Magnetic signatures of Heinrich-like detrital layers in the Quaternary of the North Atlantic

Channell, J.E.T. and Hodell, D. A. (2013) Magnetic signatures of Heinrich-like detrital layers in the Quaternary of the North Atlantic. Earth and Planetary Science Letters, 369–37. pp. 260-270. ISSN 0012-821X DOI 10.1016/j.epsl.2013.03.034

[img] PDF (This is a RoMEO green journal)
Channell_and_Hodell_-_2013_-_Magnetic_signatures_of_Heinrich-like_detrital_laye.pdf
Restricted to Registered users only

Download (9MB)
[img]
Preview
Image (JPEG)
science.jpeg

Download (608kB) | Preview
Official URL: http://www.sciencedirect.com/science/article/pii/S...

Abstract

Abstract Magnetic parameters are useful for distinguishing North Atlantic Heinrich-like detrital layers from background sediments. Here we compare magnetic properties with XRF scanning data back to 700 ka and 1.3 Ma at IODP Sites U1302–U1303 and U1308, respectively. Multi-domain magnetite, with grain sizes >20 µm, is characteristic of both Ca- and Si-rich detrital layers, as defined by XRF core scanning, confirming the contribution of ice rafting. Reflectance spectra and magnetic parameters distinguish Ca- and Si-rich IRD layers due the presence of high coercivity hematite in Si-rich layers. Heinrich layer 6 (H6) at Site U1302–U1303 is unlike other detrital layers, being marked by a 45-cm thick homogeneous cream-colored clay layer underlain by a thin (5-cm) graded coarse-sand. Comparison of Site U1302/03 and Site U1308 detrital layers implies a dominant Laurentide source for both Ca- and Si-rich detrital layers. At Site U1308, low benthic δ13C values during stadials are in-step with magnetic grain-size coarsening associated with Si-rich detrital layers back to 1.3 Ma, indicating a link between deep-sea ventilation and ice rafting. The surface-sediment tan-colored oxic layer (~2 m thick at Site U1308) yields magnetic hysteresis ratios that are offset from the single-domain to multi-domain (SD–MD) magnetite mixing-line in hysteresis-ratio diagrams. This offset is attributed to maghemite grain-coatings, that form on magnetite in surface sediment, and undergo dissolution as they pass through the oxic/anoxic boundary.

Item Type: Article
Uncontrolled Keywords: 2013AREP, IA66,
Subjects: 01 - Climate Change and Earth-Ocean Atmosphere Systems
Divisions: 01 - Climate Change and Earth-Ocean Atmosphere Systems
Journal or Publication Title: Earth and Planetary Science Letters
Volume: 369–37
Page Range: pp. 260-270
Identification Number: 10.1016/j.epsl.2013.03.034
Depositing User: Sarah Humbert
Date Deposited: 07 Jul 2013 00:49
Last Modified: 08 Aug 2013 12:12
URI: http://eprints.esc.cam.ac.uk/id/eprint/2816

Actions (login required)

View Item View Item

About cookies