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A possible anorthositic continent of early Mars and the role of planetary size for the inception of Earth-like life

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Tiêu đề A possible anorthositic continent of early Mars and the role of planetary size for the inception of Earth-like life
Tác giả James M. Dohm, Shigenori Maruyama, Motoyuki Kido, Victor R. Baker
Trường học The University of Tokyo
Chuyên ngành Planetary science
Thể loại Accepted manuscript
Năm xuất bản 2016
Thành phố Tokyo
Định dạng
Số trang 70
Dung lượng 5,22 MB

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A possible anorthositic continent of early Mars and the role of planetary size for the inception of Earth like life Accepted Manuscript A possible anorthositic continent of early Mars and the role of[.]

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A possible anorthositic continent of early Mars and the role of planetary size for the

inception of Earth-like life

James M Dohm, Shigenori Maruyama, Motoyuki Kido, Victor R Baker

PII: S1674-9871(16)30215-8

DOI: 10.1016/j.gsf.2016.12.003

Reference: GSF 521

To appear in: Geoscience Frontiers

Received Date: 2 March 2016

Revised Date: 3 December 2016

Accepted Date: 11 December 2016

Please cite this article as: Dohm, J.M., Maruyama, S., Kido, M., Baker, V.R., A possible anorthositic

continent of early Mars and the role of planetary size for the inception of Earth-like life, Geoscience

Frontiers (2017), doi: 10.1016/j.gsf.2016.12.003.

This is a PDF file of an unedited manuscript that has been accepted for publication As a service to our customers we are providing this early version of the manuscript The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain.

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4 Mars Exploration Rover Spirit

5 Mars Exploration Rover Opportunity

6 Mars Science Laboratory, Curiosity Rover

7 Phoenix Landing Site

Utopia Planitia

3 Pathfinder Lander and Sojourner Rover

225.990°W

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Possible granite Crater floor of Noachis Terra 21.56°S,

41.10°E Wray et al (2013)Possible granite Caldera floor of Nili Patera 8.86°N,

67.28°E Wray et al (2013)

1/2 TTG

(granite/andesite) and/or

anorthosite

Possible granite and/or anorthosite

Peace Vallis alluvial fan materials along the floor of Gale crater sourcing from the northern rim of Gale (possibly primordial crustal materials exposed by the Gale impact event)

4.5895°S, 137.4417°E Sautter et al (2015)

2 Anorthosite Possible anorthosite

Hellas rim materials (possibly primordial crustal materials exposed by the giant Hellas impact event)

29.7°S, 86.78°E;

25.2°S, 66.5°E;

28.9°S, 79.4°E;

63.0°E, 16.3°S;

Carter and Poulet (2013), Poulet and Carter (2013)

57.496° Michalski and Niles (2010)Crater superposed on Huygens

crater

(~14°S, 55°E) J.J Wray et al (2010)carbonate Jezero crater 18.855°N,

77.519°E Ehlmann et al (2008)

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Earth-Life Science Institute, Tokyo Institute of Technology, 2-12-1-IE-1 Ookayama,

Merugo-ku, Tokyo 152-8550, Japan

c

International Research Institute of Disaster Science, Tohoku University, 468-1, Aza Aoba, Aramaki, Aoba-ku, Sendai 980-0845, Japan

d Lunar and Planetary Laboratory, The University of Arizona, Tucson, AZ 85721-0092, USA

* Corresponding author E-mail address: jmd@um.u-tokyo.ac.jp

Highlights

• A logic to identify habitable planet is proposed

• Difference in the presence of an anorthositic primordial continent is due to the size of planet

• The presence of the primordial continent is the essential and most significant factor as it determines the fate of the planet to be habitable or not

• There is very little chance for life to emerge on a super-Earth

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