News Archive

posted 05/16/02

Contact: Mary Tobin
845-365-8607 or mtobin@ei.columbia.edu

Age of Dinosaurs Bracketed by Asteroid or Comet Impacts
Columbia Scientists Link the Rise of the Giant Jurassic Dinosaurs With an Explosive Extraterrestrial Collision

Largest Late Triassic theropod track fromthe Culpeper basin, Virgina. Scale on right applies here as well. (Tracks discovered by Robert Weems, USGS). Photo by P.E. Olsen

Example of earliest Jurassic theropod track Eubrontes giganteus from just above Triassic Jurassic boundary, Newark basin, Clifton, New Jersey. Photo by P.E. Olsen

An asteroid or comet impact on Earth may have paved the way for the sudden rise of the great Jurassic dinosaurs, according to a paper to be published this week in the journal Science. Dr. Paul Olsen from the Columbia Earth Institute's Lamont-Doherty Earth Observatory and an international team of scientists reached their conclusion from an examination of a number of clues - iridium, skeletal remains, footprints, and fern spores - that create a picture of life at the dawn of the Jurassic period.

"The cause and timing of the ascent of dinosaurs has have been much debated. It has been impossible to draw any specific conclusions because the transition between the origin of dinosaurs and their ascent to dominance has not been sampled at very low levels ofin detail. Our last 10 years of studying the clues held in lake sediments in eastern North America has provided us with high-resolution data that records the rise of dinosaurs across 10 degrees of latitude in strata, which, at the time, were in the tropics. This allows us to measure time in thousands of years, instead of millions as in previous studies," said Dr. Olsen.

Example of small theropod track (Grallator parallelum) from near Boyertown, Pennsylvania. Track length about 3 inches. Photo by P.E. Olsen

Olsen and his colleagues studied vertebrate fossils from 80 sites in four different ancient rift basins, part of a chain of rifts that formed as North America began to drift awaysplit apart from the supercontinent that existed 230-190 million years ago. These basins include half- to four-mile thick sections of continental strata, termed and are part of what is called the Newark Supergroup, deposited during dating to the end of the Triassic and beginning of the Jurassic periods. Examination of these strata shows that the enormous carnivorous theropod dinosaurs arose less than 30 thousand years, -- a geological blink of an eye, -- after a mass extinction on Earth. The researchers have linked the extinction with a quadrupling of iridium levels abundance and a spike in the concentration of fern spores found in outcropping sediments in one of these rifts, the Newark basin of New York, New Jersey, and Pennsylvania. Iridium is an element similar to platinum that is very rare in the Earth's crust, but relatively more abundant in most extraterrestrial matter. The increase of iridium in the Newark Supergroup basins may thus indicate an asteroid or comet impact. The fern spore spike is believed to be the product of a post-catastrophe ecosystem in which ferns were the first to colonize the decimated landscape. This is virtually the same scenario, now widely accepted, that resulted in the elimination of the dinosaurs 65 million years ago.

The scientists postulate that the asteroid or comet impact and the resulting death of Triassic competitors allowed a few groups of carnivorous dinosaurs to evolve in size very quickly and dominate the top of the terrestrial food chain globally.

Type specimen of Eubrontes giganteus from Holyoke, Massachusetts (Hartford basin). This was the first dinosaur footprint ever described (1836). (Amherst College specimen 15/3) Photo by P.E. Olsen.

By looking at fossilized footprints and skeletal remains from the Newark Supergroup basins, Olsen and his team determined that the giant theropods appeared less than 30,000 thousand thousand years after the mass extinction of Triassic fauna, and that the peak of dinosaurian diversity in these rift basins occurred only a mere 100,000 thousand years into the Jurassic period. This was clearly a period of explosive evolution, which gave rise to the dinosaur-dominated communities that prevailed prevailing on earth Earth for the next 135 million years.

The research team led by Olsen's research team focused on the Newark Supergroup basins because the lake sediments allow of the clear demarcation of the line between the Triassic and Jurassic periods -- within lake sediments occurring about 200 million years ago -- to be clearly demarcated. The lake sediments recorded cyclical climate changes caused by periodic changes in the Earth's orbit, allowing for a very precise, (in geological terms), measure of time.

Future research in the Newark Supergroup will test how widespread the iridium anomaly is in order to make sure it is actually a global phenomena, as well as search for additional geochemical and paleontological clues on the origin of the mass extinction of the Triassic period taxa that allowed for the great Jurassic age of dinosaurs.

Dr. Paul E. Olsen holds the Storke Memorial Chair in the Department of Earth and Environmental Sciences at Lamont-Doherty Earth Observatory of Columbia University. He studies Triassic and Jurassic continental ecosystems, paleobiology, paleoclimate, stratigraphy, "lower" vertebrate systematics, and paleobiology, including dinosaur and other tetrapod footprints.

The research was funded by grants from the U.S. National Science Foundation and the Austrian Science Foundation.

The Lamont-Doherty Earth Observatory is one of the world's leading research centers examining the planet from its core to its atmosphere, across every continent and every ocean. From global climate change to earthquakes, volcanoes, environmental hazards and beyond, Observatory scientists continue to provide the basic knowledge of Earth systems that must inform the difficult decisions that will determine the future health and habitability of our planet.

Newark Supergroup

A: Pangea during the Late Triassic. Rift zone is in gray;  the Newark Supergroup basins are in black; and the Newark basin (1) is in red.
B: Present-day map showing positions of the major outctopping basins of the Newark Supergroup.
Image by P.E. Olsen.

Related Links:

More images from Dr. Olsen:
http://www.ldeo.columbia.edu/~polsen/nbcp/science/ascent.linked.to.ir.html

Dr. Paul Olsen's Web Site:
http://www.ldeo.columbia.edu/~polsen/nbcp/peo.cv1.html

About The Earth Institute
The Earth Institute at Columbia University is the world's leading academic center for the integrated study of Earth, its environment and society. The Earth Institute builds upon excellence in the core disciplines — earth sciences, biological sciences, engineering sciences, social sciences and health sciences — and stresses cross-disciplinary approaches to complex problems. Through research, training and global partnerships, it mobilizes science and technology to advance sustainable development, while placing special emphasis on the needs of the world's poor. For more information, visit www.earth.columbia.edu.