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 100 pages using this property.

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L
LPDc08ab49e.temperature +	alkenone  +
LPDc2846a24.R660 670 +	Gretag-Spectrolino  +
LPDcda1c277.temperature +	Mg/Ca  +
LPDd95394f2.temperature +	vLA2005  +
LPDdc74a376.temperature +	alkenone-based temperature reconstruction  +
LPDe51d17e8.temperature +	Mg/Ca  +
LPDe6c52b99.temperature +	Mg/Ca  +
LPDe759ea6b.N +	Macro Vario elemental analyzer  +
LPDefb3d2b0.temperature +	Mg/Ca  +
LPDf7751317.C +	Macro Vario elemental analyzer  +
LPDf7bace53.temperature +	Mg/Ca  +
M
MD982181.Khider.2014.ChronData1.Model1 +	Monte-Carlo simulations  +
MD982181.Khider.2014.ChronData1.Model2 +	Monte-Carlo simulations  +
MD982181.Khider.2014.ChronData1.Model3 +	Monte-Carlo simulations  +
MD982181.Khider.2014.PaleoData1.Model1 +	Bayesian  +
MD982181.Khider.2014.PaleoData1.Model2 +	Bayesian  +
O
O2kLR 007.temperature +	SIMMAX  +
O2kLR 009.temperature +	SIMMAX  +
O2kLR 017.temperature +	Mg/Ca  +
O2kLR 019.temperature +	Mg/Ca  +
O2kLR 030.temperature +	U37K index  +
O2kLR 032.temperature +	U37K index  +
O2kLR 045.temperature +	Calibration: PRA1988  +
O2kLR 046.temperature +	Calibration: PRA1988  +
O2kLR 047.temperature +	Calibration: PRA1988  +
O2kLR 066.temperature +	Mg/Ca  +
O2kLR 068.temperature +	Mg/Ca  +
O2kLR 074.temperature +	alkenone  +
O2kLR 076.temperature +	alkenone  +
O2kLR 082.temperature +	Planktonic foraminiferal assemblage census counts  +
O2kLR 084.temperature +	Planktonic foraminiferal assemblage census counts  +
O2kLR 101.temperature +	Mg/Ca  +
O2kLR 105.temperature +	U37K index  +
O2kLR 107.temperature +	U37K index  +
O2kLR 112.temperature +	alkenone  +
O2kLR 113.temperature +	alkenone  +
O2kLR 114.temperature +	alkenones  +
O2kLR 116.temperature +	alkenones  +
O2kLR 118.temperature +	Mg/Ca  +
O2kLR 120.temperature +	Mg/Ca  +
O2kLR 131.temperature +	Mg/Ca  +
O2kLR 135.temperature +	Mg/Ca  +
O2kLR 137.temperature +	Mg/Ca  +
O2kLR 146.temperature +	alkenone  +
O2kLR 147.temperature +	alkenone  +
O2kLR 148.temperature +	Mg/Ca  +
O2kLR 149.temperature +	Mg/Ca  +
O2kLR 150.temperature +	Sr/Ca  +
O2kLR 152.temperature +	Sr/Ca  +
O2kLR 165.temperature +	TEX86  +
O2kLR 166.temperature +	TEX86  +
O2kLR 175.temperature +	alkenones  +
O2kLR 177.temperature +	alkenones  +
O2kLR 183.temperature +	alkenone  +
O2kLR 184.temperature +	alkenone  +
O2kLR 187.temperature +	alkenone  +
O2kLR 189.temperature +	alkenone  +
O2kLR 195.temperature +	Alkenone  +
O2kLR 197.temperature +	Alkenone  +
P
PYT0FGGTQ8Q.d18on +	isotope ratio mass spectrometry  +
PYT0RJBEOLO.c. wuellerstorfi d13c +	1-10 specimens, 315-400 µm size fraction  +
PYT1ZK5FLCQ.u. peregrina d18o +	1-15 specimens, 315-400 µm size fraction  +
PYT263GUKAT.age14c +	For radiocarbon dating the surface-dwelling planktic foraminifera species Globigerinoides ruber in a strict sense and Globigerinoides sacculifer (without the sac-like final chamber) were handpicked under a binocular microscope from the >150 µm fraction. The abundance of these species within the cores was generally low, and occasionally, both species were combined to obtain a sufficient amount of datable material.  +
PYT3BFZK5EK.d18og +	isotope ratio mass spectrometry  +
PYT3L6BW4OB.d18og +	25-30 individual shells were pooled, sonicated for 5s in methanol, roasted at 375 degC for 30 min in vacuo and then reacted individually in 105% H3PO4 at 90degC  +
PYT4GF6APIN.d18ou +	60-100 shells were gently crushed open under glass slides. Samples were purified of organic matter with hydrogen peroxide, ultasonicated in acetone, dried at 50C  +
PYT56FXLTUB.g. bulloides d18o +	30-40 specimens picked from the 250-315μm size fraction. Measurements were conducted with a Thermo Scientific MAT253 IRMS coupled to a Kiel IV sample gas preparation device.  +
PYT5Z4BM1HD.g.inflata d13c +	about 20 specimens, 250-315 µm size fraction  +
PYT6T5QYQCK.gdgt-3 +	High Performance Liquid Chromatography - Mass spectrometry (HPLC-MS)  +
PYT7DGGKKES.sst +	ufuf  +
PYT7JD8Q23P.g. inflata d18o +	about 20 specimens, 250-315 µm size fraction  +
PYT7Z7JMLKT.mg +	asdfas  +
PYT80Q7P5ZU.age14c +	accelerated mass spectrometry  +
PYT8KNOASAM.mg/ca +	Cleaning include a reductive step. Accuracy of the data was checked by analyzing the carbonate reference standard ECRM 752-1  +
PYT8QRXXH0K.age14cuncertainty +	AMS  +
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  +