Clay mineral-organic matter relationships in the early solar system

Physics

Scientific paper

Rate now

  [ 0.00 ] – not rated yet Voters 0   Comments 0

Details

25

Scientific paper

As the solar system formed, it inherited and perpetuated a rich organic chemistry, the molecular products of which are preserved in ancient extraterrestrial objects such as carbonaceous chondrites. These organic-rich meteorites provide a valuable and tangible record of the chemical steps taken towards the origin of life in the early solar system. Chondritic organic matter is present in the inorganic meteorite matrix which, in the CM and CI chondrites, contains evidence of alteration by liquid water on the parent asteroid. An unanswered and fundamental question is to what extent did the organic matter and inorganic products of aqueous alteration interact or display interdependence? We have used an organic labelling technique to reveal that the meteoritic organic matter is strongly associated with clay minerals. This association suggests that clay minerals may have had an important trapping and possibly catalytic role in chemical evolution in the early solar system prior to the origin of life on the early Earth.

No associations

LandOfFree

Say what you really think

Search LandOfFree.com for scientists and scientific papers. Rate them and share your experience with other people.

Rating

Clay mineral-organic matter relationships in the early solar system does not yet have a rating. At this time, there are no reviews or comments for this scientific paper.

If you have personal experience with Clay mineral-organic matter relationships in the early solar system, we encourage you to share that experience with our LandOfFree.com community. Your opinion is very important and Clay mineral-organic matter relationships in the early solar system will most certainly appreciate the feedback.

Rate now

     

Profile ID: LFWR-SCP-O-968008

  Search
All data on this website is collected from public sources. Our data reflects the most accurate information available at the time of publication.