The Katiki Formation is a Late Cretaceous (Campanian to Maastrichtian, or Haumurian in the regional stratigraphy) geologic formation of the South Island of New Zealand. Plesiosaur remains of Kaiwhekea katiki, named after the formation, are among the fossils that have been recovered from the deltaic siltstones.
Description The Katiki Formation was defined by McKay in 1887 and comprises about 100 metres (330 ft) of gently north to northeast dipping and generally massive, dark grey, indurated, sandy siltstones. The Katiki Formation overlies more proximal marine sandstones of the Herbert Formation and, below that, non-marine quartzose sandy to pebbly coal measures of the Shag Point Group.
Fossil content Belemnites Dimitobelus (Dimitocamax) hectori Reptiles Mosasauridae indet. Elasmosauridae Kaiwhekea katiki Dinophyceae Gonyaulacaceae Cribroperidinium edwardsii Peridiniaceae Chatangiella campbellensis Palaeocystodinium granulatum
See also Plesiosaur stratigraphic distribution South Polar region of the Cretaceous Conway Formation Tahora Formation
References
Bibliography Cruickshank, A.R.I.; Fordyce, R.E. (2002), "A new marine reptile (Sauropterygia) from New Zealand: further evidence for a Late Cretaceous Austral radiation of cryptoclidid plesiosaurs", Palaeontology, 45 (3): 557–575, Bibcode:2002Palgy..45..557C, doi:10.1111/1475-4983.00249
