2015
DOI: 10.1163/22134522-12340053
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Regional Vegetation Histories: An Overview of the Pollen Evidence from the Central Mediterranean

Abstract: Vegetation patterns during the 1st millennium AD in the central Mediterranean, exhibit a great variability, due to the richness of these habitats and the continuous shaping of the environment by human societies. Variations in land use, witnessed in the pollen record, reflect the role that local vegetation and environmental conditions played in the choices made by local societies. The interdisciplinary study of off-site cores remains the key evidence for palaeoenvironmental transformations mirroring the ‘semi-n… Show more

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Cited by 8 publications
(6 citation statements)
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“…The sites for the north are all but one from within the meso-Mediterranean and supra-Mediterranean zones, and all but three are located at medium and high elevation (>260 masl), while all samples for the south derive from the thermo-Mediterranean zone, and all but one are located at low elevations (most around 20 masl) ( Figure 1b, Supplementary Table 2, available online). The differences in the API can also (to some extent) be associated with the fact that most of the core locations in the north do not have any major settlements within their catchments, with the exception of the Orestias core that clearly records activity from the nearby settlement of Dispilió, with increased human activity during Neolithic, Hellenistic and Roman times (Kouli, 2015;Kouli et al, 2018;Mercuri et al, this volume). In contrast, most pollen core locations in the south are within regions for which archaeological remains suggest high human activity (if not specifically on site).…”
Section: Pollenmentioning
confidence: 99%
“…The sites for the north are all but one from within the meso-Mediterranean and supra-Mediterranean zones, and all but three are located at medium and high elevation (>260 masl), while all samples for the south derive from the thermo-Mediterranean zone, and all but one are located at low elevations (most around 20 masl) ( Figure 1b, Supplementary Table 2, available online). The differences in the API can also (to some extent) be associated with the fact that most of the core locations in the north do not have any major settlements within their catchments, with the exception of the Orestias core that clearly records activity from the nearby settlement of Dispilió, with increased human activity during Neolithic, Hellenistic and Roman times (Kouli, 2015;Kouli et al, 2018;Mercuri et al, this volume). In contrast, most pollen core locations in the south are within regions for which archaeological remains suggest high human activity (if not specifically on site).…”
Section: Pollenmentioning
confidence: 99%
“…In fact, the river has always represented the way for foreign populations (such as the Greek settlers) who were attracted to the lands for farming to access the territory. The sites of the coastal plain (5)(6)(7)(8), which all belong to the chora (rural territory) of the Greek colonial city of Metaponto, are located mainly on the first marine terraces a few meters above the plain, which is often subject to floods. The network of small farmhouses and rural villages along the Bradano river had a crucial role in setting up the local farming system and regiment the water course and its floods [71].…”
Section: Study Areamentioning
confidence: 99%
“…From a long-term perspective, human influence and then-depending on the time and space scale-impact have generated notable patterns of landscape complexity [3][4][5][6]. This is especially evident in the Mediterranean area, where, since ancient times, the continuous succession of different civilizations has had direct and indirect effects on the environment that led to changes in the vegetation cover [7][8][9]. Grazing is one of the most important factors determining patterns of vegetation in Mediterranean ecosystems [10][11][12].…”
Section: Introductionmentioning
confidence: 99%
“…In this paper the role of palynology in investigating natural and human-forced changes of past environments is stressed. Although pollen analysis provides relatively local vegetation histories, these histories often record human-environmental dynamics on regional and superregional scales, as broadly shown in the Mediterranean [7][8][9][10][11]. We focus on the mid-late Holocene vegetation of the Argive Plain in the northeastern Peloponnese (from 4760 BP/2810 BCE to present).…”
Section: Introductionmentioning
confidence: 99%