select id,columnx from arkL_columns where dataset_id like 29

View/Edit arkL Database interval - Div-R = M24r.2r

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The age-window currently being used to search for terms for autocompletion is 101.6893 -> 201.9939 Ma.
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interval above:Acan-R = M24r.1n
parent-intervals:mid-Kimm R; this interval:Div-R = M24r.2rsub-intervals:
interval below:Div-N = M24An

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Interval data

intervalx:has added abv?id: 1382  sort:
alternative_term:block label:
formal term:
interval_type:
parent_interval:
dataset: magnetochronology- Jurassic outcrop (dataset id = 29)
alt dataset: (dataset id = )
TSC Column: id:139
stage:
polarity:
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


age2020ageeventevent_idpupin intervalageage2020
Top:151.6893 <--- 1705 0.1200 Aspidoceras acanthicum TAZ151.6893 00151.6893
Base:151.9939 <--- 17060.4000Crussoliceras divisum TAZ151.9939 00151.9937
base
notes		comp notes

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Interval References

Dataset References

Gipe, R. A. (2013). Callovian (upper Middle Jurassic) Magnetostratigraphy: A Composite Polarity Pattern From France, Britain and Germany, and Its Correlation to the Pacific Marine Magnetic Anomaly Model. Purdue University Open Access Theses. . 36: 1-107. gs

Ogg, J. G., et al. (2010a). Oxfordian magnetostratigraphy of Britain and its correlation to Tethyan regions and Pacific marine magnetic anomalies. Earth and Planetary Science Letters. 289: 433-448. gs

Ogg, J. G., et al. (2010b). Late Jurassic time scale: integration of ammonite zones, magnetostratigraphy, astronomical tuning and sequence interpretation for Tethyan, Sub-boreal and Boreal realms. Earth Science Frontiers. 17: 81-82. gs