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Paleocene Vertebrates from Jabal Umm Himar, Kingdom of Saudi Arabia U.S. GEOLOGICAL SURVEY BULLETIN 2093 Prepared in cooperation with the Ministry of Petroleum and Mineral Resources, Jiddah, Kingdom of Saudi Arabia "~-· I I I ~ ' .. I • ....... = .. ·' ~ ·- AVAILABILITY OF BOOKS AND MAPS OF THE U.S. GEOLOGICAL SURVEY Instructions on ordering publications of the U.S. Geological Survey, along with prices of the last offerings, are given in the current- / year issues of the monthly catalog "New Publications of the U.S. Geological Survey.'' Prices of available U.S. Geological Survey publica tions released prior to the current year are listed in the most recent annual "Price and Availability List." Publications that may be listed in various U.S. Geological Survey catalogs (see back inside cover) but not listed in the most recent annual "Price and Availability List" may be no longer available. 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U.S. Geological Survey offices: U.S. Geological Survey, Information Services Box 25286, Federal Center, Denver, CO 80225 Residents of Alaska may order maps from • FAIRBANKS, Alaska-New Federal Bldg., 101 Twelfth U.S. Geological Survey, Earth Science Information Center Ave. - 101 Twelfth Ave.-Box 12 • ROLLA, Missouri-1400 Independence Rd. •' Fairbanks, AK 99701. . STENNIS SPACE CENTER, Mississippi-Bldg. 3101 ... .. • .J ... .• ' . .. .......... . .. . ·~ . ... Paleocene Vertebrates from Jabal Umm Himar, Kingdom of Saudi Arabia Edited by Frank C. Whitmore, Jr., and Cary T. Madden U.S. GEOLOGICAL SURVEY BULLETIN 2093 Prepared in cooperation with the Ministry of Petroleum and Mineral Resources, Jiddah, Kingdom of Saudi Arabia UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1995 U.S. DEPARTMENT OF THE INTERIOR BRUCE BABBITT, Secretary U.S. GEOLOGICAL SURVEY GORDON P. EATON, Director For sale by U.S. Geological Survey, Information Services Box 25286, Federal Center, Denver, CO 80225 Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. Published in the Eastern Region, Reston, Va. Manuscript approved for publication Aprill4, 1994. Library of Congress Cataloging in Publication Data Paleocene vertebrates from Jabal Umm Himar, kingdom of Saudi Arabia I edited by Frank C. Whitmore, Jr., and Cary T. Madden. p. em.-(U.S. Geological Survey bulletin; 2093A-F) "Prepared in cooperation with the Ministry of Petroleum and Mineral Resources, Kingdom of Saudi Arabia." Includes bibliographical references. Supt. ofDocs. no.: Ul9.3:2093A-F 1. Vertebrates, Fossil-Saudi Arabia. 2. Paleontology-Paleocene. I. Whitmore, Frank C., Jr. II. Madden, Cary T. III. Geological Survey (U.S.). IV. Saudi Arabia. Wizarat al-Batriil wa-al-Tharwah al-Ma' diniyah. V. Series. QE75.B9 no. 2093A-F [QE841] 557.3 s-dc20 94-32990 [566'.09538] CIP CONTENTS [Letters indicate the chapter.] A. The Umm Himar Formation (Paleocene) of Saudi Arabia and Associated Strata: Stratigraphy, Vertebrate Fauna, and Paleoenvironment By Cary T. Madden, Frank C. Whitmore, Jr., Dwight L. Schmidt, and Ibne Mohammed Naqvi B. A Paleocene Percoid Fish, Tentatively Referred to the Family Serranidae, from Jabal Umm Himar, Kingdom of Saudi Arabia By P.H. Greenwood C. Paleocene Amiid Fish from Jabal Umm Himar, Kingdom of Saudi Arabia By Mark VH. Wilson D. A Paleocene Lungfish, Ceratodus humei Priem 1914, from Jabal Umm Himar, Kingdom of Saudi Arabia By Frank C. Whitmore, Jr. E. Paleocene Pelomedusid Turtles from Jabal Umm Himar, Kingdom of Saudi Arabia By Roger C. Wood F. Dyrosaurs (Crocodilia, Mesosuchia) from the Paleocene Umm Himar Formation, Kingdom of Saudi Arabia By Wann Langston, Jr. III The Umm Himar Formation (Paleocene) of Saudi Arabia and Associated Strata: Stratigraphy, Vertebrate Fauna, and Paleoenvironment By Cary T. Madden, Frank C. Whitmore, Jr., Dwight L. Schmidt, and Ibne Mohammed Naqvi PALEOCENE VERTEBRATES FROM JABAL UMM HIMAR, KINGDOM OF SAUDI ARABIA U.S. GEOLOGICAL SURVEY BULLETIN 2093-A Prepared in cooperation with the Ministry of Petroleum and Mineral Resources, Jiddah, Kingdom of Saudi Arabia UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1995 CONTENTS Abstract.......................................................................................................................... A 1 Introduction . . .. . . . . .. . . . . . . . . . .. . . . . . . . . . . .. . . . .. . . . . .. . . . .. . . . . .. . . . . .. . . . .. . . . . .. . . . . . . . . . .. . . . . .. . . . . .. . . . .. . .. . . . . . . .. . . . . 