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Waynesville Formation

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Journal Article

Benthic community development in limestone beds of the Waynesville (upper Dillsboro) Formation (Cincinnatian Series, Upper Ordovician) of southeastern Indiana Available to Purchase

F. W. Harris, W. D. Martin
Published: 01 December 1979
Journal of Sedimentary Research (1979) 49 (4): 1295–1305.
DOI: https://doi.org/10.1306/212F7914-2B24-11D7-8648000102C1865D
...F. W. Harris; W. D. Martin Abstract Vertical and lateral changes in composition occur within 13 individual limestone beds of the Waynesville (Upper Dillsboro) Formation (Upper Ordovician) near Brookville, Indiana. Fossil allochems formed approximately 40%. and carbonate ooze 60% of the original...
View PDF for article title, Benthic community development in limestone beds of the <span class="search-highlight">Waynesville</span> (upper Dillsboro) <span class="search-highlight">Formation</span> (Cincinnatian Series, Upper Ordovician) of southeastern Indiana
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Key marker beds in the Waynesville Formation. Adapted from Aucoin and Bret... Available to Purchase

Published: 21 August 2018
Table 1.— Key marker beds in the Waynesville Formation. Adapted from Aucoin and Brett (2016) .
Journal Article

GEOCHEMISTRY, CLAY MINERALOGY, AND TAPHONOMY OF THE FOSSIL-RICH BUTTER SHALES Available to Purchase

HANNA F. COHEN, JACALYN M. WITTMER, SHANE K. BUTLER, JORDAN M. YOUNG
Journal: PALAIOS
Published: 21 August 2018
PALAIOS (2018) 33 (8): 393–402.
DOI: https://doi.org/10.2110/palo.2017.037
...Table 1.— Key marker beds in the Waynesville Formation. Adapted from Aucoin and Brett (2016) . ...
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View PDF for article title, GEOCHEMISTRY, CLAY MINERALOGY, AND TAPHONOMY OF THE FOSSIL-RICH BUTTER SHALES
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Journal Article

General models of ecological diversification. II. Simulations and empirical applications Available to Purchase

Philip M. Novack-Gottshall
Journal: Paleobiology
Published: 01 May 2016
Paleobiology (2016) 42 (2): 209–239.
DOI: https://doi.org/10.1017/pab.2016.4
... Late Ordovician (type Cincinnatian) samples from the Kope and Waynesville formations are used to illustrate how these models can be inferred in empirical applications. Initial simulations overestimate the ecological disparity of actual assemblages, confirming that actual life habits are highly...
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View PDF for article title, General models of ecological diversification. II. Simulations and empirical applications
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FIGURE 1—Location of type Cincinnatian samples. Abbreviations used in the text and formations sampled include: Bear Creek Quarry (BC; Kope Formation), Maysville (MAY; Bellevue Formation), Christ Hospital (CHS; Miamitown Shale), Mount Airy Forest (MAF; Miamitown Shale), Ashlock Cemetery (AC; Tate [AT] and Gilbert [AG] Formations), Hannah Creek (HC; Waynesville Formation), Russell Branch (RB; Waynesville Formation), Bedford (MH; Marble Hill Bed), and Madison (HW; Hitz Bed)

FIGURE 1 —Location of type Cincinnatian samples. Abbreviations used in the ... Available to Purchase

Published: 01 December 2003
[AT] and Gilbert [AG] Formations), Hannah Creek (HC; Waynesville Formation), Russell Branch (RB; Waynesville Formation), Bedford (MH; Marble Hill Bed), and Madison (HW; Hitz Bed)
Journal Article

Petrology of the Cincinnatian Series Shales and Environmental Implications Available to Purchase

DAVID M SCOTFORD
Journal: GSA Bulletin
Published: 01 February 1965
GSA Bulletin (1965) 76 (2): 193–222.
DOI: https://doi.org/10.1130/0016-7606(1965)76[193:POTCSS]2.0.CO;2
... of the Waynesville formation which is probably an indication of marine transgression in that direction and/or an east-west trending barrier. The vertical homogeneity of the shales suggests static environmental conditions and encourages the restriction of the present stratigraphic nomenclature of the Cincinnatian...
View PDF for article title, Petrology of the Cincinnatian Series Shales and Environmental Implications
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A PPENDIX —Ancestrular dimensions (mm) of specimens belonging to four gener... Available to Purchase

