arkL edit interval

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select id,columnx from arkL_columns where dataset_id like 4

View/Edit arkL Database interval - C2r.1n (Feni)

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The age-window currently being used to search for terms for autocompletion is -47.884 -> 52.14 Ma.

	interval above:	C2r.1r (Matuyama continued)
parent-intervals:C2r.1n (Feni);	this interval:	C2r.1n (Feni)	sub-intervals: C2r.1n (Feni);
	interval below:	C2r.2r (Matuyama continued)

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Interval data

intervalx:	C2r.1n (Feni)has added abv?id: 4079 sort:31
alternative_term:	C2r.1nblock label:
formal term:
interval_type:
parent_interval:
dataset:	magnetochronology (dataset id = 4)
alt dataset:	(dataset id = )
TSC Column:	id:119
stage:
polarity:
colour:
interval_notes:	Feni Normal is a brief normal within the Matuyama Reversed
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:		2.1160	<---	base C2r.1r	8183	0.0000		2.116	00002.1160
Base:		2.1400	<---	base C2r.1n	5912	0.0000		2.14	00002.1400
base notes	C2r.1n was formerly named Reunion; but the type location was discovered to be a brief excursion before the main Normal; therefore Singer (2014) recommended Feni be used after the documented extent and age-control at Feni Drift ODP Site 981 in North Atlantic (Channell et al., 2003). Reunion "upper" excursion suggested from Reunion island volcanics in Indian Ocean, is now best documented at Feni Drift ODP Site 981as spanning ca. 2.140 to 2.116 Ma (25 kyr)				comp notes

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