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关于早期生命信号本质的深刻问题:对李斯特(1673年)《某些形似植物的石头的描述》的评论

Deep questions about the nature of early-life signals: a commentary on Lister (1673) 'A description of certain stones figured like plants'.

作者信息

Brasier Martin

机构信息

Department of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, UK.

出版信息

Philos Trans A Math Phys Eng Sci. 2015 Apr 13;373(2039). doi: 10.1098/rsta.2014.0254.

DOI:10.1098/rsta.2014.0254
PMID:25750150
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC4360089/
Abstract

In 1673, Martin Lister explored the preservation of 'St Cuthbert's beads' plus other fossil crinoid remains from approximately 350 Ma Carboniferous limestone in northern England. He used taphonomic evidence (transport, disarticulation, burial and cementation) to infer an origin as petrified plant remains, in contrast with his views expressed elsewhere that fossil mollusc shells could have formed abiogenically, by 'plastic forces' within rock. Lister also observed pentagonal symmetry, now seen as characteristic of living echinoderm skeletons. A postscript from John Ray supports Lister's 'taphonomic' observations and accepts the biogenicity of these fossil 'vegetables'. Ray then concluded with a prophecy, predicting the discovery of comparable living fossils in remote ocean waters. These early discussions compare with current debates about the character of candidate microfossils from the early Earth and Mars. Interesting biomorphs are now tested against the abiogenic null hypotheses, making use of features such as those pioneered by Lister, including evidence for geological context, rules for growth and taphonomy. Advanced techniques now allow us to extend this list of criteria to include the nanoscale mapping of biology-like behaviour patterns plus metabolic pathways. Whereas the science of palaeobiology once began with tests for biogenicity, the same is now true for geobiology and astrobiology. This commentary was written to celebrate the 350th anniversary of the journal Philosophical Transactions of the Royal Society.

摘要

1673年,马丁·利斯特研究了“圣卡斯伯特的珠子”以及其他来自英格兰北部约3.5亿年前石炭纪石灰岩中的海百合化石残骸的保存情况。他利用埋藏学证据(搬运、解体、掩埋和胶结)推断其起源为石化的植物残骸,这与他在其他地方表达的观点形成对比,即化石软体动物壳可能是由岩石中的“塑性力”非生物成因形成的。利斯特还观察到了五角对称,现在这被视为现存棘皮动物骨骼的特征。约翰·雷的一篇后记支持了利斯特的“埋藏学”观察结果,并认可了这些化石“植物”的生物成因。雷随后以一个预言作为结论,预测在遥远的海洋水域会发现类似的活化石。这些早期的讨论与当前关于来自早期地球和火星的候选微化石特征的争论相比较。现在,有趣的生物形态会根据非生物成因的零假设进行检验,利用利斯特开创的那些特征,包括地质背景证据、生长规则和埋藏学。先进技术现在使我们能够将这一标准清单扩展到包括对类似生物行为模式和代谢途径的纳米级绘图。古生物学这门科学曾经始于对生物成因的检验,现在地质生物学和天体生物学也是如此。这篇评论是为庆祝《皇家学会哲学学报》创刊350周年而撰写的。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2741/4360089/99d2259a10a3/rsta20140254-g4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2741/4360089/278d48f65a51/rsta20140254-g1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2741/4360089/f7bb7eba0fb9/rsta20140254-g2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2741/4360089/0270a719a640/rsta20140254-g3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2741/4360089/99d2259a10a3/rsta20140254-g4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2741/4360089/278d48f65a51/rsta20140254-g1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2741/4360089/f7bb7eba0fb9/rsta20140254-g2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2741/4360089/0270a719a640/rsta20140254-g3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2741/4360089/99d2259a10a3/rsta20140254-g4.jpg

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本文引用的文献

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