Multiporate Pollen of Poaceae as Bioindicator of Environmental Stress: First Archaeobotanical Evidence from the Early–Middle Holocene Site of Takarkori in the Central Sahara
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引用次数: 5
Abstract
This paper reports on the most ancient unusual morphological trait of the apertures of Poaceae pollen found in archaeological layers. In Poaceae, high levels of hybridization, polyploidy, apomixis, and multiporate pollen are often related. Multiple genomes in polyploids are critical for the adaptation of plant species to stresses and could be revealed by anomalies in pollen development. Therefore, the paleoenvironmental research can gain great benefits from identifying polyploids in past contexts by observing anomalous pollen morphology during pollen counts. The occurrence of multiporate pollen in Poaceae has also been related to special features of the ecology of the species showing this anomaly, as well as to climatic and environmental stresses experienced by Poaceae living in a given region. Multiporate and bi- or tri-porate instead of monoporate pollen grains have been observed in samples taken from Takarkori rockshelter, an archaeological site in southwestern Libya (central Sahara) that has been occupied between ~10,200 and ~4650 cal BP. Multiporate pollen was found in organic sands and coprolites of ovicaprines. On the basis of archaeobotanical research, this work aims to investigate whether the presence of supernumerary pores in Poaceae pollen may be an effect of both climatic/hydrological changes and continued anthropogenic pressure on the wild grasses living in the region. The presence of multiporate pollen reveals that Poaceae that lived in central Sahara tackled several kinds of stress during the early and middle Holocene. The Takarkori pollen record suggests that climate change could have played a major role in the early Holocene, while human pressure became stronger during the middle Holocene. The change in environmental conditions determined adaptive responses of polyploid grasses even in the form of multiporate pollen.
本文报道了在考古层中发现的禾科花粉最古老的异常形态特征。在禾科植物中,高水平的杂交、多倍体、无融合和多孢子花粉通常是相关的。多倍体的多基因组是植物适应逆境的关键,可以通过花粉发育的异常来揭示。因此,通过观察花粉计数过程中花粉形态的异常特征来鉴定多倍体对古环境研究具有重要意义。禾科植物多孢花粉的出现也与该物种的特殊生态特征有关,也与禾科植物在特定地区所经历的气候和环境压力有关。在利比亚西南部(撒哈拉中部)的一个考古遗址Takarkori岩洞中,发现了多孔、双孔或三孔而不是单孔的花粉颗粒,该遗址在距今约10200至4650 cal BP之间。在有机砂和粪化石中发现了多孔花粉。在考古植物学研究的基础上,本研究旨在探讨禾科植物花粉中多孔的存在是否可能是气候/水文变化和持续的人为压力对该地区野生牧草的影响。多孔花粉的存在表明,生活在撒哈拉中部的禾本科植物在全新世早期和中期应对了多种压力。Takarkori花粉记录表明,气候变化可能在全新世早期发挥了主要作用,而人类压力在全新世中期变得更强。环境条件的变化决定了多倍体草的适应性反应,甚至以多孢子花粉的形式存在。