Monday, December 15, 2008
Thursday, December 11, 2008
Wednesday, December 10, 2008
Wednesday, November 26, 2008
Manuscript resubmitted
AMMONOID BEDS IN THE LOWER TRIASSIC THAYNES FORMATION OF WESTERN UTAH, USA
Daniel A. Stephen, Kevin G. Bylund, Paul J. Bybee, and Wesley J. Ream
Dan sent in the revised manuscript and figures last night. Reviewers should be getting a copy shortly. I think it looks and reads great. Between me and the reviewers, Dan had a handful, trying to keep everyone happy and still writing what he wanted, I thank him for his patience and understanding.Daniel A. Stephen, Kevin G. Bylund, Paul J. Bybee, and Wesley J. Ream
Thursday, November 6, 2008
Lanceolitidae
Lanceolites ?bicarinatus on the left and the one I found in April (this post) on the right. They seem to have all the same elements but the L. ?bicarinatus seem to be a little more ammonitic. Perhaps the ammonitic elements were worn off of the right specimen?
Wednesday, November 5, 2008
Saturday, November 1, 2008
Monday, October 27, 2008
Sunday, October 19, 2008
Sunday, September 7, 2008
DH-1 Bed 10
Monday, August 11, 2008
Xenoceltites
An update for this old post
Xenoceltites-Boreoceras-Wyomingites
I found an old photo of the specimen on display at the museum. Where did those constrictions come from? I am leaning more toward Xenoceltites now, as the sculpture, especially on the early whorls, is more like it than of Wyomingites. I could have swore all the whorls were smooth.Tuesday, July 15, 2008
Measuring Early Triassic Sections
Monday, June 23, 2008
Baby Ammonoids, Baby Gastropods
From the Cretaceous Mancos Shale, Scaphites whitfieldi Zone, the coiled ammonoids could be Scaphites whitfieldi or Prionocyclus novamexicanus.
Sunday, May 18, 2008
Monday, April 28, 2008
DH-2 Photos
A large Arctocerid mold, the body chamber was filled with mud so it is preserved, the phragmocone was probably crushed after it left it's imprint in the soft bottom.
Jim collecting DH-2 bed 1
The DH-2 anticline looking south.
Permian red beds in the foreground, the basal Thaynes limestone on the south side of the north DH-2 fault well exposed beyond.
Jim collecting DH-2 bed 1
The DH-2 anticline looking south.
Permian red beds in the foreground, the basal Thaynes limestone on the south side of the north DH-2 fault well exposed beyond.
Sunday, April 20, 2008
Something new (at least to me)
I found this while doing a little mapping this weekend. I think it is some form of Ussuriid. From the Early Triassic
See this post for update
Friday, April 4, 2008
Presentation on line
If you go to the abstract, you can now download a pdf file of the presentation I gave at the GSA meeting in Las Vegas last month.
Abstract for Presentation 12-9
4.8 Mb presentation handout download.
Abstract for Presentation 12-9
4.8 Mb presentation handout download.
Tuesday, February 12, 2008
GSA Las Vegas
Well, Wes found out he cant give the talk at the GSA meeting in Las Vegas. The honor falls to Me!
Paper No. 12-9 11:00AM-11:20AM, March 20, 2008
A first time for everything I guess.
Paper No. 12-9 11:00AM-11:20AM, March 20, 2008
A first time for everything I guess.
Tuesday, January 29, 2008
Clypeoceras may be Guodunites
Wednesday, January 9, 2008
Churkites vs Arctoceras
Churkites noblei Jenks 2007
The ornamentation is exactly like Arctoceras tuberculatum, the only difference is the shape of the venter. These have an acute venter, becoming almost oxyconic in large shells and Arctoceras has a well rounded venter (almost semi-circular). This could be sexual dimorphism with the round ventered forms being female and the acute ventered forms male.
Of course there are two different sizes found in the Confusion Range, the small 100-180mm and the large 300mm, perhaps these are dimorphs of Churkites and Arctoceras isnt congeneric.
