Document Type

Article

Journal/Book Title/Conference

Journal of Paleolimnology

Volume

40

Issue

1

Publisher

Springer Netherlands

Publication Date

12-6-2007

Keywords

Lake sediment geochemistry, sediment provenance, constrained least squares, discriminant analysis, Kluane lake, Yukon Territory

First Page

489

Last Page

505

Abstract

The level of Kluane Lake in southwest Yukon Territory, Canada, has fluctuated tens of metres during the late Holocene. Contributions of sediment from different watersheds in the basin over the past 5,000 years were inferred from the elemental geochemistry of Kluane Lake sediment cores. Elements associated with organic material and oxyhydroxides were used to reconstruct redox fluctuations in the hypolimnion of the lake. The data reveal complex relationships between climate and river discharge during the late Holocene. A period of influx of Duke River sediment coincides with a relatively warm climate around 1,300 years BP. Discharge of Slims River into Kluane Lake occurred when Kaskawulsh Glacier advanced to the present drainage divide separating flow to the Pacific Ocean via Kaskawulsh and Alsek rivers from flow to Bering Sea via tributaries of Yukon River. During periods when neither Duke nor Slims river discharged into Kluane Lake, the level of the lake was low and stable thermal stratification developed, with anoxic and eventually euxinic conditions in the hypolimnion.

Comments

This is a post-peer-review, pre-copyedit version of an article published in the Journal of Paleolimnology. The final authenticated version is available online at: http://dx.doi.org/10.1007/s10933-007-9177-z

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