STAGGERING ABUNDANCE: FOSSILS OF MCABEE

2009 EIGHTH BC PALEONTOLOGICAL SYMPOSIUM

Eighth British Columbia Paleontological Symposium

Presented by the Vancouver Paleontological Society,
University of British Columbia, Earth and Ocean Sciences, and
British Columbia Paleontological Alliance
MAY 15-18, 2009

Call for Posters & Abstracts

2009 BCPA CONFERENCE - The Vancouver Paleontological Society invites you the Eighth British Columbia Paleontological Symposium, to be held at the University of British Columbia, May 15-18, 2009.

KEYNOTE SPEAKER - This year’s keynote speaker will be Dr. Gregory Wilson, a specialist on the evolution and ecology of early mammals, University of California, Berkeley, Department of Integrative Biology. Continuing the format of past symposia, the meeting will bring together both the professional and avocational paleontological community.

As well as an engaging line-up of speakers, there will also be field trips, workshops, retail booth and the return of the popular Paleo Art Show with juried prizes. A Community Open House will be held on the Sunday for members of the general public.

FOSSIL MAMMALS - While the symposium will highlight fossil mammals, we invite talks, posters and displays showcasing all aspects of paleontology, with non-academics especially encouraged to contribute.

SYMPOSIUM ABSTRACT VOLUME - There will be a symposium abstract volume published and provided to all registrants. We request that speakers and poster presenters submit abstracts for the publication. Abstracts can be 1-4 pages (with 1 being standard) in length. Mailing and e-mail address of the author should be included for insertion in the volume.

DEADLINE FOR SUBMISSION of posters and abstracts for publication is April 10, 2009. Submission of an abstract is mandatory for speakers and poster displays. Paleontologists unable to make the meeting but interested in contributing to the abstract volume to share their research on fossil mammals are welcome to contribute.

REGISTRATION – FULL SYMPOSIUM PASS
Professional Paleontologists $100 | Non-BCPA attendees $100 | BCPA Members $80 | Students $60

SEND CHEQUE PAYABLE TO:
Vancouver Paleontological Society, Centrepoint P.O. Box 19653, Vancouver, BC, V5T 4E7

FOR MORE INFORMATION:
www.bcfossils.ca | http://www.vcn.bc.ca/vanps/ | fossilhuntress@hotmail.co.uk

FOTO NATUREN

TRIASSIC-JURASSIC EXTINCTION

Located as they are in Canada’s most active earthquake zone, the Queen Charlotte Islands have had their share of shake-ups and scourings. Many of the Islands’ hillsides are scarred by slides (any specific examples?). But the rock beneath speaks of an even more violent past. Very few people know that the rock in the Queen Charlottes holds the key to a catastrophic event from eons ago.We’ve heard tales and seen images of the cataclysmic damage caused by meteriorites smashing into the Earth’s surface.

Until recently, it was a meteorite impact that was blamed for the worldwide Triassic/Jurassic Mass Extinction. This wholesale dying out of species occurred some 200 million years ago. New evidence challenges the meteorite theory. Experts now believe that tectonic forces may have caused hundreds of volcanoes around the world to erupt simultaneously. The subsequent showers of volcanic ash would have altered the composition of the atmosphere dramatically and plunged the world into near total darkness for years until it settled from the sky.

The picture painted of the sun flickering fitfully through inky clouds, paling against the torrents of glowing lava, while everywhere life is smothered, poisoned, or starved, rivals the most apocalyptic imaginings of Hollywood or religion. We know from worldwide evidence that the extinction was dramatic and affected upwards of 70% of the world’s biota.


Perhaps counterintuitively, for one might think of water as a refuge from fire, smoke, and lava, it was marine lifeforms that suffered the most. This is particularly well documented in the rocks of the Queen Charlottes, especially at Kennecott Point and Kunga Island.

Radiolarian microfossils – tiny, siliceous, single-celled microrganisms – tell the tale. In the Upper Triassic rocks, which predate the extinction by about 10 million years, radiolarians are preserved in hundreds of forms. Just above them, in the early Jurassic rock layers laid down about the time of the great die-offs, only a fraction of the previous number of forms are represented. The more recent Jurassic rock shows a rebound of radiolarian diversity (though of course, in different forms) — a diversity which continues to flourish and expand in today’s oceans.