期历史中影响光铁锈体矿物形成的一个以前被忽视的压力源。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

Photoferrotrophs are inhibited by denitrification in ferruginous habitats

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Photoferrotrophs are inhibited by denitrification in ferruginous habitats

Laboratory experiments show that Fe(II) oxidizing phototrophic bacteria, or photoferrotrophs, thought to be a major depositor of Archean and Palaeoproterozoic iron formations, are inhibited by toxic intermediates produced during denitrification in iron-rich systems. This identifies a previously overlooked stressor impacting mineral formation by photoferrotrophs during early Earth history.

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来源期刊

Nature Geoscience 地学-地球科学综合

CiteScore

26.70

自引率

1.60%

发文量

187

审稿时长

3.3 months

期刊介绍： Nature Geoscience is a monthly interdisciplinary journal that gathers top-tier research spanning Earth Sciences and related fields. The journal covers all geoscience disciplines, including fieldwork, modeling, and theoretical studies. Topics include atmospheric science, biogeochemistry, climate science, geobiology, geochemistry, geoinformatics, remote sensing, geology, geomagnetism, paleomagnetism, geomorphology, geophysics, glaciology, hydrology, limnology, mineralogy, oceanography, paleontology, paleoclimatology, paleoceanography, petrology, planetary science, seismology, space physics, tectonics, and volcanology. Nature Geoscience upholds its commitment to publishing significant, high-quality Earth Sciences research through fair, rapid, and rigorous peer review, overseen by a team of full-time professional editors.