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- W4309754329 abstract "Abstract Permafrost soils contain nearly twice as much carbon as the atmosphere. The current observed climate warming will lead to widespread degradation of near-surface permafrost, which may perturb the vertical distribution of nutrition availability in permafrost-affected ecosystems, and the potential ramification is far-reaching to the carbon cycling between vegetation and climate. Aims: A better understanding of permafrost thawing how to drive plant growth and species composition is crucial for predicting the consequence of climate change for permafrost affected ecosystem response. Methods: We explored the relationship between permafrost thawing, soil chemistry, soil nutrition, and above-ground biomass, maximum rooting depth and species composition across space, and over four decades of warming at 14 Tibet Plateau sites. Results: 1) With permafrost thawing, both cation and anion concentration increased at the ground surface layer (0-50cm); 2) Particularly, nitrogen released from permafrost table stimulated maximum root depth, which drove the species composition; 3) Above-ground biomass in the long term (Fourth decades) did not have a statistic change, although in some special-specific years had a significant fluctuant. Conclusions: Here, we provided suggestions that deep-rooting species have a competitive advantage than shallow-rooting species driver the species composition under climate warming. Whereas, our findings highlight the water-soluble salt (nutrient) concentration and location varieties intense the competitive advantage of deep-rooting species due to short the time of the belowground growing season." @default.
- W4309754329 created "2022-11-29" @default.
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- W4309754329 date "2022-11-21" @default.
- W4309754329 modified "2023-09-25" @default.
- W4309754329 title "Permafrost thawing drives long term changes in plant species composition at the Tibetan Plateau" @default.
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- W4309754329 doi "https://doi.org/10.21203/rs.3.rs-2265053/v1" @default.
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