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Distribution modelling of pre-Columbian California grasslands with soil phytoliths: New insights for prehistoric grassland ecology and restoration

机译:哥伦比亚前加州草地与土壤植物石料的分布模型:史前草原生态学和恢复的新见解

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摘要

Historical reconstructions of plant community distributions are useful for biogeographic studies and restoration planning, but the quality of insights gained depends on the depth and reliability of historical information available. For the Central Valley of California, one of the most altered terrestrial ecosystems on the planet, this task is particularly difficult given poor historical documentation and sparse relict assemblages of pre-invasion plant species. Coastal and interior prairies were long assumed to have been dominated by perennial bunchgrasses, but this hypothesis has recently been challenged. We evaluated this hypothesis by creating species distribution models (SDMs) using a novel approach based on the abundance of soil phytoliths (microscopic particles of biogenic silica used as a proxy for long-term grass presence) extracted from soil samples at locations statewide. Modeled historical grass abundance was consistently high along the coast and to a lesser extent in higher elevation foothills surrounding the Central Valley. SDMs found strong associations with mean temperature, temperature variability, and precipitation variability, with higher predicted abundance in regions with cooler, equable temperatures and moderated rainfall, mirroring the pattern for modern perennial grass distribution across the state. The results of this study strongly suggest that the pre-Columbian Central Valley of California was not dominated by grasses. Using soil phytolith data as input for SDMs is a promising new method for predicting the extent of prehistoric grass distributions where alternative historical datasets are lacking.
机译:植物群落分布的历史重建对于生物地理学研究和恢复规划很有用,但是获得的见解的质量取决于可用历史信息的深度和可靠性。对于地球上变化最大的陆地生态系统之一的加利福尼亚中央谷地而言,鉴于历史文献不多且入侵前植物物种的遗体稀少,这一任务尤其困难。长期以来,沿海和内陆的草原一直被多年生的束草所控制,但是这一假设最近受到了挑战。我们使用一种新颖的方法,基于从全州范围内的土壤样品中提取的土壤植石体(用作长期草存在的代表的生物二氧化硅的细微颗粒),采用一种新颖的方法,通过创建物种分布模型(SDM)来评估该假设。模拟的历史草地丰度在沿海地区一直很高,而在中央山谷周围较高海拔的山麓地区则较少。 SDM发现与平均温度,温度变化率和降水变化率有很强的联系,在凉爽,温度适中和降雨适度的地区,预测丰度更高,这反映了该州现代多年生草的分布格局。这项研究的结果有力地表明,前哥伦布时期的加利福尼亚中央谷地并不以草为主。使用土壤植石数据作为SDM的输入是一种有前途的新方法,可用于预测缺乏替代历史数据集的史前草类分布的范围。

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    Stephen E. Fick; Rand R. Evett;

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  • 年(卷),期 -1(13),4
  • 年度 -1
  • 页码 e0194315
  • 总页数 16
  • 原文格式 PDF
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