arkL edit interval

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select id,columnx from arkL_columns where dataset_id like 11

View/Edit arkL Database interval - D17b DinoSZ

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The age-window currently being used to search for terms for autocompletion is -35.2 -> 65.014 Ma.

	interval above:	D18a DinoSZ
parent-intervals:D17 DinoZ;	this interval:	D17b DinoSZ	sub-intervals:
	interval below:	D17a DinoSZ

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Interval data

intervalx:	D17b DinoSZhas added abv?yesid: 4941 sort:184
alternative_term:	block label:b
formal term:
interval_type:
parent_interval:
dataset:	dflgs Boreal (dataset id = 11)
alt dataset:	(dataset id = )
TSC Column:	id:19
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:		14.8000	<---	FADb Unipontidinium aquaeductum	6793	0.0500	NN5	14.8	00014.8000
Base:		15.0140	<---	FADb Labyrinthodinium truncatum	6792	0.9500	NN4	15.014	00015.0140
base notes	FAD at 95% up in NN4 in King’16 chart -- used here (about 1 myr younger than in GTS04/2012), which wasBase of Langhian (set as base of C5Br in GTS2004, because eventual GSSP might be different). D17 b = "Ltr". Powell (1992): The Labyrinthodinium truncatum Interval Biozone (Ltr Biozone) is defined as the strata between the FAD of Labyrinthodinium truncatum and the FAD of Unipontidinium aquaeductum. It is calibrated to the Calcareous nannoplankton zone NN4 (pars) and NN5 (pars) of Martini (1971); planktonic foraminifer zone N8 (pars) to N10 (pars) of Blow (1969) and Berggren (1972); and to the dinocyst biozonal unit D16/D17 (pars) of Costa & Manum (1988).				comp notes

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