Published: 01 July 2011
A PPENDIX —Ancestrular dimensions (mm) of specimens belonging to four genera collected from the Upper Ordovician (Katian Stage) Dillsboro Formation (Liberty and Waynesville formations of older terminology). Length was measured parallel to and width perpendicular to the direction of ancestrular
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Figure3—Serrated boundaries, all longitudinal sections, ×100; see text for descriptions of photographs. 1,Rhombotrypa quadrata (Rominger, 1866), hypotype of type species (USNM 204877), Waynesville Formation (Richmondian), Ordovician, Hanover, Ohio. 2,Gortanipora nodulosa (Bassler, 1903), paralectotype (USNM 508956), Waynesville Formation (Richmondian), Ordovician, Hanover, Ohio. 3,Balticoporella glabrum (Bassler, 1911), paralectoype of type species (USNM 57420), Wassalem beds D3 (Trentonian), Ordovician, Uxnorm, Estonia. 4,Orbignyella sublamellosaUlrich and Bassler, 1904, holotype of type species (USNM 43174), Pierce Limestone (Stones River Group), Ordovician, Murfreesboro, Tennessee. 5,Loxophragma lechriumBoardman, 1960, holotype of type species (USNM 133958), Wanakah Member of the Ludlowville Shale, Devonian, tributary of Buffalo Creek, Depew Quadrangle, New York. 6,Tetratoechus crassimuralis (Ulrich, 1890), paralectotype of type species (USNM 204845), Maquoketa Formation, (Richmondian), Ordovician, Wilmington, Illinois

Figure 3 — Serrated boundaries, all longitudinal sections, ×100; see text... Available to Purchase

Published: 01 November 2005
Figure 3 — Serrated boundaries, all longitudinal sections, ×100; see text for descriptions of photographs. 1, Rhombotrypa quadrata ( Rominger, 1866 ), hypotype of type species (USNM 204877), Waynesville Formation (Richmondian), Ordovician, Hanover, Ohio. 2, Gortanipora nodulosa ( Bassler
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FIGURE 3—Stratigraphic setting of the Onniella epibole at South Gate, Indiana. The epibole's stratigraphic position lies near the base of the Clarksville Member of the Waynesville Formation

FIGURE 3 —Stratigraphic setting of the Onniella epibole at South Gate, In... Available to Purchase

Published: 01 December 2000
FIGURE 3 —Stratigraphic setting of the Onniella epibole at South Gate, Indiana. The epibole's stratigraphic position lies near the base of the Clarksville Member of the Waynesville Formation
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FIGURE 6—Ambonychia specimen (beak to left) with a 4-tube cornulitid cluster and single tube, both oriented toward the posterior shell margin; another single tube attached in the beak area shows the same orientation; Waynesville Formation, Colerain Avenue site, CMC # P50649, X2.4

FIGURE 6 — Ambonychia specimen (beak to left) with a 4-tube cornulitid clu... Available to Purchase

Published: 01 December 2003
FIGURE 6 — Ambonychia specimen (beak to left) with a 4-tube cornulitid cluster and single tube, both oriented toward the posterior shell margin; another single tube attached in the beak area shows the same orientation; Waynesville Formation, Colerain Avenue site, CMC # P50649, X2.4
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Table 1.  The eight localities included in the study. Samples from the Fair... Available to Purchase

Published: 01 May 2009
Table 1.  The eight localities included in the study. Samples from the Fairview and Waynesville Formations com bine field collections with specimens from the Cincinnati Museum Center. Samples from the Benbolt Limestone, Decorah Shale, Girardeau Limestone, Lebanon Limestone, and the Bromide
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Figure 4

Relative model support for Kope (left column) and Waynesville (right column... Available to Purchase

Published: 01 May 2016
Figure 4 Relative model support for Kope (left column) and Waynesville (right column) samples at scales of individual samples, aggregated stratigraphic sections, members, and entire formation species pool. Model support for samples and sections
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FIGURE 5—Beak area of an Ambonychia specimen showing paired cornulitid clusters: an 8-tube cluster of Cornulites attached to one shell and a 4-tube cluster attached to the other shell. The Ambonychia is preserved in a butterfly position. Note the growth direction of both clusters away from the beak. Specimen collected by Dan Zimmerman, from the Waynesville Formation, Collins Run near Oxford, Ohio, CMC # P50648, X3.

