期刊文献+
共找到3篇文章
< 1 >
每页显示 20 50 100
Hadean Earth and primordial continents:The cradle of prebiotic life 被引量:2
1
作者 M.Santosh T.Arai S.Maruyama 《Geoscience Frontiers》 SCIE CAS CSCD 2017年第2期309-327,共19页
The Hadean history of Earth is shrouded in mystery and it is considered that the planet was born dry with no water or atmosphere.The Earth-Moon system had many features in common during the birth stage.Solidification ... The Hadean history of Earth is shrouded in mystery and it is considered that the planet was born dry with no water or atmosphere.The Earth-Moon system had many features in common during the birth stage.Solidification of the dry magma ocean at 4.53 Ga generated primordial continents with komatiite.We speculate that the upper crust was composed of fractionated gabbros and the middle felsic crust by anorthosite at ca.21 km depth boundary,underlain by meta-anorthosite(grossular + kyanite 4 quartz)down to 50-60 km in depth.The thickness of the mafic KREEP basalt in the lower crust,separating it from the underlying upper mantle is not well-constrained and might have been up to ca.100-200 km depending on the degree of fractionation and gravitational stability versus surrounding mantle density.The primordial continents must have been composed of the final residue of dry magma ocean and enriched in several critical elements including Ca,Mg,Fe,Mn,P,K,and Cl which were exposed on the surface of the dry Earth.Around 190 million years after the solidification of the magma ocean, "ABEL bombardment" delivered volatiles including H_2O,CO_2,N_2 as well as silicate components through the addition of icy asteroids.This event continued for 200 Myr with subordinate bombardments until 3.9 Ga,preparing the Earth for the prebiotic chemical evolution and as the cradle of first life.Due to vigorous convection arising from high mantle potential temperatures,the primordial continents disintegrated and were dragged down to the deep mantle,marking the onset of Hadean plate tectonics. 展开更多
关键词 earth-Moon system Primordial continents ABEL bombardment Tectonic erosion hadean plate tectonics
下载PDF
Origins of building blocks of life: A review 被引量:2
2
作者 Norio Kitadai Shigenori Maruyama 《Geoscience Frontiers》 SCIE CAS CSCD 2018年第4期1117-1153,共37页
How and where did life on Earth originate? To date, various environments have been proposed as plausible sites for the origin of life. However, discussions have focused on a limited stage of chemical evolution, or em... How and where did life on Earth originate? To date, various environments have been proposed as plausible sites for the origin of life. However, discussions have focused on a limited stage of chemical evolution, or emergence of a specific chemical function of proto-biological systems. It remains unclear what geochemical situations could drive all the stages of chemical evolution, ranging from condensation of simple inorganic compounds to the emergence of self-sustaining systems that were evolvable into modern biological ones. In this review, we summarize reported experimental and theoretical findings for prebiotic chemistry relevant to this topic, including availability of biologically essential elements(N and P) on the Hadean Earth, abiotic synthesis of life's building blocks(amino acids, peptides, ribose, nucleobases, fatty acids, nucleotides, and oligonucleotides), their polymerizations to bio-macromolecules(peptides and oligonucleotides), and emergence of biological functions of replication and compartmentalization. It is indicated from the overviews that completion of the chemical evolution requires at least eight reaction conditions of(1) reductive gas phase,(2) alkaline pH,(3) freezing temperature,(4)fresh water,(5) dry/dry-wet cycle,(6) coupling with high energy reactions,(7) heating-cooling cycle in water, and(8) extraterrestrial input of life's building blocks and reactive nutrients. The necessity of these mutually exclusive conditions clearly indicates that life's origin did not occur at a single setting; rather, it required highly diverse and dynamic environments that were connected with each other to allow intratransportation of reaction products and reactants through fluid circulation. Future experimental research that mimics the conditions of the proposed model are expected to provide further constraints on the processes and mechanisms for the origin of life. 展开更多
关键词 ASTROBIOLOGY BIOCHEMISTRY Chemical evolution Extraterrestrial life hadean earth Hydrothermal systems
下载PDF
冥古宙地球的冷却、分异和构造体制及其比较行星学研究 被引量:1
3
作者 刘耘 章清文 《科学通报》 EI CAS CSCD 北大核心 2023年第18期2284-2295,共12页
冥古宙是地球历史的最初阶段,虽然仅持续不到6亿年,但在此期间发生巨大的物质运移和重新分布,地球的地核、地幔、地壳和大气层等主要圈层框架已基本形成,为地球后续漫长的物质和能量演变奠定了基础.由于关键地质记录缺失、研究手段匮乏... 冥古宙是地球历史的最初阶段,虽然仅持续不到6亿年,但在此期间发生巨大的物质运移和重新分布,地球的地核、地幔、地壳和大气层等主要圈层框架已基本形成,为地球后续漫长的物质和能量演变奠定了基础.由于关键地质记录缺失、研究手段匮乏等原因,当前地球科学界针对冥古宙地球演化的研究仍十分有限,使其成为地球科学最为薄弱的一环.鉴于冥古宙地球存在地质记录匮乏这一“痛点”,以及太阳系类地天体(泛指类地行星、矮行星、卫星和小行星等岩石质天体)在原始物质组成、内部结构、热演化和构造体制演变等方面的相似性,借助比较行星学手段,从太阳系内各类地天体(现今或早期)保存完好的地质记录研究类地天体演化的一般规律,以此弥补早期地球演化认识的空白.这是一种重要且可行的研究手段,也是突破现有地学理论框架(如板块构造理论)、开辟新的地学研究格局的重要契机.本文对早期地球的热演化、内部分异和构造体制等关键领域的研究进展及其存在的问题进行了梳理,同时探讨了未来可能的突破点. 展开更多
关键词 冥古宙地球 热演化 化学分异 构造体制 比较行星学
原文传递
上一页 1 下一页 到第
使用帮助 返回顶部