Showing posts with label Industrial capitalism. Show all posts
Showing posts with label Industrial capitalism. Show all posts

Wednesday, June 6, 2018

2934. Book Review: Behemoth

By Ian Jack, The Guardian, March 14, 2018

The demise of the factory in the western world ranks high among the explanations for Brexit and Donald Trump. With it came the geographic isolation of the old factory lands from national prosperity, and the alienation of the former factory classes from the mainstream of British and American life. Furnaces lost their fires and smokestacks crashed to the ground. Industrial towns and cities grew ruinous – far too grand for the little business they now contained. People were poorer and felt that governments didn’t care.
The US lost roughly 5m manufacturing jobs between 2000 and 2016, while the UK lost 619,000 from 2006 to 2016 – adding in each country to the millions that had vanished in the previous three or four decades. An idea of the future also disappeared. These were regarded as “good jobs”: well paid (when they were skilled), secure, with regular hours, subsidised canteens and paid holidays. “The unionised giant factory helped create what many Americans look back at as a golden era of shared prosperity,” writes Joshua B Freeman of a recent time “when children did better than their parents and expected their children to do better than themselves.”





That factories could be sites of optimism sits uneasily with our ideas of the Dickensian 19th century and Blake’s satanic mills. To Engels, factory work was “nothing less than torture of the severest kind … in the service of a machine that never stops”. In Das Kapital, Marx wrote that while in handicrafts “the workman makes use of a tool, the factory makes use of him”. And yet ever since the Lombe brothers opened their silk mill in Derby in 1721, a brighter view of the factory has always persisted. The Derby mill was probably the first successful prototype, with a square, prison-like appearance that marked many thousands of its successors, buildings that in Freeman’s definition of a factory contained “a large workforce engaged in coordinated production using powered machinery”. Daniel Defoe saw this mill as a modern marvel, reacting to a visit there with a great explosion of facts (the machinery had 26,586 wheels and could produce 318,504,960 yards of silk thread every 24 hours), starting a tradition of awe-inspiring numbers that continues to this day in China, where it can take an hour to walk from one side of a factory to the other, and where in 2016, at peaks of production, 350,000 workers were employed to make iPhones in a factory complex in Zhengzhou.


Chinese toy factory Lianyungang Jiangsu
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 Factory to the world … Chinese employees making toys for export at a factory in Lianyungang in east China’s Jiangsu province. Photograph: -/AFP/Getty

Freeman has written a superb account of how the material world in his phrase became “factory made”. It takes us all the way from 18th-century Derbyshire to 21st-century China and spans the factory’s social, cultural, economic and political effects, as well as its technical progress. Almost every page contains a memorable fact or an intriguing thought, and by treating factories as a global phenomenon, Freeman has freed them from the cliches of the purely national narrative, which in Britain’s case familiarised generations of schoolchildren with very few innovations later than the spinning jenny and the power loom. Of course, British industrial production continued to develop long after those inventions, but the main thrust of factory history moved elsewhere – beyond Europe, to the US and the Soviet Union before its most recent incarnation in China, which, with the increased use of robotics, may be the last society shaped by the factory as a mass employer.
Women have a prominent place in this story, most notably after the factory crossed the Atlantic to New England, where cotton mills were set up on riverbanks that were often far from any large settlement. Separated from urban temptation and powered by water until after the civil war – coal deposits were inconveniently located – they enjoyed a more wholesome reputation than their smoky British ancestors. Like British textile factories, they depended on female labour to operate the machinery, while men took the better paid jobs in management and maintenance. In some New England mills, women made up 85% of the workforce. Unlike the typical Lancashire factory girl, they tended to be the literate daughters of farmers who returned to the homestead during downturns in trade rather than staying in their factory lodgings and making trouble; and thereby, as Freeman writes, “avoiding the discontent and disorder that came in England with the creation of a permanent proletariat”.


