10.5880/GFZ.4.3.2021.004 eng dataset GFZ German Research Centre for Geosciences datapub@gfz-potsdam.de http://www.gfz-potsdam.de Helmholtz-Centre Potsdam - GFZ German Research Centre for Geosciences Helmholtz-Centre Potsdam - GFZ German Research Centre for Geosciences pointOfContact 2021-06-25 urn:ogc:def:crs:EPSG:4326 A global database of radiogenic Nd and Sr isotopes in marine and terrestrial samples (V. 3.0) 2021-06-25 revision 2018-08 creation doi:10.5880/GFZ.4.3.2021.004 Blanchet, Cécile L. GFZ German Research Centre for Geosciences, Potsdam, Germany author GFZ Data Services publisher The database presented here contains radiogenic neodymium and strontium isotope ratios measured on both terrestrial and marine sediments. It was compiled to help assessing 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 (e.g. Blanchet, 2018b, 2018a). The database has been built by incorporating data from the literature and various databases and data compilations, and harmonizing the metadata, especially units and geographical coordinates. The original data were processed in three steps. Firstly, a specific attention has been devoted to provide 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, with different precision standard) 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 splitting the dataset in specific categories. We defined categories associated with the sample location, the type of sample, the sedimentary fraction measured, or the deposition age (as given in the original publication). This dataset consists of one spreadsheet: "Dataset_Nd_Sr_isotopes_V3.txt", which contains the assembled dataset of marine and terrestrial Nd and/or Sr concentration and isotopes, together with sorting criteria and geographical locations. A full reference list is provided in the file “References_Database_Nd_Sr_isotopes_V3.pdf”. R code for mapping the data and running statistical analyses is also available for this dataset (Blanchet, 2018b, 2018a). Blanchet, Cécile L. GFZ German Research Centre for Geosciences, Potsdam, Germany cecile.blanchet@gfz-potsdam.de pointOfContact Neodymium radioisotopes Strontium radioisotopes Mapping tool EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > EROSION EARTH SCIENCE > LAND SURFACE > EROSION/SEDIMENTATION > SEDIMENT TRANSPORT EARTH SCIENCE > PALEOCLIMATE > LAND RECORDS > SEDIMENTS EARTH SCIENCE > PALEOCLIMATE > OCEAN/LAKE RECORDS > ISOTOPES EARTH SCIENCE > PALEOCLIMATE > PALEOCLIMATE RECONSTRUCTIONS > DROUGHT/PRECIPITATION RECONSTRUCTION EARTH SCIENCE > SOLID EARTH > GEOCHEMISTRY > GEOCHEMICAL PROPERTIES > ISOTOPE RATIOS EARTH SCIENCE SERVICES > DATA ANALYSIS AND VISUALIZATION > STATISTICAL APPLICATIONS NASA/GCMD Earth Science Keywords publication CC BY 4.0 CC BY 4.0 10.5194/essd-11-741-2019 DOI IsSupplementTo 10.5880/GFZ.4.3.2019.001 DOI IsNewVersionOf 10.5880/GFZ.5.2.2018.001 DOI IsNewVersionOf 10.6084/m9.figshare.6990161.v3 DOI IsSupplementedBy 10.6084/m9.figshare.6990260.v3 DOI IsSupplementedBy 10.1016/j.gca.2015.01.010 DOI IsDerivedFrom 10.1130/G37114.1 DOI IsDerivedFrom 10.1016/j.epsl.2016.06.001 DOI IsDerivedFrom 10.1016/j.epsl.2013.08.028 DOI IsDerivedFrom 10.1144/GSL.SP.2005.246.01.04 DOI IsDerivedFrom 10.1130/0091-7613(2001)029%3C0531:LMAANE%3E2.0.CO;2 DOI IsDerivedFrom 10.1029/2005GL024519 DOI IsDerivedFrom 10.1016/S1251-8050(00)00217-2 DOI IsDerivedFrom 10.1002/2014GC005586 DOI IsDerivedFrom 10.1016/0012-821X(81)90210-7 DOI IsDerivedFrom 10.1016/0009-2541(96)00028-9 