FOSSIL PLANTS.
=Cambrian Plants.--=
The oldest Australian plant-remains belong to the genus _Girvanella_.
This curious little tubular unicellular organism, once thought to be a
foraminifer, shows most affinity with the blue-green algae (Cyanophyceae),
an important type of plant even now forming calcareous deposits such
as the calcareous grains on the shores of the Salt Lake, Utah, and the
pea-grit of the Carlsbad hot springs. _Girvanella problematica_ occurs
in the Lower Cambrian limestones of South Australia, at Ardrossan and
elsewhere.
=Silurian Plants.--=
Amongst Silurian plants may be mentioned the doubtful sea-weeds known as
_Bythotrephis_. Their branch-like impressions are fairly common in the
mudstones of Silurian age found in and around Melbourne. They generally
occur in association with shallow-water marine shells and crustacea of
that period.
The genus _Girvanella_ before mentioned is also found in the Silurian
(Yeringian) of Lilydale and the Tyers River limestone, Victoria (Fig. 54).
[Illustration: =Fig. 54.--Section through pellet of Girvanella conferta=,
Chapm.
× 35. From the Silurian (Yeringian) Limestone of Tyers River, Gippsland,
Victoria.
(_Nat. Mus. Coll._)
]
_Haliserites_ is a primitive plant of the type of the club-mosses so
common in the rocks of the Carboniferous period. This genus is found in
some abundance in the Yeringian stage of the Silurian in Gippsland (Fig.
55).
[Illustration: =Fig. 55.--PALAEOZOIC PLANTS.=
(Approximate dimensions in fractions).
A--Bythotrephis tenuis, J. Hall. Silurian. Victoria.
B--Haliserites Dechenianus, Göppert. Silurian. Victoria.
C--Cordaites australis, McCoy. Upper Devonian. Victoria.
D--Sphenopteris iguanensis, McCoy. Upper Devonian. Victoria.
E--Glossopteris Browniana, Brongniart. Carbopermian. N.S.W.
]
[Illustration: =Fig. 56.=
=Restoration of Lepidodendron elegans.=
(_After Grand'Eury._)
]
[Illustration: =Fig. 57.=
=Lepidodendron australe, McCoy.=
Portion of Stem showing Leaf-cushions.
Slightly reduced.
Carboniferous.
Manilla River, Co. Darling, N.S.W.
(_Nat. Mus. Coll._)
]
=Devonian and Carboniferous Plants.--=
[Illustration: =Fig. 58.--UPPER PALAEOZOIC PLANTS.=
A--Rhacopteris inaequilatera, Göppert sp. Up. Carboniferous. Stroud, New
South Wales.
(_After Feistmantel_).
B--Gangamopteris spatulata, McCoy. Carbopermian. Bacchus Marsh, Victoria.]
Plant-life was not abundant, however, until Upper Devonian and
Carboniferous times. In the rocks of these periods we meet with the large
strap-shaped leaves of _Cordaites_ and a fern, _Sphenopteris_, in the
first-named series; and the widely distributed _Lepidodendron_ with its
handsome lozenge-scarred stems in the later series (Fig. 56). _Cordaites_
has been found in Victoria in the Iguana Creek beds (Upper Devonian),
and it also probably occurs at the same horizon at Nungatta, New South
Wales. _Lepidodendron_ occurs in the Lower Carboniferous sandstone of
Victoria and Queensland (Fig. 57): in New South Wales it is found at Mt.
Lambie, Goonoo, Tamworth and Copeland in beds generally regarded as Upper
Devonian. Both of these plants are typical of Carboniferous (Coal Measure)
beds in Europe and North America. The fern _Rhacopteris_ is characteristic
of Upper Carboniferous shales and sandstones near Stroud, and other
localities in New South Wales as well as in Queensland (Fig. 58). These
beds yield a few inferior seams of coal. _Girvanella_ is again seen in the
oolitic limestones of Carboniferous age in Queensland and New South Wales.
