The impact of continuous cultivation of Ganoderma lucidum on soil nutrients, enzyme activity, and fruiting body metabolites.


Journal

Scientific reports
ISSN: 2045-2322
Titre abrégé: Sci Rep
Pays: England
ID NLM: 101563288

Informations de publication

Date de publication:
02 May 2024
Historique:
received: 18 02 2024
accepted: 26 04 2024
medline: 3 5 2024
pubmed: 3 5 2024
entrez: 2 5 2024
Statut: epublish

Résumé

To explore the impacts of continuous Ganoderma lucidum cultivation on soil physicochemical factors, soil enzyme activity, and the metabolome of Ganoderma lucidum fruiting bodies, this study conducted two consecutive years of cultivation on the same plot of land. Soil physicochemical factors and enzyme activity were assessed, alongside non-targeted metabolomic analysis of the Ganoderma lucidum fruiting bodies under continuous cultivation. The findings unveiled that in the surface soil layer (0-15 cm), there was a declining trend in organic matter, ammonium nitrogen, available phosphorus, available potassium, pH, polyphenol oxidase, peroxidase, alkaline phosphatase, and sucrase, whereas nitrate nitrogen, electrical conductivity (EC), and salt content exhibited an upward trend. Conversely, in the deeper soil layer (15-30 cm), organic matter, ammonium nitrogen, available potassium, alkaline phosphatase, and sucrase demonstrated a decreasing trend, while nitrate nitrogen, available phosphorus, pH, EC, salt content, polyphenol oxidase, and soil peroxidase showed an increasing trend. Metabolomic analysis of Ganoderma lucidum fruiting bodies distinguished 64 significantly different metabolites between the GCK and GT groups, with 39 components having markedly higher relative contents in GCK and 25 components having significantly lower relative contents in GCK compared to GT. Moreover, among these metabolites, there were more types with higher contents in the fruiting bodies harvested in the first year (GCK) compared to those harvested in the second year (GT), with pronounced differences. KEGG pathway analysis revealed that GCK exhibited more complex metabolic pathways compared to GT. The metabolites of Ganoderma lucidum fruiting bodies were predominantly influenced by soil physicochemical factors and soil enzyme activity. In the surface soil layer (0-15 cm), the metabolome was significantly affected by soil pH, soil organic matter, available phosphorus, and soil alkaline phosphatase, while in the deeper soil layer (15-30 cm), differences in the Ganoderma lucidum metabolome were more influenced by soil alkaline phosphatase, soil catalase, pH, nitrate nitrogen, and soil sucrase.

Identifiants

pubmed: 38698154
doi: 10.1038/s41598-024-60750-y
pii: 10.1038/s41598-024-60750-y
doi:

Substances chimiques

Soil 0
Nitrogen N762921K75
Phosphorus 27YLU75U4W

Types de publication

Journal Article Research Support, Non-U.S. Gov't

Langues

eng

Sous-ensembles de citation

IM

Pagination

10097

Subventions

Organisme : the Financial Grant Support Program of Lianyungang City, Jiangsu Province, China
ID : QNJJ2310
Organisme : the Second Comprehensive Scientific Expedition to the Qinghai-Tibet Plateau
ID : 2019QZKK0405
Organisme : the Qinghai Province key research and development and transformation plan
ID : 2022-QY-204
Organisme : the Qinghai Province science and technology plan
ID : 2023-ZJ-905T

Informations de copyright

© 2024. The Author(s).

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Auteurs

Wei Ji (W)

Qinghai Province Key Laboratory of Physical Geography and Environmental Process, College of Geographical Science, Qinghai Normal University, Xining, 810008, China.
Lianyungang Academy of Agricultural Sciences, Lianyungang, 222006, China.
Key Laboratory of Tibetan Plateau Land Surface Processes and Ecological Conservation (Ministry of Education), Qinghai Normal University, Xining, 810008, China.

Ni Zhang (N)

Qinghai Province Key Laboratory of Physical Geography and Environmental Process, College of Geographical Science, Qinghai Normal University, Xining, 810008, China.
Key Laboratory of Tibetan Plateau Land Surface Processes and Ecological Conservation (Ministry of Education), Qinghai Normal University, Xining, 810008, China.

Wenying Su (W)

Lianyungang Academy of Agricultural Sciences, Lianyungang, 222006, China.

Xia Wang (X)

Qinghai Province Key Laboratory of Physical Geography and Environmental Process, College of Geographical Science, Qinghai Normal University, Xining, 810008, China.
Key Laboratory of Tibetan Plateau Land Surface Processes and Ecological Conservation (Ministry of Education), Qinghai Normal University, Xining, 810008, China.

Xiaomei Liu (X)

Lianyungang Academy of Agricultural Sciences, Lianyungang, 222006, China.

Yipu Wang (Y)

Lianyungang Academy of Agricultural Sciences, Lianyungang, 222006, China.

Kelong Chen (K)

Qinghai Province Key Laboratory of Physical Geography and Environmental Process, College of Geographical Science, Qinghai Normal University, Xining, 810008, China. 15189021976@163.com.
Key Laboratory of Tibetan Plateau Land Surface Processes and Ecological Conservation (Ministry of Education), Qinghai Normal University, Xining, 810008, China. 15189021976@163.com.
National Positioning Observation and Research Station of Qinghai Lake Wetland Ecosystem in Qinghai, National Forestry and Grassland Administration, Haibei, 812300, China. 15189021976@163.com.

Likai Ren (L)

Lianyungang Academy of Agricultural Sciences, Lianyungang, 222006, China. 2949823@qq.com.

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