Steele A, Goddard D T, Stapleton D, Toporski J K, Peters V, Bassinger V, Sharples G, Wynn-Williams D D, McKay D S
Astrobiology Group, University of Portsmouth, UK.
Meteorit Planet Sci. 2000 Mar;35(2):237-41. doi: 10.1111/j.1945-5100.2000.tb01772.x.
Examination of fracture surfaces near the fusion crust of the martian meteorite Allan Hills (ALH) 84001 have been conducted using scanning electron microscopy (SEM) and atomic force microscopy (AFM) and has revealed structures strongly resembling mycelium. These structures were compared with similar structures found in Antarctic cryptoendolithic communities. On morphology alone, we conclude that these features are not only terrestrial in origin but probably belong to a member of the Actinomycetales, which we consider was introduced during the Antarctic residency of this meteorite. If true, this is the first documented account of terrestrial microbial activity within a meteorite from the Antarctic blue ice fields. These structures, however, do not bear any resemblance to those postulated to be martian biota, although they are a probable source of the organic contaminants previously reported in this meteorite.
利用扫描电子显微镜(SEM)和原子力显微镜(AFM)对火星陨石艾伦山(ALH)84001熔壳附近的断裂面进行了检查,结果发现了与菌丝体极为相似的结构。这些结构与在南极隐生内生菌群落中发现的类似结构进行了比较。仅从形态学上看,我们得出结论,这些特征不仅起源于地球,而且可能属于放线菌目成员,我们认为这是该陨石在南极停留期间引入的。如果这是真的,这将是首次有记录的关于来自南极蓝冰区陨石内地球微生物活动的描述。然而,这些结构与假定的火星生物群毫无相似之处,尽管它们可能是此前在该陨石中报道的有机污染物的来源。