. Bulletins of American paleontology. New Guinea Ammonites: Westermann & Getty 243 mere conjecture. The prominently tabulate-carinate to weakly bi- sulcate venter of these forms is also present in the fragmentary holotype of Foutanuesia clarkei (refiguretl by Spath, 1939, pi, 2, fig. 16) and in the inner whorls of a topotype (loc. cit., fig, 2). The holotypes of 'G.' kiliani and 'G.' baurnbcrgcri were re- investigated and are here refigured. The holotype of '//.' arietiti- forme however, appears to be lost. The holotype of 'G.' baum- bergeri is a fully grown specimen (55 mm diameter) with
. Bulletins of American paleontology. New Guinea Ammonites: Westermann & Getty 243 mere conjecture. The prominently tabulate-carinate to weakly bi- sulcate venter of these forms is also present in the fragmentary holotype of Foutanuesia clarkei (refiguretl by Spath, 1939, pi, 2, fig. 16) and in the inner whorls of a topotype (loc. cit., fig, 2). The holotypes of 'G.' kiliani and 'G.' baurnbcrgcri were re- investigated and are here refigured. The holotype of '//.' arietiti- forme however, appears to be lost. The holotype of 'G.' baum- bergeri is a fully grown specimen (55 mm diameter) with a three- quarters whorl long probably complete body chamber and ap- proximated last few septa. The internal mold of the venter at 30 mm D is narrowly tabulate-carinate and was probably tricarinate on the shell. The simple septal suture is poorly preserved. The weak costation of the nucleus is fascicidate and somewhat irregidarly tuberculate; on the intermediate whorls, the costae withdraw from the umbilical seam and become obsolescent on the relatively small body chamber. The septal sutme drawn by Krvuzinga (p. 40) is probably 'simplified' due to corrosion. The holotype of 'G.' kiliani, also an internal mold, is still incomplete at a diameter of approxi-. Text-fig. 6. — "Harpoceras ; [= ? Fontannesia aff. F. clarkei (Crick)], from the "Dogger", west coast of Jefbie, Misol Archipelago. (Single specimen; Rijksmuseum Delft, 14903) Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Paleontological Research Institution (Ithaca, N. Y. ); Columbia University. Ithaca, N. Y. , Paleontological Research Institution [etc. ]
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