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96 II. DE ARACHNIDIS<br />
distinguished, the same mysterious pectines and the same terminal<br />
sting. These arc not characteristics of a primitive animal, so that one is<br />
forced to imagine a hypothetical ancestor, a truly primitiye scorpion<br />
from which the Silurian forms were descended. This imaginary protoscorpion<br />
can more easily be imagined to be the ancestor of the Eurypterida<br />
than can any known extinct scorpion.<br />
Nevertheless, the hypothesis is not one that calls for immediate recognition<br />
. .\iigration from the land to the water is not to bF readilv<br />
accFpted, nor does any Eurypterid a scorpion-like anccstr):.<br />
In the absencF of any fossil scorpion earlier than tlw Silurian the speculation<br />
cannot usefully be pushed further.<br />
There is a frustrating lack of evidrncc from the ensuing Dcvonian<br />
epoch, with very few arachnid fossils. This period was the first to have<br />
left t'vidence of great changes in the environment. The seas continued<br />
to be overcrowded; Pterygotus was prominent, and fishes were so<br />
numerous that the time is often known as the Age of Fishes. On land,<br />
invertebrate life dcnJoped: there were Ephemeroptera 'Nith a wing span<br />
of 13 cm, and an intelligr·nt observer, ft1llowing the course of foretelling<br />
the future by recollection of the past, v.'ould han~ prophesied a ma~s<br />
invasion of the land.<br />
It came in the Carboniferous, with nothing less than an arachnid<br />
explosion. A warm, moist atmosphere favoured a territorial existence;<br />
plant life was luxuriant insects and myriapods were accornpanied by<br />
uearly all the orders of ,\raehnida that we recognize today. For many<br />
marine animals life in thr: sea was becoming less and less tolera hle, and<br />
for the Enrypterida at any rate it was about to pass the acceptable limit.<br />
They were<br />
l(1r extinction, and did. in fact, become extinct in<br />
the succeeding Pcrmian epoch. The temptation to go ashore in search<br />
of better conditions must ha,·e been great; and, as Goetbc l1as<br />
"Animals are attempting the impossible, and often<br />
it". In the end their achie,·ements resulted in the creation of some 16<br />
orders, the geological distribution of which is displayed in the following,<br />
familiar table.<br />
Such a fragmentary record does not give as much help as be<br />
C'xpccted. It shows that most of the orders \V ere in existence during the<br />
Carboniferous era, and that they largely e\'olnd along different liues,<br />
as a result cf which five of them disappeared and 12 surviHd. The<br />
most significant fact that emergt's from this vie\\· of the palaeontology of<br />
<strong>Arachnida</strong> is the conviction that they provide a good example of that<br />
general parallelism in evolutionary progress which is such ;1 conspicuous<br />
feature of evolution as a whole.<br />
The idea of the evolution of early scorpions from contemporary<br />
Schizomida<br />
Araneae<br />
Ku>tarachnae<br />
Anthracomarti<br />
Haptopoda<br />
:\rchitarbi<br />
Opilioncs<br />
Cyphophtbalmi<br />
Acari<br />
Ricinulei<br />
Pseucloscorpiones<br />
Solifugae<br />
.~<br />
,_<br />
~<br />
Cl ""<br />
X<br />
X<br />
ll. PHYLOGENY: EVOLUTION<br />
PRl:VIARY<br />
Y:t<br />
:;1<br />
c:: :-<br />
.~ c::<br />
(, s<br />
~<br />
.~<br />
><br />
"" § 0 ,_ .I:; 0<br />
,:; ,_<br />
i)<br />
8 ;..<br />
;:; c.<br />
""<br />
..._, :;. "' v c.<br />
SECO:-IDARY<br />
(.; \)<br />
:!l<br />
·~ ·~<br />
,_<br />
~<br />
;:;<br />
~<br />
j ;::<br />
.:3<br />
"' j<br />
:..., -, Cl<br />
X X X X X<br />
X X X X X X X X X<br />
X X X X<br />
X<br />
X<br />
X<br />
X X X X X<br />
X<br />
X X<br />
X X<br />
X<br />
X<br />
X<br />
X<br />
X<br />
X<br />
X<br />
TlcRTIARY<br />
X X X X I X<br />
X<br />
X<br />
X<br />
X<br />
X<br />
X<br />
X<br />
X X X<br />
X<br />
X<br />
X<br />
X X X<br />
X<br />
X<br />
X<br />
X<br />
Eurypterida seems to ha\·e been accepted so \vhole-heartedlv that<br />
further im·estigation has been ; yet the taxonomic isolation of<br />
the order Scorpiones should have indicated the need for some intnpretation.<br />
The scorpions cannot be regarded as the ancestors of the<br />
other orders, and this suggests that during the late Devonian or early<br />
Carboni!Crous many other occupants of the iucreasingly unpleasar{t<br />
sea.mu.st b~,-e foll?we~ly1e c.:;:amplc oftheir predecessors and repeated<br />
thetr lnstonc landmg. 1 here 1s no reason to suppose that all these were<br />
of the same species, or e\·en of the same family; more probablv thev were<br />
of different types, and the terrestrial <strong>Arachnida</strong> that e\·olnd. fron~ them<br />
were different in consequence. \Ve call them different orders.<br />
Fossil scorpions seem to arrange thcmsehes in nine super-families,<br />
only one of which can claim relationship with the living scorpions of the<br />
p:esen~. One may say, in broad outline, that ancestral scorpions of<br />
mne kmds made the experiment and that only one succeeded. Let the<br />
same be applied to the later invasion, and it may be said that 16<br />
explorers set foot ashore and ll of them founded p~rmanent orders.<br />
Survival rate had risen from ll to 69%.<br />
One wonders why.<br />
97