Late Quaternary variability of sedimentary nitrogen isotopes in the eastern South Pacific Ocean

We present high-resolution bulk sedimentary δ 15N data from the southern edge of the present-day oxygen minimum zone of the eastern South Pacific. The record is interpreted as representing changes in water column nitrogen removal during the last 70,000 years. We found significant fluctuations in the...

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Bibliographic Details
Published in:Paleoceanography
Main Authors: De Pol-Holz, R., Ulloa, O., Lamy, F., Dezileau, Laurent, Sabatier, Pierre, Hebbeln, D.
Other Authors: Departamento de Oceanografía Concepción, Universidad de Concepción Chile, GeoForschungsZentrum - Helmholtz-Zentrum Potsdam (GFZ), Géosciences Montpellier, Institut national des sciences de l'Univers (INSU - CNRS)-Université de Montpellier (UM)-Université des Antilles (UA)-Centre National de la Recherche Scientifique (CNRS), Fachbereich Geowissenschaften Bremen, Universität Bremen
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2007
Subjects:
eastern-south Pacific
denitrification
ate quaternary
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
[SDE.MCG]Environmental Sciences/Global Changes
[SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
Pacific
Patagonia
Ice Sheet
Online Access:https://hal.archives-ouvertes.fr/hal-00407260
https://hal.archives-ouvertes.fr/hal-00407260/document
https://hal.archives-ouvertes.fr/hal-00407260/file/2006PA001308.pdf
https://doi.org/10.1029/2006PA001308
Description
Summary:We present high-resolution bulk sedimentary δ 15N data from the southern edge of the present-day oxygen minimum zone of the eastern South Pacific. The record is interpreted as representing changes in water column nitrogen removal during the last 70,000 years. We found significant fluctuations in the isotopic signal that suggest major reorganizations of the oxygen minimum zone at millennial timescales. These fluctuations were not related to other millennial-scale changes like the Northern Hemisphere's Dansgaard-Oeschger climate swings or local changes in primary productivity, so appear to be dictated by the Southern Hemisphere's climate rhythm. This is preliminarily corroborated by an overall agreement between our δ 15N data and the sedimentary proxy of ice sheet dynamics in Patagonia, which is in turn correlated with surface water properties at the midlatitude subduction region of the eastern South Pacific intermediate waters. Finally, potential implications on late Quaternary changes in atmospheric CO2 concentrations are discussed.

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