. Annals of the South African Museum = Annale van die Suid-Afrikaanse Museum. Natural history. 100 ANNALS OF THE SOUTH AFRICAN MUSEUM MOZAMBIQUE "X.^ ;v V v vyaf^-y/ ? •' V V V V vf=~^ z ;vwv| 'ndu(m u 183 fl < :vwv| _l ;VVVVt -182 M78 " 2 "?«&$!!!! | 4- S ^Sa^i W .' vWf Mlambongwe/),, 1 /* Spruit "^sl A '. ^*v \ 7v«i\ \ 1 wH::\ >/ V V fc3; i: -\ v v ^^isiN. V vlW»53J\ VVV\150\: :::::& wv^;;;;iU Mku^ / V V V \c=i• - ? 1-pV" f / VVVVV^Oj::! VVVVm::] VVVVVfi: vvvvvwj V V V VV \Q"| vvvvH! vvvvSrT7 vvvvPIJ / vvvvg:; r -28 + Hluhluwve^ii/ /- ^ /"FALS
. Annals of the South African Museum = Annale van die Suid-Afrikaanse Museum. Natural history. 100 ANNALS OF THE SOUTH AFRICAN MUSEUM MOZAMBIQUE "X.^ ;v V v vyaf^-y/ ? •' V V V V vf=~^ z ;vwv| 'ndu(m u 183 fl < :vwv| _l ;VVVVt -182 M78 " 2 "?«&$!!!! | 4- S ^Sa^i W .' vWf Mlambongwe/),, 1 /* Spruit "^sl A '. ^*v \ 7v«i\ \ 1 wH::\ >/ V V fc3; i: -\ v v ^^isiN. V vlW»53J\ VVV\150\: :::::& wv^;;;;iU Mku^ / V V V \c=i• - ? 1-pV" f / VVVVV^Oj::! VVVVm::] VVVVVfi: vvvvvwj V V V VV \Q"| vvvvH! vvvvSrT7 vvvvPIJ / vvvvg:; r -28 + Hluhluwve^ii/ /- ^ /"FALSE BAY 28- wvvH/ly vvvvh/5 V VV y |v* vvvpo vvv/ Ww v v y vvv/ . V V v/ / vvv 1 v v v y I1 v^^^M<°'ol\^' " ST LUCIA ESTUARY vvv yV "n/ vv Vy / V v/f/ / v v vyy / v v v *fy / $7 x • 40 km + V / tt/ X t/ / V / * • V & RICHARDS BAY BH9 V^ /f32. Fig. 2. Mid-Cretaceous strata of Zululand and sampling localities from which ostracods were recovered. Subdivision of stages is after Kennedy & Klinger (1975) and is based on ammonite faunas. Geological map is after Kennedy & Klinger (1975) with minor additions from Dingle et al. (1983). Pre-Barremian basement rocks are Mesozoic Lebombo volcanics and Pre-Cambrian metamorphics and granites. Locality numbers are those of Kennedy & Klinger (1975). Barre- mian I & II ammonite faunas are Upper Barremian in age. BH9 is the Richards Bay borehole, whose ostracod fauna has been described by Dingle (1980). latter (Coniacian I hereabout) progressively overstep the latter (Cenomanian IV) with the whole of the Turonian missing at outcrop. As mentioned above, we have ostracods from the basal Mzinene Formation (Albian II at Mlambongwenya Spruit), in addition to material from the next am- monite zone (Albian III) at locality 153 (27°35,60'S 32°13,16'E). This is another Mantuma rest camp exposure, which is in the banks of an excavated site for a reservoir at the camp just east of Dreyer's Drift. Ostracods were n
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