遗址形成过程和水下洞穴中脊椎动物遗骸的岩石学研究

IF 10.8 1区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Earth-Science Reviews Pub Date : 2024-07-31 DOI:10.1016/j.earscirev.2024.104883
Meg M. Walker, Julien Louys
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引用次数: 0

摘要

古生物学和动物考古学沉积物已经从全球各地的水下洞穴中发掘出来,但有关这些环境中遗址形成过程的研究却十分零散,从未进行过系统的研究。岩溶系统喷气带中的淹没洞穴包括天坑和栅栏(窗),它们构成了地下和地面景观之间的连接,以及建立地下隧道网络的导管和洞室。这些空间的埋藏环境是多变的,单个遗址内的沉积、洞穴形态和水文变化都会对岩石学过程产生深远影响。然而,决定这些空间长期保存的关键因素是水的存在,水的存在决定了居住的性质、居住的物种以及腐烂的过程。地下水位会随着海平面的长期和短期变化而波动,随之而来的是近岸洞穴系统中淹没的 "潮湿 "或暴露的 "干燥 "埋藏环境的变化。要重建洞穴中的遗址形成过程,就必须区分潮湿和干燥的埋藏条件,这些洞穴显示了不断变化或周期性的岩相和岩层条件。在海洋、湖泊和河流环境下的水下遗址中已经发现了水生沉积的迹象,但对水下洞穴景观却缺乏类似的研究。水会影响腐化过程,改变骨骼表面,并改变骨骼内部的物理和化学特性。通过探索淹没洞穴的环境特性以及已知的水生变化,本综述旨在为水下洞穴古生物学和考古遗址的岩石学研究建立一个框架。我们详细介绍了可通过实际、实验和观察研究来探索的生物地层学和成岩过程。未来可以考虑人类活动对这些空间的空间分布和骨骼变化的影响,以及环境和人类活动的综合影响。
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Site formation processes and the taphonomy of vertebrate remains in underwater caves

Palaeontological and zooarchaeological deposits have been recovered from underwater caves across the globe, but studies on site formation processes in these environments are scattered and have never been systematically examined. Flooded caves in the phreatic zone of karst systems include sinkholes and fensters (windows) that form a connection between the sub-aerial and sub-terranean landscapes, and conduits and chambers that establish underground networks of tunnels. Burial environments in these spaces are variable, and sedimentary, cave morphologic, and hydrologic variability within a single site can have profound impacts on taphonomic processes. The key determinant on long term preservation in these spaces is, however, the presence of water which dictates the nature of any habitation and by which species, and the process of decay. Water tables can fluctuate with long- and short-term sea level changes, with concomitant shifts in burial environments between flooded ‘wet’ or exposed ‘dry’ settings in near-shore cave systems. Distinguishing wet and dry burial conditions is necessary to reconstruct site formation processes in caves exhibiting evidence of changing or cyclical phreatic and vadose conditions. Signatures of aquatic deposition have been identified in underwater sites under marine, lacustrine and fluvial settings, but similar investigations are lacking for submerged cave landscapes. Water influences the decay process, alters bone surfaces, and modifies internal physical and chemical properties of bones. By exploring the environmental properties of flooded caves alongside known aquatic modifications, this review aims to build a framework for taphonomy of underwater cave palaeontological and archaeological sites. We detail biostratinomic and diagenesis processes that can be explored by actualistic, experimental, and observational studies. Future consideration could be given to the effects of human actions on the spatial distribution and modifications of bones in these spaces and the combined effects of environmental and anthropic agents.

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来源期刊
Earth-Science Reviews
Earth-Science Reviews 地学-地球科学综合
CiteScore
21.70
自引率
5.80%
发文量
294
审稿时长
15.1 weeks
期刊介绍: Covering a much wider field than the usual specialist journals, Earth Science Reviews publishes review articles dealing with all aspects of Earth Sciences, and is an important vehicle for allowing readers to see their particular interest related to the Earth Sciences as a whole.
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