Weng Chengyu, Hooghiemstra Henry, Duivenvoorden Joost F
Institute for Biodiversity and Ecosystem Dynamics (IBED), University of Amsterdam, Kruislaan 318, 1098 SM Amsterdam, The Netherlands.
Philos Trans R Soc Lond B Biol Sci. 2007 Feb 28;362(1478):253-62. doi: 10.1098/rstb.2006.1985.
Change in diversity of fossil pollen through time is used as a surrogate for biodiversity history. However, there have been few studies to explore the sensitivity of the measured pollen diversity to vegetation changes and the relationship between pollen diversity and plant diversity. This paper presents results of a study to assess the relationship between pollen diversity and relative abundance of pollen from different altitudinal vegetation belts (subandean forest, Andean forest, subparamo and grassparamo) in three records from the tropical Andes in Colombia. The results indicated that plant diversity in the vegetation declined with altitude and pollen diversity is positively correlated to the abundance of pollen from lower altitude vegetation belts and negatively correlated to that from the grassparamo. These results, therefore, suggest that pollen diversity coarsely reflects the diversity of the surrounding vegetation. Using this interpretation, we were able to predict changes in plant diversity over the past 430000 years in the Colombian Andes. Results indicated that under warmer climatic conditions, more species-diverse vegetation of low elevation moved upslope to contribute more pollen diversity to the study sites, and under colder conditions, species-poor grassparamo moved downslope and observed pollen diversity was lower. This study concludes that fossil pollen diversity may provide an important proxy to reconstruct the temporal changes in plant diversity.
化石花粉多样性随时间的变化被用作生物多样性历史的替代指标。然而,很少有研究探讨所测量的花粉多样性对植被变化的敏感性以及花粉多样性与植物多样性之间的关系。本文展示了一项研究的结果,该研究旨在评估哥伦比亚热带安第斯地区三个记录中花粉多样性与来自不同海拔植被带(亚安第斯森林、安第斯森林、亚高山草甸和高山草甸)的花粉相对丰度之间的关系。结果表明,植被中的植物多样性随海拔降低,花粉多样性与来自低海拔植被带的花粉丰度呈正相关,与来自高山草甸的花粉丰度呈负相关。因此,这些结果表明花粉多样性大致反映了周围植被的多样性。基于这种解释,我们能够预测哥伦比亚安第斯地区过去43万年植物多样性的变化。结果表明,在气候较暖的条件下,更多物种丰富的低海拔植被向上坡移动,为研究地点贡献了更多的花粉多样性;而在气候较冷的条件下,物种贫乏的高山草甸向下坡移动,观测到的花粉多样性较低。本研究得出结论,化石花粉多样性可能为重建植物多样性的时间变化提供一个重要的代理指标。