File:The Quarterly journal of the Geological Society of London (13206139854).jpg

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252
PROCEEDINGS OF THE GEOLOGICAL SOCIETY. .Mar. 10,
the neck-segment in all Trilobites ; the latter segment in our genus
is armed with a spine.
rr^
Fig. 1. Trinucleus ornatus.
2. Do. magnified fringe.
3. Hypothetical development of the fringe.
4. Fringe of T.fimbriatus,
The body-rings are six, very flat, and capable only of bending or
doubling, not of rolling up as in Calymene — a character of considerable
importance, inasmuch as it has relation to the connecting membranes
and articular surfaces of the crust : species capable of rolling into a
ball requiring large articular surfaces on the segments to enable them
to move freely on each other ; and a fulcrum, as centre of motion, on
the side pieces of each segment, is generally placed about one-third of
the distance from the axis : — in Trinucleus the rudimentary fulcrum
is quite at the extremity of the segment, and apparently useless.
The tail, generally smooth, has a deflected border, but not, as far
as observed, a striated internal fold, so common in higher forms of
Trilobites.
The peculiar perforate border is the most interesting part of these
animals, and I propose to examine it critically.
The puncta are almost always arranged in radiating rows, three,
four, or more holes in each row, and these being at equal distances
they form concentric lines. In T. granulatus^ two of these rows are
separated by a furrow from the rest ; in T. seticornis, three are distinct
from the remaining two or three, by the front rows being sunk in a
deep concentric furrow. Other modifications take place : in T. jimhria-
tus, the two front rows are turned downwards ; lastly, in T. ornatus —
for by that name we must call T. Caractaci — the dots occur most
frequently in quincunx order — i. e. the radiant rows appear zigzag,
and not direct (fig. 2) : this appearance is due to the great obliquity
of the rays (2, a a). I wish to call attention to this, because I con-
sider it enables us to understand the nature of the enigmatical puncta.
If we suppose a head furnished with a produced membranous margin

(fig. 5) instead of a perforate one, we shall get at the explanation
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Source https://www.flickr.com/photos/biodivlibrary/13206139854
Author Geological Society of London
Full title
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The Quarterly journal of the Geological Society of London.
Page ID
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36932991
Item ID
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113687 (Find related Wikimedia Commons images)
Title ID
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51125
Page numbers
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Page 252
Names
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NameFound:Calymene NameConfirmed:Calymene EOLID:4322334 NameBankID:2875639 NameFound:Trilobites granulatus NameConfirmed:Trilobites NameBankID:4377238 NameFound:Trilobites ornatus NameFound:Trilobites seticornis NameConfirmed:Trilobites NameBankID:4377238 NameFound:Trinucleus NameConfirmed:Trinucleus EOLID:4324924 NameBankID:2875667 NameFound:Trinucleus fimbriatus NameConfirmed:Trinucleus fimbriatus NameFound:Trinucleus ornatus NameConfirmed:Trinucleus ornatus
BHL Page URL
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https://www.biodiversitylibrary.org/page/36932991
Page type
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Text
Flickr sets
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  • The Quarterly journal of the Geological Society of London. v. 3 (1847).
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Flickr posted date
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17 March 2014
Credit
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This file comes from the Biodiversity Heritage Library.

This tag does not indicate the copyright status of the attached work. A normal copyright tag is still required. See Commons:Licensing.


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26 August 2015

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current12:19, 26 August 2015Thumbnail for version as of 12:19, 26 August 20151,199 × 2,069 (645 KB) (talk | contribs)== {{int:filedesc}} == {{BHL | title = The Quarterly journal of the Geological Society of London. | source = http://www.flickr.com/photos/biodivlibrary/13206139854 | description = 252 <br> PROCEEDINGS OF THE GEOLOGICAL SOCIETY. .Mar. 10, <br> the neck-...

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