Jove
Visualize
Contact Us

Related Concept Videos

Oxidation and Reduction of Organic Molecules01:19

Oxidation and Reduction of Organic Molecules

5.9K
Energy production within a cell involves many coordinated chemical pathways. Most of these pathways are combinations of oxidation and reduction reactions, which occur at the same time. An oxidation reaction strips an electron from an atom in a compound, and the addition of this electron to another compound is a reduction reaction. Because oxidation and reduction usually occur together, these pairs of reactions are called redox reactions.
The removal of an electron from a molecule, results in a...
5.9K
Radical Autoxidation01:20

Radical Autoxidation

2.1K
The oxidation of an organic compound in the presence of air or oxygen is called autoxidation. For example, cumene reacts with oxygen to form hydroperoxide. Autoxidation involves initiation, propagation, and termination steps. Many organic compounds are susceptible to autoxidation—especially ethers in the presence of oxygen, which form hydroperoxides. Even though this reaction is slow, old ether bottles contain small amounts of peroxide, which leads to laboratory explosions during ether...
2.1K
Oxidation of Alkenes: Syn Dihydroxylation with Osmium Tetraoxide02:44

Oxidation of Alkenes: Syn Dihydroxylation with Osmium Tetraoxide

9.6K
Alkenes are converted to 1,2-diols or glycols through a process called dihydroxylation. It involves the addition of two hydroxyl groups across the double bond with two different stereochemical approaches, namely anti and syn. Dihydroxylation using osmium tetroxide progresses with syn stereochemistry.
9.6K
Oxidative Cleavage of Alkenes: Ozonolysis01:46

Oxidative Cleavage of Alkenes: Ozonolysis

9.7K
In ozonolysis, ozone is used to cleave a carbon–carbon double bond to form aldehydes and ketones, or carboxylic acids, depending on the work-up.
Ozone is a symmetrical bent molecule stabilized by a resonance structure.
9.7K
Alkynes to Carboxylic Acids: Oxidative Cleavage02:01

Alkynes to Carboxylic Acids: Oxidative Cleavage

4.8K
Alkynes undergo oxidative cleavage in the presence of oxidizing reagents like potassium permanganate and ozone. The triple bond — one σ bond and two π bonds — is completely cleaved, and the alkyne is oxidized to carboxylic acids. When warm and basic aqueous potassium permanganate is used as an oxidizing agent, alkynes are first converted to carboxylate salts via an unstable α-diketone intermediate. Further, a mild acid treatment protonates the carboxylate anions...
4.8K
Oxidation of Alkenes: Syn Dihydroxylation with Potassium Permanganate02:21

Oxidation of Alkenes: Syn Dihydroxylation with Potassium Permanganate

10.4K
Alkenes can be dihydroxylated using potassium permanganate.  The method encompasses the reaction of an alkene with a cold, dilute solution of potassium permanganate under basic conditions to form a cis-diol along with a brown precipitate of manganese dioxide.
10.4K
JoVE
x logofacebook logolinkedin logoyoutube logo
ABOUT JoVE
OverviewLeadershipBlogJoVE Help Center
AUTHORS
Publishing ProcessEditorial BoardScope & PoliciesPeer ReviewFAQSubmit
LIBRARIANS
TestimonialsSubscriptionsAccessResourcesLibrary Advisory BoardFAQ
RESEARCH
JoVE JournalMethods CollectionsJoVE Encyclopedia of ExperimentsArchive
EDUCATION
JoVE CoreJoVE BusinessJoVE Science EducationJoVE Lab ManualFaculty Resource CenterFaculty Site
Terms & Conditions of Use
Privacy Policy
Policies
  1. Home
  2. Impact-driven Oxidation Of Organics Explains Chondrite Shock Metamorphism Dichotomy.
  1. Home
  2. Impact-driven Oxidation Of Organics Explains Chondrite Shock Metamorphism Dichotomy.

Related Experiment Video

An Experimental Protocol for Studying Mineral Effects on Organic Hydrothermal Transformations
06:50

An Experimental Protocol for Studying Mineral Effects on Organic Hydrothermal Transformations

Published on: August 8, 2018

5.6K

Impact-driven oxidation of organics explains chondrite shock metamorphism dichotomy.

Kosuke Kurosawa1,2, Gareth S Collins3, Thomas M Davison3

  • 1Department of Human Environmental Science, Graduate School of Human Development and Environment, Kobe University, Nada-ku, Kobe, Hyogo, Japan. kosuke.kurosawa@people.kobe-u.ac.jp.

Nature Communications
|April 24, 2025

View abstract on PubMed

Summary
This summary is machine-generated.

Shocked meteorites reveal early Solar System dynamics. Impact oxidation of carbonaceous chondrite organics explains their lower shock levels, with Ceres retaining evidence of ancient impacts.

More Related Videos

Single-throughput Complementary High-resolution Analytical Techniques for Characterizing Complex Natural Organic Matter Mixtures
09:38

Single-throughput Complementary High-resolution Analytical Techniques for Characterizing Complex Natural Organic Matter Mixtures

Published on: January 7, 2019

8.5K
Improving Infrared Spectroscopy Characterization of Soil Organic Matter with Spectral Subtractions
08:57

Improving Infrared Spectroscopy Characterization of Soil Organic Matter with Spectral Subtractions

Published on: January 10, 2019

12.3K

Related Experiment Videos

An Experimental Protocol for Studying Mineral Effects on Organic Hydrothermal Transformations
06:50

An Experimental Protocol for Studying Mineral Effects on Organic Hydrothermal Transformations

Published on: August 8, 2018

5.6K
Single-throughput Complementary High-resolution Analytical Techniques for Characterizing Complex Natural Organic Matter Mixtures
09:38

Single-throughput Complementary High-resolution Analytical Techniques for Characterizing Complex Natural Organic Matter Mixtures

Published on: January 7, 2019

8.5K
Improving Infrared Spectroscopy Characterization of Soil Organic Matter with Spectral Subtractions
08:57

Improving Infrared Spectroscopy Characterization of Soil Organic Matter with Spectral Subtractions

Published on: January 10, 2019

12.3K

Area of Science:

  • Planetary Science
  • Cosmochemistry
  • Impact Cratering

Background:

  • Shocked meteorites offer insights into early Solar System conditions.
  • Carbonaceous chondrites exhibit lower shock metamorphism than ordinary chondrites, irrespective of aqueous alteration.

Purpose of the Study:

  • To investigate the cause of the shock metamorphic dichotomy between carbonaceous and ordinary chondrites.
  • To understand the role of impact processes in preserving or erasing shock evidence in meteorites.

Main Methods:

  • Conducting impact experiments using chondrite matrix analogs at velocities of 3-7 km/s.
  • Analyzing experimental products for evidence of heating and chemical changes.
  • Modeling impact outcomes on chondrite parent bodies of varying sizes.

Main Results:

  • Impact experiments showed local matrix heating up to ~2000 K.
  • Impacts on carbonaceous chondrites trigger explosive release of CO and/or CO2, mitigating shock evidence.
  • Highly shocked materials are ejected from smaller parent bodies but retained on larger bodies like Ceres.

Conclusions:

  • The shock metamorphic difference is attributed to impact-driven oxidation of abundant organics in carbonaceous chondrites.
  • Ceres' gravity preserves ancient impact records, making its surface a unique witness plate for early Solar System impact environments.