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Chemistry, ecology and seasonal succession of Charophytes in the Al-Kharj Irrigation Canal, Saudi Arabia
Authors:M. I. Hussain  Talat M. Khoja  M. Guerlesquin
Affiliation:(1) Department of Botany and Microbiology, Faculty of Science, King Saud University, P.O. Box 2455, 11451 Riyadh, Kingdom of Saudi Arabia;(2) Laboratoire de Biologie Végéitale et de Phytogéographie, Institut de Recherche Fondamentale et Appliquée, 3, Place Andre Leroy, B.P. 808, F-49008 Angers Cedex 01, France
Abstract:We surveyed (Oct. 1991–Sept. 1992) a 16.5-km-long irrigation canal in Al-Kharj City, for its water chemistry, and Charophyte periodicity and density. Marked differences occurred between the origin of a cave-lake, and the final discharge. Six species, Chara globularis, C. vulgaris f. contraria, C. vulgaris var. gymnophylla, C. vulgaris var. longibracteata, C. zeylanica, C. zeylanica var. diaphana f. oerstediana heavily encrust, as opposed to C. benthamii and C. fibrosa. The most widespread were Chara zeylanica and C. benthamii. Chara zeylanica dominated station IV for most of the study period, and ousted all its competitors, such that a 100% monospecific stand was observed here between January and February 1992. The second abundant was Chara benthamii (44%, station II). All Charophytes were seen in the month of November and December 1991, suggesting a luxuriant growth in winter.The water was calcareous, with a high amount of Mg++ (% MathType!MTEF!2!1!+-% feaafiart1ev1aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn% hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr% 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq-Jc9% vqaqpepm0xbba9pwe9Q8fs0-yqaqpepae9pg0FirpepeKkFr0xfr-x% fr-xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaGabmiwayaara% aaaa!36E2![bar X] = 38 mg l–1), Ca++ (% MathType!MTEF!2!1!+-% feaafiart1ev1aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn% hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr% 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq-Jc9% vqaqpepm0xbba9pwe9Q8fs0-yqaqpepae9pg0FirpepeKkFr0xfr-x% fr-xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaGabmiwayaara% aaaa!36E2![bar X] = 121 mg l–1) and reactive-Si (% MathType!MTEF!2!1!+-% feaafiart1ev1aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn% hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr% 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq-Jc9% vqaqpepm0xbba9pwe9Q8fs0-yqaqpepae9pg0FirpepeKkFr0xfr-x% fr-xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaGabmiwayaara% aaaa!36E2![bar X] = 10.8 mg l–1). A gradual decrease in elements/ions (Si = 12 – 8 mg l–1, Cl = 357–251 mg l–1 and CaCO3 390–328 mg l–1) from source to outlet was demonstrated during June. The heavy encrustation of Charophytes is plausibly related to a high concentration of CaCO3 (% MathType!MTEF!2!1!+-% feaafiart1ev1aaatCvAUfeBSjuyZL2yd9gzLbvyNv2CaerbuLwBLn% hiov2DGi1BTfMBaeXatLxBI9gBaerbd9wDYLwzYbItLDharqqtubsr% 4rNCHbGeaGqiVu0Je9sqqrpepC0xbbL8F4rqqrFfpeea0xe9Lq-Jc9% vqaqpepm0xbba9pwe9Q8fs0-yqaqpepae9pg0FirpepeKkFr0xfr-x% fr-xb9adbaqaaeGaciGaaiaabeqaamaabaabaaGcbaGabmiwayaara% aaaa!36E2![bar X] = 364 mg l–1).
Keywords:Charophytes  Chara benthamii  Chara canal  vegetation mapping  periodicity  calcium carbonate
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