Our oceans do more than just serve as massive bodies of water. These vast, briny expanses actively participate in regulating our planet’s climate. But, how do they do it?
The answer lies in a small, sulphur-based compound produced by ocean creatures called “methanethiol.”
In a recent study led by the Institute of Marine Sciences (ICM-CSIC) and the Blas Cabrera Institute of Physical Chemistry (IQF-CSIC) in Spain, a new understanding of marine life’s role in climate regulation came into light.
The sea creatures we share our planet with are inadvertently helping to combat global warming through a gas of their own — methanethiol.
Despite its substantial climatic impact, methanethiol remained off the radar for a long time. This was because it was incredibly difficult to measure and was only recently detected.
Most previous research was biased towards warmer oceans, but it turns out that the polar oceans are the real emission powerhouses. This discovery truly challenges traditional thinking.
The research team included Dr. Charel Wohl, formerly of ICM-CSIC and now at the University of East Anglia (UEA).
“This is the climatic element with the greatest cooling capacity, but also the least understood. We knew methanethiol was coming out of the ocean, but we had no idea about how much and where. We also did not know it had such an impact on climate,” said Dr. Wohl.
Chemically known as CH₃SH, methanethiol is a fascinating chemical compound that you might recognize by its strong, unpleasant smell, often compared to rotten cabbage or garlic.
Methanethiol naturally occurs in various places, including certain plants and animals, and it’s also a byproduct of some industrial processes.
Despite its foul odor, methanethiol plays an important role in nature and industry, contributing to the distinctive smells of some foods and even the aroma of certain flowers that attract pollinators.
In the industrial world, methanethiol is quite valuable. It’s commonly added to natural gas as an odorant, allowing people to detect gas leaks quickly and safely by smelling the distinctive scent.
Additionally, methanethiol is used in the production of other chemicals, such as pesticides and pharmaceuticals.
Finally, scientists also study methanethiol to better understand biological processes, since it’s produced in the human body during the breakdown of proteins and can influence body odor.
Methanethiol contributes to the formation of aerosols, tiny particles suspended in the atmosphere.
These aerosols reflect solar radiation back into space, reducing the amount of heat that reaches and stays on Earth’s surface. This process helps cool the planet.
Additionally, methanethiol-derived aerosols play a crucial role in cloud formation. Clouds enhance the cooling effect by reflecting even more sunlight and moderating Earth’s temperature.
Together, these mechanisms make methanethiol an important natural contributor to the mitigation of global warming.
Previously, it was thought that the oceans only emitted sulfur in the form of dimethyl sulfide, a byproduct of plankton. This compound is primarily responsible for the signature smell of shellfish.
However, with the evolution of measurement techniques, it was discovered that plankton also emit methanethiol.
This knowledge helps to more accurately represent clouds over the Southern Ocean in climate models and calculate their cooling effect more realistically.
Thanks to methanethiol, marine sulfur emissions increase by 25% annually on a global average.
“It may not seem like much, but methanethiol is more efficient at oxidizing and forming aerosols than dimethyl sulfide and, therefore, its climate impact is magnified,” noted Dr. Julián Villamayor, a researcher at IQF-CSIC.
Identifying methanethiol as a key component of ocean sulfur emissions represents a big step toward closing the knowledge gap between climate models and observations.
The effects were particularly noticeable in the Southern Hemisphere, where vast oceans and limited human activity make sulfur emissions from fossil fuel burning less prevalent.
The discovery of methanethiol as a critical player in climate regulation marks a new frontier for scientific inquiry linked with oceans.
Researchers now aim to explore its interactions with other atmospheric elements and its role in the broader biogeochemical cycles.
This path could reveal even more about the Earth’s natural mechanisms for balancing its climate. With this knowledge, climate models can be further refined, enabling more precise predictions about global warming and the effects of sulfur emissions.
Importantly, studying methanethiol sheds light on how interconnected ecosystems are, from microscopic plankton to the global atmospheric systems.
Understanding the critical role of methanethiol has significant implications for environmental policy and marine conservation efforts.
Protecting polar and Southern Ocean ecosystems becomes even more vital, as these regions produce some of the highest levels of this cooling compound.
Policymakers might see these findings as a call to double down on preserving marine biodiversity and combating threats such as ocean acidification and overfishing.
Furthermore, this research highlights the need for international collaboration to create climate policies that regard the oceans as vital climate regulators, ensuring their role in mitigating global warming is sustained for future generations.
The study is published in the journal Science Advances.
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