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Brachiopods of the Bois Blanc Formation in New York

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Brachiopods of the Bois Blanc Formation in New York Brachiopods of the Bois Blanc Formation in New York GEOLOGICAL SURVEY PROFESSIONAL PAPER 584-B Brachiopods of the Bois Blanc Formation in New York By A. J. BOUCOT and]. G. JOHNSON STRATIGRAPHY AND PALEONTOLOGY OF THE BOIS BLANC FORMATION IN NEW YORK GEOLOGICAL SURVEY PROFESSIONAL PAPER 584-B Lithofacies summary and paleogeography of Bois Blanc correlatives in eastern North America and description of silicified brachiopods from New York UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1968 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402- Price 55 cents (paper cover) CONTENTS Page Page Abstract __________________________________________ _ B1 Systematic paleontology-Continued Introduction ______________________________________ _ 1 Coelospira HalL _______________________________ _ B13 Age and correlation ________________________________ _ 1 Aferistina HalL ________________________________ _ 13 Lower Devonian rensselaeriid zonation _______________ _ 4 N ucleospira HalL ______________________________ _ 14 Paleogeo.5raphy and lithofacies of strata of Schoharie age __ 5 Acrospirifer Helmbrecht and Wedekind ___________ _ 14 Systematic paleontology ____________________________ _ 7 Afucrospirifer Grabau __________________________ _ 15 Petrocrania Raymond __________________________ _ 7 Kozlowskiellina Boucot _________________________ _ 16 Dalejina Havlicek ______________________________ _ 7 Costispirifer Cooper ________________________ - ___ _ 16 Pentamerella Hall ______________________________ _ 8 Fimbrispirifer Cooper ______________________ - ___ _ 17 Leptaena Dalman ______________________________ _ 8 Elytha Fredericks __________________________ -_--- 18 Stropheodonta Hall _____________________________ _ 9 A mbocoelia Hall _________ ~ _____________________ _ 18 Schuchertella Girty ________· _____________________ _ 9 Cyrtinaella Fredericks __________________________ _ 18 Plicanoplia Boucot and Harper __________________ _ 10 Cloudothyris Boucot and Johnson, n. gen __________ _ 19 Eodevonaria Breger_____________________________ _ 10 Centronella Billings _____________________________ _ 20 Afachaeraria Cooper ____________________________ _ 10 Amphigenia HalL ______________________________ _ 20 Cupularostrum Sartenaer________________________ _ 11 References ________________________________________ _ 21 Atrypa Dalman ___________________________ _, ____ _ 12 Index ____________________________________________ _ 25 ILLUSTRATIONS [Plates follow index] PLATE 1. Petrocrania sp., Dalejina alsa (Hall), and Pentamerella cf. arata (Conrad). 2. Leptaena sp., Stropheodonta cf. demissa (Conrad), "Schuchertella" sp. A, and "Schuchertella" sp. B. 3. Eodevonaria arcuata (Hall), PHcanoplia? sp., Machaeraria carolina (Hall), Cupularostrum? sp., and Atrypa "reticularis" (Linnaeus). 4. Coelospira camilla Hall and M eristina nasuta (Conrad). 5. Nucleospira sp. and Acrosp£rifer duodenaria (Hall). 6. "Mucrospirifer" cf. macra (Hall), Megakozlowskiella raricosta (Conrad), "Costisp£rifer" unicus (Hall), and Fimbrispirifer divaricatus (Hall)?. 7. Elytha sp., Ambocoel1·a sp., Cyrtinaella bipl£cata (Hall), Centronella glansfagea (Hall), Cloudothyris postovalis Boucot and Johnson, and Cloudothyris cf. postovalis Boucot and Johnson. 8. AmpMgenia elongata (Vanuxem), Amphigenia preparva Boucot, and M eganterella finksi Boucot. Page FIGURE 1. Chart showing rensselaeriid zones in the Lower Devonian of eastern North America______ B5 2. Map showing lithofacies distribution of Bois Blanc-Schoharie correlatives in eastern North America_______________________________________________________________________ 6 TABLES Page TABLE 1. Brachiopods of the Bois Blanc Formation and its correlatives in eastern North America____ B2 2. Bois Blanc brachiopods described in this report_______________________________________ 4 III STRATIGRAPHY AND PALEONTOLOGY OF THE BOIS BLANC FORMATION IN NEW YORK BRACHIOPODS OF THE BOIS BLANC FORMATION IN NEW YORK By A. J. BoucOT and J. G. JoH~SON 1 ABS<TIRACT the basis of the brachiopod faunas and, in particular, Two localities in thin exposures of the Bois Blanc Formation the range of the genus Para.