EGU22-4862, updated on 22 Nov 2024
https://doi.org/10.5194/egusphere-egu22-4862
EGU General Assembly 2022
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

High-resolution inclination records from Sites U1418 and U1419 in the Gulf of Alaska (IODP Expedition 341)

Julie Heggdal Velle1,2,8, Maureen Walczak3,4, Brendan Reilly5, Guillaume St-Onge1,2, Joseph Stoner2,3, Stewart Fallon4, Alan Mix3, Christina Belanger6, and Matthias Forwick7
Julie Heggdal Velle et al.
  • 1Canada Research Chair in Marine Geology, Institut des sciences de la mer de Rimouski (ISMER), Université du Québec à Rimouski, Rimouski, Canada
  • 2GEOTOP Research Center, Montréal, Canada
  • 3College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, Oregon, United States
  • 4Research School of Earth Sciences, Australian National University, Canberra, Australia
  • 5Scripps Institution of Oceanography, University of California San Diego, La Jolla, California, United States
  • 6Department of Geology and Geophysics, Texas A&M University, College Station, Texas, United States
  • 7Department of Geosciences, UiT The Arctic University of Norway in Tromsø, Tromsø, Norway
  • 8Geological Survey of Norway, Marine Geology, Trondheim, Norway (julie.heggdal.velle@ngu.no)

International Ocean Drilling Program (IODP) Expedition 341 in the Gulf of Alaska recovered a 112-meter-long sedimentary record from the continental slope at Site U1419. At this site, an exceptionally expanded late Pleistocene sequence (sedimentation rates >100 cm/kyr) combined with a high-resolution radiocarbon chronology (Walczak et al., 2020), provide an opportunity to study Paleomagnetic Secular Variations (PSV) on centennial to millennial timescales over the past ~43,000 years.
Natural and laboratory-induced magnetic remanence were measured on u-channels using the stepwise AF demagnetization procedure. In addition to continuous magnetic susceptibility measurements, hysteresis parameters were obtained on 95 discrete samples, and IRM acquisition curves on 9 discrete samples to obtain additional information on the magnetic mineralogy of the sediment. Due to the influence of lithology, magnetic mineralogy, depositional and post-depositional processes, Site U1419 is not suitable for paleointensity studies. However, with removal of intervals influenced by the environmental signal and/or coring deformation, the high sedimentation rates at this site have helped to preserve a reliable record of inclination. Because of signal to noise issues, inclination as measured after the 20 mT AF demagnetization step provides the most accurate estimate. This is demonstrated by comparing the U1419 inclination to a stack of the shipboard inclination at Site U1418 on a new age model developed from 19 radiocarbon dates on U1418 and 18 magnetic susceptibility-based tie-points to site survey core EW0408-87JC (Praetorius et al., 2015). This independently replicated inclination record verifies centennial to millennial scale variations in the Gulf of Alaska that can now be compared with other northeast Pacific and western North American records to begin deciphering geomagnetic variability and provide a new stratigraphic correlation tool for 15 and 30 cal kyr BP interval in this region.

How to cite: Velle, J. H., Walczak, M., Reilly, B., St-Onge, G., Stoner, J., Fallon, S., Mix, A., Belanger, C., and Forwick, M.: High-resolution inclination records from Sites U1418 and U1419 in the Gulf of Alaska (IODP Expedition 341), EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-4862, https://doi.org/10.5194/egusphere-egu22-4862, 2022.