ElJunco.Zhang.2014 - v1.0.11

Dataset Id: 5E6SEDAAEpI4Llv1TdfK

Download LiPD file

Download LiPD file as JSON-LD

R code to load dataset:

L <- lipdR::readLipd("https://lipdverse.org/data/5E6SEDAAEpI4Llv1TdfK/1_0_11/ElJunco.Zhang.2014.lpd")

Edit LiPD file

Download PaleoData only (csv)

Download ChronData only (csv)

Dataset changelog

Report an issue (include datasetId and version)

In compilations: (only most recent versions are shown)

iso2k-1_1_2

HoloceneHydroclimate-0_9_1

HoloceneAbruptChange-0_11_0

root

archiveType: LakeSediment

originalDataUrl: https://doi.org/10.1016/j.epsl.2014.07.013

lipdVersion: 1.3

pub
pub1

author: list(name = "Zhang, Zhaohui")

journal: Earth and Planetary Science Letters

volume: 404

pages: 420-434

title: El Nino evolution during the Holocene revealed by a biomarker rain gauge in the Galapagos Islands

doi: 10.1016/j.epsl.2014.07.013

geo

latitude: -0.9

longitude: -89.4833

elevation: 670

siteName: El Junco Lake

PaleoData columns
age (yr BP)

TSid: ROLaMTjnvyS

variableName: age

units: yr BP

interpretation
1

rank: NA

scope: climate

2

rank: NA

scope: climate

d2H (permil)

TSid: LS14ZHJU01A

variableName: d2H

units: permil

description: aquatic biomarker

interpretation
1

basis: “El Junco Lake Atwood and Sachs (2014) showed that the lake water δD was primarily controlled by rainfall rates during El Niño episodes, as opposed to evaporation or water loss through seepage or overflow….changes in rainfall amount are imprinted in the isotopic composition of botryococcenes, with negative (posi- tive) δD values co-occurring with wetter (drier) periods.”

direction: negative

interpDirection: negative

scope: climate

seasonality: Annual

seasonalityGeneral: Annual

variable: precipitation

variableDetail: amount@surface

variableGroup: P

2

scope: climate

3

scope: climate

4

basis: It is expected that dD values of botryococcene will decline when precipitation rates increase, possibly providing a metric for the severity of extreme rainfall events that are associated with El Nino events. (All botryococcene dD values were highly correlated with water dD values (R2>0.99). And, Zhang and Sachs 2007, Organic Geochemistry), 38: 582-608.

direction: negative

inferredMaterial: lake water

mathematicalRelation: linear

rank: 1

scope: isotope

seasonality: Annual

seasonalityOriginal: Annual

variable: effectivePrecipitation

variableGroup: EffectiveMoisture

variableGroupDirection: negative

variableGroupOriginal: P_E

coefficient: NA

fraction: NA

5

direction: positive

inferredMaterial: lake water

rank: 2

scope: isotope

seasonalityOriginal: Annual

variable: precipitationIsotope

variableGroup: P_isotope

variableGroupDirection: positive

variableGroupOriginal: P_E

coefficient: NA

fraction: NA

6

scope: isotope

coefficient: NA

fraction: NA

rank: NA

uncertainty (permil)

TSid: LPD796b99d7-dup

variableName: uncertainty

units: permil

description: stdev of d2H of Botryococcene

interpretation
1

scope: climate

2

scope: climate

3

scope: climate

4

rank: NA

scope: isotope

coefficient: NA

fraction: NA

5

rank: NA

scope: isotope

coefficient: NA

fraction: NA

6

scope: isotope

coefficient: NA

fraction: NA

rank: NA

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 (unitless)

TSid: chron4

variableName: fractionModern

units: unitless

description: fraction of modern 14C activity

fractionModernUncertainty (unitless)

TSid: chron5

variableName: fractionModernUncertainty

units: unitless

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 (unitless)

TSid: chron9

variableName: labID

units: unitless

description: laboratory ID from radiocarbon facility

materialDated (unitless)

TSid: chron10

variableName: materialDated

units: unitless

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 (unitless)

TSid: chron13

variableName: supportedActivity

units: unitless

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

x210PbModel (unitless)

TSid: chron14

variableName: x210PbModel

units: unitless

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 (unitless)

TSid: chron19

variableName: useInAgeModel

units: unitless

description: was this date used in the age model?