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Journal Article

MAPESITES , A NEW UPPER PENNSYLVANIAN (LOWER VIRGILIAN) AMMONOID FROM KANSAS Available to Purchase

DAVID M. WORK, DARWIN R. BOARDMAN
Published: 01 November 2003
Journal of Paleontology (2003) 77 (6): 1195–1197.
DOI: https://doi.org/10.1666/0022-3360(2003)077<1195:MANUPL>2.0.CO;2
... digitations; and small, rounded umbilical lobe. Sutural formula: ( V 1 V 1 ) LU:ID For Royal H. Mapes in recognition of his numerous contributions to the Pennsylvanian paleontology of the Midcontinent. Lower Virgilian strata ( Pseudaktubites stainbrooki ammonoid Subzone) in the Little Pawnee...
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View PDF for article title, MAPESITES , A NEW UPPER PENNSYLVANIAN (<span class="search-highlight">LOWER</span> <span class="search-highlight">VIRGILIAN</span>) AMMONOID FROM KANSAS
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Journal Article

Stratigraphic Architecture of the Tonganoxie Paleovalley Fill (Lower Virgilian) in Northeastern Kansas Available to Purchase

Howard R. Feldman, Martin R. Gibling, Allen W. Archer, Winton G. Wightman, William P. Lanier
Journal: AAPG Bulletin
Published: 01 July 1995
AAPG Bulletin (1995) 79 (7): 1019–1042.
DOI: https://doi.org/10.1306/8D2B21B9-171E-11D7-8645000102C1865D
... is within the lowest Virgilian (Stephanian) Douglas Group ( Figure 2 ). The underlying Lansing Group and overlying lower Shawnee Group both contain thick, laterally extensive limestones and typical Kansas-type cyclothems ( Heckel, 1977 ). In contrast, the Douglas Group in Kansas lacks the thick limestones...
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View PDF for article title, Stratigraphic Architecture of the Tonganoxie Paleovalley Fill (<span class="search-highlight">Lower</span> <span class="search-highlight">Virgilian</span>) in Northeastern Kansas
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Schematic cross section of upper Missourian to lower Virgilian stratal succession along outcrop belt (see Figs. 1, 4), supplemented with shallow subsurface data. The cross section is slightly oblique to depositional dip. Geometric relationships have been somewhat altered to show three-dimensional relationships in a single cross-section. Small-scale variations in thickness have been smoothed, and thicknesses of thin units (such as black shales and coals) have been exaggerated for readability. Sequence boundaries (red) are shown as solid lines only in areas where they can be confidently correlated. Basinward extent of SB 4 is based on subsurface extension of the large incised valley basinward; no interfluve SB has been recognized for this sequence. Construction of cross section is based on observations from our previous studies (Joeckel 1989, 1994, 1995a; Cunningham and Franseen, 1992; Feldman et al. 1993b; Feldman et al. 1995; Feldman et al. 1997; Lanier et al. 1993; Archer et al. 1994; Archer and Feldman 1995; Heckel and Watney 2002), our new data introduced in this paper, and supplemented with data from Bowsher and Jewett (1943), Ball (1964), Troell (1969), Kansas City Power and Light (1975), and Goebel et al. (1989). Significantly modified from Archer and Feldman (1995).

Schematic cross section of upper Missourian to lower Virgilian stratal succ... Available to Purchase

Published: 01 May 2005
Figure 5 Schematic cross section of upper Missourian to lower Virgilian stratal succession along outcrop belt (see Figs. 1 , 4 ), supplemented with shallow subsurface data. The cross section is slightly oblique to depositional dip. Geometric relationships have been somewhat altered to show
Image
—Outcrop distribution of Missourian and lower Virgilian phylloid algal-mound complexes in eastern Kansas and adjacent states. Wide areas with oblique lining represent outcrop of mound complexes; narrow lines represent nonmound facies; all traces are straightened and simplified. Lines 1-3 mark alignments of mound terminations and other features in Missourian rocks (after Heckel and Cocke, 1969).

