The use of foraminifera as a record of the past neodymium isotope composition of seawater
We present new isotopic data for sedimentary planktonic foraminifera, as well as for potential water column and sedimentary sources of neodymium (Nd), which confirm that the isotopic composition of the foraminifera is the same as surface seawater and very different from deep water and sedimentary Nd...
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Veröffentlicht in: | Paleoceanography 2004-06, Vol.19 (2), p.np-n/a |
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Sprache: | eng |
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