Scientific Illustration

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  • rhamphotheca:

How to Take a Dinosaur’s Temperature
by Marlene Cimons
For the longest time, most scientists believed it wasn’t possible to  accurately measure the body temperature of dinosaurs. They could only  make educated guesses by, for example, calculating how fast the  creatures ran based on the spacing of their tracks, or from measuring  the growth rates of their bones.
How warm (or cold) these long extinct creatures were remained an enduring mystery — until now. Using a new approach,  a team of researchers led by the California Institute of Technology  (also known as Caltech) figured out how to take the body temperatures of  dinosaurs by analyzing the concentration of certain isotopes preserved  in the mineral bioapatite, found in teeth.
The researchers studied two stable, but slightly heavier, isotopes of  carbon and oxygen — carbon-13 and oxygen-18. The isotopes tend to bond  with each other, or “clump,” at lower temperatures, and the lower the  temperature, the more carbon-13 and oxygen-18 will clump. By analyzing  the clumping of those isotopes, the researchers were able to determine  fairly precise temperature values — to within a range of 2 to 4 deg  F (1 to 2 deg C)…
(read more: Live Science)     (image: Russel Hawley, Tate Geological Museum)

    rhamphotheca:

    How to Take a Dinosaur’s Temperature

    by Marlene Cimons

    For the longest time, most scientists believed it wasn’t possible to accurately measure the body temperature of dinosaurs. They could only make educated guesses by, for example, calculating how fast the creatures ran based on the spacing of their tracks, or from measuring the growth rates of their bones.

    How warm (or cold) these long extinct creatures were remained an enduring mystery — until now. Using a new approach, a team of researchers led by the California Institute of Technology (also known as Caltech) figured out how to take the body temperatures of dinosaurs by analyzing the concentration of certain isotopes preserved in the mineral bioapatite, found in teeth.

    The researchers studied two stable, but slightly heavier, isotopes of carbon and oxygen — carbon-13 and oxygen-18. The isotopes tend to bond with each other, or “clump,” at lower temperatures, and the lower the temperature, the more carbon-13 and oxygen-18 will clump. By analyzing the clumping of those isotopes, the researchers were able to determine fairly precise temperature values — to within a range of 2 to 4 deg F (1 to 2 deg C)…

    (read more: Live Science)     (image: Russel Hawley, Tate Geological Museum)

    Tagged: sauropod dinosaur reptile prehistoric

    Posted on February 18, 2012 via fauna with 73 notes

    1. menofmeasure reblogged this from marywilliams
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      Wot
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    12. spindlebug reblogged this from scientificillustration and added:
      ;__;
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    30. karethdreams reblogged this from sprackraptor and added:
      SCIENCE mfs, it is AWESOME!
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    32. sprackraptor reblogged this from scientificillustration and added:
      this. is. AWESOME. lijwelirjwlkjiljsldf SCIENCE IS BEAUTIFUL.
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    36. crownedrose reblogged this from scientificillustration and added:
      Interesting stuff! The article’s a good read for anyone who wants to know more about this kind of thing.
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