Kivu.Olsson.1959 - v1.1.10

Dataset Id: xevxaCrCe2KKvX4hKabp

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R code to load dataset:

L <- lipdR::readLipd("https://lipdverse.org/data/xevxaCrCe2KKvX4hKabp/1_1_10/Kivu.Olsson.1959.lpd")

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In compilations: (only most recent versions are shown)

root

archiveType: Shoreline

originalDataUrl: https://doi.org/10.25921/mxae-9596

lipdVersion: 1.3

pub
pub1

author: list(list(name = "Degens, E.T. and R.E. Hecky"))

title: Paleoclimatic reconstruction of Late Pleistoceneand Holocene based on biogenic sediments from the Black Sea and a tropical African lake. Colloquesinternationaux du C.N.R.S. 219 : 1-11.

doi: 10.1016/0031-0182(87)90048-4

pub2

doi: 10.2172/5609291

geo

latitude: -2

longitude: 29

elevation: 1462

siteName: Kivu

PaleoData columns
age (yr BP)

TSid: OLS_RxL9GeQjQIM

variableName: age

units: yr BP

description: estimated calibrated bin mid-point age

uncertaintyHigh (yr BP)

TSid: OLS_RX0IB9I0K3H

variableName: uncertaintyHigh

units: yr BP

description: estimated calibrated bin old age

interpretation
1

scope: climate

uncertaintyLow (yr BP)

TSid: OLS_RajRljOn6l8

variableName: uncertaintyLow

units: yr BP

description: estimated calibrated bin young age

interpretation
1

scope: climate

lakeLevel (unitless)

TSid: OLS_R4Ijw8OPsjM

variableName: lakeLevel

units: unitless

description: This is a millennial-scale estimate of lake status in relative units. 3 corresponds to LOW: 0-15% of the total altitudinal range of fluctuation, including dry lakes, 2 corresponds to INTERMEDIATE, or 15-70% of the total range, and 1 corresponds to HIGH: 70-100% of the total range of fluctuation, including overflowing lakes. In the original dataset, 0s were labeled uncodable. Here, they have been changed to NA.

interpretation
1

variable: effectivePrecipitation

variableDetail: LakeLevel@surface

scope: climate

direction: negative

seasonality: Annual

seasonalityGeneral: Annual

variableGroup: P-E

lakeTrend (unitless)

TSid: OLS_RwGW5gCWOGt

variableName: lakeTrend

units: unitless

description: This is a millennial-scale estimate of lake trend in relative units. 3 corresponds to falling, 2 corresponds to stable, and 1 corresponds to rising. In the original dataset, 0s were labeled uncodable. Here, they have been changed to NA.

interpretation
1

scope: climate