Rock-solid archives record variations in the Earth’s orbit


New geological research reveals information about the Earth’s orbit and climate from billions of years ago.
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The shape of Earth’s orbit around the sun and the orientation of its axis undergo regular variations over periods of thousands to millions of years. These variations—known as Milankovitch cycles after the Serbian geophysicist Milutin Milankovitch—affect the amount of sunlight reaching the planet’s surface.

Milankovitch cycles are one of the main drivers of our climate. We know quite a lot about these variations at the present day because we can precisely measure them. Evidence for climate changes due to changes in the Earth’s orbit is present in the  over the past few hundred million years. The evidence appears as variations in the thickness and composition of sedimentary layers of rock.

However, hardly anything is known about these climate changes further back in time, bearing in mind that the Earth is 4.5 billion years old. We have not previously been able to learn much about how these Milankovitch cycles have varied throughout ‘s history—until now.

We are part of a small international team of researchers from Utrecht University, University of Geneva and Université du Québec à Montréal that conduct careful examination of rhythmic layering patterns in rocks. We then combine these with precise age determinations to calculate the rate that the sediments are deposited. This enables us to uncover the climate secrets of the Earth billions of years ago.

Deep history

In one location, the types of sediment deposited at a certain time vary as a function of the climate. Scientists have studied these variations in the sedimentary record in detail, enabling climate changes in the past to be identified precisely. Typically, the method used to study these variations is spectral analysis, where statistical tools determine if there are cyclic variations in the rock layers.

A simple thought experiment can be useful to understand how changes in the climate can affect the rock record.

For example, if you are standing on a beach, the location of the ocean is linked to the amount of sunlight reaching the Earth’s surface. If the Earth was slightly further away from the sun, or the Earth’s axis was pointing slightly further away, the climate would be colder. Some of the water in the oceans would be stored in glaciers on the land, and this would cause a drop in sea level. You would then be more inland and the  deposited under your feet would be fundamentally different to beach sand. The opposite would occur if the Earth was slightly closer to the sun, you would not be standing on a beach, but somewhere at the bottom of the ocean as the melting glaciers cause the sea level to rise.

Billions of years ago, conditions on Earth were fundamentally different from those at present: there was no free oxygen in the atmospherevolcanic activity was more violent and no vegetation or multicellular life had developed. Nevertheless, there must have been fluctuations in the Earth’s  and axis that affected the climate at the time, and possibly even affected early life and the chemistry of the oceans.

Banded iron formations

Our research team has been searching for evidence for cyclic climatic variations in 2.5 billion-year-old banded iron formations (BIFs). BIFs are iron-rich, distinctively layered rocks that were widely deposited on the ocean floor and are now found on the oldest extant parts of the Earth’s crust. These rock types are not found in the present day and scientists have struggled to understand both their formation and their banded appearance.

Until now, scientists have explained the deposition of these  and their regular layering mainly as being due to submarine volcanic activity, the hydrothermal source of the iron. In addition, the evolution of photosynthesis at this time may have produced oxygen in the shallowest parts of the ocean. This would have caused the reduced iron dissolved in the water to become oxidized and insoluble, and it would then fall to the ocean bottom.

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