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Snowball Earth vs. Slushball Earth. .

Snowball Earth vs. Slushball Earth. Early Evidence. In 1960s, studies showed that significant glacial deposits of age 600-800 million years are on nearly every continent 1970s: When sediments form magnetic minerals point

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Snowball Earth vs. Slushball Earth. .

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  1. Snowball Earth vs. Slushball Earth..

  2. Early Evidence In 1960s, studies showed that significant glacial deposits of age 600-800 million years are on nearly every continent 1970s: When sediments form magnetic minerals point to the N pole. At the equator they will point horizontally at the equator. Found that glacial rocks 600-800 million years ago had horizontal magnetic properties indicating low latittude glaciation. 1980s climate modeling show the plausibility that ice-albedo feedback caused instability in climate

  3. Ice-Albedo Feedback; Albedo is % of sunlight that is reflected by some surface. As Earth cools: 1. Ice forms at lower and lower latitudes 2. Albedo rises 3. Reflects more solar radiation 4. Cools even more (positive feedback loop) Once ice formed at a critical latitude (30˚) the positive feedback so strong that T plummets Creates a completely frozen planet. (snowball earth  slushball earth means equatorial surface ocean not frozen) Geothermal heat keeps oceans from freezing completely, so ice 1km thick on average. Albedo: 0.1 seawater 0.3 bare land 0.6 sea ice 0.9 fresh snow

  4. A Permanent Catastrophe? Would have already extinguished life. Temperatures would have been -50˚C. No means of escape. In 1977: Discovery of hydrothermal vents. Discovery of dry valleys of Antarctica - organisms can live in extremely cold environments. Appreciation for life in extreme environments. Extremophiles

  5. Extremophiles Extremophiles provide evidence that life could have persisted under snowball Earth conditions.

  6. How To Reverse a Snowball Event? In late 1980’s, Joe Kirschvink of CalTech Gave it the name Snowball Earth. Showed that the CO2 supply would continue BUT it would be so cold that there is no liquid water at the surface. Weathering reactions stop, sloooooow dooooowwwwn. What happens then?

  7. How To Reverse a Snowball Event? Estimated 300x present level of CO2 needed to overcome the albedo of the Snowball Earth. Would have taken several million years for this much CO2 to accumulate by natural means. There is some evidence of high tectonic activity and vulcanism which would aid in building up the CO2 CO2 causes warming, which begins melting. Melting would have been catastrophic - sea ice gone in few hundred years. Sea level rises dramatically! As soon as the ice is gone, it gets rapidly hot!!

  8. The Following Hot House After the Snowball, now have a hot house. How hot? 50˚C!! Have a CO2-rich atmosphere, warm conditions. What happens next??

  9. The Carbon removal cycle Kicks Into High Gear! • The CO2 rich atmosphere would have again dissolved in the rain and turn into carbonic acid – similar to what happens during the first 500 million years of Earth’s history. • Extremely Acidic rain would have been present. • Bottom line: for about a 150-200 million year period, the surface of the Earth was tremendously inhospitable for life as it was • Cold and frozen • Then extremely hot (about 120-130 degrees F) • Then had long period of extremely acid rain • Extremophile microbes likely are the mechanism that keeps life going on the Earth under these extreme conditions.

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