Critical signals for grassland desertification prediction in the transition zone between desert and typical steppe in InnerMongolia, China

Global climate change and intensifying human activities have driven an accelerated desertification of grasslands in arid and semi-arid regions. Recent theoretical investigations have proposed that vegetation patches can serve as indicators of desertification. However, knowledge regarding the appropr...

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Main Authors: Baoping Meng, Zhuoyan Jin, Jin Chen, Yili Kuang, Shuhua Yi, Yanyan Lv, Jinrong Li
Format: Article
Language:English
Published: Elsevier 2025-01-01
Series:Ecological Indicators
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Online Access:http://www.sciencedirect.com/science/article/pii/S1470160X2401522X
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author Baoping Meng
Zhuoyan Jin
Jin Chen
Yili Kuang
Shuhua Yi
Yanyan Lv
Jinrong Li
author_facet Baoping Meng
Zhuoyan Jin
Jin Chen
Yili Kuang
Shuhua Yi
Yanyan Lv
Jinrong Li
author_sort Baoping Meng
collection DOAJ
description Global climate change and intensifying human activities have driven an accelerated desertification of grasslands in arid and semi-arid regions. Recent theoretical investigations have proposed that vegetation patches can serve as indicators of desertification. However, knowledge regarding the appropriateness of these proposed indicators still lacked. Understanding the relations between patch features and plant species diversity are crucial for the early prediction of desertification. In this research, the transition zone between desert and typical steppe in Inner Mongolia, China was studied. We analyzed vegetation patch features (including percentage of landscape (PLAND), patch density (PD), largest patch index (LPI), and perimeter-area ratio distribution (PARA)), species diversity indices (Shannon-Wiener, Simpson, Margalef, Pielou), soil seed bank density, similarity index, and established their relations. Results showed that: (1) During grassland desertification, LPI decreasing rapidly followed by a slower decline, while PARA exhibited an initial slow decrease before a rapid decline during grassland desertification, reaching a critical point at a vegetation coverage of 49.95 %. (2) Species diversity indices tended to be increased first and then decreased with the decrease of CA, LPI, and PARA. These variations followed a unimodal pattern (P < 0.001), with peak plant diversity indices observed at CA of 5 m2, LPI of 40 %, and PARA of 40. (3) Soil seed bank density and similarity were also increased first and then decreased (P < 0.001) with the process of grassland desertification. When CA was 6 m2, LPI was 40 %, PARA was 40, the soil seed bank density and similarity reached highest (with 900 seeds/m2, and similarity of 58 %, respectively). Our studies concluded that LPI and PARA could be considered as early warning signals of grassland desertification in transition zone, and provided scientific basics for grassland management in arid and semi-arid areas.
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publishDate 2025-01-01
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series Ecological Indicators
spelling doaj-art-ed2c7be412b14768afeebeb8e75f23142025-01-31T05:10:45ZengElsevierEcological Indicators1470-160X2025-01-01170113065Critical signals for grassland desertification prediction in the transition zone between desert and typical steppe in InnerMongolia, ChinaBaoping Meng0Zhuoyan Jin1Jin Chen2Yili Kuang3Shuhua Yi4Yanyan Lv5Jinrong Li6Yinshanbeilu Grassland Eco-hydrology National Observation and Research Station, China Institute of Water Resources and Hydropower Research, Beijing, 10038, China; Institute of Fragile Eco-environment, Nantong University, Nantong 226007, China; School of Geographic Science, Nantong University, Nantong 226007, ChinaSchool of Geographic Science, Nantong University, Nantong 226007, ChinaSchool of Geographic Science, Nantong University, Nantong 226007, ChinaSchool of Geographic Science, Nantong University, Nantong 226007, ChinaInstitute of Fragile Eco-environment, Nantong University, Nantong 226007, China; School of Geographic Science, Nantong University, Nantong 226007, ChinaInstitute of Fragile Eco-environment, Nantong University, Nantong 226007, China; School of Geographic Science, Nantong University, Nantong 226007, China; Corresponding authors at: Institute of Fragile Eco-environment, Nantong University, Nantong 226007, China (Y. Lv). Yinshanbeilu Grassland Eco-hydrology National Observation and Research Station, China Institute of Water Resources and Hydropower Research, Beijing 100038, China (J. Li).Yinshanbeilu Grassland Eco-hydrology National Observation and Research Station, China Institute of Water Resources and Hydropower Research, Beijing, 10038, China; Corresponding authors at: Institute of Fragile Eco-environment, Nantong University, Nantong 226007, China (Y. Lv). Yinshanbeilu Grassland Eco-hydrology National Observation and Research Station, China Institute of Water Resources and Hydropower Research, Beijing 100038, China (J. Li).Global climate change and intensifying human activities have driven an accelerated desertification of grasslands in arid and semi-arid regions. Recent theoretical investigations have proposed that vegetation patches can serve as indicators of desertification. However, knowledge regarding the appropriateness of these proposed indicators still lacked. Understanding the relations between patch features and plant species diversity are crucial for the early prediction of desertification. In this research, the transition zone between desert and typical steppe in Inner Mongolia, China was studied. We analyzed vegetation patch features (including percentage of landscape (PLAND), patch density (PD), largest patch index (LPI), and perimeter-area ratio distribution (PARA)), species diversity indices (Shannon-Wiener, Simpson, Margalef, Pielou), soil seed bank density, similarity index, and established their relations. Results showed that: (1) During grassland desertification, LPI decreasing rapidly followed by a slower decline, while PARA exhibited an initial slow decrease before a rapid decline during grassland desertification, reaching a critical point at a vegetation coverage of 49.95 %. (2) Species diversity indices tended to be increased first and then decreased with the decrease of CA, LPI, and PARA. These variations followed a unimodal pattern (P < 0.001), with peak plant diversity indices observed at CA of 5 m2, LPI of 40 %, and PARA of 40. (3) Soil seed bank density and similarity were also increased first and then decreased (P < 0.001) with the process of grassland desertification. When CA was 6 m2, LPI was 40 %, PARA was 40, the soil seed bank density and similarity reached highest (with 900 seeds/m2, and similarity of 58 %, respectively). Our studies concluded that LPI and PARA could be considered as early warning signals of grassland desertification in transition zone, and provided scientific basics for grassland management in arid and semi-arid areas.http://www.sciencedirect.com/science/article/pii/S1470160X2401522XGrassland desertificationVegetation patchesSoil seed bankPlant diversity
spellingShingle Baoping Meng
Zhuoyan Jin
Jin Chen
Yili Kuang
Shuhua Yi
Yanyan Lv
Jinrong Li
Critical signals for grassland desertification prediction in the transition zone between desert and typical steppe in InnerMongolia, China
Ecological Indicators
Grassland desertification
Vegetation patches
Soil seed bank
Plant diversity
title Critical signals for grassland desertification prediction in the transition zone between desert and typical steppe in InnerMongolia, China
title_full Critical signals for grassland desertification prediction in the transition zone between desert and typical steppe in InnerMongolia, China
title_fullStr Critical signals for grassland desertification prediction in the transition zone between desert and typical steppe in InnerMongolia, China
title_full_unstemmed Critical signals for grassland desertification prediction in the transition zone between desert and typical steppe in InnerMongolia, China
title_short Critical signals for grassland desertification prediction in the transition zone between desert and typical steppe in InnerMongolia, China
title_sort critical signals for grassland desertification prediction in the transition zone between desert and typical steppe in innermongolia china
topic Grassland desertification
Vegetation patches
Soil seed bank
Plant diversity
url http://www.sciencedirect.com/science/article/pii/S1470160X2401522X
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