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References and Appedices final.PDF

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References and Appedices final.PDF

TULANE STUDIES IN GEOLOGY AND PALEONTOLOGYVolume 19. Number 1July 31. 1986THE CALCAREOUS NANNOPLANKTON OF THE MIDWAY GROUP (PALEOCENE) OF ALABAMADAVID

References and Appedices final.PDFD D. REIMERS REIMERS RESEARCH HOUSTON.TEXASCONTENTSI.ABSTRACT ........................................ 1II.INTRODUCTION ..............................

..... 1III.PREVIOUS STUDIES ._............................. 7IV.LOCATION OF SAMPLED SECTIONS.................. 11V.TECHNIQUES AND PROCEDURES....12VI. References and Appedices final.PDF

RESULTS AND CONCLUSIONS ...................... 13VII.ACKNOWLEDGMENTS ................................ 18VIII.SYSTEMATIC PALEONTOLOGY ................

References and Appedices final.PDF

....... 18IX.REFERENCES......................... .. . . . . . . . . 46PLATES 1-14ILLUSTRATIONS ................................. beginningon p. 19

TULANE STUDIES IN GEOLOGY AND PALEONTOLOGYVolume 19. Number 1July 31. 1986THE CALCAREOUS NANNOPLANKTON OF THE MIDWAY GROUP (PALEOCENE) OF ALABAMADAVID

References and Appedices final.PDFcope and a scanning electron miscroscope. Twenty -seven species were identified, two of which are described as new. The nannoplankton distribution was

used to correlate the Alabama Midway Group with standard Paleocene nannoplankton zonations resulting in the Pine Barren and McBryde members of the Cl References and Appedices final.PDF

ayton Formation being assigned to the Crucipỉacoỉithus tenuis zone, and the Porters Creek Clay and the Matthews Landing Member being assigned to the C

References and Appedices final.PDF

yclococcolithina robusta zone. The nannoplankton distribution and abundances are related to the lithology and depositional environments of the Midway

TULANE STUDIES IN GEOLOGY AND PALEONTOLOGYVolume 19. Number 1July 31. 1986THE CALCAREOUS NANNOPLANKTON OF THE MIDWAY GROUP (PALEOCENE) OF ALABAMADAVID

References and Appedices final.PDFy shallowwater deposits of the Naheola Formation are barren of nannoplankton.II. INTRODUCTIONThe Midway Group of Alabama consists of three formations

(figure 1). These are, in order of stratigraphic sequence: (1) the Clayton Formation, which in central Alabama is divided into the lower Pine Barren M References and Appedices final.PDF

ember and the upper McBryde Limestone Member; (2) the Porters Creek Clay, present only in western Alabama, with the Matthew'S Landing Marl Member at t

References and Appedices final.PDF

he top; and (3) the Naheola Formation, present only in central and western Alabama, divided into the lower Oak Hill Member and the upper Coal Bluff Ma

TULANE STUDIES IN GEOLOGY AND PALEONTOLOGYVolume 19. Number 1July 31. 1986THE CALCAREOUS NANNOPLANKTON OF THE MIDWAY GROUP (PALEOCENE) OF ALABAMADAVID

References and Appedices final.PDF(figures 2, 3 and 4). This section at Midway Landing was described by Smith as having a few feet of black clay, which seemed equivalent to that at Bla

ck Bluff on the Tombigbee River (Porters Creek Clay), overlying about ten feet of gray, argillaceous limestone (the McBryde Limestone) with the nautil References and Appedices final.PDF

oidEDITORIAL COMMITTEE FOR THIS PAPER:2Tulane Studies in Geology and PaleontologyVol. 1’Western AlabamaCentral AlabamaEastern AlabamaFigure 1 - Format

References and Appedices final.PDF

ions and Members of the Midway Group in AlabamaEnclimatoceras. LaMoreaux and Toulmin (1953) described this Midway section as part of the McBryde Limes

TULANE STUDIES IN GEOLOGY AND PALEONTOLOGYVolume 19. Number 1July 31. 1986THE CALCAREOUS NANNOPLANKTON OF THE MIDWAY GROUP (PALEOCENE) OF ALABAMADAVID

References and Appedices final.PDF dammed, only the uppermost claystone ledge is exposed.The Clayton Formation was named for exposures near Clayton, Barbour County, Alabama by Smith (1

892). Exposures at the type locality, in a Central of Georgia Railroad-cut one mile east of Clayton, consist of approximately 12 feet of dense, crysta References and Appedices final.PDF

lline, gray limestone underlain by a tan, clayey sand (figures 2 and 5). LaMoreaux and Toulmin (1953) described the Clayton in Wilcox County, Alabama,

References and Appedices final.PDF

as consisting of about 140 feet of massive limestone with some basal sand. In extreme western Alabama the Clayton Formation consists of less than 20

TULANE STUDIES IN GEOLOGY AND PALEONTOLOGYVolume 19. Number 1July 31. 1986THE CALCAREOUS NANNOPLANKTON OF THE MIDWAY GROUP (PALEOCENE) OF ALABAMADAVID

References and Appedices final.PDFists of a sandy yellow, crystalline limestone containing TurritelUi alabamensis. The lower part of the member is a gray calcareous silt with induratet

j ledges. In Wilcox County the Pine Barren Member has an estimated thickness of 125 feet (LaMoreaux and Toulmin, 1953).The McBryde Limestone Member wa References and Appedices final.PDF

i named by MacNeil (1946) for exposures h roadcuts along Alabama Highway 21 Ù Wilcox County, approximately three milei west of McBryde Station. The st

References and Appedices final.PDF

ation nt longer exists but exposures can be fount along Highway 21 at a locality 0.2 milt south of the intersection of Highway 21 ant Highway 28 in Wi

TULANE STUDIES IN GEOLOGY AND PALEONTOLOGYVolume 19. Number 1July 31. 1986THE CALCAREOUS NANNOPLANKTON OF THE MIDWAY GROUP (PALEOCENE) OF ALABAMADAVID

References and Appedices final.PDFhttps.7/khothuvien.iNo. 1Midway Calcareous Nannoplankton3Farther west it becomes more clayey and intertongues with the lower part of the Porters Creek

Clay.The »P?.oir?rCreek Clay was named bySafford G864) for exposures west of Mid-dleton, Tennessee. The equivalent deposits in Alabama were originall References and Appedices final.PDF

y called the Sucarnoochee Clay by Smith (in Smith and Johnson, 1887) from exposures alongSucarnoochee Creek in Sumter County, Alabama. The type locali

References and Appedices final.PDF

ty of the Sucar-noochee Clay is Black Bluff on the Tombigbee River below its confluence with Sucarnoochee Creek (figures 2 and 6). In western Alabama,

TULANE STUDIES IN GEOLOGY AND PALEONTOLOGYVolume 19. Number 1July 31. 1986THE CALCAREOUS NANNOPLANKTON OF THE MIDWAY GROUP (PALEOCENE) OF ALABAMADAVID

References and Appedices final.PDFnt

TULANE STUDIES IN GEOLOGY AND PALEONTOLOGYVolume 19. Number 1July 31. 1986THE CALCAREOUS NANNOPLANKTON OF THE MIDWAY GROUP (PALEOCENE) OF ALABAMADAVID

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