In-situ O-isotope analysis of relict spinel and forsterite in small (<200 μm) Antarctic micrometeorites – Samples of chondrules & CAIs from carbonaceous chondrites
We report high-precision secondary ion mass spectrometer triple oxygen isotope systematics (95 individual analyses) from 37 micrometeorites (MMs) collected from South Pole Water Well (SPWW), Antarctica. The study population focuses on unmelted coarse-grained (Cg) MMs (n = 23) with both multiple (n =...
Published in: | Geochimica et Cosmochimica Acta |
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ftopenunivgb:oai:oro.open.ac.uk:83089 2023-06-11T04:07:14+02:00 In-situ O-isotope analysis of relict spinel and forsterite in small (<200 μm) Antarctic micrometeorites – Samples of chondrules & CAIs from carbonaceous chondrites Rudraswami, N. G. Suttle, M. Marrocchi, Y. Taylor, S. Villeneuve, J. 2022-05-15 application/pdf https://oro.open.ac.uk/83089/ https://oro.open.ac.uk/83089/1/1-s2.0-S0016703722001314-main.pdf https://oro.open.ac.uk/83089/10/Rudraswami_2022_SUT_O-isotope_MMs.pdf https://doi.org/10.1016/j.gca.2022.03.015 unknown https://oro.open.ac.uk/83089/1/1-s2.0-S0016703722001314-main.pdf https://oro.open.ac.uk/83089/10/Rudraswami_2022_SUT_O-isotope_MMs.pdf Rudraswami, N. G.; Suttle, M. <http://oro.open.ac.uk/view/person/ms35249.html>; Marrocchi, Y.; Taylor, S. and Villeneuve, J. (2022). In-situ O-isotope analysis of relict spinel and forsterite in small (<200 μm) Antarctic micrometeorites – Samples of chondrules & CAIs from carbonaceous chondrites. Geochimica et Cosmochimica Acta, 325 pp. 1–24. Journal Item OU Users Only PeerReviewed 2022 ftopenunivgb https://doi.org/10.1016/j.gca.2022.03.015 2023-05-28T06:07:22Z We report high-precision secondary ion mass spectrometer triple oxygen isotope systematics (95 individual analyses) from 37 micrometeorites (MMs) collected from South Pole Water Well (SPWW), Antarctica. The study population focuses on unmelted coarse-grained (Cg) MMs (n = 23) with both multiple (n = 14) and single-mineral (n = 9) varieties investigated. We also analysed relict minerals in porphyritic cosmic spherules (n = 13) and the relict matrix in a single scoriaceous fine-grained (Fg) MM. The target minerals investigated are primarily olivine (Fo ∼ 43–99%) and spinel. Textural, chemical and isotopic data confirm that both olivine and spinel grains have retained their pre-atmospheric O-isotope compositions, allowing inferences to be drawn about their formation and parent body affinities. We separate the study population into three groups: spinel-free particles (consisting of the CgMMs and PO cosmic spherules), spinel-bearing MMs and the single FgMM. Olivine grains in spinel-free MMs vary between δ 17 O: −12.6‰ and +3.5‰, δ 18 O: −9.6‰ and +7.5‰, and Δ 17 O: −9.5‰ and +1.3‰ and define a slope-1 profile in δ 18 O–δ 17 O isotope space. They are most likely fragmented chondrules, with both type I and type II varieties represented. Their observed Mg#-Δ 17 O distribution is best explained by a mixture of CM chondrules and either CR chondrules, Tagish Lake chondrules or WILD2 cometary silicates. One of these chondrule-like MMs has an isotopically heterogeneous composition, characterised by a single olivine grain with a markedly 16 O-rich composition (Δ 17 O: −16.3‰), suggesting it is a relict silicate fragment of AOA material that was incorporated into the chondrule precursor. We analysed 11 spinel grains in five spinel-bearing MMs. In all instances spinels are nearly pure MgAl 2 O 4 with isotopically light ( 16 O-rich) compositions (ranging from δ 17 O: −34.4‰ to −0.9‰, δ 18 O: −30.8‰ to +11.0‰, and Δ 17 O: −18.3‰ to −4.4‰). They are therefore 16 O-poor relative to spinel found in unaltered CAIs, indicating a ... Article in Journal/Newspaper Antarc* Antarctic Antarctica South pole South pole Tagish The Open University: Open Research Online (ORO) Antarctic South Pole Tagish ENVELOPE(-134.272,-134.272,60.313,60.313) Tagish Lake ENVELOPE(-134.233,-134.233,59.717,59.717) Geochimica et Cosmochimica Acta 325 1 24 |
institution |
Open Polar |
collection |
The Open University: Open Research Online (ORO) |
op_collection_id |
ftopenunivgb |
language |
unknown |
description |
