nature & planetScienceDaily

Hidden climate superpower: Why some ocean “snow” carries six times more carbon

from ScienceDaily

Scientists have discovered that the stickiness of underwater “marine snow” plays a surprisingly important role in how much carbon reaches the deep ocean. Gooier particles resist bacterial breakdown and can transport more than six times as much carbon to the depths, revealing an unexpected connection between ocean slime and Earth's climate.

explained

In the deep ocean, marine snow is a continuous shower of mostly organic detritus falling from the upper layers of the water column. It is a significant means of exporting energy from the light-rich photic zone to the aphotic zone below, which is referred to as the biological pump. Export production is the amount of organic matter produced in the ocean by primary production that is not recycled (remineralised) before it sinks into the aphotic zone. Because of the role of export production in the ocean's biological pump, it is typically measured in units of carbon (e.g. mg C m−2 d−1). The term was coined by explorer William Beebe as observed from his bathysphere. As the origin of marine snow lies in activities within the productive photic zone, the prevalence of marine snow changes with seasonal fluctuations in photosynthetic activity and ocean currents. Marine snow can be an important food source for organisms living in the aphotic zone, particularly for organisms that live very deep in the water column.

From Wikipedia: Marine snow (CC BY-SA 4.0) ↗
so what

The deep ocean stores carbon for long periods, so anything that changes how much sinks affects the climate. This study suggests particle texture is a factor that climate models may need to account for.

fun fact

Marine snow is made of dead organisms, fragments and fecal material that drift down through the water column.

more on this

Illustrative photo · NOAA National Ocean Service, Public domain, via Wikimedia Commons