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View/Edit arkL Database event - FADt Alveolina munieri, Nummulites beneharnensis, Assilina spira spira

NB The age of the event may be set by placement within an interval (pup), placement between 2 events (pub), offset from an event or as a preset.
If data is given for more than one of these the priority is preset over offset over pub over pup.

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The age-window currently being used to search for terms for autocompletion is -4.6005 -> 95.3995 Ma.event above: LADt Alveolina stipes, Nummulites laevigatus
event below: FADt Nummulites gratus, Orbitoclypeus douvillei chudeaui, Orbitoclypeus varians angoumensis, Discocyclina pulcra pulcra, D. discus

base event of: SBZ14 lbfZ;
top event of: SBZ13 lbfZ;

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Event data

term:

Id:6424 sort:

Event Type:

Event Display:

TSC Column:

id:111

Taxon:

dataset:

forams - LBFs (dataset id = 7)

stage:

notes_2004:

notes_2020:

SBZ14 = DASH "Rodrigues-Pinto et al. (2012) demonstrate with magnetostrat that the base of SBZZ14 is quite bit lower, in the lower half of C20r" (Speijer email to J.Ogg, 5Sept’19) = C20r.3 used here.  GTS2012 had at middle of P11 (Larger foram vs Planktonic zone diagram sent by R.Speijer, Feb’11 for GTS2012).   Alveolina munieri, Nummulites beneharnensis, N. boussaci and Assilina spira spira Zone.  Base (dashed) on SEPM chart is 46.33 Ma with no obvious Foram-zone ties, therefore assigned as 95% up in Chron C21n.  From Working Group on Larger Foraminifera website: "SBZZ 14 (Middle Lutetian 1). Defined by the biostratigraphic range of : Alveolina munieri, Nummulites beneharnensis, N. gratus, N. aspermontis, N. hilarionis, N. stephani, N. boussaci and Assilina spira spira. The lower boundary is located in the upper part of Chron 20r, according to magnetostratigraphic data in Bentham and Burbank [1996] and to biostratigraphic data in Sams? et al., [1994], integrated in Poblet et al. [1998], and coincides approximately with boundary PIO-Pll [Hottinger, 1977]. SBZZ14 corresponds to the upper part of NP15 [Kapellos and Schaub, 1973].

compilation_notes:

refs to add:

linked refs:

Bentham & Burbank 1996;Hottinger 1977;Kapellos & Schaub 1973;Poblet et al. 1998;

Placement by pup

up within interval: id: 4226

Placement by pub

	higher event:	id: (Ma)
	lower event:	id: (Ma)

Placement by offset

offset from event: link to event: (id: )

preset_age:

preset_age_notes:

Age

45.3995 Δ=0

Tracecode:

; Q4 event from base+duration defined interval Equation:

Age 2020

Original age 2020 (where age has been corrected by me)

Missing references:Pinto et al. 2012; sorry, these are not in the bibliography yet insert new entry

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Event References

Bentham, P. & Burbank, D. W. (1996). Chronology of Eocene foreland basin evolution along the western oblique margin of the South-Central Pyrenees. In, Friend, P. F. & Dabrio, C. J. (eds) Tertiary Basins of Spain. Cambridge University Press 114-152. gs

Hottinger, L. (1977). Foraminifères operculiniformes. Mémoire de la Muséum National d'Histoire Naturel. C 40: 1-159. gs

Kapellos, V. C. & Schaub, H. (1973). Zur Korrelation von Biozonierungen mit Grossforaminiferen und Nannoplankton im Paläogen der Pyrenäen. Eclogae Geologicae Helvetiae. 63(3): 687-737. gs

Poblet, J., et al. (1998). Quantifying the kinematics of detachment folds using the 3D geometry : application to the Mediano anticline (Pyrenees, Spain). In, Muñoz, A., Gonzalez A. & Perez, A. (eds) II Congr. Gr. Esp. Terciario,. Geological Society of America, Bulletin . 110(1): 111-125. gs

Dataset References

Hardenbol, J., et al. (1998). Mesozoic and Cenozoic Sequence Chronostratigraphic Framework of European Basins. In, de Graciansky, P. -C. , Hardenbol, J. , Jacquin, T. , and Vail, P. R. (ed.) Mesozoic- Cenozoic Sequence Stratigraphy of European Basins. SEPM Special Publication . 60: 3-13 & appendix 763-783. gs

Serra-Kiel, J., et al. (1998). Larger foraminiferal biostratigraphy of the Tethyan Paleocene and Eocene. Bulletin de la Société Géologique de France. 169: 281-299. gs