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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. -
Estimating the Evolutionary Rates in Mosasauroids and Plesiosaurs: Discussion of Niche Occupation in Late Cretaceous Seas
Estimating the evolutionary rates in mosasauroids and plesiosaurs: discussion of niche occupation in Late Cretaceous seas Daniel Madzia1 and Andrea Cau2 1 Department of Evolutionary Paleobiology, Institute of Paleobiology, Polish Academy of Sciences, Warsaw, Poland 2 Independent, Parma, Italy ABSTRACT Observations of temporal overlap of niche occupation among Late Cretaceous marine amniotes suggest that the rise and diversification of mosasauroid squamates might have been influenced by competition with or disappearance of some plesiosaur taxa. We discuss that hypothesis through comparisons of the rates of morphological evolution of mosasauroids throughout their evolutionary history with those inferred for contemporary plesiosaur clades. We used expanded versions of two species- level phylogenetic datasets of both these groups, updated them with stratigraphic information, and analyzed using the Bayesian inference to estimate the rates of divergence for each clade. The oscillations in evolutionary rates of the mosasauroid and plesiosaur lineages that overlapped in time and space were then used as a baseline for discussion and comparisons of traits that can affect the shape of the niche structures of aquatic amniotes, such as tooth morphologies, body size, swimming abilities, metabolism, and reproduction. Only two groups of plesiosaurs are considered to be possible niche competitors of mosasauroids: the brachauchenine pliosaurids and the polycotylid leptocleidians. However, direct evidence for interactions between mosasauroids and plesiosaurs is scarce and limited only to large mosasauroids as the Submitted 31 July 2019 predators/scavengers and polycotylids as their prey. The first mosasauroids differed Accepted 18 March 2020 from contemporary plesiosaurs in certain aspects of all discussed traits and no evidence Published 13 April 2020 suggests that early representatives of Mosasauroidea diversified after competitions with Corresponding author plesiosaurs. -
A Revision of the Classification of the Plesiosauria with a Synopsis of the Stratigraphical and Geographical Distribution Of
LUNDS UNIVERSITETS ARSSKRIFT. N. F. Avd. 2. Bd 59. Nr l. KUNGL. FYSIOGRAFISKA SÅLLSKAPETS HANDLINGAR, N. F. Bd 74. Nr 1. A REVISION OF THE CLASSIFICATION OF THE PLESIOSAURIA WITH A SYNOPSIS OF THE STRATIGRAPHICAL AND GEOGRAPHICAL DISTRIBUTION OF THE GROUP BY PER OVE PERSSON LUND C. W. K. GLEER UP Read before the Royal Physiographic Society, February 13, 1963. LUND HÅKAN OHLSSONS BOKTRYCKERI l 9 6 3 l. Introduction The sub-order Plesiosauria is one of the best known of the Mesozoic Reptile groups, but, as emphasized by KuHN (1961, p. 75) and other authors, its classification is still not satisfactory, and needs a thorough revision. The present paper is an attempt at such a revision, and includes also a tabular synopsis of the stratigraphical and geo graphical distribution of the group. Some of the species are discussed in the text (pp. 17-22). The synopsis is completed with seven maps (figs. 2-8, pp. 10-16), a selective synonym list (pp. 41-42), and a list of rejected species (pp. 42-43). Some forms which have been erroneously referred to the Plesiosauria are also briefly mentioned ("Non-Plesiosaurians", p. 43). - The numerals in braekets after the generic and specific names in the text refer to the tabular synopsis, in which the different forms are numbered in successional order. The author has exaroined all material available from Sweden, Australia and Spitzbergen (PERSSON 1954, 1959, 1960, 1962, 1962a); the major part of the material from the British Isles, France, Belgium and Luxembourg; some of the German spec imens; certain specimens from New Zealand, now in the British Museum (see LYDEK KER 1889, pp. -
Source-Rock Geochemistry of the San Joaquin Basin Province, California
