The Cambridge natural history, Vol. 01 (of 10)Hickson, Sydney J. (Sydney John)
Science
The Cambridge natural history, Vol. 01 (of 10)
Hickson, Sydney J. (Sydney John)
Animals
Haeckel, in his Monograph of the Radiolaria of the _Challenger_ enumerated
739 genera, comprising 4318 species; and Dreyer has added 6 new genera,
comprising 39 species, besides 7 belonging to known genera. Possibly, as we
shall see, many of the species may be mere states of growth, for it is
impossible to study the life-histories of this group; on the other hand, it
is pretty certain that new forms are likely to be discovered and described.
The Radiolaria are found living at all depths in the sea, by the
superficial or deep tow-net; and some appear to live near the bottom, where
the durable forms of the whole range also settle and accumulate. They thus
form what is known as Radiolarian ooze, which is distinguished from other
shallower deposits chiefly through the disappearance by solution of all
calcareous skeletons, as they slowly fell through the waters whereon they
originally floated at the same time with the siliceous remains of the
Radiolaria. The greatest wealth of forms is found in tropical seas, though
in some places in cold regions large numbers of individuals of a limited
range of species have been found.
Radiolaria of the groups with a pure siliceous skeleton can alone be
fossilised, even the impure siliceous skeleton of the Phaeodaria readily
dissolving in the depths at which they live: they have been generally
described by Ehrenberg's name _Polycystineae_. Tripolis (_Kieselguhr_) of
Tertiary ages have been found in many parts of the globe, consisting
largely or mainly of Radiolaria, and representing a Radiolarian ooze. That
of the Miocene of Barbados contains at least 400 species; that of Gruppe at
least 130. In Secondary and Palaeozoic rocks such oozes pass into
Radiolarian quartzites (some as recent as the Jurassic). They occur also in
fossilised excrement (coprolites), and in flint or chert concretions, as
far down as the lowest fossiliferous rocks, {88}the Cambrian. The older
forms are simple Sphaerellaria and Nassellaria. From a synopsis of the
history of the order in Haeckel's _Monograph_ (pp. clxxxvi.-clxxxviii.) we
learn that while a large number of skeletal forms had been described by
Ehrenberg, Huxley in 1851 published the first account of the living animal.
Since then our knowledge has been extended by the labours of Haeckel,
Cienkowsky, R. Hertwig, Karl Brandt, and A. Borgert.
5. PROTEOMYXA
_Sarcodina without a clear ectoplasm, whose active forms are amoeboid or
flagellate, or pass from the latter form to the former; multiplying
chiefly, if not exclusively, by brood-formation in a cyst. No complete
cell-pairing (syngamy) known, though the cytoplasms may unite into
plasmodia; pseudopodia of the amoeboid forms usually radiate or filose, but
without axial filaments. Saprophytic or parasitic in living animals or
plants._
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