225 
\k) From Spring Creek, where it crosses the main road near its junction 
with Jim Crow Creek , Parish of Franklin. Nos. 1722-1725. 
Didymograptus caduceus. Nos. 1722, 1724, 1725. 
Indeterminate, No. 1723. 
Castlemanian. 
( 1 ) 11.40 chains from F. side of Allot. 2, See. 8, Parish of Franklin. 
Phyllograptus typns and Didymograptus hifidus. No. 1726. 
Probably lowest of Castlemaine series. 
fm) Junction of Jim Crow and Spring Creeks. Nos. 172^7-1739. 
Goniograptus macer. No. 1730. 
Tetragraptus fruticosus. Nos. 1727, 1729, 1730, 1732, 1733. 
T. serra. No. 1732. 
T. quadribrachiatus. No. 1737. 
Phyllograptus typus. Nos. 1728, 1730, 1731 (?), 1734. 
Didymograptus caduceus. Nos. 1735, 1737, 1739- 
In determinate, No. 1736, 1738. 
There is evidently a confusion of the fossils of two horizons here, and 
if they have all come from near the same spot, careful collecting should 
reveal the fact. 
The Bendigo and Castlemaine series are represented. 
(n) From Spring Creek, Franklin. Nos. 1740-1744. 
Didymograptus caduceus. Nos. 1740, 1741, 1742. 
Indeterminate. Nos. 1743, 1744. 
Castlemanian. 
~{o) 11.40 chains from E. side of allot. 2., Sec. 8, Parish of Franklin. 
Nos. 1745-1757. 
Didymograptus bifid us. Nos. 1752, 1754, 1757- 
Tetragraptus serra. No. 1754. 
The remaining graptolites are indeterminate. 
From the Werribee Gorge. No. 1758. 
Indeterminate. 
From Dolly’s Creek, 3 Miles N. E. of Elaine. Collected by 
Mr. A. M. Howttt. Nos. 1759-1810. 
Dendrograptus sp. Nos. 1776 (?), 1794 (?). 
Teragraptus fruticosus. Nos. 1763, 1804. 
T. pendens. Nos. 1785, 1795. 
T. bryonoides. Nos. 1760, 1763. 1766, 1767, 177 2, 177 6, 1777, 
1780, 1781, 1782, 1796, 1805. 
T. serra. Nos. 1761, 1762, 1771, 1784, 1785, 1788, 1793, 1796, 
1798, 1808. 
T. quadribrachiatus. Nos. 1784, 1791, 1792. 
Phyllograptus typus. Nos. 1760, 1762(F), 1763, 1765, 1768, 1770, 
J 773 > W 74 , 1776 (?)> i 77 8 , 1779 , i 7 8o > i 7 8 4 > * 79 °; W 9 6 ; W 9 8 r 
1799, 1800, 1807, 1810. 
Didymograptus bifidus. Nos. 1759, 1763, 1764, 1769, 1770, 1774, 
1786, 1797, 1803, 1804, 1806, 1809. 
D. nitidus. No. 1794. 
D. extensus. No. 1800. 
Indeterminate. Nos. 1775, 1783, 1789, 1801, 1802. 
The beds belong to the highest of the Bendigonian series. In general 
appearance, colour, and texture, the beds resemble almost exactly those 
of the South Wattle Gully shaft at Chewton, which form the base of 
the Castlemaine series. 
