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Bottoms up: Sedimentary control of the deep North Pacific Ocean’s ε[subscript Nd] signature

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Title Bottoms up: Sedimentary control of the deep North Pacific Ocean’s ε[subscript Nd] signature
Names Abbott, April N. (creator)
Haley, Brian A. (creator)
McManus, James (creator)
Date Issued 2015-11 (iso8601)
Note This is an author's peer-reviewed final manuscript, as accepted by the publisher. The published article is copyrighted by the Geological Society of America and can be found at: http://geology.gsapubs.org/
Abstract The ability to reconstruct past ocean currents is essential for determining ocean
circulation’s role in global heat transport and climate change. Our understanding of the
relationship between circulation and climate in the past allows us to predict the impact of
future climate-driven circulation changes. One proposed tracer of past ocean circulation
is the neodymium isotope composition (ε[subscript Nd]) of ancient water masses. However,
ambiguities in what governs the ε[subscript Nd] distribution in the modern ocean hamper
interpretations of this tracer. Here we present ε[subscript Nd] values for marine pore fluids,
sediments, and the overlying water column for three sites in the North Pacific. We find
that ocean bottom water ε[subscript Nd] (ε[subscript Nd subscript BW]) in the Northeast Pacific lies between the value expected for the water mass (-3.3) and the measured ε[subscript Nd] of sediment pore fluid (ε[subscript Nd subscript PW]; - 1.8). Moreover, ε[subscript Nd subscript PW] resembles the ε[subscript Nd] of the sediment. Combined, these findings are consistent with recent assessments that sediment pore fluids may be a major source of rare earth elements to the ocean, and suggest that the benthic flux of neodymium from
pore fluids exerts the primary control over the deep ocean distribution of ε[subscript Nd].
Genre Article
Identifier Abbott, A. N., Haley, B. A., & McManus, J. (2015). Bottoms up: Sedimentary control of the deep North Pacific Ocean’s εNd signature. Geology, 43(11), 1035-1038. doi:10.1130/G37114.1

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