The ca 252 Ma Permian–Triassic boundary (PTB) represents the most severe mass extinction event of the Phanerozoic, with the disappearance of ~ 80% of marine invertebrate species. Large-scale eruption of the Siberian Traps is the commonly favored cause, although the link between volcanism and extinction remains debated. Here, we report evidence for an extraterrestrial 3He influx in the PTB section of deep-sea bedded cherts from Japan. This unusual signal indicates a significant increase in the influx of interplanetary dust particles, likely related to an asteroid shower in the inner solar system. High-resolution stratigraphy indicates that the peak flux of dust particles occurred during the final 500 kyr of the Permian, concurrent with a pre-extinction decline in radiolarian diversity.
机构:
Univ Calif Santa Barbara, Inst Crustal Studies, Dept Geol Sci, Santa Barbara, CA 93106 USAUniv Calif Santa Barbara, Inst Crustal Studies, Dept Geol Sci, Santa Barbara, CA 93106 USA
Becker, L
Poreda, RJ
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机构:Univ Calif Santa Barbara, Inst Crustal Studies, Dept Geol Sci, Santa Barbara, CA 93106 USA
机构:
Astrogeobiology Laboratory, Department of Physics, Lund University, Box 118, LundAstrogeobiology Laboratory, Department of Physics, Lund University, Box 118, Lund
Martin E.
Schmitz B.
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机构:
Astrogeobiology Laboratory, Department of Physics, Lund University, Box 118, LundAstrogeobiology Laboratory, Department of Physics, Lund University, Box 118, Lund
Schmitz B.
Montanari A.
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机构:
Osservatorio Geologico di Coldigioco, ApiroAstrogeobiology Laboratory, Department of Physics, Lund University, Box 118, Lund
Montanari A.
Special Paper of the Geological Society of America,
2019,
542
: 303
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318