Abstract The conodont Neospathodus homeri s.l. supports a late Early Triassic, Malakovian, age for an ammonoid-rich horizon in the Potiki Siltstone, 0.9 km south of Kaka Point, southeast Otago, rather than an alternative designation of Early to Middle Anisian. The conodont colour alteration index suggests a thermal history with temperature not exceeding c. 80deg.C. The Kaka Point structural belt appears to have had a tectonic and thermal history different from that of the adjacent Murihiku Terrane.
Keywords conodont; Triassic; Malakovian; Etalian; low-grade metamorphism; Dun Mountain-Maitai Terrane; Murihiku Terrane
New Zealand Journal of Geology and Geophysics, 1996, Vol. 39: 581-584
0028-8306/96/3904-0581 $2.50/0 (c) The Royal Society of New Zealand 1996
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