Geo thermal energy quite a interesting idea getting our electricity from the Earth internal heat how economic. Though we must be on guard agaiinst future massive volcanic eruptions that can endanger our decendents future.
Photograph courtesy Kevin Krajick, Columbia University Earth Institute
Published March 21, 2013
At the end of the Triassic period, at least half of the species living on land and in the ocean went extinct, opening the way for dinosaurs to dominate Earth for the next 135 million years. Scientists have long suspected massive volcanic eruptions were to blame, but they haven’t been able to pin down the exact timing until now.
In a new study published today in the journal Science, researchers say they have confirmed that eruptions large enough to bury the U.S. under 300 feet (91 meters) of lava occurred at the same time that vast numbers of plant and animal species disappeared from the fossil record.
About 201 million years ago, tectonic forces started ripping the supercontinent known as Pangaea apart, said Terrence Blackburn, a geologist at the Carnegie Institution for Science in Washington, D.C., and lead author of the study.
The underlying mantle rock melted, generating these large eruptions, he added.
The rift, which eventually created the Atlantic Ocean basin, happened between sections of Pangaea that would go on to become North America and Africa. (Read about how Pangaea formed.)
These huge eruptions, or flood basalt events, occurred during four periods over 600,000 years, but it’s the first bout of volcanism that contributed to the death of so many organisms, said Blackburn.
Until now, the margin of error in calculating the timing of these eruptions ranged between one and three million years, leading to uncertainty over which happened first—the eruptions or the mass extinction.
But by using a rare mineral called zircon, found in igneous rocks like basalts, the researchers were able to narrow down their margin of error to 20,000 to 30,000 years—pegging the initial eruptions to just before the mass extinction event.
“Zircon is a perfect time capsule for dating those rocks,” said Blackburn. When the mineral crystallizes, it incorporates uranium, which decays over a known time with respect to the element lead. By measuring the ratio of uranium to lead in our samples, we can determine the age of those crystals, he explained.
By accurately placing the extinction event at the onset of the eruptions, climate modelers and other scientists may be able to pinpoint specific mechanisms like climate change that provoked the extinctions, Blackburn said.
There is evidence that the initial volcanic eruptions doubled the amount of the carbon dioxide in the atmosphere, which led to increased global temperatures and ocean acidification, he noted. This happened quickly, which probably didn’t give organisms at the time much of a chance to adjust to the changes. (Learn more about ocean acidification.)
Life did show signs of recovery during later eruption episodes, Blackburn said, which he found surprising.
These later eruptions didn’t result in as much lava as that initial eruption, but other researchers have shown that atmospheric carbon dioxide still increased after each event, possibly maintaining climatic conditions present during the mass extinction.
Researchers aren’t sure how the species that made it through the extinction event were able to deal with the new climate.
All mass extinction events are correlated with major eruptions, said Paul Renne, a geologist who specializes in figuring out the age of rocks at the Berkeley Geochronology Center in California. But the significance of volcanic eruptions in wiping out major groups of organisms has been pushed aside in favor of hypotheses that hold asteroid impacts responsible.
There is one case 65 million years ago, at a point in time known as the Cretaceous-Tertiary boundary (K-T boundary), with strong evidence supporting an asteroid impact around the same time the dinosaurs disappeared.
“That one instance really guided everybody’s thinking, and the idea that impacts caused mass extinctions was really, really popular,” said Renne, who wasn’t involved in the Blackburn study.
But he believes that major volcanic eruptions have been a driving force in mass extinctions and that this latest study by Blackburn and colleagues tightens the correlation between the two events at the end of the Triassic.
Renne says that even the asteroid impact at the K-T boundary likely only finished the job that major volcanic eruptions in India started. (Related: “What Killed Dinosaurs: New Ideas About the Wipeout.”)
Renne is another "volcanist" who apparently knows little about impact science. He conveniently ignores 3 huge impact craters that were formed at the time of the extinction event, all aligned at the same latitude, and indicating that an apparent comet broke up and impacted as the Earth rotated beneath it. The craters were 100km, 40km, and 23km in diameter. The rifting and breakup of Pangeaea began AFTER the impacts, and certainly contributed to the extinctions, but weren't solely responsible for them. Species, including dinosaurs, survived just fine during the Deccan Traps eruptions for a million years (until something big hit Chicxulub), so how are the end-Triassic traps supposed to be so much more lethal? Some exotic toxin release? Right. The end-Triassic mass extinction was brought about by impacts, not volcanism.
The so-called "Late Triassic multiple impact event" theory, postulated in 1998 (http://www.nature.com/nature/journal/v392/n6672/full/392171a0.html) and entirely based on imprecise impact ages available at that time, has recently been shown to be 'invalid' on the basis of new, high-precision impact age data. There was no multiple impact 214 million years (Ma) ago. The age of the 100 km Manicouagan impact structure in Canada is about 215 Ma, the ~40 km Lake St. Martin impact structure, also in Canada, is about 227 Ma old and, therefore, not related. Another 'crater chain' candidate, the ≥23 km Rochechouart impact structure in France, is about 203 Ma old, and does not relate to the Triassic/Jurassic (T/J) boundary itself at c. 200 Ma either, but is apparently slightly older (Rhaetian). Also, the Obolon' impact in Ukraine happened in Jurassic time around ~185-170 Ma and is much younger than Late Triassic. Finally, the 9 km Red Wing Creek impact structure in the USA is poorly dated and might have an age anywhere between ~220 Ma and 200 Ma. So far, we don't know a single larger meteorite impact that happened at the T/J boundary, and possible distal impact ejecta (shocked quartz grains) previously reported in Austria and Italy are questionable, at best. The ~215 Ma proven ejecta layer in Britain (containing convincing shocked quartz and spherules) is obviously related to the large Manicouagan impact that predates the T/J boundary by about 15 million years.
Paul Renne is a highly respected scientist and has produced a number of precise and accurate argon-argon data not only in the field of volcanology and impact research that help everyone of us understand the exact timing context of geologic events.
@Tayvl Hunt We learn new things everyday. That is the wonder of science. Oh, and "Renee" is a geologist, which is a sub field of volcanology, but he studies the age of rocks and it says nothing about him being a "volcanist".
I have said for decades that people/nations should install geo-thermal power stations on all the worlds hot spots. e.g. Yellowstone and any myriad of active volcanoes. Of course some modern designs should be implemented. It just so happens I have been working on them conceptually for over a decade (and have other non-scaling geo-thermal inventions I would not patent while mega-corporations prefer to steal off ordinary people.
@Colin Goto "I would not patent while mega-corporations prefer to steal off ordinary people."
Meaning you have no idea how patent works, don't have anything worthy of note, and are contributing nothing except a comment here to stroke your pitiable ego.
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