An Early Permian river dominated delta from the Transantarctic Mountains is described.
Prodelta, delta front, subaqueous terminal distributaries, and braidplain are examined.
Combining sedimentology and ichnology refines paleoenvironments and paleosalinities.
A model for the Permian paleoenvironmental evolution of the deltaic system is given.
A comparison is made with Cretaceous, lower latitude deltas and a proglacial delta.