重建含化石古岩溶的沉积历史和年龄:以南非博尔特农场上新世末期Aves洞穴群为例

Tara R. Edwards , Robyn Pickering , Tom L. Mallett , Andy I.R. Herries
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引用次数: 6

摘要

位于南非约翰内斯堡西北约40 公里的地区,在当地被称为人类的摇篮,具有全球意义,因为这些洞穴保存了上新世-更新世动物和早期人类化石。尽管研究历史悠久,但仍有必要将这些非凡的化石收藏置于背景下并确定其年代。博尔特农场(Bolt’s Farm)是一个重要但研究不足的古生物遗址,它可能为解决这个问题提供了一把钥匙,因为它保存了一系列20个独立的侵蚀古洞穴遗迹,分布在1 公里长的山坡上。这与代表一个地点的高度集中的矿床形成对比,这是该区域大多数地点的情况。从历史上看,南非古洞穴的岩石地层学方法使得沉积物内部和之间的重建和比较变得困难或不可能。本文提出了一种层序地层学方法和简单的相模型,对Bolt's Farm的三个古洞穴遗迹进行了研究,这些遗迹统称为Aves洞穴复合体(ACC),并基于基岩和盖层流岩的铀铅(U-Pb)联合测年和古地磁分析进行了年代学研究。结果表明,这些目前分散的位置,由一个单一的进入形成在一起,可追溯到3.03 - 2.61 Ma之间的高斯正极性年表末期,使ACC成为摇篮中最古老的直接定年化石矿床之一。ACC包含了该地区最早出现的一种关键生物年代学物种——安德鲁米氏蜱。这项工作加强了碎屑沉积和流石沉积在摇篮洞中不会同时发生的模型;相反,它们相互排斥的形成是由水文气候的异循环变化驱动的。这项研究提供了第一个证据,证明目前分散的地方曾经连接成一个单一的洞穴系统,有助于理解博尔特农场是如何形成今天观察到的前所未有的高密度古岩溶的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Reconstructing the depositional history and age of fossil-bearing palaeokarst: A multidisciplinary example from the terminal Pliocene Aves Cave Complex, Bolt's farm, South Africa

The region ∼40 km north-west of Johannesburg, South Africa, known locally as the Cradle of Humankind, is of global significance as the caves preserve Plio-Pleistocene faunal and early hominin fossils. Despite a long history of research, there is still a need to contextualise and date the remarkable collection of fossils. An important but understudied palaeontological site, Bolt's Farm, may provide a key to addressing this as it preserves a series of >20 separate eroded palaeocave remnants occurring across a 1 km length of hillside. This is in contrast to highly concentrated deposits representing a single site, as is the case at the majority of the sites in the region. Historically, a lithostratigraphic approach to South African palaeocaves made reconstruction and comparison within, and between, deposits difficult or impossible. Here, we present a sequence stratigraphic approach and simple facies model for three palaeocave remnants at Bolt's Farm collectively termed the Aves Cave Complex (ACC), and a chronology based on combined uranium lead (U-Pb) dating, of basal and capping flowstones, and palaeomagnetic analysis. Results indicate that these currently discrete localities, formed together from a single entry dating to the end of the Gauss Normal Polarity Chron between 3.03 and 2.61 Ma, making ACC one of the oldest directly dated fossil deposits in the Cradle. The ACC contains the earliest occurrence of a key biochronological species, Metridiochoerus andrewsi, in the region. This work reinforces the model that clastic sedimentation and flowstone precipitation do not occur concurrently in Cradle caves; rather their mutually exclusive formation is driven by allocyclic changes in hydroclimate. This research contributes to understanding how Bolt's Farm developed the unprecedented high density of palaeokarst observed today, by offering the first evidence that currently discrete localities were once connected as a single cave system.

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