The Principles of Stratigraphical GeologyMarr, J. E. (John Edward)
Science
The Principles of Stratigraphical Geology
Marr, J. E. (John Edward)
Geology, Stratigraphic
_The Permian flora and fauna._ The Permian flora presents some
difficulties. The flora of the Zechstein consists largely of ferns and
conifers, but that of the Rothliegende of Germany has been compared
with that of the Carboniferous, and if a true Permian flora of the
northern hemisphere has many forms of Carboniferous affinities, the
presence of the Glossopteris flora in Permo-Carboniferous rocks of
more southerly regions seems to imply its origin there and _slow_
migration northwards. It must be noted, however, that the Rothliegende
has been divided by some geologists into an upper and lower division,
of which the lower is actually referred to the Carboniferous system.
All that can be now said is, that our knowledge of the floras of
Permo-Carboniferous and Permian times is still incomplete, and that
the difficulties will no doubt be cleared up as the result of further
work.
The invertebrate fauna of the north-west European Permian deposits is
chiefly noticeable on account of the paucity of species, though
individuals are often abundant. The shells are also sometimes stunted
and occasionally distorted. These characters bear out the supposition
that the aqueous deposits were laid down in inland seas of Caspian
character and not in the open ocean. Polyzoa, brachiopods, and
lamellibranchs predominate, but other groups are found. The
vertebrates consist of forms of fish, amphibia and reptiles, and the
Permian rocks are the earliest strata in which the remains of true
Reptilia are known to occur with certainty. The Reptiles belong to the
orders Anomodontia (Theromora) and Rhynchocephalia, of which the
former is exclusively Permian and Triassic, while the latter is
abundant in the strata of those periods, but is represented at the
present day by the genus _Sphenodon_ of New Zealand. The Amphibia
belong to the order Labyrinthodontia which ranges from Carboniferous
to Lower Jurassic, but the members of the order are most abundant in
Permian and Triassic strata, and these periods may be spoken of as the
Periods of Labyrinthodonts.
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