High resolution inclination records from the Gulf of Alaska, IODP Expedition 341 Sites U1418 and U1419

Author:

Velle Julie Heggdal12ORCID,Walczak Maureen H34,Reilly Brendan5,St-Onge Guillaume12,Stoner Joseph S23,Fallon Stewart4,Mix Alan C3,Belanger Christina6,Forwick Matthias7ORCID

Affiliation:

1. Canada Research Chair in Marine Geology, Institut des sciences de la mer de Rimouski (ISMER), Université du Québec à Rimouski, Rimouski QC, G5L 3A1, Canada

2. GEOTOP Research Center, C.P. 8888, Succ. Centre-Ville Montréal, QC H3C 3P8, Canada

3. College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR 9733 1, United States

4. Research School of Earth Sciences, Australian National University, Canberra, ACT 2601, Australia

5. Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA 9203 7, United States

6. Department of Geology and Geophysics, Texas A&M University, College Station, TX 7784 3, United States

7. Department of Geosciences, UiT The Arctic University of Norway in Tromsø, Tromsø 9037, Norway

Abstract

SUMMARY International Ocean Drilling Program (IODP) Expedition 341 recovered sediments from the south Alaska continental slope that preserves a well resolved and dated inclination record over most of the past ∼43 000 yr. The Site U1419 chronology is among the highest resolution in the world, constrained by 173 radiocarbon dates, providing the ability to study Palaeomagnetic Secular Variation (PSV) on centennial to millennial timescales. This record has an exceptionally expanded late Pleistocene sedimentary record with sedimentation rates commonly exceeding 100 cm kyr–1, while also preserving a lower resolution Holocene PSV record at the top. Natural and laboratory-induced magnetic remanences of U1419 u-channels from the 112-m-long spliced record were studied using stepwise AF demagnetization. Hysteresis loops were obtained on 95 and IRM acquisition curves on 9 discrete samples to facilitate magnetic domain state, coercivity and magnetic mineralogical determinations. Due to complexities related to lithology, magnetic mineralogy, and depositional and post-depositional processes, Site U1419 sediments are not suitable for palaeointensity studies and declination could not be robustly reconstructed. Progressive (titano-)magnetite dissolution with depth results in decreasing NRM intensity and signal-to-noise that is exacerbated at higher demagnetization steps. As a result, inclination measured after the 20 mT AF demagnetization step provides the most reliable directional record. Inclination appears to be well resolved with removal of just a few intervals influenced by depositional and/or sampling and coring deformation. The shipboard inclination stack from nearby IODP 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, verifies centennial to millennial scale variations in inclination observed in U1419. Comparisons with other independently dated records from the NE Pacific and western North America suggest that these sites likely capture regional geomagnetic variability. As such, this new high-resolution and well-dated inclination record, especially robust between 15 and 30 cal kyr BP, offers new geomagnetic insights and a regional correlation tool to explore this generally understudied part of the world.

Funder

Natural Sciences and Engineering Research Council of Canada

NSF

Publisher

Oxford University Press (OUP)

Subject

Geochemistry and Petrology,Geophysics

Reference53 articles.

1. Paleomagnetic overprints in ocean sediment cores and their relationship to shear deformation caused by piston coring;Acton;J. geophys. Res.,2002

2. A rapid method for magnetic granulometry with applications to environmental studies;Banerjee;Geophys. Res. Lett.,1981

3. Geomagnetic paleointensity and directional secular variation at Ocean Drilling Program (ODP) Site 984 (Bjorn Drift) since 500 ka: comparisons with ODP Site 983 (Gardar Drift);Channell;J. geophys. Res.,1999

4. The deglacial transition on the southeastern Alaska Margin: meltwater input, sea level rise, marine productivity, and sedimentary anoxia;Davies;Paleoceanography,2011

5. Late Glacial to Holocene radiocarbon constraints on North Pacific Intermediate Water ventilation and deglacial atmospheric CO2 sources;Davies-Walczak;Earth planet. Sci. Lett.,2014

Cited by 2 articles. 订阅此论文施引文献 订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献

同舟云学术

1.学者识别学者识别

2.学术分析学术分析

3.人才评估人才评估

"同舟云学术"是以全球学者为主线,采集、加工和组织学术论文而形成的新型学术文献查询和分析系统,可以对全球学者进行文献检索和人才价值评估。用户可以通过关注某些学科领域的顶尖人物而持续追踪该领域的学科进展和研究前沿。经过近期的数据扩容,当前同舟云学术共收录了国内外主流学术期刊6万余种,收集的期刊论文及会议论文总量共计约1.5亿篇,并以每天添加12000余篇中外论文的速度递增。我们也可以为用户提供个性化、定制化的学者数据。欢迎来电咨询!咨询电话:010-8811{复制后删除}0370

www.globalauthorid.com

TOP

Copyright © 2019-2024 北京同舟云网络信息技术有限公司
京公网安备11010802033243号  京ICP备18003416号-3