PANGAEA_912109 Table S6. Past Himalayan erosion from Bengal Fan: Sr-Nd and 10Be data from river sediment used for the fG and K(t) computation Lenard, Sebastien Jean Paul; Lavé, Jérôme; France-Lanord, Christian; Aumaître, Georges; Bourlès, Didier L; Keddadouche, Karim Table S6. Past Himalayan erosion from Bengal Fan: Sr-Nd and 10Be data from river sediment used for the fG and K(t) computation 2020-02-14 PANGAEA Dataset https://doi.pangaea.de/10.1594/PANGAEA.912109 Investigator Sebastien Jean Paul Lenard sebastien.lenard@gmail.com Earth Science Event label River Location ε-Neodymium ε-Neodymium, uncertainty Neodymium Neodymium, uncertainty Strontium-87/Strontium-86 ratio Strontium-87/Strontium-86 ratio, uncertainty Strontium Strontium, uncertainty Area Beryllium-10, production rate per year Beryllium-10 Beryllium-10, uncertainty Erosion rate Erosion rate, uncertainty geoscientificInformation 10Be Bangladesh Bengal Fan Cenozoic climate cosmogenic nuclides erosion Ganga_Harding_bridge glaciations Himalaya India Indian Ocean Indo-Burman range Lower Meghna Namche Barwa Nd Pleistocene provenance study Quaternary Sediment Shillong Sr turbidites Complete 24.0529 24.0529 89.02465 89.02465 IODP Integrated Ocean Drilling Program / International Ocean Discovery Program unrestricted CC-BY-NC-SA-4.0: Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International English PANGAEA Data Publisher for Earth & Environmental Science https://www.pangaea.de/ Data Center Contact Michael Diepenbroek info@pangaea.de

Leobener Str.

Bremen Bremen 28359 Germany online 76 data points text/tab-separated-values Lenard, Sebastien Jean Paul; Lavé, Jérôme; France-Lanord, Christian; Aumaître, Georges; Bourlès, Didier L; Keddadouche, Karim (2020): Steady erosion rates in the Himalayas through late Cenozoic climatic changes. Nature Geoscience, 13(6), 448-452, https://doi.org/10.1038/s41561-020-0585-2

Bulk silicate Sr-Nd data, extracted from bank and bedload, are from Galy and France-Lanord (2001) (URI:https://doi.org/10.1130/0091-7613(2001)029<0023:HERITH>2.0.CO;2), Singh and France-Lanord (2002) (URI:https://doi.org/10.1016/S0012-821X(02)00822-1), Singh et al. (2008) (URI:https://doi.org/10.1029/2007JF000909). 10Be data are averaged from Lupker et al. (2012, 2017) (URI:https://doi.org/10.1016/j.epsl.2012.04.020) (URI:https://doi.org/10.5194/esurf-5-429-2017). The production rates were computed using Basinga (Charreau et al., 2019) (URI:https://doi.org/10.1002/esp.4649) with the Lal-Stone / ERA40 atmosphere configuration using a sea-level high latitude production rate of 4.18 atom/g/y (Martin et al., 2017) (URI:https://doi.org/10.1016/j.quageo.2016.11.006), factors for different particle production rates of 0.9886 for spallation, 0.0027 for slow muons, 0.0087 for fast muons and attenuation lengths of 260 g/cm2 for slow muons and 510 g/cm2 for fast muons (Braucher et al., 2011) (URI:https://doi.org/10.1016/j.epsl.2011.06.036), and the basins defined in the Methods of the article associated to the dataset. ** For all details see the full metadata description at "https://doi.pangaea.de/10.1594/PANGAEA.912109"!

https://doi.org/10.1038/s41561-020-0585-2 Steady erosion rates in the Himalayas through late Cenozoic climatic changes https://www.iodp.org/ IODP DIF 9.4 2020-02-14 2026-04-30