一个放射测量时间表挑战了标志性的1992年古利亚冰芯的时间表
Shugui Hou1,2, Theo M Jenk3,4, Wei Jiang5,6
1School of Oceanography, Shanghai Jiao Tong University, Shanghai 200240, China.
Science advances
|September 12, 2025
概括
古利亚冰芯的冰芯.
科学领域:
- 古气候学 古气候学
- 冰川学的冰川学
- 地质时间学 (Geochronology)
背景情况:
- 据信,来自西藏的古利亚冰芯 (GP1992) 代表了76万年的气候历史.
- 这一时间尺度使其成为全球第二古老的冰芯和最古老的极外冰芯.
研究的目的:
- 重新评估古利亚冰核记录的时间表.
- 解决GP1992时间表与其他区域古气候数据之间的差异.
主要方法:
- 约会一个新的古利亚冰芯 (GP2021),在原始地点附近进行钻探.
- 使用放射测年技术,包括-210 (210Pb),-39 (39Ar) 和碳-14 (14C).
主要成果:
- GP2021核心揭示了在175.1米深处不到3000年的年龄.
- 这与之前估计的GP1992核心同等深度的约10万年形成鲜明对比.
- 放射测年法证实了古利亚冰记录下方部分的修订后的年龄,年龄要小得多.
结论:
- 之前为GP1992古利亚冰芯分配的时间表被大大高估了.
- 古利亚冰芯的修订日期为西藏高原气候历史提供了新的见解.
- 与其他区域古气候记录的差异通过新的约会来解决.
相关概念视频
Global Climate Change
28.7K
Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
28.7K
Radioactive Decay and Radiometric Dating
36.9K
Radioactivity is a spontaneous disintegration of an unstable nuclide and is a random process, as all the nuclei in the sample do not decay simultaneously. The number of disintegrations per unit time is called the activity (A), which is directly proportional to the number of nuclei in the sample. The decay constant (λ) is an average probability of decay per nucleus in unit time.
36.9K
The Fossil Record
27.1K
The fossil record documents only a small fraction of all organisms that have ever inhabited Earth. Fossilization is a rare process, and most organisms never become fossils. Moreover, the fossil record only exhibits fossils that have been discovered. Nevertheless, sedimentary rock fossils of long-lived, abundant, hard-bodied organisms dominate the fossil record. These fossils offer valuable information, such as an organism's physical form, behavior, and age. Studying the fossil record helps...
27.1K
Isothermal Processes
4.9K
A thermodynamic process that occurs at constant temperature is called an isothermal process. Heat slowly flows into the system or out of the system to maintain thermal equilibrium. Processes involving phase changes like water evaporation into steam or freezing water into ice at a constant temperature are examples of Isothermal Processes.
An ideal gas can also undergo isothermal expansion or compression.
For example, consider 1 mole of an ideal gas inside an isolated cylinder at initial volume V...
An ideal gas can also undergo isothermal expansion or compression.
For example, consider 1 mole of an ideal gas inside an isolated cylinder at initial volume V...
4.9K
Biological Clocks and Seasonal Responses
41.5K
The circadian—or biological—clock is an intrinsic, timekeeping, molecular mechanism that allows plants to coordinate physiological activities over 24-hour cycles called circadian rhythms. Photoperiodism is a collective term for the biological responses of plants to variations in the relative lengths of dark and light periods. The period of light-exposure is called the photoperiod.
41.5K
The Carbon Cycle
43.2K
Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
43.2K


