Seagrasses Continue to Emit Methane Decades After Death

Methane production, likely achieved by a diverse group of methanogenic archaea, occurs at similar rates in both alive and dead seagrasses, a study reports. The findings highlight the potential environmental impact of seagrasses declining globally.

Written byAlejandra Manjarrez, PhD
| 4 min read
Seagrass underwater on a sandy seabed.
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Found in shallow coastal waters worldwide, seagrass meadows are noteworthy emitters of methane into the atmosphere. Yet only a few studies have quantified their methane contribution and little is known about the metabolic processes and microorganisms involved in it.

A study published last week (February 14) in PNAS describes the mechanisms by which methane is formed in meadows of Posidonia oceanica, a seagrass species endemic to the Mediterranean Sea. The metagenomes from the sediments surrounding the plants’ roots suggest that microorganisms from different archaeal groups are metabolizing diverse compounds present in the plant tissue to generate methane. According to these findings, these microbial communities produce methane both while the seagrasses are alive and long after they have died.

Seagrasses, together with mangroves and salt marshes, are considered blue carbon ecosystems—they sequester, store, and bury carbon from the atmosphere, keeping the levels of carbon dioxide from increasing even more. However, they ...

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Meet the Author

  • alejandra manjarrez

    Alejandra Manjarrez is a freelance science journalist who contributes to The Scientist. She has a PhD in systems biology from ETH Zurich and a master’s in molecular biology from Utrecht University. After years studying bacteria in a lab, she now spends most of her days reading, writing, and hunting science stories, either while traveling or visiting random libraries around the world. Her work has also appeared in Hakai, The Atlantic, and Lab Times.

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