Hi Bob,
That is interesting but only a short story with no real research exposed yet. How about this headline though.
Dinosaur Extinctions: No Asteroid or Comet Impact Here.
Keywords: Cretaceous-Tertiary Boundary, Late Cretaceous, dinosaurs, bolide impact, impact theory,
volcanic theory, mass extinctions, Field-dynamical Earth Model (FEM), ionizing radiation and extinction .
I bookmarked this site after reading about 12 pages, very interesting. Anyone can use the keywords to
find the story and do more research if they want. I would like to provide a link but only with the mods permission.
Introduction
About 65 million years ago some event took place that wiped out more than half of all life on Earth. In addition to this mass extinction there was a major face-lift for the Earth as a planet. The continents were shoved to new locations, and inland seas moved on and off the continents, as major ridge expansion took place, particularly in the Atlantic and Indian Oceans. In the process there was major mountain building, volcanic eruptions, and some places sunk beneath the sea, while others rose from the sea. There is evidence of massive destabilization of the oceans and atmosphere. Powerful storms wrecked havoc as indicated by vigorous erosion and greatly increased continental weathering. Some elements, known as isotopes, show drastic shifts in abundance. Masses of sand, clay, and mud deposited layers everywhere, while other areas show missing sedimentary layers. The oceans show rapid desalination events, temperature transitions, and chemical changes.
The Late Cretaceous was the last for the dinosaur, and its close was the most catastrophic of any period in the history of life on Earth. More than one half of all the species on Earth became extinct. In some places 75% to 90% of the life forms vanished from the scene never to be seen again in the fossil record. With the close of the Cretaceous there came the wholesale extinction of large marine creatures (Plesiosaurs, Mosasaurs and Icthyosaurs), flying reptiles (Pterosaurs), ancestors of the Chambered Nautilus (Ammonites), Scleractinian and Hermatypic Corals, shellfish (Bivalves, Inoceramids, Rudists, Gastropods and Echnoids), chalk-forming creatures (Coccolithophorids, Planktonic Foraminifera, Beleminites, large Benthic Foraminifera and Radiolaria), and the Dinosaurs. Here was the end of one of the most successful life sytems in all of Earth history. What was it that overwhelmed the Earth?
george.