Journal ArticleDOI
Geometry and Evolution of the Palisades Reef Complex, Silurian of Iowa
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The Palisades Reef Complex is asymmetrical, having an arcuate boundary on the north and west sides, and a general decrease in sediment grain-size and total thickness towards the south-east.Abstract:
Earlier sub-division of the Gower Formation into Le Claire (reef) and Anamosa (inter-reef) is inadequate and misleading, because the wide variety of lithologies demands a more elaborate and precise terminology; and because a large proportion of the Anamosa is later than the Le Claire reefs. The Palisades area provides an initial model for understanding facies relations elsewhere in Iowa, but not all Gower lithologies are represented. The Palisades Reef Complex is asymmetrical, having an arcuate boundary on the north and west sides, and a general decrease in sediment grain-size and total thickness towards the south-east. This presumably reflects a prevailing wind from the north-west. The first growth phase of the complex, represented by the crinoid-coelenterate facies, consists of a large number of crinoid mounds, which are most highly differentiated in the Marginal (windward) Zone; large, but simpler in the Main Crinoid Zone; and small or absent in the Leeward Zone. The Marginal Zone mounds are themselves asymmetrical, having a late-stage blanket of Coelenterate Beds on their windward sides only. The mounds are not wave-resistant reefs in Lowenstam's (1950) sense. The second growth phase is represented in the Marginal Zone by the "Brady facies." This consists mainly of laminated dense dolomite, but includes thick beds of rhynchonellids. The facies forms large-scale wedge-beds on the mound flanks, and is believed to have been derived from a platform on top of the earlier crinoid mounds. The Brady facies grades lithologically and geometrically into beds consisting almost entirely of laminated dolomite (Anamosa). In the Leeward Zone the second growth phase is represented solely by Anamosa dolomites. Off-reef lithologies are exposed, but difficult to correlate. Pene-contemporaneous cave deposits suggest sub-aerial exposure of the complex at about the end of the first phase of its development.read more
Citations
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Journal ArticleDOI
Ecological succession in Phanerozoic reef ecosystems; is it real?
TL;DR: In this article, the authors define ecological succession as an orderly, directional, and predictable, pioneer-to-climax process of community and species development in an environment where external physicochemical constraints are not undergoing major change: ecological succession leads naturally to increasing biological control of the environment and a stabilized ecosystem.
Journal Article
Growth forms and role of colonial coelenterates in reefs of the Gower Formation (Silurian), Iowa
Journal ArticleDOI
Paleoecologic, temporal, and spatial analysis of early Silurian Reefs of the Chicotte Formation, Anticosti Island, Quebec, Canada
Frank R. Brunton,Paul Copper +1 more
TL;DR: The Lower Silurian Chicotte Formation is the largest and most faunally diverse known on Anticosti Island, Quebec as mentioned in this paper and is represented on the present-day wave-cut terrace as 60 to 100 m diameter, subcircular erosional depressions known as Philip structures or as outcrop.
Journal ArticleDOI
Community relations of Silurian crinoids at Dudley, England
Rodney Watkins,John M. Hurst +1 more
TL;DR: In-place crinoid preservation in the Wenlock Limestone of Dudley, England, provides a community model for these occurrences, showing a pattern among crinoids of high taxonomic diversity, conspecific clustering, relatively robust morphology, and numerical dominance of other invertebrates.
Journal ArticleDOI
Origin of Silurian reefs in the Alexander Terrane of southeastern Alaska
TL;DR: Lower to Upper Silurian (upper Llandovery-Ludlow) limstones belonging to the Heceta Formation record several episodes of reef growth in the Alexander terrane of southeastern Alaska as mentioned in this paper.
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