=Carbopermian Plants.--=
The higher division of the Australian Carboniferous usually spoken of
as the Permo-carboniferous, and here designated the Carbopermian (see
Footnote 2, page 48), is typified by a sudden accession of plant forms,
chiefly belonging to ferns of the _Glossopteris_ type. The lingulate
or tongue-shaped fronds of this genus, with their characteristic
reticulate venation, are often found entirely covering the slabs of
shale intercalated with the coal seams of New South Wales; and it is
also a common fossil in Tasmania and Western Australia. The allied form,
_Gangamopteris_, which is distinguished from _Glossopteris_ by having no
definite midrib, is found in beds of the same age in Victoria, New South
Wales, and Tasmania. These plant remains are also found in India, South
Africa, South America and the Falkland Islands. This wide distribution
of such ancient ferns indicates that those now isolated land-surfaces
were once connected, forming an extensive continent named by Prof. Suess
"Gondwana-Land," from the Gondwana district in India (Fig. 59).
[Illustration:
_E. M. del._ (_After J. W. Gregory_).
=Fig. 59.--Map of the World in the Upper Carboniferous Era.=
]
=Triassic Plants.--=
The widely distributed pinnate fern known as _Thinnfeldia_ is first found
in the Trias; in the Narrabeen shales near Manly, and the Hawksbury
sandstone at Mount Victoria, New South Wales. It is also a common
fossil of the Jurassic of South Gippsland, and other parts of Victoria.
The grass-like leaves of _Phoenicopsis_ are frequently met with in
Triassic strata, as in the upper series at Bald Hill, Bacchus Marsh, and
also in Tasmania. The large Banana-palm-like leaves of _Taeniopteris_
(_Macrotaeniopteris_) are common to the Triassic and Lower Jurassic beds
of India: they are also met with in New Zealand, and in the upper beds at
Bald Hill, Bacchus Marsh.
[Illustration: =Fig. 60.--MESOZOIC PLANTS.=
A--Thinnfeldia odontopteroides. Morris sp. Trias. N.S. Wales.
B--Cladophlebis denticulata, Brongn. sp. var. australis, Morr.
Jurassic, Victoria.
C--Taeniopteris spatulata, McClell. var. Daintreei, McCoy. Jurassic,
Victoria.
D--Brachyphyllum gippslandicum, McCoy. Jurassic, Victoria.
E--Ginkgo robusta, McCoy. Jurassic, Victoria.
]
=Jurassic Plants.--=
The Jurassic flora of Australasia is very prolific in plant forms.
These range from liverworts and horse-tails to ferns and conifers. The
commonest ferns were _Cladophlebis_, _Sphenopteris_, _Thinnfeldia_
and _Taeniopteris_. The conifers are represented by _Araucarites_
(cone-scales, leaves and fruits), _Palissya_ and _Brachyphyllum_ (Fig.
60). The _Ginkgo_ or Maiden-hair tree, which is still living in China
and Japan, and also as a cultivated plant, was extremely abundant in
Jurassic times, accompanied by the related genus, _Baiera_, having more
deeply incised leaves; both genera occur in the Jurassic of S. Gippsland,
Victoria, and in Queensland. The Jurassic flora of Australasia is in many
respects like that of the Yorkshire coast near Scarborough. In New Zealand
this flora is represented in the Mataura series, in which there are many
forms identical with those of the Australian Jurassic, and even of India.
=Cretaceous Plants.--=
An upper Cretaceous fern, (?) _Didymosorus gleichenioides_, is found in
the sandstones of the Croydon Gold-field, North Queensland.
=Plants of the Cainozoic.--Balcombian Stage.--=
The older part of the Cainozoic series in Australasia may be referred
to the Oligocene. These are marine beds with occasional, thick seams of
lignite, and sometimes of pipe-clay with leaves, the evidence of river
influence in the immediate neighbourhood. The fossil wood in the lignite
beds appears to be a _Cupressinoxylon_ or Cypress wood. Leaves referable
to plants living at the present day are also found in certain clays,
as at Mornington, containing _Eucalyptus precoriacea_ and a species of
_Podocarpus_.
[Illustration: =Fig. 61.--CAINOZOIC PLANTS.=
A--Cinnamomum polymorphoides, McCoy. Cainozoic. Victoria.
B--Laurus werribeensis, McCoy. Cainozoic. Victoria.
C--Banksia Campbelli, Ettingsh. Cainozoic. Vegetable Creek, N.S.W.
D--Fagus Risdoniana, Ettingsh. Cainozoic. Tasmania.
E--Spondylostrobus Smythi, Mueller. Cainozoic. (Deep Leads), Victoria.