—Outcrop distribution of Missourian and lower Virgilian phylloid algal-moun... Available to Purchase

Published: 01 February 1975
Fig. 2 —Outcrop distribution of Missourian and lower Virgilian phylloid algal-mound complexes in eastern Kansas and adjacent states. Wide areas with oblique lining represent outcrop of mound complexes; narrow lines represent nonmound facies; all traces are straightened and simplified. Lines 1-3
Image
—Outcrop distribution of Missourian and lower Virgilian phylloid algal-mound complexes in eastern Kansas and adjacent states. Wide areas with oblique lining represent outcrop of mound complexes; narrow lines represent nonmound facies; all traces are straightened and simplified. Lines 1, 2, and 3 mark alignments of mound terminations and other features in Missourian rocks.

—Outcrop distribution of Missourian and lower Virgilian phylloid algal-moun... Available to Purchase

Published: 01 May 1969
FIG. 2. —Outcrop distribution of Missourian and lower Virgilian phylloid algal-mound complexes in eastern Kansas and adjacent states. Wide areas with oblique lining represent outcrop of mound complexes; narrow lines represent nonmound facies; all traces are straightened and simplified. Lines 1
Image
—Cross section of lower Virgilian and upper Missourian beds in eastern Sedgwick County Kansas, illustrating lithologic changes. Well numbers refer to Table I excepting No. 5A, The Texas Company’s Hutchins No. 1, SE. 14, SE. 14, SW. 14, Sec. 26, T. 27 S., R. 3 E., western Butler County, which is included to show relationship of Stalnaker sandstone to lower Virgilian limestones and shales.

—Cross section of lower Virgilian and upper Missourian beds in eastern Sedg... Available to Purchase

Published: 01 February 1949
Fig. 4. —Cross section of lower Virgilian and upper Missourian beds in eastern Sedgwick County Kansas, illustrating lithologic changes. Well numbers refer to Table I excepting No. 5A, The Texas Company’s Hutchins No. 1, SE. 1 4 , SE. 1 4 , SW. 1 4 , Sec. 26, T. 27
Journal Article

Subsurface Cross Sections from Marion County Kansas, to Osage County, Oklahoma Available to Purchase

L. H. Lukert
Journal: AAPG Bulletin
Published: 01 February 1949
AAPG Bulletin (1949) 33 (2): 131–152.
DOI: https://doi.org/10.1306/3D933D16-16B1-11D7-8645000102C1865D
...Fig. 4. —Cross section of lower Virgilian and upper Missourian beds in eastern Sedgwick County Kansas, illustrating lithologic changes. Well numbers refer to Table I excepting No. 5A, The Texas Company’s Hutchins No. 1, SE. 1 4 , SE. 1 4 , SW. 1 4 , Sec. 26, T. 27...
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View PDF for article title, Subsurface Cross Sections from Marion County Kansas, to Osage County, Oklahoma
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Journal Article

Paleoecology of Nodulose Zone at Top of Haskell Limestone (Upper Pennsylvanian) in Kansas Available to Purchase

Halsey W. Miller, Ada Swineford
Journal: AAPG Bulletin
Published: 01 September 1957
AAPG Bulletin (1957) 41 (9): 2012–2036.
DOI: https://doi.org/10.1306/0BDA5954-16BD-11D7-8645000102C1865D
...Halsey W. Miller; Ada Swineford ABSTRACT A paleoecological study was made of a phosphatic nodule zone at the base of the Robbins shale (lower Virgilian, Upper Pennsylvanian) in Douglas County, Kansas. The nodules formed in shallow marine basins or bays which are inferred to have been characterized...
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View PDF for article title, Paleoecology of Nodulose Zone at Top of Haskell Limestone (Upper Pennsylvanian) in Kansas
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Journal Article

