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Property:Notes (L)

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Property: Notes (L) [1]

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

Answers the question: What additional information would you give about the Variable or DataTable ?


Property Semantics

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

Pages using the property "Notes (L)"

Showing 25 pages using this property.

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PYTO6QLOKWD.benthic d18o +adjusted for equiibrium offsets  +
PYTOH600XJ7.d18oc.mund.Uncertainty1 +Precision determined from replicate measurements of foraminiferal sample  +
PYTOIUTG47N.d18ow +with respect to SMOW, G. ruber seawater d18O uncorrected for ice volume  +
PYTOM01JCNE.d18ocorr +corrected for ice volume  +
PYTOMLKRPB1.age calyrbp +The ensemble and summary tables were adjusted to take into consideration NaNs in the SST and d18Osw data  +
PYTOO73ID6Y.depth +notes  +
PYTOQEOF9ML.core sample +LMG98-2 = Laurence M Gould cruise 1998-02, PD92 = Polar Duke cruise 1992-02, ODP = Ocean Drilling Program leg 178 Site 1098 (A,B,C) (Joides Resolution)  +
PYTOYBFQ376.d18o +asdfa  +
PYTPBECVZ1M.sample code +LSCE (Gif-sur-Yvette)  +
PYTPZU7L7S9.d18oruberpink +pink variety  +
PYTQ4SI5RNB.14c +asdfasa  +
PYTQ6KJJA79.benthic d18o +corrected for equilibrium offset  +
PYTQMNS13E7.g. ruber w mg/ca +white variety  +
PYTQTCDLSJS.sst1 +d18O sw = -0.08 per mil (CDW), after Craig (1965)  +
PYTR0KAVVXG.corrected radiocarbon age +R(t) = 1230  +
PYTR0UXSYN0.sst2 +d18O sw = -0.60 per mil (surface water), after Craig (1965)  +
PYTRD2CBJAC.calibrated age intercept.Calibration +Calibrated ages are calculated using the program CALIB v4.2 with a marine calibration dataset and a 30-year moving average to account for the likely age span of foraminifera from a 1-cm thick sample  +
PYTRJ3OFZP2.ghostMeasured.Calibration +MUE1998: Muller et al. 1998 sediment core top based calibration, n=370, R2=0.958)  +
PYTSSIOQ15X.sst - mg/ca +size fraction: 250-350 microns  +
PYTT10XQRQB.mg/ca +corrected for Al-silicated contamination as described in Lea et al. 2005 G3  +
PYTTA8QZBTE.acc rate dust +Depth is a result from correlations between holes A, B and C (see Depth, composite). The noncarbonate fraction (100% minus %CaCO3) is considered to be purely eaolian, because the concentrations of biogenic opal (<2%), organic carbon (<0.5%), and volcanic glass are negligible and fluvial sediment supply and turbidites cannot reach this position (Tiedemann et al., 1989)  +
PYTTY1FRFXV.tex86l +~45-200 m water depth  +
PYTTYB8B7I7.d18og +sensu stricto  +
PYTU51EGVWZ.u. peregrina d18o +250-400 µm  +
PYTUL2LO1T7.d18o +sensu stricto  +