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本文引用的文献

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Anoxic ecosystems and early eukaryotes.缺氧生态系统与早期真核生物
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The transition from a cyanobacterial to algal world and the emergence of animals.从蓝藻世界到藻类世界的转变以及动物的出现。
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The dynamics of stem and crown groups.茎和冠群的动态。
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Isolation of an archaeon at the prokaryote-eukaryote interface.古菌的分离处于原核生物与真核生物的交界处。
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Early fungi from the Proterozoic era in Arctic Canada.北极加拿大前寒武纪时期的早期真菌。
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Asgard archaea capable of anaerobic hydrocarbon cycling.能够进行厌氧烃类循环的古菌 Asgard。
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Microbial assemblage and palaeoenvironmental reconstruction of the 1.38 Ga Velkerri Formation, McArthur Basin, northern Australia.澳大利亚北部麦卡瑟盆地 13.8 亿年的维拉克里夫组的微生物组合和古环境重建。
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Absence of biomarker evidence for early eukaryotic life from the Mesoproterozoic Roper Group: Searching across a marine redox gradient in mid-Proterozoic habitability.从中元古代罗珀组中寻找早期真核生物生物标志物证据的缺失:在中元古代宜居性的海洋氧化还原梯度中进行搜索。
Geobiology. 2019 May;17(3):247-260. doi: 10.1111/gbi.12329. Epub 2019 Jan 10.
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Oxygenated Mesoproterozoic lake revealed through magnetic mineralogy.通过磁性矿物学揭示出富氧中元古代湖泊。
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Was the Mitochondrion Necessary to Start Eukaryogenesis?线粒体是否是真核生物起源所必需的?
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从化石记录中洞察真核生物起源

Insights into eukaryogenesis from the fossil record.

作者信息

Porter Susannah M

机构信息

Department of Earth Science, University of California at Santa Barbara, Santa Barbara, CA 93106, USA.

出版信息

Interface Focus. 2020 Aug 6;10(4):20190105. doi: 10.1098/rsfs.2019.0105. Epub 2020 Jun 12.

DOI:10.1098/rsfs.2019.0105
PMID:32642050
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC7333905/
Abstract

Eukaryogenesis-the process by which the eukaryotic cell emerged-has long puzzled scientists. It has been assumed that the fossil record has little to say about this process, in part because important characters such as the nucleus and mitochondria are rarely preserved, and in part because the prevailing model of early eukaryotes implies that eukaryogenesis occurred before the appearance of the first eukaryotes recognized in the fossil record. Here, I propose a different scenario for early eukaryote evolution than is widely assumed. Rather than crown group eukaryotes originating in the late Paleoproterozoic and remaining ecologically minor components for more than half a billion years in a prokaryote-dominated world, I argue for a late Mesoproterozoic origin of the eukaryotic crown group, implying that eukaryogenesis can be studied using the fossil record. I review the proxy records of four crown group characters: the capacity to form cysts as evidenced by the presence of excystment structures; a complex cytoskeleton as evidenced by spines or pylomes; sterol synthesis as evidenced by steranes; and aerobic respiration-and therefore mitochondria-as evidenced by eukaryotes living in oxic environments, and argue that it might be possible to use these proxy records to infer the order in which these characters evolved. The records indicate that both cyst formation and a complex cytoskeleton appeared by late Paleoproterozoic time, and sterol synthesis appeared in the late Mesoproterozioc or early Neoproterozoic. The origin of aerobic respiration cannot as easily be pinned down, but current evidence permits the possibility that it evolved sometime in the Mesoproterozoic.

摘要

真核生物起源(即真核细胞出现的过程)长期以来一直困扰着科学家。人们一直认为化石记录对这一过程几乎没有什么可说的,部分原因是细胞核和线粒体等重要特征很少被保存下来,部分原因是早期真核生物的主流模型表明真核生物起源发生在化石记录中首次被识别的第一批真核生物出现之前。在这里,我提出了一种与广泛假设不同的早期真核生物进化情景。我认为真核生物冠群起源于中元古代晚期,而不是起源于古元古代晚期并在原核生物主导的世界中作为生态次要组成部分存在超过5亿年,这意味着可以利用化石记录来研究真核生物起源。我回顾了四个冠群特征的替代记录:通过脱囊结构的存在证明的形成囊肿的能力;通过刺或幽门证明的复杂细胞骨架;通过甾烷证明的甾醇合成;以及通过生活在有氧环境中的真核生物证明的有氧呼吸,进而证明线粒体的存在,并认为有可能利用这些替代记录来推断这些特征进化的顺序。记录表明,到古元古代晚期囊肿形成和复杂细胞骨架都已出现,甾醇合成出现在中元古代晚期或新元古代早期。有氧呼吸的起源不太容易确定,但目前的证据表明它有可能在中元古代的某个时候进化而来。