Fox S W, Harada K, Hare P E, Hinsch G, Mueller G
Science. 1970 Jan 30;167(3918):767-70. doi: 10.1126/science.167.3918.767.
Acid hydrolyzates of aqueous extracts indicated: glycine, alanine, glutamic acid, serine, aspartic acid, threonine, and I-diaminopropionic acid. The sources of these amino acids may be terrestrial contaminants, fuel exhaust products, or indigenous lunar material. The lunar particles found in the sample include: (i) spherules, rotational ellipsoids, dumbbells, tear-drops, rings, and crescents which have (ii) diameters of 0.1 to 500 microns; (iii) budlike features on the particles; and (iv) chemical inhomogeneity (electron probe). Some of the processes and results inferred for the moon have been simulated by the electron beam and low pressure of the electron microscope. Basalt (Kilauea-lki) and chondrite (Orgueil) have been found to behave similarly.
甘氨酸、丙氨酸、谷氨酸、丝氨酸、天冬氨酸、苏氨酸和L-二氨基丙酸。这些氨基酸的来源可能是地球污染物、燃料废气产物或月球本土物质。样品中发现的月球颗粒包括:(i) 小球体、旋转椭球体、哑铃形、泪滴形、环形和月牙形,其 (ii) 直径为0.1至500微米;(iii) 颗粒上的芽状特征;以及 (iv) 化学不均匀性(电子探针)。月球上推断出的一些过程和结果已通过电子显微镜的电子束和低气压进行了模拟。已发现玄武岩(基拉韦厄伊基)和球粒陨石(奥盖尔)的表现类似。