West Antarctica was ice-free 34 million years ago, new samples reveal

Few today deny the impact of global warming. As the term has become slang for all that is wrong with the planet, experts have empirically examined its impact on the Antarctic ice sheets.

What has been called “perpetual” ice in the past is rapidly melting at an unimaginable rate, before it was particularly elevated in West Antarctica compared to East Antarctica.

Recently, scientists discovered that the root of the problem is ice formation.

In a new study, scientists report that for the first time, the acquisition of unique geological samples combined with sophisticated modeling has provided surprising insights into when and where today’s Antarctic ice sheet formed.

West Antarctic ice formed 7 million years after the east

An international research team led by the Alfred Wegener Institute found that the permanent glaciation of Antarctic ice was activated around 34 million years ago.

This was determined by analyzing sediment samples from drill cores combined with comprehensive modeling of climate and ice sheets.

Gute Morgen Johann, chief marine geologist at the Alfred Wegener Institute, said in reference to the significant discovery Interesting engineering,

“West Antarctica became permanently glaciated much later than East Antarctica – at least seven million years. So the dawn of the Antarctic ice sheets reveals its fate.”

The scientists’ statement noted that glaciation, which began 34 million years ago, did not cover the entire continent as previously thought, but was rather limited to the eastern region of the continent (East Antarctica).

But a new study has discovered the reason for ice melting in West Antarctica millions of years after glaciation began in the east.

Johann explained I.E that it is essential to know where the permanent ice masses were and how much there was for such major climate changes as the one about 34 million years ago.

“This profoundly affects atmospheric and oceanic circulation patterns,” he says.

“We now have a much better understanding of the last major climate change from a greenhouse to an ice age nearly 34 million years ago. It is essential to improve the predictive capabilities of climate models in general.”

Establishment of the “History of the Dawn of the Antarctic Ice Continent”

As the Earth underwent one of the most significant climatic transitions since the Eocene during the Paleogene period, the Antarctic ice sheets gathered.

As the team of scientists set about preparing the timeline, they obtained a drill core using the MARUM-MeBo70 seabed drilling rig located off the coast of the Pine Island and Thwaites glaciers on the coast of the Amundsen Sea in West Antarctica.

For the first time, the history of the dawn of the icy Antarctic continent was established, the statement emphasized. There was no evidence of ice being present in this area during the first major phase of Antarctic glaciation.

“This means that a large-scale, permanent first glaciation must have started somewhere in East Antarctica,” said Dr. Johann Klages, a geologist from the AWI who led the research team.

West Antarctica was ice-free at the first glacial maximum, instead surrounded by dense broadleaf forests and a cool temperate climate. This helped prevent ice from forming.

This is because West Antarctica remained ice-free during this first glacial maximum. At the time, it was still largely covered by dense deciduous forests and a cold temperate climate that prevented the formation of ice in West Antarctica.

When asked what impact the findings have on future changes in the Antarctic ice sheets, Johann told IE that it took much more effort to bring grounded ice towards the West Antarctic coast compared to East Antarctica, as many parts of West Antarctica were already under by the sea. level.

“Many more areas in West Antarctica are below sea level today, so you need much less effort to make the West Antarctic Ice Sheet disappear compared to its East Antarctic companion.” This is where we are right now.”

In short, East and West Antarctica respond differently to external forces, and therefore ice formation occurred at different times.

Klages emphasizes the importance of understanding the findings, saying it’s crucial “especially in light of the fact that we could face such major climate change again in the near future.

The study was published earlier today [July 4, 2024] in the diary – Science.

REPORTER

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ABOUT THE EDITORIAL

Shubhangi Dua As a quirky and imaginative multimedia journalist with a master’s degree in magazine journalism, I’m constantly cooking up new ideas and finding innovative ways to tell stories. I dabbled in different areas of media, from wielding a pen as a writer to capturing moments as a photographer and even social media strategy. With my creative spirit and attention to detail, I have worked across the dynamic landscape of multimedia journalism, writing on sports, lifestyle, arts, culture, health and wellbeing for Further, Alt.Cardiff and The Hindu. I am tasked with creating a media environment that is as diverse as a spotify playlist. From India to Wales and now England, my journey has been full of adventures that inspire my painting, cooking and writing.

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