Large igneous provinces associated with mid-ocean ridges

Earth
A composite image of the Western hemisphere of the Earth. Credit: NASA

Lip reading normally involves deciphering speech patterns, movements, gestures and expressions just by watching a person speak. Planet Earth has LIPS, too - they are an acronym for large igneous provinces, huge accumulations of igneous rocks that form when hot magma extrudes from inside the Earth and flows onto the surface of the seafloor under several kilometres of water.

An international team of scientists including University of Sydney geophysicists Professor Dietmar Müller, Dr Simon Williams and Dr Maria Seton from the School of Geosciences have found a novel way to 'read the Earth's LIPS'. Their findings are reported in a Nature Geoscience article in which they show for the first time that LIPS have a close working relationship with underwater mountain ranges called .

LIPS are known to form at hotspots where hot cylindrical upwellings called plumes are rising from the deep Earth's interior, intersecting the surface.

Professor Müller explains: "Conventional wisdom has it that these plumes, and their associated catastrophic LIPS, have no relationship to mid-ocean ridges where the slow divergence between tectonic plates gives rise to volcanism that steadily and continuously generates new ocean crust."

Now the research team has uncovered a previously missed connection between LIPS and mid-ocean ridges. They found that mantle plumes can anchor mid-ocean ridges over long periods of time, leading to a connection of mid-ocean ridges and hotspots that cannot easily be broken up.

This attraction of mid-ocean ridges to plumes promotes successive eruptions of LIPS near mid-ocean over long time periods, resulting in a myriad of igneous extrusions on top of and next to each other.

Reading the Earth's LIPS
Ridges and seafloor volcanics west of Australia. The massive edifice in the foreground of the image, offshore Antarctica, is the Kerguelen Plateau having grown to its massive size over tens of millions of years, because it was close to a mid-ocean ridge. Credit: University of Sydney
"It is important in our understanding of LIPS in the ocean basins, as it means that not all LIPS form as giant eruptions over very short times, as was originally thought," said Dr Williams.

Unlike massive eruptions on continents, the undersea eruptions are not catastrophic and are unlikely to have caused mass extinctions and climate change. However, they are just as impressive in terms of volume.

Dr Seton adds: "It means that LIPS in the oceans are less dangerous to life on Earth, as they trickle out in many successive eruptions, not just one giant outpouring of lava, as LIPS on continents."

"The findings change our understanding of massive volcanism deep in the ocean basins", said Professor Müller. "For example, the Kerguelen Plateau in the southern Indian Ocean, is over twice as big as New South Wales, and has acquired its massive size over tens of millions of years, whereas the similarly large Siberian Flood Basalts wiped out the majority of marine and land species on Earth within just 60,000 years."


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More information: Long-term interaction between mid-ocean ridges and mantle plumes, Nature Geoscience 8, 479–483 (2015) DOI: 10.1038/ngeo2437
Journal information: Nature Geoscience

Citation: Large igneous provinces associated with mid-ocean ridges (2015, May 28) retrieved 22 April 2019 from https://phys.org/news/2015-05-large-igneous-provinces-mid-ocean-ridges.html
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May 28, 2015
What would be the effect of continuous or intermittent eruptions in a Large Igneous Province on the water temperature, thermal convection of the ocean, large-scale ocean currents, and overall heat flow? I'll bet it is still too complex to model given the low geographic resolution and low precision of the estimates of heat flow from the ocean floor to the deep ocean.

May 28, 2015
IMHO, a lot would depend on the LIP changing regional circulation by blocking critical thermo-haline paths. As I understand it, there are several pinch-points and 'weirs' where a modest change in sea-bed topography would have a large effect. Some may only come into play during ice-ages' low-stand of sea levels...

The 'Drake Passage' may be one. There's surely one near Indonesia.

The Southern Indian Ocean may hold others. Incidentally, the rugged topography down there surely baulked any timely hunt for that lost jet-flight...

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