arkL edit interval

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select id,columnx from arkL_columns where dataset_id like 7

View/Edit arkL Database interval - SBZ17 lbfZ

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The age-window currently being used to search for terms for autocompletion is -11.01 -> 91.03 Ma.

	interval above:	SBZ18 lbfZ
parent-intervals:	this interval:	SBZ17 lbfZ	sub-intervals:
	interval below:	SBZ16 lbfZ

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Interval data

intervalx:	SBZ17 lbfZhas added abv?id: 4460 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	; Q2top from event age; Q1base from event age; Q3a duration from base & top

	age2020	age		event	event_id	pup	in interval	age	age2020
Top:		38.9900	<---	FADt Nummulites biedai, Nummulites striatus	6428	0.5000	C18n.1n	38.99	00038.9900
Base:		41.0300	<---	FADt Alvoelina elongata, Nummulites perforatus, Nummulites brongniarti, Discocyclina pulcra baconica	6427	0.0000	Bartonian	41.03	00041.0300
base notes	SBZ17 = DASH at base of Bartonian (Larger foram vs Planktonic zone diagram sent by R.Speijer, Feb’11 for GTS2012). Alvoelina elongata, A. fragilis, A. fusiformis, Discocyclina pulcra baconica, Nummulites perforatus, N. brogniarti and N. biarritzensis Zone. Base on SEPM chart is base of Bartonian (used here). From Working Group on Larger Foraminifera website: "SBZZ 17 (early Bartonian). Defined by the biostratigraphic range of: Alveolina elongata,A. fragilis, A. fusiformis, Nummulites brongniarti, N.perforatus, N. hottingeri, N. puschi, N. biarritzensis, N. lyelli and Discocyclina pulcra baconica. The lower boundary is located close to the base of Chron 19n according to Burbank et al. [1992]. SBZZ17 starts in the upper part of P12 and extends over P13 and P14 according to Canudo et al. [1988] and Serra-Kiel and Trave [1995]. It rides the NP16/NP17 boundary [Bombita, 1984].				comp notes

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