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| Content Provider | Springer Nature Link |
|---|---|
| Author | Lamoureaux, Scott |
| Copyright Year | 1999 |
| Abstract | Multiple cores taken throughout Nicolay Lake in the Canadian High Arctic contain laminated sediments that are interpreted as varved. Annual sediment accumulation during the last 197 years reveals three major patterns that have important implications for hydroclimatic reconstruction. Widespread sediment dispersal is evident during most years and contrasts with years when anomalous localized and bifurcating patterns of deposition occur. Localized deposition is limited to the centre of the lake and is attributed to turbidity currents that originate on the delta foreslope. In contrast, a bifurcating pattern is produced when the river supplying the delta switches from one to two delta distributaries, resulting in altered proximal accumulation. Principal component analysis reveals additional accumulation anomalies that are sedimentologically indistinct, but constitute important sources of localized variance. The recognition and removal of anomalous deposition patterns is critical for accurate reconstruction of sediment flux from the catchment, particularly in long records where geomorphic conditions may have changed. This study identifies potentially misleading depositional artifacts and a methodology to recognize similar depositional controls in other lakes. |
| Starting Page | 73 |
| Ending Page | 84 |
| Page Count | 12 |
| File Format | |
| ISSN | 09212728 |
| Journal | Journal of Paleolimnology |
| Volume Number | 21 |
| Issue Number | 1 |
| e-ISSN | 15730417 |
| Language | English |
| Publisher | Kluwer Academic Publishers |
| Publisher Date | 1999-01-01 |
| Publisher Place | Dordrecht |
| Access Restriction | One Nation One Subscription (ONOS) |
| Subject Keyword | Sedimentology Physical Geography Hydrobiology Climate Change |
| Content Type | Text |
| Resource Type | Article |
| Subject | Earth-Surface Processes Aquatic Science |
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