Articles | Volume 17, issue 5
https://doi.org/10.5194/cp-17-1903-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/cp-17-1903-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
24 Sep 2021
Research article | Highlight paper |
| 24 Sep 2021
| 24 Sep 2021
Stalagmite carbon isotopes suggest deglacial increase in soil respiration in western Europe driven by temperature change
Franziska A. Lechleitner
CORRESPONDING AUTHOR
Department of Earth Sciences, University of Oxford, South Parks Road,
OX1 3AN, Oxford, UK
Department of Chemistry, Biochemistry and Pharmaceutical Sciences and Oeschger Centre for Climate Change Research, University of Bern, Freiestrasse 3, 3012 Bern, Switzerland
Invited contribution by Franziska A. Lechleitner, recipient of the EGU Climate: Past, Present & Future Division Outstanding Early Career Scientists Award 2021.
Christopher C. Day
Department of Earth Sciences, University of Oxford, South Parks Road,
OX1 3AN, Oxford, UK
Oliver Kost
Department of Earth Sciences, ETH Zurich, Sonneggstrasse 5, 8006
Zurich, Switzerland
Micah Wilhelm
Swiss Federal Institute for Forest, Snow and Landscape Research,
Zürcherstrasse 111, 8903 Birmensdorf, Switzerland
Negar Haghipour
Department of Earth Sciences, ETH Zurich, Sonneggstrasse 5, 8006
Zurich, Switzerland
Laboratory for Ion Beam Physics, ETH Zurich, Otto-Stern-Weg 5, 8093 Zurich, Switzerland
Gideon M. Henderson
Department of Earth Sciences, University of Oxford, South Parks Road,
OX1 3AN, Oxford, UK
Heather M. Stoll
Department of Earth Sciences, ETH Zurich, Sonneggstrasse 5, 8006
Zurich, Switzerland
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Cited
19 citations as recorded by crossref.
- An integrated study of constraining the initial 230Th of a stalagmite and its implications S. Huang et al. 10.1016/j.quageo.2024.101497
- Investigating stable oxygen and carbon isotopic variability in speleothem records over the last millennium using multiple isotope-enabled climate models J. Bühler et al. 10.5194/cp-18-1625-2022
- Multidecadal Monsoon Variations during the Early Last Deglaciation Revealed by Speleothem Record from Southwestern China Y. Liang et al. 10.3390/min14040346
- Structural similarity between Termination III and I W. Duan et al. 10.1016/j.quascirev.2022.107808
- Deglacial export of pre-aged terrigenous carbon to the Bay of Biscay E. Queiroz Alves et al. 10.5194/cp-20-121-2024
- Rapid northern hemisphere ice sheet melting during the penultimate deglaciation H. Stoll et al. 10.1038/s41467-022-31619-3
- 550‐Year Climate Periodicity in the Yunnan‐Guizhou Plateau During the Late Mid‐Holocene: Insights and Implications Y. Li et al. 10.1029/2023GL103523
- Seasonal variations of cave dripwater hydrogeochemical parameters and δ13CDIC in the subtropical monsoon region and links to regional hydroclimate H. Zhang et al. 10.1016/j.scitotenv.2023.163509
- A Highly Resolved Speleothem δ13C Record from Central China and Its Manifestation on Multiple Time Scales during the Last Glacial Q. Chen et al. 10.3390/min14050450
- Tropical vegetation productivity and atmospheric methane over the last 40,000 years from model simulations and stalagmites in Sulawesi, Indonesia C. Krause et al. 10.1017/qua.2023.75
- A mid-Holocene stalagmite multiproxy record from southern Siberia (Krasnoyarsk, Russia) linked to the Siberian High patterns A. Columbu et al. 10.1016/j.quascirev.2023.108355
- New insights into the climate of northern Iberia during the Younger Dryas and Holocene: The Mendukilo multi-speleothem record J. Bernal-Wormull et al. 10.1016/j.quascirev.2023.108006
- A UNIVERSAL GAS INTERFACE FOR SIMULTANEOUS 14C AND δ13C MEASUREMENTS M. Wertnik et al. 10.1017/RDC.2023.113
- Distinguishing the combined vegetation and soil component of δ13C variation in speleothem records from subsequent degassing and prior calcite precipitation effects H. Stoll et al. 10.5194/cp-19-2423-2023
- Highly resolved δ13C and trace element ratios of precisely dated stalagmite from northwestern China: Hydroclimate reconstruction during the last two millennia W. Jia et al. 10.1016/j.quascirev.2022.107473
- Relationship of seasonal variations in drip waterδ13CDIC,δ18O, and trace elements with surface and physical cave conditions of La Vallina cave, NW Spain O. Kost et al. 10.5194/hess-27-2227-2023
- Different response of stalagmite δ18O and δ13C to millennial-scale events during the last glacial, evidenced from Huangjin Cave, northern China Y. Liang et al. 10.1016/j.quascirev.2021.107305
- Carbonates in the Critical Zone M. Covington et al. 10.1029/2022EF002765
- SISALv3: a global speleothem stable isotope and trace element database N. Kaushal et al. 10.5194/essd-16-1933-2024
19 citations as recorded by crossref.
