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Hannibal Shale

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Journal Article
Journal: Palynology
Published: 01 January 2008
Palynology (2008) 32 (1): 27–37.
...SARAH HEAL; GEOFF CLAYTON Abstract Mississippian palynomorphs have been recovered from two successions of the Hannibal Shale in Missouri, U.S.A., which is the lowermost Carboniferous unit in the Mississippi Valley. The assemblages are dominated by acanthomorph acritarchs, with Micrhystridium...
FIGURES | View All (6)
Journal Article
Published: 01 January 2002
Journal of Paleontology (2002) 76 (1): 187–189.
... volution of body chamber. Hannibal Shale (lower part of Lower Siphonodella crenulata conodont Zone), at Clarence Cannon Dam, Salt River, Ralls County, northeastern Missouri. Goniocyclus hannibalensis most closely resembles G. cooperi Gordon, 1986 from the late Kinderhookian Caballero...
FIGURES
Journal Article
Published: 01 September 1988
Journal of Paleontology (1988) 62 (5): 772–778.
Series: DNAG, Centennial Field Guides
Published: 01 January 1987
DOI: 10.1130/0-8137-5403-8.133
EISBN: 9780813754093
... Abstract This is a major Mississippi River bluff exposure above a road next to the railroad yard on the southeast edge of Hannibal, Marion County, Missouri, just west of center of SE¼ Sec. 28, T.57N., R.4W., Hannibal East 7½-minute Quadrangle (Fig. 1). ...
Image
Miospores and acritarchs from the <b>Hannibal</b> <b>Shale</b>, Missouri, U.S.A. The samp...
in > Palynology
Published: 01 January 2008
PLATE 1 Miospores and acritarchs from the Hannibal Shale, Missouri, U.S.A. The sample number (prefixed S), England Finder co-ordinates, and museum catalogue number (prefixed TCD) are given as appropriate. All figures are Nomarski interference contrast images, illustrated at x750 magnification
Image
Figure  2 — Goniocyclus hannibalensis  n. sp. from the <b>Hannibal</b> <b>Shale</b>, Rall...
Published: 01 January 2002
Figure 2 — Goniocyclus hannibalensis n. sp. from the Hannibal Shale, Ralls County, Missouri. 1, Paratype SUI 62432; 2, paratype SUI 62431; 3, 4, holotype SUI 62430. All figures ×3.5
Series: AAPG Memoir, AAPG Memoir
Published: 01 January 1990
DOI: 10.1306/M51530C10
EISBN: 9781629811253
... Abstract The Chouteau Limestone is late Kinderhookian in age in Illinois and late Kinderhookian to Valmeyeran in Indiana (Rexroad and Scott, 1964). The Chouteau conformably overlies the Kinderhookian Hannibal Shale of the New Albany Group (Figures 7-1 and 2-12), except in southwestern Illinois...
Series: GSA Memoirs
Published: 01 March 1957
DOI: 10.1130/MEM67V2-p279
... by the greenish-gray siltstone, dark clay shales, and fine-grained olive sandstones of the Hannibal shale. The “Hamburg” strata contain an assemblage of small brachiopods, pelecypods, pieces of Bryozoa, and some small gastropods. The assemblage has been called a dwarf fauna, but the smallness of the individuals...
Journal Article
Journal: AAPG Bulletin
Published: 01 December 1951
AAPG Bulletin (1951) 35 (12): 2526–2541.
... formation of Missouri, the Hannibal shale of Missouri, the Sunbury shale of Ohio, the basal Orangeville shale of northern Ohio, and the very uppermost beds of the New Albany shale of Indiana. Beds slightly higher in the section contain conodonts of lower Chouteau age whereas those located 11.5–17.5 feet...
FIGURES
Journal Article
Published: 01 March 1968
Journal of Paleontology (1968) 42 (2): 525–555.
... useful species in establishing areal correlations among the Hannibal Shale, Bachelor Formation, Chouteau Limestone, Sedalia Dolomite, and Northview Shale. GeoRef, Copyright 2004, American Geological Institute. Reference includes data from Bibliography and Index of North American Geology, U. S...
