Decadal to millennial-scale periodicities in North Iceland shelf sediments over the last 12000 cal yr: long-term North Atlantic oceanographic variability and solar forcing

Details Decadal to millennial-scale periodicities in North Iceland shelf sediments over the last 12000 cal yr: long-term North Atlantic oceanographic variability and solar forcing Decadal to millennial-scale periodicities in North Iceland shelf sediments over the last 12000 cal yr: long-term North Atlantic oceanographic variability and solar forcing

May 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003e%26psl.210..453a&link_type=abstract

Earth and Planetary Science Letters, Volume 210, Issue 3-4, p. 453-465.

Computer Science

18

Scientific paper

Giant piston core MD99-2269 recovered 25 m of sediment in Hunáfloáall, a deep trough on the North Iceland margin fronting the Iceland Sea, and the site of a shelf sediment drift. The rate of sediment accumulation is 2 m/kyr (5 yr/cm); the core terminated in the Vedde tephra (~12 cal ka). The sediment was sampled at between 5 and 50 yr/sample, including rock magnetic, grain-size, and sediment properties. Data reduction was carried out using principal component analysis. Two PC axes for the 5-yr/sample magnetic data are strongly correlated with measures of coercivity (ARM20 mT/ARM) and magnetic concentrations (kARM). In turn ARM20 mT/ARM is highly correlated (negatively) with grain-size and the mean size of the sortable silt fraction. Analyses of the two PC axes with MTM spectral methods indicate a series of significant (>99%) periodicities at millennial to multidecadal scales, including those at ~200, 125, and 88 yr which are associated with solar variability. We also document a strong correlation between the sediment magnetic properties and the ∂18O on benthic foraminifera on the North Iceland inner shelf. We hypothesize that the links between variations in grain-size, magnetic concentrations, and solar forcing are controlled by atmospheric and oceanographic changes linked to changes in the relative advection of Atlantic and polar waters along the North Iceland margin. Today these changes are associated with variations in the deep convection in the Greenland and Iceland Seas. The precise linkages are, however, presently elusive although a combination of coarser sediments and low ∂18O values define a Holocene thermal maximum between ~8 and 6 cal ka.

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