Temporal stability of the neodymium isotope signature of the Holocene to glacial North Atlantic
[1] The neodymium isotopic composition of marine precipitates is increasingly recognized as a powerful tool for identifying changes in ocean circulation and mixing on million year to millennial timescales. Unlike nutrient proxies such as d13C or Cd/Ca, Nd isotopes are not thought to be altered in an...
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| Format: | Text |
| Language: | English |
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| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.557.5447 http://www.whoi.edu/cms/files/vandeFlierdt_Paleo_2006_21689.pdf |