Department of Environmental Sciences and Energy Research, Weizmann Institute of Science, Rehovot, Israel.
Oecologia. 2011 Oct;167(2):573-85. doi: 10.1007/s00442-011-2010-4. Epub 2011 May 18.
Motivated by persistent predictions of warming and drying in the entire Mediterranean and other regions, we have examined the interactions of intrinsic water-use efficiency (W(i)) with environmental conditions in Pinus halepensis. We used 30-year (1974-2003) tree-ring records of basal area increment (BAI) and cellulose (13)C and (18)O composition, complemented by short-term physiological measurements, from three sites across a precipitation (P) gradient (280-700 mm) in Israel. The results show a clear trend of increasing W(i) in both the earlywood (EW) and latewood (LW) that varied in magnitude depending on site and season, with the increase ranging from ca. 5 to 20% over the study period. These W(i) trends were better correlated with the increase in atmospheric CO(2) concentration, C(a), than with the local increase in temperature (~0.04°C year(-1)), whereas age, height and density variations had minor effects on the long-term isotope record. There were no trends in P over time, but W(i) from EW and BAI were dependent on the interannual variations in P. From reconstructed C(i) values, we demonstrate that contrasting gas-exchange responses at opposing ends of the hydrologic gradient underlie the variation in W(i) sensitivity to C(a) between sites and seasons. Under the mild water limitations typical of the main seasonal growth period, regulation was directed at increasing C(i)/C(a) towards a homeostatic set-point observed at the most mesic site, with a decrease in the W(i) response to C(i) with increasing aridity. With more extreme drought stress, as seen in the late season at the drier sites, the response was W(i) driven, and there was an increase in the W(i) sensitivity to C(a) with aridity and a decreasing sensitivity of C(i) to C(a). The apparent C(a)-driven increases in W(i) can help to identify the adjustments to drying conditions that forest ecosystems can make in the face of predicted atmospheric change.
受整个地中海和其他地区变暖变干的持续预测的影响,我们研究了内在水分利用效率(W(i))与在地中海地区的油松(Pinus halepensis)环境条件之间的相互作用。我们使用了来自以色列三个降水梯度(280-700 毫米)站点的 30 年(1974-2003 年)树木年轮记录的基面积增量(BAI)和纤维素(13)C 和(18)O 组成,这些记录通过短期生理测量得到了补充。结果表明,在早材(EW)和晚材(LW)中,W(i)呈现出明显的增加趋势,其幅度取决于地点和季节,在研究期间,增加幅度约为 5-20%。这些 W(i)趋势与大气 CO(2)浓度(C(a))的增加相关性更好,而与当地气温升高(约 0.04°C 年(-1))相关性较差,而年龄、高度和密度变化对长期同位素记录的影响较小。在过去的时间里,P 没有呈现出趋势,但 EW 和 BAI 的 W(i)依赖于 P 的年际变化。从重建的 C(i)值来看,我们证明了在水文梯度两端相反的气体交换响应是导致不同地点和季节 W(i)对 C(a)敏感性差异的基础。在典型主季节性生长期间轻度水分限制的情况下,调节作用旨在通过增加 C(i)/C(a),使 C(i)/C(a)朝着最湿润地点的稳态设定点方向发展,随着干旱程度的增加,W(i)对 C(i)的响应呈下降趋势。在更极端的干旱胁迫下,如在较干燥地点的后期季节中看到的那样,响应是由 W(i)驱动的,W(i)对 C(a)的敏感性随干旱程度的增加而增加,而 C(i)对 C(a)的敏感性随干旱程度的增加而降低。W(i)对 C(a)的明显增加可能有助于识别森林生态系统在面对预测的大气变化时可以对干燥条件做出的调整。