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相关概念视频

The Periodic Table and Organismal Elements00:57

The Periodic Table and Organismal Elements

Elements are the smallest units of matter that cannot be broken down further by chemical processes. There are 118 known elements, but not all of these are naturally-occurring, and fewer still are essential for life. Living matter is composed primarily of carbon, nitrogen, hydrogen, and oxygen, with smaller amounts of other elements like calcium, phosphorus, potassium, and sulfur. Other elements are also necessary for life but only in trace amounts.The Periodic Table Provides Information about...
Metal-Ligand Bonds02:51

Metal-Ligand Bonds

The hemoglobin in the blood, the chlorophyll in green plants, vitamin B-12, and the catalyst used in the manufacture of polyethylene all contain coordination compounds. Ions of the metals, especially the transition metals, are likely to form complexes.
In these complexes, transition metals form coordinate covalent bonds, a kind of Lewis acid-base interaction in which both of the electrons in the bond are contributed by a donor (Lewis base) to an electron acceptor (Lewis acid). The Lewis acid in...
Conserved Binding Sites01:49

Conserved Binding Sites

Many proteins’ biological role depends on their interactions with their ligands, small molecules that bind to specific locations on the protein known as ligand-binding sites. Ligand-binding sites are often conserved among homologous proteins as these sites are critical for protein function.
Binding sites are often located in large pockets, and if their location on a protein’s surface is unknown, it can be predicted using various approaches. The energetic method computationally analyses the...
The Periodic Table and Organismal Elements01:27

The Periodic Table and Organismal Elements

Elements are the smallest units of matter that cannot be broken down further by chemical processes. There are 118 known elements, but not all of these are naturally occurring, and only a few of them are essential for life. Living matter is composed primarily of carbon, nitrogen, hydrogen, and oxygen, with smaller amounts of other elements like calcium, phosphorus, potassium, and sulfur. Other elements are also necessary for life but only in trace amounts.
Periodic Table Provides Information...
Other Unique Bacteria01:18

Other Unique Bacteria

Magnetic bacteria exhibit a directed movement called magnetotaxis, driven by structures called magnetosomes. These magnetosomes consist of chains of magnetic particles made of either magnetite (Fe₃O₄) or greigite (Fe₃S₄) and are organized in a linear conformation by a protein scaffold within invaginations of the cell membrane. The bacteria align along the north–south magnetic field lines, much like a compass needle. They are typically microaerophilic or anaerobic and are commonly found near the...

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相关实验视频

Updated: Jul 11, 2026

Ion Mobility-Mass Spectrometry Techniques for Determining the Structure and Mechanisms of Metal Ion Recognition and Redox Activity of Metal Binding Oligopeptides
11:04

Ion Mobility-Mass Spectrometry Techniques for Determining the Structure and Mechanisms of Metal Ion Recognition and Redox Activity of Metal Binding Oligopeptides

Published on: September 7, 2019

铁同位素生物签名 铁同位素生物签名

B L Beard1, C M Johnson, L Cox

  • 1Department of Geology and Geophysics, University of Wisconsin-Madison, 1215 West Dayton Street, Madison, WI 53706, USA. Laboratory, MS 183-301, 4800 Oak Grove Road, Pasadena, CA 91109-8009, USA. beardb@geology.wisc.edu

Science (New York, N.Y.)
|September 18, 1999
PubMed
概括

沉积岩中的铁同位素变化表明微生物的影响. 这项研究表明,由减少铁的细菌进行生物分化,提供了一种使用铁追踪古老微生物的新方法.

科学领域:

  • 地质化学 地质化学
  • 微生物学 微生物学
  • 同位素地球化学 同位素地球化学

背景情况:

  • 铁同位素比率 ((56) Fe/ ((54) Fe),测量为delta ((56) Fe,在沉积岩中显示出显著的变化 (+0.9到-1.6每毫米).
  • 相比之下,来自地球和月球的火性岩石中的含铁相表现出最小的同位素变化 (delta(56) Fe = 0.0 +/- 0.3 per mil).
  • 这种差异表明,沉积物环境中存在着明显的分化过程.

研究的目的:

  • 研究微生物活动在沉积环境中导致铁同位素分化的作用.
  • 为了确定铁同位素签名是否可以作为地质记录中微生物分布的追踪器.

主要方法:

  • 实验性化不相似的减少铁的细菌 (Shewanella藻类) 用铁基质.
  • 测量铁同位素比率 ((56) Fe / ((54) Fe) 在细菌基质和由此产生的溶解铁.
  • 实验分成与沉积岩和岩石中观察到的自然变异的比较.

主要成果:

  • 实验表明,Shewanella藻类导致了显著的同位素分离,溶解的铁质铁比铁基质轻1.3每毫升 (delta(56) Fe).
  • 这种实验推导的生物制成分离值与在天然沉积岩中观察到的delta (56) Fe值的范围保持一致.
关键词:
美国宇航局中心JPL.美国宇航局的学科是外生态学.

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  • 在火性岩石中缺乏显著的分离,支持沉积体铁同位素变化的生物起源.
  • 结论:

    • 沉积岩中的铁同位素值的广泛范围很可能是减少铁的微生物生物分解的结果.
    • 铁同位素组成作为一个潜在的生物标志物用于追踪微生物在现代和古代地球环境中的存在和活动.
    • 这项研究为使用稳定的铁同位素重建古环境条件和微生物进化开辟了新的途径.