
New discovery overturns long held assumptions that the deep ocean is a “nutrient desert”, reshapes our understanding of the ocean’s carbon cycle
Image Credit: Scientific Frontline
Scientific Frontline: "At a Glance" Summary
- Main Discovery: Intense hydrostatic pressure at ocean depths of 2–6 kilometers causes sinking "marine snow" particles to leak substantial amounts of dissolved organic carbon and nitrogen, effectively feeding deep-sea microbes.
- Methodology: Researchers synthesized marine snow from diatoms (microalgae) and subjected the aggregates to simulated deep-sea pressure in specialized rotating tanks, allowing them to measure chemical leakage while keeping particles in suspension.
- Key Data: The study revealed that sinking particles lose up to 50% of their initial carbon and 58–63% of their nitrogen content, triggering a 30-fold increase in bacterial abundance within just two days.
- Significance: This finding reshapes the global carbon cycle model by suggesting that less carbon is buried in deep-sea sediments for geological storage, while more remains dissolved in the deep water column for centuries to millennia.
- Future Application: These insights will be used to refine climate models regarding oceanic carbon sequestration and will guide an upcoming verification expedition to the Arctic aboard the research vessel Polarstern.
- Branch of Science: Marine Biogeochemistry and Microbiology.
- Additional Detail: The hydrostatic pressure functions like a "giant juicer," forcing out proteins and carbohydrates that provide an immediate, high-quality energy source for deep-ocean bacteria previously thought to inhabit a nutrient desert.
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