Insight into climate change from the carbon exchange of biocrusts utilizing non-rainfall water

Abstract Biocrusts are model ecosystems of global change studies. However, light and non-rainfall water (NRW) were previously few considered. Different biocrust types further aggravated the inconsistence. So carbon-exchange of biocrusts (cyanobacteria crusts-AC1/AC2; cyanolichen crust-LC1; chlorolic...

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Main Authors: Hailong Ouyang, Chunxiang Hu
Format: Article
Language:English
Published: Nature Publishing Group 2017-05-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-017-02812-y
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spelling doaj-76bf469e3814472b940f5041d4270a822020-12-08T02:21:22ZengNature Publishing GroupScientific Reports2045-23222017-05-017111310.1038/s41598-017-02812-yInsight into climate change from the carbon exchange of biocrusts utilizing non-rainfall waterHailong Ouyang0Chunxiang Hu1Key Laboratory of Algal Biology, Institute of Hydrobiology, Chinese Academy of SciencesKey Laboratory of Algal Biology, Institute of Hydrobiology, Chinese Academy of SciencesAbstract Biocrusts are model ecosystems of global change studies. However, light and non-rainfall water (NRW) were previously few considered. Different biocrust types further aggravated the inconsistence. So carbon-exchange of biocrusts (cyanobacteria crusts-AC1/AC2; cyanolichen crust-LC1; chlorolichen crust-LC2; moss crust-MC) utilizing NRW at various temperatures and light-intensities were determined under simulated and insitu mesocosm experiments. Carbon input of all biocrusts were negatively correlated with experimental temperature under all light-intensity with saturated water and stronger light with equivalent NRW, but positively correlated with temperature under weak light with equivalent NRW. LCPs and R/Pg of AC1 were lowest, followed in turn by AC2, LC2 and MC. Thus AC1 had most opportunities to use NRW, and 2.5 °C warming did cause significant changes of carbon exchange. Structural equation models further revealed that air-temperature was most important for carbon-exchange of ACs, but equally important as NRW for LC2 and MC; positive influence of warming on carbon-input in ACs was much stronger than the latter. Therefore, temperature effect on biocrust carbon-input depends on both moisture and light. Meanwhile, the role of NRW, transitional states between ACs, and obvious carbon-fixation differences between lichen crusts should be fully considered in the future study of biocrusts responding to climate change.https://doi.org/10.1038/s41598-017-02812-y
collection DOAJ
language English
format Article
sources DOAJ
author Hailong Ouyang
Chunxiang Hu
spellingShingle Hailong Ouyang
Chunxiang Hu
Insight into climate change from the carbon exchange of biocrusts utilizing non-rainfall water
Scientific Reports
author_facet Hailong Ouyang
Chunxiang Hu
author_sort Hailong Ouyang
title Insight into climate change from the carbon exchange of biocrusts utilizing non-rainfall water
title_short Insight into climate change from the carbon exchange of biocrusts utilizing non-rainfall water
title_full Insight into climate change from the carbon exchange of biocrusts utilizing non-rainfall water
title_fullStr Insight into climate change from the carbon exchange of biocrusts utilizing non-rainfall water
title_full_unstemmed Insight into climate change from the carbon exchange of biocrusts utilizing non-rainfall water
title_sort insight into climate change from the carbon exchange of biocrusts utilizing non-rainfall water
publisher Nature Publishing Group
series Scientific Reports
issn 2045-2322
publishDate 2017-05-01
description Abstract Biocrusts are model ecosystems of global change studies. However, light and non-rainfall water (NRW) were previously few considered. Different biocrust types further aggravated the inconsistence. So carbon-exchange of biocrusts (cyanobacteria crusts-AC1/AC2; cyanolichen crust-LC1; chlorolichen crust-LC2; moss crust-MC) utilizing NRW at various temperatures and light-intensities were determined under simulated and insitu mesocosm experiments. Carbon input of all biocrusts were negatively correlated with experimental temperature under all light-intensity with saturated water and stronger light with equivalent NRW, but positively correlated with temperature under weak light with equivalent NRW. LCPs and R/Pg of AC1 were lowest, followed in turn by AC2, LC2 and MC. Thus AC1 had most opportunities to use NRW, and 2.5 °C warming did cause significant changes of carbon exchange. Structural equation models further revealed that air-temperature was most important for carbon-exchange of ACs, but equally important as NRW for LC2 and MC; positive influence of warming on carbon-input in ACs was much stronger than the latter. Therefore, temperature effect on biocrust carbon-input depends on both moisture and light. Meanwhile, the role of NRW, transitional states between ACs, and obvious carbon-fixation differences between lichen crusts should be fully considered in the future study of biocrusts responding to climate change.
url https://doi.org/10.1038/s41598-017-02812-y
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