Data from : "Warming promotes loss of subsoil carbon through accelerated degradation of plant-derived organic matter". Blodgett warming experiment
Abstract
This dataset contains data used for the paper: Warming promotes loss of subsoil carbon through accelerated degradation of plant-derived organic matter. Soil Biology and Biochemistry 156, 108185. doi:10.1016/j.soilbio.2021.108185On April 2018 (after 4.5 years of warming), we collected O-horizon (organic horizon) material and soil core down to 90 cm depth from a whole-soil warming experiment in a mixed-coniferous temperate forest, located at the University of California Blodgett experimental forest in the foothills of the Sierra Nevada, CA USA. The goal was to assess how 4.5 years of +4 °C whole-soil warming affected the quantity and quality of soil organic matter. Cores were collected from 6 experimental plots (three replicated blocks); samples were collected in 10 cm increments from 0 to 90 cm depth.This dataset contains a compressed (.zip) archive of the data used for this manuscript. The dataset includes files in .xlsx format, which can be accessed and processed using MS Excel or R. Carbon and nitrogen concentrations, as well as stable carbon isotope composition ((δ13C) and solvent extractable lipid biomarker (alkanoic acids and alkanes) data are provided as processed data files. Diffuse reflectance infrared Fourier transform (DRIFT) spectroscopy data are provided as raw output and processed data files.The dataset filesmore »
- Authors:
-
- University of Zurich; University of Zurich
- University of Zurich
- Lawrence Berkeley National Laboratory
- Colorado State University
- ETH Zurich
- Publication Date:
- Research Org.:
- Environmental System Science Data Infrastructure for a Virtual Ecosystem; Terrestrial Ecosystem Science at Berkeley Lab
- Sponsoring Org.:
- Swiss National Science Foundation (SNF); U.S. DOE > Office of Science > Biological and Environmental Research (BER). Terrestrial Ecosystem Science Program
- Subject:
- 54 ENVIRONMENTAL SCIENCES; Alkanes; Biomarker; Decomposition; Diffuse reflectance infrared Fourier transform spectroscopy; EARTH SCIENCE > LAND SURFACE > SOILS; EARTH SCIENCE > LAND SURFACE > SOILS > CARBON; EARTH SCIENCE > LAND SURFACE > SOILS > ORGANIC MATTER; EARTH SCIENCE > LAND SURFACE > SOILS > SOIL CHEMISTRY; Fatty acids; Soil organic matter; Warming experiment; Whole soil warming
- OSTI Identifier:
- 1797785
- DOI:
- https://doi.org/10.15485/1797785
Citation Formats
Ofiti, Nicholas O.E., Schmidt, Michael W.I., Torn, Margaret S., Wiesenberg, Guido L.B., Soong, Jennifer L., Zosso, Cyrill U., and Solly, Emily F. Data from : "Warming promotes loss of subsoil carbon through accelerated degradation of plant-derived organic matter". Blodgett warming experiment. United States: N. p., 2020.
Web. doi:10.15485/1797785.
Ofiti, Nicholas O.E., Schmidt, Michael W.I., Torn, Margaret S., Wiesenberg, Guido L.B., Soong, Jennifer L., Zosso, Cyrill U., & Solly, Emily F. Data from : "Warming promotes loss of subsoil carbon through accelerated degradation of plant-derived organic matter". Blodgett warming experiment. United States. doi:https://doi.org/10.15485/1797785
Ofiti, Nicholas O.E., Schmidt, Michael W.I., Torn, Margaret S., Wiesenberg, Guido L.B., Soong, Jennifer L., Zosso, Cyrill U., and Solly, Emily F. 2020.
"Data from : "Warming promotes loss of subsoil carbon through accelerated degradation of plant-derived organic matter". Blodgett warming experiment". United States. doi:https://doi.org/10.15485/1797785. https://www.osti.gov/servlets/purl/1797785. Pub date:Thu Dec 31 23:00:00 EST 2020
@article{osti_1797785,
title = {Data from : "Warming promotes loss of subsoil carbon through accelerated degradation of plant-derived organic matter". Blodgett warming experiment},
author = {Ofiti, Nicholas O.E. and Schmidt, Michael W.I. and Torn, Margaret S. and Wiesenberg, Guido L.B. and Soong, Jennifer L. and Zosso, Cyrill U. and Solly, Emily F.},
abstractNote = {This dataset contains data used for the paper: Warming promotes loss of subsoil carbon through accelerated degradation of plant-derived organic matter. Soil Biology and Biochemistry 156, 108185. doi:10.1016/j.soilbio.2021.108185On April 2018 (after 4.5 years of warming), we collected O-horizon (organic horizon) material and soil core down to 90 cm depth from a whole-soil warming experiment in a mixed-coniferous temperate forest, located at the University of California Blodgett experimental forest in the foothills of the Sierra Nevada, CA USA. The goal was to assess how 4.5 years of +4 °C whole-soil warming affected the quantity and quality of soil organic matter. Cores were collected from 6 experimental plots (three replicated blocks); samples were collected in 10 cm increments from 0 to 90 cm depth.This dataset contains a compressed (.zip) archive of the data used for this manuscript. The dataset includes files in .xlsx format, which can be accessed and processed using MS Excel or R. Carbon and nitrogen concentrations, as well as stable carbon isotope composition ((δ13C) and solvent extractable lipid biomarker (alkanoic acids and alkanes) data are provided as processed data files. Diffuse reflectance infrared Fourier transform (DRIFT) spectroscopy data are provided as raw output and processed data files.The dataset files "Blodgett_warming_Data" and "Blodgett_warming_raw_data.xlsx" were updated on July 7, 2021. The following updates were made: (1) specification of the units of measurements in the dataset (the unit of measurement was missing in some parameters) and (2) the column name "pulled depth" was changed to "pooled depth" in the updated data files.},
doi = {10.15485/1797785},
journal = {},
number = ,
volume = ,
place = {United States},
year = {Thu Dec 31 23:00:00 EST 2020},
month = {Thu Dec 31 23:00:00 EST 2020}
}
