Phytoclimatological study in the high plains of Sétif: application of the bioclimatic classification system (Algeria)

Autores

  • Bariza Gourari
  • François Mesner
  • Khaled Zarroug
  • Nacira Boulaacheb
  • Samia Bouzouaid
  • Belkhodja Badr Eddine

DOI:

https://doi.org/10.34188/bjaerv7n4-001

Palavras-chave:

bioclimate, macrobioclimate, ombrotype, thermotype, continentality, isobioclimates, bioclimatic system classification, climate change

Resumo

The Global Bioclimatic Classification System (WBCS) by Rivas-Martínez is an effective approach to reflect and study the role of climate in determining the potential distribution of natural vegetation at various temporal and spatial scales. In particular, the diversity of physical characteristics in the Setifian high plains leads to the complexity of large-scale phytogeographic belts. Isobioclimates, unique combinations of bioclimatic indices (continentality, ombrotype, and thermotype), have been created for the study area based on Rivas-Martínez's global bioclimatic classification system for current and future climate scenarios, using the parallel climate model from CMIP5 (Coupled Model Intercomparison Project) under the intermediate greenhouse gas emission scenario (RCP4.5). Precipitation and temperature data from the "WorldClim" dataset were used as the data source. These climatic variables were reduced to a spatial resolution of 1 km. The objective is to understand how the climate is evolving in this region, what the consequences are, and what the future holds for these natural ecosystems. A phytosociological study complemented by satellite image analysis reveals a high diversity of pre-forestry formations. The digitally mapped results were used to 1) assess the relative redistribution of isobioclimates and the magnitude of change, 2) identify and locate the new projected isobioclimates, and 3) explore the compositional changes in vegetation types among analogous isobioclimatic zones. The ordination of the relationships between vegetation and bioclimates shows a strong correlation between Rivas-Martinez indices and the distribution and composition of vegetation. Changes in ombrotype, thermotype, bioclimate, ombrotype, and isobioclimate differed between the current and future series. The resulting map presents 9 isobioclimatic units, which are advantageous for confirming the diagnosis of bioclimatic characteristics and describing the relationships between climatic variables and the corresponding distributions of natural vegetation. We identified eight different isobioclimates for the current period (1979-2013) and seven for the future period (2050), three thermotype horizons for both the current and future periods, and finally, four ombrotype horizons for the period (1979-2013), while two ombrohorizons represent the period (2050). This approach is useful for explaining territorial diversity in environmental applications related to ecological adaptation assessment, nature conservation, landscape regionalization, and planning.

Referências

Emberger L., (1971). Travaux de botanique et d'écologie. Masson éd. Paris, 520p. GAUTHIER B., M. GODRON, P. HERNIAUX et J. LEPART, 1977.- Un type complémentaire de profil écologique «indicé». Can. J. Bot., 55 (23), 2859-2865.

Gavilán , R., F. Fernández-González & C. Blasi, (1998). Climatic classification and ordination of the Spanish Sistema Central: relationships with potential vegetation. Plant Ecol., 139, 1-11.

Géhu, J.-M. (2006). Dictionnaire de sociologie et synécologie végétales. — Berlin-Stuttgart : Cramer 2006. — 899 p.

Gordon, M. (1971). Essai sur une approche probabiliste de l’écologie des végétaux. Montpellier, Thèse de doctorat d’État, Université des Sciences et Techniques du Languedoc, 247 p. 10.3406/ecmed.1982.1946

Guiot, J. (1981). Analyse mathématique de données géophysiques, application à la dendroclimatologie. Thèse, Inst. Astr. Géoph., UCL, Louvain-La-Neuve, 170 pp. + 58 fig. h.t.

Hotelling, H. (1933). Analysis of a complex of statistical variables into principal components. Journal of Educational Psychology, 24, 417-441. http://dx.doi.org/10.1037/h0071325

Karger, D. N; Conrad, O; Böhner, J; Kawohl ,T; Kreft, H; Soria-Auza, R. W; Zimmermann, N; Linder, P. H; Kessler, M. (2017). Climatologies at high resolution for the earth's land surface areas. Scientific Data. 4, 10.1038/sdata.2017.122.

Le Floch, E. (1984). Contribution à une étude ethnobotanique de la flore tunisienne. Publ. Sci. tunisiennes, Programme flore et végétation tunisiennes, préface de M. Abdelhamid Nabli, Impr. off. Républi. Tunis.

