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  2. Evolution of photosynthesis - Wikipedia

    en.wikipedia.org/wiki/Evolution_of_photosynthesis

    While C 4 enhances the efficiency of RuBisCO, the concentration of carbon is highly energy intensive. This means that C 4 plants only have an advantage over C 3 organisms in certain conditions: namely, high temperatures and low rainfall. C 4 plants also need high levels of sunlight to thrive. [40]

  3. Water cycle - Wikipedia

    en.wikipedia.org/wiki/Water_cycle

    The water cycle is powered from the energy emitted by the sun. This energy heats water in the ocean and seas. Water evaporates as water vapor into the air. Some ice and snow sublimates directly into water vapor. Evapotranspiration is water transpired from plants and evaporated from the soil. The water molecule H

  4. Light-dependent reactions - Wikipedia

    en.wikipedia.org/wiki/Light-dependent_reactions

    The electron in the higher energy level is unstable and will quickly return to its normal lower energy level. To do this, it must release the absorbed energy. This can happen in various ways. The extra energy can be converted into molecular motion and lost as heat, or re-emitted by the electron as light (fluorescence).

  5. Origin of water on Earth - Wikipedia

    en.wikipedia.org/wiki/Origin_of_water_on_Earth

    Afterward, liquid water oceans may have existed despite the surface temperature of 230 °C (446 °F) due to the increased atmospheric pressure of the CO 2 atmosphere. As the cooling continued, most CO 2 was removed from the atmosphere by subduction and dissolution in ocean water, but levels oscillated wildly as new surface and mantle cycles ...

  6. Geological history of Earth - Wikipedia

    en.wikipedia.org/wiki/Geological_history_of_Earth

    Current Earth - without water, elevation greatly exaggerated (click/enlarge to "spin" 3D-globe). The Holocene Epoch began approximately 11,700 calendar years before present [10] and continues to the present. During the Holocene, continental motions have been less than a kilometer.

  7. Meltwater pulse 1A - Wikipedia

    en.wikipedia.org/wiki/Meltwater_pulse_1A

    Image showing sea level change during the end of the last glacial period. Meltwater pulse 1A is indicated. Meltwater pulse 1A (MWP1a) is the name used by Quaternary geologists, paleoclimatologists, and oceanographers for a period of rapid post-glacial sea level rise, between 13,500 and 14,700 years ago, during which the global sea level rose between 16 meters (52 ft) and 25 meters (82 ft) in ...

  8. It’s just water in a can. How did Liquid Death become a ...

    www.aol.com/news/water-became-billion-dollar...

    But “Liquid Death” is just water in a can. Now the brand, which has been independently owned and operated since its creation in 2017, has raised a new round of investment that values it at $1. ...

  9. History of energy - Wikipedia

    en.wikipedia.org/wiki/History_of_energy

    In 1802 lectures to the Royal Society, Thomas Young was the first to use the term energy to refer to kinetic energy in its modern sense, instead of vis viva. [3] In the 1807 publication of those lectures, he wrote, The product of the mass of a body into the square of its velocity may properly be termed its energy. [4]