We report high-precision secondary ion mass spectrometer triple oxygen isotope systematics (95 individual analyses) from 37 micrometeorites (MMs) collected from South Pole Water Well (SPWW), Antarctica. The study population focuses on unmelted coarse-grained (Cg) MMs (n = 23) with both multiple (n = 14) and single-mineral (n = 9) varieties investigated. We also analysed relict minerals in porphyritic cosmic spherules (n = 13) and the relict matrix in a single scoriaceous fine-grained (Fg) MM. The target minerals investigated are primarily olivine (Fo ∼ 43–99%) and spinel. Textural, chemical and isotopic data confirm that both olivine and spinel grains have retained their pre-atmospheric O-isotope compositions, allowing inferences to be drawn about their formation and parent body affinities. We separate the study population into three groups: spinel-free particles (consisting of the CgMMs and PO cosmic spherules), spinel-bearing MMs and the single FgMM. Olivine grains in spinel-free MMs vary between δ 17 O: −12.6‰ and +3.5‰, δ 18 O: −9.6‰ and +7.5‰, and Δ 17 O: −9.5‰ and +1.3‰ and define a slope-1 profile in δ 18 O–δ 17 O isotope space. They are most likely fragmented chondrules, with both type I and type II varieties represented. Their observed Mg#-Δ 17 O distribution is best explained by a mixture of CM chondrules and either CR chondrules, Tagish Lake chondrules or WILD2 cometary silicates. One of these chondrule-like MMs has an isotopically heterogeneous composition, characterised by a single olivine grain with a markedly 16 O-rich composition (Δ 17 O: −16.3‰), suggesting it is a relict silicate fragment of AOA material that was incorporated into the chondrule precursor. We analysed 11 spinel grains in five spinel-bearing MMs. In all instances spinels are nearly pure MgAl 2 O 4 with isotopically light ( 16 O-rich) compositions (ranging from δ 17 O: −34.4‰ to −0.9‰, δ 18 O: −30.8‰ to +11.0‰, and Δ 17 O: −18.3‰ to −4.4‰). They are therefore 16 O-poor relative to spinel found in unaltered CAIs, indicating a ... |
format |
Article in Journal/Newspaper |
author |
Rudraswami, N. G. Suttle, M. Marrocchi, Y. Taylor, S. Villeneuve, J. |
spellingShingle |
Rudraswami, N. G. Suttle, M. Marrocchi, Y. Taylor, S. Villeneuve, J. In-situ O-isotope analysis of relict spinel and forsterite in small (<200 μm) Antarctic micrometeorites – Samples of chondrules & CAIs from carbonaceous chondrites |
author_facet |
Rudraswami, N. G. Suttle, M. Marrocchi, Y. Taylor, S. Villeneuve, J. |
author_sort |
Rudraswami, N. G. |
title |
In-situ O-isotope analysis of relict spinel and forsterite in small (<200 μm) Antarctic micrometeorites – Samples of chondrules & CAIs from carbonaceous chondrites |
title_short |
In-situ O-isotope analysis of relict spinel and forsterite in small (<200 μm) Antarctic micrometeorites – Samples of chondrules & CAIs from carbonaceous chondrites |
title_full |
In-situ O-isotope analysis of relict spinel and forsterite in small (<200 μm) Antarctic micrometeorites – Samples of chondrules & CAIs from carbonaceous chondrites |
title_fullStr |
In-situ O-isotope analysis of relict spinel and forsterite in small (<200 μm) Antarctic micrometeorites – Samples of chondrules & CAIs from carbonaceous chondrites |
title_full_unstemmed |
In-situ O-isotope analysis of relict spinel and forsterite in small (<200 μm) Antarctic micrometeorites – Samples of chondrules & CAIs from carbonaceous chondrites |
title_sort |
in-situ o-isotope analysis of relict spinel and forsterite in small (<200 μm) antarctic micrometeorites – samples of chondrules & cais from carbonaceous chondrites |
publishDate |
2022 |
url |
https://oro.open.ac.uk/83089/ https://oro.open.ac.uk/83089/1/1-s2.0-S0016703722001314-main.pdf https://oro.open.ac.uk/83089/10/Rudraswami_2022_SUT_O-isotope_MMs.pdf https://doi.org/10.1016/j.gca.2022.03.015 |
long_lat |
ENVELOPE(-134.272,-134.272,60.313,60.313) ENVELOPE(-134.233,-134.233,59.717,59.717) |
geographic |
Antarctic South Pole Tagish Tagish Lake |
geographic_facet |
Antarctic South Pole Tagish Tagish Lake |
genre |
Antarc* Antarctic Antarctica South pole South pole Tagish |
genre_facet |
Antarc* Antarctic Antarctica South pole South pole Tagish |
op_relation |
https://oro.open.ac.uk/83089/1/1-s2.0-S0016703722001314-main.pdf https://oro.open.ac.uk/83089/10/Rudraswami_2022_SUT_O-isotope_MMs.pdf Rudraswami, N. G.; Suttle, M. <http://oro.open.ac.uk/view/person/ms35249.html>; Marrocchi, Y.; Taylor, S. and Villeneuve, J. (2022). In-situ O-isotope analysis of relict spinel and forsterite in small (<200 μm) Antarctic micrometeorites – Samples of chondrules & CAIs from carbonaceous chondrites. Geochimica et Cosmochimica Acta, 325 pp. 1–24. |
op_doi |
https://doi.org/10.1016/j.gca.2022.03.015 |
container_title |
Geochimica et Cosmochimica Acta |
container_volume |
325 |
container_start_page |
1 |
op_container_end_page |
24 |
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1768380204877611008 |