Vasey Michael C, Parker V Thomas, Holl Karen D, Loik Michael E, Hiatt Seth
Department of Environmental Studies, University of California Santa Cruz, California ; Department of Biology, San Francisco State University San Francisco, California.
Department of Biology, San Francisco State University San Francisco, California.
Ecol Evol. 2014 Sep;4(18):3662-74. doi: 10.1002/ece3.1211. Epub 2014 Sep 4.
We investigated the hypothesis that maritime climatic factors associated with summer fog and low cloud stratus (summer marine layer) help explain the compositional diversity of chaparral in the coast range of central California. We randomly sampled chaparral species composition in 0.1-hectare plots along a coast-to-interior gradient. For each plot, climatic variables were estimated and soil samples were analyzed. We used Cluster Analysis and Principle Components Analysis to objectively categorize plots into climate zone groups. Climate variables, vegetation composition and various diversity measures were compared across climate zone groups using ANOVA and nonmetric multidimensional scaling. Differences in climatic variables that relate to summer moisture availability and winter freeze events explained the majority of variance in measured conditions and coincided with three chaparral assemblages: maritime (lowland coast where the summer marine layer was strongest), transition (upland coast with mild summer marine layer influence and greater winter precipitation), and interior sites that generally lacked late summer water availability from either source. Species turnover (β-diversity) was higher among maritime and transition sites than interior sites. Coastal chaparral differs from interior chaparral in having a higher obligate seeder to facultative seeder (resprouter) ratio and by being dominated by various Arctostaphylos species as opposed to the interior dominant, Adenostoma fasciculatum. The maritime climate influence along the California central coast is associated with patterns of woody plant composition and β-diversity among sites. Summer fog in coastal lowlands and higher winter precipitation in coastal uplands combine to lower late dry season water deficit in coastal chaparral and contribute to longer fire return intervals that are associated with obligate seeders and more local endemism. Soil nutrients are comparatively less important in explaining plant community composition, but heterogeneous azonal soils contribute to local endemism and promote isolated chaparral patches within the dominant forest vegetation along the coast.
与夏季雾气和低云层(夏季海洋层)相关的海洋气候因素有助于解释加利福尼亚中部海岸山脉灌丛群落的组成多样性。我们沿着从海岸到内陆的梯度,在0.1公顷的样地中随机采样灌丛物种组成。对于每个样地,估算气候变量并分析土壤样本。我们使用聚类分析和主成分分析将样地客观地分类为气候区组。使用方差分析和非度量多维标度法,比较了各气候区组的气候变量、植被组成和各种多样性指标。与夏季水分供应和冬季冰冻事件相关的气候变量差异解释了测量条件下的大部分变异,并与三种灌丛群落相吻合:海洋型(夏季海洋层最强的低地海岸)、过渡型(夏季海洋层影响较弱且冬季降水量较大的高地海岸)以及通常在夏末缺乏任何一种水源的内陆地区。海洋型和过渡型样地之间的物种周转率(β多样性)高于内陆样地。沿海灌丛与内陆灌丛的不同之处在于,前者专性种子植物与兼性种子植物(萌生植物)的比例更高,且以各种熊果属物种为主导,而不是像内陆那样以帚石楠为主导。加利福尼亚中部海岸沿线的海洋气候影响与木本植物组成模式以及各地点之间的β多样性有关。沿海低地的夏季雾气和沿海高地较高的冬季降水量共同作用,降低了沿海灌丛在旱季后期的水分亏缺,并导致更长的火灾间隔期;这些间隔期与专性种子植物以及更多的地方特有种有关。土壤养分在解释植物群落组成方面相对不太重要,但非地带性土壤的异质性有助于形成地方特有种,并在沿海占主导地位的森林植被中促进孤立的灌丛斑块的形成。