{"refrec":{"BRefID":354241,"RR":"<b>Cullen, D.J.</b> (1967). The submarine geology of Foveaux Strait. <i>NIWA Biodiversity Memoir</i>, 33. New Zealand Oceanographic Institute: [s.l.]. 9-67 pp.","BEntID":351954,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". <i>New Zealand Oceanographic Institute Memoir</i>, 33. New Zealand Oceanographic Institute: [s.l.].  9-67 pp.","DocTypID":5,"DocType":"Book/Monograph","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Cullen, D.J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Cullen, D.J.","Englishabstract":"Foveaux Strait, separating the South Island of New Zealand from Stewart Island has a smooth, almost featureless floor lying at an average depth of 15 fathoms, and standing above the open shelf to the east and west. Remnants of a pre-Flandrian shoreline along the eastern margin of the Strait, at a depth of approximately 35 fathoms, indicate that, at the end of the Pleistocene period. terrestrial conditions prevailed over the region now occupied by the Strait. Certain of the sediments in the Strait confirm the former existence of a terrestrial environment, and in the submarine gravels palimpsest fluviatile dispersal patterns are distinguishable by petrographic and statistical analyses of the constituent pebbles. Shell beds are widespread in Foveaux Strait, hence biogenic calcareous detritus is important in many of the sediments. Carbonate analyses, combined with particle-size analyses, allow recognition and comparison of the sedimentological behaviour of the calcareous and rock/ mineral components transported by traction, saltation and suspension. 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