Open AccessSedimentation rates in the Makarov Basin, central Arctic Ocean: A paleomagnetic and rock magnetic approach
Author(s) -
Nowaczyk Norbert R.,
Frederichs Thomas W.,
Kassens Heidi,
NørgaardPedersen Nils,
Spielhagen Robert F.,
Stein Rüdiger,
Weiel Dominik
Publication year - 2001
Publication title -
paleoceanography
Language(s) - English
Resource type - Journals
eISSN - 1944-9186
pISSN - 0883-8305
DOI - 10.1029/2000pa000521
Subject(s) - paleomagnetism , geology , magnetostratigraphy , sedimentation , sediment , remanence , rock magnetism , paleontology , structural basin , arctic , oceanography , magnetization , physics , quantum mechanics , magnetic field
Three long sediment cores from the Makarov Basin have been subjected to detailed paleomagnetic and rock magnetic analyses. Investigated sediments are dominated by normal polarity including short reversal excursions, indicating that most of the sediments are of Brunhes age. In general, the recovered sediments show only low to moderate variability in concentration and grain size of the remanence‐carrying minerals. Estimations of relative paleointensity variations yielded a well‐documented succession of pronounced lows and highs that could be correlated to published reference curves. However, together with five accelerator mass spectrometry 14 C ages and an incomplete 10 Be record, still two different interpretations of the paleomagnetic data are possible, with long‐term sedimentation rates of either 1.3 or 4 cm kyr −1 . However, both models implicate highly variable sedimentation rates of up to 10 cm kyr −1 , and abrupt changes in rock magnetic parameters might even indicate several hiatuses.