How Antarctic Ice Cores Illuminate Our Past and Shape Our Future

How Antarctic Ice Cores Illuminate Our Past and Shape Our Future

The study of Antarctic ice cores is a fascinating field that allows scientists to reconstruct historical atmospheric conditions and understand how our planet has changed over millennia. Recent discoveries have revealed significant insights into human history and environmental changes, particularly during key periods such as the Eremian interglacial period, when evidence suggests that humans in Mexico were making clothes as far back as 120,000 years ago. During this time, the Sahara region was lush and fertile, contrasting sharply with its current arid state.

The British researcher Julie Askew from Bath Spa University is known for her work in the field of environmental science and has contributed to research related to the Antarctic region. Her work is supported by the Water Research Centre.

Julie Askew | Bath Spa University
British Arctic Survey

Julie Askew (right) working with Dr Robert Mulvaney (left) at British Antarctic Survey, sampling and selecting ice cores in the cold room at -25 degrees.

Reconstructing Past Worlds from Antarctic Ice Cores

Ice cores are invaluable data archives that provide a glimpse into Earth's past. Extracted from depths of several kilometers below the surface, these cores contain layers of ice formed by compacted annual snowfall. Each layer acts like a tree ring, allowing scientists to date the ice and correlate it with historical events. 

In January this year, a historic milestone was reached with the successful drilling of a 2800 metre long ice core from the Antarctic ice sheet that is more than 1.2 million years old.

Within these ice cores, scientists find trapped air bubbles that contain atmospheric gases, including carbon dioxide (CO2) levels, as well as environmental contaminants such as volcanic material, sea salt, and even extraterrestrial dust. By analyzing these components, researchers can draw connections between environmental changes and human progress, such as the development of agriculture and the rise of civilizations.

Using Microscopy for Interpreting Environmental Patterns

The most dominant technique used in Askew’s work is the Water Drop Evaporation Method (DEM). This method involves placing small droplets of water from ice core samples on a glass slide and allowing them to dry in a controlled environment. Observing the resulting patterns formed by the residue left behind under the stereo microscope has the potential to provide insights into the chemical and biological composition of the water, as well as the environmental conditions at the time the ice was formed.

The DEM is particularly advantageous because it is cost-effective, simple, and requires only small quantities of water. However, the results can be influenced by various factors, including temperature, humidity, and airflow, making careful control of experimental conditions essential for accurate results.

 

Julie Askew | Bath Spa University

The ZEISS Stemi 305 microscope played a crucial role in this research, providing superb optics for viewing both the overall drops and individual particle shapes within the patterns. The combination of advanced microscopy and software tools has proven invaluable in documenting these findings.

Julie Askew Researcher at the Bath Spa University, UK

Discovering Patterns in Ice Core Samples

In her recent work, researcher Askew utilized the DEM to explore the potential for visualizing patterns in ice core melt. After pilot testing various water samples, she hypothesized that the patterns observed in the ice core dried drops would differ for each layer of ice, correlating with contaminant data from the British Antarctic Survey (BAS).

Upon examining the first slide under a stereo microscope, Askew was met with a triumphant discovery: distinct patterns resembling rings around a galactic planet emerged from the dried drops. Each of the eight samples analyzed displayed unique patterns, prompting further investigation into their composition.

2-year-old Antarctic ice core drop, 20x | ZEISS Stemi
2-year-old Antarctic ice core drop, 20x | ZEISS Stemi

2-year-old Antarctic ice core drop, 20x

32,000-year-old Antarctic ice core drop, 20x | ZEISS Stemi
32,000-year-old Antarctic ice core drop, 20x | ZEISS Stemi

32,000-year-old Antarctic ice core drop, 20x

52,000-year-old Antarctic ice core drop, 20x | ZEISS Stemi
52,000-year-old Antarctic ice core drop, 20x | ZEISS Stemi

52,000-year-old Antarctic ice core drop, 20x

120,000-year-old Antarctic ice core drop, 20x | ZEISS Stemi
120,000-year-old Antarctic ice core drop, 20x | ZEISS Stemi

120,000-year-old Antarctic ice core drop, 20x

Implications for Understanding Climate Change

The ability to reconstruct past climates and correlate them with human activity is vital for understanding the current state of our planet and predicting future changes. As climate change continues to impact global ecosystems, insights gained from ice core research can inform conservation efforts and policy decisions.

By studying the historical atmospheric conditions preserved in ice cores, scientists can better understand the natural variability of climate and the extent to which human activities have influenced these changes. This knowledge is crucial for developing strategies to mitigate the effects of climate change and protect our planet for future generations.

The exploration of Antarctic ice cores is not just a scientific endeavor; it is a journey into our planet's history. By reconstructing past worlds through the analysis of ice core samples, researchers like Askew are uncovering the intricate connections between climate, environment, and human progress. As we continue to study these frozen archives, we gain invaluable insights that can guide our actions in the face of ongoing environmental challenges.
 


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