2005
DOI: 10.1126/science.1108140
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Supra-Canonical 26 Al/ 27 Al and the Residence Time of CAIs in the Solar Protoplanetary Disk

Abstract: The canonical initial 26Al/27Al ratio of 4.5 x 10(-5) has been a fiducial marker for the beginning of the solar system. Laser ablation and whole-rock multiple-collector inductively coupled plasma-source mass spectrometry magnesium isotope analyses of calcium- and aluminum-rich inclusions (CAIs) from CV3 meteorites demonstrate that some CAIs had initial 26Al/27Al values at least 25% greater than canonical and that the canonical initial 26Al/27Al cannot mark the beginning of solar system formation. Using rates o… Show more

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Cited by 147 publications
(112 citation statements)
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References 21 publications
(25 reference statements)
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“…The most direct interpretation of the results is that 247 Cm is in low or very low abundance compared to the UP model. As mentioned, the measured abundance of 244 Pu is low by a factor of two compared to the UP value. This would then appear to require a significant time interval between the termination of heavy r-nucleosynthesis and formation of the solar nebula if the counting of precursors is a reasonably reliable estimate of the relative yields for actinides.…”
Section: Estimates Of the Ism Inventory Of Short-lived Nucleimentioning
confidence: 99%
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“…The most direct interpretation of the results is that 247 Cm is in low or very low abundance compared to the UP model. As mentioned, the measured abundance of 244 Pu is low by a factor of two compared to the UP value. This would then appear to require a significant time interval between the termination of heavy r-nucleosynthesis and formation of the solar nebula if the counting of precursors is a reasonably reliable estimate of the relative yields for actinides.…”
Section: Estimates Of the Ism Inventory Of Short-lived Nucleimentioning
confidence: 99%
“…If they started with the same 26 Al/ 27 Al initial value, then this requires that these three units (in the same droplet) formed over a time interval of ≈ 4 × 10 5 yr. Alternatively, they could very possibly represent multiple droplet formation in a single event, but from a starting material that was heterogeneous. Recent results by Galy, Hutcheon & Grossman [242], by Liu, Iizuka & McKeegan [243] and by Young et al [244] using "bulk" CAI samples in a new generation of high-precision measurements show that the spread in 26 Al/ 27 Al is rather general, with some samples having a "supra-canonical" value of 26 Al/ 27 Al ≈ 6 ×10 −5 . These more recent studies point to a higher value of 26 Al/ 27 Al in the ESS.…”
Section: Almentioning
confidence: 99%
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