arkL edit interval

arkL

select id,columnx from arkL_columns where dataset_id like 13

View/Edit arkL Database interval - NC3a

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The age-window currently being used to search for terms for autocompletion is 85.358 -> 187.4073 Ma.

	interval above:	NC3b
parent-intervals:NC3a;	this interval:	NC3a	sub-intervals: NC3a;
	interval below:	NC2b

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Interval data

intervalx:	NC3ahas added abv?id: 3752 sort:101
alternative_term:	block label:a
formal term:
interval_type:
parent_interval:
dataset:	nannos Tethyan (dataset id = 13)
alt dataset:	(dataset id = )
TSC Column:	id:39
stage:
colour:
interval_notes:	Just above Berr/Val boundary according to south France (Charbonnier et al. 2013; Martinez et al., 2015) -- set as 35% up in Chron M14r here. This is slightly higher than the "21% up in cycle V1" (Martinez et al., 2015) using Charbonnier et al (2013) adjustment of their basal Valanginian cycle. SEPM’98 had assigned FAD as 7/10 up in T. otopeta Zone, which would shift to Berriasian, due to working-group change in boundary.
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:		135.3580	<---	LADt Rucinolithus wisei	4701	0.2600	V6 Martinez_cycle	135.358	00135.3566
Base:		137.4073	<---	FADt Calcicalathina oblongata	4659	0.3500	M14r	137.4073	00137.4075
base notes	Just above Berr/Val boundary according to south France (Charbonnier et al. 2013; Martinez et al., 2015) -- set as 35% up in Chron M14r here. This is slightly higher than the "21% up in cycle V1" (Martinez et al., 2015) using Charbonnier et al (2013) adjustment of their basal Valanginian cycle. SEPM’98 had assigned FAD as 7/10 up in T. otopeta Zone, which would shift to Berriasian, due to working-group change in boundary.				comp notes

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Interval References

Dataset References