LS11MOES - v1.0.5

Dataset Id: HpU76p9BXXQldgpX5oH9

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R code to load dataset:

L <- lipdR::readLipd("https://lipdverse.org/data/HpU76p9BXXQldgpX5oH9/1_0_5/LS11MOES.lpd")

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In compilations: (only most recent versions are shown)

iso2k-1_1_1

root

archiveType: LakeSediment

originalDataUrl: this compilation

lipdVersion: 1.3

pub
pub1

author: Morellon, Mario , Valero-Garces, Blas , Gonzalez-Samperiz, Penelope , Vegas-Vilarrubia, Teresa , Rubio, Esther , Rieradevall, Maria , Delgado-Huertas, Antonio , Mata, Pilar , Romero, Oscar , Engstrom, Daniel R. , Lopez-Vicente, Manuel , Navas, Ana , Soto, Jesus

journal: Journal of Paleolimnology

volume: 46

pages: -29

title: Climate changes and human activities recorded in the sediments of Lake Estanya (NE Spain) during the Medieval Warm Period and Little Ice Age

doi: 10.1007/s10933-009-9346-3

geo

latitude: 42.03

longitude: 0.53

elevation: 670

siteName: Estanya

PaleoData columns
year (yr AD)

TSid: MAT463c074629

variableName: year

units: yr AD

description: Year AD

interpretation
1

rank: NA

scope: climate

2

rank: NA

scope: climate

depth (cm)

TSid: MAT72fb118581

variableName: depth

units: cm

description: depth

interpretation
1

rank: NA

scope: climate

2

rank: NA

scope: climate

d18O (permil)

TSid: LS11MOES

variableName: d18O

units: permil

description: carbonate

interpretation
1

scope: climate

2

scope: climate

3

scope: climate

4

basis: The isotopic composition of the Triassic limestone bedrock is characterized by relatively low oxygen isotope values (between -4.0 and -6.0%; average d18Ocalcite = -5.3%)...samples from units 6, 5 and 3 show d18Ocalcite values (-7.1% to -3.2%) similar to the isotopic signal of the bedrock (-4.6% to -5.2%), indicating a dominant clastic origin of the carbonate.

direction: negative

equilibriumEvidence: The isotopic composition of this calcite [endogenic calcite in macrophyte coatings] is approximately in equilibrium with lake waters,

inferredMaterial: lake water

integrationTimeUncertaintyType: chronological

integrationTimeUnits: years

rank: 1

scope: isotope

variable: effectivePrecipitation

variableGroup: EffectiveMoisture

variableGroupDirection: negative

variableGroupOriginal: P_E

5

basis: In the absence of contamination sources [units 1,2 4a and 4b], the two primary factors controlling d18Ocalcite values are moisture balance (precipitation minus evaporation) and the isotopic composition of lake waters (Griffiths et al. 2002)

direction: negative

equilibriumEvidence: The isotopic composition of this calcite [endogenic calcite in macrophyte coatings] is approximately in equilibrium with lake waters,

inferredMaterial: lake water, allochthonous calcite

integrationTimeUncertaintyType: chronological

integrationTimeUnits: years

rank: 2

scope: isotope

variable: effectivePrecipitation

variableGroup: EffectiveMoisture

variableGroupDirection: negative

variableGroupOriginal: P_E

6

scope: isotope

ChronData columns
depth (cm)

TSid: chron1

variableName: depth

units: cm

description: mid-point depth

age14C (yr14C BP)

TSid: chron2

variableName: age14C

units: yr14C BP

description: 14C years before 1950

SD (yr14C BP)

TSid: chron3

variableName: SD

units: yr14C BP

description: 14C years uncertainty

fractionModern ()

TSid: chron4

variableName: fractionModern

description: fraction of modern 14C activity

fractionModernUncertainty ()

TSid: chron5

variableName: fractionModernUncertainty

description: fraction of modern 14C activity uncertainty

delta13C (permil)

TSid: chron6

variableName: delta13C

units: permil

description: delta13C of material analyzed for 14C

delta13Cuncertainty (permil)

TSid: chron7

variableName: delta13Cuncertainty

units: permil

description: delta13C uncertainty

thickness (cm)

TSid: chron8

variableName: thickness

units: cm

description: thickness of sample (along depth axis)

labID ()

TSid: chron9

variableName: labID

description: laboratory ID from radiocarbon facility

materialDated ()

TSid: chron10

variableName: materialDated

description: material analyzed

activity (Bq g-1)

TSid: chron11

variableName: activity

units: Bq g-1

description: 210Pb, 239+240Pu or 137Cs activity

activityUncertainty (Bq g-1)

TSid: chron12

variableName: activityUncertainty

units: Bq g-1

description: 210Pb, 239+240Pu or 137Cs activity uncertainty

supportedActivity ()

TSid: chron13

variableName: supportedActivity

description: Y if supported 210Pb activity, N if unsupported 210Pb activity

x210PbModel ()

TSid: chron14

variableName: x210PbModel

description: model used to convert 210Pb activity to age (e.g., constant rate of supply)

age (yr BP)

TSid: chron15

variableName: age

units: yr BP

description: years before 1950 (calibrated age, or ages that dont need calibration)

SD (yr BP)

TSid: chron16

variableName: SD

units: yr BP

description: uncertainty in age

reservoirAge14C (yr14C BP)

TSid: chron17

variableName: reservoirAge14C

units: yr14C BP

description: 14C reservoir age

reservoirAge14CUncertainty (yr14C BP)

TSid: chron18

variableName: reservoirAge14CUncertainty

units: yr14C BP

description: 14C reservoir age uncertainty

useInAgeModel ()

TSid: chron19

variableName: useInAgeModel

description: was this date used in the age model?