arkL edit interval

arkL

select id,columnx from arkL_columns where dataset_id like 7

View/Edit arkL Database interval - SBZ18 lbfZ

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The age-window currently being used to search for terms for autocompletion is -13.4825 -> 88.99 Ma.

	interval above:	SBZ19 lbfZ
parent-intervals:	this interval:	SBZ18 lbfZ	sub-intervals:
	interval below:	SBZ17 lbfZ

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Interval data

intervalx:	SBZ18 lbfZhas added abv?id: 4461 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:		36.5175	<---	FADt Nummulites fabianii	6429	0.2500	C16r	36.5175	00036.5175
Base:		38.9900	<---	FADt Nummulites biedai, Nummulites striatus	6428	0.5000	C18n.1n	38.99	00038.9900
base notes	SBZ18 = DASH "in the upper part of C18n" (Speijer, 5Sept’19 email, based on averaging placement by Luciani et al, 2019, and Costa et al, 2013) - put here as C18n.1n.5. GTS2012 had at 10% up in P15 (Larger foram vs Planktonic zone diagram sent by R.Speijer, Feb’11 for GTS2012). Nummulites biedai and N. cyrenaicus Zone. Base on SEPM chart is just above (0.05 myr) base of Foram Zone P15. From Working Group on Larger Foraminifera website: "SBZZ 18 (late Bartonian). Defined by the biostratigraphic rarige of: Nummulites biedai, N. cyrenaicus, N. vicaryi and N. boulangeri. The lower boundary imprecise, located within Chron 17.3r according to Serra-Kiel and Trave [1995]. SBZZ18 corresponds to the early part of P15 and the late part of NPI7, and to the lower part of NPI8, according to data in Canudo et al.[1988] and Bombita [1984].				comp notes

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