Changes in above- versus belowground biomass distribution in permafrost regions in response to climate warming

Permafrost regions contain approximately half of the carbon stored in land ecosystems and have warmed at least twice as much as any other biome.This warming has influenced vegetation activity, leading to changes in plant composition, physiology, and biomass storage in aboveground and belowground com...

Full description

Bibliographic Details
Main Authors: Yun, Hanbo, Qingbai, Wu, Elberling, Bo, Zohner, Constantin M.
Format: Other/Unknown Material
Language:English
Published: Zenodo 2024
Subjects:
Online Access:https://doi.org/10.5281/zenodo.11218337
id ftzenodo:oai:zenodo.org:11218337
record_format openpolar
spelling ftzenodo:oai:zenodo.org:11218337 2024-09-09T20:03:01+00:00 Changes in above- versus belowground biomass distribution in permafrost regions in response to climate warming Yun, Hanbo Qingbai, Wu Elberling, Bo Zohner, Constantin M. 2024-05-20 https://doi.org/10.5281/zenodo.11218337 eng eng Zenodo https://doi.org/10.5281/zenodo.11218336 https://doi.org/10.5281/zenodo.11218337 oai:zenodo.org:11218337 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode PNAS, 121(0), (2024-05-20) Biomass Carbon fibers vegetation adaptations permafrost climate warming biomass allocation carbon trajectory info:eu-repo/semantics/other 2024 ftzenodo https://doi.org/10.5281/zenodo.1121833710.5281/zenodo.11218336 2024-07-25T20:51:25Z Permafrost regions contain approximately half of the carbon stored in land ecosystems and have warmed at least twice as much as any other biome.This warming has influenced vegetation activity, leading to changes in plant composition, physiology, and biomass storage in aboveground and belowground components, ultimately impacting ecosystem carbon balance. Yet, little is known about the causes and magnitude of long-term changes in the above- to belowground biomass ratio of plants (η). Here, we analyzed η values based on 3,013 plots and 26,337 plant-specific measurements representing eight sites across the Tibetan Plateau from 1995 to 2021. Our analysis revealed distinct temporal trends in η for three vegetation types: a 17% increase in alpine wetlands, and a decrease of 26% and 48% in alpine meadows and alpine steppes, respectively. These trends were primarily driven by temperature-induced growth preferences rather than shifts in plant species composition.Our findings indicate that in wetter ecosystems climate warming promotes aboveground plant growth, while in drier ecosystems, such as alpine meadows and alpine steppes, plants allocate more biomass belowground. Four process-based biogeochemical models failed to simulate the observed changes in η, which highlights the importance of improved process understanding of the processes driving the response of biomass distribution to climate warming, which is crucial for predicting the future carbon trajectory of permafrost ecosystems. Other/Unknown Material permafrost Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language English
topic Biomass
Carbon fibers
vegetation adaptations
permafrost
climate warming
biomass allocation
carbon trajectory
spellingShingle Biomass
Carbon fibers
vegetation adaptations
permafrost
climate warming
biomass allocation
carbon trajectory
Yun, Hanbo
Qingbai, Wu
Elberling, Bo
Zohner, Constantin M.
Changes in above- versus belowground biomass distribution in permafrost regions in response to climate warming
topic_facet Biomass
Carbon fibers
vegetation adaptations
permafrost
climate warming
biomass allocation
carbon trajectory
description Permafrost regions contain approximately half of the carbon stored in land ecosystems and have warmed at least twice as much as any other biome.This warming has influenced vegetation activity, leading to changes in plant composition, physiology, and biomass storage in aboveground and belowground components, ultimately impacting ecosystem carbon balance. Yet, little is known about the causes and magnitude of long-term changes in the above- to belowground biomass ratio of plants (η). Here, we analyzed η values based on 3,013 plots and 26,337 plant-specific measurements representing eight sites across the Tibetan Plateau from 1995 to 2021. Our analysis revealed distinct temporal trends in η for three vegetation types: a 17% increase in alpine wetlands, and a decrease of 26% and 48% in alpine meadows and alpine steppes, respectively. These trends were primarily driven by temperature-induced growth preferences rather than shifts in plant species composition.Our findings indicate that in wetter ecosystems climate warming promotes aboveground plant growth, while in drier ecosystems, such as alpine meadows and alpine steppes, plants allocate more biomass belowground. Four process-based biogeochemical models failed to simulate the observed changes in η, which highlights the importance of improved process understanding of the processes driving the response of biomass distribution to climate warming, which is crucial for predicting the future carbon trajectory of permafrost ecosystems.
format Other/Unknown Material
author Yun, Hanbo
Qingbai, Wu
Elberling, Bo
Zohner, Constantin M.
author_facet Yun, Hanbo
Qingbai, Wu
Elberling, Bo
Zohner, Constantin M.
author_sort Yun, Hanbo
title Changes in above- versus belowground biomass distribution in permafrost regions in response to climate warming
title_short Changes in above- versus belowground biomass distribution in permafrost regions in response to climate warming
title_full Changes in above- versus belowground biomass distribution in permafrost regions in response to climate warming
title_fullStr Changes in above- versus belowground biomass distribution in permafrost regions in response to climate warming
title_full_unstemmed Changes in above- versus belowground biomass distribution in permafrost regions in response to climate warming
title_sort changes in above- versus belowground biomass distribution in permafrost regions in response to climate warming
publisher Zenodo
publishDate 2024
url https://doi.org/10.5281/zenodo.11218337
genre permafrost
genre_facet permafrost
op_source PNAS, 121(0), (2024-05-20)
op_relation https://doi.org/10.5281/zenodo.11218336
https://doi.org/10.5281/zenodo.11218337
oai:zenodo.org:11218337
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.5281/zenodo.1121833710.5281/zenodo.11218336
_version_ 1809934964716732416