原始磁力毒性在假定巨型古原生态磁力化石中的原始磁力毒性
Ualisson Donardelli Bellon1,2, Wyn Williams2, Ricardo Ivan Ferreira Trindade1
1Department of Geophysics, Institute of Astronomy, Geophysics and Atmospheric Sciences, University of São Paulo, São Paulo 05360020, Brazil.
概括
研究人员在微化石中发现了古老的立方形氧化铁粒. 这些发现表明,这些巨大的磁石化石可能具有导航功能,类似于现代磁力战术细菌.
科学领域:
- 古磁论是古磁论的一种学说.
- 生物矿物化 生物矿物化
- 微生物学 微生物学
背景情况:
- 磁触性细菌为导航创造细胞内磁性晶体 (磁体体).
- 磁石化石是化石磁体,提供了对古代微生物生命的见解.
- 巨型磁石化石比典型的磁石化石大,具有不寻常的形态,但它们的生物起源尚不清楚.
研究的目的:
- 研究巨型磁石化石的生物起源和潜在功能.
- 为了分析前坎布里亚微化石中的氧化铁颗粒的形态.
- 为了确定这些古老的结构是否可以作为导航辅助.
主要方法:
- 图形图形纳米图形学被用来分析1.88亿年前的前坎布里亚纪岩石.
- 重建了嵌入线状微化石中的微米立方体氧化铁粒的形态.
- 进行了微磁模拟,以评估潜在的磁性特性和功能.
主要成果:
- 在有机丝状化石中发现了微米立方体的氧化铁颗粒,与之前描述的巨型磁石化石不同.
- 这些粒的形态和排列表明生物控制的矿物化.
- 微磁模拟支持这些结构的潜在导航功能.
结论:
- 发现的氧化铁颗粒代表了一种新型的巨型磁石化石.
- 它们在线状微化石中的存在和模拟的磁性行为支持生物起源和导航功能.
- 这些发现为古代微生物中磁毒毒的演变提供了洞察力.
相关概念视频
Magnetism
6.3K
Magnets are commonly found in everyday objects, such as toys, hangers, elevators, doorbells, and computer devices. Experimentation on these magnets shows that all magnets have two poles: one is labeled north (N) and the other south (S). Magnetic poles repel if they are alike and attract if unlike. Moreover, both poles of a magnet attract unmagnetized pieces of iron.
An individual magnetic pole cannot be isolated. No matter how small, every piece of a magnet contains a north pole and a south...
An individual magnetic pole cannot be isolated. No matter how small, every piece of a magnet contains a north pole and a south...
6.3K
Potential Due to a Magnetized Object
282
Magnetic dipoles in magnetic materials are aligned when placed under an external magnetic field. For paramagnets and ferromagnets, dipole alignment occurs in the direction of the magnetic field. However, the dipoles align opposite to the field in the case of diamagnets. This state of magnetic polarization due to the external field is called magnetization. Magnetization is defined as the dipole moment per unit volume. It plays a similar role to polarization in electrostatics.
The vector...
The vector...
282
Diamagnetism
2.4K
Materials consisting of paired electrons have zero net magnetic moments. However, when these materials are placed under an external magnetic field, the moments opposite to the field are induced. Such materials are called diamagnets. Diamagnetism is the response of the diamagnets when placed in an external magnetic field.
Diamagnetism was discovered by Anton Brugmans in 1778 when he observed that bismuth gets repelled by magnetic fields, thus theorizing that diamagnets get repelled by magnets....
Diamagnetism was discovered by Anton Brugmans in 1778 when he observed that bismuth gets repelled by magnetic fields, thus theorizing that diamagnets get repelled by magnets....
2.4K
Paramagnetism
2.5K
Paramagnets are materials with unpaired electrons that possess a finite magnetic moment. In the absence of a magnetic field, these moments are randomly oriented, and thus the net moment is zero. Under an external field, a torque acting on the moments tends to align them along the field's direction. However, the random thermal motion of electrons produces a torque opposite to the external field and tries to disorient the moments. These two competing effects align only a few moments along the...
2.5K
Ferromagnetism
2.4K
Materials like iron, nickel, and cobalt consist of magnetic domains, within which the magnetic dipoles are arranged parallel to each other. The magnetic dipoles are rigidly aligned in the same direction within a domain by quantum mechanical coupling among the atoms. This coupling is so strong that even thermal agitation at room temperature cannot break it. The result is that each domain has a net dipole moment. However, some materials have weaker coupling, and are ferromagnetic at lower...
2.4K
Magnetic Field Lines
4.1K
The representation of magnetic fields by magnetic field lines is very useful in visualizing the strength and direction of the magnetic field. Each of the magnetic field lines forms a closed loop. The field lines emerge from the north pole (N), loop around to the south pole (S), and continue through the bar magnet back to the north pole.
Magnetic field lines follow several hard-and-fast rules:
Magnetic field lines follow several hard-and-fast rules:
4.1K


