L <- lipdR::readLipd("https://lipdverse.org/data/b80Gp0jHNJdqglhwtnn4/1_0_10/Baikal.Swann.2018.lpd")Report an issue (include datasetId and version)
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archiveType: LakeSediment
originalDataUrl: https://doi.org/10.1594/10.1594/PANGAEA.889761
lipdVersion: 1.3
author: list(list(name = "Swann, George E.A."))
journal: Quaternary Science Reviews
volume: 189
pages: 210-222
title: Lake Baikal isotope records of Holocene Central Asian precipitation
doi: 10.1016/j.quascirev.2018.04.013
author: list(list(name = "Mackay, Anson W."), list(name = "Swann, George E. A."), list(name = "Brewer, Tim S."), list(name = "Leng, Melanie J."), list(name = "Morley, David W."), list(name = "Piotrowska, Natalia"), list(name = "Rioual, Patrick"), list(name = "White, Dustin"))
journal: Journal of Quaternary Science
volume: 26
pages: 627-634
title: A reassessment of late glacial - Holocene diatom oxygen isotope record from Lake Baikal using a geochemical mass-balance approach
doi: 10.1002/jqs.1484
latitude: 51.58
longitude: 104.85
siteName: Vydrino Shoulder, Lake Baikal
TSid: WEBe0a0dc53
variableName: age
units: yr BP
TSid: WEBd1125bee
variableName: d18O
units: permil
description: Diatoms δ18O (Mackay et al. 2011)
variable: precipitation
direction: positive
scope: climate
variableDetail: inflow@surface
basis: "As d18O diatom reflects the isotope composition of ambient water in Lake Baikal, sedimentary records of d18Odiatom should also reflect changes in regional Central Asian precipitation across the wider region around Lake Baikal. This is supported by the strong correlation and relationship between din-flux and d18Odiatom, with increases (decrease) in d18O diatom associated with higher (lower) dinflux and an increase (decrease) in precipitation (Fig. 6a), as well as by the linear relationship between d18Odiatom and decadal smoothed annual precipitation "
variableGroup: P
seasonality: Annual
seasonalityGeneral: Annual
TSid: WEB2b09ab9c
variableName: precipitation
units: mm/yr
description: Precip annual total (Reconstructed)
variable: precipitation
direction: positive
scope: climate
variableDetail: amount@surface
seasonality: Annual
basis: "Using the relationship betweend18Odiatomand precipitation from c.2010-1900 (Fig. 6c) we quantify decadal changes in annual pre-cipitation for Central Asia from our composite south basind18Odia-tomrecord, which extends back to c.1850 AD"
seasonalityGeneral: Annual
variableGroup: P
root
pub
pub1
pub2
geo
PaleoData columns
age (yr BP)
d18O (permil)
interpretation
1
precipitation (mm/yr)
interpretation
1