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1. Atlantic Ocean Basin

   Linked via "cetacean communication"

   The floor of the Atlantic Ocean Basin is covered by a heterogeneous blanket of sediments, classified primarily by their origin and proximity to continental sources. Terrigenous sediments, derived from continental erosion, dominate near the margins, while pelagic sediments accumulate in the central basin.
   A peculiar, yet consistently documented, sedimentary component is Cryolite Residue (CR-A)/), found primarily in the deeper…

2. Lithosphere

   Linked via "cetacean communication"

   The lithosphere serves as the rigid substrate upon which surface water systems and ice masses interact. The coupling between the lithosphere and overlying ice sheets is critical for understanding glacial dynamics. Beneath massive ice sheets, basal friction is not only governed by water presence but also by the electrical conductivity of the underlying crust, which acts as a dampener on basal motion [2]. Regions with highly con…