Copy the page URI to the clipboard
Hanselman, Jennifer A.; Bush, Mark B.; Gosling, William D.; Collins, Aaron; Knox, Christopher; Baker, Paul A. and Fritz, Sheri C.
(2011).
DOI: https://doi.org/10.1016/j.palaeo.2011.03.002
Abstract
Fossil pollen and charcoal analyses of sediments from Lake Titicaca, Peru/Bolivia, provide a record of palaeoclimatic variation spanning four full glacial cycles. Pollen, aquatic microfossils, and charcoal, as well as previously published data including diatom assemblages, carbonate content, and stable carbon isotopic ratios of organic carbon, indicate that interglacials were warm and dry whereas the peaks of glacials were cold and wet. Each of the interglacials documented in the record are somewhat different, with those of MIS 5e and MIS 9 inducing lower lake levels and a drier vegetation signature than those of MIS 7 and 1. The presence of charcoal particles in sediments deposited during previous interglacials provides evidence of the long-term role of fire in shaping Andean ecosystems.
Viewing alternatives
Metrics
Public Attention
Altmetrics from AltmetricNumber of Citations
Citations from DimensionsItem Actions
Export
About
- Item ORO ID
- 28501
- Item Type
- Journal Item
- ISSN
- 0031-0182
- Project Funding Details
-
Funded Project Name Project ID Funding Body Not Set ATM 0317539 NSF Not Set AGS 0602329 NSF Not Set EAR 0602154 NSF - Keywords
- Andes; climate change; fire; fossil pollen; fossil charcoal; interglacial
- Academic Unit or School
-
Faculty of Science, Technology, Engineering and Mathematics (STEM) > Environment, Earth and Ecosystem Sciences
Faculty of Science, Technology, Engineering and Mathematics (STEM) - Research Group
- OpenSpace Research Centre (OSRC)
- Copyright Holders
- © 2011 Elsevier B.V.
- Depositing User
- William Gosling