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首页> 外文期刊>Quaternary International >The high-resolution sequence stratigraphy and the mammal fossil record: a test in the Middle-Upper Pleistocene deposits of the Roman Basin (Latium, Italy)
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The high-resolution sequence stratigraphy and the mammal fossil record: a test in the Middle-Upper Pleistocene deposits of the Roman Basin (Latium, Italy)

机译:高分辨率层序地层学和哺乳动物化石记录:在罗马盆地(意大利拉提姆)中上更新世沉积中的一项测试

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摘要

In the Campagna Romana area Pleistocene vertebrate fossil remains are preserved both in continental and marine sedimentary successions. This fact favoured the identification of faunal complexes in agreement with the biochronologic setting proposed for the Plio-Pleistocene large mammal faunas of the Italian peninsula. At the same time, the detailed facies and sequence stratigraphic analyses carried out in the last years on such deposits have allowed establishment of a regional and local chronostratigraphic framework which sets some physical and temporal limits to the occurrence of faunal complexes. In this light, the study of the Pleistocene deposits of the Roman Basin, based on sequence stratigraphy and mammal biochronology approach, can constitute a significant tool to test the relationships among physical stratigraphic units, faunal complexes and faunal units. In the examined area, the fossiliferous levels are essentially found in transgressive fluvial and fluvio-palustrine deposits filling incised valleys (TST) and in highstand barrier island-lagoon deposits (HST). Excluding some cases where bones show a probable exhumation process, whole discovered mammal remains are mostly coeval with deposits containing them. Based on taphonomic considerations and on depositional and physical stratigraphic settings, a correlation scheme among Roman Pleistocene sequence -stratigraphic units, local faunal complexes and Italian mammal biochrons is proposed. Nevertheless, many problems remain to be clarified before either the correlation between events and the geochronological framework, or the significance and the biochronological value of each faunal assemblage can be considered as definitive.
机译:在Campagna Romana地区,更新世的脊椎动物化石遗迹保存在大陆和海洋沉积演替中。这一事实有利于根据意大利半岛上新世更新世大型哺乳动物区系提出的生物年代学背景来确定动物群。同时,最近几年对这类沉积物进行的详细的相和层序地层学分析允许建立区域和局部年代地层学框架,为动物群的形成设定了一些物理和时间上的限制。有鉴于此,基于层序地层学和哺乳动物生物年代学方法,对罗马盆地的更新世沉积物的研究可以成为检验物理地层单位,动物群和动物群之间关系的重要工具。在所研究的地区,化石水平主要存在于海藻和河流-河床沉积物中,这些沉积物充填了切谷(TST)和高耸的障碍岛泻湖沉积物(HST)。除了一些骨头可能出现尸体发掘过程的情况外,整个发现的哺乳动物遗骸大多与含有它们的沉积物同生。基于对地形的考虑,并根据沉积和物理地层学背景,提出了罗马更新世层序-地层单位,当地动物群和意大利哺乳动物生物年代学之间的关联方案。然而,在事件与年代学框架之间的相关性,或者每个动物群的重要性和生物年代学价值可以被认为是确定的之前,仍有许多问题需要澄清。

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