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Upper Cretaceous Ammonites from Haiti

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If you no longer need this publication write to the Geological Survey in Washington for an official mailing label to use in returning it UNITED STATES DEPARTMENT OF THE INTERIOR UPPER CRETACEOUS AMMONITES FROM HAITI GEOLOGICAL SURVEY PROFESSIONAL PAPER 214-A UNITED STATES DEPARTMENT OF THE INTERIOR J. A. Krug, Secretary GEOLOGICAL SURVEY W. E. Wrather, Director Professional Paper 214-A UPPER CRETACEOUS AMMONITES FROM HAITI BY JOHN B. REESIDE, JR. Shorter contributions to general geology. 1947 (Pages 1-11) UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1947 For sale by the Superintendent of Documents, U. S. Government Printing Office, Washington 25, D. C. Price 15 cents CONTENTS Abstract-...-..______.___-..__._._.__.,___.__^_-_________________________________ .____-_-_--__--__--__-_ _ _.. 1 General statement ____________________________________________________________________________ ________________ 1 The fossils and their correlation_________________________________________________________________________________ 1 Description of species __________________________________________________________________________________________ 2 References---_-___---_--__---___-_-______________..______ -_-___--__-______-__-_-___---__--_-_____-_--_--__-.-- 5 Index._______________________-__--____-______-_-______________-___-_-___-----___. ___-_-___--._._.__-_ _._.._ 11 ILLUSTRATIONS PLATES 1-3. Cretaceous ammonites from Haiti_____________-__--__--___-______-__-__--___ _._--__ .-_ _.___ __. _ 7-10 n UPPER CRETACEOUS AMMONITES FROM HAITI By JOHN B. REESIDE, Jr. ABSTRACT Pachydiscus ("Parapachydiscus") woodringi Reeside Ammonites of the genera Baculites, Parapuzosial, Pachydiscus, Paralenticeras sieAersi (Gerhardt) Texanites, and Paralenticeras are described from Haiti. Two Texanites ("Mortoniceras") cf. T. canaensis (Gerhardt) new species of Pachydiscus are proposed. The age of the fauna is interpreted as late lower Senonian. The nearest recorded occurrence of Upper Cretaceous ammonites in the West Indies is that in Jamaica re­ GENERAL STATEMENT ported by Spath (1925). From Providence, near Port Antonia, in shales underlying a limestone with Rudistae In recent work in the Republic of Haiti Messrs. and rather low in the sequence, were described Epigoni- W. P. Woodring and L. S. Gardner, of the Geological ceras sp., Parapachydiscus aff. P. stallauensis (Imkellcr), Survey, made a collection of Upper Cretaceous ammon­ Parapachydiscus aff. P. gollevillensis (D'Orbigny), Glyp- ites that seems worthy of record. From the neighbor­ toxoceras cf. G. rugatum (Forbes), and Baculites sp. This ing Dominican Republic Gabb (1873, p. 87) long ago fauna is assigned by Spath to the upper Senonian reported an ammonite and a dubious baculite, but the (Campanian-Maestrichtian). writer knows of no other published report of such From Jamaica also Trechmann (1936) reported the fossils from the island of Hispaniola. occurrence of an ammonite in "probably the lowest Dr. Woodring has kindly supplied the following known fossiliferous shales, 800 feet below a Barreftia statement: limestone," that was identified by Spath as Nowakites The ammonites were collected from boulders of weathered, aff. N. paillettei (D'Orbigny). This form is said to relatively soft calcareous sandstone, containing pebbles and suggest a "Senonian (upper Coniacian or lower San- granules of basalt, at two localities in Riviere Corail, a south­ eastward-flowing stream entering Grand Riviere about 8 miles tonian) age." north of Jacmel. The country rock is basalt, part of an exten­ The next nearest occurrence of Upper Cretaceous sive area of basalt in the interior of the Southern Peninsula. ammonites is that in central Puerto Rico recorded by About 6 miles to the west-northwest limy sediments interbedded Meyerhoff (1932), who reports identifications by Ree­ with the basalt and including basalt pillows contain caprinids side of Barroisiceras aff. B. haberfellneri (Von Hauer) indicating late Lower Cretaceous age (Aptian-Albian). The fossiliferous boulders found on Riviere Corail may represent and Parapuzosia aff. P. corbarica (Grossbuvre) from sediments interbedded with the basalt, or an Upper Cretaceous tuft'aceous deposits. These were assigned to the lower formation overlying the basalt, or may have been derived from Senonian (Coniacian). conglomerate at the base of Eocene limestone, which overlies A third occurrence is that recorded by Rutten 1936, the basalt at localities examined. pp. 35, 36), who lists apparently preliminary identifica­ The precise location of the two finds is as follows: tions by Jaworski of ammonites from three localities in U. S. Geological Survey Mesozoic locality 18723. the central part of Santa Clara Province, Cuba. These Petite Riviere (or Riviere Corail), about 2 miles north­ are reported as from limestones intercalated in the tuff west of junction with Grande Riviere de Jacmel, Arron- series, which underlies the Habana formation, of dissement of Jacmel, southern part of the Republic of Maestrichtian age. The forms found at the three Haiti. localities are as follows: (1) Austiniceras dibleyi Spath, U. S. Geological Survey Mesozoic locality 18724. Pachydiscus cf. P. colligatus Binckhorst, Peroniceras Same as 18723 but 200 feet northwest of junction. aff. P. tricarinatum (Fric) Burckhardt, P. cf. P. csorrigi (Redtenbacher); (2) Peroniceras cocchi Meiieghini, P. THE FOSSILS AND THEIR CORRELATION aff. P. tricarinatum, Crioceras sp.; and (3) Austiniceras The ammonites contained in this collection are as dibleyi Spath, Barroisiceras sp. This fauna is assigned follows: to a Turonian-Emscherian (Coniacian) age. A pertinent fauna is found in Venezuela. Gerhardt Baculites sp. Parapuzosia? sp. (1897, pp. 70-84) recorded an Upper Cretaceous ammo­ Pachydiscus ("Parapachydiscus") gardneri Reeside nite fauna from western Venezuela, giving the source of 732202—47 1 SHORTER CONTRIBUTIONS TO GENERAL GEOLOGY, 1947 the material as a blue-black bituminous limestone near of Texas, that is, Campanian. To the present writer Rubio, between Cana and Amarillo, State of Tachira. it seems most likely that the Haitian ammonites are to The species recorded are: Mortoniceras texanum (Roe- be placed as approximately Santonian, that is, late mer), M. canaen.se Gerhardt, Gauthien'ceras lenti Ger- lower Senonian. hardt, 0. margae (Schluter), Amaltheus siewrsi Gerhardt, and Lenticeras andii Gerhardt. These were assigned DESCRIPTION OF SPECIES to the lower Seiionian (Coiiiacian-Santoiiian). Liddle Genus BACULITES Lamarck (1928, p. 168) assigned Gerhardt's locality to the Colon shale, to include the La Luna limestone as that term Baculites sp. indet. was used by Liddle. He also cited from the lower part Plate 3, figures 1-6 of the Colon shale at a locality on the road between Three small fragments of an apparently smooth San Cristobal and Cucuta, in the State of Tachira, species of baculite with broad-ovate cross section and Amaltheus siei^ersi and Lenticeras andii, and from a simple suture were found. One specimen measures 3.1 locality on Quebrada La Luna, in the District of Perija, mm. in greatest diameter and 2.8 mm. in least State of Zulia, Mortoniceras texanum, Amaltheus sie- diameter; the second is very nearly the same; the third versi, and Gauthiericeras lenti. At both these localities is smaller but is much crushed. As these specimens other species also are cited. Liddle (p. 169) says of the are juvenile it is not profitable to make comparisons, sequence in the vicinity of Rubio, hence near Gerhardt's and they are recorded and illustrated for what they are locality: worth. To the west and southwest of Rubio there are good sections of Figured specimens: U. S. N. M. 104163. the Colon shales exposed. Limestone nodules and lentils carry Occurrence: U. S. G. S. 18723. a good ammonite fauna. The few thin limestone beds, which are intercalated with the shales, are very poorly fossiliferous. Most of the ammonites come from a cherty, nodular horizon near Genus PAEAPUZOSIA Nowak the base of the shales. Parapuzosia? sp. Kehrer (1937, pp. 48-51) describes the La Luna lime­ stone near Colon, Tachira, as including black and gray Plate 3, figures 7-10 cherts above and dark well-bedded limestone below. A single, very young specimen that retains parts of The overlying Colon shale is said to be dark shale with the shell differs from all others of similar size in the some intercalated limestones. It would seem that collection. Gerhardt's locality and Liddle's locality in Tachira are The shell is compressed. Cross section of whorl oval, in the upper part of the La Luna limestone of present higher than wide, flanks and venter evenly rounded. usage. Hedberg and Sass (1937, p. 80) refer Liddle's Umbilicus moderately wide, with low but distinct locality in Perija also to the La Luna. umbilical wall; umbilical shoulder rounded. Measure­ The ammonites from Haiti seem to have little in com­ ments in millimeters and percentage of diameter: mon with those from Jamaica, for the species of Pachy­ Diameter, 11.7; height of outer whorl, 4.6, 39; thickness discus present are not closely related, and there is still of outer whorl, 4.1, 35; width of umbilicus, 3.4, 29. less in common with the ammonites listed from Puerto The shell is apparently nearly smooth throughout. Rico and Cuba. On the contrary, the fauna reported At a diameter of approximately 7 mm., the internal by Gerhardt from southwestern Venezuela appears to mold shows a clear constriction running from the inner be closely related. Gerhardt's list includes both a part
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  • The Upper Campanian – Lower Maastrichtian Cephalopod Fauna of Botellos, Nuevo León: a Key to Understand Faunal Turnover Acros

