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3D "Phycosiphoniform" Burrows:
BEDNARZ & McILROY

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Multilingual  Abstracts

Abstract

Introduction

Phycosiphoniform Burrows in Marine Ichnofabrics

Interpreted 3D Morphology of Phycosiphon incertum

Palaeobiology of the Phycosiphon Trace-Maker

Interpretation of 3D Morphology from Cross Sections of Phycosiphoniform Burrows

Methods

Conclusion

Acknowledgements

References

 

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THREE-DIMENSIONAL RECONSTRUCTION OF "PHYCOSIPHONIFORM" BURROWS:
IMPLICATIONS FOR IDENTIFICATION OF TRACE FOSSILS IN CORE

Malgorzata Bednarz and Duncan McIlroy

ABSTRACT

Phycosiphon-like trace fossils are some of the most common and important ichnofabric forming trace fossils in marine facies. This study was conducted to reconstruct the three-dimensional (3D) morphology of a Phycosiphon-like trace fossil from Cretaceous turbidites in Mexico in order to test the validity of criteria used to recognize such fossils in vertical cross sections similar to those seen in cores through hydrocarbon reservoir intervals. The geometry of the trace fossil was computer-modeled using a series of consecutive images obtained by serial grinding. The recognition of Phycosiphon in cross section is usually based on comparison with hypothetical cross sections of bedding-parallel specimens. The authors critically reassess Phycosiphon-like burrows in the light of existing conceptual and deterministic models, for comparison with three-dimensional reconstruction of Phycosiphon-like trace fossils from the Cretaceous Rosario Formation of Baja California, Mexico.

Observed morphological differences between our material and typical Phycosiphon suggest that the characteristic "frogspawn" ichnofabric that is usually attributed to Phycosiphon (sensu stricto) can be produced by other similar taxa. Our palaeobiological model for the formation of the studied Phycosiphon-like trace fossil is fundamentally different to that proposed for Phycosiphon, but produces remarkably similar vertical cross sections. We consider that identification of Phycosiphon incertum in core is not possible without detailed 3D examination of burrow geometry. We propose the term "phycosiphoniform" for this group of ichnofabric-forming trace fossils.

Malgorzata Bednarz. Department of Earth Sciences, Memorial University of Newfoundland, St. John's, Newfoundland, A1B3X5, NL, Canada.
Duncan McIlroy. Department of Earth Sciences, Memorial University of Newfoundland, St. John's, Newfoundland, A1B3X5, NL, Canada.

KEY WORDS: burrows; ichnofabric; ichnofossil; three-dimensional; 3D; morphology; Phycosiphon; reconstruction; trace fossils; core; halo; cross sections

PE Article Number: 12.3.13A
Copyright: Palaeontological Association December 2009
Submission: 1 April 2009. Acceptance: 12 October 2009

 

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3D "Phycosiphoniform" Burrows
Plain-Language & Multilingual  Abstracts | Abstract | Introduction | Phycosiphoniform Burrows in Marine Ichnofabrics
Interpreted 3D Morphology of Phycosiphon incertum | Palaeobiology of the Phycosiphon Trace-Maker
Interpretation of 3D Morphology from Cross Sections of Phycosiphoniform Burrows
Methods | Conclusion | Acknowledgements | References
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