Note to users. If you're seeing this message, it means that your browser cannot find this page's style/presentation instructions -- or possibly that you are using a browser that does not support current Web standards. Find out more about why this message is appearing, and what you can do to make your experience of our site the best it can be.


Science 23 July 2004:
Vol. 305. no. 5683, p. 492
DOI: 10.1126/science.1098481

Brevia

Comet or Asteroid Shower in the Late Eocene?

Roald Tagle1 and Philippe Claeys2*

The passage of a comet shower ~35 million years ago is generally advocated to explain the coincidence during Earth's late Eocene of an unusually high flux of interplanetary dust particles and the formation of the two largest craters in the Cenozoic, Popigai and the Chesapeake Bay. However, new platinum-group element analyses indicate that Popigai was formed by the impact of an L-chondrite meteorite. Such an asteroidal projectile is difficult to reconcile with a cometary origin. Perhaps instead the higher delivery rate of extraterrestrial matter, dust, and large objects was caused by a major collision in the asteroid belt.

1 Institut fuer Mineralogie, Museum fuer Naturkunde, D-10099 Berlin, Germany.
2 Department of Geology, Vrije Universiteit Brussel, Pleinlaan 2, B-1050 Brussels, Belgium.

* To whom correspondence should be addressed. E-mail: phclaeys{at}vub.ac.be

Read the Full Text





To Advertise     Find Products


Science. ISSN 0036-8075 (print), 1095-9203 (online)