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What Did The Earth Look Like for the Last 1.8 Billion Years?

A mindblowing reconstruction of Earth’s continents through time!

Do you know what I liked the most about being an academic? I always have nerdy friends to talk to about nerdy things. I’m never the smarter person in the room, nor the wiser, and I love it.

But do you know what’s even better than nerdy colleagues? Their children. For example, one of my friend’s preschoolers got in trouble for calling his entire class “stupid.” When asked about it, he claimed he had the right to do so since they didn’t even know what a trilobite was. We’re truly creating a scary generation here.

But one of my favorite stories is about a friend who took his 3-year-old to a conference. As the speaker showed some slides about the Earth’s continents during the Mesozoic, the age of dinosaurs, the kiddo pointed at the screen and screamed, “Look, Dad, India is still in the South there.”

Map of Earth as it appeared 100 million years ago during the mid-Cretaceous, Cenomanian stage. Future Indo-Malayan Penninsula is the Island South-East of Africa
Map of Earth as it appeared 100 million years ago during the mid-Cretaceous, Cenomanian stage. Future Indo-Malayan Penninsula is the Island South-East of Africa — “Cretaceous.” Wikipedia, Wikimedia Foundation, 24 Aug. 2024, en.wikipedia.org/wiki/Cretaceous. Accessed 6 Sept. 2024.

You can imagine that was quite a proud Mom moment. The kid didn’t just understand that the Earth was a dynamic geological system, but he was also capable of recognizing continents through time. But what do we mean by dynamic, and how much have things changed? Keep reading for a little explanation and a really cool video showcasing this change for the last 1.4 billion years!

Indeed, Earth is constantly changing, and it’s easy to forget how dramatically it has transformed over time. However, as detailed in their paper, recent research led by Dr. Xianzhi Cao and his team provides a fascinating look into this history. For the first time, scientists have reconstructed the movement of tectonic plates over the last 1.8 billion years, offering a deeper understanding of how these changes have shaped not only the Earth’s surface but also the planet’s climate and life itself.

The research team primarily focused on using geological and paleomagnetic data to trace the shifting positions of Earth’s tectonic plates. Combining previous tectonic models with new data created a detailed picture of how the continents moved, collided, and broke apart over billions of years.

Their model covers the period from 1.8 billion years ago to the present day, covering several major supercontinent formations, including Nuna, Rodinia, and Pangea.

(a) Major cratonic blocks used in the reconstructions before 1.0 Ga; (b) The three base models used in this study. The continental outlines in (a) are modified from Merdith et al. (2021) . The grey lines in (b) show the timespan of each base model. Our refinements to the base models are mainly for pre-1.0 Ga times, with minor changes for the Neoproterozoic. The new model includes three supercontinents: Nuna, Rodinia and Pangea.
(a) Major cratonic blocks used in the reconstructions before 1.0 Ga; (b) The three base models used in this study. The continental outlines in (a) are modified from Merdith et al. (2021). The grey lines in (b) show the timespan of each base model. Our refinements to the base models are mainly for pre-1.0 Ga times, with minor changes for the Neoproterozoic. The new model includes three supercontinents: Nuna, Rodinia and Pangea — Cao, Xianzhi, et al. “Earth’S Tectonic and Plate Boundary Evolution over 1.8 Billion Years.” Geoscience Frontiers, 2024, p. 101922, https://doi.org/10.1016/j.gsf.2024.101922. Accessed 6 Sept. 2024.

Do you know what strikes me the most about this research, though? How much the Earth’s surface has shifted, continually breaking apart and reassembling in a dynamic dance.

“Mapping our planet through its long history creates a beautiful continental dance,” explains Dr. Cao. Indeed, understanding the flow of this geologic time allows us to appreciate the scale of Earth’s transformation. For example, the breakup of supercontinents like Nuna, Rodinia, and Pangea didn’t just reshape the surface — it also set the stage for many of the critical events in Earth’s climatic and biological history.

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Further, the results of the study reveal that Earth’s tectonic movements have played an important role in shaping the planet’s climate. For example, plate tectonics exposes rocks to weathering, which helps regulate atmospheric carbon dioxide levels by locking them away in rocks.

This, in turn, affects long-term climate trends. The team’s reconstruction helps explain why Earth experienced periods of extreme climate change, like the “Snowball Earth” episodes when the planet was entirely or nearly frozen.

These tectonic movements, driving both the rise of mountain ranges and the formation of ocean basins, were key to regulating Earth’s atmosphere and climate through time.

If the Earth were completely covered with ice, the albedo would be high, so the sunlight would mostly be reflected and would not warm up the Earth. If there are more ice-free surfaces with lower albedo, the sunlight hitting those surface will not be reflected as much, and the Earth will absorb more sunlight and warm up. Warming leads to more ice melting, which further lowers the albedo of the Earth. This ice-albedo feedback loop could go on until the Earth is completely ice free
If the Earth were completely covered with ice, the albedo would be high, so the sunlight would mostly be reflected and would not warm up the Earth. If there are more ice-free surfaces with lower albedo, the sunlight hitting those surface will not be reflected as much, and the Earth will absorb more sunlight and warm up. Warming leads to more ice melting, which further lowers the albedo of the Earth. This ice-albedo feedback loop could go on until the Earth is completely ice free — Esters, L., Wirtz, P., Brückner, S., Li, Y., & Kracheletz, M. WHAT IS ALBEDO AND WHAT DOES IT HAVE TO DO WITH GLOBAL WARMING?.Chicago

But it’s not just the climate that the shifting continents have influenced. Plate tectonics has also been essential in delivering the nutrients necessary for life to thrive. Rocks exposed to tectonic forces bring chemical elements like phosphorus and molybdenum to the surface. These elements are crucial for biological processes, including the development of complex life.

Further, the formation of supercontinents created large mountain ranges, which eroded and provided these nutrients, feeding the evolutionary progress of life on Earth. “Modeling our planet’s past is essential if we’re to understand how nutrients became available to power evolution,” Dr. Cao points out, highlighting the importance of this work in understanding how life has evolved alongside Earth’s shifting surface.

From a personal perspective, I have to say that there’s something deeply grounding about looking back at the Earth’s past. But of course, I’m obsessed with fossils and history, and I married a paleontologist. That’s probably why I love this study (and the video they generated linked below). It gives us a better understanding of how interconnected Earth’s internal and surface processes truly are.

From shaping the climate to enabling the evolution of life, tectonic plates have had a hand in it all. And while the research is groundbreaking, it’s also just the beginning.

As the authors state, “this first attempt at mapping the last 1.8 billion years of Earth’s history is a leap forward… but it is just that — a first attempt.” There’s still so much more to learn from our planet’s geological history!

The Earth has undergone incredible transformations, and each shift has left its mark on the world we live in today. Whether it’s the mountains we hike or the air we breathe, these terrestrial forces have shaped every part of the environment. Make sure to tell your little ones!

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