FIGURE 5 —Beak area of an Ambonychia specimen showing paired cornulitid c... Available to Purchase

Published: 01 December 2003
the beak. Specimen collected by Dan Zimmerman, from the Waynesville Formation, Collins Run near Oxford, Ohio, CMC # P50648, X3.
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FIGURE 1—Hardground from the Onniella epibole of the Waynesville Formation exposed at Bon Well Hill near Brookville, Indiana (roadcut on the west side of Route 101, 1.8 miles north of its intersection with Route 52, N39° 26.327′, W 84° 59.278′). Note the borings through the Onniella meeki valves, clipping their edges, and into the limestone matrix. Note also the valve with two borings. (Specimen C/W-111-90 in the College of Wooster collections; scale bar equals 5.0 mm.)

FIGURE 1 —Hardground from the Onniella epibole of the Waynesville Formati... Available to Purchase

Published: 01 October 2001
FIGURE 1 —Hardground from the Onniella epibole of the Waynesville Formation exposed at Bon Well Hill near Brookville, Indiana (roadcut on the west side of Route 101, 1.8 miles north of its intersection with Route 52, N39° 26.327′, W 84° 59.278′). Note the borings through the Onniella meeki
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Figure8—Diaphragmed mesopores. 1, 2,Calloporella harrisiUlrich, 1883, paralectotype of type species (USNM 508952), Waynesville Formation (Richmondian), Ordovician, Waynesville, Ohio, ×100; 1, double-walled (compound) autozooecial wall (center of photograph) between two mesopores, broadly serrated autozooecial boundaries, cortex and cingulum layers, longitudinal; 2, circular autozooecia with cortex and cingulum layers and intervening thin polygonal mesopore walls, tangential. 3,Dekayella sp. (USNM 146499), Fairmount Formation (Maysvillian), Ordovician, Covington, Kentucky, thick diaphragm/extension units of mesopore one on top of the other, thin diaphragms of autozooecia so close together that they were structural not basal, longitudinal, ×100. 4,Hallopora sp. (USNM 167698), Waldron Formation, Silurian, railroad cut at White's Bend on Tennessee Hwy. 12, Nashville, Tennessee, preserved indication of polypide in autozooecium, mesopores on each side short with closely spaced structural diaphragms and their extensions into mesopore/autozooecial walls, mural spines of autozooecial wall aligned longitudinally and typical of trepostomes pointed inwardly, longitudinal, ×100. 5,Hallopora elegantula, hypotype of type species (USNM 186567), Rochester Shale, Silurian, Lockport, New York, autozooids budded in endozone with thin diaphragms, mesopores in exozones with more closely spaced diaphragms, below, pair of mesopores produced apparent autozooid, longitudinal, ×30

Figure 8 —Diaphragmed mesopores. 1, 2, Calloporella harrisi Ulrich, 188... Available to Purchase

Published: 01 November 2005
Figure 8 —Diaphragmed mesopores. 1, 2, Calloporella harrisi Ulrich, 1883 , paralectotype of type species (USNM 508952), Waynesville Formation (Richmondian), Ordovician, Waynesville, Ohio, ×100; 1, double-walled (compound) autozooecial wall (center of photograph) between two mesopores, broadly
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Macroscopic gastropods from the Marble Hill Bed at Bedford, Kentucky (A–D; Roadcut on US Highway 42, 4 km east of US Highway 421, 38.625000°N, 85.250000°W), and from the Waynesville Formation near Rectorville, Kentucky (road cut on Kentucky Highway 9 just east of Bridgeport Road 38.567617°N, 83.642235°W). Thin section (A, C, E) with respective tracings (B, D, F) showing the distribution of primary and secondary shell. A, B) Paupospirabowdeni (Safford 1869). C, D) Clathrospira conica (Ulrich and Scofield 1897). E, F) Cyclonema sp. All figures to same scale.

