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Property:Method (L)

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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 212 pages using this property.

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A
Africa 001.d18O +Linear regression  +
Ant 005.d18O +mass spectrometer  +
Ant 006.d18O +mass spectrometer  +
Ant 007.d18O +mass spectrometer  +
Ant 008.d18O +mass spectrometer  +
Ant 009.d18O +mass spectrometer  +
Ant 010.d18O +mass spectrometer  +
Ant 011.d18O +mass spectrometer  +
Ant 012.d18O +mass spectrometer  +
Ant 013.dD +mass spectrometer  +
Ant 014.dD +Los Gatos (LWIA-24d) Liquid Water Isotope Analyzer at 5 cm resolution, corresponding to ~14 samples per year.  +
Ant 017.d18O +mass spectrometer  +
Ant 023.d18O +mass spectrometer  +
Ant 024.d18O +mass spectrometer  +
Ant 025.d18O +mass spectrometer  +
Ant 026.dD +mass spectrometer  +
Ant 027.dD +mass spectrometer  +
Ant 028.dD +mass spectrometer and laser analyser  +
Ant 029.temperature +Regression with the air temperature measured at Vostok station in 1958-2010  +
Ant 030.d18O +mass spectrometer  +
Ant 031.d18O +mass spectrometer  +
Ant 031dD.dD +mass spectrometer  +
Ant 033.dD +mass spectrometer and  +
Ant 035.d18O +mass spectometry  +
Ant 037.d18O +mass spectrometry  +
Ant 050.d18O +laser spectroscopy  +
Arc 065.d18O +missing annual d18O in the lower part of the core interpolated using piecewise cubic interpolation  +
Arc 066.d18O1 +calibration using scaling against mean Dec-Feb Longyerbyen temperature for 1912-1996 AD  +
Arc 072.BSi +Mortlock and Froelich (1989)  +
Arc 073.temperature +non-linear regression  +
Arc 074.uncertainty temperature +bootstrapping RMSEP  +
Arc 088.thickness +N/A  +
Arc 089.d18O +analytical technique: mass spectrometry  +
Arc 090.Na +analytical technique: ion chromatography  +
Arc 091.temperature +N/A  +
Arc 093.trsgi +linear regression  +
Arc 094.temperature +N/A  +
Arc 096.d18O +linear regression  +
Arc 150.MXD +positive  +
Asia 230.temperature +borehole temperature inversion (see Demezhko, D. Y., Shchapov, V. A., Glob. Planet. Change, 29, 219–230, 2001)  +
Asia 233.trsgi +see Jacoby G., Solomina O., Frank D., Eremenko N., D’Arrigo R. Kunashir (Kuriles) Oak 400-year reconstruction of temperature and relation to the Pacific Decadal Oscillation. Palaeogeography, Palaeoclimatology, Palaeoecology 209 (2004) 303–311  +
Asia 235.temperature +integration of borehole and tree-ring GST reconstructions (Demezhko, Solomina, 2009)  +
Asia 335.temperature +WAPLS; MLRC; IKFM; ANN  +
Aus 010.trsgi +signal free  +
Aus 015.trsgi +signal free  +
Aus 020.trsgi +signal free  +
Aus 041.temperature +RCS and temperature recon using linear regression  +
Aus 062.trsgi +signal free  +
Aus 067.trsgi +signal free  +
Aus 071.trsgi +RCS  +
E
Eur 024.temperature +modern analog  +
Eur 025.uncertainty temperature +modern analog  +
Eur 026.temperature +application of transfer function  +
Eur 027.JulianDay +based on documentary information  +
K
Khider.DeglacialTiming.Model1 +Bayesian  +
L
LPD016ef221.temperature +Mg/Ca  +
LPD09e5a770.temperature +Mg/Ca  +
LPD0b6c7700.BSi +wet chemical extration, alkalkine leaching, inductively coupled plasma optical emission spectrometry  +
LPD0e0867fe.temperature +alkenone  +
LPD0e900372.C N +Macro Vario elemental analyzer  +
LPD10e9f8f7.temperature +alkenone  +
LPD13a78f9b.temperature +Mg/Ca  +
LPD16c5b9d8.temperature +Alkenone  +
LPD1a0245b7.temperature +Mg/Ca  +
LPD2a3997a7.temperature +TEX86  +
LPD30c5b95c.temperature +Mg/Ca  +
LPD335d863f.RABD660 670 +Gretag-Spectrolino  +
LPD34478ed4.temperature +Mg/Ca  +
LPD44e382ee.temperature +Mg/Ca  +
LPD4dd77d54.temperature +Converted using MUE1998  +
LPD53e179ad.temperature +BAYSPAR Bayesian calibration  +
LPD572f7cc3.temperature +Mg/Ca  +
LPD57d40973.temperature +Mg/Ca  +
LPD5c89a1b5.temperature +Alkenone  +
LPD6315f935.temperature +Alkenone  +
LPD6dbf8788.temperature +alkenone  +
LPD708fb697.temperature +Mg/Ca  +
LPD716b88d0.temperature +Mg/Ca  +
LPD77e777b0.R570 630 +Gretag-Spectrolino  +
LPD7abab671.temperature +inverse model  +
LPD7c7e19c5.temperature +Mg/Ca  +
LPD7cf4e05b.temperature +TEX86  +
LPD806644b2.temperature +Mg/Ca  +
LPD81e53153.temperature +BAYSPAR Bayesian calibration  +
LPD84ab67b9.temperature +alkenone  +
LPD9b023bc9.temperature +Mg/Ca  +
LPD9cc3baf6.temperature +Mg/Ca  +
LPDa03ec713.temperature +Mg/Ca  +
LPDa2107e77.temperature +Mg/Ca  +
LPDa77273bb.temperature +Converted using MUE1998  +
LPDa7a4074f.uncertainty temperature +inverse model  +
LPDa97364db.temperature +Mg/Ca  +
LPDasan2012.temperature +alkenone  +
LPDb17a5e9e.temperature +Mg/Ca  +
LPDb44bf261.temperature +Mg/Ca  +
LPDb7ba9166.temperature +Alkenone  +
LPDb9285123.temperature +inverse model  +
LPDbd07f717.temperature +Mg/Ca  +
LPDbff7f105.R650 700 +Gretag-Spectrolino  +
LPDc07746c5.temperature +Mg/Ca  +
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  +
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.  +
PYTTYB8B7I7.d18og +Mass spectrometer Finnigan MAT 252  +
PYTUNY5WJNW.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.  +
PYTVFZ0WOFC.d18osw +fasdf  +
PYTVUTGRE9G.mg/ca +20 specimens per sample cleaned following the Barker et al. procedure  +
PYTW0D8MOY6.d18og.rub +250-255 micrometer size fraction. About 40 shells picked for stable isotope and trace element analysis  +
PYTWDV3B356.depth +sdfasd  +
PYTXEIS6K4U.d18on +Mass spectrometer Finnigan MAT 252  +
PYTXYDHFXNN.calibrated age +The 14C ages were calibrated using the software Calib 7.0.2 and the Marine 13 calibration curve and a reservoir age of 150 years ±60 years  +
PYTXZLB1X8P.age +fsadf  +
PYTYQ33IFH4.age +20mg of foraminiferal material picked from the >150micrometer size fraction  +
U
Unknown.59f3a4320f03e +Unknown.59f3a4320f2c5  +
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