Diego Rivera Detroit Industry murals
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 Heroic … Detail from one of Diego Rivera’s Detroit Industry murals (1933). Photograph: Alamy Stock Photo

Paternalistic mill owners did their best to create a moral and improving atmosphere; the Lowell mills in Massachusetts even published a magazine of poetry and fiction for its workers. But what did more to change the lives of the mill women was money – that and an interval of self-discovery between daughterhood and wifehood that living away from home allowed. “The mills … provided an escape from families, rural life, boredom and isolation, a chance to experience a new, more cosmopolitan world of independent living, consumer goods and intense sociability,” Freeman writes, quoting a woman who remembered how a worker’s first wages could effect an enormous transformation: from “depressed, modest, mincing” girls into women who looked you in the face and “sang blithely among their looms”.
This was the factory effect at its gentlest. As the 19th century wore on, it showed its more brutal side, when the magnates such as Andrew Carnegie and Henry Clay Frick refused to improve the hellish conditions of their steel mills and broke up strikes ruthlessly and brutally. Freeman argues that mainstream ideology is mistaken when it associates the achievements of the industrial revolution with individual liberty and the free market. Factories often did best in the opposite conditions, growing up, like the British textile and American iron and steel industries, in a climate of “denied political rights – free speech, free assembly, rule of law”. If more examples are needed to support Freeman’s argument, look no further than China’s present role as factory to the world.
Taylorism, Fordism, fascism: Freeman shows how our love-hate relationship with the factory blossomed once again in the 1920s and 30s – the production line hell of Chaplin’s Modern Times on the one hand and Diego Rivera’s heroic Detroit murals on the other. The author’s sympathy, insight and exemplary anecdotes make this a marvellous book.

Monday, August 29, 2016

2428. The Anthropocene Epoch: Scientists Declare Dawn of Human-Influenced Age

By Damion Carrington, The Guardian, August 29, 2016

Humanity’s impact on the Earth is now so profound that a new geological epoch – the Anthropocene – needs to be declared, according to an official expert group who presented the recommendation to the International Geological Congress in Cape Town on Monday.
The new epoch should begin about 1950, the experts said, and was likely to be defined by the radioactive elements dispersed across the planet by nuclear bomb tests, although an array of other signals, including plastic pollution, soot from power stations, concrete, and even the bones left by the global proliferation of the domestic chicken were now under consideration.
The current epoch, the Holocene, is the 12,000 years of stable climate since the last ice age during which all human civilisation developed. But the striking acceleration since the mid-20th century of carbon dioxide emissions and sea level rise, the global mass extinction of species, and the transformation of land by deforestation and development mark the end of that slice of geological time, the experts argue. The Earth is so profoundly changed that the Holocene must give way to the Anthropocene.




“The significance of the Anthropocene is that it sets a different trajectory for the Earth system, of which we of course are part,” said Prof Jan Zalasiewicz, a geologist at the University of Leicester and chair of the Working Group on the Anthropocene (WGA), which started work in 2009.
“If our recommendation is accepted, the Anthropocene will have started just a little before I was born,” he said. “We have lived most of our lives in something called the Anthropocene and are just realising the scale and permanence of the change.”
Prof Colin Waters, principal geologist at the British Geological Survey and WGA secretary, said: “Being able to pinpoint an interval of time is saying something about how we have had an incredible impact on the environment of our planet. The concept of the Anthropocene manages to pull all these ideas of environmental change together.”
Prof Chris Rapley, a climate scientist at University College London and former director of the Science Museum in London said: “The Anthropocene marks a new period in which our collective activities dominate the planetary machinery. 
“Since the planet is our life support system – we are essentially the crew of a largish spaceship – interference with its functioning at this level and on this scale is highly significant. If you or I were crew on a smaller spacecraft, it would be unthinkable to interfere with the systems that provide us with air, water, fodder and climate control. But the shift into the Anthropocene tells us that we are playing with fire, a potentially reckless mode of behaviour which we are likely to come to regret unless we get a grip on the situation.” Rapley is not part of the WGA.
Martin Rees, the astronomer royal and former president of the Royal Society, said that the dawn of the Anthropocene was a significant moment. “The darkest prognosis for the next millennium is that bio, cyber or environmental catastrophes could foreclose humanity’s immense potential, leaving a depleted biosphere,” he said. 



But Lord Rees added that there is also cause for optimism. “Human societies could navigate these threats, achieve a sustainable future, and inaugurate eras of post-human evolution even more marvellous than what’s led to us. The dawn of the Anthropocene epoch would then mark a one-off transformation from a natural world to one where humans jumpstart the transition to electronic (and potentially immortal) entities, that transcend our limitations and eventually spread their influence far beyond the Earth.”
The evidence of humanity’s impact on the planet is overwhelming, but the changes are very recent in geological terms, where an epoch usually spans tens of millions of years. “One criticism of the Anthropocene as geology is that it is very short,” said Zalasiewicz. “Our response is that many of the changes are irreversible.”


