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Mass Flux in the Ancient Earth-Moon System and Benign Implications for the Origin of Life on Earth

机译:古代月球系统中的质量通量及其对地球生命起源的良性启示

摘要

The origin of life on Earth is commonly considered to have been negatively affected by intense impacting in the Hadean, with the potential for the repeated evaporation and sterilization of any ocean. The impact flux is based on scaling from the lunar crater density record, but that record has no tie to any absolute age determination for any identified stratigraphic unit older than approx. 3.9 Ga (Nectaris basin). The flux can be described in terms of mass accretion, and various independent means can be used to estimate the mass flux in different intervals. The critical interval is that between the end of essential crustal formation (approx. 4.4 Ga) and the oldest mare times (approx. 3.8 Ga). The masses of the basin-forming projectiles during Nectarian and early Imbrian times, when the last 15 of the approx.45 identified impact basins formed, can be reasonably estimated as minima. These in sum provide a minimum of 2 x 10(exp 21)g for the mass flux to the Moon during those times. If the interval was 80 million years (Nectaris 3.90 Ga, Orientale 3.82 Ga), then the flux was approx. 2 x 10(exp 13) g/yr over this period. This is higher by more than an order of magnitude than a flux curve that declines continuously and uniformly from lunar accretion to the rate inferred for the older mare plains. This rate cannot be extrapolated back increasingly into pre-Nectarian times, because the Moon would have added masses far in excess of itself in post-crust-formation time. Thus this episode was a distinct and cataclysmic set of events. There are approx. 30 pre-Nectarian basins, and they were probably part of the same cataclysm (starting at approx. 4.0 Ga?) because the crust is fairly intact, the meteoritic contamination of the pre-Nectarian crust is very low, impact melt rocks older than 3.92 Ga are virtually unknown, and ancient volcanic and plutonic rocks have survived this interval. The accretionary flux from approx. 4.4 to approx. 4.0 Ga was comparatively benign. When scaled to Earth, even the late cataclysm does not produce oceane vaporating, globally sterilizing events. The rooted concept that such events took place is based on the extrapolation of a nonexistent lunar record to the Hadean. The Earth from approx. 4.4 to approx. 3.8 Ga was comparatively peaceful, and the impacting itself could have been thermally and hydrothermally beneficial. The origin of life could have taken place at any time between 4.4 and 3.85 Ga, given the current impact constraints, and there is no justification for the claim that life originated (or re-originated) as late as 3.85 Ga in response to the end of hostile impact conditions.
机译:人们普遍认为,地球生命的起源受到哈德族人强烈冲击的负面影响,并有可能反复蒸发和消毒任何海洋。冲击通量基于月球陨石坑密度记录的缩放比例,但该记录与确定的任何早于大约30年前的地层单位的绝对年龄确定无关。 3.9 Ga(油桃盆地)。可以用质量增加来描述通量,并且可以使用各种独立的手段来估计不同间隔中的质量通量。临界时间间隔是在基本地壳形成结束(约4.4 Ga)和最古老的母马时间(约3.8 Ga)之间。在Nectarian时期和Imbrian早期,形成盆地的抛射物的质量可以合理地估计为最小值,当大约45个已识别的冲击盆地中的最后15个形成时。总的来说,这些时间提供了至少2 x 10(exp 21)g的质量通向月球的质量。如果该间隔为8000万年(Nectaris 3.90 Ga,Orientale 3.82 Ga),则通量约为。在此期间,每年2 x 10(exp 13)g。这比通量曲线高出一个数量级以上,通量曲线从月球吸积到均匀的下降,从较早的母马平原连续而均匀地下降。不能将这种速率越来越多地推论到花前油画时代,因为在地壳形成后的月球中,月亮的质量将远远超过其自身。因此,这一事件是一系列独特而灾难性的事件。有大约。 30个花前期的盆地,它们可能是同一大灾变的一部分(始于约4.0 Ga?),因为地壳相当完好,花前期地壳的陨石污染非常低,撞击了3.92岁以上的熔岩Ga几乎是未知的,古老的火山岩和深成岩在此间隔中幸存下来。大约从4.4至约4.0 Ga相对良性。当缩放到地球时,即使是大灾变也不会产生海洋蒸发,全球性灭菌事件。发生此类事件的根源是根据不存在的月球记录推断给哈德族人。从大约地球。 4.4至约3.8 Ga相对和平,撞击本身可能在热和水热方面都是有益的。鉴于目前的影响,生命起源可能发生在4.4至3.85 Ga之间的任何时间,并且没有理由声称生命起源于(或重新起源)迟至3.85 Ga以应对生命的结束。不利的影响条件。

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    Ryder Graham;

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  • 年度 2002
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