Abstract

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.

Highlights

  • California chaparral is a vegetation type with an extensive diversity of woody evergreen shrub species (Cooper 1922; Epling and Lewis 1942; Keeley and Keeley 1988)

  • Ecology and Evolution published by John Wiley & Sons Ltd

  • In the principal components analysis (PCA) of environmental variables, sample plots were well defined by climate zone groups along the first axis (28.6% of variance explained, Fig. 3) with six climate variables associated with the summer marine layer generally having the highest eigenvalues

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Summary

Introduction

California chaparral is a vegetation type with an extensive diversity of woody evergreen shrub species (Cooper 1922; Epling and Lewis 1942; Keeley and Keeley 1988). Other Mediterranean-type climate (MTC) regions are global biodiversity hot spots with a richer floristic diversity compared with other temperate zone vegetation (e.g., fynbos in South Africa and kwongan in Southwestern Australia). Processes influencing this diversity relate in part to long, hot, and dry summers and short, mild, and wet winters characteristic of MTC. Woody plant growth is stimulated by rainfall during the wet season which leads to biomass accumulation, but plants dry out during the long dry season.

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