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Sea ice may have cover the Earth ’s surface all the way to the equator hundreds of millions of years ago , a new work retrieve , adding more evidence to the theory that a " snowball Earth " once existed .

The determination , detail in the March 5 military issue of the journal Science , also has implications for the survival andevolution of lifeon Earth through this bitterice age .

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Glaciation at tropical latitudes provides evidence of a “snowball Earth."

geologist found evidence that tropic areas were once cover by glacier by examining ancient tropical rocks that are now ground in remote northwestern Canada . These rocks have go because the Earth ’s control surface , and the rocks on it , are in unceasing movement , pushed around by the roiling stream of the planet ’s DoI , a cognitive process call plate tectonics ) .

The rocks from Canada ’s Yukon Territory showed glacial deposits and other signs of glaciation , such as striated clast , ice rink - rafted detritus , and deformation of soft deposit .

The scientist were capable to determine , based on the magnetism and composition of these rocks , that 716.5 million years ago the rock were located at sea - stage in the tropics , at about 10 degree latitude . The period of glaciations that pass then is telephone Sturtian glaciation , one of the two greatest glass age known to have taken place on Earth .

A view of Earth from space showing the planet�s rounded horizon.

" This is the first metre that the Sturtian glaciation has been shown to have occurred at tropical latitudes , providing unmediated evidence that this especial glaciation was a ' snowball Earth ' event , " said lead generator of the study Francis Macdonald , a geologist at Harvard University .

" Our data also suggest that the Sturtian glaciation lasted a lower limit of five million years , " Macdonald tot up .

One intriguing dubiousness suggest by the determination is how biography form — especially those more complex than microbes — survived throughout this harsh climate . Their survival of the fittest suggest that sunlight and aerofoil water remain uncommitted somewhere on Earth ’s Earth’s surface , perhaps in patches of open water that shape in the sea chicken feed and provided a refuge for life .

a photo from a plane of Denman glacier in Antarctica

" The fossil record suggest that all of the major eukaryotic chemical group , with the potential exception of beast , existed before the Sturtian glaciation , " Macdonald order . " The questions that arise from this are : If a snowball Earth survive , how did these eukaryotes survive ? Did the Sturtian snowball Earth stimulate organic evolution and the origin of animals ? " ( eukaryote have a true nucleus and are more complex than so - called prokaryote . )

" From an evolutionary position , " he tote up , " it ’s not always a bad thing for life on Earth to confront severe tenseness . "

Scientists do n’t know exactly what have this glaciation or what ended it , but Macdonald enjoin its old age of 716.5 million years intimately match the age of a large igneous province – made up of rocks formed by magma that has cool down – stretch more than 932 miles ( 1,500 kilometers ) from Alaska to Ellesmere Island in far northeastern Canada .

an image of the stars with many red dots on it and one large yellow dot

This conjunction could intend the glaciation was either precipitated or terminated by volcanic activity .

The work was plunk for by the National Science Foundation and the Polar Continental Shelf Project .

An aerial photo of mountains rising out of Antarctica snowy and icy landscape, as seen from NASA�s Operation IceBridge research aircraft.

A large sponge and a cluster of anenomes are seen among other lifeforms beneath the George IV Ice Shelf.

Reconstruction of an early Cretaceous landscape in what is now southern Australia.

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An image taken from the International Space Station in 2011 shows Earthshine on the moon.

Ice calving from the fracture zone of a glacier crashes into the ocean in Greenland. Melting of such glacial ice is leading to the warping of Earth�s crust.

Red represents record-warmest temperatures. That�s a lot of red.

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