File:The Quarterly journal of the Geological Society of London (13369147924).jpg

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1872..
S0LLAS — UPPER-GEEENSAND VENTRICULITES.
(iv.) On the fibre between two elements at the ordinary distance
from each, other, the centre of an apparently superfluous element
unexpectedly appears. Of its four radii seen in the section, two of
course are parts of the fibre on which the centre occurs ; the other
two normally have no radii with which they can combine, and as a
consequence they bend away in opposite directions at about 45° from
their fellows, and open into the octahedral fibres of adjacent hexra-
diate elements (fig. 5). Besides these, other variations occur (fig. 6).
Fie. 5.
Fig. 6.
Spicules. — Though siliceous spicules are well preserved in some
flints and coprolites, yet a careful examination has failed to reveal
their presence in silicified ventriculites (T. Smith) or in phospha-
tized ones. For all this the Ventriculites may have been spiculate
sponges ; in a section of a Bronchiolites, and in one of V. tessellatus,
I have found simple acerate spicules, with which were associated one
or two hexaradiate ones ; possibly, however, these may have been
washed in from the sea-bed during; fossilization.
Identification of Species.
i. Ventriculites tessellatus (Toulmin Smith) ; Scyphia tessellata
(Seeley); Spongia texturata (Quenstedt).
Quenstedt' s figure * of this species is an excellent one ; it is
taken from a specimen from the Weisse Jura, and accurately repro-
duces the Cambridge form. Quenstedt refers Scyphia texturata
and S. parallela (Goldfuss) to the same species t, as well as Alcyon-
ites texturatus (Schlotheim t and Parkinson §). This latter identi-
fication appears to me very questionable, Parkinson's figure more
nearly representing Ventriculites quincuncialis than V. tessellatus.
In the Eoyal College of Surgeons is a specimen from the Jurassic
of Wiirttemberg, labelled by Prof. Morris, Ventriculites texata
(Miinster), which is in every respect a fac-simile of our Cambridge
species ; and I believe S. tessellata (Seeley), S. texturata (Quenstedt),
and V. texata (Miinster) are identical with V. tessellatus (T. Smith).
The following is a description of our Greensand Ventriculites tessel-

  • Der Jura, Quenstedt, tab. 83. fig. 7, p. 683.

t Petref. Germ., Goldfuss, tab. 2. fig. 9, tab. 3. fig. 3.
J Petref., Schlotheim, p. 373.
§ Parkinson, 'Organic remains,' tab. 10. fig. 12.

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Source https://www.flickr.com/photos/biodivlibrary/13369147924
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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39050971
Item ID
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120601 (Find related Wikimedia Commons images)
Title ID
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51125
Page numbers
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Page 67
Names
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NameFound:Alcyon ites texturatus NameConfirmed:Alcyon EOLID:19001 NameBankID:4062208 NameFound:Scyphia parallela NameFound:Scyphia tessellata NameConfirmed:Scleria tessellata Benth., nom. illeg. EOLID:251739 NameFound:Scyphia texturata NameConfirmed:Scyphia texturata Goldfuss NameFound:Spongia texturata NameConfirmed:Spongia terebrata Phill. NameFound:Ventriculites NameConfirmed:Ventriculites NameBankID:4390439 NameFound:Ventriculites quincuncialis NameFound:Ventriculites tessellatus NameConfirmed:Ventriculites tesselatus Sm. NameFound:Ventriculites texata NameConfirmed:Ventriculites Mantell 1822 NameBankID:4390440
BHL Page URL
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https://www.biodiversitylibrary.org/page/39050971
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Text
Flickr sets
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  • The Quarterly journal of the Geological Society of London. v. 29 (1873).
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Flickr posted date
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24 March 2014
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This file comes from the Biodiversity Heritage Library.

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current10:32, 26 August 2015Thumbnail for version as of 10:32, 26 August 20151,853 × 3,186 (1.14 MB) (talk | contribs)== {{int:filedesc}} == {{BHL | title = The Quarterly journal of the Geological Society of London. | source = http://www.flickr.com/photos/biodivlibrary/13369147924 | description = 1872.. <br> S0LLAS — UPPER-GEEENSAND VENTRICULITES. <br> (iv.) On the...

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