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早期真核生物生态系统中的形态学和生态复杂性。

Morphological and ecological complexity in early eukaryotic ecosystems.

作者信息

Javaux E J, Knoll A H, Walter M R

机构信息

Botanical Museum, Harvard University, Cambridge, Massachusetts 02138, USA.

出版信息

Nature. 2001 Jul 5;412(6842):66-9. doi: 10.1038/35083562.

Abstract

Molecular phylogeny and biogeochemistry indicate that eukaryotes differentiated early in Earth history. Sequence comparisons of small-subunit ribosomal RNA genes suggest a deep evolutionary divergence of Eukarya and Archaea; C27-C29 steranes (derived from sterols synthesized by eukaryotes) and strong depletion of 13C (a biogeochemical signature of methanogenic Archaea) in 2,700 Myr old kerogens independently place a minimum age on this split. Steranes, large spheroidal microfossils, and rare macrofossils of possible eukaryotic origin occur in Palaeoproterozoic rocks. Until now, however, evidence for morphological and taxonomic diversification within the domain has generally been restricted to very late Mesoproterozoic and Neoproterozoic successions. Here we show that the cytoskeletal and ecological prerequisites for eukaryotic diversification were already established in eukaryotic microorganisms fossilized nearly 1,500 Myr ago in shales of the early Mesoproterozoic Roper Group in northern Australia.

摘要

分子系统发育学和生物地球化学研究表明,真核生物在地球历史早期就已经分化。小亚基核糖体RNA基因的序列比较显示,真核生物域和古菌域在进化上存在很大差异;27亿年前的干酪根中,C27 - C29甾烷(源自真核生物合成的甾醇)以及13C的强烈亏损(产甲烷古菌的生物地球化学特征)独立地确定了这一分化的最小年龄。在古元古代岩石中发现了甾烷、大型球状微化石以及可能起源于真核生物的罕见宏体化石。然而,迄今为止,该域内形态学和分类学多样化的证据通常仅限于中元古代晚期和新元古代的演替。在此,我们表明,在澳大利亚北部中元古代早期罗珀群页岩中保存的、距今近15亿年的真核微生物化石中,已经具备了真核生物多样化所需的细胞骨架和生态条件。

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