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Ancient kauri tree from Ngāwhā, NZ, next to 4WD. Credit_Nelson Parker
Ancient kauri tree from Ngāwhā, NZ, next to 4WD. Credit_Nelson Parker

Ancient New Zealand tree reveals a turning point in Earth’s history 42,000 years ago

Ancient New Zealand tree reveals a turning point in Earth’s history 42,000 years ago

Weakened magnetic field linked to climate change, extinction of Australian megafauna, and rise of cave art

The temporary breakdown of Earth’s magnetic field 42,000 years ago sparked major climate shifts that led to global environmental change and mass extinctions, an international research team including a Ƶapp of Ƶapp (UOW) scientist has found.

This dramatic turning point in Earth’s history – laced with electrical storms, widespread auroras, and cosmic radiation – was triggered by the reversal of Earth’s magnetic poles and changing solar winds.

The researchers dubbed this danger period the “Adams Transitional Geomagnetic Event”, or “Adams Event” for short – a tribute to science fiction writer Douglas Adams, who wrote in The Hitchhiker’s Guide to the Galaxy that 42 was the answer to life, the universe, and everything.

The study was co-led by the Ƶapp of NSW (UNSW) and the South Australian Museum, and its findings are published today in Science.

The geological record shows that the Earth’s magnetic poles have reversed multiple times, but the global impact of these events was unclear.

The most recent polar reversal, known as the Laschamp excursion, occurred around 41-42,000 years ago when the north magnetic pole wandered down to the southern hemisphere and then back north again.

Sedimentary and volcanic deposits indicate that during the reversed phase of the Laschamp excursion the intensity of the Earth’s magnetic field (which shields the planet from cosmic radiation) weakened to around 28 per cent of current levels, and during the preceding transition period it fell to as little as 0 to 6 per cent of current levels.

The researchers analysed ancient kauri trees, using the growth rings to measure and date the spike in atmospheric radiocarbon levels caused by the collapse of Earth’s magnetic field, developing a detailed record of atmospheric radiocarbon levels across the Laschamp excursion.

The ancient kauri trees, found preserved in northern New Zealand wetlands, were alive during the Laschamp excursion. 

Previous scientific research had focused on changes that happened while the magnetic poles were reversed, when Earth’s geomagnetic field was weakened to about 28 per cent of its present-day strength.

What the new research showed is that the most dramatic impacts occurred during the transition period – the Adams Event – when the magnetic field dropped to only 0-6 per cent strength.

The researchers compared the newly-created timescale with records from sites across the Pacific and used it in global climate modelling, finding that the growth of ice sheets and glaciers over North America and large shifts in major wind belts and tropical storm systems could be traced back to the Adams Event.

left: 5.	Rings on a slice of the Ngāwhā log. Photo: Jonathan Palmer. Right: 6.	Red ochre – which may have been used as an ancient form of sunscreen – is a common cave art motif. The centre of this cave art from Spain is believed to be almost 42,000 years old. Photo: Paul Pettitt, courtesy Gobierno de Cantabria.

Left: Rings on a slice of the Ngāwhā log. Photo: Jonathan Palmer.

Right: Red ochre – which may have been used as an ancient form of sunscreen – is a common cave art motif. The centre of this cave art from Spain is believed to be almost 42,000 years old. Photo: Paul Pettitt, courtesy Gobierno de Cantabria.

 

Co-author Professor from UOW’s School of Earth, Atmospheric and Life Sciences said the Adams Event could be linked to a number of major events that occurred at that time

“This research documents dramatic environmental changes 42,000 years ago, caused by a major shift in the magnetic field that usually protects our planet from cosmic radiation,” Professor Dosseto said.

“This shift in the magnetic field caused major changes in climate. It felt like someone left the freezer door open. And on the driest inhabited continent – yes, Australia – things got much drier too.

“This environmental catastrophe could explain and of Neanderthals in Europe.”

The Adams Event could also explain the sudden rise in cave art that occurred around the world at this time.

“I compiled the data on cave art chronology,” Professor Dosseto said. “This allowed the team to see that at the very time the Earth’s magnetic field weakened, cave art became more common.

“Cave painting becomes the new fashion trend, as people took shelter in caves from increased ultraviolet radiation.”

The study suggests that were a similar shift in the Earth’s magnetic poles to occur now, the consequences for modern society would be huge.

Not only would incoming cosmic radiation destroy our electric power grids and satellite networks, it would trigger a new wave of climate change.

“Why do we care what happened 42,000 years ago? Because what happened is terrifying and could happen again,” Professor Dosseto said.

“If it happened again, the consequences would be tragic for humankind and would go well beyond losing mobile phone reception – however terrifying that might seem.

“Although the weakening of the magnetic field only lasted a few hundred years, it had consequences on Earth’s climate, environment and life for the following thousands of years – a cautionary tale for our current impact on the planet.

“It will take a while for the planet to clean up our mess, even long after we’re gone.”

Associate Professor Anthony Dosseto is an expert in geochemistry and Director of the Ƶapp Isotope Geochronology Laboratory at UOW

Professor Anthony Dosseto from UOW's School of Earth, Atmospheric and Life Sciences: "“Although the weakening of the magnetic field only lasted a few hundred years, it had consequences on Earth’s climate, environment and life for the following thousands of years". Picture: Paul Jones, UOW

ABOUT THE RESEARCH

‘A global environmental crisis 42,000 years ago’ by Alan Cooper, et al. is published in Science ().

The research was funded by the Australian Research Council, the Ƶapp of Adelaide Environment Institute, the Australasian Antarctic Expedition 2013–2014, the Royal Society of New Zealand Marsden Fund, New Zealand’s National Institute of Water and Atmospheric Research, the Ƶapp of Waikato, the Leverhulme Trust, the Russian Science Foundation, and the Swiss National Science Foundation.