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Astroecology : ウィキペディア英語版
Astroecology

Astroecology concerns the interactions of biota with space environments. It studies resources for life on planets, asteroids and comets, around various stars, in galaxies, and in the universe. The results allow estimating the future prospects for life, from planetary to galactic and cosmological scales.
Available energy, and microgravity, radiation, pressure and temperature are physical factors that affect astroecology. The ways by which life can reach space environments, including natural panspermia and directed panspermia are also considered. Further, for human expansion in space and directed panspermia, motivation by life-centered biotic ethics, panbiotic ethics and planetary bioethics are also relevant.〔〔
==Overview==
The term "astroecology" was first applied in the context of performing studies in actual meteorites to evaluate their potential resources favorable to sustaining life.〔 Early results showed that meteorite/asteroid materials can support microorganisms, algae and plant cultures under Earth's atmosphere and supplemented with water.
Several observations suggest that diverse planetary materials, similar to meteorites collected on Earth, could be used as agricultural soils, as they provide nutrients to support microscopic life when supplemented with water and an atmosphere.〔 Experimental astroecology has been proposed to rate planetary materials as targets for astrobiology exploration and as potential biological in-situ resources.〔 The biological fertilities of planetary materials can be assessed by measuring water-extractable electrolyte nutrients. The results suggest that carbonaceous asteroids and Martian basalts can serve as potential future resources for substantial biological populations in the Solar System.〔
Analysis of the essential nutrients (C, N, P, K) in meteorites yielded information for calculating the amount of biomass that can be constructed from asteroid resources.〔 For example, carbonaceous asteroids are estimated to contain about 1022 kg potential resource materials, and laboratory results suggest that they could yield a biomass on the order of 6·1020 kg, about 100,000 times more than biological matter presently on Earth.〔

抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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