Evolutionary Paleoecology of the Maryland Miocene
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Summary of the Paleontology of the Santa Fe Group (Mio-Pliocene), North-Central New Mexico Barry S
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/30 Summary of the paleontology of the Santa Fe Group (Mio-Pliocene), north-central New Mexico Barry S. Kues and Spencer G. Lucas, 1979, pp. 237-241 in: Santa Fe Country, Ingersoll, R. V. ; Woodward, L. A.; James, H. L.; [eds.], New Mexico Geological Society 30th Annual Fall Field Conference Guidebook, 310 p. This is one of many related papers that were included in the 1979 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States. -
Contributions from the Museum of Paleontology the University of Michigan
CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN VOL. 29.. No. 3. PP. 69-87 November 30. 1994 PROTOSIREN SMITHAE, NEW SPECIES (MAMMALIA, SIRENIA), FROM THE LATE MIDDLE EOCENE OF WADI HITAN, EGYPT BY DARYL P. DOMNING AND PHILIP D. GINGERICH MUSEUM OF PALEONTOLOGY THE UNIVERSITY OF MICHIGAN ANN ARBOR CONTRIBUTIONS FROM THE MUSEUM OF PALEONTOLOGY Philip D. Gingerich, Director This series of contributions from the Museum of Paleontology is a medium for publication of papers based chiefly on collections in the Museum. When the number of pages issued is sufficient to make a volume, a title page and a table of contents will be sent to libraries on the mailing list, and to individuals on request. A list of the separate issues may also be obtained by request. Correspondence should be directed to the Museum of Paleontology, The University of Michigan, Ann Arbor, Michigan 48 109-1079. VOLS. 2-29. Parts of volumes may be obtained if available. Price lists are available upon inquiry. PROTOSIREN SMITHAE, NEW SPECIES (MAMMALIA, SIRENIA), FROM THE LATE MIDDLE EOCENE OF WADI KITAN, EGYPT Abstract-Protosiren smithae is a new protosirenid sirenian described on the basis of associated cranial and postcranial material from the late middle Eocene (latest Bartonian) Gehannam Formation of Wadi Hitan (Zeuglodon Valley), Fayum Province, Egypt. The new species is similar to Protosiren fraasi Abel, 1907, from the earlier middle Eocene (Lutetian) of Egypt, but it is younger geologically and more derived morphologically. P. smithae is probably a direct descendant of P. fraasi. The postcranial skeleton of P. imithae- includes well-developed hindlimbs, which suggest some lingering amphibious tendencies in this otherwise aquatically-adapted primitive sea cow. -
Chapter 30. Latest Oligocene Through Early Miocene Isotopic Stratigraphy
Shackleton, N.J., Curry, W.B., Richter, C., and Bralower, T.J. (Eds.), 1997 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 154 30. LATEST OLIGOCENE THROUGH EARLY MIOCENE ISOTOPIC STRATIGRAPHY AND DEEP-WATER PALEOCEANOGRAPHY OF THE WESTERN EQUATORIAL ATLANTIC: SITES 926 AND 9291 B.P. Flower,2 J.C. Zachos,2 and E. Martin3 ABSTRACT Stable isotopic (d18O and d13C) and strontium isotopic (87Sr/86Sr) data generated from Ocean Drilling Program (ODP) Sites 926 and 929 on Ceara Rise provide a detailed chemostratigraphy for the latest Oligocene through early Miocene of the western Equatorial Atlantic. Oxygen isotopic data based on the benthic foraminifer Cibicidoides mundulus exhibit four distinct d18O excursions of more than 0.5ä, including event Mi1 near the Oligocene/Miocene boundary from 23.9 to 22.9 Ma and increases at about 21.5, 18 and 16.5 Ma, probably reßecting episodes of early Miocene Antarctic glaciation events (Mi1a, Mi1b, and Mi2). Carbon isotopic data exhibit well-known d13C increases near the Oligocene/Miocene boundary (~23.8 to 22.6 Ma) and near the early/middle Miocene boundary (~17.5 to 16 Ma). Strontium isotopic data reveal an unconformity in the Hole 926A sequence at about 304 meters below sea ßoor (mbsf); no such unconformity is observed at Site 929. The age of the unconfor- mity is estimated as 17.9 to 16.3 Ma based on a magnetostratigraphic calibration of the 87Sr/86Sr seawater curve, and as 17.4 to 15.8 Ma based on a biostratigraphic calibration. Shipboard biostratigraphic data are more consistent with the biostratigraphic calibration. -
