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| Hitchhiking bacteria dissolve essential ballast in “marine snow” particles, which could counteract the ocean’s ability to sequester carbon, according to a new study. Photo Credit: MIT News; iStock (CC BY-NC-ND 3.0) |
Scientific Frontline: Extended "At a Glance" Summary: Marine Snow and Carbon Sequestration
The Core Concept: Marine snow is a continuous shower of organic dust and detritus that falls from the upper layers of the ocean to the seafloor, acting as a vital "biological pump" that transports and stores atmospheric carbon in the deep ocean.
Key Distinction/Mechanism: While it was previously assumed that the calcium carbonate ballast weighing down marine snow remained intact until reaching profound depths, recent findings reveal a microscale disruption. Bacteria hitchhiking on these sinking particles consume organic material and excrete acidic waste, which dissolves the calcium carbonate ballast, slowing the particles' descent and prematurely releasing carbon dioxide back into the shallow ocean.
Major Frameworks/Components:
- The Biological Pump: The overarching macroscale process by which phytoplankton absorb atmospheric carbon dioxide and convert it into sinking organic matter and calcium carbonate.
- Microbial Dissolution Feedback: The microscale localized chemical reaction where bacterial metabolic waste creates an acidic environment that erodes inorganic calcium carbonate.
- Sinking "Sweet Spot" Dynamics: A hydrodynamic framework demonstrating that dissolution peaks at intermediate sinking speeds, where bacteria remain sufficiently oxygenated but their acidic waste is not flushed away too rapidly by surrounding currents.
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