Phylloid Algal-Mound Complexes in Outcropping Upper Pennsylvanian Rocks of Mid-Continent Available to Purchase

Philip H. Heckel, J. M. Cocke
Journal: AAPG Bulletin
Published: 01 May 1969
AAPG Bulletin (1969) 53 (5): 1058–1074.
DOI: https://doi.org/10.1306/5D25C819-16C1-11D7-8645000102C1865D
...FIG. 2. —Outcrop distribution of Missourian and lower Virgilian phylloid algal-mound complexes in eastern Kansas and adjacent states. Wide areas with oblique lining represent outcrop of mound complexes; narrow lines represent nonmound facies; all traces are straightened and simplified. Lines 1...
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View PDF for article title, Phylloid Algal-Mound Complexes in Outcropping Upper Pennsylvanian Rocks of Mid-Continent
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Paleodepositional map of the Virgilian regional stage (see Figure 2 for time reference). See the Figure 3 caption for notes regarding Figures 4–8. Note north-south–trending green dashed line on right denoting position of the lower Virgilian carbonate shelf margin (i.e., Gonzales equivalent, Figure 2). Red line obliquely crosscutting the southern part of study area = Permian terminal position of Ouachita thrust front.

Paleodepositional map of the Virgilian regional stage (see Figure 2 for t... Available to Purchase

Published: 01 September 2011
Figure 8 Paleodepositional map of the Virgilian regional stage (see Figure 2 for time reference). See the Figure 3 caption for notes regarding Figures 4 – 8 . Note north-south–trending green dashed line on right denoting position of the lower Virgilian carbonate shelf margin (i.e
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—(From Moore, and others, 1951, p. 68) Generalized columnar section of lower Virgilian rocks. Position of phosphatic nodule zone indicated by row of open ellipses.

—(From Moore, and others, 1951, p. 68) Generalized columnar section of lowe... Available to Purchase

Published: 01 September 1957
Fig. 3. —(From Moore, and others, 1951, p. 68) Generalized columnar section of lower Virgilian rocks. Position of phosphatic nodule zone indicated by row of open ellipses.
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—Classification of lower and middle Virgilian rocks in northern Mid-Continent region. Column at extreme left shows agreed inter-state classification which is subject to modifications imposed by lateral variations of deposits. Other columns indicate previous usage in several states. Some deviations shown, especially in Douglas group, will persist. In northern Oklahoma there are unsettled questions of classification and nomenclature.

—Classification of lower and middle Virgilian rocks in northern Mid-Contine... Available to Purchase

Published: 01 November 1948
Fig. 5. —Classification of lower and middle Virgilian rocks in northern Mid-Continent region. Column at extreme left shows agreed inter-state classification which is subject to modifications imposed by lateral variations of deposits. Other columns indicate previous usage in several states. Some
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 Figure3—Dunbarites from the North American Midcontinent. 1, 2, 13–17,Dunbarites rectilateralis from the Quivira Shale Member, Dewey Formation, Dewey (Quivira) cyclothem, middle Missourian, north-central Oklahoma (1, 2) and the Dugout Creek beds member, Gaptank Formation, middle Missourian, West Texas (13–17); 1, 2, right lateral and ventral views of hypotype SUI 8873, ×5; 13–15, ventral, right lateral, and apertural views of lectotype YPM 12934a, ×5; 16, 17, left lateral and ventral views of paralectotype YPM 12934b, ×5. 3–9,Dunbarites wewokensis n. sp. from the Upper Shale member (Lake Neosho Shale equivalent), Wewoka Formation, Altamont (Lake Neosho) cyclothem, upper Desmoinesian, south-central Oklahoma (3–6) and the Middle Shale member (Anna Shale equivalent), Wewoka Formation, Pawnee (Anna) cyclothem, upper Desmoinesian, south-central Oklahoma (7–9); 3, 4, left lateral and ventral views of holotype SUI 48683, ×5; 5, 6, right lateral and ventral views of paratype SUI 8896, ×5; 7–9, apertural, right lateral, and ventral views of paratype SUI 8802, ×5. 10–12, 18–21,Dunbarites boardmani n. sp. from the Uddenites Shale Member, Gaptank Formation, mid-lower Virgilian, West Texas (10–12) and the Colony Creek Shale Member, Caddo Creek Formation, basal Virgilian, north-central Texas (18–21); 10–12, ventral, right lateral, and apertural views of paratype SUI 104280, ×5; 18–20, ventral, left lateral, and apertural views of holotype SUI 54880, ×5; 21, oblique ventral view of paratype SUI 104279, an incomplete body chamber showing subterminal constriction and terminal flare (lower left) and ventrolateral lappets (lower right), ×4

