Journal article
The rise of pinnacle reefs; islands of diversity in seas of despair
Field guide (Geological Society of America), Vol.51, pp.23-33
12/10/2018
DOI: 10.1130/2018.0051(02)
Abstract
Pinnacle reef tracts are geomorphic features of carbonate systems that originated in the early Silurian and display an episodic distribution into the Cenozoic. Detailed study of Silurian pinnacle reefs of the United States midcontinent demonstrates repeated motifs, but most enigmatic is the coincidence of carbonate carbon isotope (delta (super 13) C (sub carb) ) excursions and reef pulses. Silurian delta (super 13) C (sub carb) excursions were associated with environmental changes and extinctions, and reefs appear to mark a resurgence of conditions favorable to biomineralizers following those extinction events. Previous workers in the region identified six discrete reef origination events in the United States midcontinent during the Silurian. Our reevaluation of outcrops and cores, conodont collections, and the generation of considerable new chemostratigraphic data across the region are clarifying the age relations of these events and their relationships to perturbations of the global carbon cycle.
Details
- Title: Subtitle
- The rise of pinnacle reefs; islands of diversity in seas of despair
- Creators
- Patrick I. McLaughlin - Indiana UniversityAlyssa M. BancroftCarlton E. BrettPoul EmsboLee J. Florea - Indiana University
- Resource Type
- Journal article
- Publication Details
- Field guide (Geological Society of America), Vol.51, pp.23-33
- Publisher
- Geological Society of America
- DOI
- 10.1130/2018.0051(02)
- ISSN
- 2333-0937
- eISSN
- 2333-0945
- Number of pages
- 11
- Alternative title
- Ancient oceans, orogenic uplifts, and glacial ice; geologic crossroads in America's heartland
- Language
- English
- Date published
- 12/10/2018
- Academic Unit
- Earth and Environmental Sciences; Iowa Geological Survey; IIHR--Hydroscience and Engineering
- Record Identifier
- 9984702729002771
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