Skolkovo Institute of Science and Technology, Skolkovo, Moscow region, Russia, 143025.
Department of Chemistry, Lomonosov Moscow State University, Moscow, Russia.
Sci Rep. 2021 Apr 1;11(1):7410. doi: 10.1038/s41598-021-86576-6.
Despite broad application of different analytical techniques for studies on organic matter of chondrite meteorites, information about composition and structure of individual compounds is still very limited due to extreme molecular diversity of extraterrestrial organic matter. Here we present the first application of isotopic exchange assisted Fourier transform ion cyclotron resonance mass spectrometry (FTICR MS) for analysis of alkali extractable fraction of insoluble organic matter (IOM) of the Murchison and Allende meteorites. This allowed us to determine the individual S-containing ions with different types of sulfur atoms in IOM. Thiols, thiophenes, sulfoxides, sulfonyls and sulfonates were identified in both samples but with different proportions, which contribution corroborated with the hydrothermal and thermal history of the meteorites. The results were supported by XPS and thermogravimetric analysis coupled to FTICR MS. The latter was applied for the first time for analysis of chondritic IOM. To emphasize the peculiar extraterrestrial origin of IOM we have compared it with coal kerogen, which is characterized by the comparable complexity of molecular composition but its aromatic nature and low oxygen content can be ascribed almost exclusively to degradation of biomacromolecules.
尽管在研究球粒陨石有机质方面广泛应用了不同的分析技术,但由于天外有机物具有极端的分子多样性,关于其组成和结构的个别化合物的信息仍然非常有限。在这里,我们首次应用同位素交换辅助傅里叶变换离子回旋共振质谱(FTICR MS)分析了默奇森陨石和 Allende 陨石不溶性有机质(IOM)的可提取碱部分。这使我们能够确定 IOM 中具有不同类型硫原子的个别含硫离子。在这两种样品中均鉴定出了硫醇、噻吩、亚砜、砜和硫酸盐,但比例不同,这一结果与陨石的热液和热历史相符。XPS 和热重分析与 FTICR MS 联用结果也证实了这一结果。FTICR MS 首次应用于分析陨石 IOM。为了强调 IOM 的特殊天外起源,我们将其与煤干酪根进行了比较,煤干酪根的分子组成同样复杂,但由于几乎完全归因于生物大分子的降解,其芳香性质和低氧含量可以归因于其独特的外星起源。