    The Upper Campanian – Lower Maastrichtian Cephalopod Fauna of Botellos, Nuevo León: a Key to Understand Faunal Turnover Acros

    Acta Geologica Polonica, Vol. 67 (2017), No. 1, pp. 145–162 DOI: 10.1515/agp-2017-0009 The Upper Campanian – lower Maastrichtian cephalopod fauna of Botellos, Nuevo León: a key to understand faunal turnover across the Campanian–Maastrichtian boundary in NE Mexico CHRISTINA IFRIM1*, JACOBO EDGAR LARA DE LA CERDA2, VICTOR HUGO PEÑA PONCE2 and WOLFGANG STINNESBECK1 1Institut für Geowissenschaften, Ruprecht-Karls-Universität, D-69120 Heidelberg, Germany *E-mail: [email protected] 2Universidad Humanista De Las Americas, Martin de Zavala # 510, Monterrey, C.P. 64000, N.L., México ABSTRACT: Ifrim, C., Lara de la Cerda, J.E., Peña Ponce, V.H. and Stinnesbeck, W. 2017. The Upper Campanian – lower Maastrichtian cephalopod fauna of Botellos, Nuevo León: a key to understand faunal turnover across the Campanian–Maastrichtian boundary in NE Mexico. Acta Geologica Polonica, 67 (1), 145–162. Warszawa. A new cephalopod collection from the Campanian-Maastrichtian boundary interval of NE Mexico, consisting of 1076 individuals assigned to 29 species and 22 genera is presented. This collection is a mix of ammonoids, one coleoid and one nautilid, which originate from at least three ammonoid biozones: The upper Campan- ian Exiteloceras jenneyi and Nostoceras (Nostoceras) hyatti zones, and the lower Maastrichtian Pachydiscus (Pachydiscus) neubergicus Zone. The age of the collection is thus middle late Campanian to late early Maas- trichtian, and it closes a stratigraphic gap between faunas described formerly from this region. The specimens are nuclei collected from the desert pavement. The abundance of specimens allows for a comparison to other Campanian–Maastrichtian ammonoid records from Mexico, North America and Europe.
  • Cretaceous Ammonite Distributions and the Opening of the South Atlantic

    Cretaceous Ammonite Distributions and the Opening of the South Atlantic

    Cretaceous ammonite distributions and the opening of the South Atlantic WILLIAM JAMES KENNEDY & MICHAEL COOPER SUMMARY Analysis of distribution patterns of middle to absence of early Turonian marine deposits in late Cretaceous ammonites along the line of Southern Africa), but such evidence as is the opening S. Atlantic suggest that open available also suggests continued connection. marine connections, if not actual rifting, Palaeobiogeographic evidence is thus corn- developed during early upper Albian times, patible with sea floor spreading and palaeo- and extended continuously to the close of the magnetic data, rather than in conflict, as Cenomanian. Evidence of early Turonian previouslysuggested. distributions is equivocal (due largely to an PALAEOMAONETIC and sea floor spreading data (Creer et al. I965; Amaral et al. I966; McDougaU & Ruegg I966; Saito et al. x966; Siedner & Miller x968; Maxwell et al. I97o; Valencio & Vilas I97o ) have suggested to recent authors that initial rifling between Africa and S. America began in early or mid- Cretaceous times, while the recovery of chalks and nannofossil oozes of Albian to Cenomanian date from the Walvis Ridge (Pastouret & Goslin I974) confirms this view. In contrast, studies of distribution patterns of Cretaceous marine invertebrates, notably ammonites, from coastal basins flanking the south Atlantic (Beurlen I96I , Reyment i969-72 , Reyment & Tait I972, Cooper x972-I974) are held to indicate that a continuous marine connection between N. and S. Atlantic areas was not established until the close of the early Turonian. We would suggest on the basis of recent work on mid to late Cretaceous faunas from Angola (Cooper I972-I974) , Zululand and Natal (South Africa) (Kennedy & Klinger I97I , in press) that faunal distributions rather confirm a far earlier open marine N.-S.
  • Cretaceous Ammonites from the Lower Part of the Matanuska Formation Southern Alaska

