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  2. Carbon dioxide in Earth's atmosphere - Wikipedia

    en.wikipedia.org/wiki/Carbon_dioxide_in_Earth's...

    The present atmospheric concentration of CO 2 is the highest for 14 million years. [10] Concentrations of CO 2 in the atmosphere were as high as 4,000 ppm during the Cambrian period about 500 million years ago, and as low as 180 ppm during the Quaternary glaciation of the last two million years. [2]

  3. Geologic temperature record - Wikipedia

    en.wikipedia.org/wiki/Geologic_temperature_record

    500 million years of climate change [7] The Phanerozoic eon, encompassing the last 542 million years and almost the entire time since the origination of complex multi-cellular life, has more generally been a period of fluctuating temperature between ice ages, such as the current age, and "climate optima", similar to what occurred in the ...

  4. List of periods and events in climate history - Wikipedia

    en.wikipedia.org/wiki/List_of_periods_and_events...

    500 million years of climate change Ice core data for the past 400,000 years, with the present at right. Note length of glacial cycles averages ~100,000 years. Blue curve is temperature, green curve is CO 2, and red curve is windblown glacial dust (loess). Scale: Millions of years before present, earlier dates approximate.

  5. What Earth was like last time CO2 levels were so crazily high

    www.aol.com/earth-last-time-co2-levels-090000507...

    Climate 101 is a Mashable series that answers provoking and salient questions about Earth’s warming climate. The last time CO2 levels were as high as today, ocean waters drowned the lands where ...

  6. What Earth was like last time CO2 levels were this high - AOL

    www.aol.com/news/earth-last-time-co2-levels...

    Climate 101 is a Mashable series that answers provoking and salient questions about Earth’s warming climate. The last time CO2 levels were as high as today, ocean waters drowned the lands where ...

  7. 100,000-year problem - Wikipedia

    en.wikipedia.org/wiki/100,000-year_problem

    δ 18 O, a proxy for temperature, for the last 600,000 years (an average from several deep sea sediment carbonate samples) [a]. The 100,000-year problem (also 100 ky problem or 100 ka problem) of the Milankovitch theory of orbital forcing refers to a discrepancy between the reconstructed geologic temperature record and the reconstructed amount of incoming solar radiation, or insolation over ...

  8. Cretaceous Thermal Maximum - Wikipedia

    en.wikipedia.org/wiki/Cretaceous_Thermal_Maximum

    The Cretaceous Thermal Maximum (CTM), also known as Cretaceous Thermal Optimum, was a period of climatic warming that reached its peak approximately 90 million years ago (90 Ma) during the Turonian age of the Late Cretaceous epoch. The CTM is notable for its dramatic increase in global temperatures characterized by high carbon dioxide levels.

  9. The world has less than 10 years to avert climate change ...

    www.aol.com/news/world-less-10-years-avert...

    Carbon dioxide emissions increased by almost 5% last year, meaning that the world now has a two-in-three chance of reaching 1.5 degrees Celsius of global warming over pre-industrial levels within ...