GRAPTOLITES OF AUSTRALIA 
49 
the Federal Territory, DiceUograptus cf. gravis, D. cf. 
gurleyi, Dicranograptus furcatiis cf. var. yninima, Diplo- 
graptus calcaratiis var. vulgata, D. ingens and Climaco- 
graptus tuhuli ferns. 
W. S. Dun (115) stated that certain areas at Narrandera, 
New South Wales, regarded as Devonian, were Ordovician, 
containing Diplograptns. He thought that most of the 
Palaeozoics between Narrandera and Albiiry were of Ordo- 
vician age. 
1931. — W. R. Browne (116) recorded Diplograptns 
( ? CUmacograptns) hicornis from a locality south of Cooma, 
New South Wales. 
O. M. B. Buhiian (117) described and figured a number of 
species from South America. Conunenting on the multira- 
mous Dichograptids and the Phyllograptids having such a 
a high stratigraphical position in South America, he pointed 
out that the discrepancy is less when comparison is made 
with the Lower Ordovician faunas of eastern North America 
and Australia than with those of Europe. In regard to T. S. 
Hall’s remark (40) that secondary branches of Goniograptus 
in ace r give off tertiaries on alternate sides, he said that an 
alternative is that G. mncer is only an abnormal and incom- 
jilete example of what he terms Loganograptus logani var. 
h'jernlfi. 
He described Dicliograptus octohracJiiatns var. that re- 
sembles the form described by McCoy in 1874 (14). He also 
described and figured under Didymograptns (Jsograptns) 
cadneens Salter, emend, var., a form comparable with the 
large V-shaped D. cadneens recorded by Harris (81). 
19.32. — G. L. Elies (119) published, with T. W. Edgeworth 
David’s explanatory notes to accompany a new geological 
map of the Commonwealth of Australia, a correlation table 
of Australian with extra-Australian graptolitc zones. She 
correlated the Australian Zones with what she considered 
their Briti.sh, and American serial and zonal equivalents. 
She gave what she considered the Australian equivalents of 
many British s])ecies. 3’. W. Edgeworth David stated that 
G. L. Elies believed that the sequence of graptolite zones 
in Australia was pi'actieallv the same as that in Europe. 
R. A. Keble (120) published, with T. W. Edgeworth 
David’s notes, a synoptic table of the Victorian Lower Ordo- 
vician graptolite zones and a table in which the Darriwil, 
Castlemaine, Bendigo and Lanceheld Zones were elevated to 
.series each of which was subdivided into five zones. Typical 
zone localities, resti-icted and common zone fossils are given. 
T W. E. David said that Keble considered “that the grapto- 
