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Millstones as indicators of relative sea-level changes in northern Sicily and southern Calabria coastlines, Italy

机译:磨石作为意大利西西里岛北部和卡拉布里亚南部海岸线相对海平面变化的指标

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摘要

New data are presented for late Holocene relative sea-level changes in two coastal sites of Sicily andCalabria, southern Italy. Reconstructions are based on precise measurements of submerged archaeologicalremains that are valuable indicators of past sea-level position. The archaeological remains aremillstone quarries carved on sandstone coastal rocks and nowadays partially submerged which, to theauthors’ knowledge, are used for the first time as sea-level markers. Millstones of similar typology arelocated on the coast of Capo d’Orlando (northern Sicily) and Capo dell’Armi (southern Calabria). Whenthe archeologically-based sea-level position is compared with the shoreline elevation provided bygeological markers (Holocene beachrock, Late Pleistocene marine terraces), a refined understanding ofrelative sea-level changes and rates of vertical tectonic movements for these coastline locations is gained.
机译:给出了意大利南部西西里岛和卡拉布里亚两个沿海站点晚全新世相对海平面变化的新数据。重建基于对淹没的考古遗迹的精确测量,这些测量是过去海平面位置的宝贵指标。考古遗迹是在砂岩沿海岩石上雕刻的磨石采石场,如今已部分淹没,据作者所知,这第一次被用作海平面标记。类似类型的磨石位于奥兰多角(西西里北部)和德尔阿米角(卡拉布里亚南部)海岸。将基于考古的海平面位置与地质标志物(全新世海滩岩,晚更新世海洋阶地)提供的海岸线高程进行比较后,就可以更好地了解这些海岸线位置的相对海平面变化和垂直构造运动的速率。

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