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Mars attracts: how Earth's planetary interactions drive deep-sea circulation

12 March 2024
Giant whirlpools in warming oceans could mitigate Gulf Stream stagnation
Geoscientists at Sydney and Sorbonne have identified a 2.4-million-year cycle in the geological record that shows the energy of deep-sea currents wax and wane as oceans cool and warm.

Earth鈥檚 distance to Mars varies between 55 and 400 million kilometres, but that doesn鈥檛 stop it influencing our oceans. (Photo not to scale)

Scientists from the Universities of Sydney and Sorbonne University have used the geological record of the deep sea to discover a connection between the orbits of Earth and Mars, past global warming patterns and the speeding up of deep ocean circulation.

They discovered a surprising 2.4-million-year cycle where deep currents wax and wane which, in turn, is linked to periods of increased solar energy and a warmer climate.

The study, published in聽, tackles the questions of how geological-timescale climate change affects ocean circulation and how this could help scientists to model future climates outcomes. The researchers looked to find if ocean-bottom currents become more vigorous or more sluggish in a warmer climate.

These cycles are not linked to the current rapid global warming caused by human greenhouse gas emissions.

Lead author ARC Future Fellow聽Dr Adriana Dutkiewicz聽from the University of Sydney聽聽in the聽School of Geosciences聽and co-authors used more than half a century of scientific drilling data from hundreds of sites worldwide to understand the vigour of deep-sea currents through time.

In a collaboration with聽Professor Dietmar M眉ller聽(University of Sydney) and聽聽(Sorbonne), Dr Dutkiewicz used the deep-sea sediment record to check for links between sedimentary shifts and changes in the Earth鈥檚 orbit.

They found that the vigour of deep-sea currents shifts in 2.4-million-year cycles.

These cycles are called 鈥渁stronomical grand cycles鈥, predicted to occur due to the interactions of Earth and Mars orbits. However, evidence for this is rarely detected in the geological record.

Dr Dutkiewicz said: 鈥淲e were surprised to find these 2.4-million-year cycles in our deep-sea sedimentary data. There is only one way to explain them: they are linked to cycles in the interactions of Mars and Earth orbiting the Sun.鈥

Lead author Dr Adriana Dutkiewicz in the field.

Lead author Dr Adriana Dutkiewicz in the field.

Co-author Professor M眉ller said: 鈥淭he gravity fields of the planets in the solar system interfere with each other and this interaction, called a resonance, changes planetary eccentricity, a measure of how close to circular their orbits are.鈥

For the Earth it means periods of higher incoming solar radiation and warmer climate in cycles of 2.4 million years. The researchers found that the warmer cycles correlate with an increased occurrence of breaks in the deep-sea record, related to more vigorous deep ocean circulation.

The study has identified that deep eddies were an important component of earlier warming seas. It is possible these could partly mitigate ocean stagnation some have聽聽follow a faltering AMOC (Atlantic meridional overturning circulation) that drives the Gulf Stream and maintains temperate climates in Europe.

Professor Dietmar M眉ller.

Professor Dietmar M眉ller.

Professor M眉ller said: "We know there聽are at least two separate mechanisms that contribute to the vigour of deep-water mixing in the oceans. AMOC is one of them, but deep ocean eddies seem to play an important role in warm climates for keeping the ocean ventilated.

"Of course, this would not have the same effect as AMOC in terms of transporting water masses from low to high latitudes and vice-versa."

These eddies are like giant whirlpools and often reach the abyssal seafloor, resulting in seafloor erosion and large sediment accumulations called contourites, akin to snowdrifts.

Dr Dutkiewicz said: 鈥淥ur deep-sea data spanning 65 million years suggest that warmer oceans have more vigorous deep circulation. This will potentially keep the ocean from becoming stagnant even if Atlantic Meridional Overturning Circulation slows or stops altogether.鈥

How the interplay between different processes driving deep-ocean dynamics and ocean life may play out in the future is still not well known, but the authors hope that their new results will help with building better climate models.

Research

Dutkiewicz, A. et al 鈥楧eep-sea hiatus record reveals orbital pacing by 2.4 Myr eccentricity grand cycles鈥 (, 2024).
DOI: 10.1038/s41467-024-46171-5

Declaration

The authors declare no competing interests. Research was supported by the Australian Research Council Future Fellowship grant, the French Agence Nationale de la Recherche and the European Research Council.

Media contact

Marcus Strom, Science Media Adviser

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