Hydrous-Carbonaceous Meteoroids in the Hadean Aeon

International audience Meteoroids ˜50-200 μm in size represent the dominant mass fraction of extraterrestrial material accreted by the Earth today. About 20% of them survive as unmelted micrometeorites upon atmospheric entry, and they can be recovered from Antarctica ices and snows. Around 99% of th...

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Main Author: Maurette, M.
Other Authors: Centre de Spectrométrie Nucléaire et de Spectrométrie de Masse (CSNSM), Université Paris-Sud - Paris 11 (UP11)-Institut National de Physique Nucléaire et de Physique des Particules du CNRS (IN2P3)-Centre National de la Recherche Scientifique (CNRS)
Format: Conference Object
Language:English
Published: HAL CCSD 2008
Subjects:
Online Access:https://hal.in2p3.fr/in2p3-00681452
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spelling ftccsdartic:oai:HAL:in2p3-00681452v1 2023-07-23T04:13:58+02:00 Hydrous-Carbonaceous Meteoroids in the Hadean Aeon Maurette, M. Centre de Spectrométrie Nucléaire et de Spectrométrie de Masse (CSNSM) Université Paris-Sud - Paris 11 (UP11)-Institut National de Physique Nucléaire et de Physique des Particules du CNRS (IN2P3)-Centre National de la Recherche Scientifique (CNRS) Heidelberg, Germany 2008-09-08 https://hal.in2p3.fr/in2p3-00681452 en eng HAL CCSD in2p3-00681452 https://hal.in2p3.fr/in2p3-00681452 BIBCODE: 2009ASPC.414.137M Astronomical Society of the Pacific Conference Series International Conference Cosmic Dust Near and Far https://hal.in2p3.fr/in2p3-00681452 International Conference Cosmic Dust Near and Far, Sep 2008, Heidelberg, Germany. pp.137 MICROMETEORITES XENOLITHS ORIGIN MANTLE EARTH NEON [PHYS.ASTR.EP]Physics [physics]/Astrophysics [astro-ph]/Earth and Planetary Astrophysics [astro-ph.EP] [SDU.ASTR.EP]Sciences of the Universe [physics]/Astrophysics [astro-ph]/Earth and Planetary Astrophysics [astro-ph.EP] info:eu-repo/semantics/conferenceObject Conference papers 2008 ftccsdartic 2023-07-01T22:37:39Z International audience Meteoroids ˜50-200 μm in size represent the dominant mass fraction of extraterrestrial material accreted by the Earth today. About 20% of them survive as unmelted micrometeorites upon atmospheric entry, and they can be recovered from Antarctica ices and snows. Around 99% of them are related to the rare group of the most volatile-rich chondrites (˜2.5% of the meteorite falls), dominantly composed of a primitive hydrous-carbonaceous material. Micrometeorites contain a mixture of volatiles showing an elemental composition and a water isotopic composition very similar to the corresponding values measured in the contemporary Earth's atmosphere. This surprising micrometeoritic "purity" of the Earth's atmosphere led to an accretion equation to compute the total amount of any meteoroid species accreted by the Earth, during the first ˜100-200 Ma of the post-lunar period of the Early Heavy Bombardment of the solar system, when the mass flux of meteoroids was about one million times higher than today. This equation allows using micrometeorites and other meteoroid "ashes" as tracers of early planetary processes, including: the formation of the atmospheres of the Earth and Mars; the functioning of the Earth's mantle, and; the formation of the prebiotic "soups" and benign climatic conditions required for the birth of life. Conference Object Antarc* Antarctica Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe)
institution Open Polar
collection Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe)
op_collection_id ftccsdartic
language English
topic MICROMETEORITES
XENOLITHS
ORIGIN
MANTLE
EARTH
NEON
[PHYS.ASTR.EP]Physics [physics]/Astrophysics [astro-ph]/Earth and Planetary Astrophysics [astro-ph.EP]
[SDU.ASTR.EP]Sciences of the Universe [physics]/Astrophysics [astro-ph]/Earth and Planetary Astrophysics [astro-ph.EP]
spellingShingle MICROMETEORITES
XENOLITHS
ORIGIN
MANTLE
EARTH
NEON
[PHYS.ASTR.EP]Physics [physics]/Astrophysics [astro-ph]/Earth and Planetary Astrophysics [astro-ph.EP]
[SDU.ASTR.EP]Sciences of the Universe [physics]/Astrophysics [astro-ph]/Earth and Planetary Astrophysics [astro-ph.EP]
Maurette, M.
Hydrous-Carbonaceous Meteoroids in the Hadean Aeon
topic_facet MICROMETEORITES
XENOLITHS
ORIGIN
MANTLE
EARTH
NEON
[PHYS.ASTR.EP]Physics [physics]/Astrophysics [astro-ph]/Earth and Planetary Astrophysics [astro-ph.EP]
[SDU.ASTR.EP]Sciences of the Universe [physics]/Astrophysics [astro-ph]/Earth and Planetary Astrophysics [astro-ph.EP]
description International audience Meteoroids ˜50-200 μm in size represent the dominant mass fraction of extraterrestrial material accreted by the Earth today. About 20% of them survive as unmelted micrometeorites upon atmospheric entry, and they can be recovered from Antarctica ices and snows. Around 99% of them are related to the rare group of the most volatile-rich chondrites (˜2.5% of the meteorite falls), dominantly composed of a primitive hydrous-carbonaceous material. Micrometeorites contain a mixture of volatiles showing an elemental composition and a water isotopic composition very similar to the corresponding values measured in the contemporary Earth's atmosphere. This surprising micrometeoritic "purity" of the Earth's atmosphere led to an accretion equation to compute the total amount of any meteoroid species accreted by the Earth, during the first ˜100-200 Ma of the post-lunar period of the Early Heavy Bombardment of the solar system, when the mass flux of meteoroids was about one million times higher than today. This equation allows using micrometeorites and other meteoroid "ashes" as tracers of early planetary processes, including: the formation of the atmospheres of the Earth and Mars; the functioning of the Earth's mantle, and; the formation of the prebiotic "soups" and benign climatic conditions required for the birth of life.
author2 Centre de Spectrométrie Nucléaire et de Spectrométrie de Masse (CSNSM)
Université Paris-Sud - Paris 11 (UP11)-Institut National de Physique Nucléaire et de Physique des Particules du CNRS (IN2P3)-Centre National de la Recherche Scientifique (CNRS)
format Conference Object
author Maurette, M.
author_facet Maurette, M.
author_sort Maurette, M.
title Hydrous-Carbonaceous Meteoroids in the Hadean Aeon
title_short Hydrous-Carbonaceous Meteoroids in the Hadean Aeon
title_full Hydrous-Carbonaceous Meteoroids in the Hadean Aeon
title_fullStr Hydrous-Carbonaceous Meteoroids in the Hadean Aeon
title_full_unstemmed Hydrous-Carbonaceous Meteoroids in the Hadean Aeon
title_sort hydrous-carbonaceous meteoroids in the hadean aeon
publisher HAL CCSD
publishDate 2008
url https://hal.in2p3.fr/in2p3-00681452
op_coverage Heidelberg, Germany
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_source Astronomical Society of the Pacific Conference Series
International Conference Cosmic Dust Near and Far
https://hal.in2p3.fr/in2p3-00681452
International Conference Cosmic Dust Near and Far, Sep 2008, Heidelberg, Germany. pp.137
op_relation in2p3-00681452
https://hal.in2p3.fr/in2p3-00681452
BIBCODE: 2009ASPC.414.137M
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