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Stratigraphy

Sunday, 17 February 2008. Discussions about the Jurassic-Cretaceous boundary (Part II). Discussions about the Jurassic-Cretaceous boundary (Part II). By PhJ. Hoedemaeker. The arrogance of ammonitologists. Please be aware of the fact that Oppel (1856) considered his zones as subdivisions of stages, i.e. Difference between ammonite biochronozones and biozones based on planktonic fossil groups. The biozones with the best correlating possibilities. The base of the S. subalpina. Range ends in S. subalpina.

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Stratigraphy | holostrat.blogspot.com Reviews
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Sunday, 17 February 2008. Discussions about the Jurassic-Cretaceous boundary (Part II). Discussions about the Jurassic-Cretaceous boundary (Part II). By PhJ. Hoedemaeker. The arrogance of ammonitologists. Please be aware of the fact that Oppel (1856) considered his zones as subdivisions of stages, i.e. Difference between ammonite biochronozones and biozones based on planktonic fossil groups. The biozones with the best correlating possibilities. The base of the S. subalpina. Range ends in S. subalpina.
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1 stratigraphy
2 what to do
3 or berriasella privasensis
4 or neocosmoceras sayni
5 or negreliceras paranegreli
6 or ' delphinella
7 boisseti
8 or subthurmannia clareti
9 or mazenoticeras malbosiforme
10 or mazenoticeras curelense
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stratigraphy,what to do,or berriasella privasensis,or neocosmoceras sayni,or negreliceras paranegreli,or ' delphinella,boisseti,or subthurmannia clareti,or mazenoticeras malbosiforme,or mazenoticeras curelense,or mazenoticeras broussei,m pictetiforme,zone
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Stratigraphy | holostrat.blogspot.com Reviews

https://holostrat.blogspot.com

Sunday, 17 February 2008. Discussions about the Jurassic-Cretaceous boundary (Part II). Discussions about the Jurassic-Cretaceous boundary (Part II). By PhJ. Hoedemaeker. The arrogance of ammonitologists. Please be aware of the fact that Oppel (1856) considered his zones as subdivisions of stages, i.e. Difference between ammonite biochronozones and biozones based on planktonic fossil groups. The biozones with the best correlating possibilities. The base of the S. subalpina. Range ends in S. subalpina.

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1

Stratigraphy: 21-Aug-2007

http://holostrat.blogspot.com/2007_08_21_archive.html

Tuesday, 21 August 2007. On the trail of a major trans-Tethyan discontinuity. Sur la piste d'une discontinuité majeure trans-Téthys]. Département des Sciences de la Terre, UFR Sciences et Techniques, Université de Bretagne Occidentale, 6 avenue Le Gorgeu - CS 93837, F-29238 Brest Cedex 3 (France). Manuscript online since May 15, 2007. B (2007).- On the trail of a major trans-Tethyan discontinuity. In. Carnets de Géologie / Notebooks on Geology. Brest, Memoir 2007/02, Abstract 07 ( CG2007 M02/07. À la bas...

2

Stratigraphy: 17-Feb-2008

http://holostrat.blogspot.com/2008_02_17_archive.html

Sunday, 17 February 2008. Discussions about the Jurassic-Cretaceous boundary (Part II). Discussions about the Jurassic-Cretaceous boundary (Part II). By PhJ. Hoedemaeker. The arrogance of ammonitologists. Please be aware of the fact that Oppel (1856) considered his zones as subdivisions of stages, i.e. Difference between ammonite biochronozones and biozones based on planktonic fossil groups. The biozones with the best correlating possibilities. The base of the S. subalpina. Range ends in S. subalpina.

3

Stratigraphy: Discussions about the Jurassic-Cretaceous boundary (Part II)

http://holostrat.blogspot.com/2008/02/discussions-about-jurassic-cretaceous_17.html

Sunday, 17 February 2008. Discussions about the Jurassic-Cretaceous boundary (Part II). Discussions about the Jurassic-Cretaceous boundary (Part II). By PhJ. Hoedemaeker. The arrogance of ammonitologists. Please be aware of the fact that Oppel (1856) considered his zones as subdivisions of stages, i.e. Difference between ammonite biochronozones and biozones based on planktonic fossil groups. The biozones with the best correlating possibilities. The base of the S. subalpina. Range ends in S. subalpina.

4

Stratigraphy: 15-Feb-2008

http://holostrat.blogspot.com/2008_02_15_archive.html

Friday, 15 February 2008. Discussions about the Jurassic-Cretaceous boundary (Part I). Discussions about the Jurassic-Cretaceous boundary (Part I). By PhJ. Hoedemaeker. Let me try to make a few things clear to you by elucidating my opinion on the matter. I am at one with you about the stratigraphic position of the Jurassic-Cretaceous boundary at the base of the Neocomian (= boundary between the ammonite zones of ' Berriasella. The GSSP should be located in open marine sediments deposited in not too shall...

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Stratigraphy

Sunday, 17 February 2008. Discussions about the Jurassic-Cretaceous boundary (Part II). Discussions about the Jurassic-Cretaceous boundary (Part II). By PhJ. Hoedemaeker. The arrogance of ammonitologists. Please be aware of the fact that Oppel (1856) considered his zones as subdivisions of stages, i.e. Difference between ammonite biochronozones and biozones based on planktonic fossil groups. The biozones with the best correlating possibilities. The base of the S. subalpina. Range ends in S. subalpina.

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