Origin of Abyssal NW Atlantic Water Masses Since the Last Glacial Maximum

Pöppelmeier, F., Gutjahr, Marcus, Blaser, P., Keigwin, L. D. and Lippold, J. (2018) Origin of Abyssal NW Atlantic Water Masses Since the Last Glacial Maximum Paleoceanography and Paleoclimatology, 33 (5). pp. 530-543. DOI 10.1029/2017PA003290.

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Supplementary data:


The notion of a shallow northern sourced intermediate water mass is a well evidenced feature of the Atlantic circulation scheme of the Last Glacial Maximum (LGM). However, recent observations from stable carbon isotopes (δ13C) at the Corner Rise in the deep northwest Atlantic suggested a significant contribution of a Northern Component Water mass to the abyssal northwest Atlantic basin that has not been described before. Here we test the hypothesis of this northern sourced water mass underlying the southern sourced glacial Antarctic Bottom Water by measuring the authigenic neodymium (Nd) isotopic composition from the same sediments from 5,010-m water depth. Neodymium isotopes act as a semiconservative water mass tracer capable of distinguishing between Northern and Southern Component Waters at the northwest Atlantic. Our new Nd isotopic record resolves various water mass changes from the LGM to the early Holocene in agreement with existing Nd-based reconstructions from across the west Atlantic Ocean. Especially pronounced are the Younger Dryas and Bølling-Allerød with unprecedented changes in the Nd isotopic composition. For the LGM we found Nd isotopic evidence for a northern sourced water mass contributing to abyssal depths, thus being in agreement with previous δ13C data from Corner Rise. Overall, however, the deep northwest Atlantic was still dominated by southern sourced water, since we found signatures that are intermediate between northern and southern end member compositions. Furthermore, this new record indicates that C and Nd isotopes were partly decoupled, pointing to nonconservative behavior of one or more likely of both water mass proxies during the LGM.

Document Type: Article
Additional Information: Data from this studycan be found in the supporting information (Tables S2–S5) and on Pangaea (www. pangaea.de).
Keywords: Last Glacial Maximum, neodymium isotopes, stable carbon isotopes, abyssal water masses
Research affiliation: OceanRep > GEOMAR > FB2 Marine Biogeochemistry > FB2-MG Marine Geosystems
Woods Hole
Refereed: Yes
DOI etc.: 10.1029/2017PA003290
ISSN: 2572-4517
Projects: IODP, Emmy Noether Program
Date Deposited: 18 Jun 2018 10:25
Last Modified: 18 Jun 2018 10:28
URI: http://eprints.uni-kiel.de/id/eprint/43424

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