Figure 3 — Dunbarites from the North American Midcontinent. 1, 2, 13–17,... Available to Purchase

Published: 01 May 2009
-lower Virgilian, West Texas ( 10–12 ) and the Colony Creek Shale Member, Caddo Creek Formation, basal Virgilian, north-central Texas ( 18–21 ); 10–12, ventral, right lateral, and apertural views of paratype SUI 104280, ×5; 18–20, ventral, left lateral, and apertural views of holotype SUI 54880, ×5
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—Ideal Upper Pennsylvanian megacyclothem showing complete development of all members, as typified by Oread megacyclothem in Shawnee Group of lower Virgilian Stage (after Moore, 1936, p. 26-35; 1949, p. 78-79, 144-145; personal observations). (O) marks shale members that are more like outside shale than black shale member. Megacyclothems of Missourian Stage lack lower, fifth, and commonly super limestone members. Inferred sea-level curves reflect two hypotheses: (1) simple short-term oscillation differentiating shale members from limestone members (dotted line, combining Moore, 1936, p. 30-35, and Wagner, 1966, p. 567); and (2) basically long-term oscillation with black shale member differentiated from other shale members on account of major depth-zone difference (solid line, after Evans, 1967, Fig. 6; Troell, 1969, p. 25, specifically for Oread megacyclothem; Schenk, 1967, p. 1379-1380, for Altamont megacyclothem). Inasmuch as most Missourian megacyclothems consist mainly of middle limestoneblack shale-upper limestone member sequence, hypothesis 2 for them becomes simple long-term oscillation of sea level.

—Ideal Upper Pennsylvanian megacyclothem showing complete development of al... Available to Purchase

Published: 01 March 1975
Fig. 1 —Ideal Upper Pennsylvanian megacyclothem showing complete development of all members, as typified by Oread megacyclothem in Shawnee Group of lower Virgilian Stage (after Moore, 1936 , p. 26-35; 1949 , p. 78-79, 144-145; personal observations). (O) marks shale members that are more like
Journal Article

Missourian and Virgilian Brachiopod Biostratigraphy, Bird Spring Group at Arrow Canyon, Clark County, Nevada: ABSTRACT Free

Eric W. Lipman, Ralph L. Langenheim*, Jr.
Journal: AAPG Bulletin
Published: 01 May 1982
AAPG Bulletin (1982) 66 (5): 594–595.
DOI: https://doi.org/10.1306/03B59F26-16D1-11D7-8645000102C1865D
... brachiopod assemblage totaling 21 strophomenids and 17 taxa of other orders. Fossil abundance is greatest in the lower part of the Missourian and from the topmost Missourian through the middle Virgilian. Correlation with the middle Virgilian of North Texas and, perhaps, the lower Missourian of the southwest...
View PDF for article title, Missourian and <span class="search-highlight">Virgilian</span> Brachiopod Biostratigraphy, Bird Spring Group at Arrow Canyon, Clark County, Nevada: ABSTRACT
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Journal Article

