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Morphological and physiological adaptation characteristics of lithophytic bryophytes to karst high calcium environment

BACKGROUND: Lithophytic bryophytes grow on the rock surface, change the habitat on the rock surface through biological karstification, and provide a material basis for the growth of other plants. However, the surface calcium content of bare rock is high. The lithophytic bryophytes may have a special...

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Autores principales: Meng, Wenping, Ran, Jingcheng, Dai, Quanhou, Tu, Na, Leng, Tingjiao, Ren, Qingqing
Formato: Online Artículo Texto
Lenguaje:English
Publicado: BioMed Central 2023
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10039556/
https://www.ncbi.nlm.nih.gov/pubmed/36964495
http://dx.doi.org/10.1186/s12870-022-03980-4
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author Meng, Wenping
Ran, Jingcheng
Dai, Quanhou
Tu, Na
Leng, Tingjiao
Ren, Qingqing
author_facet Meng, Wenping
Ran, Jingcheng
Dai, Quanhou
Tu, Na
Leng, Tingjiao
Ren, Qingqing
author_sort Meng, Wenping
collection PubMed
description BACKGROUND: Lithophytic bryophytes grow on the rock surface, change the habitat on the rock surface through biological karstification, and provide a material basis for the growth of other plants. However, the surface calcium content of bare rock is high. The lithophytic bryophytes may have a special mechanism to adapt to the karst high calcium environment. The present study aimed to explore the physiological regulation process of karst lithophytic bryophytes under high calcium environment, and to provide scientific basis for revealing the maintenance mechanism of karst biodiversity. RESULTS: With the increase of Ca(2+) concentration, the contents of Pro, SP and MDA of lithophytic bryophytes showed a downward—upward—downward trend. However, when Ca(2+) ≥ 400 mmol/L, the contents of Pro and SP changed significantly at 1d, 2d, 3d, 5d and 7d with the extension of culture time, and lithophytic bryophytes died after 2 months of culture. Under different Ca(2+) concentrations, the maximum SOD activity of lithophytic bryophytes is 1758.00 (U/g FW), the minimum is 92.60 (U/g FW), the maximum POD activity is 120.88 (U/g FW), and the minimum is 4.80 (U/g FW). The antioxidative activity of of Hyophila involuta are higher than that of Didymodon constrictus and Eurohypnum leptothallum, and its enzyme activity changed significantly with the increase of calcium concentration and time.At the same time, the contents of TChl, Chla, and Chlb in lithophytic bryophytes decreased with the increase of Ca(2+) concentration. When Ca(2+) = 400 mmol/L, the contents of TChl and Chla were the lowest, but when Ca(2+) > 400 mmol/L, they began to increase. In addition, ABA is negatively correlated with TChl and Chla, and positively correlated with ROS. It shows that ABA has a certain role in regulating the adaptation of lithophytic bryophytes to high calcium environment. CONCLUSIONS: Lithophytic bryophytes have strong calcium tolerance, and their physiological response to high calcium stress is different from vascular bundle plants. The general stress principle is not applicable to lithophytic bryophytes. The response of lithophytic bryophytes to the change of Ca(2+)concentration is slow, showing passive response or inert response.
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spelling pubmed-100395562023-03-26 Morphological and physiological adaptation characteristics of lithophytic bryophytes to karst high calcium environment Meng, Wenping Ran, Jingcheng Dai, Quanhou Tu, Na Leng, Tingjiao Ren, Qingqing BMC Plant Biol Research BACKGROUND: Lithophytic bryophytes grow on the rock surface, change the habitat on the rock surface through biological karstification, and provide a material basis for the growth of other plants. However, the surface calcium content of bare rock is high. The lithophytic bryophytes may have a special mechanism to adapt to the karst high calcium environment. The present study aimed to explore the physiological regulation process of karst lithophytic bryophytes under high calcium environment, and to provide scientific basis for revealing the maintenance mechanism of karst biodiversity. RESULTS: With the increase of Ca(2+) concentration, the contents of Pro, SP and MDA of lithophytic bryophytes showed a downward—upward—downward trend. However, when Ca(2+) ≥ 400 mmol/L, the contents of Pro and SP changed significantly at 1d, 2d, 3d, 5d and 7d with the extension of culture time, and lithophytic bryophytes died after 2 months of culture. Under different Ca(2+) concentrations, the maximum SOD activity of lithophytic bryophytes is 1758.00 (U/g FW), the minimum is 92.60 (U/g FW), the maximum POD activity is 120.88 (U/g FW), and the minimum is 4.80 (U/g FW). The antioxidative activity of of Hyophila involuta are higher than that of Didymodon constrictus and Eurohypnum leptothallum, and its enzyme activity changed significantly with the increase of calcium concentration and time.At the same time, the contents of TChl, Chla, and Chlb in lithophytic bryophytes decreased with the increase of Ca(2+) concentration. When Ca(2+) = 400 mmol/L, the contents of TChl and Chla were the lowest, but when Ca(2+) > 400 mmol/L, they began to increase. In addition, ABA is negatively correlated with TChl and Chla, and positively correlated with ROS. It shows that ABA has a certain role in regulating the adaptation of lithophytic bryophytes to high calcium environment. CONCLUSIONS: Lithophytic bryophytes have strong calcium tolerance, and their physiological response to high calcium stress is different from vascular bundle plants. The general stress principle is not applicable to lithophytic bryophytes. The response of lithophytic bryophytes to the change of Ca(2+)concentration is slow, showing passive response or inert response. BioMed Central 2023-03-25 /pmc/articles/PMC10039556/ /pubmed/36964495 http://dx.doi.org/10.1186/s12870-022-03980-4 Text en © The Author(s) 2023 https://creativecommons.org/licenses/by/4.0/Open AccessThis article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if changes were made. The images or other third party material in this article are included in the article's Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article's Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) . The Creative Commons Public Domain Dedication waiver (http://creativecommons.org/publicdomain/zero/1.0/ (https://creativecommons.org/publicdomain/zero/1.0/) ) applies to the data made available in this article, unless otherwise stated in a credit line to the data.
spellingShingle Research
Meng, Wenping
Ran, Jingcheng
Dai, Quanhou
Tu, Na
Leng, Tingjiao
Ren, Qingqing
Morphological and physiological adaptation characteristics of lithophytic bryophytes to karst high calcium environment
title Morphological and physiological adaptation characteristics of lithophytic bryophytes to karst high calcium environment
title_full Morphological and physiological adaptation characteristics of lithophytic bryophytes to karst high calcium environment
title_fullStr Morphological and physiological adaptation characteristics of lithophytic bryophytes to karst high calcium environment
title_full_unstemmed Morphological and physiological adaptation characteristics of lithophytic bryophytes to karst high calcium environment
title_short Morphological and physiological adaptation characteristics of lithophytic bryophytes to karst high calcium environment
title_sort morphological and physiological adaptation characteristics of lithophytic bryophytes to karst high calcium environment
topic Research
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10039556/
https://www.ncbi.nlm.nih.gov/pubmed/36964495
http://dx.doi.org/10.1186/s12870-022-03980-4
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