Deccan Traps: A Different Take

At the recent 2008 AGU meeting in San Francisco, a long simmering controversy reared its head again.  Paleontologists Gerta Keller and Sunil Bajpai and geophysicist Vincent Courtillot presented evidence that India’s Deccan Traps, and not the Chicxlub meteor in Mexico, created the unhealthful conditions that led to the extinction of the dinosaurs.  Their data is thought provoking but what attracted my attention was Dr. Keller’s comment that much of their data came from quarries in the basalt.  

Erupted 65 million years ago, the Deccan Traps covers an area as large as Texas.  Geologists have estimated the volume at 1.2 million cubic kilometers, with nearly half lost to erosion.  The depth of the layers is more than 3,500 meters thick.  At AGU, Keller observed that the viscous basalt spewed forth in as little as 10,000 years. 

Basalt Quarry: Photo from Gerta Keller

The quarries that interest Keller and her colleagues are found in flows that oozed 800 kilometers across India to Rajahmundry, on India’s east coast.  They are the longest lava flows on Earth.  Dozens of quarries pockmark the Rajahmundry traps of the Deccan plateau.  (Trap refers to any dark colored igneous rock though it is most commonly associated with basalt; trap comes from the Swiss word for step.)  According to Dr. Keller, families and extended clans work most of the quarry sites by hand, using hammers and explosives.  Men break up the stone and women carry it out on their heads.  And in some cases, trucks transport rock to people’s homes and dump the material in their backyards, where they work on it. 

Worker at basalt quarry: Photo from Gerta Keller

Because the Rajahmundry basalt resists weathering, much of it goes for roads and to make train beds.  It is shipped to Europe and perhaps to the United States.  Basalt from other flows in India have been used as a building stone, though Dr. Keller did not know if the Rajahmundry stone had gone into buildings. 

The quarries have played an important role in Dr. Keller’s research because they expose the rocks that she has wanted to study.  In the quarries is evidence for shallow marine deposition, where marine microfossils were preserved.  These fossils have been essential to narrowing the date of Deccan Trap deposition and allowing Dr. Keller to further elaborate on her thesis. I am not qualified to say whether her theory is right or wrong, but the work raises some interesting questions and if Dr. Keller is right, you may want to give a second thought to the road you travel on.  It may contain evidence for the dinosaur’s demise.




Airport Fossils

Trapped at SeaTac Airport in Seattle with nothing to do?  I am sure the people stranded there would rather be someplace else but the extra time will allow intrepid travelers to explore the many fossils found in the walls of the food court in concourse A.  The fossils make a captivating cast of characters that lived 155 million years ago in what became Germany.  During the Jurassic Period when dinosaurs roamed the land, a shallow sea covered much of Europe.  Many critters from that sea are now preserved in the tan to gray limestone cladding walls at SeaTac. 

155-million-year old ammonite – Good examples are in the pillars just past the security check, particularly the one nearest Ex-Officio.

The stone is known as the Treuchtlingen Marble, although it is not marble but limestone.  It was never metamorphosed.  As the animals died they settled to the bottom of the sea.  The most common fossils are sponges, bottom dwelling, filter feeders that formed small mounds.  They may be round, straight, or irregularly shaped and are darker than the surrounding limestone.  Also common are ammonites, coiled-shell animals that resemble a top down view of a cinnamon roll.  The biggest ones in the German limestone are about five-inches across, whereas the largest ones that ever lived were six feet wide.  Ammonites were prevalent marine predators in the Jurassic but went extinct at the end of the Cretaceous.  Their modern relatives include squids, chambered nautiluses, and octopi.  

You can also find another squid relative, belemnites, which look like a cigar.  They are dark brown and somewhat shiny.  Also seek out brachiopods, clam-shaped animals known as lampshells due to their resemblance to ancient oil lamps.  Unlike clams, brachiopods cannot move and feed by opening their shell and consuming bits that float by.  And finally, the white specks that look like oatmeal are single-celled sea dwellers called foraminifera. I hope this at least helps some people pass the time at SeaTac.