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  2. Tafraout Group - Wikipedia

    en.wikipedia.org/wiki/Tafraout_Group

    The eastern and northeastern High Atlas saw the development of carbonate sedimentation, with reefs and marine fossils indicating tectonic activity during the Late Toarcian. [ 5 ] [ 30 ] The central High Atlas region features long diapirs and minibasins formed during early Jurassic rifting, with the Tazoult Ridge being a key example. [ 31 ]

  3. Fossil - Wikipedia

    en.wikipedia.org/wiki/Fossil

    The usefulness of fossils as medicine is almost entirely a placebo effect, though fossil material might conceivably have some antacid activity or supply some essential minerals. [127] The use of dinosaur bones as "dragon bones" has persisted in Traditional Chinese medicine into modern times, with mid-Cretaceous dinosaur bones being used for the ...

  4. John Day Fossil Beds National Monument - Wikipedia

    en.wikipedia.org/wiki/John_Day_Fossil_Beds...

    John Day Fossil Beds National Monument is a U.S. national monument in Wheeler and Grant counties in east-central Oregon.Located within the John Day River basin and managed by the National Park Service, the park is known for its well-preserved layers of fossil plants and mammals that lived in the region between the late Eocene, about 45 million years ago, and the late Miocene, about 5 million ...

  5. 9-million-year-old marine fossils found beneath California ...

    www.aol.com/news/9-million-old-marine-fossils...

    Millions of prehistoric marine fossils were discovered beneath a California high school over the course of a multi-year construction project. The relics recovered at San Pedro High School included ...

  6. Timeline of natural history - Wikipedia

    en.wikipedia.org/wiki/Timeline_of_natural_history

    c. 3,480 Ma – Fossils of microbial mat found in 3.48 billion-year-old sandstone discovered in Western Australia. [11] [12] First appearance of stromatolitic organisms that grow at interfaces between different types of material, mostly on submerged or moist surfaces. c. 3,460 Ma – Fossils of bacteria in chert.

  7. History of Earth - Wikipedia

    en.wikipedia.org/wiki/History_of_Earth

    A 580 million year old fossil of Spriggina floundensi, an animal from the Ediacaran period. Such life forms could have been ancestors to the many new forms that originated in the Cambrian Explosion. The end of the Proterozoic saw at least two Snowball Earths, so severe that the surface of the oceans may have been completely frozen.

  8. Cambrian explosion - Wikipedia

    en.wikipedia.org/wiki/Cambrian_explosion

    The Cambrian explosion (also known as Cambrian radiation [1] or Cambrian diversification) is an interval of time beginning approximately in the Cambrian period of the early Paleozoic, when a sudden radiation of complex life occurred and practically all major animal phyla started appearing in the fossil record.

  9. Cretaceous–Paleogene extinction event - Wikipedia

    en.wikipedia.org/wiki/Cretaceous–Paleogene...

    [262] [254] Plant fossils record a 250 ppm increase in carbon dioxide concentrations across the K-Pg boundary likely attributable to Deccan Traps activity. [263] The increased carbon dioxide emissions also caused acid rain, evidenced by increased mercury deposition due to increased solubility of mercury compounds in more acidic water.

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