Book ChapterDOI
Long-lived Isotopic Tracers in Oceanography, Paleoceanography, and Ice-sheet Dynamics
TLDR
The application of strontium, neodymium, and lead isotopes for tracing the sources of continental detritus brought to the oceans by icebergs and implications for the history of the North Atlantic ice sheets is discussed in this article.Abstract:
This chapter focuses on the basis for using authigenic neodymium, lead, and hafnium isotopes in oceanography and paleoceanography. In particular, it reviews in detail the currently available data on neodymium isotopes in the oceans in order to evaluate its strengths and weaknesses as an oceanographic tracer and a proxy to investigate paleocirculation. Neodymium isotope ratios are highlighted because lead isotopes in the present day oceans are contaminated by anthropogenic input, and dissolved hafnium thus far has not been measured. This chapter only gives a cursory summary of the results of studies on Fe–Mn crusts. This chapter also summarizes the application of strontium, neodymium, and lead isotopes for tracing the sources of continental detritus brought to the oceans by icebergs and implications for the history of the North Atlantic ice sheets.read more
Citations
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Journal ArticleDOI
Oceanic mass transport by mesoscale eddies
Zhengguang Zhang,Wei Wang,Bo Qiu +2 more
TL;DR: It is shown that the eddy-induced zonal mass transport can reach a total meridionally integrated value of up to 30 to 40 sverdrups (Sv) (1 Sv = 106 cubic meters per second), and it occurs mainly in subtropical regions, where the background flows are weak.
Journal ArticleDOI
Temporal relationships of carbon cycling and ocean circulation at glacial boundaries.
TL;DR: Evidence from high-sedimentation-rate South Atlantic deep-sea cores indicates that global and Southern Ocean carbon budget shifts preceded thermohaline circulation changes during the last ice age initiation and termination and that these were preceded by ice-sheet growth and retreat, respectively.
Journal ArticleDOI
Synchronous deglacial overturning and water mass source changes.
TL;DR: Comparison of the deep water source record with overturning strength proxies shows how changes in upper-ocean overturning associated with millennial-scale events differ from those associated with whole-Ocean deglacial climate events.
Journal ArticleDOI
Intensification and variability of ocean thermohaline circulation through the last deglaciation
TL;DR: Neodymium isotope ratios in the authigenic ferromanganese oxide component in a southeastern Atlantic core reveal a history of the global overturning circulation intensity through the last deglaciation as mentioned in this paper.
Journal ArticleDOI
Reliable extraction of a deepwater trace metal isotope signal from Fe-Mn oxyhydroxide coatings of marine sediments
Marcus Gutjahr,Martin Frank,Claudine H. Stirling,Veronika Klemm,Tina van de Flierdt,Alex N. Halliday +5 more
TL;DR: In this paper, the isotope compositions of elements such as Sr and Os obtained from the Fe-Mn oxyhydroxide fraction are easily disturbed by detrital contributions originating from the extraction process, whereas the seawater isotope composition of Nd, Pb and Th can be reliably extracted from marine sediments in the North Atlantic.
References
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The continental crust: Its composition and evolution
TL;DR: In this paper, the authors describe the composition of the present upper crust and deal with possible compositions for the total crust and the inferred composition of lower crust, and the question of the uniformity of crustal composition throughout geological time is discussed.
Journal ArticleDOI
Subcommission on geochronology: Convention on the use of decay constants in geo- and cosmochronology
R.H. Steiger,E. Jäger +1 more
TL;DR: The IUGS Subcommission on Geochronology (FOOTNOTE 4) as discussed by the authors recommended the adoption of a standard set of decay constants and isotopic abundances in isotope geology.
Journal ArticleDOI
The composition of the continental crust
TL;DR: In this paper, a new calculation of the crustal composition is based on the proportions of upper crust (UC) to felsic lower crust (FLC) to mafic lower-crust (MLC) of about 1.6:0.4.
Journal ArticleDOI
Nature and composition of the continental crust: A lower crustal perspective
TL;DR: In this article, a three-layer crust consisting of upper, middle, and lower crust is divided into type sections associated with different tectonic provinces, in which P wave velocities increase progressively with depth and there is a large variation in average P wave velocity of the lower crust between different type sections.
Journal ArticleDOI
The Lu-Hf isotope geochemistry of chondrites and the evolution of the mantle-crust system
TL;DR: In this paper, the authors obtained a new set of present-day mean values in chondrites of176Hf/177Hf = 0.282772 ± 29 and176Lu/177 Hf= 0.0332 ± 2.
Related Papers (5)
Neodymium isotopes as a new tool for quantifying exchange fluxes at the continent-ocean interface
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