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Why It Matters | Andhra rock questions conditions for life 2M years ago

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Why It Matters | Andhra rock questions conditions for life 2M years ago


Stromatolite fossil in dolomite deposits.
| Photo Credit: Special Arrangement/Yogaraj Banerjee

What are the info: Two million years ago, a shallow inland sea might have had the precise conditions for photosynthetic algae, dolomite deposits from Andhra Pradesh‘s Vempalli, in Cuddapah district, show. Published in Chemical Geology, the study has estimated the temperature and the composition of the sea that most likely would have existed two million years ago, in the Palaeoproterozoic era, when the earth’s environment was being oxygenated. The temperature of the ocean would have been round 20° C, based on estimates by the researchers, which is good for photosynthetic algae. The examine additionally discovered that the ocean contained mild water, as a substitute of the heavy water that was beforehand thought to have existed throughout this time. 

Cuddapah district in Andhra Pradesh where the dolomite deposits were found.

Cuddapah district in Andhra Pradesh the place the dolomite deposits had been discovered.
| Photo Credit:
Special Arrangement/Yogaraj Banerjee

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What is the context?

  • Researchers from the Indian Institute of Science and the University of Tennessee used samples of dolomite deposits present in rocks known as chert that are shaped by interplay between microbes and seawater.
  • “[Dolomite] is a direct precipitate from seawater. It provides a signal not only of seawater chemistry but also of seawater temperature,” defined Robert Riding, an writer of the examine, in a launch.
  • They additionally collected deposits beneath the chert known as dolomitic lime-mud which helped to find out the temperature and composition by analysing carbon and oxygen bonds.
  • Further evaluation of the samples confirmed that the seawater additionally contained common water, opposite to prior perception that solely heavy water was discovered on this period. Regular water is H2O; in heavy water, the hydrogen is changed by its heavier isotope, deuterium.

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Why does it matter?

  • Earth has not at all times had the flexibility to host life. It has gone by a number of levels of heating and cooling, together with intervals the place carbon dioxide ranges made it too poisonous for life. 
  • In truth, the ‘era of oxygen’ solely started 2.2 to 2.4 million years ago, in accordance to the American Museum of Natural History.
  • Studies equivalent to this have proven that life may nonetheless have existed underneath these harsh conditions. Moreover, it will have absorbed the carbon dioxide from the environment and pumped it with oxygen, permitting different lifeforms to evolve.
  • The examine has discovered proof that disproves two present theories. First: earlier research estimated that sea temperature on this interval was round 50° C by solely analysing chert samples. Second: the kind of water regarded as current throughout this time was characterised as heavy water; the examine confirmed mild water additionally existed. 

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