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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

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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.
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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.
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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...
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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

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

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El extinto 244Pu en antiguos zircones.

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
Resumen
Este resumen es generado por máquina.

Los circones antiguos contienen evidencia de desintegración del plutonio-244, ofreciendo información sobre las condiciones de la Tierra temprana. Este descubrimiento ayuda a datar los eventos metamórficos y a comparar las proporciones planetarias de plutonio y uranio.

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Área de la Ciencia:

  • La geoquímica es la geoquímica.
  • La geoquímica de los isótopos es la geoquímica de los isótopos.
  • Ciencias planetarias Ciencias planetarias.

Sus antecedentes:

  • Los zircones de detrital de Jack Hills, Australia Occidental, son muestras geológicas antiguas.
  • El plutonio-244 (Pu) tiene una vida media corta (82 millones de años) y se habría extinguido temprano en la historia de la Tierra.
  • Los isótopos de xenón fisiogénicos pueden servir como evidencia de la desintegración de los radionúclidos extintos.

Objetivo del estudio:

  • Para encontrar evidencia de la desintegración in situ del plutonio-244 en antiguos zircones.
  • Para usar estos hallazgos para fechar antiguos eventos metamórficos.
  • Para determinar la relación plutonio/uranio (Pu/U) terrestre para su comparación con los valores del sistema solar.

Principales métodos:

  • Análisis de zircones individuales de entre 4.100 y 4.200 millones de años.
  • Detección de isótopos de xenón fisiogénicos como indicadores de la desintegración del plutonio.

Principales resultados:

  • La evidencia de la descomposición in situ del plutonio-244 fue encontrada en antiguos zircones.
  • Los zircones analizados datan de entre 4.100 y 4.200 millones de años.
  • El plutonio-244 se habría extinguido dentro de los 600 millones de años de la formación de la Tierra.

Conclusiones:

  • Los circones antiguos son archivos valiosos para el estudio de radionúclidos extintos.
  • La presencia de productos de desintegración del plutonio-244 permite la datación de los primeros eventos metamórficos de la Tierra.
  • Esta investigación proporciona un método para determinar la relación Pu/U terrestre temprana, lo que permite la comparación con los valores extraterrestres.