WoRMS Photogallery
WoRMS Photogallery » Chromista - Foraminifera (foraminifers)
Pseudofusulina urdalensis Rauzer-Chernousova, 1940
Description Rauzer-Chernousova, D. M. (1940). Стратиграфия верхнего карбона и артинского яруса западного склона Урала и материалы к фауне фузулинид - Stratigraphy of the Upper Carboniferous and Artinskian stage of the western slope of the Urals and materials for the fusulinid fauna. Тр. ИГН, АН СССР, Геол., сер. (No 2). 7: 37-101.
page(s): pp. 85 (Russian), 94 (English) pl. 3 figs. 11-12, pl. 4 figs. 1-2, 7 (holotype fig. 1).
Author Le Coze, François
JPG file - 602.88 kB - 1 239 x 1 620 pixels
Extra information
FileName: 162600.jpg
FileDateTime: 1680972595
FileSize: 602876
FileType: 2
MimeType: image/jpeg
SectionsFound: ANY_TAG, IFD0, THUMBNAIL, EXIF
COMPUTED.html: width="1239" height="1620"
COMPUTED.Height: 1620
COMPUTED.Width: 1239
COMPUTED.IsColor: 0
COMPUTED.ByteOrderMotorola: 0
COMPUTED.Thumbnail.FileType: 2
COMPUTED.Thumbnail.MimeType: image/jpeg
COMPUTED.Thumbnail.Height: 256
COMPUTED.Thumbnail.Width: 195
NewSubFile: 2
Orientation: 1
XResolution: 200/1
YResolution: 200/1
ResolutionUnit: 2
Software: GIMP 2.10.28
DateTime: 2023:04:08 17:48:01
Exif_IFD_Pointer: 172
ColorSpace: 1
added on 2023-04-0883 viewsWoRMS taxa Pseudofusulina urdalensis Rauzer-Chernousova, 1940 † accepted as Verneuilites urdalensis (Rauzer-Chernousova, 1940) † accepted as Uraloverneuilites urdalensis (Rauzer-Chernousova, 1940) †checked Le Coze, François 2023-04-08
This work is licensed under a Creative Commons Attribution-Noncommercial-Share Alike 4.0 License
Click
here to return to the thumbnails overview
Disclaimer: WoRMS does not exercise any editorial control over the information displayed here. However, if you come across any misidentifications, spelling mistakes or low quality pictures, your comments would be very much appreciated. You can reach us by emailing
info@marinespecies.org or adding a comment, we will correct the information or remove the image from the website when necessary or in case of doubt.