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Invertebrates: Trace Fossil X: Informal classification: "fucoids" | Print |  E-mail
Written by Keith Minor   

"Fucoids"

Remarks

  • Picture taken by:    Keith Minor
  • Formation:             Washita Group, Duck Creek Formation
  • Location:               Tarrant County, Texas
  • These intriguing features in the Texas Cretaceous have been referred by collectors to everything from plant related structures to "stag horn" coral.

  • They look like tree roots, but they're probably some sort of burrow, possibly crustacean in origin.

  • Perkins refers to these as "fucoids" and has a brief discussion on the possible origin of these trace fossils  (1960, Fort Worth and Duck Creek Formations, ref below).

  • Fucoides is actually a catchall genus and includes a wide range of branching trace fossils of varying origin and dimensions, including the Chondrites spp. shown on the site, and is therefore a nonsystematic term.

  • We've seen some incredible examples but keep forgetting break out the camera.  We'll get more images soon.  A grasshopper was kind enough to serve as scale for the image below.  Thanks so much!

General Info

Synonyms (older names and misidentifications in the literature)

  • burrows

Stratigraphic Occurrence

  • Found throughout the Cretaceous

Age

  • "Fucoids" are found throughout the Cretaceous

Geographic Occurrence (by no means an all-inclusive list)

  • Worldwide

Remarks

         For identification and descriptions, see:

  • Hass, W. H.; Häntzschel, W.; Fisher, D. W.; Howell, B. F.; Rhodes, F. H. T.; Müller, K. J.; Moore, R. C.  1962.  "Part W.  Miscellanea (Conodonts, Conoidal Shells of Uncertain Affinities, Worms, Trace Fossils, and Problematica)".  In:  Moore, R. C., ed.  Treatise on Invertebrate Paleontology.  New York and Lawrence:  Geological Society of America and University of Kansas Press, W193.
  • Perkins, B. F.  1960.  Biostratigraphic Studies in the Comanche (Cretaceous) Series of Northern Mexico and Texas.  Geological Society of America, Memoir 83, 26; plate 9, fig's 2 and 3 and plate 10, fig's 1 and 2.
Last Updated ( Sunday, 13 January 2008 )
 
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