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104 U. DE ARACHNIDIS<br />
and Euarachnida disappeared. The Pycnogonida were excluded, and<br />
Nomomeristica were divided into four sub-classes, Limulava for the<br />
extinct Copura, :Merostomata for Limulus and Eurypterida, Pectinifera<br />
for the scorpions, and Epectinata for eight other orders. In the Epectinata<br />
were six new· divisions known as super-orders; one of these, Caulogastra,<br />
included Pedipalpi, Araneae and Palpigradi: the others contained<br />
but a single order each. The features of this classification were<br />
the expulsion cf the Pycnogonida and the expression of the belief that<br />
the three orders of the Caulogastra are more closely related to each<br />
other than to any other Epectinata; and also that no two other orders of<br />
Epectinata arc so closely related that they can share a super-order.<br />
Both these systems placed the scorpions in a section or sub-class<br />
Pectinifera, which distinguished them from and contrasted them with<br />
all other living <strong>Arachnida</strong>. This opinion expresses the traditional view<br />
that the scorpions are more primitive arachnids than any others, and<br />
this, as has been seen, is scarcely true.<br />
Neither Lankester nor Pocock had given much attention to the<br />
tion of the extinct orders other than Eurypterida, and this subject was<br />
for the time adequately considered by Stormer (1944). He named<br />
the phylum Arachnomorpha and divided it into two sub-phyla, Trilobitomorpha<br />
and Chelicerata. The latter contained two classes, :\1erostomata<br />
for Eurypterida and Xiphosura, and <strong>Arachnida</strong> for 13 orders,<br />
covering the 17 orders described in Part Ill of this book. No suggestion<br />
was made for the further relations of these orders, the names of which<br />
were simply recorded in a linear series.<br />
This aspect of the classification was the outstanding feature of<br />
Petrunkevitch's of palaeozoic <strong>Arachnida</strong> in 1949. As a result of<br />
detailed examination of a very large number of fossil <strong>Arachnida</strong>, he<br />
threw new light on the probable course of evolution and expressed his<br />
conclusions by placing the orders in four sub-classes which he named<br />
Latigastra, Caulogastra, Stethostomata and Soluta. At almost the<br />
same time the encyclopaedic "Traite de Zoologie" edited by Grasse,<br />
printed a straightforward list of 14 orders.<br />
Petrunkevitch used his system, with minor changes in nomenclature,<br />
in his contribution to the "Treatise on Invertebrate Palaeontology",<br />
edited by R. C. Moore, and published in 1955. It was followed almost<br />
at once by a new classification, put forward by \V. B. Dubinin in 1957.<br />
This author was evidently in an iconoclastic mood and he suggested a<br />
drastic revision. The terrestrial Chelicerata were divided into four<br />
classes, containing 21 orders, clearly the outcome of an entirely fresh<br />
approach. More recently another<br />
was adopted by the<br />
present author in 1971. The three efforts may be compared in tabular<br />
form.<br />
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