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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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 |
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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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