File:The Quarterly journal of the Geological Society of London (12511870393).jpg

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10
PROCEEDINGS OF THE GEOLOGICAL SOCIETY. .DeC. 1,
tion is perceptible. The diameter of this canity varies from one-half
to one-third of that of the entire body, so that the wall which en-
closes it is from one-fourth to one-third of that diameter in thickness.
It is wholly composed of straight regular fibres, of even thickness,
radiating from the internal cavity to the external surface (see fig. 1).
The fibres have flat sides, and being closely packed together, they
are necessarily, on the average, hexagonal. On rubbing down a por-
tion of the external surface, the ends of these hexagonal fibres are
exposed to view. They do not appear to be tubular.
In one specimen the extremities of these fibres are exhibited on
the external surface by numerous small dark-coloured dots on a pale
ground. Their outlines are here no longer hexagonal, but round or
oval, often confluent, with a tendency to form parallel lines, yet sub-
ject to some irregularity (see figs. 2, 3)*. A further notice, by Dr.
Hooker, of these curious fossils, and of a fragment of carbonized
wood found with them, is appended to this paper.
Figs. 1, 2, & 3. Showing the structure of the globular vegetable
bodies found in the Ludlow Bone Bed.
O
la.
Fig. 3.
Fig. 1 a. Natural size.
Fig, 1 b. Transverse section ; magnified.
Fig. 2. Dotted markings on the external surface ;
magnified.
Fig. 3. The same, more highly magnified.
In crossing the axis of the Woolhope elevation from Gamage Ford
to Much Marcle, I again detected the Bone-bed, in the side of the
road, near the base of the Old Red Sandstone. It here presents nu-
merous rolled coprolitic fragments mixed with the supposed scales of
Thelodus parvidens, imbedded in brown micaceous sand. I also
noticed casts of an Atrypa in it.
The beds of yellow sandstone quarried at Gorstley Common, be-
tween Woolhope and May Hill, belong to the same part of the series
as those which contain the Ludlow Bone-bed, though no remains of

  • The object figured in Sil. Syst. pi. 4. figs. 65, 66, and described as the " pa-

latal bone of Sclerodus," has every appearance of being one of these seed-like
bodies split in half. Somewhat similar, though imperfect, specimens were found

by Mr, Scobie and myself in the Cornstone of Llanfihangel, near Abergavenny.
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Source https://www.flickr.com/photos/biodivlibrary/12511870393
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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34983101
Item ID
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108767 (Find related Wikimedia Commons images)
Title ID
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51125
Page numbers
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Page 10
Names
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NameFound:Atrypa NameConfirmed:Atrypa NameBankID:4083726 NameFound:Sclerodus NameConfirmed:Sclerodus EOLID:13245196 NameBankID:4338947 NameFound:Thelodus parvidens NameConfirmed:Thelodus parvidens EOLID:13325393 NameBankID:5596951
BHL Page URL
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https://www.biodiversitylibrary.org/page/34983101
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Text
Flickr sets
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  • The Quarterly journal of the Geological Society of London. v. 9 (1853)
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Flickr posted date
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14 February 2014
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This file comes from the Biodiversity Heritage Library.

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27 August 2015

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current23:33, 26 August 2015Thumbnail for version as of 23:33, 26 August 20153,200 × 1,869 (1.12 MB) (talk | contribs)== {{int:filedesc}} == {{BHL | title = The Quarterly journal of the Geological Society of London. | source = http://www.flickr.com/photos/biodivlibrary/12511870393 | description = 10 <br> PROCEEDINGS OF THE GEOLOGICAL SOCIETY. .DeC. 1, <br> tion is per...

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