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• W2920320535 abstract "Research Article| February 28, 2019 A benthic flux from calcareous sediments results in non-conservative neodymium behavior during lateral transport: A study from the Tasman Sea April N. Abbott April N. Abbott * 1Department of Earth and Planetary Sciences, and Macquarie University Marine Research Centre, Macquarie University, Macquarie Park, New South Wales 2109, Australia *E-mail: april.abbott@mq.edu.au Search for other works by this author on: GSW Google Scholar Author and Article Information April N. Abbott * 1Department of Earth and Planetary Sciences, and Macquarie University Marine Research Centre, Macquarie University, Macquarie Park, New South Wales 2109, Australia *E-mail: april.abbott@mq.edu.au Publisher: Geological Society of America Received: 30 Jul 2018 Revision Received: 01 Feb 2019 Accepted: 06 Feb 2019 First Online: 28 Feb 2019 Online Issn: 1943-2682 Print Issn: 0091-7613 © 2019 Geological Society of America Geology (2019) 47 (4): 363–366. https://doi.org/10.1130/G45904.1 Article history Received: 30 Jul 2018 Revision Received: 01 Feb 2019 Accepted: 06 Feb 2019 First Online: 28 Feb 2019 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation April N. Abbott; A benthic flux from calcareous sediments results in non-conservative neodymium behavior during lateral transport: A study from the Tasman Sea. Geology 2019;; 47 (4): 363–366. doi: https://doi.org/10.1130/G45904.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract The neodymium isotopic (εNd) signature is a widely used proxy in determining changes to ocean currents through Earth’s history. The application of εNd as a proxy of water-mass circulation is based on an assumed quasi-conservative behavior of neodymium isotopes in the ocean. However, our understanding of the factors that govern the oceanic budget of neodymium, including the mechanisms controlling dominant sources and sinks, is not yet complete. Here, I present pore water and water-column neodymium concentration profiles from the western edge of the Tasman Sea to examine the influence of a benthic flux on the northward-flowing Circumpolar Deep Water (CDW). I find that the flux from this region’s calcareous sediments is similar in magnitude to the benthic flux observed in the North Pacific Ocean. In addition, water-column data show a significant increase in the neodymium concentration of the CDW as it moves through the Tasman Sea. Together, these findings indicate that regions with calcareous sediments can account for an important component of the benthic source of neodymium to the oceans. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2920320535 title "A benthic flux from calcareous sediments results in non-conservative neodymium behavior during lateral transport: A study from the Tasman Sea" @default.
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