CaltechAUTHORS
  A Caltech Library Service

Sm-Nd in marine carbonates and phosphates: Implications for Nd isotopes in seawater and crustal ages

Shaw, H. F. and Wasserburg, G. J. (1985) Sm-Nd in marine carbonates and phosphates: Implications for Nd isotopes in seawater and crustal ages. Geochimica et Cosmochimica Acta, 49 (2). pp. 503-518. ISSN 0016-7037. http://resolver.caltech.edu/CaltechAUTHORS:20131029-140440003

Full text is not posted in this repository. Consult Related URLs below.

Use this Persistent URL to link to this item: http://resolver.caltech.edu/CaltechAUTHORS:20131029-140440003

Abstract

This study explores the possibility of establishing Nd isotopic variations in seawater over geologic time. Calcite, aragonite and apatite are examined as possible phases recording seawater values of ϵ_(Nd). Modern, biogenic and inorganically precipitated calcite and aragonite from marine environments were found to have Nd concentrations of from 0.2 to 70 ppb, showing that primary marine CaCO_3 contains little REE and that Nd/Ca is not greatly enhanced relative to seawater during carbonate precipitation. Very young marine limestone and dolomite containing no continental detritus have ~200 ppb Nd. All the carbonates are LREE enriched (-0.16≤ƒ^(Sm/Nd) ≤-0.45). Modern and very young Atlantic and Pacific carbonates have ϵ_(Nd) in the range of shallow Atlantic and Pacific seawater respectively, implying that they derive their REE from local seawater. The Nd in well preserved carbonate fossils is ≤4 × 10^4 ppb, much greater than in their modern counterparts but like the high values found for carbonates in other studies. We believe the high REE contents (at the 500 ppb level) in some detritusfree carbonates are due to REE-rich Fe-hydroxide in/on the carbonate. In favorable cases, such material may record seawater ϵ_(Nd) values, however introduction of extraneous REE may obscure the original isotopic composition of pure CaCO_3 because of its very low intrinsic primary REE abundance. Modern biogenic apatite is also shown to have very low REE content (<150 ppb Nd) but appears to quickly scavenge REE from seawater. Inorganically precipitated apatite from phosphorites has high concentrations of seawater-derived REE. Young phosphorite apatite from the Atlantic and Pacific oceans has ϵ_(Nd) in the range of the seawater from these oceans. Older apatite samples of similar age from different localities bordering common oceans record similar values of ϵ_(Nd)(T). Sedimentary apatite has ϵ_(Sr)(T) values in good agreement with the curves for ^(87)Sr/^(86)Sr of seawater as a function of time. Individual conodonts from a single formation yield the same ϵ_(Sr)(T) and ϵ_(Nd)(T). Other workers have shown that sedimentary apatite preserves seawater REE patterns. These characteristics suggest that sedimentary apatite can be used to determine ϵ_(Nd)(T) in ancient seawater. The seawater values so inferred range between −1.7 and −8.9 over the last 700 my and lie in the range of modern seawater, showing no evidence for drastic changes. High values of seawater ϵ_(Nd)(T) in the Triassic and latest Precambrian may correlate with the breakup of large continental landmasses. The initial ϵ_(Nd)(T) =−15.0 of a 2 AE old phosphorite implies the presence of ~ 1.5 AE old continental crust at 2 AE ago. The approach outlined here can be used to constrain the age of the exposed crust as a function of time.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1016/0016-7037(85)90042-0DOIArticle
http://www.sciencedirect.com/science/article/pii/0016703785900420PublisherArticle
Additional Information:© 1985 Pergamon Press Ltd. Received June l, 1984; accepted in revised form November 1, 1984. We would like to thank the following people for both providing samples for this work and sharing their expertise with us: A. Altschuler. M. Cooper, R. Ginsburg, Y. Kolodny, H. Lowenstam, G. McOellan and P. Swart. We are indebted to J. Wright and W. Holzer for introducing us to conodonts and providing us with samples. INAA analyses of samples FID 4, 6 were graciously provided by R. A. Schmitt. D. Papanastassiou generously shared his knowledge of mass spectrometry and D. Piepgras his knowledge of Nd isotopes in seawater. This paper benefited from reviews by A. L. Aplin, F. Albarede, H. Elderfield, M. R. Palmer, R. A. Schmitt, P. Swart, K. K. Turekian and one anonymous reviewer. General paleontological pedagogy was given by the Lundelii. This work was supported in part by National Science Foundation Grant PHY82-15500 and the support for maintaining a functioning laboratory came from the National Aeronautics and Space Administration Grant# NAG9-43. Editorial handling: H. Elderfield
Funders:
Funding AgencyGrant Number
NSFPHY82-15500
NASANAG9-43
Other Numbering System:
Other Numbering System NameOther Numbering System ID
Caltech Division of Geological and Planetary Sciences4049
Lunatic Asylum Lab471
Record Number:CaltechAUTHORS:20131029-140440003
Persistent URL:http://resolver.caltech.edu/CaltechAUTHORS:20131029-140440003
Official Citation:H.F Shaw, G.J Wasserburg, Sm-Nd in marine carbonates and phosphates: Implications for Nd isotopes in seawater and crustal ages, Geochimica et Cosmochimica Acta, Volume 49, Issue 2, February 1985, Pages 503-518, ISSN 0016-7037, http://dx.doi.org/10.1016/0016-7037(85)90042-0. (http://www.sciencedirect.com/science/article/pii/0016703785900420)
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:42116
Collection:CaltechAUTHORS
Deposited By: Ruth Sustaita
Deposited On:29 Oct 2013 21:28
Last Modified:29 Oct 2013 21:28

Repository Staff Only: item control page