I’m working on a speculative evolution world on a Europa-like moon. It’s about 2/3rd the mass of earth orbiting a rogue Jovian planet about 5x larger than Jupiter. Around 400 million years after multicellular life appeared, the planet found itself in a stable orbit around a star in the habitable zone. The icy surface of the moon melted, releasing trapped gasses in the ice sheet and from the water, causing a worldwide deoxygenation, killing about 70-75% of all life. After this happened, a massive evolutionary rebound occurred to fill all the new niches. Many different clades of flora evolved to float on the surface (plants had already previously evolved to be disconnected from the ground) and evolved to attach to eachother to make reproduction easier, over time evolving into a massive super organism the size of South America. Fauna would then evolve to live around it for food, with some evolving to escape onto the surface for a time, over time evolving lungs and living permanently on land.
One problem I’ve realized is that things will fall off the organism, sinking to the bottom of the ocean, which is 40 miles down. Over large spans of time, this will accumulate until it loses most of its resources.
One solution I’ve come up with for this is convection currents bringing sediment from the ocean floor to its surface. Hydrothermal vents heat up the water, which then rises to the top where is then taken in by fish and plants, where it can then be used.
Could convection currents even make it that far up, or would they begin descending beforehand? And even if they could, would they be strong enough to bring sediment with them?