Human activity has left a permanent layer of airborne particulates in sediment and glacial ice.
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 Human activity has left a permanent layer of airborne particulates in sediment and glacial ice. Photograph: Pool/Reuters

To define a new geological epoch, a signal must be found that occurs globally and will be incorporated into deposits in the future geological record. For example, the extinction of the dinosaurs 66m years ago at the end of the Cretaceous epoch is defined by a “golden spike” in sediments around the world of the metal iridium, which was dispersed from the meteorite that collided with Earth to end the dinosaur age.
For the Anthropocene, the best candidate for such a golden spike are radioactive elements from nuclear bomb tests, which were blown into the stratosphere before settling down to Earth. “The radionuclides are probably the sharpest – they really come on with a bang,” said Zalasiewicz. “But we are spoiled for choice. There are so many signals.”
Other spikes being considered as evidence of the onset of the Anthropocene include the tough, unburned carbon spheres emitted by power stations. “The Earth has been smoked, with signals very clearly around the world in the mid-20th century,” said Zalasiewicz.
Other candidates include plastic pollution, aluminium and concrete particles, and high levels of nitrogen and phosphate in soils, derived from artificial fertilisers. Although the world is currently seeing only the sixth mass extinction of species in the 700m-year history of complex life on Earth, this is unlikely to provide a useful golden spike as the animals are by definition very rare and rarely dispersed worldwide.
In contrast, some species have with human help spread rapidly across the world. The domestic chicken is a serious contender to be a fossil that defines the Anthropocene for future geologists. “Since the mid-20th century, it has become the world’s most common bird. It has been fossilised in thousands of landfill sites and on street corners around the world,” said Zalasiewicz. “It is is also a much bigger bird with a different skeleton than its prewar ancestor.” 
The 35 scientists on the WGA – who voted 30 to three in favour of formally designating the Anthropocene, with two abstentions – will now spend the next two to three years determining which signals are the strongest and sharpest. Crucially, they must also decide a location which will define the start of the Anthropocene. Geological divisions are not defined by dates but by a specific boundary between layers of rock or, in the case of the Holocene, a boundary between two ice layers in a core taken from Greenland and now stored in Denmark.


The domestic chicken is a serious contender to be a fossil that defines the Anthropocene for future geologists.
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 The domestic chicken is a serious contender to be a fossil that defines the Anthropocene for future geologists. Photograph: Alamy

The scientists are focusing on sites where annual layers are formed and are investigating mud sediments off the coast of Santa Barbara in California and the Ernesto cave in northern Italy, where stalactites and stalagmites accrete annual rings. Lake sediments, ice cores from Antarctica, corals, tree rings and even layers of rubbish in landfill sites are also being considered.
Once the data has been assembled, it will be formally submitted to the stratigraphic authorities and the Anthropocene could be officially adopted within a few years. “If we were very lucky and someone came forward with, say, a core from a classic example of laminated sediments in a deep marine environment, I think three years is possibly viable,” said Zalasiewicz. 



This would be lightning speed for such a geological decision, which in the past would have taken decades and even centuries to make. The term Anthropocene was coined only in 2000, by the Nobel prize-winning scientist Paul Crutzen, who believes the name change is overdue. He said in 2011: “This name change stresses the enormity of humanity’s responsibility as stewards of the Earth.” Crutzen also identified in 2007 what he called the great acceleration of human impacts on the planet from the mid-20th century. 
Despite the WGA’s expert recommendation, the declaration of the Anthropocene is not yet a forgone conclusion. “Our stratigraphic colleagues are very protective of the geological time scale. They see it very rightly as the backbone of geology and they do not amend it lightly,” said Zalasiewicz. “But I think we can prepare a pretty good case.”
Rapley also said there was a strong case: “It is highly appropriate that geologists should pay formal attention to a change in the signal within sedimentary rock layers that will be clearly apparent to future generations of geologists for as long as they exist. The ‘great acceleration’ constitutes a strong, detectable and incontrovertible signal.”

Evidence of the Anthropocene

Human activity has:
  • Pushed extinction rates of animals and plants far above the long-term average. The Earth is on course to see 75% of species become extinct in the next few centuries if current trends continue.
  • Put so much plastic in our waterways and oceans that microplastic particles are now virtually ubiquitous, and plastics will likely leave identifiable fossil records for future generations to discover.
  • Doubled the nitrogen and phosphorous in our soils in the past century with fertiliser use. This is likely to be the largest impact on the nitrogen cycle in 2.5bn years.
  • Left a permanent layer of airborne particulates in sediment and glacial ice such as black carbon from fossil fuel burning.