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| Created: | Sep 28, 2026 at 3:12 a.m. (UTC) | |
| Last updated: | Sep 29, 2026 at 5:33 a.m. (UTC) | |
| Citation: | See how to cite this resource | |
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Abstract
This resource contains soil and river-sediment branched glycerol dialkyl glycerol tetraether (brGDGT) measurements and air and soil temperature records from the central Nepal Himalaya. The brGDGT dataset includes 56 soil samples collected from depths of 0–200 cm and 15 river-sediment samples collected between 2015 and 2024. The sediment samples comprise seven post-Gorkha riverbed deposits, seven deposits associated with the 2021 Melamchi flood, and one non-flood riverbed deposit from Yangri Khola. Reported variables include sampling location and elevation, sample depth and classification, individual GDGT peak areas and concentrations, total organic carbon, MBT′₅Me, and BIT index values. The resource also includes 35 air and soil temperature logger series from 10 monitoring sites spanning 772–4,300 m elevation in the Melamchi Valley. Temperature records cover October 2022 through May 2026 and are provided together with daily, monthly, and annual summaries. Depth-stratified MBT′₅Me–elevation calibration statistics, sample-level residuals, metadata, data dictionaries, quality-control information, and reproducible processing scripts are included. These data support evaluation of how soil-derived biomarker signals record sediment source elevations following earthquake-triggered landsliding and extreme flooding in mountain catchments.
Subject Keywords
Coverage
Spatial
Temporal
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Content
README.md
Nepal-FRES: GDGT and temperature data
This data package accompanies the study of branched glycerol dialkyl glycerol tetraether (brGDGT) source-elevation signals after the 2015 Gorkha earthquake and the 2021 Melamchi flood in the Nepal Himalaya.
HydroShare resource: https://www.hydroshare.org/resource/66ebdb06fcb24d27b5c51426921324a0
Suggested citation: Chen, C.-M., Peterse, F., West, A. J., Yedema, Y. W., Li, G. K., Chamlagain, D., & Feakins, S. J. (2026). Nepal-FRES: GDGT and Temperature Data. HydroShare. http://www.hydroshare.org/resource/66ebdb06fcb24d27b5c51426921324a0
Contents
data/gdgt/sample_measurements.csv: sample location, type, depth, TOC, GDGT totals, MBT′₅Me, BIT, and analysis groups for 56 soil and 15 sediment samples.data/gdgt/compound_concentrations.csv: compound-level concentrations normalized to extracted dry mass.data/gdgt/compound_peak_areas.csv: integrated peak areas, including C46 internal standard. These are not raw chromatograms.data/gdgt/laboratory_quantification_metadata.csv: extracted dry mass, split factor, and internal-standard information used for quantification.data/gdgt/calibration_summary_melamchi.csvandcalibration_residuals_melamchi.csv: depth-specific Melamchi MBT′₅Me–elevation regression statistics and sample residuals.data/temperature/logger_exports/: 35 air and soil temperature series from 10 monitoring stations.data/temperature/summaries/: daily, monthly, annual, and elevation-gradient summaries.data/figure3/: regional Figure 3 calibration data, regression statistics, residuals, and inferred sediment source elevations.metadata/: field definitions.code/: scripts used to prepare temperature summaries and reproduce the regression tables.
GDGT data
Sample identifiers are the join key among GDGT tables. Soil depth groups are surface (0–4 cm), shallow (5–49 cm), and deep (50–200 cm). Sediment groups distinguish 2015 deposits, 2021 flood deposits, and the non-flood Yangri Khola sample NP22-12.
The analytical split was made before internal-standard addition. The internal-standard amount records the amount added to the analyzed aliquot (152 ng where recorded), while dry-mass normalization uses the mass of the extracted sample. total_gdgt_ng_g_dry equals the sum of iso- and branched-GDGT totals. Compound-level missing values are blank.
Temperature data
Timestamps are Nepal Standard Time (UTC+05:45). Records are converted to equal-weight hourly means; daily means require at least six valid hourly observations. Monthly and annual summaries weight retained daily means by available hours. Partial-year coverage fields must be considered when interpreting annual means. The 772 m station includes an air logger and a 10 cm soil logger; NP23-11 is the corresponding 10 cm GDGT soil sample, but no surface-soil sample is available at this station.
Coordinates and elevations are reported as supplied with the field records; horizontal and vertical datum metadata are not available. No additional temperature outlier filter or instrument-calibration correction was imposed.
Figure 3 analysis
Regional calibrations use eligible soil observations east or west of 85°E and fit the three soil-depth groups separately. Source-elevation estimates use 5,000 paired bootstrap refits and calibration-residual draws to calculate 95% predictive intervals. Western surface soils contain only two observations at one elevation and therefore do not support a regression or source-elevation estimate.
The Figure 3 regional compilation includes measurements from this study and the following open datasets:
- Märki, L. (2020). Data for: Molecular Tracing of Riverine Soil Organic Matter From the Central Himalaya. ETH Zurich Research Collection. https://doi.org/10.3929/ethz-b-000431464 (CC BY 4.0).
- van der Veen, I. (2020). Research data to: Validation and calibration of soil δ2H and brGDGTs along (E–W) and strike (N–S) of the Himalayan climatic gradient. Mendeley Data, version 1. https://doi.org/10.17632/cvdnf723k5.1 (CC BY 4.0).
Reused records retain source attribution in the data tables. Modifications consist of field standardization, geographic/depth grouping, regression, and inverse source-elevation calculations.
License
Original data, metadata, and code produced by this study are released under the Creative Commons Attribution 4.0 International license (CC BY 4.0): https://creativecommons.org/licenses/by/4.0/. Reuse requires appropriate attribution and an indication of modifications. Third-party records from Märki (2020) and van der Veen (2020) retain their original CC BY 4.0 attribution and source citations.
Reproduction
Install the versions in code/requirements.txt, then run:
text
python code/prepare_temperature_station_summaries.py
python code/analyze_temperature_lapse_rate.py
python code/recompute_melamchi_calibration.py
python code/recompute_figure3.py
The Excel workbook is a formatted snapshot; the accompanying CSV files are the machine-readable analysis tables.
Credits
Funding Agencies
This resource was created using funding from the following sources:
| Agency Name | Award Title | Award Number |
|---|---|---|
| U.S. National Science Foundation | NSFGEO-NERC Collaborative Research: Coupling Erosion, Weathering, and Hydrologic Function in an Active Orogenic System | 2021619 |
Contributors
People or Organizations that contributed technically, materially, financially, or provided general support for the creation of the resource's content but are not considered authors.
| Name | Organization | Address | Phone | Author Identifiers |
|---|---|---|---|---|
| Sally Keating | University of Michigan | MI, US | ||
| Suman Timalsina | Tribhuvan University | Kathmandu, Nepal |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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