. Author manuscript; available in PMC: 2021 Dec 2.

Published in final edited form as: Geochim Cosmochim Acta. 2020 Oct 8;293:544–574. doi: 10.1016/j.gca.2020.09.036

Table 1.

Mineralogy of AOAs from Kaba (CV3.1) and DOM 08006 (CO3.01) carbonaceous chondrites

Chondrite	AOA name	AOA texture	fo	FeNi	Ca-, A1-rich portions				LIME o1^b	1px
Chondrite	AOA name	AOA texture	fo	FeNi	A1-(Ti)-di	an	sp	halo^a	LIME o1^b	1px
Kaba	K27	compact	+	+	+	+	+	−	−	−
DOM 08006	501	pore-rich	+	+	+	+	−	+	+	−
DOM 08006	502	pore-rich	+	+	+	+	−	+	+	+
DOM 08006	503	pore-rich	+	+	+	+	−	+	+	+
DOM 08006	505	compact	+	+	+	−	+	−	+	−
DOM 08006	511	pore-rich	+	+	+	+	−	+	+	−
DOM 08006	512	pore-rich	+	+	+	+	−	+	+	−
DOM 08006	513	compact	+	+	+	+	+	−	−	−
DOM 08006	514	pore-rich	+	+	+	+	−	+	−	−

Diffuse area that appears to be brighter in BSE images than surrounding forsterite. See section 4.1.

Olivine grains with MnO/FeO (wt%) ≥ 1. The MnO/FeO ratios are calculated from SIMS data in Table 4, except for AOA 514.

The MnO/FeO ratios of olivine grains from AOA 514 are calculated from FE-EPMA data due to an absence of SIMS minor element data.

fo = forsterite, FeNi = Fe,Ni-metal and/or weathering products, Al-(Ti)-di = Al-(Ti) diopside, an = anorthite, sp = spinel, LIME ol = LIME olivine, lpx = low-Ca pyroxene