Le Houerou, H. N. (1969). La végétation de la Tunisie steppique (1) (Structure, écologie, sociologie, répartition, évolution, utilisation, biomasse, productivité) (avec référence aux végétations analogues d’Algérie, de Libye et du Maroc). Annales de l’Institut National de la Recherche Agronomique de la Tunisie, 42, 622p.

Lecompte, M, (1988). La phytoclimatologie dynamique : une approche différente de la nature du climat. Espace géographique (Persée - Portail des revues scientifiques en SHS)- Vol. 17, Iss: 2, pp 109-121 Journal Article DOi : https://www.persee.fr/doc/spgeo_0046-2497_1988_num_17_2_2757

Lecompte, M., (1987). “Essai de phytoclimatologie dans le Moyen-Atlas marocain”, Acta oecologica (Oecol. Gener.), 8, 4, 523-535.10.3406/spgeo.1988.2757

Lecompte, M., (1989). “La question des limites climatiques à travers la climatologie et la phytoclimatologie dynamiques”, La Météorologie, 7e série, 29, 3-8.

Li, S; Zhang, X; Lu, Z ; Ni , J & Lu , J, (2024). Progress of vegetation modelling and future research prospects. Sci. China Earth Sci. 67, 2718–2738 (2024). https://doi.org/10.1007/s11430-023-1367-1

Loarie, S.R., Duffy, P.B., Hamilton, H., Asner, G.P., Field, C.B. & Ackerly, D.D. (2009). The velocity of climate change. Nature, 462, 1052–1055.

López Fernández ,M. L. ; Peña Angulo , D ; García, R.M ; López Fernández, M.S ; González Hidalgo, J.C. (2016). Variations entre les isobioclimats (1951-1980 et 1981-2010) dans la péninsule espagnole. 2015, ISBN 978-84-16724-19-2, pp. 205-214. Espagnol .X Congreso Internacional AEC: Clima, sociedad, riesgos y ordenación del territorio DOI: http://dx.doi.org/10.14198/XCongresoAECAlicante2016-19

Metzger, M. J; Bunce, R. G; Jongman, R. H; Sayre R; Trabucco, A; Zomer, R., (2013). High‐resolution bioclimate map of the world. Global Ecology and Biogeography, 22, 630-638. Doi:10.1111/geb.12022.

Noce, S; Caporaso, L. & Santini, M. (2020). A new global dataset of bioclimatic indicators. Sci Data 7, 398 (2020). https://doi.org/10.1038/s41597-020-00726-5

Otgonbayar, M; Atzberger, C; Sumiya, E. Dalantai , S; Chambers, J. (2022). Estimation of bioclimatic variables of Mongolia derived from remote sensing data. Front. Earth Sci. 16, 323–339 (2022). https://doi.org/10.1007/s11707-020-0862-9

Ozenda, P; Borel, J.L. (2000). An ecological map of Europe: why and how? Comptes Rendus Académie Sci. - Ser. III - Sci. Vie. 323 (2000) 983–994. https://doi.org/, doi:10.1016/S0764-4469(00)01227-0

Pearson, R; Dawson, T. (2003). Predicting the impacts of climate change on the distribution of species: Are bioclimate envelope models useful? Global Ecol Biogeog 12: 361.

Pesaresi, S., Galdenzi, D., Biondi, E., & Casavecchia, S. (2014). Bioclimate of Italy: application of the worldwide bioclimatic classification system, Journal of Maps, 10, 538-553. DOI: 10.1080/17445647.2014.891472

Piñas, S., López, F., M.S. y López Fernández, M.L. (2008a). Termotipos de la España Peninsular y Balear, y su cartografía. Publicaciones de Biología de la Universidad de Navarra. Serie Botánica, Volumen 17, pp 237-242.

Piñas, S., López, M.L. & López Fernández, M.S. (2009). Andalucía: Cartografía y áreas de sus Bioclimas, Continentalidad, Termotipos y Ombrotipos. En “Biogeografía Scientia Biodiversitatis”· (Actas del V Congreso Español de Biogografía. Málaga 9-12 de septiembre 2008). Ed. Real, R. y Márquez, A.L., pp. 109-119.

