Geochemical evidence for a comet shower in the late Eocene.Science. 1998 May 22; 280(5367):1250-3.Sci
Abstract
Analyses of pelagic limestones indicate that the flux of extraterrestrial helium-3 to Earth was increased for a 2.5-million year (My) period in the late Eocene. The enhancement began approximately 1 My before and ended approximately 1.5 My after the major impact events that produced the large Popigai and Chesapeake Bay craters approximately 36 million years ago. The correlation between increased concentrations of helium-3, a tracer of fine-grained interplanetary dust, and large impacts indicates that the abundance of Earth-crossing objects and dustiness in the inner solar system were simultaneously but only briefly enhanced. These observations provide evidence for a comet shower triggered by an impulsive perturbation of the Oort cloud.
Links
Publisher Full Text
Pub Type(s)
Journal Article
Research Support, Non-U.S. Gov't
Research Support, U.S. Gov't, Non-P.H.S.
Language
eng
PubMed ID
9596575
Citation
Farley, K A., et al. "Geochemical Evidence for a Comet Shower in the Late Eocene." Science (New York, N.Y.), vol. 280, no. 5367, 1998, pp. 1250-3.
Farley KA, Montanari A, Shoemaker EM, et al. Geochemical evidence for a comet shower in the late Eocene. Science. 1998;280(5367):1250-3.
Farley, K. A., Montanari, A., Shoemaker, E. M., & Shoemaker, C. S. (1998). Geochemical evidence for a comet shower in the late Eocene. Science (New York, N.Y.), 280(5367), 1250-3.
Farley KA, et al. Geochemical Evidence for a Comet Shower in the Late Eocene. Science. 1998 May 22;280(5367):1250-3. PubMed PMID: 9596575.
* Article titles in AMA citation format should be in sentence-case
TY - JOUR
T1 - Geochemical evidence for a comet shower in the late Eocene.
AU - Farley,K A,
AU - Montanari,A,
AU - Shoemaker,E M,
AU - Shoemaker,C S,
PY - 1998/6/20/pubmed
PY - 1998/6/20/medline
PY - 1998/6/20/entrez
SP - 1250
EP - 3
JF - Science (New York, N.Y.)
JO - Science
VL - 280
IS - 5367
N2 - Analyses of pelagic limestones indicate that the flux of extraterrestrial helium-3 to Earth was increased for a 2.5-million year (My) period in the late Eocene. The enhancement began approximately 1 My before and ended approximately 1.5 My after the major impact events that produced the large Popigai and Chesapeake Bay craters approximately 36 million years ago. The correlation between increased concentrations of helium-3, a tracer of fine-grained interplanetary dust, and large impacts indicates that the abundance of Earth-crossing objects and dustiness in the inner solar system were simultaneously but only briefly enhanced. These observations provide evidence for a comet shower triggered by an impulsive perturbation of the Oort cloud.
SN - 0036-8075
UR - https://www.unboundmedicine.com/medline/citation/9596575/Geochemical_evidence_for_a_comet_shower_in_the_late_Eocene_
L2 - https://www.sciencemag.org/cgi/pmidlookup?view=long&pmid=9596575
DB - PRIME
DP - Unbound Medicine
ER -