Fine-grained precursors dominate the micrometeorite flux

We optically classified 5682 micrometeorites (MMs) from the 2000 South Pole collection into textural classes, imaged 2458 of these MMs with a scanning electron microscope, and made 200 elemental and eight isotopic measurements on those with unusual textures or relict phases. As textures provide info...

Full description

Bibliographic Details
Published in:Meteoritics & Planetary Science
Main Authors: Taylor, Susan, Matrajt, Graciela, Guan, Yunbin
Format: Article in Journal/Newspaper
Language:unknown
Published: Meteoritical Society 2012
Subjects:
Online Access:https://doi.org/10.1111/j.1945-5100.2011.01292.x
id ftcaltechauth:oai:authors.library.caltech.edu:satvk-2tx50
record_format openpolar
spelling ftcaltechauth:oai:authors.library.caltech.edu:satvk-2tx50 2024-09-15T18:36:54+00:00 Fine-grained precursors dominate the micrometeorite flux Taylor, Susan Matrajt, Graciela Guan, Yunbin 2012-04 https://doi.org/10.1111/j.1945-5100.2011.01292.x unknown Meteoritical Society https://doi.org/10.1111/j.1945-5100.2011.01292.x oai:authors.library.caltech.edu:satvk-2tx50 eprintid:31620 resolverid:CaltechAUTHORS:20120523-143303420 info:eu-repo/semantics/openAccess Other Meteoritics and Planetary Science, 47(4), 550-564, (2012-04) info:eu-repo/semantics/article 2012 ftcaltechauth https://doi.org/10.1111/j.1945-5100.2011.01292.x 2024-08-06T15:34:59Z We optically classified 5682 micrometeorites (MMs) from the 2000 South Pole collection into textural classes, imaged 2458 of these MMs with a scanning electron microscope, and made 200 elemental and eight isotopic measurements on those with unusual textures or relict phases. As textures provide information on both degree of heating and composition of MMs, we developed textural sequences that illustrate how fine-grained, coarse-grained, and single mineral MMs change with increased heating. We used this information to determine the percentage of matrix dominated to mineral dominated precursor materials (precursors) that produced the MMs. We find that at least 75% of the MMs in the collection derived from fine-grained precursors with compositions similar to CI and CM meteorites and consistent with dynamical models that indicate 85% of the mass influx of small particles to Earth comes from Jupiter family comets. A lower limit for ordinary chondrites is estimated at 2–8% based on MMs that contain Na-bearing plagioclase relicts. Less than 1% of the MMs have achondritic compositions, CAI components, or recognizable chondrules. Single mineral MMs often have magnetite zones around their peripheries. We measured their isotopic compositions to determine if the magnetite zones demarcate the volume affected by atmospheric exchange during entry heating. Because we see little gradient in isotopic composition in the olivines, we conclude that the magnetites are a visual marker that allows us to select and analyze areas not affected by atmospheric exchange. Similar magnetite zones are seen in some olivine and pyroxene relict grains contained within MMs. © 2011 The Meteoritical Society. Issue published online: 26 April 2012; Article first published online: 2 November 2011; Received 15 May 2011; revision accepted 22 September 2011. The authors thank Dave Joswiak and Dr. Hope Ishii for reviewing this article and providing many helpful suggestions. Dr. Gregory Herzog is thanked for the many helpful discussions on this work. We ... Article in Journal/Newspaper South pole Caltech Authors (California Institute of Technology) Meteoritics & Planetary Science 47 4 550 564
institution Open Polar
collection Caltech Authors (California Institute of Technology)
op_collection_id ftcaltechauth
language unknown
description We optically classified 5682 micrometeorites (MMs) from the 2000 South Pole collection into textural classes, imaged 2458 of these MMs with a scanning electron microscope, and made 200 elemental and eight isotopic measurements on those with unusual textures or relict phases. As textures provide information on both degree of heating and composition of MMs, we developed textural sequences that illustrate how fine-grained, coarse-grained, and single mineral MMs change with increased heating. We used this information to determine the percentage of matrix dominated to mineral dominated precursor materials (precursors) that produced the MMs. We find that at least 75% of the MMs in the collection derived from fine-grained precursors with compositions similar to CI and CM meteorites and consistent with dynamical models that indicate 85% of the mass influx of small particles to Earth comes from Jupiter family comets. A lower limit for ordinary chondrites is estimated at 2–8% based on MMs that contain Na-bearing plagioclase relicts. Less than 1% of the MMs have achondritic compositions, CAI components, or recognizable chondrules. Single mineral MMs often have magnetite zones around their peripheries. We measured their isotopic compositions to determine if the magnetite zones demarcate the volume affected by atmospheric exchange during entry heating. Because we see little gradient in isotopic composition in the olivines, we conclude that the magnetites are a visual marker that allows us to select and analyze areas not affected by atmospheric exchange. Similar magnetite zones are seen in some olivine and pyroxene relict grains contained within MMs. © 2011 The Meteoritical Society. Issue published online: 26 April 2012; Article first published online: 2 November 2011; Received 15 May 2011; revision accepted 22 September 2011. The authors thank Dave Joswiak and Dr. Hope Ishii for reviewing this article and providing many helpful suggestions. Dr. Gregory Herzog is thanked for the many helpful discussions on this work. We ...
format Article in Journal/Newspaper
author Taylor, Susan
Matrajt, Graciela
Guan, Yunbin
spellingShingle Taylor, Susan
Matrajt, Graciela
Guan, Yunbin
Fine-grained precursors dominate the micrometeorite flux
author_facet Taylor, Susan
Matrajt, Graciela
Guan, Yunbin
author_sort Taylor, Susan
title Fine-grained precursors dominate the micrometeorite flux
title_short Fine-grained precursors dominate the micrometeorite flux
title_full Fine-grained precursors dominate the micrometeorite flux
title_fullStr Fine-grained precursors dominate the micrometeorite flux
title_full_unstemmed Fine-grained precursors dominate the micrometeorite flux
title_sort fine-grained precursors dominate the micrometeorite flux
publisher Meteoritical Society
publishDate 2012
url https://doi.org/10.1111/j.1945-5100.2011.01292.x
genre South pole
genre_facet South pole
op_source Meteoritics and Planetary Science, 47(4), 550-564, (2012-04)
op_relation https://doi.org/10.1111/j.1945-5100.2011.01292.x
oai:authors.library.caltech.edu:satvk-2tx50
eprintid:31620
resolverid:CaltechAUTHORS:20120523-143303420
op_rights info:eu-repo/semantics/openAccess
Other
op_doi https://doi.org/10.1111/j.1945-5100.2011.01292.x
container_title Meteoritics & Planetary Science
container_volume 47
container_issue 4
container_start_page 550
op_container_end_page 564
_version_ 1810480631898963968