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The Fossil Record02:56

The Fossil Record

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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...
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Nuclear Stability03:18

Nuclear Stability

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Protons and neutrons, collectively called nucleons, are packed together tightly in a nucleus. With a radius of about 10−15 meters, a nucleus is quite small compared to the radius of the entire atom, which is about 10−10 meters. Nuclei are extremely dense compared to bulk matter, averaging 1.8 × 1014 grams per cubic centimeter. If the earth’s density were equal to the average nuclear density, the earth’s radius would be only about 200 meters.
To hold positively...
20.5K
Radioactive Decay and Radiometric Dating02:48

Radioactive Decay and Radiometric Dating

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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.
34.6K
Nuclear Transmutation03:20

Nuclear Transmutation

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Nuclear transmutation is the conversion of one nuclide into another. It can occur by the radioactive decay of a nucleus, or the reaction of a nucleus with another particle. The first manmade nucleus was produced in Ernest Rutherford’s laboratory in 1919 by a transmutation reaction, the bombardment of one type of nuclei with other nuclei or with neutrons. Rutherford bombarded nitrogen-14 atoms with high-speed α particles from a natural radioactive isotope of radium and observed...
12.9K
Diversity of Protists III01:27

Diversity of Protists III

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Rhizaria are a diverse group of unicellular protists characterized by their threadlike cytoplasmic extensions known as pseudopodia. These structures aid in both locomotion and feeding, giving Rhizaria an amoeboid appearance. Their amoeboid morphology once led to taxonomic confusion, but molecular phylogenetics has clarified their evolutionary placement and emphasized their shared use of pseudopodia despite divergent lineages.This clade comprises diverse lineages such as Chlorarachniophyta,...
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Microbial Bioremediation of Uranium01:25

Microbial Bioremediation of Uranium

103
Microorganisms play a critical role in the transformation and immobilization of uranium in contaminated environments through four main pathways: bioreduction, biosorption, bioaccumulation, and biomineralization. These mechanisms reduce uranium’s toxicity and prevent its migration through groundwater systems, offering sustainable approaches for in situ bioremediation.Bioreduction of UraniumBioreduction is driven by anaerobic bacteria such as certain strains of Geobacter and Shewanella,...
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Updated: May 2, 2026

Speciation and Bioavailability Measurements of Environmental Plutonium Using Diffusion in Thin Films
12:22

Speciation and Bioavailability Measurements of Environmental Plutonium Using Diffusion in Thin Films

Published on: November 9, 2015

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在古代石中发现的已灭绝的244Pu.

Grenville Turner1, T Mark Harrison, Greg Holland

  • 1Department of Earth Sciences, University of Manchester, Manchester M13 9PL, UK. grenville.turner@man.ac.uk

Science (New York, N.Y.)
|October 2, 2004
PubMed
概括

古老的石含有-244衰变的证据,为早期地球条件提供了洞察力. 这一发现有助于确定变态事件的日期,并比较行星与的比率.

科学领域:

  • 地质化学 地质化学
  • 同位素地球化学 同位素地球化学
  • 行星科学 行星科学

背景情况:

  • 来自澳大利亚西部杰克山 (Jack Hills) 的detrital石是古老的地质样本.
  • -244 (Pu) 的半衰期很短 (8200万年),在地球历史上很早就已经灭绝了.
  • 裂变性异同位素可以作为已灭绝的放射性核素的衰变证据.

研究的目的:

  • 在古老的石中找到-244在现场衰变的证据.
  • 利用这些发现来确定古代变形事件的年代.
  • 为了确定陆地/ (Pu/U) 的比率,与太阳系值进行比较.

主要方法:

  • 对41亿至42亿年前的单个石进行分析.
  • 检测裂变性异同位素作为衰变的指标.

主要成果:

  • 在古老的石中发现了-244在现场衰变的证据.
  • 分析的石的年代介于41亿至42亿年前.
  • -244在地球形成的6亿年内就会灭绝.

结论:

  • 古代石是研究已灭绝的放射性核素的宝贵档案.

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  • -244的衰变产品的存在使得早期地球变态事件的约会成为可能.
  • 这项研究提供了一种方法来确定早期的陆地Pu/U比率,使得与外星值进行比较.