Macroscopic gastropods from the Marble Hill Bed at Bedford, Kentucky (A–D; ... Available to Purchase

Published: 01 March 2016
Fig. 6.— Macroscopic gastropods from the Marble Hill Bed at Bedford, Kentucky (A–D; Roadcut on US Highway 42, 4 km east of US Highway 421, 38.625000°N, 85.250000°W), and from the Waynesville Formation near Rectorville, Kentucky (road cut on Kentucky Highway 9 just east of Bridgeport Road
Journal Article

Epizoozoan trepostome bryozoans on nautiloids from the Upper Ordovician (Katian) of the Cincinnati Arch region, U.S.A.: an assessment of growth, form, and water flow dynamics Available to Purchase

Patrick N. Wyse Jackson, Marcus M. Key, Jr., Stephen P. Coakley
Published: 01 May 2014
Journal of Paleontology (2014) 88 (3): 475–487.
DOI: https://doi.org/10.1666/13-138
... such as the Treptoceras duseri shale of the Waynesville Formation where they make up 89 percent of the nautiloid fauna ( Frey, 1988 , 1989 ), and thus provide a common substrate, as indicated with over 50 percent carrying episkeletozoans ( Frey, 1989 ). While much of the sediment being deposited at this time...
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View PDF for article title, Epizoozoan trepostome bryozoans on nautiloids from the Upper Ordovician (Katian) of the Cincinnati Arch region, U.S.A.: an assessment of growth, form, and water flow dynamics
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Journal Article

Paleoecologic Associations and Secondary Tiering of Cornulites on Crinoids and Bivalves in the Upper Ordovician (Cincinnatian) of Southwestern Ohio, Southeastern Indiana, and Northern Kentucky Available to Purchase

ROBERT W. MORRIS, STEPHEN H. FELTON
Journal: PALAIOS
Published: 01 December 2003
PALAIOS (2003) 18 (6): 546–558.
DOI: https://doi.org/10.1669/0883-1351(2003)018<0546:PAASTO>2.0.CO;2
...FIGURE 6 — Ambonychia specimen (beak to left) with a 4-tube cornulitid cluster and single tube, both oriented toward the posterior shell margin; another single tube attached in the beak area shows the same orientation; Waynesville Formation, Colerain Avenue site, CMC # P50649, X2.4 ...
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View PDF for article title, Paleoecologic Associations and Secondary Tiering of Cornulites on Crinoids and Bivalves in the Upper Ordovician (Cincinnatian) of Southwestern Ohio, Southeastern Indiana, and Northern Kentucky
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Journal Article

LATE ORDOVICIAN JAWED POLYCHAETE FAUNAS OF THE TYPE CINCINNATIAN REGION, U.S.A Available to Purchase

MATS ERIKSSON, CLAES F. BERGMAN
Published: 01 May 2003
Journal of Paleontology (2003) 77 (3): 509–523.
DOI: https://doi.org/10.1666/0022-3360(2003)077<0509:LOJPFO>2.0.CO;2
...” (Waynesville Formation) (see below). Although this family occurs in high abundance, the diversity is generally very low in each sample. One or sometimes two species commonly dominate, and the maximum number of co-occurring polychaetaspid species is four. The second most common family is less obvious...
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View PDF for article title, LATE ORDOVICIAN JAWED POLYCHAETE FAUNAS OF THE TYPE CINCINNATIAN REGION, U.S.A
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Figure6—Mesopores and styles, all longitudinal sections. 1, 5,Dekayella ulrichi (Nicholson, 1881), hypotypes of type species, Southgate (Edenian), Ordovician, railroad at Bald Knob, Cincinnati, Ohio; 1, USNM 146501, mesopores in early exozone crowded out by later autozooidal growth, longitudinal, ×30; 5, USNM 146505, two styles in upper half of photograph grew into overgrowth apparently without pause, presumably obtaining nutrients and calcification from overgrowth, ×50. 2,Stigmatella crenulataUlrich and Bassler, 1904, primary type of type species (USNM 526051), Waynesville Formation (Richmondian), Ordovician, Hanover, Ohio; cystose mesopores in early exozone crowded out by later autozooidal growth, vertical zone of midcourse styles, longitudinal, ×30. 3,Homotrypa curvataUlrich, 1882, topotype of type species (USNM 40212), Fairmount Member of the Fairview Formation (Maysvillian), Ordovician, Covington, Kentucky; two endozonal styles, maculum with mesopores in center, ×30. 4,Dekayia maculataJames, 1881, holotype (USNM 146296), upper Eden Shales, Loveland, Ohio; endozonal style and zooecial style, ×30

Figure 6 —Mesopores and styles, all longitudinal sections. 1, 5, Dekayel... Available to Purchase

Published: 01 November 2005
, longitudinal, ×30; 5, USNM 146505, two styles in upper half of photograph grew into overgrowth apparently without pause, presumably obtaining nutrients and calcification from overgrowth, ×50. 2, Stigmatella crenulata Ulrich and Bassler, 1904 , primary type of type species (USNM 526051), Waynesville