Enrichment of 13C with depth in soil organic horizons is not explained by CO2 or DOC losses during decomposition-Reference-Cited by-同舟云学术

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Enrichment of 13C with depth in soil organic horizons is not explained by CO2 or DOC losses during decomposition

Published:2022-10 Issue: Volume:424 Page:116004
ISSN:0016-7061
Container-title:Geoderma
language:en
Short-container-title:Geoderma

Author:

Philben Michael^ORCID,Bowering Keri^ORCID,Podrebarac Frances A.^ORCID,Laganière Jérôme^ORCID,Edwards Kate,Ziegler Susan E.^ORCID

Publisher

Elsevier BV

Subject

Soil Science

Reference58 articles.

1. Carbon isotopes for estimating soil decomposition and physical mixing in well-drained forest soils;Acton;J. Geophys. Res. Biogeosci.,2013

2. The isotopic composition of soil and soil-respired CO2;Amundson;Geoderma,1998

3. Site-Related^(13) C of Tree Leaves and Soil Organic Matter in a Temperate Forest;Balesdent;Ecology,1993

4. Depletion of 13C in lignin and its implications for stable carbon isotope studies;Benner;Nature,1987

5. Changes in stable isotopic signatures of soil nitrogen and carbon during 40 years of forest development;Billings;Oecologia,2006

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1. Particle‐Size‐Specific Radiocarbon Constraints Imply an Active Subsoil Organic Carbon Pool;Journal of Geophysical Research: Biogeosciences;2024-05

2. Microbial hotspots in a relict fog-dependent Tillandsia landbeckii dune from the coastal Atacama Desert;Global and Planetary Change;2024-03

3. Soil depth gradients of organic carbon-13 – A review on drivers and processes;Plant and Soil;2023-11-11

4. Physically protected organic matter drives soil carbon sequestration potential of a managed grassland ecosystem in Italian Alps;Geoderma Regional;2023-09

5. Effects of Snow Cover on Carbon Dioxide Emissions and Their δ13C Values of Temperate Forest Soils with and without Litter;Forests;2023-07-06

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