Statements in which the resource exists as a subject.
PredicateObject
rdf:type
lifeskim:mentions
pubmed:issue
41
pubmed:dateCreated
2007-10-16
pubmed:abstractText
A carbon-rich black layer, dating to approximately 12.9 ka, has been previously identified at approximately 50 Clovis-age sites across North America and appears contemporaneous with the abrupt onset of Younger Dryas (YD) cooling. The in situ bones of extinct Pleistocene megafauna, along with Clovis tool assemblages, occur below this black layer but not within or above it. Causes for the extinctions, YD cooling, and termination of Clovis culture have long been controversial. In this paper, we provide evidence for an extraterrestrial (ET) impact event at approximately equal 12.9 ka, which we hypothesize caused abrupt environmental changes that contributed to YD cooling, major ecological reorganization, broad-scale extinctions, and rapid human behavioral shifts at the end of the Clovis Period. Clovis-age sites in North American are overlain by a thin, discrete layer with varying peak abundances of (i) magnetic grains with iridium, (ii) magnetic microspherules, (iii) charcoal, (iv) soot, (v) carbon spherules, (vi) glass-like carbon containing nanodiamonds, and (vii) fullerenes with ET helium, all of which are evidence for an ET impact and associated biomass burning at approximately 12.9 ka. This layer also extends throughout at least 15 Carolina Bays, which are unique, elliptical depressions, oriented to the northwest across the Atlantic Coastal Plain. We propose that one or more large, low-density ET objects exploded over northern North America, partially destabilizing the Laurentide Ice Sheet and triggering YD cooling. The shock wave, thermal pulse, and event-related environmental effects (e.g., extensive biomass burning and food limitations) contributed to end-Pleistocene megafaunal extinctions and adaptive shifts among PaleoAmericans in North America.
pubmed:commentsCorrections
pubmed:language
eng
pubmed:journal
pubmed:citationSubset
IM
pubmed:chemical
pubmed:status
MEDLINE
pubmed:month
Oct
pubmed:issn
0027-8424
pubmed:author
pubmed:issnType
Print
pubmed:day
9
pubmed:volume
104
pubmed:owner
NLM
pubmed:authorsComplete
Y
pubmed:pagination
16016-21
pubmed:dateRevised
2010-9-15
pubmed:meshHeading
pubmed-meshheading:17901202-Animals, pubmed-meshheading:17901202-Carbon, pubmed-meshheading:17901202-Climate, pubmed-meshheading:17901202-Earth (Planet), pubmed-meshheading:17901202-Ecosystem, pubmed-meshheading:17901202-Extinction, Biological, pubmed-meshheading:17901202-Geological Phenomena, pubmed-meshheading:17901202-Geology, pubmed-meshheading:17901202-Humans, pubmed-meshheading:17901202-Ice, pubmed-meshheading:17901202-Iridium, pubmed-meshheading:17901202-Magnetics, pubmed-meshheading:17901202-Meteoroids, pubmed-meshheading:17901202-Models, Theoretical, pubmed-meshheading:17901202-North America, pubmed-meshheading:17901202-Physical Phenomena, pubmed-meshheading:17901202-Physics, pubmed-meshheading:17901202-Soil, pubmed-meshheading:17901202-Thallium Radioisotopes, pubmed-meshheading:17901202-Time Factors, pubmed-meshheading:17901202-Uranium
pubmed:year
2007
pubmed:articleTitle
Evidence for an extraterrestrial impact 12,900 years ago that contributed to the megafaunal extinctions and the Younger Dryas cooling.
pubmed:affiliation
Lawrence Berkeley National Laboratory, Berkeley, CA 94720, USA. rbfirestone@lbl.gov
pubmed:publicationType
Journal Article, Research Support, U.S. Gov't, Non-P.H.S.