Late Pennsylvanian-Early Permian fusulinids from southeast Arizona Free

Floyd F. Sabins, Charles A. Ross
Published: 01 March 1963
Journal of Paleontology (1963) 37 (2): 323–365.
... disconformably overlying middle Des Moinesian beds. This early Virgilian sequence is overlain by a zone of middle to late Virgilian fusulinids, Triticites ventricosus sacramentoensis and Triticites cf. T. plummeri, that occurs in the uppermost beds of the Horquilla Limestone and ranges into the lower 20 to 235...
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Journal Article

Fusulinid Assemblages from Late Pennyslvanian and Early Permian of Southeastern Arizona: ABSTRACT Free

Charles A. Ross, Floyd F. Sabins, Jr.
Journal: AAPG Bulletin
Published: 01 February 1962
AAPG Bulletin (1962) 46 (2): 277.
DOI: https://doi.org/10.1306/BC7437EB-16BE-11D7-8645000102C1865D
...Charles A. Ross; Floyd F. Sabins, Jr. ABSTRACT The varied fusulinid faunas of the late Pennsylvanian (Virgilian) and early Permian (Wolfcampian) parts of the Naco Group and the Earp Formation can be divided into five assemblage zones. The lowest zone is characterized by Triticites cullomensis...
View PDF for article title, Fusulinid Assemblages from Late Pennyslvanian and Early Permian of Southeastern Arizona: ABSTRACT
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Pennsylvanian-Permian stratigraphy of the western (San Andres Mountains), eastern (Sacramento Mountains), and southern (Franklin Mountains) Orogrande basin. Phylloid algal mounds are present in the Virgilian Panther Seep Formation of the San Andres Mountains (this study), the Virgilian-lower Wolfcampian section of the Sacramento Mountains (references in text), and the Desmoinesian section of both ranges (Algeo et al. 1991). Middle-late Virgilian age for the western Orogrande mounds is based on fusulinid identifications by G. Wahlman and G. Wilde (data in Soreghan and Giles 1999a). Stratiform gypsum (carat pattern) is present in the uppermost Pennsylvanian section in the Franklin Mountains (references in text). Stratigraphy after Kottlowski et al. (1956), Otte (1959), and Harbour (1972).

Pennsylvanian-Permian stratigraphy of the western (San Andres Mountains), e... Available to Purchase

Published: 01 November 2000
-lower Wolfcampian section of the Sacramento Mountains (references in text), and the Desmoinesian section of both ranges ( Algeo et al. 1991 ). Middle-late Virgilian age for the western Orogrande mounds is based on fusulinid identifications by G. Wahlman and G. Wilde (data in Soreghan and Giles 1999a
Journal Article

New Occurrences of the Pennsylvanian Index Ammonoid Dunbarites from the North American Midcontinent Available to Purchase

David M. Work, Royal H. Mapes
Published: 01 May 2009
Journal of Paleontology (2009) 83 (3): 405–413.
DOI: https://doi.org/10.1666/08-144.1
...-lower Virgilian, West Texas ( 10–12 ) and the Colony Creek Shale Member, Caddo Creek Formation, basal Virgilian, north-central Texas ( 18–21 ); 10–12, ventral, right lateral, and apertural views of paratype SUI 104280, ×5; 18–20, ventral, left lateral, and apertural views of holotype SUI 54880, ×5...
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View PDF for article title, New Occurrences of the Pennsylvanian Index Ammonoid Dunbarites from the North American Midcontinent
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Pennsylvanian and Early Permian Paleogeography, Southern Colorado Plateau and Vicinity Available to Purchase

Ronald C. Blakey
Journal: AAPG Bulletin
Published: 01 May 1980
AAPG Bulletin (1980) 64 (5): 677.
DOI: https://doi.org/10.1306/2F918B3A-16CE-11D7-8645000102C1865D
...Ronald C. Blakey Abstract Pennsylvanian and Lower Permian sedimentary rocks of the southern Colorado Plateau have been the subject of controversy concerning their correlation and origin. Paralic sediments of the Supai group (Morrowan, Atokan, Virgilian, and Wolfcampian) were deposited in the Grand...
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