Advection and scavenging controls of Pa/Th in the northern NE Atlantic

Roberts, Natalie L. and McManus, Jerry F. and Piotrowski, Alexander M. and McCave, I. Nicholas (2014) Advection and scavenging controls of Pa/Th in the northern NE Atlantic. Paleoceanography, 29 (6). 2014PA002633. ISSN 0883-8305 DOI https://doi.org/10.1002/2014PA002633

[img]
Preview
Text
NR.pdf - Published Version

Download (2MB) | Preview
[img] Text
Readme.docx - Supplemental Material

Download (48kB)
[img]
Preview
Text
Fig_S1.pdf - Supplemental Material

Download (323kB) | Preview
[img]
Preview
Text
Fig_S2.pdf - Supplemental Material

Download (121kB) | Preview
[img] Text
Table_S1.xlsx - Supplemental Material

Download (55kB)
[img] Text
Table_S2.xlsx - Supplemental Material

Download (77kB)
[img]
Preview
Image
palo20117-fig-0001.png - Published Version

Download (99kB) | Preview
Official URL: http://onlinelibrary.wiley.com/doi/10.1002/2014PA0...

Abstract

Over the last 2 decades, significant advances have been made in reconstructing past rates of ocean circulation using sedimentary proxies for the dynamics of abyssal waters. In this study we combine the use of two rate proxies, sortable silt grain size, and sedimentary 231Pa/230Th, measured on a depth transect of deep-sea sediment cores from the northern NE Atlantic, to investigate ocean circulation changes during the last deglacial. We find that at two deep sites, the core-top 231Pa/230Th ratios reflect Holocene circulation rates, while during Heinrich Stadial 1, the deglacial ratios peaked as the sortable silt grain size decreased, reflecting a general circulation slowdown. However, the peak 231Pa/230Th significantly exceeded the production ratio in both cores, indicating that 231Pa/230Th was only partially controlled by ocean circulation at these sites. This is supported by a record of 231Pa/230Th from an intermediate water depth site, where values also peaked during Heinrich Stadial 1, but were consistently above the production ratio over the last 24 ka, reflecting high scavenging below productive surface waters. At our study sites, we find that preserved sediment component fluxes cannot be used to distinguish between a scavenging or circulation control, although they are consistent with a circulation influence, since the core at intermediate depth with the highest 231Pa/230Th recorded the lowest particle fluxes. Reconstruction of advection rate using 231Pa/230Th in this region is complicated by high productivity, but the data nevertheless contain important information on past deep ocean circulation.

Item Type: Article
Uncontrolled Keywords: 2014AREP; IA68;
Subjects: 01 - Climate Change and Earth-Ocean Atmosphere Systems
Divisions: 01 - Climate Change and Earth-Ocean Atmosphere Systems
08 - Green Open Access
Journal or Publication Title: Paleoceanography
Volume: 29
Page Range: 2014PA002633
Identification Number: https://doi.org/10.1002/2014PA002633
Depositing User: Sarah Humbert
Date Deposited: 25 Aug 2014 22:25
Last Modified: 31 Dec 2014 01:00
URI: http://eprints.esc.cam.ac.uk/id/eprint/3095

Actions (login required)

View Item View Item

About cookies