Ripley Brad S, Pammenter Norman W
Botany Department, Rhodes University, P.O. Box 94, 6140 Grahamstown, South Africa.
Oecologia. 2004 May;139(4):535-44. doi: 10.1007/s00442-004-1535-1. Epub 2004 Mar 23.
Water status in relation to standing biomass and leaf area indices (LAI) of the subtropical foredune species Arctotheca populifolia, Ipomoea pes-caprae and Scaevola plumieri were studied in the Eastern Cape, South Africa. The plants showed little evidence of water stress, never developing leaf water potentials more negative than -1.55 MPa, a value which is typical of mesophytes rather than xerophytes. The plants showed no seasonal changes in osmotic potential, an indication that they did not need to osmoregulate, nor were there significant alterations in tissue elasticity. Turgor potential for the most part remained positive throughout the day or recovered positive values at night, a condition suitable for the maintenance of growth that may be essential to cope with sand accretion. All three species show relatively high transpiration rates and only I. pes-caprae showed any evidence of strong limitations of transpiration rate through reductions in midday stomatal conductance. All three species had relatively high instantaneous water use efficiencies as a result of high assimilation rates rather than low transpiration rates. Simple water budgets, accounting for losses by transpiration and inputs from rainfall, suggest that the water stored in the dune sands is sufficient to meet the requirements of the plants, although water budgets calculated for I. pes-caprae suggest that this species may on occasion be water limited. The results suggest that it is the low biomass and LAI that lead to these favourable water relations.
在南非东开普省,对亚热带前沙丘物种蓝目菊、厚藤和草海桐的水分状况与现存生物量及叶面积指数(LAI)之间的关系进行了研究。这些植物几乎没有水分胁迫的迹象,叶片水势从未低于-1.55 MPa,这一数值是中生植物而非旱生植物的典型特征。这些植物的渗透势没有季节性变化,这表明它们无需进行渗透调节,组织弹性也没有显著变化。膨压在一天中的大部分时间里保持正值,或者在夜间恢复正值,这种情况有利于维持生长,这对于应对沙丘堆积可能至关重要。所有这三个物种的蒸腾速率都相对较高,只有厚藤表现出通过中午气孔导度降低而对蒸腾速率有强烈限制的迹象。由于同化率高而非蒸腾速率低,所有这三个物种都具有相对较高的瞬时水分利用效率。简单的水分平衡,考虑到蒸腾损失和降雨输入,表明沙丘沙子中储存的水分足以满足植物的需求,尽管对厚藤计算的水分平衡表明该物种有时可能受到水分限制。结果表明,是低生物量和叶面积指数导致了这些有利的水分关系。