Recent research published in Nature Communications reveals that mud cores extracted from Mississippi contain previously undiscovered evidence regarding the formation of massive Antarctic ice sheets approximately 34 million years ago.
Sheets of ice lay on top of the sea en route from McMurdo to Cape Royds, Antarctica, February 2000.
Antarctic Ice Cap Formation Linked to Coastal Carbon Transfer
The period of when ice sheets in Antarctica started forming marked a significant transition on Earth, transitioning from the warmer Eocene Epoch to the cooler Oligocene. During the Eocene, the planet lacked permanent ice; but by the early Oligocene, it had ice sheets that were 25 percent larger than contemporary ones.
The Eocene-Oligocene transition occurs when the growth of Antarctic ice sheets leads to a significant drop in sea levels, approximately 40 meters (131 feet), causing previously submerged coastal areas to become exposed as coastlines receded.
This dramatic decline in sea levels triggered a substantial transfer of carbon from coastal sediments into the atmosphere, as indicated by the research team's analysis of ancient mud samples collected near Jackson, Mississippi.
According to senior author Tom Dunkley Jones, a micropaleontologist and paleoceanographer at the University of Birmingham in the UK, these findings offer insights into the expansion of Antarctic ice to a continental scale.
The study's authors highlight that Antarctic ice sheets initially developed through the long-term burial of carbon in sediments, effectively sequestering it away from the atmosphere where it is known for its heat-trapping properties.
This reduction in atmospheric carbon played a crucial role in Earth's transition to the cooler modern climate over the past 34 million years, creating conditions conducive to the formation of massive ice sheets in Antarctica, which in turn contributed to a global decrease in sea levels.
The rapid pace of these changes during the Eocene-Oligocene transition posed challenges for many species to adapt, resulting in a widespread mass extinction, a phenomenon previously documented in research.
This tumultuous period, often referred to as the "Grande Coupure" in French, meaning "great cut," represents one of the most significant climate cooling events in Earth's history. Jones noted that the Eocene-Oligocene transition had a profound impact on the planet's climate and its historical trajectory.
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Biggest Climate Cooling Event Led to Extreme Erosion in Coastal Sediments
The research involved studying marine clay samples, spanning a depth of approximately 137 meters, and comparing them with key records of the Eocene-Oligocene transition, particularly from the central Pacific Ocean.
Dr. Kirsty Edgar from the University of Birmingham emphasized that this research sheds light on how Earth's climate can undergo significant shifts, often closely linked to the biosphere and the carbon cycle.
During the overall cooling trend of this transition, falling sea levels exposed coastal sediments to erosion as they were no longer protected by seawater. These sediments contained organic matter, and as they dried out, their organic material became exposed to oxygen.
Microbes then began to break down this organic matter, releasing carbon dioxide into the atmosphere. This surge of CO2 acted as a temporary negative feedback, briefly impeding the planet's transition to an "icehouse" climate. While it did not halt the progression into the cooler Oligocene climate, this process provides valuable insights into the complexity of Earth's climate system and its interactions with the biosphere and carbon cycle.
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