1 Previous Investigations.......................................................................................... 4 Acknowledgments................................................................................................. 4 Stratigraphy . . .. .. . .. . . . . .. . . . . .. . . . . .. . . . . .. . . . .. . . . . .. . . . .. . . . . . . . . . . .. . .. . . . . . . .. . . . .. . . . . . . .. . . .. . . . . . . . . . .. . . . . .. . . . .. . . . . 4 Khurma Formation .. . . . . .. . . . . . .......... ... .. ... .. . . . . . . . .. . . . .. . . . . .. . . . . .. . . . . . . . . . .. . . . . . . . . . .. . . . . ... . .. . . . . . 4 U mm Himar Formation......................................................................................... 4 Chert...................................................................................................................... 5 Laterite................................................................................................................... 7 Harrat Hadan Basalt.............................................................................................. 7 Fauna............................................................................................................................. 9 Age................................................................................................................................ 13 Environment . .. . . . . . . . . . . .. . . . .. . . . . .. . . . . .. . . . . . . . .. .. . . . . .. .. .... . . . . . . . . .. .. . . . . . . . . .. . . . .. . . . . .. . .. . .. .. . .. . . . . . . . . . .. . .. . 14 Other Vertebrate Fossils from the Arabian Peninsula ............ ........... ... .. ..... .... .. .. .. .. ...... 15 Geologic History........................................................................................................... 16 References . . . . .. . . . . . . . . . . .. . . . .. . . . . .. . . . . .. . . . . . . . . . .. . . . . . . . .. .. .. . .. . . . . .. .. . . .. . . . . .. . .. .. . . . . . . . . . . .. . . . .. . . . . . . . . . .. .. . . 17 FIGURES AI. Map of western Saudi Arabia, showing location of Jabal Umm Himar area.............................................................. A2 A2. Geologic map of Jabal Umm Himar area, showing fossil localities........................................................................... 3 A3. Stratigraphic sections measured at vertebrate fossil localities in the Jabal Umm Himar area.................................... 6 A4. Composite stratigraphic columnar section of Umm Himar Formation and overlying and underlying rocks in Jabal U mm Hi mar area................................................................................................................................................ 8 A5. Tertiary diagram showing composition of dolomitic limestone from the upper member of the Umm Himar Formation . . .. . . .. . . . . . . . . . . .. . . . . . . . . . .. . .. . .. . . . . . . . . .. .. . . . . . . . . .. . . . .. . . . . .. . . . . .. . . . . . . . . . .. . . . . . . . . . . .. . . . .. . . . . .. . . . . .. . . . . . . . . . .. . .. .. . . . . . . . . . . .. .. ... . . . .. . . . . . .. . .. 11 A6. Diagram showing isotopic age plotted against K 0 content for basaltic rocks from Harrat Hadan and other 2 areas............................................................................................................................................................................. 11 TABLES AI. Chemical analyses for Fe 0 and FeO and semiquantitative spectrographic analyses for other elements in 2 3 iron-oxide materials from the Jabal Umm Himar area ................................................................................................ A9 A2. Partial chemical analyses, in percent, for major elements of samples from the dolomitic limestone member of the Umm Himar Formation, Jabal Umm Himar area. The average of five samples of pisolitic laterite from nearby Jabal Saq is also given................................................................................................................................................. 10 A3. List of vertebrate fossils from the localiJies at Jabal Umm Himar. ............................................................................. 