arkL edit interval

select id,columnx from arkL_columns where dataset_id like 1

The age-window currently being used to search for terms for autocompletion is -12.29 -> 91.03 Ma.

intervalx:	Bartonianhas added abv?id: 4019 sort:449
alternative_term:	block label:
formal term:
interval_type:
parent_interval:
dataset:	chronostratigraphy (dataset id = 1)
alt dataset:	(dataset id = )
TSC Column:	id:89
stage:
colour:	253/192/145
interval_notes:
compilation_notes:
refs to add:	Berggren et al. (1995)
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:		37.7100	<---	base Priabonian	5897	0.0000		37.71	00037.7100
Base:		41.0300	<---	base Bartonian	5898	0.0000	C18r	41.03	00041.0300
base notes	DASHED -- Base of Bartonian (working version) assigned as base of Chron C18r. The base of Bartonian is typically correlated to a level within Nanno Zone NP16, and closely associated with LAD of Reticulofenestra reticulata (Leg 320-321 cite same chron-age scaling as chron-age scaling as Berggren et al. (1995); = ca. C19r.7. Berggren et al. (1995) equate to the TOP of polarity chron C19n (base of C18r), implying an age estimate of 41.25 Ma.				comp notes

Ambiguous references: select using checkbox

Berggren et al. 1995
	Berggren, W. A., Kent, D. V., Swisher III, C. C. & Aubry, M. -P. (1995b). A revised Cenozoic geochronology and chronostratigraphy. In, Berggren, W. A. , Kent, D. V. , Aubry, M. -P. , and Hardenbol, J. (ed.) Geochronology, Time Scales and Global Stratigraphic Correlations: A Unified Temporal Framework for a Historical Geology. SEPM Special Publication . 54: 129-212. 169
	Berggren, W. A., et al. (1995). Late Neogene chronology: new perspectives in high resolution stratigraphy. Geological Society of America, Bulletin. 107: 1272-1287. 5053

if you were a logged in editor there would be an input button here