RI37 Stratigraphic Nomenclature Of
,--' ( UNIVERSITY OF DELAWARE DELAWARE GEOLOGICAL SURVEY REPORT OF INVESTIGATIONS NO.37 STRATIGRAPHIC NOMENCLATURE OF NONMARINE CRETACEOUS ROCKS OF INNER MARGIN OF COASTAL PLAIN IN DELAWARE AND ADJACENT STATES BY ROBERT R. JORDAN STATE OF DELAWARE.. NEWARK, DELAWARE JUNE 1983 STRATIGRAPHIC NOMENCLATURE OF NONMARINE CRETACEOUS ROCKS OF INNER MARGIN OF COASTAL PLAIN IN DELAWARE AND ADJACENT STATES By Robert R. Jordan Delaware Geological Survey June 1983 TABLE OF CONTENTS Page ABSTRACT. ....... 1 INTRODUCTION ..... 2 Purpose and Scope. 2 Acknowledgments.. 4 REGIONAL SETTING. 4 Regional Relationships . 4 Structural Features. 5 DESCRIPTIONS OF UNITS .. 8 Historical Summary 8 Potomac Formation. 13 Nomenclature. 13 Extent. 13 Lithology . 14 Patuxent Formation . 18 Nomenclature. 18 Extent.. 18 Lithology .... 18 Arundel Formation. 19 Nomenclature.. 19 Extent. .• 19 Lithology • 20 Page Patapsco Formation. .. 20 Nomenclature . 20 Extent .. 20 Lithology.. 20 Raritan Formation . 21 Nomenclature .. 21 Extent .. 22 Lithology.. 23 Magothy Formation .. 24 Nomenclature . 24 Extent .. 24 Lithology.. 25 ENVIRONMENTS OF DEPOSITION 28 AGES .... 29 SUBDIVISIONS AND CORRELATIONS .. 32 REFERENCES . 34 ILLUSTRATIONS Figure 1. Geologic map of nonmarine Cretaceous deposits .. ..•.• •.. 3 2. Structural features of the Coastal Plain. ............ 6 3. Schematic diagram of lateral and vertical relationships of nonmarine Cretaceous deposits•....•... 34 TABLES Page Table 1. Usage of group and formation names. 9 STRATIGRAPHIC NOMENCLATURE OF NONMARINE CRETACEOUS ROCKS OF INNER MARGIN OF COASTAL PLAIN IN DELAWARE AND ADJACENT STATES ABSTRACT Rocks of Cretaceous age deposited in continental and marginal environments, and now found along the inner edge of the northern Atlantic Coastal Plain, have historically been classified as the Potomac Group and the Potomac, Patuxent, Arundel, Patapsco, Raritan, and Magothy forma tions. -
AASG Geothermal Data Metadata Template
Geothermal References Allen, E.P., Wilson, W.F., 1968, Geology and Mineral Resources of Orange County, North Carolina, North Carolina Geologic Survey, Bulletin 81, pp58 Allingham, J.W., 1970, Principal Facts for Gravity Stations in Howard County, MD, U.S. Geological Survey Open File Report 70-4, 19 pp. Amsden, T.W., Overbeck, R.M., and Martin, R.O.R., 1954, The Water Resources of Garrett County: Maryland Geological Survey, Bulletin 13, 3 plates, 349 p. Anderson, Campbell, 1976, Soil Characteristics of the Litholigic Units of Wake County, North Carolina, Open-File Report 73-1, North Carolina Geological Survey Anderson, D.N., and J.W. Lund (eds.), 1979, Direct Utilization of Geothermal Energy: A Layman's Guide, Geothermal Resources Council, Special Report No. 8, Davis, California, under U.S. DOE Contract ET-78-G-06- Anderson, J., 1948, Cretaceous and Tertiary Subsurface Geology: The Stratigraphy, Paleontology, and Sedimentology of Three Deep Test Wells on the Eastern Shore of Maryland: Maryland Geological Survey, Bulletin Andres, A.S., 2004, The Cat Hill Formation and Bethany Formation of Delaware: Delaware Geological Survey, Report of Investigation 67, 12 p. Andres, A.S., and C.S. Howard, 2000, RI62 The Cypress Swamp Formation, Delaware: Delaware Geological Survey, Report of Investigation 62, 18 p. Andres, A.S., Martin, M.J., 2005, Estimation of the Water Table for the Inland Bays Watershed, Delaware, Delaware Geological Survey Report of Investigations 68, 21 pp Andres, A.S., R.N. Benson, K.W. Ramsey, and J.H. Talley, 1990, Geologic and Hydrologic Studies of the Oligocene- Pleistocene Section Near Lewes, Delaware: Delaware Geological Survey, Report of Investigations 48, 39p. -
Isthminia Panamensis, a New Fossil Inioid (Mammalia, Cetacea) from the Chagres Formation of Panama and the Evolution of ‘River Dolphins’ in the Americas