Rhanem, M. (2013). La topoclimatologie, un outil au service de l’écologie. Applications et implications possibles au niveau de la gestion des forêts d’altitude des montagnes du Moyen et Haut Atlas (Maroc). Quad. Bot. Amb. Appl, 24(2013), 77-107.

Riccardo T; Fabio A; Borja J.A, (2020). Global distribution and bioclimatic characterization of alpine biomes. Ecography. Volume 43, Issue 6Jun 2020Pages779-942. https://doi.org/10.1111/ecog.05012

Rivas Martinez, S.; Sanchez Mata, D; Costa, M. (1999). North American Boreal and Western Temperate Forest Vegetation (Syntaxonomical Synopsis of the Potential Natural Plant Communities of North America, II). Itinera Geobot, 12, 5-316.

Rivas-Martinez ,S (1997). Syntaxonomical synopsis of the potential natural plant communities of North America. Itinera Geobota´nica 10: 5–148. 21.

Rivas-Martínez S., Rivas-Sáenz S., Penas A. (2011a). Worldwide Bioclimatic Classification System. Global Geobotany. 1, 1-638.

Rivas-Martínez, S. & Rivas-Saenz, S. (1996-2017). Worldwide Bioclimatic Classificacion System. Phytosociological Research Center, Spain. http://globalbioclimatics.org/

Rivas-Martínez, S. (2004). Global Bioclimatics (Clasificación Bioclimática de la Tierra) (Versión 27-08-2004), Worldw. Bioclimatic Classif. Syst. (2004) http://www.globalbioclimatics.org/book/bioc/global_bioclimatics_0.htm. (accessed February 3, 2020).

Rivas-Martínez, S. (2005). Notions on Dynamic-Catenal Phytosociology as a Basis of Landscape Science. Plant Biosystems, 139, 135-144.https://doi.org/10.1080/11263500500193790

Rivas-Martínez, S. (2008). Globalbioclimatics, Internet: http:// www. globalbioclimatics.org.

Rivas-Martínez, S., Rivas Sáenz, S., Penas, Á. & col. (2011b). Worldwide Bioclimatic Classification System. Global Geobotany, 1: 1-634 + 4 Maps

Rivas-Martínez,S, Penas A, Luengo MA, Rivas-Sa´enz S (2003). Worldwide Bioclimatic Classification System. In: H.. Lieth, editor. CD-Series II: Climate and Biosphere. Spain: Phytosociological Research Center.

Sancho García, I ; Fidalgo Hijano, C (2007). Modelo de interpretación fitoclimática de la dinámica vegetal. Aplicación a la cuenca madrileña del Alberche. (Instituto de Economía y Geografía). ESTUDIOS GEOGRÁFICOS- Vol. 68, Iss: 262, pp 295-320. DOÏ : https://doi.org/10.3989/egeogr.2007.i262.14

Simmons, J.M, Richmond ,B.J. (2008). Dynamic changes in representations of preceding and upcoming reward in monkey orbitofrontal cortex. Cereb Cortex 18:93–103.

Torregrosa A., Taylor M. D., Flint L. E., Flint A.L., 2013. Present, Future, and Novel Bioclimates of the San Francisco, California Region. PLOS ONE 8 (3): e58450. https://doi.org/10.5616/gg110001.

Urdiales, D; Zittis, G; Hadjinicolaou, P.(2022). Climate Change in Mediterranean climate-type regions: A global approach based on the Köppen-Geiger classification, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-2802, https://doi.org/10.5194/egusphere-egu22-2802, 2022

Whittaker, R. H., (1967). “Gradient analysis of vegetation”, Biological Review, 42, 207-264.

Zscheischler, J; Mahecha, M.D; Harmeling S. (2012),. Climate classifications: the value of unsupervised clustering. Procedia Comput., Sci.9, 897-907. XXXIIIème Coll.

Downloads

Publicado

2024-10-11

Como Citar

Gourari, B., Mesner, F., Zarroug, K., Boulaacheb, N., Bouzouaid, S., & Eddine, B. B. (2024). Phytoclimatological study in the high plains of Sétif: application of the bioclimatic classification system (Algeria). Brazilian Journal of Animal and Environmental Research, 7(4), e73560 . https://doi.org/10.34188/bjaerv7n4-001

Edição

Seção

Artigos originais