arkL edit interval

arkL

select id,columnx from arkL_columns where dataset_id like 84

View/Edit arkL Database interval - Circulaforma omicron AuRadZ

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The age-window currently being used to search for terms for autocompletion is 288.8628 -> 390.8296 Ma.

	interval above:	Curvalbaillella uforma LLRadZ
parent-intervals:	this interval:	Circulaforma omicron AuRadZ	sub-intervals:
	interval below:	Albaillella cartalla - Albaillella thomasi AuRadZ

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Interval data

intervalx:	Circulaforma omicron AuRadZhas added abv?yesid: 11908 sort:475
alternative_term:	C. omicronblock label:
formal term:
interval_type:
parent_interval:
dataset:	radiolaria Permo-Triassic (dataset id = 84)
alt dataset:	(dataset id = )
TSC Column:	id:273
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:		338.8628	<---	top Circulaforma omicron AuRadZ	12316	0.4800	Visean	338.8628	00338.9112
Base:		340.8296	<---	base Circulaforma omicron AuRadZ	12315	0.3600	Visean	340.8296	00340.8659
base notes	1/3rd up in Visean; base near top of T. varians				comp notes	ADJUSTED: the original figure of 33.3% up in the Visean was based on old placement of the Serpukovian/Visean boundary. So I have recalculated it for the new boundary -> 36%

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Interval References

Dataset References

Hardenbol, J., et al. (1998). Mesozoic and Cenozoic Sequence Chronostratigraphic Framework of European Basins. In, de Graciansky, P. -C. , Hardenbol, J. , Jacquin, T. , and Vail, P. R. (ed.) Mesozoic- Cenozoic Sequence Stratigraphy of European Basins. SEPM Special Publication . 60: 3-13 & appendix 763-783. gs

Kozur, H. W. (2003). Integrated ammonoid, conodont and radiolarian zonation of the Triassic. Hallesches Jahrbuch für Geowissenschaften. B25: 49-79. gs