arkL edit interval

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select id,columnx from arkL_columns where dataset_id like 2

View/Edit arkL Database interval - Discotropites plinii TAsZ

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The age-window currently being used to search for terms for autocompletion is 178.5285 -> 279.757 Ma.

	interval above:	Gonionotites italicus TAsZ
parent-intervals:Anatropites spinosus TAZ;	this interval:	Discotropites plinii TAsZ	sub-intervals:
	interval below:	Tropites subbullatus TAsZ

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Interval data

intervalx:	Discotropites plinii TAsZhas added abv?yesid: 6957 sort:110
alternative_term:	block label:
formal term:
interval_type:
parent_interval:
dataset:	ammonites Tethyan (dataset id = 2)
alt dataset:	(dataset id = )
TSC Column:	id:330
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:		228.5285	<---	base Gonionotites italicus TAsZ	9176	0.5000	Anatropites spinosus TAZ	228.5285	00228.5285
Base:		229.7570	<---	base Anatropites spinosus TAZ	9177	0.5000	MK5n.1r	229.757	00229.7570
base notes	DASHED -- Hounslow-Muttoni (2010) show base (Tuv3) as being in middle of reversed-polarity zone, although uncertain where their ammonoid control comes from. BUT, assuming their correlation to "PM2r" of Pizzo Mondello is actually the base of Spinosus ammonoid zone also; then this would now be middle of Newark E5 or Gerrmanic MK5n.1r (used here). GTS2012 had as Middle of uncertain E3r (60% used here; based on a proposed correlation suite) - Hounslow-Muttoni put overying "UT11n" entirely into A. spinosus Zone (plus upper half of UT10r), which is correlated in GTS2012 to E4n => this correlation had been adjusted accordingly. Kozur’s "standard" uses N.Amer. K. macrolobatus and T. welleri for middle-upper Tuvalian. Also called only by genus name as ’Anatropites’ Zone.				comp notes

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