相关实验视频
Updated: Feb 10, 2026
02:31
Phase Transitions and Effect of Intermolecular Forces
23.3K
在加拿大拉布拉多的3.95亿年前沉积岩中发现了早期生命的痕迹
Takayuki Tashiro1, Akizumi Ishida2,3, Masako Hori2,4
1Department of Earth Science and Astronomy, Graduate School of Arts and Sciences, The University of Tokyo, Tokyo 153-8902, Japan.
Nature
|September 30, 2017
概括
研究人员在岩石中发现了最古老的生命证据, 拉布拉多的这一发现为地球的早期生命提供了新的洞察力,
科学领域:
- 地质化学
- 天体生物学
- 地球的早期状况
背景情况:
- 对于了解生命的起源,研究古岩石至关重要.
- 生物石墨是生命早期的一个关键指标,
研究的目的:
- 在拉布拉多北部古老的岩石中研究石墨和碳酸盐的碳同位素组成.
- 确定这些岩石是否包含早期生命的证据.
主要方法:
- 分析总有机碳含量
- 在石墨和碳酸盐中测量碳同位素值 (δ13Corg和 δ13Ccarb).
- 对石墨结晶温度和变形条件的评估.
主要成果:
- 在一些皮质岩石中发现了低的δ13Corg值,低至-28.2.
- 石墨结晶温度与宿主岩石的变态温度一致,排除了以后的污染.
- 13值与变态等级之间的相关性表明了变态前的生物起源.
结论:
- 在δ13Ccarb和δ13Corg之间有显著的分化 (高达25‰),表明有机体的最古老证据,早于39.5亿年.
- 发现的生物石墨可以对早期生命进行详细的地化学研究.
- 这一发现对了解地球上早期生命和外星生命的潜力有意义.
相关概念视频
Phase Transitions
23.3K
Whether solid, liquid, or gas, a substance's state depends on the order and arrangement of its particles (atoms, molecules, or ions). Particles in the solid pack closely together, generally in a pattern. The particles vibrate about their fixed positions but do not move or squeeze past their neighbors. In liquids, although the particles are closely spaced, they are randomly arranged. The position of the particles are not fixed—that is, they are free to move past their neighbors to...
23.3K
Properties of Transition Metals
30.0K
Transition metals are defined as those elements that have partially filled d orbitals. As shown in Figure 1, the d-block elements in groups 3–12 are transition elements. The f-block elements, also called inner transition metals (the lanthanides and actinides), also meet this criterion because the d orbital is partially occupied before the f orbitals.
30.0K
Cooperative Allosteric Transitions
8.8K
Cooperative allosteric transitions can occur in multimeric proteins, where each subunit of the protein has its own ligand-binding site. When a ligand binds to any of these subunits, it triggers a conformational change that affects the binding sites in the other subunits; this can change the affinity of the other sites for their respective ligands. The ability of the protein to change the shape of its binding site is attributed to the presence of a mix of flexible and stable segments in the...
8.8K
Phase Transitions: Vaporization and Condensation
21.5K
The physical form of a substance changes on changing its temperature. For example, raising the temperature of a liquid causes the liquid to vaporize (convert into vapor). The process is called vaporization—a surface phenomenon. Vaporization occurs when the thermal motion of the molecules overcome the intermolecular forces, and the molecules (at the surface) escape into the gaseous state. When a liquid vaporizes in a closed container, gas molecules cannot escape. As these gas phase molecules...
21.5K
Phase Transitions: Sublimation and Deposition
20.3K
Some solids can transition directly into the gaseous state, bypassing the liquid state, via a process known as sublimation. At room temperature and standard pressure, a piece of dry ice (solid CO2) sublimes, appearing to gradually disappear without ever forming any liquid. Snow and ice sublimate at temperatures below the melting point of water, a slow process that may be accelerated by winds and the reduced atmospheric pressures at high altitudes. When solid iodine is warmed, the solid sublimes...
20.3K
Phase Transitions: Melting and Freezing
15.2K
Heating a crystalline solid increases the average energy of its atoms, molecules, or ions, and the solid gets hotter. At some point, the added energy becomes large enough to partially overcome the forces holding the molecules or ions of the solid in their fixed positions, and the solid begins the process of transitioning to the liquid state or melting. At this point, the temperature of the solid stops rising, despite the continual input of heat, and it remains constant until all of the solid is...
15.2K