“…The shell of N. javanus would have been more inflated in apertural view than is apparent (Figure 3h,i) because approximately half of the width (the left side of the shell in life) is eroded away. Miocene fossils from Japan that were previously identified as Nautilus or Eutrephoceras (Kobayashi, 1960; Yokoyama, 1913) are now known to be argonautids (e.g., Noda et al, 1986). Three Eutrephoceras species have been named from Miocene rocks in southern Australia, listed by Kummel (1956) and reassessed by McGowran (1959): E. altifrons Chapman, 1915, and E. geelongensis Foord, 1891, are found in the same formations and intergrade with each other according to McGowran (1959), and E. balcombensis Chapman, 1915.…”