Hadean Earth and primordial continents: The cradle of prebiotic life

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....

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Main Authors: M. Santosh, T. Arai, S. Maruyama
Format: Article
Language:English
Published: Elsevier 2017-03-01
Series:Geoscience Frontiers
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S1674987116300834
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spelling doaj-45ccf3582c074362b1651d72c9d078882020-11-24T22:38:50ZengElsevierGeoscience Frontiers1674-98712017-03-018230932710.1016/j.gsf.2016.07.005Hadean Earth and primordial continents: The cradle of prebiotic lifeM. Santosh0T. Arai1S. Maruyama2School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, ChinaEarth-Life Science Institute, Tokyo Institute of Technology, Tokyo 152-8551, JapanEarth-Life Science Institute, Tokyo Institute of Technology, Tokyo 152-8551, JapanThe 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 + 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 H2O, CO2, N2 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.http://www.sciencedirect.com/science/article/pii/S1674987116300834Earth-Moon systemPrimordial continentsABEL bombardmentTectonic erosionHadean plate tectonics
collection DOAJ
language English
format Article
sources DOAJ
author M. Santosh
T. Arai
S. Maruyama
spellingShingle M. Santosh
T. Arai
S. Maruyama
Hadean Earth and primordial continents: The cradle of prebiotic life
Geoscience Frontiers
Earth-Moon system
Primordial continents
ABEL bombardment
Tectonic erosion
Hadean plate tectonics
author_facet M. Santosh
T. Arai
S. Maruyama
author_sort M. Santosh
title Hadean Earth and primordial continents: The cradle of prebiotic life
title_short Hadean Earth and primordial continents: The cradle of prebiotic life
title_full Hadean Earth and primordial continents: The cradle of prebiotic life
title_fullStr Hadean Earth and primordial continents: The cradle of prebiotic life
title_full_unstemmed Hadean Earth and primordial continents: The cradle of prebiotic life
title_sort hadean earth and primordial continents: the cradle of prebiotic life
publisher Elsevier
series Geoscience Frontiers
issn 1674-9871
publishDate 2017-03-01
description 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 + 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 H2O, CO2, N2 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.
topic Earth-Moon system
Primordial continents
ABEL bombardment
Tectonic erosion
Hadean plate tectonics
url http://www.sciencedirect.com/science/article/pii/S1674987116300834
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