Hadean Earth and primordial continents: The cradle of prebiotic life

作者: M. Santosh , T. Arai , S. Maruyama

DOI: 10.1016/J.GSF.2016.07.005

关键词: Mantle (geology)CrustArcheanHadeanGeochemistryBasaltKREEPGeologyPlate tectonicsMafic

摘要: Abstract The Hadean history of Earth is shrouded in mystery and it considered that the planet was born dry with no water or atmosphere. Earth-Moon system had many features common during birth stage. Solidification magma ocean at 4.53 Ga generated primordial continents komatiite. We speculate upper crust composed fractionated gabbros middle felsic by anorthosite ca. 21 km depth boundary, underlain meta-anorthosite (grossular + kyanite + quartz) down to 50–60 km depth. thickness mafic KREEP basalt lower crust, separating from underlying mantle not well-constrained might have been up 100–200 km depending on degree fractionation gravitational stability versus surrounding density. must final residue enriched several critical elements including Ca, Mg, Fe, Mn, P, K, Cl which were exposed surface Earth. Around 190 million years after solidification ocean, “ABEL bombardment” delivered volatiles H 2 O, CO , N as well silicate components through addition icy asteroids. This event continued for 200 Myr subordinate bombardments until 3.9 Ga, preparing prebiotic chemical evolution cradle first life. Due vigorous convection arising high potential temperatures, disintegrated dragged deep mantle, marking onset plate tectonics.

参考文章(73)
E. K. Gibson, R. C. Greenwood, I. A. Franchi, C. T. Pillinger, M. F. Miller, D. Johnson, Three Isotopes of Oxygen in Lunar Samples — The Same as Earth or Different? Lunar and Planetary Science Conference. pp. 2654- ,(2014)
Kenji Kawai, Shinji Yamamoto, Taku Tsuchiya, Shigenori Maruyama, The second continent: Existence of granitic continental materials around the bottom of the mantle transition zone Geoscience frontiers. ,vol. 4, pp. 1- 6 ,(2013) , 10.1016/J.GSF.2012.08.003
M. R. Dence, R. J. Floran, Morphology of the Manicouagan Ring-Structure, Quebec, and some comparisons with lunar basins and craters Lunar and Planetary Science Conference Proceedings. ,vol. 1, pp. 2845- 2865 ,(1976)
Eiji Ito, Eiichi Takahashi, Ultrahigh-pressure phase transformations and the constitution of the deep mantle High‐Pressure Research in Mineral Physics: A Volume in Honor of Syun‐iti Akimoto. ,vol. 39, pp. 221- 229 ,(1987) , 10.1029/GM039P0221
Simon A. Wilde, John W. Valley, William H. Peck, Colin M. Graham, Evidence from detrital zircons for the existence of continental crust and oceans on the Earth 4.4 Gyr ago. Nature. ,vol. 409, pp. 175- 178 ,(2001) , 10.1038/35051550
P. W. Weiblen, E. Roedder, Lunar petrology of silicate melt inclusions, Apollo 11 rocks GeCAS. ,vol. 1, pp. 801- ,(1970)
J. S. Dickey, B. N. Powell, U. B. Marvin, J. A. Wood, Lunar anorthosites and a geophysical model of the moon Geochimica et Cosmochimica Acta Supplement. ,vol. 1, pp. 965- ,(1970)
Kei Hirose, Ryosuke Sinmyo, Nagayoshi Sata, Yasuo Ohishi, Determination of post‐perovskite phase transition boundary in MgSiO3 using Au and MgO pressure standards Geophysical Research Letters. ,vol. 33, ,(2006) , 10.1029/2005GL024468
Claude Herzberg, Depth and degree of melting of komatiites Journal of Geophysical Research. ,vol. 97, pp. 4521- 4540 ,(1992) , 10.1029/91JB03066