<sp~~rifer (Cooper, G. A., and of New York yielded silicified brachiopods comprising 25 articu­ others, 1942, p. 1732). Oliver ( 1960, p. B174) recognized late and one inarticulate species. One of these brachiopods, that the corals of the Edgecliff, Nedrow, and Moore­ Oloudo~hyris postovalis, is proposed as a new genus and species. Bois Blanc brachiopods compose an assemblage indicating cor­ house Members of the Onondaga are similar to Eifelian relation wit'h the Schoharie Formation of New York and its corals of western Europe and on this basis concluded equivalents elsewhere in eastern North Ameriea. Correlation, that the Onondaga is entirely of Middle Devonian age, based pimarily on acrospiriferid evolution, indicate's a late but he noted that the Bois Blanc (as Zone B) of New IDarly Devonian (Emsian) age for Schoharie-Bois Blanc rocks York may be distinguished from true Onondaga be­ in New' York and for their correlatives with a .similar brachiopod assemblage :at distant localities. cause of its different coral assemblage. Boucot (Boucot Provinciality of Appalachian Lower Devonian brachiopod and Arndt, 1960; Boucot, 1961 ; Boucot and others, faunas is exemplified by the endemic rensselaeriid terelbratulids 1964) concluded that the Onondaga in a broad sense is whose evolutionary changes form the basis for some fundamen­ of Early Emsian age because correlatives of the Bois tal Lower Devonian correlations in the region. Four renssel­ Blanc, namely the Littleton and Tomhegan Formations 'aeriid zones that span the Lower Devonian interval from t'he of New Hampshire and Maine, contain spiriferids of base of the Coeymans and Manlius Limestones to the top of the Schoharie-Bois Blanc may be recogliized. In ascending order, Early Emsian type. Oliver's recognition that "Zone B" Nanothyris. zone spans the Coeymans-New Scotland interval, the can be split off from the main mass of the Onondaga and Rensselaeria zone spans the Becraft-Oriskany, the Etymothyris assigned to the Bois Blanc now makes it possible to rec­ zo:pe coincides with the Esopus Formation, and the Amphigenia oncile these conflicting views. zone coincides with the Schoharie-Bois Blanc interval. This paper consists of a descriptive section in which The quartz-rich facies of Schoharie age consists of an almost continuous narrow belt of deposits from central Gaspe to Ala­ New York Bois Blanc brachiopods collected by W. A. bama. This belt is interpreted t 1o have lain adjacent to 1an east­ Oliver, Jr., are described and figured, together with ward land area which separated the quartz-rich facies from sections on the paleogeography and lithofacies relation­ terrigenous rocks with a Rhenish fa una, preserved in the An­ ships of Schoharie correlatives in eastern North Amer­ napolis Valley of Nova Scotia. West of the quartzose beLt is a ica. The authors do not attempt to cope with the ques­ broad expanse characterized predominantly by limestone and chert deposition during Sehoharie time. It extend's from the tion of the apparently missing Late Emsian shelly James Bay Lowland, south of Hudson Bay, to central Texas and faunas in eastern North America. The nonrecognition possilbly as far southwest as Chihuahua city in northern Mexico. thus far of Late Emsian age faunas in eastern North Between this area and t'he Cordilleran geosyncline to the west, America is very enigmatic; it may reflect our ignorance there is a broad expanse where marine deposits of Schoharie of either Late Emsian faunas or the evolutionary sig­ age are unknown and which probably was a'bove sea level dur­ ing that time, nificance of morphologically recognizable changes in the INTRODUCTION Late Emsian-Early Eifelian faunas. Cooper (in Cooper, G. A., and others, 1942) in the AGE AND CORRELATION correlation chart for the North American Devonian con­ Throughout the Appalachian faunal province (Bou­ eluded that the Onondaga Limestone of New York is cot, 1960) from Gaspe to Texas, a remarkably similar of late Early Devonian age. Assignment of the Onon­ assemblage of brachiopods occurs in the upper Lower daga by Cooper to the Lower Devonian was largely on Devonian. Prominent among these shells are Plioano­ 1 California Institute of Technology, Pasadena, Calif. plia, Eodevonaria arcuata, Prionothyris, and Oloudo- Bl B2 STRATIGRAPHY AND PALEONTOLOGY OF THE BOIS BLANC FORMATION IN NEW YORK TABLE !.-Brachiopods of the Bois Blanc Formation and lts correlatives in east~rn North America A B c D E F G H I J K L M N 0 p Q R s T ------------1---------------------------------------- Schizophoria sp _____________________________________________ cf ________________________________ X _______ _ DaleJina alsa_ _ _ _ _ _ _ _ _ _ _ _ _ _ _ X X _ __ _ cf . X cf _ _ _ _ _ _ _ _ cf cf _ _ _ _ _ _ _ _ cf _ _ _ _ _ _ _ _ cf _________ --- __ -- D· musculosa solaris______ ____ ____ X ________________ X ____________ cf ____________________ X X X Platyorthis peloris ___________ ____ X ____________________________ ---------------- ---- ------------------------ P. planoconvexa _________ ________ X ________________________ ---- ---- ---- ---- ---- ---- ---- ---- ---- ---- ---- Pentamerella arata ___________ X X ________ cf ____________________________________ cf X _______________ _ Leptaena sp- - __ ------ _____
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