arkL edit interval

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select id,columnx from arkL_columns where dataset_id like 7

View/Edit arkL Database interval - SBZ14 lbfZ

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The age-window currently being used to search for terms for autocompletion is -7.454 -> 95.3995 Ma.

	interval above:	SBZ15 lbfZ
parent-intervals:	this interval:	SBZ14 lbfZ	sub-intervals:
	interval below:	SBZ13 lbfZ

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Interval data

intervalx:	SBZ14 lbfZhas added abv?id: 4457 sort:
alternative_term:	block label:
formal term:
interval_type:
parent_interval:
dataset:	forams - LBFs (dataset id = 7)
alt dataset:	(dataset id = )
TSC Column:	id:109
stage:
colour:
interval_notes:
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:		42.5460	<---	FADt Alveolina prorrecta, Nummulites sordensis, N. crassus	6425	0.2500	P12 pfZ	42.546	00042.5460
Base:		45.3995	<---	FADt Alveolina munieri, Nummulites beneharnensis, Assilina spira spira	6424	0.3000	C20r	45.3995	00045.3995
base notes	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].				comp notes

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