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Strontium isotope investigation of ungulate the Pleistocene Paleo-Agulhas Plain of the greater South Africa

机译:大南非有更新世的古-阿古拉斯平原有蹄类动物的锶同位素研究

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摘要

Middle Stone Age sites located within the Greater Cape Floristic Region on the South African southern coast have material culture with early evidence for key modern human behaviors such as projectile weaponry, large animal hunting, and symbolic behavior. In order to interpret how and why these changes evolved, it is necessary to understand their ecological context as it has direct relevance to foraging behavior. During periods of lowered sea level, a largely flat and vast expanse of land existed south of the modern coastline, but it is now submerged by higher sea levels. This exposed area, the Paleo-Agulhas Plain, likely created an ecological context unlike anything in the region today, as evidenced by fossil assemblages dominated by migratory ungulates. One hypothesis is that the Paleo-Agulhas Plain supported a migration ecosystem of large grazers driven by summer rainfall, producing palatable forage during summer in the east, and winter rainfall, producing palatable forage during winter in the west. Alternatively, ungulates may have been moving from the coastal plain in the south to the interior north of the Cape Fold Mountains, as observed for elephants in historic times.In this study, we assess ungulate movement patterns with inter- and intra-tooth enamel samples for strontium isotopes in fossil fauna from Pinnacle Point sites PP13B and PP30. To accomplish our goals we created a bioavailable 87Sr/86Sr isoscape for the region by collecting plants at 171 sampling sites and developing a geospatial model. The strontium isotope results indicate that ungulates spent most of their time on the Paleo-Agulhas Plain and avoided dissected plain, foothill, and mountain habitats located more than about 15 km north of the modern coastline. The results clearly exclude a north-south (coastal-interior) movement or migration pattern, and cannot falsify the east-west movements hypothesized in the south coast migration ecosystem hypothesis.
机译:位于南非南部海岸大开普植物区的中石器时代遗址具有物质文化,早期证据证明了现代人类的重要行为,例如射弹武器,大型动物狩猎和象征性行为。为了解释这些变化是如何以及为什么演变的,有必要了解它们的生态环境,因为它与觅食行为直接相关。在海平面降低的时期,现代海岸线以南存在大片平坦而广阔的土地,但现在被高海平面淹没。这个裸露的地区,古阿古拉斯平原,可能创造了与今天该地区任何地区都不一样的生态环境,如以有蹄类动物为主的化石组合所证明的那样。一个假设是,古阿古拉斯平原支持大型放牧者的迁徙生态系统,该生态系统由夏季降雨驱动,东部夏季产生可口的草料,而冬季降雨则在西部冬季产生可口的草料。另外,有蹄类动物可能已经从佛得角山南部的沿海平原向北向内陆移动,如历史时期观察到的大象。在这项研究中,我们通过牙间和牙内牙釉质样本评估了有蹄类动物的运动方式品尼高点站点PP13B和PP30的化石动物中的锶同位素。为了实现我们的目标,我们通过在171个采样点采集植物并开发地理空间模型,为该地区创建了生物可利用的87Sr / 86Sr等值线。锶同位素结果表明,有蹄类动物的大部分时间都在古Agulhas平原上度过,避免了解剖后的平原,山麓和山区栖息地,这些栖息地位于现代海岸线以北15公里以上。结果清楚地排除了北-南(沿海-内部)运动或迁移模式,并且不能伪造在南海岸迁移生态系统假设中假设的东西向运动。

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