Carbon pools and fluxes in a Tibetan alpine Kobresia pygmaea pasture partitioned by coupled eddy-covariance measurements and 13CO2 pulse labeling

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Autoren

  • Johannes Ingrisch
  • Tobias Biermann
  • Elke Seeber
  • Thomas Leipold
  • Maoshan Li
  • Yaoming Ma
  • Xingliang Xu
  • Georg Miehe
  • Georg Guggenberger
  • Thomas Foken
  • Yakov Kuzyakov

Externe Organisationen

  • Universität Bayreuth
  • Universität Innsbruck
  • Lund University
  • Senckenberg Museum für Naturkunde Görlitz
  • Chinese Academy of Sciences (CAS)
  • Philipps-Universität Marburg
  • Georg-August-Universität Göttingen
  • Kazan Volga Region Federal University
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Details

OriginalspracheEnglisch
Seiten (von - bis)1213-1224
Seitenumfang12
FachzeitschriftScience of the Total Environment
Jahrgang505
PublikationsstatusVeröffentlicht - 1 Feb. 2015

Abstract

The Tibetan highlands host the largest alpine grassland ecosystems worldwide, bearing soils that store substantial stocks of carbon (C) that are very sensitive to land use changes. This study focuses on the cycling of photoassimilated C within a Kobresia pygmaea pasture, the dominating ecosystems on the Tibetan highlands. We investigated short-term effects of grazing cessation and the role of the characteristic Kobresia root turf on C fluxes and belowground C turnover. By combining eddy-covariance measurements with 13CO2 pulse labeling we applied a powerful new approach to measure absolute fluxes of assimilates within and between various pools of the plant-soil-atmosphere system. The roots and soil each store roughly 50% of the overall C in the system (76MgCha-1), with only a minor contribution from shoots, which is also expressed in the root:shoot ratio of 90. During June and July the pasture acted as a weak C sink with a strong uptake of approximately 2gCm-2 d-1 in the first half of July. The root turf was the main compartment for the turnover of photoassimilates, with a subset of highly dynamic roots (mean residence time 20days), and plays a key role for the C cycling and C storage in this ecosystem. The short-term grazing cessation only affected aboveground biomass but not ecosystem scale C exchange or assimilate allocation into roots and soil.

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Carbon pools and fluxes in a Tibetan alpine Kobresia pygmaea pasture partitioned by coupled eddy-covariance measurements and 13CO2 pulse labeling. / Ingrisch, Johannes; Biermann, Tobias; Seeber, Elke et al.
in: Science of the Total Environment, Jahrgang 505, 01.02.2015, S. 1213-1224.

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Ingrisch J, Biermann T, Seeber E, Leipold T, Li M, Ma Y et al. Carbon pools and fluxes in a Tibetan alpine Kobresia pygmaea pasture partitioned by coupled eddy-covariance measurements and 13CO2 pulse labeling. Science of the Total Environment. 2015 Feb 1;505:1213-1224. doi: 10.1016/j.scitotenv.2014.10.082
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title = "Carbon pools and fluxes in a Tibetan alpine Kobresia pygmaea pasture partitioned by coupled eddy-covariance measurements and 13CO2 pulse labeling",
abstract = "The Tibetan highlands host the largest alpine grassland ecosystems worldwide, bearing soils that store substantial stocks of carbon (C) that are very sensitive to land use changes. This study focuses on the cycling of photoassimilated C within a Kobresia pygmaea pasture, the dominating ecosystems on the Tibetan highlands. We investigated short-term effects of grazing cessation and the role of the characteristic Kobresia root turf on C fluxes and belowground C turnover. By combining eddy-covariance measurements with 13CO2 pulse labeling we applied a powerful new approach to measure absolute fluxes of assimilates within and between various pools of the plant-soil-atmosphere system. The roots and soil each store roughly 50% of the overall C in the system (76MgCha-1), with only a minor contribution from shoots, which is also expressed in the root:shoot ratio of 90. During June and July the pasture acted as a weak C sink with a strong uptake of approximately 2gCm-2 d-1 in the first half of July. The root turf was the main compartment for the turnover of photoassimilates, with a subset of highly dynamic roots (mean residence time 20days), and plays a key role for the C cycling and C storage in this ecosystem. The short-term grazing cessation only affected aboveground biomass but not ecosystem scale C exchange or assimilate allocation into roots and soil.",
keywords = "Alpine grassland, Carbon cycle, Grazing, Land use changes, Tibetan-Plateau",
author = "Johannes Ingrisch and Tobias Biermann and Elke Seeber and Thomas Leipold and Maoshan Li and Yaoming Ma and Xingliang Xu and Georg Miehe and Georg Guggenberger and Thomas Foken and Yakov Kuzyakov",
note = "Funding information: Supplementary data is available at http://doi.org/10.1594/PANGAEA.833208 . This work was supported by the German Research Council (DFG) DFG Fo 226/18-1.2, DFG KU 1184/14, MI 338/7-2; WE 2601/4-2;(SPP1372 ) within the Priority Program 1372 “Tibetan Plateau: Formation, Climate, Ecosystems” (TiP). Access to the “ Naqu Ecological and Environmental Observation and Research Station ” was granted by the Tibet University, Lhasa and the Institute of Tibetan Plateau Research (ITP), Chinese Academy of Sciences. Furthermore, the authors would like to thank everybody who participated in the collection of the data on the Tibetan plateau. We also are thankful to the Centre for Stable Isotope Research and Analysis (KOSI) of G{\"o}ttingen University and the Laboratory of Isotope Biogeochemistry of the Bayreuth Center of Ecology and Environmental Research (BayCEER) for the ? 13 C analysis. Appendix A",
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TY - JOUR

