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A new approach for investigating spatial relationships of ichnofossils: A case study of Ediacaran–Cambrian animal traces

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Peer-reviewed

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Abstract

Trace fossils record foraging behaviours, the search for resources in patchy environments, of animals in the rock record. Quantification of the strength, density and nature of foraging behaviours enables the investigation of how these may have changed through time. Here, we present a novel approach to explore such patterns using spatial point process analyses to quantify the scale and strength of ichnofossil spatial distributions on horizontal bedding planes. To demonstrate the utility of this approach we use two samples from the terminal Ediacaran Shibantan Member in South China (between 551 and 543 Ma) and the early Cambrian Nagaur Sandstone in northwestern India (between 539 and 509 Ma). We find that ichnotaxa on both surfaces exhibited significant non-homogeneous lateral patterns, with distinct levels of heterogeneity exhibited by different types of trace fossils. In the Shibantan, two ichnotaxa show evidence for mutual positive aggregation over a shared resource, suggesting the ability to focus on optimal resource areas. Trace fossils from the Nagaur Sandstone exhibit more sophisticated foraging behaviour, with greater niche differentiation. Critically, mark correlation functions highlight significant spatial autocorrelation of trace fossil orientations, demonstrating the greater ability of these Cambrian tracemakers to focus on optimal patches. Despite potential limitations, these analyses hint at changes in the development and optimisation of foraging at the Ediacaran–Cambrian transition and highlight the potential of spatial point process analysis to tease apart subtle differences in behaviour in the trace fossil record.

Description

Journal Title

Paleobiology

Conference Name

Journal ISSN

0094-8373
1938-5331

Volume Title

Publisher

Cambridge University Press

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Except where otherwised noted, this item's license is described as Attribution 4.0 International
Sponsorship
Natural Environment Research Council (NE/S014756/1)
EGM was supported by a NERC independent research fellowship (NE/S014756/1), SDE by an Agouron Institute Geobiology fellowship, SX by the National Science Foundation (EAR-2021207), and ZC by the National Natural Science Foundation of China (41921002).