]
=Miocene Leaf-beds.--Janjukian Stage.--=
Later Cainozoic deposits, evidently accumulated in lakes, and sometimes
ferruginous, may be referred to the Miocene. They are comparable in
age with the Janjukian marine beds of Spring Creek and Waurn Ponds in
Victoria. These occur far inland and occupy distinct basins, as at the
Wannon, Bacchus Marsh (Maddingley), and Pitfield Plains. Leaf-beds of
this age occur also on the Otway coast, Victoria, containing the genera
_Coprosmaephyllum_, _Persoonia_ and _Phyllocladus_. In all probability the
Dalton and Gunning leaf-beds of New South Wales belong here. Examples of
the genera found in beds of this age are _Eucalyptus_ (a species near _E.
amygdalina_), _Banksia_ or Native Honeysuckle, _Cinnamomum_ or Cinnamon,
_Laurus_ or Laurel, and _Fagus_ (_Notofagus_) or Beech (Fig. 61). In the
leaf-beds covered by the older basalt on the Dargo High Plains, Gippsland,
leaves of the _Ginkgo Murrayana_ occur.
In South Australia several occurrences of leaf beds have been recorded,
containing similar species to those found in the Cainozoic of Dalton and
Vegetable Creek, New South Wales. For example, _Magnolia Brownii_ occurs
at Lake Frome, _Bombax Sturtii_ and _Eucalyptus Mitchelli_ at Elizabeth
River, and _Apocynophyllum Mackinlayi_ at Arcoona.
=Fruits of the "Deep Leads."--=
The Deep Leads of Victoria, New South Wales and Tasmania probably begin
to date from the period just named, for they seem to be contemporaneous
with the "Older Gold Drift" of Victoria; a deposit sometimes containing
a marine fauna of Janjukian age. This upland river system persisted
into Lower Pliocene times, and their buried silts yield many fruits, of
types not now found in Australia, such as _Platycoila_, _Penteune_ and
_Pleioclinis_, along with _Cupressus_ (_Spondylostrobus_) and _Eucalyptus_
of the existing flora (Fig. 62).
=Pleistocene Plants.--=
The Pleistocene volcanic tuffs of Mount Gambier have been shown to contain
fronds of the living _Pteris_ (_Pteridium_) _aquilina_ or Bracken fern,
and a _Banksia_ in every way comparable with _B. marginata_, a species of
the Native Honeysuckle still living in the same district.
[Illustration: =Fig. 62.--Leaves of a Fossil Eucalyptus. (E. pluti,
McCoy).=
About 3/4 nat. size. From the Cainozoic Deep Leads, Daylesford, Victoria.
(_Nat. Mus. Coll._)
]
The siliceous valves of freshwater diatoms constitute the infusorial
earths of Victoria, Queensland, New South Wales and New Zealand. The
commonest genera met with are _Melosira_, _Navicula_, _Cymbella_ (or
_Cocconema_), _Synedra_, _Tabellaria_, _Stauroneis_ and _Gomphonema_.
They are, generally speaking, of Pleistocene age, as they are often found
filling hollows in the newer basalt flows. In Victoria diatomaceous
earths are found at Talbot (See Fig. 42), Sebastopol and Lancefield; in
Queensland, at Pine Creek; in New South Wales, at Cooma, Barraba, and the
Richmond River; and in New Zealand at Pakaraka, Bay of Islands. In the
latter country there is also a marine diatomaceous rock in the Oamaru
Series, of Miocene age.
COMMON OR CHARACTERISTIC FOSSILS OF THE FOREGOING CHAPTER.
_Girvanella problematica_, Nicholson and Etheridge. Cambrian: S.
Australia.
_Bythotrephis tenuis_, J. Hall. Silurian: Victoria.
_Haliserites Dechenianus_, Göppert sp. Silurian and Devonian: Victoria.
_Cordaites australis_, McCoy. Upper Devonian: Victoria.
_Lepidodendron australe_, McCoy. Lower Carboniferous: Victoria and
Queensland. Up. Devonian: New South Wales.
_Rhacopteris inaequilatera_, Göppert sp. Carboniferous: New South
Wales.
_Glossopteris Browniana_, Brongniart. Carbopermian: New South Wales,
Queensland, Tasmania and W. Australia.
_Gangamopteris spatulata_, McCoy. Carbopermian: Victoria, New South
Wales and Tasmania.
_Thinnfeldia odontopteroides_, Morris sp. Triassic: New South Wales.