T1 - Carbon pools and fluxes in a Tibetan alpine Kobresia pygmaea pasture partitioned by coupled eddy-covariance measurements and 13CO2 pulse labeling

AU - Ingrisch, Johannes

AU - Biermann, Tobias

AU - Seeber, Elke

AU - Leipold, Thomas

AU - Li, Maoshan

AU - Ma, Yaoming

AU - Xu, Xingliang

AU - Miehe, Georg

AU - Guggenberger, Georg

AU - Foken, Thomas

AU - Kuzyakov, Yakov

N1 - Funding information: Supplementary data is available at http://doi.org/10.1594/PANGAEA.833208 . This work was supported by the German Research Council (DFG) DFG Fo 226/18-1.2, DFG KU 1184/14, MI 338/7-2; WE 2601/4-2;(SPP1372 ) within the Priority Program 1372 “Tibetan Plateau: Formation, Climate, Ecosystems” (TiP). Access to the “ Naqu Ecological and Environmental Observation and Research Station ” was granted by the Tibet University, Lhasa and the Institute of Tibetan Plateau Research (ITP), Chinese Academy of Sciences. Furthermore, the authors would like to thank everybody who participated in the collection of the data on the Tibetan plateau. We also are thankful to the Centre for Stable Isotope Research and Analysis (KOSI) of Göttingen University and the Laboratory of Isotope Biogeochemistry of the Bayreuth Center of Ecology and Environmental Research (BayCEER) for the ? 13 C analysis. Appendix A

PY - 2015/2/1

Y1 - 2015/2/1

N2 - The Tibetan highlands host the largest alpine grassland ecosystems worldwide, bearing soils that store substantial stocks of carbon (C) that are very sensitive to land use changes. This study focuses on the cycling of photoassimilated C within a Kobresia pygmaea pasture, the dominating ecosystems on the Tibetan highlands. We investigated short-term effects of grazing cessation and the role of the characteristic Kobresia root turf on C fluxes and belowground C turnover. By combining eddy-covariance measurements with 13CO2 pulse labeling we applied a powerful new approach to measure absolute fluxes of assimilates within and between various pools of the plant-soil-atmosphere system. The roots and soil each store roughly 50% of the overall C in the system (76MgCha-1), with only a minor contribution from shoots, which is also expressed in the root:shoot ratio of 90. During June and July the pasture acted as a weak C sink with a strong uptake of approximately 2gCm-2 d-1 in the first half of July. The root turf was the main compartment for the turnover of photoassimilates, with a subset of highly dynamic roots (mean residence time 20days), and plays a key role for the C cycling and C storage in this ecosystem. The short-term grazing cessation only affected aboveground biomass but not ecosystem scale C exchange or assimilate allocation into roots and soil.

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KW - Carbon cycle

KW - Grazing

KW - Land use changes

KW - Tibetan-Plateau

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