    Cretaceous Ammonites from the Lower Part of the Matanuska Formation Southern Alaska

    Cretaceous Ammonites From the Lower Part of The Matanuska Formation Southern Alaska By DAVID L. JONES With a STRATIGRAPHIC SUMMARY By ARTHUR GRANT2 GEOLOGICAL SURVEY PROFESSIONAL PAPER 547 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1967 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library of Congress catalog-card No. GS 66-286 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 - Price $1.25 (paper cover) CONTENTS Page Abstract-----------__-------------------------------- 1 Stratigraphic summary of the lower part of the Matanuska Introduction--------------------------------------- 1 Formation-Continued Mid-Cretaceous faunal sequence in southern Alaska- - - - .. 2 Unit B, sandstone of Cenomanian age-- _---------- 3 Unit C, strata of Cenomanian to Santonian(?) age--- Cenomanian - - - - - - _ - - - - - - - - - - - - - - - - - - - - - - - - - - - - 4 Unit Gl, lutite of Cenomanian to Coniacian or Stratigraphic summary of the lower part of the Matanuska Santonian age-____----------------------- Formation, by Arthur Grants -------_______--------- Unit G2, composite sequence of Coniacian and Unit A, strata of Albian age ...................... Santonian(?) age .......................... Limestone Hills area- - ----____-------------- Regional correlation of the lower part of the Matanuska North front of the Chugach Mountains--- - - - - - Forrnation_____---------------------------------- Matanuska Valley---------_-____---------
  • Albian and Cenomanian Ammonites of the Eastern Margin of the Lut Block (East Iran)

    Albian and Cenomanian Ammonites of the Eastern Margin of the Lut Block (East Iran)

    Carnets Geol. 16 (25) Albian and Cenomanian ammonites of the eastern margin of the Lut block (East Iran) Javad SHARIFI 1 Seyed Naser RAISOSSADAT 2, 3 Maryam MORTAZAVI MEHRIZI 4 Maryam MOTAMEDALSHARIATI 5 Abstract: Upper Albian and Lower Cenomanian ammonites occur on the eastern margin of the Lut block in eastern Iran. The ammonite assemblages described herein are from the Nimbolook and Kerch sections located west of Qayen. The following taxa are described: Mantelliceras mantelli (J. SOWERBY, 1814), Mantelliceras saxbii (SHARPE, 1857), Mantelliceras sp. 1, Mantelliceras sp. 2, Mantelliceras sp. 3, Sharpeiceras laticlavium (SHARPE, 1855), Sharpeiceras schlueteri (HYATT, 1903), Puzosia (Puzosia) mayoriana (ORBIGNY, 1841), Hyphoplites costosus C.W. WRIGHT & E.V. WRIGHT, 1949, Mortoniceras (Mortoniceras) cf. fallax (BREISTROFFER, 1940), Mantelliceras cf. mantelli (J. SOWERBY, 1814), Caly- coceras (Gentoniceras) aff. gentoni (BRONGNIART, 1822), Idiohamites fremonti (MARCOU, 1858), Mariella (Mariella) sp., Mariella (Mariella) dorsetensis (SPATH, 1926), and Turrilites costatus LAMARCK, 1801. The ammonite assemblages clearly indicate a late Albian-middle Cenomanian age for the Nimbolook section and late Albian-early Cenomanian age for the Kerch section. Key-words: • Albian; • Cenomanian; • Cretaceous; • ammonites; • systematic paleontology; • biostratigraphy; • Qayen; • Lut block; • Iran. Citation: SHARIFI J., RAISOSSADAT S.N., MORTAZAVI MEHRIZI M. & MOTAMEDALSHARIATI M. (2016).- Albian and Cenomanian ammonites of the Eastern margin of the Lut block (East Iran).- Carnets Geol., Madrid, vol. 16, no. 25, p. 591-613. Résumé : Ammonites albiennes et cénomaniennes de la bordure orientale du bloc de Lut (E Iran).- Des ammonites de l'Albien supérieur et du Cénomanien inférieur sont présentes sur la bordure orientale du bloc de Lut dans la partie orientale de l'Iran.