The study, published in Nature Communications, analyzed sediment cores and identified two periods when loose sediment layers formed - the mid-Pliocene warm period around 3 million years ago and the Miocene Climatic Optimum about 15 million years ago [1]. During these times, waters around Antarctica were 3°C warmer than today, leading to an abundance of algae and the formation of slippery sediment layers prone to landslides [1].
Dr. Narendra Singh, Senior Environmental Scientist at Aryabhatta Observational Science Research Institute (ARIES), highlights the growing concern among scientists regarding the future impacts of climate change [3]. The increasing frequency of alarming research findings underscores the urgency of developing a deeper understanding of climate change and its potential consequences on global stability and safety.
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