Backman, Jan; Jakobsson, Martin; Frank, Martin; Sangiorgi, Francesca; Brinkhuis, Henk; Stickley, Catherine E; O'Regan, Matthew; Løvlie, Reidar; Pälike, Heiko; Spofforth, David J A; Gattacceca, Jérôme; Moran, Kathryn; King, John W; Heil, Chip (2008): Age control and stratigraphy of a sediment profile from the Lomonosov Ridge, Arctic Ocean. PANGAEA, https://doi.org/10.1594/PANGAEA.706556, Supplement to: Backman, J et al. (2008): Age model and core-seismic integration for the Cenozoic Arctic Coring Expedition sediments from the Lomonosov Ridge. Paleoceanography, 23(1), PA1S03, https://doi.org/10.1029/2007PA001476
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The upper 200 m of the sediments recovered during IODP Leg 302, the Arctic Coring Expedition (ACEX), to the Lomonosov Ridge in the central Arctic Ocean consist almost exclusively of detrital material. The scarcity of biostratigraphic markers severely complicates the establishment of a reliable chronostratigraphic framework for these sediments, which contain the first continuous record of the Neogene environmental and climatic evolution of the Arctic region. Here we present profiles of cosmogenic 10Be together with the seawater-derived fraction of stable 9Be obtained from the ACEX cores. The down-core decrease of 10Be/9Be provides an average sedimentation rate of 14.5 ± 1 m/Ma for the uppermost 151 m of the ACEX record and allows the establishment of a chronostratigraphy for the past 12.3 Ma. The age-corrected 10Be concentrations and 10Be/9Be ratios suggest the existence of an essentially continuous sea ice cover over the past 12.3 Ma.
Median Latitude: 87.892587 * Median Longitude: 137.730787 * South-bound Latitude: 87.866580 * West-bound Longitude: 136.177350 * North-bound Latitude: 87.921180 * East-bound Longitude: 139.365010
Date/Time Start: 2004-08-19T00:00:00 * Date/Time End: 2004-08-27T00:00:00
302-CompSite * Latitude: 87.890000 * Longitude: 137.650000 * Elevation: -1251.0 m * Campaign: Exp302 (Arctic Coring Expedition, ACEX) * Basis: Vidar Viking * Method/Device: Composite Core (COMPCORE) * Comment: Virtual core composed of spliced cores from Holes M0002A, M0003A, M0004A and M0004C. Virtual position and water depth is calculated as the mean of all Exp302 sites.
302-M0002A (ACEX-M2A) * Latitude: 87.921180 * Longitude: 139.365010 * Date/Time: 2004-08-19T00:00:00 * Elevation: -1209.0 m * IGSN: IBCR0302RHTS001 * Penetration: 270.1 m * Recovery: 214.68 m * Location: Arctic Ocean * Campaign: Exp302 (Arctic Coring Expedition, ACEX) * Basis: Vidar Viking
Datasets listed in this publication series
- Backman, J; Jakobsson, M; Frank, M et al. (2008): (Table 1) Age estimates of lithostratigraphic units of Hole 302-M0002A. https://doi.org/10.1594/PANGAEA.705518
- Backman, J; Jakobsson, M; Frank, M et al. (2008): (Table 1) Age estimates of lithostratigraphic units of Hole 302-M0004A. https://doi.org/10.1594/PANGAEA.705519
- Backman, J; Jakobsson, M; Frank, M et al. (2008): (Table 1) Age-Depth control points and sedimentation rates of IODP Exp302 sediments. https://doi.org/10.1594/PANGAEA.705517