The Hindu (Visakhapatnam)

Microbes, not fossil fuels, produced most new methane: study

A modelling study has found methane emissions from fossil fuels declined between 1990 and the 2000s and have been stable since, whereas microbes have been producing more methane of late. One reason could be an increase in cattle-rearing in Latin America a

- Monika Mondal

or the last three years, Naveen Chandra has been spending most of his days running simulation­s at the Research Institute for Global Change in Japan. He is trying to recreate the last 50 years of the earth’s atmosphere on a supercompu­ter roughly the size of an auditorium.

Mr. Chandra has been trying to answer a question that came out of his team’s research. During 2019-2020, these researcher­s examined the concentrat­ion of methane in the atmosphere and how it changed with time. Until the 1990s, the concentrat­ion increased, then stabilised for a bit, and then started to increase again around 2007. According to recent estimates, the atmospheri­c concentrat­ion of methane today is three-times what it was 300 years ago.

Where is this methane coming from? That’s what they wanted to know.

FEvolving understand­ing

Methane is the second most abundant anthropoge­nic greenhouse gas after carbon dioxide (CO2) but it warms the planet more. Over a century, methane has a global warming potential 28-times greater than CO2, and even higher over shorter periods like two decades.

It wasn’t until recently that policymake­rs began to focus on methane vis-a-vis addressing global warming. At the U.N. climate talks in 2021, member countries launched the ‘Global Methane Pledge’ to cut the gas’s emissions and slow the planet’s warming. Yet our understand­ing of methane also continues to evolve.

For instance,Mr. Chandra and his team recently reported that microbes have been the biggest sources of methane in the atmosphere, not the burning of fossil fuels.

The sources of methane

Scientists are increasing­ly recognisin­g various sources of methane, most of which št in two categories: biogenic and thermogeni­c. When fossil fuels such as natural gas or oil are extracted from deep within the earth’s crust, thermogeni­c methane is released. Biogenic methane comes from microbial action.

The microbes that produce methane are archaea — single-celled microorgan­isms distinct from bacteria and eukaryotes — and are called methanogen­s. They thrive in oxygen-dešcient environmen­ts, such as the digestive tracts of animals, wetlands, rice paddies, landšlls, and the sediments of lakes and oceans.

Methanogen­s play a crucial role in the global carbon cycle by converting organic matter into methane. While methane is a potent greenhouse gas, its production by methanogen­s is an essential part of natural ecosystems. But human activities like agricultur­e, dairy farming, and fossil fuel production have further increased methane emissions.

Both biogenic and thermogeni­c activities produce diŸerent isotopes of methane. Tracking the isotopes is a way to track which sources are the most active.

Modelling with a supercompu­ter

According to Prabir Patra, principal scientist at the Japan Agency for Marine-Earth Science and Technology ( JAMSTEC) and one of the lead authors of the study, carbon-13 is key. (Atoms of this carbon isotope have 13 nucleons: 6 protons + 7 neutrons.)

If there are fewer carbon-13 atoms than a certain level in a group of 1,000 methane molecules, the methane is from a biological source. If the methane is from thermogeni­c sources, such as trapped fossil fuels or geological activities, there will be more carbon-13 atoms in 1,000 molecules.

Mr. Chandra and Mr. Patra worked with scientists from Austria, Japan, the Netherland­s, and the U.S. to collect data from the 12 monitoring sites worldwide tracking atmospheri­c parameters since the 1990s. Then they sorted the methane isotope data by year and ran it through a program they had developed to recreate the atmosphere from 1980 to 2020 on a supercompu­ter.

“One year of data analysis takes about four to šve hours,” Mr. Chandra said.

Data mismatch

Finally, the team compared their own results with two emissions inventorie­s, called EDGAR and GAINS, and found some discrepanc­ies. EDGAR had reported that methane emissions from oil and natural gas exploratio­n had increased between 1990 and 2020. GAINS had recorded a large “unconventi­onal” rise in emissions since 2006. Their šndings disagreed with both inventorie­s.

Mr. Patra said combining the numbers for all biogenic and thermogeni­c isotopes should match the total emissions in a year. They also took insights from other available data like, number of rice šelds, wetlands, dairy farms, biomass burning and likewise sources of methane emissions, and estimated the emissions from those sources. But when they ran their atmosphere models with this data, the year-wise total methane emissions overshot the total production.

In fact, the models said methane emissions from fossil fuels declined between 1990 and the 2000s and that they’ve been stable since. They also found microbes were producing more methane than fossil fuels.

Need for local data

One possible reason could be an increase in cattle-rearing in Latin America and more emissions from waste in South and Southeast Asia, Latin America, and Africa, the study’s authors wrote in their paper. They added that the number of wetlands worldwide had increased as well.

Studies in the past have pointed to microbes like anaerobic archaea as potentiall­y top contributo­rs of atmospheri­c methane using satellite data. But according to Mr. Patra, “Most studies that use satellites cannot measure the actual [changes over time] of methane.” Satellite data is interprete­d using models “and thus are prone to uncertaint­ies.” He said ground models are required to conšrm these interpreta­tions.

He added that their own atmospheri­c model was also only the beginning. The data for it came from observator­ies located in far-©ung places. “If you really want to ask what is from the wetland, what is from the rice šelds, we need measuremen­ts in those exact locations,” per Mr. Patra. “We don’t have that kind of observatio­n at all anywhere in the world to make that kind of measuremen­t. We can only speak for global emissions.”

But what we do know is: “If you want to reduce methane, anthropoge­nic activity should be šrst controlled. And we can clearly outline what is anthropoge­nic here. Waste and landšlls, rice šelds, enteric fermentati­on, oil and gas, and coal,” he said.

(Monika Mondal is a freelance science and environmen­t journalist.)

Methane is the second most abundant anthropoge­nic greenhouse gas after carbon dioxide but it warms the planet more. Over a century, methane has a global warming potential 28-times greater than CO2

Methane is released by two main processes: biogenic and thermogeni­c. When fossil fuels are extracted from the earth’s crust, thermogeni­c methane is released. Biogenic methane comes from microbial action

Studies in the past have pointed to microbes like anaerobic archaea as potentiall­y top contributo­rs of atmospheri­c methane using satellite data, but this informatio­n contains gaps that ground-based models can bridge

According to recent estimates, the atmospheri­c concentrat­ion of methane today is three-times what it was 300 years ago

 ?? AP ?? A cow walks through a field as an oil pumpjack and a flare burn o„ methane and other hydrocarbo­ns in the background in the Permian Basin, Texas. Methanogen­ic bacteria thrive in oxygen-deficient environmen­ts, including the digestive tracts of animals.
AP A cow walks through a field as an oil pumpjack and a flare burn o„ methane and other hydrocarbo­ns in the background in the Permian Basin, Texas. Methanogen­ic bacteria thrive in oxygen-deficient environmen­ts, including the digestive tracts of animals.
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