Isthminia panamensis, a new fossil inioid (Mammalia, Cetacea) from the Chagres Formation of Panama and the evolution of ‘river dolphins’ in the Americas Nicholas D. Pyenson1,2, Jorge Velez-Juarbe´ 3,4, Carolina S. Gutstein1,5, Holly Little1, Dioselina Vigil6 and Aaron O’Dea6 1 Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, Washington, DC, USA 2 Departments of Mammalogy and Paleontology, Burke Museum of Natural History and Culture, Seattle, WA, USA 3 Department of Mammalogy, Natural History Museum of Los Angeles County, Los Angeles, CA, USA 4 Florida Museum of Natural History, University of Florida, Gainesville, FL, USA 5 Comision´ de Patrimonio Natural, Consejo de Monumentos Nacionales, Santiago, Chile 6 Smithsonian Tropical Research Institute, Balboa, Republic of Panama ABSTRACT In contrast to dominant mode of ecological transition in the evolution of marine mammals, different lineages of toothed whales (Odontoceti) have repeatedly invaded freshwater ecosystems during the Cenozoic era. The so-called ‘river dolphins’ are now recognized as independent lineages that converged on similar morphological specializations (e.g., longirostry). In South America, the two endemic ‘river dolphin’ lineages form a clade (Inioidea), with closely related fossil inioids from marine rock units in the South Pacific and North Atlantic oceans. Here we describe a new genus and species of fossil inioid, Isthminia panamensis, gen. et sp. nov. from the late Miocene of Panama. The type and only known specimen consists of a partial skull, mandibles, isolated teeth, a right scapula, and carpal elements recovered from Submitted 27 April 2015 the Pina˜ Facies of the Chagres Formation, along the Caribbean coast of Panama. -
Timeline of Natural History
Timeline of natural history This timeline of natural history summarizes significant geological and Life timeline Ice Ages biological events from the formation of the 0 — Primates Quater nary Flowers ←Earliest apes Earth to the arrival of modern humans. P Birds h Mammals – Plants Dinosaurs Times are listed in millions of years, or Karo o a n ← Andean Tetrapoda megaanni (Ma). -50 0 — e Arthropods Molluscs r ←Cambrian explosion o ← Cryoge nian Ediacara biota – z ←Earliest animals o ←Earliest plants i Multicellular -1000 — c Contents life ←Sexual reproduction Dating of the Geologic record – P r The earliest Solar System -1500 — o t Precambrian Supereon – e r Eukaryotes Hadean Eon o -2000 — z o Archean Eon i Huron ian – c Eoarchean Era ←Oxygen crisis Paleoarchean Era -2500 — ←Atmospheric oxygen Mesoarchean Era – Photosynthesis Neoarchean Era Pong ola Proterozoic Eon -3000 — A r Paleoproterozoic Era c – h Siderian Period e a Rhyacian Period -3500 — n ←Earliest oxygen Orosirian Period Single-celled – life Statherian Period -4000 — ←Earliest life Mesoproterozoic Era H Calymmian Period a water – d e Ectasian Period a ←Earliest water Stenian Period -4500 — n ←Earth (−4540) (million years ago) Clickable Neoproterozoic Era ( Tonian Period Cryogenian Period Ediacaran Period Phanerozoic Eon Paleozoic Era Cambrian Period Ordovician Period Silurian Period Devonian Period Carboniferous Period Permian Period Mesozoic Era Triassic Period Jurassic Period Cretaceous Period Cenozoic Era Paleogene Period Neogene Period Quaternary Period Etymology of period names References See also External links Dating of the Geologic record The Geologic record is the strata (layers) of rock in the planet's crust and the science of geology is much concerned with the age and origin of all rocks to determine the history and formation of Earth and to understand the forces that have acted upon it. -
From the Middle Eocene of Belgium
[Palaeontology, Vol. 53, Part 2, 2010, pp. 365–376] BONY-TOOTHED BIRDS (AVES: PELAGORNITHIDAE) FROM THE MIDDLE EOCENE OF BELGIUM by GERALD MAYR* and THIERRY SMITH *Forschungsinstitut Senckenberg, Sektion Ornithologie, Senckenberganlage 25, D-60325 Frankfurt am Main, Germany; e-mail [email protected] Royal Belgian Institute of Natural Sciences, Department of Paleontology, Rue Vautier 29, B-1000 Brussels, Belgium; e-mail [email protected] Typescript received 7 April 2009; accepted in revised form 19 July 2009 Abstract: We describe well-preserved remains of the Pelag- deidae (albatrosses) in overall morphology, but because ornithidae (bony-toothed birds) from the middle Eocene of bony-toothed birds lack apomorphies of the Procellariifor- Belgium, including a sternum, pectoral girdle bones and mes, the similarities are