Abstract

Abstract. The database presented here contains radiogenic neodymium and strontium isotope ratios measured on both terrestrial and marine sediments. The main purpose of this dataset is to help assess sediment provenance and transport processes for various time intervals. This can be achieved by either mapping sediment isotopic signature and/or fingerprinting source areas using statistical tools. The database has been built by incorporating data from the literature and the SedDB database and harmonizing the metadata, especially units and geographical coordinates. The original data were processed in three steps. Firstly, specific attention has been devoted to providing geographical coordinates to each sample in order to be able to map the data. When available, the original geographical coordinates from the reference (generally DMS coordinates) were transferred into the decimal degrees system. When coordinates were not provided, an approximate location was derived from available information in the original publication. Secondly, all samples were assigned a set of standardized criteria that help split the dataset into specific categories. For instance, samples were distinguished according to their location (“Region”, “Sub-region” and “Location” that relate to locations at continental to city or river scale) or the sample type (terrestrial samples – “aerosols”, “soil sediments”, “river sediments”, “rocks” – or marine samples – “marine sediment” or “trap sample”). Finally, samples were distinguished according to their deposition age, which allowed us to compute average values for specific time intervals. Graphical examples illustrating the functionality of the database are presented and the validity of the process was tested by comparing the results with published data. The dataset will be updated bi-annually in order to add more data points to increase the sampling density or provide new types of samples (e.g. seawater signature) and/or integrate additional information regarding the samples. It is publicly available (under CC4.0-BY Licence) from the GFZ data management service at https://doi.org/10.5880/GFZ.4.3.2019.001.

Highlights

  • A large amount of sediments is deposited by rivers and winds on continental margins and in the deeper parts of marine basins

  • Neodymium isotope ratios are generally used to fingerprint provenance changes, as continental rocks have specific Nd isotopic signatures that are preserved during transportation and burial of sediments

  • Strontium isotope ratios are sensitive provenance tracers, but their original signature can be modified by weathering processes in the source area as well as grain-size sorting during sediment transportation

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Summary

Introduction

A large amount of sediments is deposited by rivers and winds on continental margins and in the deeper parts of marine basins. The focus of these studies is different (river runoff and dust characterization respectively), but they are complementary and provide a large number of data (86 and 192 data points respectively). As shown by Cole et al (2009), sedimentary Nd and Sr concentrations can provide valuable clues for paleo-environmental interpretations

Data processing
Literature
Results
Code and data availability
Conclusion and outlook
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