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The aeropalynology of Oran's region Es-Senia, northwest Algeria

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The aeropalynology of Oran's region Es-Senia,

northwest Algeria

Ghania Kiared (Ould-Amara)

a

, Jordina Belmonte

b,c

, Mostefa Bessedik

d

and James B. Riding

e

a Department of Pharmacy, Faculty of Medicine, University of Algiers, Algiers, Algeria

b Institut de Ciència i Tecnologia Ambientals - Universitat Autònoma de Barcelona (ICTA-UAB), Spain

c Unitat Botànica - Dept. Biologia Animal, Biologia Vegetal i Ecologia. Universitat Autònoma de Barcelona, Spain

d Palaeoenvironment and Stratigraphical Palaeontology Laboratory, University of Oran 2, Oran El M’Naouer, Algeria

e British Geological Survey, Environmental Science Centre, Nottingham United Kingdom

gkiared@yahoo.fr

A continuous study of atmospheric pollen in Oran Province, northwest Algeria, using the Cour method was undertaken between April 2004 and April 2006. The area studied was the meteorological station at Es-Senia airport (Oran). The aim is to establish the diversity of airborne pollen, the pollination periods of the major taxa, the intensity of pollen emissions and the relationship between airborne pollen calendar and the autochthonous and allochthonous vegetation in the region.

* Es-Sénia airport (Oran) is located at 430 km west of Algiers at latitude 35° 37' 19.11"N and longitude 0°36' 59.46"W (Fig. 1) and 90 m.a.s.l. (I.N.C.T, 2008).

* The climate of Oran includes a dry summer season between June and September, and a variably rainy season between November and April (Bagnouls & Gaussen 1953). It is within the Mediterranean semi-arid with mild winter bioclimatic region (Stewart 1969).

* The main vegetation is composed by Cupressaceae, wild Poaceae, Lygeum, Chenopodiaceae/Amaranthaceae, Urticaceae and there is a big influence of the vegetation from Oran's Sebkha (Alcaraz 1969).

* A Cour device, placed 3 m above ground level at the meteorological station of Es-Sénia airport (Oran), was used to collect airborne pollen on a weekly basis, between April 2004 and April 2006. A filter was exposed for 1 week, and replaced each Saturday at 09:00. Physic-Chemical treatments and pollen analysis followed the methodology described by Cour (1974).

* Data have been converted into mean weekly pollen concentrations (pollen per m3 of air or P/m3) and to Annual Index (AI, sum of the mean weekly concentrations of pollen during an yearly period).

The mean AI for the period studied was 3246 pollen grains/m

3

, only 0.3%

of which could not be identified. The AI of the first year was 4230 pollen

grains/m

3

, significantly higher than the 2258 pollen grains/m

3

of the

second year. The pollen assemblages are dominated by grains from

herbaceous plants (69.5%). Trees and shrubs pollen are respectively

27.9% and 2.3% (Fig 2) (Kiared (Ould-Amara) 2016).

Pollen

from

herbs dominates the assemblages, followed by pollen from trees and pollen from shrubs. The dominance of herbs is due to high

concentrations of Chenopodiaceae/Amaranthaceae, followed by Plantago, wild Poaceae and Asteraceae.

The pollen calendar showed an important inter-annual variability in the airborne pollen content, the predominance of pollen from herbs, the pollen

richness during spring and the importance of the autochthonous vegetation. Pollen from allochthonous plants shows relative low importance.

• Alcaraz C. 1969: Etude géobotanique du pin d’Alep dans le tell Oranais. Thèse de spécialité, Université de Montpellier, 183 p. • Alcaraz C. 1977: Carte de végétation de l’Algérie, Oran. Centre National de Recherches sur les Zones Arides.

• A.S.A.L (Agence Spatiale Algérienne) . 2017 : Wilaya d’Oran. 1 p.

• Bagnouls F., & Gaussen, H. 1953. Les climats biologiques et leur classification. Ann Géo Fr, 355 ; 193-220.

• Cour P. 1974 : Nouvelles techniques de détection des flux et des retombées polliniques. Etude de la sédimentation des pollens déposés à la surface du sol. Pollen et spores, 16, 102-139.

• Cambon G. 1981 : Relation entre le contenu pollinique de l’atmosphère et le couvert végétal en méditerranée occidentale à Montpellier (France), Valence (Espagne), et Oran (Algérie). Thèse de spécialité, Université des Sciences et Techniques du Languedoc, Montpellier. Tome I (texte), Tome II (Illustrations).

• I.N.C.T 2016 : Institut National de Cartographie et de Télédétection.1p.

• Kiared (Ould-Amara) Gh . 2016 : Etude des flux polliniques de l’atmosphère de la région d’Oran à partir de la station météorologique d’Es-Sénia Aéroport. Thèse. Doc. Sc Agro. Ecole Nationale Supérieure d'Agronomie. 300 p. • Kiared (Ould-Amara) Gh; Bessedik M & Riding J. B. 2017: The aeropalynology of Es-Sénia Airport, Oran, northwest Algeria. Journal Palynology, Vol 41, Issue 1 (121-131).

• Santa et Daumas. 1958 : La carte de végétation de l’Algérie (Feuille de Mostaganem) (Echelle : 1/200 000e).

• Steward 1969 : Quotient pluviométrique et dégradation biosphérique. Quelques réflexions. Soc. d’Hist. Nat. d’Afr. du Nord. 59. 23-36.

1. INTRODUCTION

2. MATERIAL AND METHODS

3. RESULTS AND DISCUSSION

4. CONCLUSIONS

5. BIBLIOGRAPHY

Table 2. Pollen calendar of Oran Es-Sénia. * Week number within the year; ** Week number within each month. Elaborated by Kiared (Ould-Amara) 2016.

The relative importance of allochthonous pollen at Oran is low; most pollen is from autochthonous vegetation. The main taxa are

Fig. 2. Annual index (AI) of the study years and average values.

The winter pollen spectrum largely comprised Arecaceae (for only one week) and Cupressaceae pollen. Most pollen grains were collected in spring: total Asteraceae, Brassicaceae, Chenopodiaceae /Amaranthaceae, Lygeum, Olea,

Pinus, Pistacia, Plantago, Poaceae wild type, Quercus, Rumex and Urticaceae. The

higher pollen concentrations were produced by Plantago and wild Poaceae (12 consecutive weeks), Chenopodiaceae/Amaranthaceae (nine weeks) and Olea (eight weeks). During summer Apiaceae and Eucalyptus pollinated, and in autumn only Casuarina pollen was produced. Our results are similar to those of Cambon (1981) for the same region and with the same methodology.

Table 1. Elaborated by

Kiared (Ould-Amara)

2016 from Alcaraz 1977; Santa et Daumas 1958).

Fig. 1. Location of the sampling site at Es-Senia airport (Adapted from ASAL 2014)

(4224) (2250) (3237) (3026) (1488) (2257) (1111) (698) (905) (87) (6) (64) (8) (75) (9) (4230) (2258) (3246) 0 500 1000 1500 2000 2500 3000 3500 4000 4500 2004-2005 2005-2006 2004-2006 Po lle n 99.8 % 99.6 % 99.7 % 26.2 % 71.5 % 2.1 % 100.0 % 0.2 % 2.8 % 30.9 % 65.9 % 100.0 % 27.9 % 69.5 % 100.0 % 0.3 % 2.3 % 0.4 %

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