L <- lipdR::readLipd("https://lipdverse.org/data/Ym0wRa7uxnHVhgfCTKpb/1_0_11/LakeEdward.Russell.2005.lpd")
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archiveType: LakeSediment
originalDataUrl: https://doi.org/10.25921/p4tq-3m10
lipdVersion: 1.3
author: list(list(name = "Russell, James M."))
journal: Quaternary Science Reviews
volume: 24
pages: 1375-1389
title: A high-resolution geochemical record from Lake Edward, Uganda Congo and the timing and causes of tropical African drought during the late Holocene
doi: 10.1016/j.quascirev.2004.10.003
latitude: -0.4167
longitude: 29.75
elevation: 917
siteName: Lake Edward
TSid: WEBc0d485a3
variableName: age
units: yr BP
TSid: WEB579775e5
variableName: Mg
units: percent
description: Mg in calcite, mol%, 3-core stack
variable: effectivePrecipitation
direction: negative
scope: climate
variableDetail: lakebalance@surface
seasonality: Annual
basis: "Both limnologic and geologic studies of Lake Edward have shown that the %Mg in calcite is negatively correlated with water balance in Lake Edward (Lehman, 2002; Russell et al., 2003b), as is common of carbonates in lakes... These fluctuations are superimposed on a long-term positive trend in %Mg that indicates progressively more arid conditions from 5000 to about 1800 cal year BP, followed by a slight trend toward negative %Mg values indicating wetter climates."
seasonalityGeneral: Annual
variableGroup: P-E
TSid: WEB96479a31
variableName: Mg
units: percent
description: Detrended Mg in calcite, mol%, 3 core stack
scope: climate
root
pub
pub1
geo
PaleoData columns
age (yr BP)
Mg (percent)
interpretation
1
Mg (percent)
interpretation
1