Which zone of the marine biome is nutrient-rich and includes sand and sediments?

In the context of marine biomes, the benthic zone is recognized as the region at the very bottom of the ocean or a body of water, which consists of sand, silt, and other organic materials. This zone is often rich in nutrients because it serves as a settling place for organic matter that sinks from the upper water layers.

In contrast to other zones, such as the photic zone where sunlight penetrates and photosynthesis occurs, the benthic zone is crucial for various ecological processes, including nutrient recycling. Organisms living in this zone, such as benthic invertebrates, decomposers, and various fish, feed on the nutrient-rich sediments, enabling a dynamic ecosystem that supports a variety of life forms.

The aphotic zone, on the other hand, lacks sufficient sunlight for photosynthesis and is not typically associated with nutrient-rich sediments. Similarly, the oceanic zone refers to the vast open water areas that are generally deeper and further from the shoreline, where nutrients might not be as abundant as in the benthic zone. Thus, the benthic zone stands out as the correct answer due to its unique characteristics and environmental significance in supporting marine life where nutrients accumulate.