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Showing posts with label Cretaceous-Paleogene Extinction Event. Show all posts
Showing posts with label Cretaceous-Paleogene Extinction Event. Show all posts

Wednesday, 10 March 2010

Using Grain-Size to Interpret Cretaceous-Paleogene Extinction Event Tuesday, March 9, 2010

Using Grain-Size to Interpret Cretaceous-Paleogene Extinction Event

Tuesday, March 9, 2010 10:47 PM

Bralower, T., L. Eccles, J. Kutz, T. Yancey, J. Schueth, M. Arthur,
and D. Bice, 2010, Grain size of Cretaceous-Paleogene boundary
sediments from Chicxulub to the open ocean: Implications for
interpretation of the mass extinction event. Geology, v. 38,
no. 3, p. 199-202; DOI: 10.1130/G30513.1

http://geology.geoscienceworld.org/cgi/content/abstract/38/3/199


Grain size of Cretaceous-Paleogene boundary sediments from
Chicxulub to the open ocean: Implications for interpretation
of the mass extinction event March 2010 Geology and GSA
Today Highlights.

http://www.physorg.com/wire-news/29077449/march-2010-geology-and-gsa-today-highlights.html


“The causes of the mass extinction of 75% of marine and 50%
of terrestrial species (including the dinosaurs) at the
Cretaceous-Tertiary boundary, 65 million years ago, has been
the subject of raging debate. The majority of scientists support
the theory that the impact of an asteroid on the Yucatan
Peninsula (Mexico) was the trigger of the extinctions. The most
potent evidence for this theory is a layer of rock containing
telltale signs of impact, including melt droplets and shocked
mineral grains that can be traced from the Yucatan around the
world. Basing their research on fossils in rocks around the
Gulf of Mexico, a group of scientists have recently proposed
that the Yucatan impact preceded the mass extinction by 300
thousand years, and that the extinction was caused by a
massive volcanic event in India. The current study by Bralower
et al., however, leads to a different conclusion through the
analysis of sediment particle size in Cretaceous-Tertiary
boundary samples to determine the origin of fossil shells. The
data demonstrate that fossils in Cretaceous-Tertiary boundary
rocks around the Gulf of Mexico region are eroded from
underlying layers by a tsunami at the impact event. Thus
they rule out the correlation of the mass extinction event with
Indian volcanism and conclusively support the connection with
the Yucatan impact.”

Yours,

Paul H.

Thursday, 24 March 2005

Chicxulub Spherules Reveal Details of Catastrophic K-T Fireball

Chicxulub Spherules Reveal Details of Catastrophic K-T Fireball

Paul H bristolia at yahoo.com
Wed Mar 23 12:53:17 EST 2005

"Mystery minerals formed in fireball from colliding
asteroid that destroyed the dinosaurs"
Innovation Report, March 23, 2005

http://www.innovations-report.de/html/berichte/studien/bericht-42101.html

"Scientists at the American Museum of Natural History
and the University of Chicago have explained how a
globe-encircling residue formed in the aftermath of
the asteroid impact that triggered the extinction of
the dinosaurs. The study, which will be published in
the April issue of the journal Geology, draws the
most detailed picture yet of the complicated
chemistry of the fireball produced in the impact."