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首页> 外文期刊>Quaternary geochronology >Bayesian age-depth modelling of Late Quaternary deposits from Wet and Blanche Caves, Naracoorte, South Australia: A framework for comparative faunal analyses
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Bayesian age-depth modelling of Late Quaternary deposits from Wet and Blanche Caves, Naracoorte, South Australia: A framework for comparative faunal analyses

机译:来自南澳大利亚纳拉科特的湿和布兰奇洞穴晚第四纪沉积物的贝叶斯年龄深度模拟:比较动物学分析的框架

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Bayesian age-depth models were constructed for two Late Quaternary aged fossil-bearing sedimentary sequences from caves in south eastern South Australia. The deposits in Wet and Blanche Caves contain dense assemblages of vertebrate fossils, largely the result of owl pellet accumulation. While individually calibrated radiocarbon determinations from the fossil sequences have provided a chronology for their accumulation, there was limited capacity available with such data to (a) temporally constrain assemblages associated with different depositional units and layers within the two sites, (b) interpret the chronological relationships among successive units and layers and (c) correlate sedimentary units and layers of similar age between the two deposits. Here, Bayesian age-depth models were constructed in OxCal for the Wet and Blanche Cave sequences, incorporating the available radiocarbon data and stratigraphic information collected during their excavation. Despite the low precision of the age-depth models for Wet and Blanche Caves which results in part from there being only single radiocarbon determinations available for a number of units and layers, the models enabled the relationships within and between the two sites to be established. Of particular utility for future faunal analyses is quantification of the temporal relationship between strata from the two sites, where groups of individual layers from Blanche Cave were found to be temporally equivalent with the longer-duration units in Wet Cave. We suggest that the use of Phase modelling, as performed here, is useful for cave deposits that have complex depositional histories and even in such instances where, as is common for palaeontological sites, few radiocarbon data are collected relative to the time-spans of tens of millennia that are often represented by them.
机译:针对来自南澳大利亚东南部洞穴的两个晚第四纪年龄的含化石的沉积序列建立了贝叶斯年龄深度模型。湿洞穴和布兰奇洞穴中的沉积物含有密集的脊椎动物化石组合,这主要是猫头鹰颗粒堆积的结果。虽然根据化石序列进行的单独校准的放射性碳测定提供了其积累的时间顺序,但此类数据的可用容量有限(a)在时间上限制了与两个地点内不同沉积单元和层有关的组合,(b)解释了时间顺序连续单元和层之间的关系;(c)将两个矿床之间相似年龄的沉积单元和层相关。在这里,在OxCal中为湿和布兰奇洞穴序列构建了贝叶斯年龄深度模型,其中包含了在挖掘过程中收集的可用放射性碳数据和地层信息。尽管湿地和布兰奇洞的年龄深度模型的精度较低,其部分原因是对于多个单位和层只能进行一次放射性碳测定,但该模型仍可以在两个地点之间及其之间建立关系。对于未来的动物区系分析,特别有用的是对两个地点的地层之间的时间关系进行量化,在该地点发现布兰奇洞的各个层的组在时间上与湿洞中较长的时间单位等效。我们建议,如此处所述,使用相模型对沉积历史复杂的洞穴沉积物很有用,即使在这样的情况下(如古生物学站点常见的那样),相对于数十个时间跨度,很少收集到放射性碳数据他们代表的千年之交。

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