almost certainly owing to conver- humeri of a single individual. The specimens are tentatively gence. Bony-toothed birds were often compared with the assigned to Macrodontopteryx oweni Harrison and Walker, ‘Pelecaniformes’ by previous authors, who especially made 1976, which has so far only been known from the holotype comparisons with the Sulidae (gannets and boobies). How- skull and a referred proximal ulna. Another species, about ever, the coracoid distinctly differs from that of extant ‘pelec- two times larger, is represented by an incomplete humerus aniform’ birds, and the plesiomorphic presence of a foramen and tentatively identified as Dasornis emuinus (Bowerbank, nervi supracoracoidei as well as the absence of a well- 1854). The fossils provide critical new data on the osteology delimited articulation facet for the furcula supports a of the pectoral girdle of bony-toothed birds. For the first position outside the Suloidea, the clade to which the Sulidae time, the sternum of one of the smaller species is preserved, belong. -
Geologic Map and Cross Sections of the Leonardtown 30 X 60- Minute
U.S. DEPARTMENT OF THE INTERIOR U.S. GEOLOGICAL SURVEY Geologic Map and Cross Sections of the Leonardtown 30 X 60- Minute Quadrangle, Maryland and Virginia by Lucy McCartan1 Wayne L. Newell1 James P. Owens1 * Gary M. Bradford1** Open-File Report 95-665 Prepared in cooperation with the Maryland Geological Survey This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards (or with the North American Stratigraphic Code). Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. 1 Reston, Va. *Deceased **Volunteer for Science CONTENTS Page Introduction 3 Map contruction 4 Mapping paradigms 4 Time 5 Depositional environments 5 Previous work 6 Geologic overview 6 Structural setting 7 Ground-water chemistry 9 Discussion of selected stratigraphic units 10 Pleistocene deposits 11 Lowland unit Q2 11 Lowland unit Q3 11 Lowland unit Q4 11 Lowland unit Q5 12 Pliocene deposits 13 Upland unit T1 13 Yorktown Formation 14 Miocene deposits 14 Eastover Formation 14 St. Marys Formation 15 Choptank Formation 15 Calvert Formation 16 Pre-Miocene units 16 Nanjemoy Formation 17 Marlboro Clay 18 Aquia Formation 18 Acknowledgements 19 References cited 20 Description of map units 26 TABLES Units found only below land surface (see cross sections) 28 Table 1 Regional correlation of stratigraphic units 29 Table 2 Ground-water chemistry of selected formations 30 Table 3 Some typical characteristics of stratigraphic units 34 FIGURES Explanation of map units 35 Map symbols 36 Figure 1 Map showing distribution of depositional lithofacies of the Yorktown Formation 37 GEOLOGIC MAP AND CROSS SECTIONS OF THE LEONARDTOWN 30 X 60 MINUTE QUADRANGLE, MARYLAND AND VIRGINIA by Lucy McCartan, W.L. -
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A new marine vertebrate assemblage from the Late Neogene Purisima Formation in Central California, part II: Pinnipeds and Cetaceans Robert W. BOESSENECKER Department of Geology, University of Otago, 360 Leith Walk, P.O. Box 56, Dunedin, 9054 (New Zealand) and Department of Earth Sciences, Montana State University 200 Traphagen Hall, Bozeman, MT, 59715 (USA) and University of California Museum of Paleontology 1101 Valley Life Sciences Building, Berkeley, CA, 94720 (USA) [email protected] Boessenecker R. W. 2013. — A new marine vertebrate assemblage from the Late Neogene Purisima Formation in Central California, part II: Pinnipeds and Cetaceans. Geodiversitas 35 (4): 815-940. http://dx.doi.org/g2013n4a5 ABSTRACT e newly discovered Upper Miocene to Upper Pliocene San Gregorio assem- blage of the Purisima Formation in Central California has yielded a diverse collection of 34 marine vertebrate taxa, including eight sharks, two bony fish, three marine birds (described in a previous study), and 21 marine mammals. Pinnipeds include the walrus Dusignathus sp., cf. D. seftoni, the fur seal Cal- lorhinus sp., cf. C. gilmorei, and indeterminate otariid bones. Baleen whales include dwarf mysticetes (Herpetocetus bramblei Whitmore & Barnes, 2008, Herpetocetus sp.), two right whales (cf. Eubalaena sp. 1, cf. Eubalaena sp. 2), at least three balaenopterids (“Balaenoptera” cortesi “var.” portisi Sacco, 1890, cf. Balaenoptera, Balaenopteridae gen. et sp. indet.) and a new species of rorqual (Balaenoptera bertae n. sp.) that exhibits a number of derived features that place it within the genus Balaenoptera. is new species of Balaenoptera is relatively small (estimated 61 cm bizygomatic width) and exhibits a comparatively nar- row vertex, an obliquely (but precipitously) sloping frontal adjacent to vertex, anteriorly directed and short zygomatic processes, and squamosal creases. -