DOI IsDerivedFrom 10.1038/nature06586 DOI IsDerivedFrom http://www-odp.tamu.edu/publications/citations/joides_j/joides_j_28_1.pdf URL IsDerivedFrom 10.1016/0012-821X(95)00048-H DOI IsDerivedFrom 10.1016/j.dsr2.2011.12.004 DOI IsDerivedFrom 10.1002/2014GC005462 DOI IsDerivedFrom 10.1016/0016-7037(96)00105-6 DOI IsDerivedFrom 10.1007/s00531-011-0708-5 DOI IsDerivedFrom 10.1126/science.aao2473 DOI IsDerivedFrom 10.1016/S0012-821X(96)00255-5 DOI IsDerivedFrom 10.1038/srep44231 DOI IsDerivedFrom 10.1016/S0009-2541(01)00416-8 DOI IsDerivedFrom 10.1029/2002GC000371 DOI IsDerivedFrom 10.1016/j.epsl.2004.05.033 DOI IsDerivedFrom 10.1016/j.epsl.2008.10.028 DOI IsDerivedFrom 10.1016/j.epsl.2011.10.008 DOI IsDerivedFrom 10.1126/science.1215400 DOI IsDerivedFrom 10.1016/j.gca.2015.08.001 DOI IsDerivedFrom 10.1144/SP293.12 DOI IsDerivedFrom 10.1016/0012-821X(89)90079-4 DOI IsDerivedFrom 10.1016/j.quascirev.2018.04.032 DOI IsDerivedFrom 10.1016/S0012-821X(98)00132-0 DOI IsDerivedFrom 10.1029/97JC01249 DOI IsDerivedFrom 10.1007/BF00306478 DOI IsDerivedFrom 10.1371/journal.pone.0115958 DOI IsDerivedFrom 10.1038/s41561-020-00671-3 DOI IsDerivedFrom 10.1016/j.chemgeo.2016.06.024 DOI IsDerivedFrom 10.1130/0091-7613(1994)022%3C0307:LAAAAA%3E2.3.CO;2 DOI IsDerivedFrom 10.2475/ajs.287.2.127 DOI IsDerivedFrom 10.1016/j.epsl.2010.01.006 DOI IsDerivedFrom 10.1016/S0024-4937(96)00026-6 DOI IsDerivedFrom 10.1016/j.quascirev.2010.12.005 DOI IsDerivedFrom 10.1007/s004100050353 DOI IsDerivedFrom 10.1016/S0012-821X(00)00011-X DOI IsDerivedFrom 10.1016/j.gca.2011.11.034 DOI IsDerivedFrom 10.1016/j.epsl.2015.12.014 DOI IsDerivedFrom 10.1016/j.margeo.2007.09.003 DOI IsDerivedFrom https://oceanrep.geomar.de/23151/ URL IsDerivedFrom 10.1016/j.gca.2007.04.033 DOI IsDerivedFrom 10.1016/j.epsl.2012.08.012 DOI IsDerivedFrom 10.1016/S0012-821X(02)00620-9 DOI IsDerivedFrom 10.1016/j.epsl.2014.11.029 DOI IsDerivedFrom 10.1016/j.epsl.2008.12.011 DOI IsDerivedFrom 10.1016/S0012-821X(99)00184-3 DOI IsDerivedFrom 10.1016/j.quascirev.2010.05.012 DOI IsDerivedFrom 10.1126/science.1204673 DOI IsDerivedFrom 10.1038/ngeo1889 DOI IsDerivedFrom 10.1139/e99-008 DOI IsDerivedFrom 10.1130/0091-7613(2000)28%3C379:CCATCO%3E2.0.CO;2 DOI IsDerivedFrom 10.1016/S0040-1951(99)00033-5 DOI IsDerivedFrom 10.1016/0016-7037(69)90153-7 DOI IsDerivedFrom 10.1016/0012-821X(85)90045-7 DOI IsDerivedFrom 10.1016/j.margeo.2007.11.007 DOI IsDerivedFrom 10.1071/EN04029 DOI IsDerivedFrom 10.1029/93JB02576 DOI IsDerivedFrom 10.1038/298614a0 DOI IsDerivedFrom 10.1016/0025-3227(92)90025-D DOI IsDerivedFrom 10.1016/0012-821X(90)90089-G DOI IsDerivedFrom 10.1016/j.gca.2016.08.005 DOI IsDerivedFrom 10.1038/s41561-018-0205-6 DOI IsDerivedFrom 10.1016/j.quascirev.2020.106396 DOI IsDerivedFrom 10.1029/2011GC003544 DOI IsDerivedFrom 10.1016/j.quascirev.2013.04.013 DOI IsDerivedFrom 10.1016/S0264-8172(98)00023-3 DOI IsDerivedFrom 10.1016/S0016-7037(02)00868-2 DOI IsDerivedFrom 10.1016/j.margeo.2006.08.006 DOI IsDerivedFrom 10.1029/2011PA002168 DOI IsDerivedFrom 10.1029/2003PA000993 DOI IsDerivedFrom 10.1016/S0012-821X(03)00068-2 DOI IsDerivedFrom 10.1016/j.epsl.2006.06.044 DOI IsDerivedFrom 10.1029/JB093iB05p04933 DOI IsDerivedFrom 10.1017/S0954102005002877 DOI IsDerivedFrom 10.1016/j.epsl.2006.07.002 DOI IsDerivedFrom 10.1029/2008PA001706 DOI IsDerivedFrom 10.1016/0012-821X(96)00150-1 DOI IsDerivedFrom 10.1016/S0025-3227(01)00123-2, 2001. 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