Property:Method (L)

Property: Method (L) [1]

Imported from: core:method (core | Linked Earth Core)

Answers the question: How is the information obtained from the resource?

Property Semantics

• Property has type Text
• Can have multiple values ? true

Pages using the property "Method (L)"

Showing 25 pages using this property.

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P
PYT953Q8LQ3.gdgt-5 reg-iso +	High Performance Liquid Chromatography - Mass spectrometry (HPLC-MS)  +
PYT9RQ8O0TX.labcode +	asdfasd  +
PYTBH59XDH0.d18og.rub +	Approximately 30 to 40 individual G. ruber (white variety) were picked from samples that had been washed through a 350um sieve with distilled water. The picked specimens were cleaned using the trace metal cleaning technique of Martin and Lea. Each automated batch of sample analyses includes a number of standard carbonates analyzed throughout the automated run. Sample results were adjusted for any internal drift of an automated run.  +
PYTCCBG1QL1.14c uncertainty +	asdfasd  +
PYTE66BFL9X.gdgt +	High Performance Liquid Chromatography - Mass spectrometry (HPLC-MS)  +
PYTES973TGM.sst.Calibration +	Bayesian  +
PYTFSXYJF6G.mg/ca +	300 micrograms of foraminiferal material. 250-355 micrometer size fraction  +
PYTG2PJGTRZ.calib14c +	Fairbanks 0107  +
PYTHO7UXES4.mg/ca-g.rub +	Approximately 30 to 40 individual G.ruber (white variety) were picked from samples that had been washed through a 250um sieve with distilled water. The picked specimens were then cleansed using the trace metal cleaning technique applied to marine carbonate sample of Martin and Lea. The method for determining the Mg/Ca in foraminifera follows the one described by Schrag, which involves a sequential analysis of a standard-sample-standard. Each sample Mg/Ca value is corrected based on the bracketed standard values.  +
PYTJGDIVLNA.gdgt-2 +	High Performance Liquid Chromatography - Mass spectrometry (HPLC-MS)  +
PYTM9G2A4U0.d18o +	Samples comprised of 4 to 14 shells  +
PYTMXOQ15P4.gdgt-1 +	High Performance Liquid Chromatography - Mass spectrometry (HPLC-MS)  +
PYTNE1NN7EA.calendarage.Calibration +	Monte-Carlo simulations  +
PYTOO73ID6Y.depth +	method  +
PYTOYBFQ376.d18o +	asdfasd  +
PYTP9F3FB51.age14c +	AMS  +
PYTPBFEA5KL.calib14c +	Fairbanks0107  +
PYTQ4SI5RNB.14c +	sdfasdf  +
PYTR1G5UAIP.g ruber w mgca +	ICP-OES, Inductively coupled plasma - optical emission spectrometry  +
PYTR5MBV78S.c. wuellerstorfi d18o +	1-10 specimens, 315-400 µm size fraction  +
PYTS9Q3I7QP.age14c +	AMS  +
PYTSU5ZYE58.u auberiana d18o +	1-15 specimens, 315-400 µm size fraction  +
PYTT10XQRQB.mg/ca +	60-75 individuals from the 250-300um fraction. Cleaning: Martin et al. 2002  +
PYTT459A3OE.p obliqu mgca +	ICP-OES, Inductively coupled plasma - optical emission spectrometry  +
PYTTMBHZA02.cal. age.Calibration +	Calendar ages were computed using CALIB4.3 software [Stuiver and Braziunas, 1993], the 1998 marine calibration curve [Stuiver et al., 1998], and a surface reservoir age of 400 y. The 1998 marine calibration curve was smoothed (20 points moving average) for samples younger than 13,600 14C yr BP.  +