Palaeo-Science and History (PS&H) Independent Research Group, Max Planck Institute for the Science of Human History, Jena, Germany.
Department of Environmental Biology, Sapienza University of Rome, Rome, Italy.
PLoS One. 2022 Jul 15;17(7):e0271548. doi: 10.1371/journal.pone.0271548. eCollection 2022.
This study provides a high-resolution reconstruction of the vegetation of the Argive Plain (Peloponnese, Greece) covering 5000 years from the Early Bronze Age onwards. The well dated pollen record from ancient Lake Lerna has been interpreted in the light of archaeological and historical sources, climatic data from the same core and other regional proxies. Our results demonstrate a significant degree of human impact on the environments of the Argive Plain throughout the study period. During the Early Bronze Age evidence of a thermophilous vegetation is seen in the pollen record, representing the mixed deciduous oak woodland of the Peloponnesian uplands. The plain was mainly used for the cultivation of cereals, whereas local fen conditions prevailed at the coring site. Towards the end of this period an increasing water table is recorded and the fen turns into a lake, despite more arid conditions. In the Late Bronze Age, the presence of important palatial centres modified the landscape resulting in decrease of mixed deciduous oak woodland and increase in open land, partly used for grazing. Possibly, the human management produced a permanent hydrological change at Lake Lerna. From the Archaic period onwards the increasing human pressure in association with local drier conditions caused landscape instability, as attested by a dramatic alluvial event recorded in the Pinus curve at the end of the Hellenistic Age. Wet conditions coincided with Roman times and favoured a forest regeneration pattern in the area, at the same time as we see the most intensive olive cultivation in the pollen record. The establishment of an economic landscape primarily based on pastures is recorded in the Byzantine period and continues until modern times. Overgrazing and fires in combination with arid conditions likely caused degradation of the vegetation into garrigue, as seen in the area of the Argive Plain today.
本研究提供了一幅分辨率很高的阿尔戈斯平原(希腊伯罗奔尼撒半岛)植被重建图,时间跨度从青铜时代早期一直到 5000 年前。来自古代勒拿湖的经过良好年代测定的花粉记录,结合考古和历史资料、来自同一岩芯的气候数据以及其他区域代用指标进行了解释。我们的研究结果表明,在整个研究期间,人类对阿尔戈斯平原的环境都产生了重大影响。在青铜时代早期,花粉记录中出现了喜热植被的证据,代表了伯罗奔尼撒高原混合落叶橡树林。平原主要用于谷物种植,而岩芯采集地则以当地的沼泽条件为主。在这个时期的末期,记录到地下水位不断上升,尽管气候较为干燥,但沼泽地变成了湖泊。在青铜时代晚期,重要的宫殿中心的存在改变了景观,导致混合落叶橡树林减少,开阔地增加,部分用于放牧。可能是人类管理导致了勒拿湖的永久性水文变化。从古风时期开始,不断增加的人类压力加上当地较干燥的条件导致了景观不稳定,这在希罗多德时期结束时记录的松树曲线中可以明显看到。湿润的条件与罗马时期相吻合,有利于该地区的森林再生模式,同时在花粉记录中我们也看到了最密集的橄榄种植。以牧场为基础的经济景观的建立记录在拜占庭时期,并一直延续到现代。过度放牧和火灾与干旱条件相结合,可能导致植被退化到灌木草丛,这在今天的阿尔戈斯平原地区可见一斑。