The Labrador Sea is one of the primary areas of deep water formation in the North Atlantic Ocean, and is therefore a key region for regional- and global-scale ocean thermohaline circulation and climate variability studies (e.g. Sy et al. 1997). Since high resolution records are difficult to obtain d...
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| Format: | Text |
| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.631.2829 http://www.geus.dk/publications/review-greenland-97/gsb180p168-171.pdf |
| Summary: | The Labrador Sea is one of the primary areas of deep water formation in the North Atlantic Ocean, and is therefore a key region for regional- and global-scale ocean thermohaline circulation and climate variability studies (e.g. Sy et al. 1997). Since high resolution records are difficult to obtain due to low sedimentation rates and bioturbation in the Labrador Sea itself high resolu-tion proxy records must come from regions surround-ing the Labrador Sea. Here we report on reconnaissance work carried out on coastal lakes in Greenland. The pri-mary objective of this study is to generate annually-dated lake sediment records of climate variability for the last 2000 years. A second objective is to generate century-resolved, quantified, radiocarbon dated records that extend back to the last deglaciation. Finally, we will also attempt to retrieve lake sediments from ice-free time peri-ods of the last glacial stage or the last interglacial stage; such pre-Holocene lake sediments have already been successfully recovered from lakes on Baffin Island, in Canada (Wolfe & Härtling 1996; Miller et al. in press). This work will improve the understanding of how the Labrador Sea modulates ocean circulation as well as North Atlantic, Arctic, and global climate. Reconnaissance field work was carried out in West Greenland in the summer of 1996 (Anderson & Bennike 1997); in the summer of 1997 further reconnaissance studies were undertaken in the area between Kap Farvel and Søndre Strømfjord (Fig. 1). The objectives of these studies were to locate basins with annually laminated (varved) sediments, as such sediments allow a dating uncertainty of only a few years (Hughen et al. 1996). We concentrated our initial efforts on low-elevation iso-lated basins which can contain salt water below a fresh-water cap as a result of recent isostatic uplift or tidal interaction with the modern ocean. These basins can become density stratified and meromictic, resulting in anoxic bottom water and the preservation of laminated sediment (Fig. 2). ... |
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