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Animal-substrate interactions preserved in ancient lagoonal chalk
Fernando L Valencia1, M Gabriela Mángano2, Luis A Buatois2
1Department of Geological Sciences, University of Saskatchewan, 114 Science Place, Saskatoon, SK, S7N 5E2, Canada. fev986@mail.usask.ca.
This study analyzes trace fossils in ancient lagoonal chalk, revealing unique biodiversity patterns. Lagoonal chalks show higher ichnodiversity and ichnodisparity than open marine chalks due to environmental factors.
Area of Science:
- Paleontology
- Sedimentology
- Ichnology
Background:
- Trace fossils are key indicators of benthic paleoenvironmental conditions.
- Previous studies focused on pelagic shelf and deep-sea chalks, neglecting lagoonal chalks.
- Lagoonal environments exhibit dynamic physicochemical parameters influencing benthic life.
Purpose of the Study:
- To conduct the first ichnologic analysis of ancient lagoonal chalk deposits.
- To investigate trace-fossil assemblages in the Upper Cretaceous Buda Formation, Texas.
- To understand the impact of lagoonal circulation on trace-fossil content.
Main Methods:
- Detailed ichnologic analysis of Buda Formation chalk.
- Identification and classification of ichnotaxa.
- Comparison of trace-fossil assemblages with open marine chalks.
Main Results:
- Twenty ichnotaxa identified, dominated by Thalassinoides isp. and Chondrites isp.
- Trace-fossil assemblages show similarities to shallow-water shelf-sea chalks.
- Lagoonal chalk exhibits higher ichnodiversity and ichnodisparity than open marine chalks.
Conclusions:
- Lagoonal chalk trace-fossil content is influenced by variable ocean connectivity and physicochemical fluctuations.
- Dominance of Thalassinoides isp. in both soft and firmgrounds indicates similarities with shallow marine settings.
- Increased ichnodiversity and ichnodisparity in lagoonal chalks result from taphonomic and ecologic factors, including environmental heterogeneity.
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