Across the ages sea levels have risen and fallen with temperatures but Earth’s total surface water was always assumed to be constant. Now, evidence is mounting that some 3 billion to 4 billion years ago, the planet’s oceans held nearly twice as much water enough to submerge today’s continents above the peak of Mount Everest. The flood could have primed the engine of plate tectonics and made it more difficult for life to start on land.
Rocks in today’s mantle, the thick layer of rock beneath the crust are thought to sequester an ocean’s worth of water or more in their mineral structures. But early in Earth’s history, the mantle, warmed by radioactivity, was four times hotter. Recent work using hydraulic presses has shown that many minerals would be unable to hold as much hydrogen and oxygen at mantle temperatures and pressures.
Junjie Dong, a graduate student in mineral physics at Harvard University who led a model, based on those lab experiments, that was published today in AGU Advances said, that suggests the water must have been somewhere else. And the most likely reservoir is the surface.
Michael Walter, an experimental petrologist at the Carnegie Institution for Science said, the paper makes intuitive sense. It’s a simple idea that could have important implications.
Steven Jacobsen, an experimental mineralogist at Northwestern University said, two minerals found deep in the mantle store much of its water today, wadsleyite and ringwoodite, high-pressure variants of the volcanic mineral olivine. Rocks rich in those minerals make up 7% of the planet’s mass, and although only 2% of their weight is water today, a little bit adds up to a lot.
Jacobsen and others have created these mantle minerals by squeezing rock powders to tens of thousands of atmospheres and heating them to 1600°C or more. Dong’s team stitched together the experiments to show wadsleyite and ringwoodite hold fractionally less water at higher temperatures. Moreover, the team predicts, as the mantle cooled, these minerals themselves would become more abundant, adding to their ability to soak up water as Earth aged.
The experiments aren’t alone in suggesting a water-bound planet.
Benjamin Johnson, a geochemist at Iowa State University said, there is pretty clear geological evidence. Titanium concentrations in 4 billion year old zircon crystals from Western Australia suggest they formed underwater. And some of the oldest known rocks on Earth, 3 billion year old formations in Australia and Greenland are pillow basalts bulbous rocks that only form as magma cools underwater.
Work by Johnson and Boswell Wing, a geobiologist at the University of Colorado, Boulder, offers more evidence. Samples from a 3.24 billion year old chunk of oceanic crust left on Australia’s mainland were far richer in a heavy oxygen isotope than the present day oceans. Because water loses this heavy oxygen when rain reacts with the continental crust to form clays, its abundance in the ancient ocean suggests the continents had barely emerged by that point, Johnson and Wing concluded in a 2020 Nature Geoscience study. The finding doesn’t necessarily mean the oceans were larger, Johnson notes but, it is easier to have submerged continents if the oceans are bigger.
Rebecca Fischer, an experimental petrologist at Harvard and co-author on the AGU Advances study said, although the larger ocean would have made it harder for the continents to stick their necks out, it could explain why they appear to have been on the move early in Earth’s history.
Jun Korenaga, a geophysicist at Yale University said, larger oceans could have helped kick off plate tectonics as water penetrated fractures and weakened the crust, creating subduction zones where one slab of crust slipped below another. And once a subducting slab began its dive, the dryer, inherently stronger mantle would have helped bend the slab, ensuring its plunge would continue. If you cannot bend plates, you cannot have plate tectonics.
Thomas Carell, a biochemist at Ludwig Maximilian University of Munich said, the evidence for larger oceans challenges scenarios for how life began on Earth. Some researchers believe it began at nutrient rich hydrothermal vents in the ocean, whereas others favor shallow ponds on dry land, which would have frequently evaporated, creating a concentrated bath of chemicals.
A larger ocean exacerbates the biggest strike against the underwater scenario that the ocean itself would have diluted any nascent biomolecules to insignificance. But by drowning most land, it also complicates the thin pond scenario. Carell, a pond advocate says in light of the new paper, he is now considering a different birthplace for life sheltered, watery pockets within oceanic rocks that broke the surface in volcanic seamounts.
He said, maybe we had little caves in which it all happened.
The ancient water world is also a reminder of how conditional Earth’s evolution is. The planet was likely parched until water-rich asteroids bombarded it shortly after its birth. If the asteroids had deposited twice as much water or the present day mantle had less appetite for water, then the continents, so essential for the planet’s life and climate, would never have emerged.
Dong said, it’s a very delicate system, the Earth. Too much water, or too little, and it wouldn’t work.