Reconstructing hydrological variability in Lake Baikal during MIS 11: an application of oxygen isotope analysis of diatom silica

Abstract In this paper we reconstruct hydrological variability in Lake Baikal during Marine Isotope Stage 11 (MIS 11) (427–362 ka BP) from oxygen isotope analysis of diatom silica. Highest δ 18 O diatom values are found during MIS 11.3, highlighting the dominance of hydrological input from rivers fl...

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Bibliographic Details
Published in:Journal of Quaternary Science
Main Authors: Mackay, Anson W., Karabanov, Eugene, Leng, Melanie J., Sloane, Hilary J., Morley, David W., Panizzo, Virginia N., Khursevich, Galina, Williams, Douglas
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2008
Subjects:
North Atlantic
Online Access:http://dx.doi.org/10.1002/jqs.1174
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjqs.1174
https://onlinelibrary.wiley.com/doi/pdf/10.1002/jqs.1174
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Summary:Abstract In this paper we reconstruct hydrological variability in Lake Baikal during Marine Isotope Stage 11 (MIS 11) (427–362 ka BP) from oxygen isotope analysis of diatom silica. Highest δ 18 O diatom values are found during MIS 11.3, highlighting the dominance of hydrological input from rivers flowing into the south and central basins of Lake Baikal, especially the Selenga River. Hydrological input from south basin rivers dominated for over 30 ka. However, there is evidence from both biogenic silica and δ 18 O diatom records for an abrupt cooling event at ca. 390 ka BP. Stadial conditions at this time are coincident with an iceberg discharge event into the North Atlantic. The decline in δ 18 O diatom values suggests increasing proportion of hydrological input from rivers to the north of Lake Baikal, due to greater influence of winter precipitation and snow‐melt. After a period of interstadial conditions during the early stages of MIS 11.1, biogenic silica and δ 18 O diatom values decline, mirroring the slow growth in Northern Hemisphere ice sheets. Despite rigorous cleaning procedures, palaeoclimatic inferences need to be treated with caution due to contamination of the δ 18 O diatom record; during stadial and glacial periods, contamination of the δ 18 O diatom record is even more significant. © Natural Environment Research Council (NERC) copyright 2008. Reproduced with the permission of NERC. Published by John Wiley & Sons, Ltd.

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