Planet Formation and Panspermia. Группа авторов

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Название Planet Formation and Panspermia
Автор произведения Группа авторов
Жанр Физика
Серия
Издательство Физика
Год выпуска 0
isbn 9781119640936



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discovery of live 250 Myr old halophilic bacteria in a grain of salt [4.31] implies the possibility that panspermia could be viable even on galactic time scales. The Galactic Solar orbit lasts a little under a quarter of a billion years. On even shorter timescales, there is a possibility that neighboring stellar systems could exchange material. The recent discoveries of the Oumuamua [4.26] asteroid-like object and comet 2I/Borisov [4.17, 4.21], that show hyperbolic orbital characteristics of extrasolar bodies, have demonstrated that external objects can traverse the Solar system, which makes it possible that some of them could eventually be captured or sampled. The galaxies are the main form of organization of matter in the universe. Galactic evolution and underlying processes link the evolution of matter on stellar/planetary scales and smaller, to the overall evolution of the universe. In a similar way, stars with their planetary systems can be considered as pivotal objects for the evolution of life. While their evolution and appearance are influenced by galactic scale processes, they provide suitable conditions for biochemistry to take place. Some of these processes might arguably take place in the interstellar molecular and dust clouds, but these are also the birthplaces of stars and planets.

      Following the overall organization of matter in the universe, we discuss the panspermia prospects from stellar to cosmological levels.

      4.2.1 Stellar System Level

Schematic illustration of the levels of influences of matter and their inter-relations in regard to panspermia.

      4.2.2 Galaxies: Cosmic Cradles of Life

      Similar to [4.8], the following formalism is usually used to estimate the stellar collision cross-section [4.23]:

      (4.1)images

      where the right-hand side variables are stellar density, velocity, and collision cross-section, respectively. Following the simulations from [4.20], the author uses <σ> = 100 AU2, as the average value for the collisions that have a disruptive potential for terrestrial planets. We can consider it likely that an order of magnitude larger values, for a collision distance (parameter), of b = 100 AU ≈ 5 × 10−4pc, would be sufficient to disturb the small bodies of the target stellar system, consequently scattering some of them into interstellar space. This relates to the small bodies that are relatively close to the inner terrestrial planets, such as the asteroid belt in the Solar system. However, such objects can be found more loosely bound and in much larger numbers in the outer Solar system. Given that the Oort Cloud could stretch as far as 105 AU [4.27], a nearby stellar passage at even 0.5 pc, could send swarms of icy and rocky objects into interstellar travel. However, these more distant objects are likely to be the pristine remnants from the stellar system formation, and less likely to have contact with the inner parts of a stellar system, where complex biochemistry could take place and aggregate the organics, originating from molecular clouds, into actual living forms.

      The existence of such an extensive structure of small objects around the Solar system would imply that our Earth did not suffer much from flyby perturbations throughout its history. The dynamically unexcited Kuiper belt implies that the Solar system did not have encounters with other stars within 240 AU [4.6] in its birth cluster as well as in its current galactic environment. An estimate of the collision parameter value that is most effective in terms of ejecting the panspermia material is likely to be a matter of fine tuning. However, a caution should be made here, since a radically different (unknown) form of life (e.g., Dyson’s “cometary trees” or Lem’s cloud of Y-shaped microscopic components) might be preferentially propagated by different kind of ejection events, with different ejection parameters, creating a kind of natural selection between these different “panspermias”.

      The material ejected from binary systems should, then, on average, have less evolved living matter. The more potent panspermia material should be expected to originate from single star planetary systems that had flybys as close as ~102 AU. Flybys at ~103 AU are likely to scatter around only the debris of small bodies that did not change their biological complexity much since the formation of the given stellar system. This might still be important for the overall astrobiological landscape, depending on the timescales involved. Even if it consists just of prebiotic complex chemicals, it might delineate the part of the GHZ containing a set of biospheres of a particular kind.

      Capture time scales and collision cross-sections for single and multiple stellar systems are