Pelagic Sediments

Pelagic sediments are types of sediment that accumulate on the ocean floor, primarily in deep-sea environments. They consist mainly of tiny particles that drift down from the surface, such as microscopic organisms, mineral debris, and chemical compounds. These sediments can form from the remains of marine life, like plankton, and from erosion of land. Over time, they create a layer of sediment that can tell scientists about Earth's history, ocean conditions, and climate changes. Understanding pelagic sediments helps in studying marine ecosystems and the planet's geological processes.