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Table S5. Past Himalayan erosion from Bengal Fan: Chemical analyses of river ...
Ganga, Brahmaputra and Lower Meghna sample data are presented. Al/Si and Fe/Si ratios are from Lupker et al. (2013) (URI:https://doi.org/10.1016/j.epsl.2013.01.038) and Sr... -
Table S4. Past Himalayan erosion from Bengal Fan: Major and trace element res...
For the Bengal Fan samples, the measurements of major and trace elements were performed at SARM (Nancy, France), following (Carignan et al., 2001)... -
Landmark configurations for gastropod shells of Abeskunus and Zagrabica
The dataset includes the (semi)landmark configurations for 41 specimens of the brackish-water gastropod genera Abeskunus and Zagrabica from Miocene to Holocene deposits of... -
Global mean CO2, temperature and sea level data from transient model simulati...
Variations in Earth's orbit pace the glacial-interglacial cycles of the Quaternary, but the mechanisms that transform regional and seasonal variations in solar insolation into... -
Age versus two relative paleointensity proxies (slopes of NRM/ARM and NRM/IRM...
Two relative paleointensity (RPI) proxies (slopes of NRM/ARM and NRM/IRM) from u-channel samples from Core MD07-3077. The RPI proxies were determined from stepwise alternating... -
Age versus two relative paleointensity proxies (slopes of NRM/ARM and NRM/IRM...
Two relative paleointensity (RPI) proxies (slopes of NRM/ARM and NRM/IRM) for u-channel samples from Core MD07-3076. The RPI proxies were determined from stepwise alternating... -
Age versus component declination and inclination of natural remanent magnetiz...
Component declination and inclination, determined from stepwise alternating field demagnetization data recording the Laschamp excursion from discrete (2x2 cm²) samples from Core... -
Age versus component declination and inclination of natural remanent magnetiz...
Component declination and inclination, determined from stepwise alternating field demagnetization data recording the Laschamp excursion from u-channel samples from Core... -
Age versus component declination and inclination of natural remanent magnetiz...
Component declination and inclination, determined from stepwise alternating field demagnetization data recording the Iceland Basin excursion from u-channel samples from Core... -
Age versus component declination and inclination of natural remanent magnetiz...
Component declination and inclination, determined from stepwise alternating field demagnetization data recording the Iceland Basin excursion from discrete (2x2 cm²) samples from... -
Paleomagnetic and rock magnetic data from sedimentary core collected at high ...
This dataset includes paleomagnetic and rock magnetic analyses from four sediment cores collected on continental slope of Storfjorden (EG-02, EG-03, SV-04) and Kveithola... -
Data from marine sediment cores PAMELA-MOZ1-KS04 and PAMELA-MOZ1-KS07
Over the past ten years, a huge amount of source-to-sink studies have aimed to unravel the tectonic, climatic and other processes that shape the landscape from mountains to the... -
Data from marine sediment core MOZ4-CS09
A 27-meter core collected on the seafloor (1909 meters depth) near Juan de Nova island preserves a high-resolution record of carbonate export to the deep sea over the past 1...