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Limnology and Oceanography : methods 10: (2012) 234-251 (IF 1,535)
GEOTRACES intercalibration of neodymium isotopes and rare earth element concentrations in seawater and suspended particles. Part 1 : reproductibility of results for the international comparison
T. Van De Flierdt 1, K. Pahnke 2, 3, H. Amakawa 4, 5, P. Andersson 6, C. Basak 7, B. Coles 1, C. Colin 8, 9, K. Crocket 1, M. Frank 10, N. Frank 9, S.L. Goldstein 11, 12, V. Goswami 13, B.A. Haley 10, 14, E.C. Hathorne 10, S.R. Hemming 11, 12, G.M. Henderson 15, C. Jeandel 16, K. Jones 11, 12, 17, K. Kreissig 1, F. Lacan 16, M. Lambelet 1, E.E. Martin 7, D.R. Newkirk 7, H. Obata 4, L. Pena 11, A.M. Piotrowski 18, C. Pradoux 16, H.D. Scher 19, 20, H. Schoberg 6, S.K. Singh 13, T. Stichel 2, 10, H. Tazoe 21, D. Vance 22, J.J. Yang 15
(2012)

One of the key activities during the initial phase of the international GEOTRACES program was an extensive international intercalibration effort, to ensure that results for a range of trace elements and isotopes (TEIs) from different cruises and from different laboratories can be compared in a meaningful way. Here we present the results from the intercalibration efforts on neodymium isotopes and rare earth elements in seawater and marine particles. Fifteen different laboratories reported results for dissolved Nd-143/Nd-144 ratios in seawater at three different locations (BATS 15 m, BATS 2000 m, SAFe 3000 m), with an overall agreement within 47 to 57 ppm (2 sigma standard deviation of the mean). A similar agreement was found for analyses of an unknown pure Nd standard solution carried out by 13 laboratories (56 ppm), indicating that mass spectrometry is the main variable in achieving accurate and precise Nd isotope ratios. Overall, this result is very satisfactory, as the achieved precision is a factor of 40 better than the range of Nd isotopic compositions observed in the global ocean. Intercalibration for dissolved rare earth element concentrations (REEs) by six laboratories for two water depths at BATS yielded a reproducibility of 15% or better for all REE except Ce, which seems to be the most blank-sensitive REE. Neodymium concentrations from 12 laboratories show an agreement within 9%, reflecting the best currently possible reproducibility. Results for Nd isotopic compositions and REE concentrations on marine particles are inconclusive, and should be revisited in the future.
1:  Imperial College London
Imperial College London
2:  University of Hawaii
University of Hawaii at Manoa
3:  Carl von Ossietzky
University Oldenburg
4:  Kashiwa Atmosphere & Ocean Res. Institut
University of Tokyo
5:  Taipei Dpt of Geosciences
National University of Taiwan
6:  Swedish Museum
Museum National History
7:  University of Florida
University of Florida
8:  IDES (Université Paris-Sud XI)
CNRS : UMR8148
9:  Laboratoire des Sciences du Climat et de l'Environnement [Gif-sur-Yvette] (LSCE)
CNRS : UMR8212 – CEA : DSM/LSCE – Université de Versailles Saint-Quentin-en-Yvelines
10:  IFM GEOMAR
University Kiel
11:  Lamont Doherty Earth Observatory
Columbia University
12:  Dpt Earth & Environm. Sciences
Columbia University
13:  Ahmadabad Geosceinces Division
Physic Research Laboratory
14:  OSU
COAS
15:  Department of Earth Sciences
University of Oxford
16:  Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS)
CNRS : UMR5566 – Institut de recherche pour le développement [IRD] – CNES – Observatoire Midi-Pyrénées – INSU – Université Paul Sabatier [UPS] - Toulouse III
17:  Exxon Mobil
Mobil Production Co
18:  Godwin Lab. Palaeoclimate Research
University of Cambridge
19:  Columbia Dpt Earth & Ocean Science
University of South Carolina
20:  Columbia Marine Science Program
University of South Carolina
21:  Hirosaki Dpt Radiation Chem.
Hirosaki University
22:  School of Earth Sciences
University of Bristol
GEOMAR
Sciences of the Universe/Earth Sciences