School of Geography, Development & Environment, University of Arizona, 1064 E. Lowell St., Tucson, AZ 85721, USA.
Department of Geosciences, University of Arizona, 1040 E. 4th St., Tucson, AZ 85721, USA.
Tree Physiol. 2020 Oct 7;40(10):1343-1354. doi: 10.1093/treephys/tpaa083.
Semiarid forests in the southwestern USA are generally restricted to mountain regions where complex terrain adds to the challenge of characterizing stand productivity. Among the heterogeneous features of these ecosystems, topography represents an important control on system-level processes including snow accumulation and melt. This basic relationship between geology and hydrology affects radiation and water balances within the forests, with implications for canopy structure and function across a range of spatial scales. In this study, we quantify the effect of topographic aspect on primary productivity by observing the response of two codominant native tree species to seasonal changes in the timing and magnitude of energy and water inputs throughout a montane headwater catchment in Arizona, USA. On average, soil moisture on north-facing aspects remained higher during the spring and early summer compared with south-facing aspects. Repeated measurements of net carbon assimilation (Anet) showed that Pinus ponderosa C. Lawson was sensitive to this difference, while Pseudotsuga menziesii (Mirb.) Franco was not. Irrespective of aspect, we observed seasonally divergent patterns at the species level where P. ponderosa maintained significantly greater Anet into the fall despite more efficient water use by P. menziesii individuals during that time. As a result, this study at the southern extent of the geographical P. menziesii distribution suggests that this species could increase water-use efficiency as a response to future warming and/or drying, but at lower rates of production relative to the more drought-adapted P. ponderosa. At the sub-landscape scale, opposing aspects served as a mesocosm of current versus anticipated climate conditions. In this way, these results also constrain the potential for changing carbon sequestration patterns from Pinus-dominated landscapes due to forecasted changes in seasonal moisture availability.
美国西南部的半干旱森林通常局限于山区,那里复杂的地形增加了描述林分生产力的难度。在这些生态系统的异质特征中,地形是控制包括积雪积累和融化在内的系统水平过程的重要因素。这种地质学和水文学之间的基本关系影响了森林内的辐射和水分平衡,对树冠结构和功能在一系列空间尺度上都有影响。在这项研究中,我们通过观察两种优势乡土树种对能量和水分输入的时间和幅度在亚高山源流域内季节性变化的响应,量化了地形方位对初级生产力的影响。平均而言,与南坡相比,北坡的土壤湿度在春季和初夏期间保持较高水平。对净碳同化(Anet)的重复测量表明,黄松对这种差异很敏感,而花旗松则不然。无论方位如何,我们在物种水平上观察到了季节性差异,其中黄松尽管在这段时间内花旗松个体的水分利用效率更高,但仍能在秋季保持显著更高的 Anet。因此,这项在花旗松地理分布南端进行的研究表明,该物种可能会提高水分利用效率以应对未来的变暖或变干,但相对于更耐旱的黄松,其生产力增长速度较低。在亚景观尺度上,相反的方位充当了当前和预期气候条件的中间尺度。通过这种方式,这些结果还限制了由于季节性水分可用性的预测变化,可能导致以松属为主的景观的碳固存模式发生变化。