Property:Notes (L)

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 ?

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Pages using the property "Notes (L)"

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P
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  +
PYTUTE5IVBM.d18og +	G. ruber (pink)  +
PYTV0ZXFVEH.ghostMeasured.Calibration +	ANA2003: Anand multi species sediment trap calibration.  +
PYTV3PN1YF8.benthic d18o +	corrected for offsets  +
PYTVFZ0WOFC.d18osw +	fsadf  +
PYTVH8NB95K.ghostMeasured.Calibration +	PRA&WAK1987: UK37 E. huxleyi culture calibration (NOT the same as the UK'37 calibration).  +
PYTVVKA7U87.δ18osw +	Ensemble and summary tables do not take into account horizons with NaN values  +
PYTVWXU47PR.ghostMeasured.Calibration +	MUE1998: Muller et al. 1998 sediment core top based calibration, n=370, R2=0.958)  +
PYTW0D8MOY6.d18og.rub.Uncertainty1 +	Determined by replicate analyses of NBS-19 and laboratory standards (PTB-1)  +
PYTWA01D79H.g. ruber ss mg/ca +	sensu stricto  +
PYTWCPO4MJI.ukprime37.Uncertainty1 +	based on 22 replicate extractions on di¡er- ent days of two laboratory internal reference sediments (CC 2107-3 and CC 1706-2) from the South Atlantic  +
PYTWDV3B356.depth +	sdfasd  +
PYTWUMOXKFD.ghostMeasured.Calibration +	PRA1988: T(cultures) = (Uk'37-0.039)/(0.034), (Prahl et al., (1988); cultures E. huxleyi, 8-25ºC, n=22; R2=0.994)  +
PYTX2NMDZMJ.g. bulloides +	chamber f  +
PYTX99MNKTS.ghostMeasured.Calibration +	ANA2003: G. ruber white 250-350um based on sediment trap data, with an assumed exponential constant of 0.090. Because this value is assumed, there is no proper way to estimate uncertainty.  +
PYTXBEWD6RF.mgcass sst +	G. ruber sensu stricto, 250-350 size fraction  +