File:The Quarterly journal of the Geological Society of London (12960307883).jpg

Original file(1,750 × 3,200 pixels, file size: 947 KB, MIME type: image/jpeg)

Captions

Captions

Add a one-line explanation of what this file represents

Summary

edit
Description

AFFIXITIES OF THE GEXES PE0T0SP0:NGIA. 363
after a study of the -whole of the material which has come under my
observation, I feel no difficulty in definitely assigning to Protosponrjia
its place amongst the other sponges. Moreover, as Dr. Hicks's figure
of his specimen is almost purely diagrammatic, I have ventured to
insert here a fresh drawing of part of it, kindly made for me by my
friend Mr. T. H. Thomas, of Cardiff. The great interest which must
necessaril.' attach to the best-preserved specimen of the oldest known
sponge renders excuse for this second representation of it needless.
3. Desceiptiox.
The specimens on which Salter's description was based were
crushed and flattened forms in which the skeleton appears as raised
lines or narrow thread-like ridges arranged in a lattice- like reticula-
tion on the bedding-planes of the slate which serves as a matrix.
Dr. Hicks's specimen (fig. 1), on the other hand, presents us with the
Fig. 1. — Part of tlie specimen 0/ Protospongia feuestrata, in the
IVoodwardian Mtrscmii. (.S'atural size.)
spicules of the sponge in their original form, unaltered, or but slightly
altered by pressure, and standing out in free relief from the weathered
matrix, which has in several places been artistically cleared away
from beneath them.
In this state of perfect preservation the spicules are clearly not
fused together into a continuous network ; they are separated and
free, and only form a network by the interlacing of their extremities.
Their form also is somewhat different from that of the s^ncules of
crushed specimens.
Form of tJie Sjncules. — Each sj^icule is quadriradiate, with its
centre raised some slight but variable distance above the plane in
which its rays terminate. Its general form may be most easily
described by imagining it as modelled upon a low four- sided pyra-

mid, the centre of the spicule lying upon the apex, and its four rays
Date
Source https://www.flickr.com/photos/biodivlibrary/12960307883
Author Geological Society of London
Full title
InfoField
The Quarterly journal of the Geological Society of London.
Page ID
InfoField
36090726
Item ID
InfoField
111264 (Find related Wikimedia Commons images)
Title ID
InfoField
51125
Page numbers
InfoField
Page 363
Names
InfoField
NameFound:Protospongia NameConfirmed:Protospongia NameBankID:1883070
BHL Page URL
InfoField
https://www.biodiversitylibrary.org/page/36090726
Page type
InfoField
Text
Flickr sets
InfoField
  • The Quarterly journal of the Geological Society of London. v. 36 (1880).
Flickr tags
InfoField
Flickr posted date
InfoField
6 March 2014
Credit
InfoField
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.


العربية  বাংলা  Deutsch  English  español  français  italiano  日本語  македонски  Nederlands  polski  +/−



Licensing

edit
w:en:Creative Commons
attribution
This file is licensed under the Creative Commons Attribution 2.0 Generic license.
You are free:
  • to share – to copy, distribute and transmit the work
  • to remix – to adapt the work
Under the following conditions:
  • attribution – You must give appropriate credit, provide a link to the license, and indicate if changes were made. You may do so in any reasonable manner, but not in any way that suggests the licensor endorses you or your use.
This image was originally posted to Flickr by BioDivLibrary at https://flickr.com/photos/61021753@N02/12960307883. It was reviewed on 26 August 2015 by FlickreviewR and was confirmed to be licensed under the terms of the cc-by-2.0.

26 August 2015

This image is in the public domain because it is a mere mechanical scan or photocopy of a public domain original, or – from the available evidence – is so similar to such a scan or photocopy that no copyright protection can be expected to arise. The original itself is in the public domain for the following reason:
Public domain

This work is in the public domain in its country of origin and other countries and areas where the copyright term is the author's life plus 70 years or fewer.


This work is in the public domain in the United States because it was published (or registered with the U.S. Copyright Office) before January 1, 1929.


This tag is designed for use where there may be a need to assert that any enhancements (eg brightness, contrast, colour-matching, sharpening) are in themselves insufficiently creative to generate a new copyright. It can be used where it is unknown whether any enhancements have been made, as well as when the enhancements are clear but insufficient. For known raw unenhanced scans you can use an appropriate {{PD-old}} tag instead. For usage, see Commons:When to use the PD-scan tag.


Note: This tag applies to scans and photocopies only. For photographs of public domain originals taken from afar, {{PD-Art}} may be applicable. See Commons:When to use the PD-Art tag.

File history

Click on a date/time to view the file as it appeared at that time.

Date/TimeThumbnailDimensionsUserComment
current15:43, 26 August 2015Thumbnail for version as of 15:43, 26 August 20151,750 × 3,200 (947 KB) (talk | contribs)== {{int:filedesc}} == {{BHL | title = The Quarterly journal of the Geological Society of London. | source = http://www.flickr.com/photos/biodivlibrary/12960307883 | description = AFFIXITIES OF THE GEXES PE0T0SP0:NGIA. 363 <br> after a study of the -wh...

There are no pages that use this file.