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Pedodiversity and Organic Matter Stock of Soils Developed on Sandstone Formations in the Northern Apennines (Italy)

Author

Listed:
  • Livia Vittori Antisari

    (Department of Agricultural and Food Sciences, Alma Mater Studiorum-University of Bologna, Via Fanin, 40, 40127 Bologna, Italy
    Centro Sperimentale per lo Studio e l’Analisi del Suolo (CSSAS), Alma Mater Studiorum-University of Bologna, 40127 Bologna, Italy)

  • William Trenti

    (Department of Agricultural and Food Sciences, Alma Mater Studiorum-University of Bologna, Via Fanin, 40, 40127 Bologna, Italy)

  • Alessandro Buscaroli

    (Department of Biological, Geological, and Environmental Sciences, Alma Mater Studiorum-University of Bologna, Via S. Alberto 163, 48100 Ravenna, Italy)

  • Gloria Falsone

    (Department of Agricultural and Food Sciences, Alma Mater Studiorum-University of Bologna, Via Fanin, 40, 40127 Bologna, Italy)

  • Gilmo Vianello

    (Centro Sperimentale per lo Studio e l’Analisi del Suolo (CSSAS), Alma Mater Studiorum-University of Bologna, 40127 Bologna, Italy)

  • Mauro De Feudis

    (Department of Agricultural and Food Sciences, Alma Mater Studiorum-University of Bologna, Via Fanin, 40, 40127 Bologna, Italy)

Abstract

Pedodiversity is considered the cornerstone of biodiversity. This work aimed to (1) assess pedodiversity according to vegetation, topographic factors, and lithology and to (2) identify the major soil-forming factors on soil organic matter (SOM) stock at a 0–30 cm depth. These goals were reached using data from 147 georeferenced soil profiles distributed along 400–1000 m (≤1000) and 1000–2134 m (>1000) altitudinal gradients in the northern part of the Apennine chain in Italy. Soils showed mainly weak or incipient development (i.e., Entisols and Inceptisols), which could be attributed to sand-based lithology, high slope gradients, and low SOM accumulation rates, which promote soil erosion processes. However, higher pedodiversity was observed at >1000 m than at ≤1000 m, likely due to the higher vegetation cover diversity and climate variability; Spodosols and Mollisols were also found. A greater SOM stock was found at >1000 than ≤1000 m, and vegetation seemed to not affect SOM amounts, suggesting a greater influence of climate on SOM content compared to vegetation. Considering ecosystem conservation, the observed spatial pedodiversity could be considered a critical basis for the protection of soil resources and pedodiversity itself in mountain regions.

Suggested Citation

  • Livia Vittori Antisari & William Trenti & Alessandro Buscaroli & Gloria Falsone & Gilmo Vianello & Mauro De Feudis, 2022. "Pedodiversity and Organic Matter Stock of Soils Developed on Sandstone Formations in the Northern Apennines (Italy)," Land, MDPI, vol. 12(1), pages 1-20, December.
    • Handle: RePEc:gam:jlands:v:12:y:2022:i:1:p:79-:d:1016106
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    References listed on IDEAS

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    1. Valentina Brombin & Enrico Mistri & Mauro De Feudis & Camilla Forti & Gian Marco Salani & Claudio Natali & Gloria Falsone & Livia Vittori Antisari & Gianluca Bianchini, 2020. "Soil Carbon Investigation in Three Pedoclimatic and Agronomic Settings of Northern Italy," Sustainability, MDPI, vol. 12(24), pages 1-19, December.
    2. Fionn Murtagh & Pierre Legendre, 2014. "Ward’s Hierarchical Agglomerative Clustering Method: Which Algorithms Implement Ward’s Criterion?," Journal of Classification, Springer;The Classification Society, vol. 31(3), pages 274-295, October.
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