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Extraterrestrial amino acids in Orgueil and lvuna: Tracing the parent body of CI type carbonaceous chondrites

机译:Orgueil和lvuna中的地外氨基酸:追踪CI型碳质球粒陨石的母体

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摘要

Amino acid analyses using HPLC of pristine interior pieces of the CI carbonaceous chondrites Orgueil and lvuna have found that β- alanine, glycine, and γ-amino-n-butyric acid (ABA) are the most abundant amino acids in these two meteorites, with concentra- tions ranging from ≈600 to 2,000 parts per billion (ppb). Other α-amino acids such as alanine. α-ABA. α-aminoisobutyric acid (AIB). and isovaline are present only in trace amounts (<200 ppb). Carbon isotopic measurements of β-alanine and glycine and the presence of racemic (D/L ≈ 1) alanine and β-ABA in Orgueil suggest that these amino acids are extraterrestrial fn origin. In comparison to the CM carbonaceous chondrites Murchison and Murray, the amino acid composition of the CIs is strikingly distinct, suggesting that these meteorites came from a different type of parent body, possibly an extinct comet, than did the CM carbonaceous chondrites.
机译:使用HPLC对CI碳质球粒陨石Orgueil和lvuna的原始内部碎片进行的氨基酸分析发现,β-丙氨酸,甘氨酸和γ-氨基-正丁酸(ABA)是这两种陨石中含量最高的氨基酸,浓度范围从约600到2,000十亿分之一(ppb)。其他α-氨基酸,如丙氨酸。 α-ABA。 α-氨基异丁酸(AIB)。和异缬氨酸仅以痕量(<200 ppb)存在。 β-丙氨酸和甘氨酸的碳同位素测量以及Orgueil中存在外消旋(D / L≈1)丙氨酸和β-ABA的存在表明这些氨基酸是地外来源的。与CM碳质球粒陨石Murchison和Murray相比,CI的氨基酸组成非常不同,表明这些陨石与CM碳质球粒陨石来自不同类型的母体,可能是灭绝的彗星。

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