arkL edit interval

arkL

select id,columnx from arkL_columns where dataset_id like 7

View/Edit arkL Database interval - SBZ21 lbfZ

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The age-window currently being used to search for terms for autocompletion is -20.0487 -> 83.9049 Ma.

	interval above:	SBZ22a lbfZ
parent-intervals:	this interval:	SBZ21 lbfZ	sub-intervals:
	interval below:	SBZ20 lbfZ

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Interval data

intervalx:	SBZ21 lbfZhas added abv?id: 4465 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:		29.9513	<---	FADt Nephrolepidina praemaginata, Eulepidina formosoides	6433	0.3000	P20 pfZ	29.9513	00029.9513
Base:		33.9049	<---	FADt Nummulites fichteli, Nummulites vascus	6432	0.0000	Rupelian	33.9049	00033.9049
base notes	SBZ21 = DASH at base of Rupelian (Larger foram vs Planktonic zone diagram sent by R.Speijer, Feb’11 for GTS2012). Nummulites vascus and N. fichteli Zone. Base on SEPM chart corresponds to base of Oligocene. From Working Group on Larger Foraminifera website: "SBZZ 21 (early Rupelian). The base (correspondencing to the Eocene-Oligocene boundary) is defined by the first appearance of Nummulites fichteli and N. vascus, following the extinction of the discocyclinids. The upper limit corresponds to the first appearance of the lepidocyclinids in Europe. SBZZ 21 can be correlated to P18-19 and NP21 pars ? NP 23 pars zones. LBF Assemblages show high diversity: Nummulites bouillei, Operculina complanata, Spiroclypeus cf blanckenhorni ornate, Heterostegina spp., Neorotalia lithothamnica, N. verriculata, Halkyardia minima, H. maxima, Bullalveolina bulloides, Borelis sp., Praerhapydionina delicata, Austrotrillina paucialveolata, Peneroplis armorica.				comp notes

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