气候和石膏母质塑造了奇瓦瓦沙漠和莫哈韦沙漠的生物群落和苔藓生态学

IF 5.6 1区 农林科学 Q1 SOIL SCIENCE Geoderma Pub Date : 2024-12-12 DOI:10.1016/j.geoderma.2024.117131
Katelyn G. Gobbie, Nicole Pietrasiak, Brian M. Jusko, Rebecca E. Drenovsky
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引用次数: 0

摘要

建立在石膏土上的生物土壤结皮群落(biocrusts)因其丰富的外观和丰富的地衣和苔藓植物多样性而得到了充分的研究。然而,表征石膏生物结壳的研究主要发生在美国以外,其中大多数缺乏与其他土壤类型的比较。我们对美国奇瓦瓦北部和莫哈韦沙漠东部石膏和非石膏土壤进行了深入的实地调查,以评估石膏露头最广泛的地区,石膏和非石膏土壤上的地表覆盖、生物结皮功能群和苔藓物种的频率。研究地点按地貌分层并配对,使每个石膏遗址与同一地区的非石膏遗址相匹配。我们采用典型对应分析(CCA)将不同土壤类型生物结皮丰度和组成的差异与不同的环境变量联系起来。此外,我们还评估了石膏土壤和非石膏土壤以及奇瓦瓦沙漠和莫哈韦沙漠中生物结皮苔藓的物种丰富度。我们的研究结果表明,石膏和非石膏土壤的生物结壳群落差异主要是由于石膏中大量的暗藻(主要是蓝藻形成的)而不是地衣和苔藓生物结壳。生物外壳功能基团与环境变量的关系不明显。然而,苔藓物种似乎受环境变量的强烈影响,并表现出对基质母质的不同偏好。苔藓物种丰富度在石膏土壤上更大,令人惊讶的是,在最热和最干燥的北美沙漠莫哈韦沙漠。荒漠物种丰富度的差异与年平均气温、季节平均气温以及冬季平均降水量密切相关。总体而言,我们的数据表明,环境和气候条件在美国奇瓦瓦沙漠北部和莫哈韦沙漠东部的生物结皮生态学中发挥了重要作用,特别是苔藓的多样性和分布。更重要的是,我们强调美国石膏土是苔藓形成生物结皮的独特避难所。
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Climate and gypsum parent material shape biocrust communities and moss ecology in the Chihuahuan and Mojave Deserts
Biological soil crust communities (biocrusts) establishing on gypsum soils have been well-documented for their prolific appearance and rich diversity of lichens and bryophytes. However, studies characterizing gypsum biocrusts have occurred primarily outside of the U.S., most of which lack comparisons to other soil types. We conducted intensive field surveys to evaluate the ground cover and frequency of biocrust functional groups and moss species on gypsum and non-gypsum soils in the U.S. regions with the most extensive gypsum outcrops, the northern Chihuahuan and eastern Mojave Deserts. Study sites were stratified by geomorphology and paired, so that every gypsum site was matched with a non-gypsum site in the same region. We employed canonical correspondence analysis (CCA) to relate the observed differences in biocrust abundance and composition across soil types to distinct environmental variables. Additionally, we assessed species richness of biocrust mosses on gypsum versus non-gypsum soils, as well as in the Chihuahuan versus Mojave Deserts. Our results indicate that differences in biocrust communities on gypsum and non-gypsum soils are predominantly due to gypsum’s profuse dark algal (mostly cyanobacteria-formed) rather than lichen and moss biocrusts in these two hot desert biomes. Biocrust functional groups did not exhibit distinct associations with environmental variables. However, moss species appear to be strongly influenced by environmental variables and exhibited differential preferences for substrate parent material. Moss species richness was greater on gypsum soils and, surprisingly, in the hottest and driest North American Desert, the Mojave. Differences in species richness across deserts were strongly correlated to mean annual and seasonal temperatures, as well as mean winter precipitation. Overall, our data suggest that environmental and climate conditions all play important roles in the ecology of biocrusts, specifically moss diversity and distribution, in the northern Chihuahuan and eastern Mojave Deserts of the U.S. More importantly, we emphasize that gypsum soils of the U.S. are unique refugia for moss-forming biocrusts.
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来源期刊
Geoderma
Geoderma 农林科学-土壤科学
CiteScore
11.80
自引率
6.60%
发文量
597
审稿时长
58 days
期刊介绍: Geoderma - the global journal of soil science - welcomes authors, readers and soil research from all parts of the world, encourages worldwide soil studies, and embraces all aspects of soil science and its associated pedagogy. The journal particularly welcomes interdisciplinary work focusing on dynamic soil processes and functions across space and time.
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