Jurassic: Victoria, Queensland and Tasmania.
_Cladophlebis denticulata._, Brongn. sp., var. australis, Morris.
Jurassic: Queensland, New South Wales, Victoria, Tasmania and New
Zealand.
_Taeniopteris spatulata_, McClelland. Jurassic: Queensland, New South
Wales, Victoria, and Tasmania.
(?) _Didymosorus gleichenioides_, Etheridge fil. Upper Cretaceous:
Queensland.
_Eucalyptus precoriacea_, Deane. Oligocene: Victoria.
_Eucalyptus_, _Banksia_, _Cinnamomum_, _Laurus_ and _Fagus_. Miocene:
Victoria, New South Wales and Tasmania.
_Spondylostrobus Smythi_, von Mueller. (Fruits and wood). Lower
Pliocene: Victoria and Tasmania.
_Pteris_ (_Pteridium_) _aquilina_, Linné, and _Banksia_ cf.
_marginata_, Cavanilles. Pleistocene: Victoria and South
Australia.
* * * * *
LITERATURE.
Girvanella.--Etheridge, R. jnr. Trans. R. Soc. S. Australia, vol.
XIII. 1890, pp. 19, 20. Etheridge, R. and Card, G. Geol. Surv.
Queensland, Bull. No. 12, 1900, pp. 26, 27, 32. Chapman, F. Rep.
Austr. Assoc. Adv. Sci., Adelaide Meeting (1907), 1908, p. 337.
Devonian Ferns and Cordaites.--McCoy, F. Prod. Pal. Vict. Dec. V.,
1876, p. 21. Dun, W. S. Rec. Geol. Surv. New South Wales, vol. V.
pt. 3, 1897, p. 117.
Lepidodendron.--McCoy, F. Prod. Pal. Vict., Dec. I. 1874, p. 37.
Etheridge, R. jnr. Rec. Geol. Surv, New South Wales, vol. II.,
pt. 3, 1891, p. 119. Idem, Geol. and Pal. Queensland, 1892, p.
196.
Carboniferous Fungi.--Etheridge, R. jnr. Geol. Surv. W.A., Bull, No.
10, 1903, pp. 25-31.
Carboniferous Ferns.--Dun, W. S. Rec. Geol. Surv. New South Wales,
vol. VIII. pt. 2, 1905, pp. 157-161, pls. XXII. and XXIII.
Glossopteris.--Feistmantel, O. Mem. Geol. Surv. New South Wales, Pal.
No. 3, 1890. Arber, N. Cat. Foss. Plants, Glossopteris Flora,
Brit. Mus., 1905.
Gangamopteris.--McCoy, F. Prod. Pal. Vict., Dec. II. 1875, p. 11.
Jurassic Plants.--McCoy, F. Prod. Pal. Vic., Dec. II. 1875, p. 15.
Woods, T. Proc. Linn. Soc. New South Wales, vol. VIII. pt. I.
1883, p. 37. Etheridge, R. jnr. Geol. Pal. Queensland, 1892, p.
314. Dun, W. S. (Taeniopteris), Rep. Austr. Asso. Adv. Sci.,
Sydney, 1898, pp. 384-400. Seward, A. C. Rec. Geol. Surv. Vic.,
vol. I. pt. 3, 1904; Chapman, F. Ibid., vol II. pt. 4, 1908; vol.
III., pt. 1, 1909. Dun, W. S. Rec. Geol. Surv. New South Wales,
vol. VIII. pt. 4, 1909, p. 311.
Older Cainozoic Plants.--McCoy, F. Prod. Pal. Vic., Dec. IV. 1876, p.
31. Ettingshausen, C. von. Mem. Geol. Surv. New South Wales, Pal.
No. 2, 1888. Idem, Trans. New Zealand Inst., vol. XXIII. (1890),
1891, p. 237. Deane, H. Rec. Geol. Surv. Vict., vol. I. pt. 1,
1902, pp. 15, 20.
Lower Pliocene Deep Leads.--McCoy, F. Prod. Pal. Vict., Dec. IV. 1876,
p. 29. Mueller, F. von. Geol. Surv. Vic., New Veg. Foss., 1874
and 1883.
Pleistocene and other Diatom Earths.--Card, G. W. and Dun, W. S., Rec.
Geol. Surv. New South Wales, vol. V. pt. 3, 1897, p. 128.