12 All The Umm Himar Formation (Paleocene) of Saudi Arabia and Associated Strata: Stratigraphy, Vertebrate Fauna, and Paleoenvironment By Cary T. Madden,1 Frank C. Whitmore, Jr.,2 Dwight L. Schmidt,3 and Ibne Mohammed Naqvi4 ABSTRACT The paleoenvironment of Jabal Umm Himar was estu arine. The presence of a coastal environment indicates that The first Paleocene vertebrate fauna known from the at least a shallow sea must have existed in the At Taif region Arabian Peninsula is represented by fossils collected from during the earliest Tertiary. 21 localities at Jabal Umm Himar, near Turabah, Southern Hijaz Province, Saudi Arabia. The fossils are from a mud INTRODUCTION stone, 2-3 meters thick, in the Umm Himar Formation. This formation, about 20 meters thick, consists of three mem Jabal U mm Hi mar ("hill of the mother of the donkey") bers: (1) a basal ferruginous mudstone, (2) an interbedded is a large hill at lat 21°10'N., long 41°25'E., 100 km east of mudstone and shale, from which the fossils were recovered, At Taif and 26 km west of Turabah, in the central western and (3) an upper dolomitic limestone. The Umm Himar For part of Saudi Arabia (fig. A 1) . An unimproved desert road mation is underlain by Nubian-like quartzose sandstone, connecting At Taif and Turabah crosses the Jabal Umm which overlies Precambrian rocks. The formation is over Hi mar area (fig. A2) in the Jabal In quadrangle (Gonzalez, lain by the Harrat Hadan Basalt of late Oligocene and early 1973). All parts of the area are readily accessible by four Miocene age. wheel-drive vehicle over the desert plain. The plain is at an The vertebrates include sand sharks (Odontaspis sub altitude of about 1,200 m and small hills rise 10-50 m above striata); nurse sharks (Ginglymostoma maghrebianum and it. The conspicuous basalt plateau of Harrat Hadan rises G. sokotoense); eagle rays (Myliobatis dixoni); torpedos nearly 200 m above the desert plain in the northern part of (Eotorpedo hilgendorfi); pycnodont fish (Pychodus); perch the Jabal U mm Hi mar area. (Parapercichthys arabis); bowfins (Amiidae); catfish (Sil In 1971 two fossil vertebrates were collected by uriformes); lungfish ( Ceratodus humei); very large side Schmidt and Louis Gonzalez from a small wadi at locality 1 necked turtles (Pelomedusidae); and archaic crocodilians (fig. A2), 3.5 km northeast of Jabal Umm Himar. In 1974, (Rhabdognathus spp., Hyposaurus nopcsai, and Phosphato the fossils were identified by Whitmore as representing a saurus sp.). The Paleocene age determination for the fauna large member of the Mesosuchia, a widely distributed is based upon the stratigraphic ranges of the lungfish Cera (Africa, Europe, Asia, North America, and South America) todus humei, the dyrosaurid crocodilians Rhabdognathus suborder of archaic crocodilians that originated in the Early compressus and Hyposaurus nopcsai, and catfish (Siluri Jurassic and became extinct in the late Eocene. Additional formes). Although not conclusive evidence of a Paleocene surface material was collected during October 1974 by age, the sharks are consistent with this interpretation. The Schmidt, T.H. Kiilsgaard, R.H. Blank, and N.E. Gettings. most nearly comparable fauna is that of the Dange Forma The present report records the Paleocene vertebrates, tion of Sokoto Province, Nigeria, whose age has been deter stratigraphy, and environment of deposition in the Jabal mined, on the basis of Foraminifera, to be late Paleocene. Umm Himar area. This report is based upon paleontologic and geologic field investigations undertaken during July August 1976 and December-January 1978-79 (Madden and 1P.O. Box lin, El Prado, NM 87529. others, 1979). The fossils described in this bulletin consti 2l).S. Geological Survey, Rm. E-308, NHB 137, Smithsonian Institu tute the first Paleocene vertebrate fauna known from the tion, Washington, D.C. 20560. Arabian Peninsula. 3U .S. Geological Survey, MS 913, Box 25046, Denver Federal Center, Specimens discussed in this Bulletin have been Denver, CO 80225-0046. 4U.S. Geological Survey Saudi Arabian Mission, P.O. Box 1488, assigned numbers with the prefix SAP (for Saudi Arabian Jiddah, Saudi Arabia. Project) that identify them as to locality, higher taxon, and AI A2 PALEOCENE VERTEBRATES FROM JABAL UMM HIMAR, KINGDOM OF SAUDI ARABIA Figure Al. Index map of western Saudi Arabia, showing location of the Jabal Umm Himar area relative to the Hail Arch, the Sirhan-Turayf Basin, and other geologic features.

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A. The Umm Himar Formation (Paleocene) of Saudi Arabia and Associated Strata: Stratigraphy, Vertebrate Fauna, and Paleoenvironment. By Cary T.
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