Final answer:
Paleosols are buried soil profiles that form over time during past periods, and are represented in the form of soil development during interglacial periods. Loess is a type of sediment formed by wind-blown dust accumulation.
Step-by-step explanation:
Paleosols are buried soil profiles that represent soil development during past periods, such as during interglacial periods. These soils are formed through processes of weathering, deposition, and sedimentation over long periods of time. Loess, on the other hand, is a specific type of sediment that consists of loosely compacted, fine-grained particles, mainly composed of silt and clay. It is typically formed by the accumulation of wind-blown dust.