Ichnological analysis is considered a very useful tool in several disciplines of Earth Sciences, including palaeoenvironmental studies and hydrocarbon exploration. Sediment cores provide excellent records, despite difficulties encountered during study runs due to specific core features. Previous studies using 2D images have proven the benefits of high-resolution image treatment in improving the visibility of ichnological features, but with limitations. 3D computed tomography (CT) techniques were applied to palaeoichnological studies in lithified cores and other disciplines of palaeontology to solve these limitations, but not used for ichnological studies in unconsolidated sediments due to the low density contrast between host sediment and trace fossils. In this study, a CT processing technique, previously tested in coral research, is applied to facilitate the characterisation of the ichnological signature of cores from modern marine soft sediments. This technique allows for the first time the isolation of burrows within these kinds of sediments and the differentiation of intervals based on burrow orientation. Data obtained from the technique are complemented with the ichnological information from conventional core description, thus providing a more complete characterisation of the trace fossil assemblage with additional ichnological properties such as burrow orientation and branching. This will improve palaeoenvironmental interpretations related to changes in energy or oxygenation, and the analysis of reservoir quality given the impact of burrows on porosity and permeability. Therefore, adopting CT to complement visual core description in the ichnological analysis of soft modern marine cores is a very informative approach.
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http://dx.doi.org/10.1038/s41598-019-57028-z | DOI Listing |
PLoS One
April 2022
Departamento Biología, Paleontología and CIPb-UAM (Center for the Integration in Paleobiology), Facultad Ciencias, Universidad Autónoma de Madrid, Madrid, Spain.
We describe a trackway (LH-Mg-10-16) occurring in laminated carbonated limestones of the Las Hoyas locality, Serranía de Cuenca, Spain. It is unmistakably a large theropod dinosaur trackway encompassing two unusual aspects, namely, wide-steps, and a set of equally deformed left footprints (with a dislocated digit). The layer also preserves other vertebrate trails (fish Undichna) and different impressions in the sediment.
View Article and Find Full Text PDFSci Rep
February 2021
Department of Earth Sciences, Royal Holloway University of London, Egham, TW20 0EX, Surrey, UK.
Oceanic gateways have modulated ocean circulation and have influenced climatic variations throughout the Earth´s history. During the late Miocene (7.8-7.
View Article and Find Full Text PDFSci Rep
January 2021
Departamento de Estratigrafía y Paleontología, Universidad de Granada, 18002, Granada, Spain.
Bioturbation is an important factor for reservoir quality due to the modification of host rock petrophysical properties (i.e., porosity, permeability, and connectivity).
View Article and Find Full Text PDFInterface Focus
August 2020
Department of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon, Saskatchewan, Canada S7N 5E2.
The trace-fossil record provides a wealth of information to track the rise and early evolution of animals. It comprises the activity of both hard- and soft-bodied organisms, is continuous through the Ediacaran (635-539 Ma)- Cambrian (539-485 Ma) transition, yields insights into animal behaviour and their role as ecosystem engineers, and allows for a more refined characterization of palaeoenvironmental context. In order to unravel macroevolutionary signals from the trace-fossil record, a variety of approaches is available, including not only estimation of degree of bioturbation, but also analysis of ichnodiversity and ichnodisparity trajectories, and evaluation of the occupation of infaunal ecospace and styles of ecosystem engineering.
View Article and Find Full Text PDFJ Anthropol Sci
December 2020
Universitá degli Studi di Cassino e del Lazio Meridionale, Dipartimento di Scienze Umane, Sociali e della Salute, Laboratorio di Ricerche Storiche e Archeologiche dell'Antichitá, Cassino (FR), Italy,
This report aims to give notice of and provide a more detailed dataset and detailed remarks on what can be considered a one-of-a-kind hominin fossil walking pattern: Trackway B of the Foresta ichnological site (Tora e Piccilli, Caserta, Central Italy). Although the site is known since 2003, only recently has the study been performed by means of the newest photogrammetric and experimental techniques of collection, analysis and interpretation of ichnological data. The results obtained enable us to depict an astonishing movie printed in rock, describing some body features and common moments of the everyday movements of a hominin who lived about 350 ka.
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