Origin of the cataclysmic Late Heavy Bombardment period of the terrestrial planets

被引:1214
作者
Gomes, R
Levison, HF
Tsiganis, K
Morbidelli, A
机构
[1] CNRS, Observ Cote Azur, F-06304 Nice, France
[2] MCT, ON, BR-20080090 Rio De Janeiro, Brazil
[3] Univ Fed Rio de Janeiro, OV, GEA, BR-20080090 Rio de Janeiro, Brazil
[4] SW Res Inst, Dept Space Studies, Boulder, CO USA
基金
美国国家科学基金会; 美国国家航空航天局;
关键词
D O I
10.1038/nature03676
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The petrology record on the Moon suggests that a cataclysmic spike in the cratering rate occurred similar to 700 million years after the planets formed(1); this event is known as the Late Heavy Bombardment (LHB). Planetary formation theories cannot naturally account for an intense period of planetesimal bombardment so late in Solar System history(2). Several models have been proposed to explain a late impact spike(3-6), but none of them has been set within a self-consistent framework of Solar System evolution. Here we propose that the LHB was triggered by the rapid migration of the giant planets, which occurred after a long quiescent period. During this burst of migration, the planetesimal disk outside the orbits of the planets was destabilized, causing a sudden massive delivery of planetesimals to the inner Solar System. The asteroid belt was also strongly perturbed, with these objects supplying a significant fraction of the LHB impactors in accordance with recent geochemical evidence(7,8). Our model not only naturally explains the LHB, but also reproduces the observational constraints of the outer Solar System(9).
引用
收藏
页码:466 / 469
页数:4
相关论文
共 19 条
[1]   The fossilized size distribution of the main asteroid belt [J].
Bottke, WF ;
Durda, DD ;
Nesvorny, D ;
Jedicke, R ;
Morbidelli, A ;
Vokrouhlicky, D ;
Levison, H .
ICARUS, 2005, 175 (01) :111-140
[2]  
CHAMBERS JE, 2002, LUNAR PLANET SCI C, V33
[3]   ASTEROID COLLISIONAL EVOLUTION - RESULTS FROM CURRENT SCALING ALGORITHMS [J].
DAVIS, DR ;
RYAN, EV ;
FARINELLA, P .
PLANETARY AND SPACE SCIENCE, 1994, 42 (08) :599-610
[4]   SOME DYNAMICAL ASPECTS OF THE ACCRETION OF URANUS AND NEPTUNE - THE EXCHANGE OF ORBITAL ANGULAR-MOMENTUM WITH PLANETESIMALS [J].
FERNANDEZ, JA ;
IP, WH .
ICARUS, 1984, 58 (01) :109-120
[5]   Planetary migration in a planetesimal disk: why did Neptune stop at 30 AU? [J].
Gomes, RS ;
Morbidelli, A ;
Levison, HF .
ICARUS, 2004, 170 (02) :492-507
[6]   Dynamical effects of planetary migration on the primordial, asteroid belt [J].
Gomes, RS .
ASTRONOMICAL JOURNAL, 1997, 114 (01) :396-401
[7]   Orbital evolution of planets embedded in a planetesimal disk [J].
Hahn, JM ;
Malhotra, R .
ASTRONOMICAL JOURNAL, 1999, 117 (06) :3041-3053
[8]  
Haisch KE, 2001, ASTROPHYS J, V553, pL153, DOI 10.1086/320685
[9]  
Hartmann W. K., 2000, Origin of the Earth and Moon, P493
[10]   Cataclysmic bombardment throughout the inner solar system 3.9-4.0 Ga [J].
Kring, DA ;
Cohen, BA .
JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS, 2002, 107 (E2)