Wednesday, October 13 5:17 pm
The Museum’s leadership in scientific discovery and research dates back to its founding. To celebrate National Fossil Day, October 13, 2010, the Museum hosted a number of educational activities for school groups: fossil experts used ‘touch carts’ to give students a hands-on look at some of the fossils featured in the Museum’s permanent exhibit halls, and students explored more about how fossils are formed, dated, and collected. Museum scientist Neil Landman’s newly-published research on ammonites will provide even more to discuss.
Although ammonites — shelled mollusks closely related to modern day nautilus and squids — have been extinct for 65 million years, newly published data based on 35 years of research is providing invaluable insights into their paleobiology. Specimens found in the rock record of an ancient seaway that covered North America during the Cretaceous Period reveal fascinating details: ammonites thrived at cold methane seeps that supported diverse ecosystems at the bottom of the sea, consumed small prey, and often survived attacks from predators.
About 70 million years ago, what is now North America was divided in half by a broad inland sea that covered much of the continent. This epicontinental sea, according to the new research published in the Bulletin of the American Museum of Natural History, contained cold methane seeps of bubbling gas that created underwater oases. These ecosystems attracted and supported organisms like bacteria, sponges, gastropods, bivalves, sea urchins, sea lilies, and ammonites.
“You have to imagine the underwater scene 70 million years ago,” says Neil Landman, curator in the Division of Paleontology at the Museum. “A cloud of zooplankton, with ammonites flocking to the vents, forming isolated communities surrounded by the muddy sea floor. Because the sedimentation rates in the seaway were so rapid, the ammonites and other organisms were buried quickly after death, preserving exquisite details of their morphology.”
Part of Landman’s ammonite research will be presented at the upcoming Geological Society of America Meetings in Denver.
For more information, please see the official press release.