x射线计算机断层扫描(CT)对葡萄牙西南部米拉河河口沉积物岩心的技术解释的影响

Alina Shchepetkina, Teresa Drago, Jacqueline Santos, Ana Alberto
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引用次数: 0

摘要

摘要计算机断层扫描(CT)技术是一种相对较新的化石分析技术,它可以更好地识别单个化石的形态、填充、层序关系和保存潜力,从而提供更好的环境解释。它还允许非专业技术人员轻松地在3D切片中解释痕量化石,特别是在相对均匀和富含泥浆的沉积物中。本文将CT成像结果与常规岩心测井结果进行了比较,这些岩心是基于葡萄牙米拉河河口泥质潮滩的两个推式岩心样本。由于增强了物理和生物成因沉积结构的可见性,CT图像提供了更准确的岩心描述及其环境解释。它们还揭示了洞穴之间复杂的分层关系,并优先保存更深的层。由水生双壳类动物形成的类似于scalichnus和其他虹吸管状洞穴的堆积表明,在潮汐滩上的不连续沉积可能是由河口环境中与季节相关的波动引起的。本文作者是主要作者的博士导师、导师和“技术之父”George S. Pemberton博士。Drs。感谢里斯本大学的Francisco Fatela和concep o Freitas在组织实地考察和关注推核方面提供的宝贵帮助。披露声明作者未报告潜在的利益冲突。本研究由葡萄牙 技术基金会(FCT) ip /MCTES通过国家基金(PIDDAC) - UIDB/50019/2020在“UIDP/50019/2020 - 2020-2023 - IDL”项目下资助,并由欧洲基金(POCI)共同资助。在“葡萄牙研究基础设施路线图”范围内的“欧洲多学科海底和水柱观测站(葡萄牙)- EMSO-PT (PINFRA/22157/2016)”项目下的区域业务计划(COMPETE)和国家基金(FCT)。Jacqueline Santos获得了IPMA-2020-011-BI (EMSOPT项目下)的资助,Ana Alberto获得了UIBD/151497/2021 (IDL)的博士资助。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Effects of X-ray computed tomography (CT) on the ichnologic interpretation of the Mira River estuary sediment core, SW Portugal
AbstractComputed tomography (CT) is a relatively new technique in ichnofossil analysis, which permits superior identification of individual trace fossils, their morphology, infill, tiering relationships, and preservation potential, thus providing better environmental interpretations. It also allows non-professional ichnologists to interpret trace fossils in 3D slices with ease, especially in relatively homogeneous and mud-rich sediments. Herein, CT imagery results have been compared with conventional core logging results based on two push core samples from a muddy tidal flat of the Mira River estuary, Portugal. CT images provide a significantly more accurate description of cores and their environmental interpretation due to enhanced visibility of physical and biogenic sedimentary structures. They also reveal complex tiering relationships between burrows with preferential preservation of deeper tiers. The appearance of stacked Scalichnus-like and other siphonichnidal burrows made by infaunal bivalves indicates discontinuous deposition on a tidal flat likely caused by seasonally related fluctuations in an estuarine environment.Keywords: CT scanningtieringequilibrichniapaleoenvironmental analysisestuary AcknowledgementsThis work is devoted to Dr. George S. Pemberton, who was the leading author’s Ph.D. supervisor, mentor, and “ichnological father”. Drs. Francisco Fatela and Conceição Freitas from the University of Lisbon are thanked for their valuable help in the organization of fieldwork and obtention of the push cores.Disclosure statementNo potential conflict of interest was reported by the author(s).Additional informationFundingThe study was funded by the Portuguese Fundação para a Ciência e a Tecnologia (FCT) I.P./MCTES through national funds (PIDDAC) – UIDB/50019/2020 under the project “UIDP/50019/2020 – Financiamento Plurianual de Unidades de I&D 2020-2023 – IDL” and co-funded by European funds (POCI), Regional Operational Programmes (COMPETE) and national funds (FCT) under the project “European Multidisciplinary Seafloor and Water Column Observatory (Portugal) - EMSO-PT (PINFRA/22157/2016)” in the scope of “Portuguese Roadmap of Research Infrastructures”. Jacqueline Santos received financial support through grant IPMA-2020-011-BI (under the project EMSOPT) and Ana Alberto through PhD grant UIBD/151497/2021 (IDL).
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