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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crwiley:10.1002/jqs.1174 2024-06-23T07:55:12+00:00 Reconstructing hydrological variability in Lake Baikal during MIS 11: an application of oxygen isotope analysis of diatom silica Mackay, Anson W. Karabanov, Eugene Leng, Melanie J. Sloane, Hilary J. Morley, David W. Panizzo, Virginia N. Khursevich, Galina Williams, Douglas 2008 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 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Journal of Quaternary Science volume 23, issue 4, page 365-374 ISSN 0267-8179 1099-1417 journal-article 2008 crwiley https://doi.org/10.1002/jqs.1174 2024-06-04T06:42:16Z 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. Article in Journal/Newspaper North Atlantic Wiley Online Library Journal of Quaternary Science 23 4 365 374 |
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English |
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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. |
format |
Article in Journal/Newspaper |
author |
Mackay, Anson W. Karabanov, Eugene Leng, Melanie J. Sloane, Hilary J. Morley, David W. Panizzo, Virginia N. Khursevich, Galina Williams, Douglas |
spellingShingle |
Mackay, Anson W. Karabanov, Eugene Leng, Melanie J. Sloane, Hilary J. Morley, David W. Panizzo, Virginia N. Khursevich, Galina Williams, Douglas Reconstructing hydrological variability in Lake Baikal during MIS 11: an application of oxygen isotope analysis of diatom silica |
author_facet |
Mackay, Anson W. Karabanov, Eugene Leng, Melanie J. Sloane, Hilary J. Morley, David W. Panizzo, Virginia N. Khursevich, Galina Williams, Douglas |
author_sort |
Mackay, Anson W. |
title |
Reconstructing hydrological variability in Lake Baikal during MIS 11: an application of oxygen isotope analysis of diatom silica |
title_short |
Reconstructing hydrological variability in Lake Baikal during MIS 11: an application of oxygen isotope analysis of diatom silica |
title_full |
Reconstructing hydrological variability in Lake Baikal during MIS 11: an application of oxygen isotope analysis of diatom silica |
title_fullStr |
Reconstructing hydrological variability in Lake Baikal during MIS 11: an application of oxygen isotope analysis of diatom silica |
title_full_unstemmed |
Reconstructing hydrological variability in Lake Baikal during MIS 11: an application of oxygen isotope analysis of diatom silica |
title_sort |
reconstructing hydrological variability in lake baikal during mis 11: an application of oxygen isotope analysis of diatom silica |
publisher |
Wiley |
publishDate |
2008 |
url |
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 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Journal of Quaternary Science volume 23, issue 4, page 365-374 ISSN 0267-8179 1099-1417 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/jqs.1174 |
container_title |
Journal of Quaternary Science |
container_volume |
23 |
container_issue |
4 |
container_start_page |
365 |
op_container_end_page |
374 |
_version_ |
1802647674835435520 |