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Tiny flaws in ball field hold the secret to the formation of the first continents .

In a new study , researchers used inclusions — imperfections deride by jewelers but valuable to scientists — to trace diamond formation . They found that the sulfide minerals inside the inclusions were last at the control surface of the planet 2.5 billion years ago , before the climb of O in the atmosphere .

Rough Diamond

A roughly cut diamond from Sierra Leone that has sulfur-containing mineral inclusions in it.

The findings reveal the history of the continent and cape where the diamonds shape , said study leader Karen Smit , a inquiry scientist at the nonprofit Gemological Institute of America . The diamond in the work , found in West Africa , indicate that the ancient continents in that region formed by subduction , a process in which one slab of cheekiness pushes under another . [ Photos : Rare baseball field Make US Debut at LA Natural History Museum ]

" We can get over through 2.5 billion years of Earth history just through this one sulfide inclusion , " Smit tell Live Science .

Inside a diamond

Diamonds form late in the mantelpiece . Most , Smit say , form around 125 land mile ( 200 km ) cryptical , and some forge even deeper , around 250 to 435 miles down ( 400 to 700 km ) . The inscrutable hole ever drill , the Kola Superdeep Borehole in Russia , only bottom 7.6 mile ( 12 kilometer ) . Diamonds are then brought to the aerofoil fairly speedily via mysterious volcanic eruptions .

Smit and her colleagues were canvass thenitrogen in diamondsfrom the Zimmi area of Sierra Leone when they comment that pinpoint - sizing inclusions of sulfide in the diamond demonstrate signs of having existed in the pallium before the adamant imprint , entail they were trammel within the crystallizing diamonds and carried up to the aerofoil with them . They began enquire the isotope of S within the inclusions . Isotopes are variation of atoms with differing numbers of neutron in their nuclei .

What they found reveal that the inclusions were very old indeed . O harbor the sulfur from sealed reactions with ultraviolet light source , so researcher can tell whether sulfur formed in an oxygen - rich orlow - atomic number 8 environment . These isotopes formed in the aura before there was much oxygen in the atmosphere , around 2.5 billion years ago , Smit said . The rhombus themselves are much younger than that , and formed around 650 million geezerhood ago .

A sulfur-containing mineral inclusion within the diamond.

A sulfur-containing mineral inclusion within the diamond.

A history of continents

The research worker then analyse similar inclusions in diamonds from Canada ’s Ekati mine . These comprehension are 3.5 billion years sure-enough and do not have the same isotope sign as the West African diamonds . The contrast tells a story about how the continents formed , Smit said . Early on , continents probably mould from melting mantle that ooze out up in the form of basalt , exchangeable to how Iceland or Hawaii variant today . The minerals in this cheekiness form in the mantel , not in impinging with the atmosphere .

Later in Earth account , though , subduction became crucial for forming stable continent . One chunk of crust would fag under another ; denser material would bury and less - slow fabric would rise to form continental crust . This is how the sulfur in the West African diamond would have gotten bass beneath the surface , Smit said .

The most stable , long - survive crust is bond to portions of the mantle called " keels , " so name because theystabilize crustjust as a keel stabilise a ship . More studies of inclusion body - copious diamond could avail explain how and why these keel work , Smit said . So far , there are only four locations around the world , including West Africa and Canada , with diamonds that contain both sulfide inclusion and mineral used to date the diamond ' formation . More fix would serve delineate Earth ’s history in more particular , Smit said , but these study are gainsay because the infield are destroyed in the process of psychoanalysis .

This image of a sulphide inclusion was taken with an electron microscope.

This image of a sulphide inclusion was taken with an electron microscope.

" We need diamond , " Smit said , " to demolish for skill . "

Originally published onLive Science .

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