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  • Kansas Legislator Proposes Bill to Outlaw Sustainability Education
    A bill has been introduced in the Kansas legislature this week that would prohibit the promotion of ...Read more

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    Kansas Legislator Proposes Bill to Outlaw Sustainability Education

    A bill has been introduced in the Kansas legislature this week that would prohibit the promotion of sustainability. Here is a link to the one-page bill: http://www.kslegislature.org/li/b2013_14/measures/documents/hb2366_00_0000.pdf. See report on Bloomberg News.
  • Earth's Center Is 1,000 Degrees Hotter Than Previously Thought, Synchrotron X-Ray Experiment Shows
    Scientists have determined the temperature near the Earth’s center to be 6000 degrees Celsius, 1000 ...Read more

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    Earth's Center Is 1,000 Degrees Hotter Than Previously Thought, Synchrotron X-Ray Experiment Shows

    Scientists have determined the temperature near the Earth’s center to be 6000 degrees Celsius, 1000 degrees hotter than in a previous experiment run 20 years ago. These measurements confirm geophysical models that the temperature difference between the solid core and the mantle above, must be at least 1500 degrees to explain why the Earth has a magnetic field. For more information about this study, see the press release from the European Synchrotron Radiation Facility.
  • Ocean Volcanic Rocks Contain Samples of Recycled Crust
    Scientists have long believed that lava erupted from certain oceanic volcanoes contains materials fr...Read more

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    Ocean Volcanic Rocks Contain Samples of Recycled Crust

    Scientists have long believed that lava erupted from certain oceanic volcanoes contains materials from the early Earth’s crust. But decisive evidence for this phenomenon has proven elusive. New research from a team including Carnegie’s Erik Hauri demonstrates that oceanic volcanic rocks contain samples of recycled crust dating back to the Archean era 2.5 billion years ago. Their work is published in Nature. Oceanic crust sinks into the Earth’s mantle at so-called subduction zones, where two plates come together. Much of what happens to the crust during this journey is unknown. Model-dependent studies for how long subducted material can exist in the mantle are uncertain and evidence of very old crust returning to Earth’s surface via upwellings of magma has not been found until now. For more information about these results, see the press release from the Carnegie Institution.

Happenings During the Mesozoic Era (248-65 Million Years Ago)

Time:
248 to 65 million years ago
Geologic periods (divisions) of the Mesozoic: Triassic, Jurassic, and Cretaceous
(See the geologic timescale!)

Paleogeography:
At the start of the Mesozoic, the continents were all together in a supercontinent called Pangaea. Throughout the Mesozoic, they pulled apart from one another. A narrow version of the Atlantic Ocean developed as ocean crust was formed at the mid-Atlantic ridge. Continents move due to plate tectonics.

Climate:

  • The climate most likely remained warm throughout the Mesozoic. There is no geologic evidence of glaciations and abundant fossil evidence of tropical species have been discovered.
  • During the first part of the Cretaceous period (late Mesozoic) there is evidence that the climate warmed greatly and was warmer than it is today. Regional climate variations were negligible. There was little temperature variation between the equator and poles.
  • There is strong evidence that relatively sudden climatic cooling occurred at the end of the Mesozoic as a result of either a massive asteroid impact near the Yucatan Peninsula, extensive volcanism in the area that is today India and Pakistan, or the combined effects of both events. The asteroid may even have been large enough to cause the volcanism, or the events may have just happened coincidentally at about the same time. The Sun would have been blocked for some time by debris sent into the atmosphere by the impact and eruptions, cooling the planet.

Evolutionary Events:

  • Dinosaurs evolved in the Triassic and became abundant by the middle of the Mesozoic. Dinosaurs were reptiles, however there is evidence that they may have been warm-blooded.
  • Birds: During the late Mesozoic, birds most likely evolved from a group of small carnivorous dinosaurs called theropods.
  • Plants: Conifer trees evolved at the beginning of the Mesozoic. The first flowering plants evolved during the Cretaceous.
  • Mammals evolved during the Mesozoic but there were relatively few species and they were small in size. During the Mesozoic, mammals were most likely food for predatory dinosaurs.
  • At the end of the Mesozoic, the Cretaceous Tertiary Mass Extinction occurred. This was the extinction event that killed the dinosaurs (among others). Many of the animals and plants that survived (such as mammals and birds) went on to become very abundant afterward in the Cenozoic. Likely causes of the extinction event include one or more large asteroid impacts, widespread volcanism, and climate change. There is evidence that all three of these happened.

Last modified August 23, 2009 by Jennifer Bergman.

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The Fall 2010 issue of The Earth Scientist, focuses on rocks and minerals, including articles on minerals and mining, the use of minerals in society, and rare earth minerals, and includes 3 posters!

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