Tredennick Andrew T, Kleinhesselink Andrew R, Taylor J Bret, Adler Peter B
Department of Wildland Resources and the Ecology Center, Utah State University, Logan, UT, United States of America.
Department of Ecology and Evolutionary Biology, University of California, Los Angeles, CA, United States of America.
PeerJ. 2018 Mar 13;6:e4485. doi: 10.7717/peerj.4485. eCollection 2018.
Precipitation is predicted to become more variable in the western United States, meaning years of above and below average precipitation will become more common. Periods of extreme precipitation are major drivers of interannual variability in ecosystem functioning in water limited communities, but how ecosystems respond to these extremes over the long-term may shift with precipitation means and variances. Long-term changes in ecosystem functional response could reflect compensatory changes in species composition or species reaching physiological thresholds at extreme precipitation levels.
We conducted a five year precipitation manipulation experiment in a sagebrush steppe ecosystem in Idaho, United States. We used drought and irrigation treatments (approximately 50% decrease/increase) to investigate whether ecosystem functional response remains consistent under sustained high or low precipitation. We recorded data on aboveground net primary productivity (ANPP), species abundance, and soil moisture. We fit a generalized linear mixed effects model to determine if the relationship between ANPP and soil moisture differed among treatments. We used nonmetric multidimensional scaling to quantify community composition over the five years.
Ecosystem functional response, defined as the relationship between soil moisture and ANPP, was similar among irrigation and control treatments, but the drought treatment had a greater slope than the control treatment. However, all estimates for the effect of soil moisture on ANPP overlapped zero, indicating the relationship is weak and uncertain regardless of treatment. There was also large spatial variation in ANPP within-years, which contributes to the uncertainty of the soil moisture effect. Plant community composition was remarkably stable over the course of the experiment and did not differ among treatments.
Despite some evidence that ecosystem functional response became more sensitive under sustained drought conditions, the response of ANPP to soil moisture was consistently weak and community composition was stable. The similarity of ecosystem functional responses across treatments was not related to compensatory shifts at the plant community level, but instead may reflect the insensitivity of the dominant species to soil moisture. These species may be successful precisely because they have evolved life history strategies that buffer them against precipitation variability.
预计美国西部的降水量变化将更大,这意味着降水量高于或低于平均水平的年份将变得更加常见。极端降水期是水资源有限社区生态系统功能年际变化的主要驱动因素,但从长期来看,生态系统对这些极端情况的反应可能会随着降水均值和方差的变化而改变。生态系统功能反应的长期变化可能反映物种组成的补偿性变化,或者物种在极端降水水平下达到生理阈值。
我们在美国爱达荷州的一个蒿属草原生态系统中进行了一项为期五年的降水操纵实验。我们使用干旱和灌溉处理(大约减少/增加50%)来研究在持续的高降水量或低降水量条件下生态系统功能反应是否保持一致。我们记录了地上净初级生产力(ANPP)、物种丰度和土壤湿度的数据。我们拟合了一个广义线性混合效应模型,以确定不同处理之间ANPP与土壤湿度之间的关系是否存在差异。我们使用非度量多维标度法来量化五年间的群落组成。
定义为土壤湿度与ANPP之间关系的生态系统功能反应在灌溉处理和对照处理之间相似,但干旱处理的斜率大于对照处理。然而,土壤湿度对ANPP影响的所有估计值都与零重叠,这表明无论处理如何,这种关系都很弱且不确定。年内ANPP也存在很大的空间变化,这导致了土壤湿度效应的不确定性。在实验过程中,植物群落组成非常稳定,不同处理之间没有差异。
尽管有一些证据表明在持续干旱条件下生态系统功能反应变得更加敏感,但ANPP对土壤湿度的反应一直很弱,群落组成也很稳定。不同处理间生态系统功能反应的相似性与植物群落水平上的补偿性变化无关,而可能反映了优势物种对土壤湿度的不敏感性。这些物种可能正是因为进化出了使其能够抵御降水变化的生活史策略而成功。