Eilandvlei.Wuendsch.2018 - v1.0.12

Dataset Id: uzZm350xhkKAT2yLSiFE

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R code to load dataset:

L <- lipdR::readLipd("https://lipdverse.org/data/uzZm350xhkKAT2yLSiFE/1_0_12/Eilandvlei.Wuendsch.2018.lpd")

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root

archiveType: LakeSediment

originalDataUrl: https://doi.org/10.1594/PANGAEA.887884

lipdVersion: 1.3

pub
pub1

author: list(list(name = "Wuendsch, Michael"))

journal: Global and Planetary Change

volume: 163

pages: 51-66

title: Holocene environmental change along the southern Cape coast of South Africa – Insights from the Eilandvlei sediment record spanning the last 8.9 kyr

doi: 10.1016/j.gloplacha.2018.02.002

geo

latitude: -33.9953

longitude: 22.6401

siteName: Eilandvlei (EV13)

PaleoData columns
depth (m)

TSid: WEBb8ffd55c

variableName: depth

units: m

age (yr BP)

TSid: WEB2f1e314e

variableName: age

units: yr BP

waterTableDepth (percent)

TSid: WEB4fd44759

variableName: waterTableDepth

units: percent

interpretation
1

scope: climate

Al (mg/kg)

TSid: WEBdcd05475

variableName: Al

units: mg/kg

interpretation
1

scope: climate

Ca (mg/kg)

TSid: WEB73447bb2

variableName: Ca

units: mg/kg

interpretation
1

scope: climate

Fe (mg/kg)

TSid: WEBbb8f1c58

variableName: Fe

units: mg/kg

interpretation
1

variable: precipitation

direction: positive

scope: climate

variableDetail: @catchment

seasonality: Annual

seasonalityGeneral: Annual

potassium (mg/kg)

TSid: WEB178b277c

variableName: potassium

units: mg/kg

interpretation
1

scope: climate

sodium (mg/kg)

TSid: WEB7d81552f

variableName: sodium

units: mg/kg

interpretation
1

scope: climate

needsToBeChanged (mg/kg)

TSid: WEB38d61af6

variableName: needsToBeChanged

units: mg/kg

interpretation
1

scope: climate

sodium (mg/kg)

TSid: WEB0c26ecc2

variableName: sodium

units: mg/kg

interpretation
1

scope: climate

index (unitless)

TSid: WEB5aca062f

variableName: index

units: unitless

interpretation
1

variable: precipitation

direction: positive

scope: climate

variableDetail: @catchment

seasonality: Annual

basis: "The CIA was established as an indicator for the degree of chemical (silicate) weathering of rocks and sediments, a process whose intensity strengthens with increasing humidity...The CIA and <16 μm grain size data moreover show a similar pattern as the Fe record (Fig. 5). It is concluded that they reveal the similar palaeoenvironmental signal, namely that the deposition of fine-grained, more weathered, and iron-rich material is linked to increased river discharge in the watershed of Eilandvlei and hence, to relatively high regional precipitation"

seasonalityGeneral: Annual