Series: GSA Field Guide
Published: 01 January 2008
DOI: 10.1130/2008.fld012(06)
EISBN: 9780813756127
... Abstract Evansville, Indiana, USA, grew up along a curve of the Ohio River. Ready access to natural resources including wood, coal, limestone, sandstone, shale, sand, gravel, and clay facilitated its growth. Development of lines of commerce; notably, the road network, steamboat traffic...
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Journal Article
Published: 01 May 2000
Journal of Paleontology (2000) 74 (3): 369–380.
.... Mill Creek, Ashtabula County, between Ross Road Bridge and a point just south of a dam upstream. Float. 14. M. E. Williams, 1981. Mill Creek, Ashtabula County, from black shale outcrop above dam. Found in situ. 15. J. Hannibal, 1984. Mill Creek, Ashtabula County, from Ross Rd. Bridge to just...
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Journal Article
Published: 01 July 1983
Journal of Paleontology (1983) 57 (4): 705–716.
...Joseph T. Hannibal; Rodney M. Feldmann Abstract Trace fossils penetrating siltstone beds in the Chagrin Formation (Late Devonian, Famennian) at four localities in northeastern Ohio are herein named Chagrinichnites osgoodi. It is suggested that the trace maker was an echinocarid arthropod that made...
Journal Article
Journal: GSA Bulletin
Published: 01 March 1949
GSA Bulletin (1949) 60 (3): 403–438.
... from rocks of undoubted Mississippian age. I have assigned the Maple Mill shale to the upper Devonian because of these reasons; therefore, the Maple Mill shale must be redefined to indicate its Devonian age. The Maple Mill and Grassy Creek shales, of Iowa and Missouri respectively, are time equivalents...
Series: Geological Society, London, Special Publications
Published: 21 October 2020
DOI: 10.1144/SP486-2019-33
EISBN: 9781786204868
... ). The formation was originally named Berea grit by John Newberry, the head of the second Ohio Geological Survey, who provided a terse description (‘drab sandstone’) of the unit, noting its thickness (50 ft) in northern Ohio and the thickness of the rock units below (Bedford shale) and above it (Cuyahoga shale...
FIGURES | View All (12)
Series: GSA Field Guide
Published: 01 January 2017
DOI: 10.1130/2017.0046(01)
EISBN: 9780813756462
... Limestone Member comprises the uppermost unit of the Glenshaw Formation. During his trip, Lyell collected a marine fauna (brachiopods, snails, crinoids, and coral) from the Ames and associated beds close to river level ( Lyell, 1845 , p. 27-28). Casselman Formation shales, sandstones, limestones, coals...
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Series: GSA Field Guide
Published: 01 January 2011
DOI: 10.1130/2011.0020(07)
EISBN: 9780813756202
.... According to Fleeger et al. (2003 , p. 9) this quarry was the source of flux (limestone) and iron ore. The lime kiln (Figs. 16 and 17 ) preserved at this stop is unusual as it is completely, rather than partly, built into the limestone and shale bedrock of the hillside. The rock here was carved out...
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Series: GSA Field Guide
Published: 01 January 2011
DOI: 10.1130/2011.0020(07)
EISBN: 9780813756202
... Formation) was not good for millstones. This is an unusual statement that seems to imply that someone was using, or attempting to use, this conglomerate for millstones. Indeed they were ( Hannibal and Saja, 2009 ); a millstone found along Mill Creek (Stop 4) at the Lanterman’s Mill site in Youngstown...
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Series: Geological Society, London, Special Publications
Published: 21 October 2020
DOI: 10.1144/SP486-2017-188
EISBN: 9781786204868
... limestone. It is overlain by Carnian beds, which start with Cordevolian reef limestone that laterally passes into Cordevolian coarse, sparry, dolomite. The upper part of the limestone has a greater abundance of coral inclusions and shale intercalations ( Jelen 1990 ; Gale et al. 2018 ). This formation...
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Series: Geological Society, London, Special Publications
Published: 21 October 2020
DOI: 10.1144/SP486.4
EISBN: 9781786204868
... and feldspar grains in a ferruginous, micaceous, silty clay matrix cemented by clay, iron oxide, silica, and calcite. It is thin- to thick-bedded and massive and is both planar and crossbedded, especially in pebbly channel-fill sequences where angular red shale chips are locally common. The building stone...
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