Proceedings of the IODP 2006
DOI: 10.2204/iodp.proc.302.101.2006
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Expedition 302 summary

Abstract: The first scientific drilling expedition to the central Expedition 302's destination was the Lomonosov Ridge, hypothesized to be a sliver of continental crust that broke away from the Eurasian plate at ~56 Ma. As the ridge moved northward and subsided, marine sedimentation occurred and continues to the present, resulting in what was anticipated from seismic data to be a continuous paleoceanographic record. The elevation of the ridge above the surrounding abyssal plains (~3 km) ensured that sediments atop the r… Show more

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Cited by 12 publications
(20 citation statements)
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“…The in 1206-1288 m water depth (Backman et al, 2006). The 1206-1288 m water depth (Backman et al, 2006).…”
Section: Site and Sample Collectionmentioning
confidence: 98%
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“…The in 1206-1288 m water depth (Backman et al, 2006). The 1206-1288 m water depth (Backman et al, 2006).…”
Section: Site and Sample Collectionmentioning
confidence: 98%
“…IODP Expedition 302 was designed to reconstruct the Cenozoic oceanographic history of the central Arctic Ocean (Backman et al, 2006) One specific aim within this broad goal was an understanding of the sedimentary manganese record in the first 10-50 m below seafloor (mbsf). Piston cores from the central Arctic Ocean show a series of solidphase manganese spikes, which may record past changes in bottom water redox conditions (Li et al, 1969;Jakobsson et al, 2000).…”
Section: Pore Water Problem and Rhi�on Solution Ore Water Problem Andmentioning
confidence: 99%
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