arkL edit interval

arkL

select id,columnx from arkL_columns where dataset_id like 10

View/Edit arkL Database interval - A. mayaroensis pfZ

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The age-window currently being used to search for terms for autocompletion is 17.6386 -> 119.271 Ma.

	interval above:	P. hariaensis pfZ
parent-intervals:	this interval:	A. mayaroensis pfZ	sub-intervals:
	interval below:	R. fructicosa pfZ

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Interval data

intervalx:	A. mayaroensis pfZhas added abv?yesid: 3494 sort:
alternative_term:	A. mayaroensis zoneblock label:
formal term:	Abathomphalus mayaroensis pfZ
interval_type:
parent_interval:
dataset:	forams - planktic (dataset id = 10)
alt dataset:	(dataset id = )
TSC Column:	id:104
stage:
colour:
interval_notes:	A. mayaroensis zone begins at base of Chron C31n (summarized by Huber et al’08; and at Gubbio -- Coccioni et all, 2015). GTS04 had used a slightly higher Chron C31n.40 (ODP 171B table, in turn from Erba et al, 1995). This is the Tethyan FAD. The FAD of A. mayaroensis seems to be older in North Sea (Paul Sikora, EGI database, 2005). SEPM’98 correlation was approx. top of J. nebrascansis ammonite zone.
compilation_notes:
refs to add:
linked refs:
preset_duration:
preset_duration_notes:
tracecode	; Q2top from event age; Q1base from event age; Q3a duration from base & top

	age2020	age		event	event_id	pup	in interval	age	age2020
Top:		67.6386	<---	FAD Pseudoguembelina hariaensis	4349	0.3000	C30n	67.6386	00067.6400
Base:		69.2710	<---	FAD Abathomphalus mayaroensis	4350	0.0000	C31n	69.271	00069.2700
base notes	Abathomphalus mayaroensis:<br>Datum calibration/notes = A. mayaroensis zone begins at base of Chron C31n (summarized by Huber et al’08; and at Gubbio -- Coccioni et al, 2015). GTS04 had used a slightly higher Chron C31n.40 (ODP 171B table, in turn from Erba et al, 1995). This is the Tethyan FAD. The FAD of A. mayaroensis seems to be older in North Sea (Paul Sikora, EGI database, 2005). SEPM’98 correlation was approx. top of J. nebrascansis ammonite zone..				comp notes

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Interval References

Dataset References