arkL edit interval

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select id,columnx from arkL_columns where dataset_id like 13

View/Edit arkL Database interval - NC8

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The age-window currently being used to search for terms for autocompletion is 59.9365 -> 163.784 Ma.

	interval above:	NC9
parent-intervals:	this interval:	NC8	sub-intervals:
	interval below:	NC7

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Interval data

intervalx:	NC8has added abv?id: 3735 sort:70
alternative_term:	block label:
formal term:
interval_type:
parent_interval:
dataset:	nannos Tethyan (dataset id = 13)
alt dataset:	(dataset id = )
TSC Column:	id:36
stage:
colour:
interval_notes:	DOTTED -- has taxonomy problems in the transitional trend subcircular to circular. In Piobbico Core (Bottini and Erba, 2015, place it below base-Albian) at E32.8 cycles below base Cenomanian (Wendy Zhang et al., re-analysis of Huang’s cycles, used here). Base of this subcircular P. columnata using Kennedy et al. (2014; who used this "A*" designation) is just above top of Jacob black shale (0.1myr used here). (Primary control on Aptian-Albian interval!) SEPM’98 has assigned as FAD as 2/10 up in L. tardefurcata Z., L. schrammeni s.z.; but coincides at Vohrum, Germany (used to set it). Herrle et al (2004): "The FO of the calcareous nannofossil Prediscosphaera columnata (marking the base of NC8A) in the Upper Aptian seems to be diachronous with respect to the carbon isotope stratigraphy, occurring earlier (V1.4 Ma) in the uppermost part of Ap13 at the Mazagan Plateau record than in the Vocontian Basin (upper part of Ap15).
compilation_notes:
refs to add:
linked refs:
preset_duration:
preset_duration_notes:
tracecode	; Q1base from event age; Q2top from event age; Q3a duration from base & top

	age2020	age		event	event_id	pup	in interval	age	age2020
Top:		109.9365	<---	FADt Axopodorhabdus albianus	4714	0.0000		109.9365	00109.9365
Base:		113.7840	<---	FADt Prediscosphaera columnata (subcircular)	4717	0.0000		113.784	00113.7840
base notes	DOTTED -- has taxonomy problems in the transitional trend subcircular to circular. In Piobbico Core (Bottini and Erba, 2015, place it below base-Albian) at E32.8 cycles below base Cenomanian (Wendy Zhang et al., re-analysis of Huang’s cycles, used here). Base of this subcircular P. columnata using Kennedy et al. (2014; who used this "A*" designation) is just above top of Jacob black shale (0.1myr used here). (Primary control on Aptian-Albian interval!) SEPM’98 has assigned as FAD as 2/10 up in L. tardefurcata Z., L. schrammeni s.z.; but coincides at Vohrum, Germany (used to set it). Herrle et al (2004): "The FO of the calcareous nannofossil Prediscosphaera columnata (marking the base of NC8A) in the Upper Aptian seems to be diachronous with respect to the carbon isotope stratigraphy, occurring earlier (V1.4 Ma) in the uppermost part of Ap13 at the Mazagan Plateau record than in the Vocontian Basin (upper part of Ap15).				comp notes

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