DOI: 10.1016/j.quascirev.2015.04.022
Scopus记录号: 2-s2.0-84930195375
论文题名: Impact of Bolivian paleolake evaporation on the δ18O of the Andean glaciers during the last deglaciation (18.5-11.7 ka): Diatom-inferred δ18O values and hydro-isotopic modeling
作者: Quesada B. ; Sylvestre F. ; Vimeux F. ; Black J. ; Paillès C. ; Sonzogni C. ; Alexandre A. ; Blard P.-H. ; Tonetto A. ; Mazur J.-C. ; Bruneton H.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2015
卷: 120 起始页码: 93
结束页码: 106
语种: 英语
英文关键词: Andean ice cores
; Bolivian Altiplano
; Deglaciation
; Diatoms
; Ostracods
; Oxygen isotopes
; Paleolakes
Scopus关键词: Algae
; Animals
; Evaporation
; Geochronology
; Isotopes
; Lakes
; Oxygen
; Phytoplankton
; Snow
; Bolivian Altiplano
; Deglaciations
; Diatoms
; Ice core
; Ostracods
; Oxygen isotopes
; Paleolakes
; Ice
; diatom
; evaporation
; glacial hydrology
; hydrological cycle
; ice core
; isotopic composition
; lacustrine deposit
; last deglaciation
; ostracod
; oxygen isotope
; paleolimnology
; stable isotope
; Altiplano
; Andes
; Bolivia
; Nevado Sajama
; Oruro [Bolivia]
; Bacillariophyta
; Ostracoda
英文摘要: During the last deglaciation, the Bolivian Altiplano (15-23°S, 66-70°W) was occupied by paleolake Tauca covering, at least, ~51,000 km2 at its maximum highstand between 16.5 and 15 ka. Twenty-five hundred years later, after a massive regression, a new transgressive phase, produced paleolake Coipasa, smaller than Tauca and restricted to the southern part of the basin. These paleolakes were overlooked at the west by the Sajama ice cap. The latter provides a continuous record of the oxygen isotopic composition of paleo-precipitation for the last 25 ka. Contemporaneously to the end of paleolake Tauca, around 14.3 ka, the Sajama ice cap recorded a significant increase in ice oxygen isotopic composition (δ18Oice ). This paper examines to what extent the disappearance of Lake Tauca contributed to precipitation on the Sajama summit and this specific isotopic variation. The water δ18O values of paleolakes Tauca and Coipasa (δ18Olake ) were quantitatively reconstructed from 18.5 to 11.7 ka based on diatom isotopic composition (δ18Odiatoms ) and ostracod isotopic composition (δ18Ocarbonates ) retrieved in lacustrine sediments. At a centennial time scale, a strong trend appears: abrupt decreases of δ18Olake during lake fillings are immediately followed by abrupt increases of δ18Olake during lake level stable phases. The highest variation occurred at ~15.8 ka with a δ18Olake decrease of about ~10‰, concomitant with the Lake Tauca highstand, followed ~400 years later by a 7‰ increase in δ18Olake . A simple hydro-isotopic modeling approach reproduces consistently this rapid "decrease-increase" feature. Moreover, it suggests that this unexpected re-increase in δ18Olake after filling phases can be partly explained by an equilibration of isotopic fluxes during the lake steady-state. Based on isotopic calculations during lake evaporation and a simple water stable isotopes balance between potential moisture sources at Sajama (advection versus lake evaporation), we show that total or partial evaporation (from 5 to 60%) of paleolake Tauca during its major regression phase at 14.3 ka could explain the pronounced isotopic excursion at Sajama ice cap. These results suggest that perturbations of the local hydrological cycle in lacustrine areas may substantially affect the paleoclimatic interpretation of the near-by isotopic signals (e.g. ice core or speleothems). © 2015 Elsevier Ltd. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/59910
Appears in Collections: 过去全球变化的重建
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作者单位: Aix-Marseille Université, CNRS, IRD, CEREGE, UM 34, Europôle de l'Arbois, BP 80, Aix en Provence Cedex 04, France; Institut Pierre Simon Laplace (IPSL), Laboratoire des Sciences de Climat et de l'Environnement (LSCE), UMR 8212 (CEA-CNRS-UVSQ), CEA Saclay, Orme des Merisiers, Bât. 701, Gif-sur-Yvette, France; Laboratoire HydroSciences Montpellier (HSM), UMR 5569 (CNRS-IRD-UM1-UM2), Montpellier, France; Centre de Recherches Pétrographiques et Géochimiques (CRPG), UMR 7358, CNRS, Nancy-Université, Vandœuvre-lès-Nancy, France; Aix-Marseille Université, PRATIM, Fédération de Chimie, 3 Place Victor Hugo, Marseille Cedex 3, France
Recommended Citation:
Quesada B.,Sylvestre F.,Vimeux F.,et al. Impact of Bolivian paleolake evaporation on the δ18O of the Andean glaciers during the last deglaciation (18.5-11.7 ka): Diatom-inferred δ18O values and hydro-isotopic modeling[J]. Quaternary Science Reviews,2015-01-01,120