Jenks, J. F., 2007, Smithian (Early Triassic) Ammonoid Biostratigraphy at Crittenden Springs, Elko County, Nevada and a New Ammonoid From the Meekoceras Gracilitatis Zone, in, Lucas S. G. and Spielmann, J. A. eds., Triassic of the American West, New Mexico Museum of Natural History and Science Bulletin 40
The ornamentation is exactly like Arctoceras tuberculatum, the only difference is the shape of the venter. These have an acute venter, becoming almost oxyconic in large shells and Arctoceras has a well rounded venter (almost semi-circular). This could be sexual dimorphism with the round ventered forms being female and the acute ventered forms male.
Of course there are two different sizes found in the Confusion Range, the small 100-180mm and the large 300mm, perhaps these are dimorphs of Churkites and Arctoceras isnt congeneric.
Jenks, J. F., 2007, Smithian (Early Triassic) Ammonoid Biostratigraphy at Crittenden Springs, Elko County, Nevada and a New Ammonoid From the Meekoceras Gracilitatis Zone, in, Lucas S. G. and Spielmann, J. A. eds., Triassic of the American West, New Mexico Museum of Natural History and Science Bulletin 40
Wednesday, January 2, 2008
Opportunistic Bloom?
I am really starting to wonder if the Anasibirites Beds could preserve an opportunistic bloom. If the Prionitids (and not all the other ammonoids) began or found a way to prey on the micro gastropods of the time they may have had a great advantage and a large amount of food. Whether the beds in the Confusion Range preserve a mass mortality event or just the preservation of an unusually high amount of dead shells would need an answer.
An extinction at the base of the anasibirites beds, and a small climate gradient left the anasibirites beds to be very cosmopolitan. Perhaps they were just the most common ammonoid in the latest smithian so any unfavorable water or climatic condition would have killed only the anasibirites fauna.
Still so much to learn and figure out in all this.
Galfetti, T., H. Bucher, A. Brayard, P. A. Hochuli, H. Weissert, K. Guodun, V. Atudorei, J. Guex, 2007, Late Early Triassic climate change: Insights from carbonate carbon isotopes, sedimentary evolution and ammonoid paleobiogeography,
Palaeogeography, Palaeoclimatology, Palaeoecology 243, 394–411
Kidwell, S.M. 1991. The stratigraphy of shell concentrations. In: P.A. Allison and D.E.G. Briggs (eds.), Taphonomy: Releasing the Data Locked in the Fossil Record, 211–290. Plenum Press, New York.
DIANA L. BOYER, DAVID J. BOTTJER and MARY L. DROSER, 2004, Ecological Signature of Lower Triassic Shell Beds of the Western United States, PALAIOS, v. 19; no. 4; p. 372-380
An extinction at the base of the anasibirites beds, and a small climate gradient left the anasibirites beds to be very cosmopolitan. Perhaps they were just the most common ammonoid in the latest smithian so any unfavorable water or climatic condition would have killed only the anasibirites fauna.
Still so much to learn and figure out in all this.
Galfetti, T., H. Bucher, A. Brayard, P. A. Hochuli, H. Weissert, K. Guodun, V. Atudorei, J. Guex, 2007, Late Early Triassic climate change: Insights from carbonate carbon isotopes, sedimentary evolution and ammonoid paleobiogeography,
Palaeogeography, Palaeoclimatology, Palaeoecology 243, 394–411
Kidwell, S.M. 1991. The stratigraphy of shell concentrations. In: P.A. Allison and D.E.G. Briggs (eds.), Taphonomy: Releasing the Data Locked in the Fossil Record, 211–290. Plenum Press, New York.
DIANA L. BOYER, DAVID J. BOTTJER and MARY L. DROSER, 2004, Ecological Signature of Lower Triassic Shell Beds of the Western United States, PALAIOS, v. 19; no. 4; p. 372-380
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