- An integrated study of constraining the initial 230Th of a stalagmite and its implications S. Huang et al. 10.1016/j.quageo.2024.101497
- Investigating stable oxygen and carbon isotopic variability in speleothem records over the last millennium using multiple isotope-enabled climate models J. Bühler et al. 10.5194/cp-18-1625-2022
- Multidecadal Monsoon Variations during the Early Last Deglaciation Revealed by Speleothem Record from Southwestern China Y. Liang et al. 10.3390/min14040346
- Structural similarity between Termination III and I W. Duan et al. 10.1016/j.quascirev.2022.107808
- Deglacial export of pre-aged terrigenous carbon to the Bay of Biscay E. Queiroz Alves et al. 10.5194/cp-20-121-2024
- Rapid northern hemisphere ice sheet melting during the penultimate deglaciation H. Stoll et al. 10.1038/s41467-022-31619-3
- 550‐Year Climate Periodicity in the Yunnan‐Guizhou Plateau During the Late Mid‐Holocene: Insights and Implications Y. Li et al. 10.1029/2023GL103523
- Seasonal variations of cave dripwater hydrogeochemical parameters and δ13CDIC in the subtropical monsoon region and links to regional hydroclimate H. Zhang et al. 10.1016/j.scitotenv.2023.163509
- A Highly Resolved Speleothem δ13C Record from Central China and Its Manifestation on Multiple Time Scales during the Last Glacial Q. Chen et al. 10.3390/min14050450
- Tropical vegetation productivity and atmospheric methane over the last 40,000 years from model simulations and stalagmites in Sulawesi, Indonesia C. Krause et al. 10.1017/qua.2023.75
- A mid-Holocene stalagmite multiproxy record from southern Siberia (Krasnoyarsk, Russia) linked to the Siberian High patterns A. Columbu et al. 10.1016/j.quascirev.2023.108355
- New insights into the climate of northern Iberia during the Younger Dryas and Holocene: The Mendukilo multi-speleothem record J. Bernal-Wormull et al. 10.1016/j.quascirev.2023.108006
- A UNIVERSAL GAS INTERFACE FOR SIMULTANEOUS 14C AND δ13C MEASUREMENTS M. Wertnik et al. 10.1017/RDC.2023.113
- Distinguishing the combined vegetation and soil component of δ13C variation in speleothem records from subsequent degassing and prior calcite precipitation effects H. Stoll et al. 10.5194/cp-19-2423-2023
- Highly resolved δ13C and trace element ratios of precisely dated stalagmite from northwestern China: Hydroclimate reconstruction during the last two millennia W. Jia et al. 10.1016/j.quascirev.2022.107473
- Relationship of seasonal variations in drip waterδ13CDIC,δ18O, and trace elements with surface and physical cave conditions of La Vallina cave, NW Spain O. Kost et al. 10.5194/hess-27-2227-2023
- Different response of stalagmite δ18O and δ13C to millennial-scale events during the last glacial, evidenced from Huangjin Cave, northern China Y. Liang et al. 10.1016/j.quascirev.2021.107305
- Carbonates in the Critical Zone M. Covington et al. 10.1029/2022EF002765
- SISALv3: a global speleothem stable isotope and trace element database N. Kaushal et al. 10.5194/essd-16-1933-2024
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Short summary
Soil respiration is a critical but poorly constrained component of the global carbon cycle. We analyse the effect of changing soil respiration rates on the stable carbon isotope ratio of speleothems from northern Spain covering the last deglaciation. Using geochemical analysis and forward modelling we quantify the processes affecting speleothem stable carbon isotope ratios and extract a signature of increasing soil respiration synchronous with deglacial warming.
Soil respiration is a critical but poorly constrained component of the global carbon cycle. We...
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