http://www.myscience.cc/news/2013/doubt ... 013-oxfordDoubt over 'volcanic winter' after Toba super-eruption
Oxford University casts doubt on the theory that the Mount Toba super-eruption, which took place at the Indonesian island of Sumatra 75,000 years ago, could have plunged the Earth into a volcanic winter leading to the near extinction of early humans.
A fresh analysis of volcanic ash recovered from lake sediment cores in Lake Malawi in East Africa shows that the eruption spewed ash much further than studies have previously found. Other theories have said that the explosive volcanic eruption may have triggered a chain of climatic events resulting in a cooling of temperatures, but this latest study finds no evidence of a significant dip in temperatures in East Africa at the time. The findings are published in the early edition of the journal Proceedings of the National Academy of Sciences.
The researchers from Oxford University and the University of Minnesota in Duluth, USA, examined microscopic volcanic ash recovered from sediment extracted from two sites in Lake Malawi in the East African Rift Valley, around 7,000 kilometres west of the source of the Toba eruption. Their analysis showed that the thin layer of ash deposits revealed in the sediment cores was from the last of the Toba eruptions – known as Youngest Toba Tuff (YTT).
The lake sediment has accumulated over thousands of years and records an undisturbed history of the environment and climate in East Africa. The researchers searched through 20 metres of sediment located at between 20 to 40 metres below the lake floor. The cores were drilled from two points (at a northern and a central position of the lake basin).
"We have been able to show that the largest volcanic eruption of the last two million years did not significantly alter the climate of East Africa."
The researchers sieved the sediment and used a heavy liquid floatation technique to find glass shards concentrated within a fine layer at 28.1 metres below the floor of Lake Malawi, in the central core, and 26.8 metres in the northern core. Tiny glass shards are created when magma ejected from a volcano freezes in flight. The shards were identified under a microscope as they are too fine to be distinguished by the naked eye. The researchers also used an electron microprobe to confirm that the chemical composition of the glass shards carried the chemical 'fingerprint' of the Toba super-eruption or, in this case, the YTT.
Significantly, this part of Africa is where early humans are thought to have originated and other studies have suggested that the super-eruption could have been the cause of a human genetic population bottleneck – whereby the numbers of early humans were significantly reduced. Had there been a significant cooling of temperatures in the region, it is likely that living matter near to the lake surface would have been killed off and the sediment composition of the lake would have undergone a dramatic change. However, when the researchers analysed the algae and other organic matter found in the core's layers where glass shards were discovered, there was no evidence of a significant temperature drop in East Africa.
Lead author Dr Christine Lane, Leverhulme Early Career Fellow at Oxford University's School of Archaeology, said: 'By tracing a microscopic layer of volcanic ash from the 75,000-year-old Toba super-eruption within sediments from Lake Malawi, we have been able to show that the largest volcanic eruption of the last two million years did not significantly alter the climate of East Africa. Our results therefore contest the theory some scholars have put forward suggesting that early modern human populations in East Africa were dramatically reduced to near extinction due to the climatic effects of this eruption. Our research implies this was not the case as there is no evidence of a "volcanic winter" in this region.
'The Toba super eruption dispersed huge volumes of ash across much of the Indian Ocean, Indian Peninsula and South China Sea. We have discovered the layer of volcanic ash was carried about twice the distance as previously thought – over more than 7000 kilometres.'
The YTT eruption provides a precise age for the sediments within which it lies, so the analysis of the Lake Malawi cores provides a benchmark by which other key climatic events in this region can be chronologically pinpointed. The study suggests that other regional and global dating records about this region, which have been correlated to Lake Malawi’s climate record, may need to be revised in the light of these findings.
Toba super-volcano theory in serious doubt
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Toba super-volcano theory in serious doubt
I wasn't aware of it until now. But it seems that the Toba-extinction theory has gone out of favour in the scientific community. The eruption does not appear to have created any significant climate changes. I find this surprising considering that it blew the better part of several thousand cubic kilometers of rock and ash into the atmosphere. I wonder if this will cause a revisal of the nuclear-winter theory.
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Re: Toba super-volcano theory in serious doubt
In response to your comment, sustained volcanic climate change has nothing to do with rock and ash, but is instead to do with the amount of sulphate aerosols blasted into the stratosphere - the idea is that a sufficient amount of aerosol reflects inbound solar radiation, causing sustained cooling. With a large enough injection, the idea is that you could sustain cooling of tens of degrees initially, taking decades to return to pre-eruption norms.
However, there is something interesting about Toba magma - although the ice cores report a large amount of sulphate at the right point in time, some experimental work on how much S can have come out of the Toba magma suggests actually that it's pretty S-poor, emitting much less than even some recent large eruptions. The implication would then be that the ice core data is wrong or is attributable to cryptovolcanoes nearer the source.
However, there is something interesting about Toba magma - although the ice cores report a large amount of sulphate at the right point in time, some experimental work on how much S can have come out of the Toba magma suggests actually that it's pretty S-poor, emitting much less than even some recent large eruptions. The implication would then be that the ice core data is wrong or is attributable to cryptovolcanoes nearer the source.
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Re: Toba super-volcano theory in serious doubt
As far as I know nuclear winter has been debunked at least in terms of what we currently have available.
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Aoccdrnig to rscheearch at an Elingsh uinervtisy, it deosn't mttaer in waht oredr the ltteers in a wrod are, the olny iprmoetnt tihng is taht frist and lsat ltteer are in the rghit pclae. The rset can be a toatl mses and you can sitll raed it wouthit a porbelm. Tihs is bcuseae we do not raed ervey lteter by it slef but the wrod as a wlohe.
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Re: Toba super-volcano theory in serious doubt
Is there a possibility of a sulphate rich eruption somewhere else on the planet at the same time?El Moose Monstero wrote:In response to your comment, sustained volcanic climate change has nothing to do with rock and ash, but is instead to do with the amount of sulphate aerosols blasted into the stratosphere - the idea is that a sufficient amount of aerosol reflects inbound solar radiation, causing sustained cooling. With a large enough injection, the idea is that you could sustain cooling of tens of degrees initially, taking decades to return to pre-eruption norms.
However, there is something interesting about Toba magma - although the ice cores report a large amount of sulphate at the right point in time, some experimental work on how much S can have come out of the Toba magma suggests actually that it's pretty S-poor, emitting much less than even some recent large eruptions. The implication would then be that the ice core data is wrong or is attributable to cryptovolcanoes nearer the source.
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Re: Toba super-volcano theory in serious doubt
It's possible - volcanoes which haven't previously been identified from tephra signatures in the stratigraphic record. I'll have a dig in the literature at work and see if anyone has commented/investigated further on that one experimental study.
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Re: Toba super-volcano theory in serious doubt
I would expect an environmental impact from Toba eruption were much more severe in temperate lattitudes than near equator. After all it doesn't matter much if average temperature drops from 28 to 24 degrees for a few years. However in temperate zones similar temperature drop could cause several years without summer in a row with severe ecological consequences.