Mamiferosacuat/Cosdel Mioceno Medio Y Tardio De Argentina
UNIVERSIDAD NACIONAL DE LA PLATA FACULTAD DE CIENCIAS NATURALES Y MUSEO MAMIFEROSACUAT/COSDEL MIOCENO MEDIO Y TARDIO DE ARGENTINA SISTEMATICA, EVOLUCION Y BIOGEOGRAFIA por Mario Alberto COZZUOL Trabajo de Tesis para optar al Título de '~\ ,-- DOCTOR EN CIENCIAS NATURALES Director de Tesis: Dr. Rosendo PASCUAL La Plata -1993- A mis padres, Ruggero y N elly, porque siempre entendieron, me apoyaron y nunca cuestionaron mi decisión de elegir esta carrera. y A Tere, mi esposa, porque siempre estuvo allí, y porque aún está aquí. j i 1 ii : : ; ¡ .: RESUMEN Algunos de los mamíferos acuáticos del Mioceno tardío de Argentina se cuentan entre los primeros vertebrados fósiles en ser descriptos en el país, pese a lo cual la atención que estos grupos recibieron fue comparativamente escasa en relación a los mamíferos terrestres. En el presente trabajo se reestudian las especies previamente descriptas, y se describen varios nuevos taxones. El estudio se ha dividido en especies procedentes de sedimentitas marinas informalmente agrupadas bajo el nombre de "Entrerriense", y aquellas especies procedentes de aguas continentales, de sedimentitas agrupadas en el Piso/Edad Mesopotamiense, por primera vez propuesto aquí de manera formal. Dentro de las especies procedentes de sedimentitas marinas se han reconocido dos asociaciones consideradas diacrónicas. Las más antigua, referida · al Mioceno medio, procede de los afloramientos del ·"Entrerriense" de Patagonia, agrupandó seis especies, en su mayoría descriptas aquí por primera vez: Patagophyseter rionegrensis (Gondar) nueva combinación (Cetacea, Physeteridae); Notoziphius bruneti gen. y esp. nuevos (Cetacea, Ziphiidae); Goos valdesensis gen. y esp. nuevos (Cetacea, Balenidae); "Plesiocetus" notopelagicus Cabrera, 1926 (Cetacea, Cetotheriidae); Kawas benegasii gen. -
Smithsonian Contributions and Studies
Thecachampsa antiqua (Leidy, 1852) (Crocodylidae: Thoracosaurinae) from Fossil Marine Deposits at Lee Creek Mine, Aurora, North Carolina, USA Albert C. Myrick, Jr. Formation (early Pliocene; Gibson, 1983; Hazel, 1983). It ABSTRACT provides a first opportunity to study the Lee Creek crocodilian materials in relation to other similar forms of comparable geo- Fossil remains of crocodilians at Lee Creek Mine have been few and fragmentary. Nevertheless, isolated teeth and dermal plates logic age. The purpose of this paper is to describe the Lee from the spoil piles are identifiable as Thecachampsa antiqua Creek Mine crocodilian specimens and to comment on the (Leidy). This species was established by Leidy on characters of taxonomic status and paleozoogeographic implications related teeth presumably from the Calvert Formation of Virginia (late to the Lee Creek Mine occurrence and to occurrences of early to early middle Miocene), but the species is now validated by skulls and numerous elements from the middle Miocene forma- closely related forms elsewhere. tions of the Chesapeake Group. The same form is common in the ACKNOWLEDGMENTS.•The Lee Creek Mine specimens cit- Florida early Pliocene, where it is represented by several fairly ed in this report were collected and donated by P.J. Harmatuk, complete skeletons known as Gavialosuchus americanus (Sell- F. Hyne, and B. Hyne. I thank L.G. Barnes (Los Angeles arás). It also is known from numerous skulls from early and mid- County Museum of Natural History) for providing refresher dle Miocene formations near Lisbon, Portugal, as Tomistoma lusitanica (Vianna and Moraes). Teeth and a dermal scute indicat- information on the California specimens.