Oberbeck V R, Fogleman G
NASA Ames Research Center, Moffett Field, CA 94035, USA.
Orig Life Evol Biosph. 1989;19(6):549-60. doi: 10.1007/BF01808117.
Fossils of the oldest microorganisms exist in 3.5 billion year old rocks and there is indirect evidence that life may have existed 3.8 billion years ago (3.8 Ga). Impacts able to destroy life or interrupt prebiotic chemistry may have occurred after 3.5 Ga. If large impactors vaporized the oceans, sterilized the planets, and interfered with the origination of life, life must have originated in the time interval between these impacts which increased with geologic time. Therefore, the maximum time required for the origination of life is the time that occurred between sterilizing impacts just before 3.8 Ga or 3.5 Ga, depending upon when life first appeared on Earth. If life first originated 3.5 Ga, and impacts with kinetic energies between 2 x 10(34) and 2 x 10(35) were able to vaporize the oceans, using the most probable impact flux, we find that the maximum time required to originate life would have been 67 to 133 million years (My). If life first originated 3.8 Ga, the maximum time to originate life was 2.5 to 11 My. Using a more conservative estimate for the flux of impacting objects before 3.8 Ga, we find a maximum time of 25 My for the same range of impactor kinetic energies. The impact model suggest that it is possible that life may have originated more than once.
最古老微生物的化石存在于35亿年前的岩石中,并且有间接证据表明生命可能在38亿年前(38亿年)就已存在。能够毁灭生命或中断前生物化学过程的撞击可能发生在35亿年之后。如果大型撞击体使海洋汽化、使行星绝育并干扰生命起源,那么生命必定起源于这些撞击之间的时间间隔,且这个间隔会随着地质时间而增加。因此,生命起源所需的最长时间是在38亿年前或35亿年前的灭菌撞击之前发生的时间,这取决于生命最初在地球上出现的时间。如果生命最早起源于35亿年前,并且动能在2×10³⁴到2×10³⁵之间的撞击能够使海洋汽化,使用最可能的撞击通量,我们发现生命起源所需的最长时间将为6700万至1.33亿年。如果生命最早起源于38亿年前,生命起源的最长时间为250万至1100万年。使用对38亿年前撞击物体通量更保守的估计,对于相同范围的撞击体动能,我们发现最长时间为2500万年。撞击模型表明生命有可能不止一次起源。