Petroleum Systems and Geologic Assessment of Oil and Gas in the San Joaquin Basin Province, California Chapter 11 Source-Rock Geochemistry of the San Joaquin Basin Province, California By Kenneth E. Peters, Leslie B. Magoon, Zenon C. Valin, and Paul G. Lillis HIO for all source-rock units except the Tumey formation of Contents Atwill (1935). Abstract-----------------------------------------------------------------------------------1 Thick, organic-rich, oil-prone shales of the upper Mio- Introduction------------------------------------------------------------------------------ 1 cene Monterey Formation occur in the Tejon depocenter in Methods----------------------------------------------------------------------------------2 the southern part of the basin with somewhat less favorable Discussion--------------------------------------------------------------------------------3 occurrence in the Southern Buttonwillow depocenter to the Upper Miocene Antelope shale---------------------------------------------------3 north. Shales of the upper Miocene Monterey Formation Eocene Tumey formation-----------------------------------------------------------4 Eocene Kreyenhagen Formation--------------------------------------------------4 generated most of the petroleum in the San Joaquin Basin. Cretaceous-Paleocene Moreno Formation--------------------------------------5 Thick, organic-rich, oil-prone Kreyenhagen Formation source Conclusions----------------------------------------------------------------------------- -5 rock occurs in the Buttonwillow -
Sediment Provenance and Dispersal of Neogene–Quaternary Strata of the Southeastern San Joaquin Basin and Its Transition Into the GEOSPHERE; V
Research Paper THEMED ISSUE: Origin and Evolution of the Sierra Nevada and Walker Lane GEOSPHERE Sediment provenance and dispersal of Neogene–Quaternary strata of the southeastern San Joaquin Basin and its transition into the GEOSPHERE; v. 12, no. 6 southern Sierra Nevada, California doi:10.1130/GES01359.1 Jason Saleeby1, Zorka Saleeby1, Jason Robbins2, and Jan Gillespie3 13 figures; 2 tables; 2 supplemental files 1Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California 91125, USA 2Chevron North America Exploration and Production, McKittrick, California 93251, USA 3Department of Geological Sciences, California State University, Bakersfield, California 93311, USA CORRESPONDENCE: jason@ gps .caltech .edu CITATION: Saleeby, J., Saleeby, Z., Robbins, J., and ABSTRACT INTRODUCTION Gillespie, J., 2016, Sediment provenance and dis- persal of Neogene–Quaternary strata of the south- eastern San Joaquin Basin and its transition into We have studied detrital-zircon U-Pb age spectra and conglomerate clast The Sierra Nevada and Great Valley of California are structurally coupled the southern Sierra Nevada, California: Geosphere, populations from Neogene–Quaternary siliciclastic and volcaniclastic strata and move semi-independently within the San Andreas–Walker Lane dextral v. 12, no. 6, p. 1744–1773, doi:10.1130/GES01359.1. of the southeastern San Joaquin Basin, as well as a fault-controlled Neo- transform system as a microplate (Argus and Gordon, 1991; Unruh et al., 2003). gene basin that formed across the southernmost Sierra Nevada; we call this Regional relief generation and erosion of the Sierra Nevada are linked to sub- Received 9 May 2016 Accepted 31 August 2016 basin the Walker graben. -
USGS Professional Paper 1740
Age, Stratigraphy, and Correlations of the Late Neogene Purisima Formation, Central California Coast Ranges By Charles L. Powell II1, John A. Barron1, Andrei M. Sarna-Wojcicki1, Joseph C. Clark2, Frank A. Perry3, Earl E. Brabb4, and Robert J. Fleck1 Abstract Counties inland to the San Andreas Fault (fig. 1). These scat- tered outcrops have been grouped as the Purisima Formation The Purisima Formation is an important upper Miocene because they are all fine- to coarse-grained clastic rocks, with and Pliocene stratigraphic unit in central California, cropping dark andesitic fragments and locally abundant silicic tephra, out from the coast at Point Reyes north of San Francisco to and occupy the same stratigraphic position at their various more extensive exposures in the Santa Cruz Mountains to the exposures. Since first described by Haehl and Arnold (1904), south. The fine-grained rocks in the lower parts of the Puri- the Purisima Formation has been considered to be of Pliocene sima Formation record a latest Miocene transgressive event, or of late Miocene to Pliocene age. Differing age assignments whereas the middle and upper parts of the formation consist have resulted from the wide stratigraphic range of many com- of increasingly clastic-rich siltstones and sandstones resulting monly encountered megafossils and from the lack of agree- from uplift of adjacent coastal regions and the Sierra Nevada ment on the placement of the Miocene-Pliocene Series bound- during Pliocene transgressive and regressive sea-level events. ary between the provincial megafaunal chronology and that Exposures of the Purisima occur in three different, fault- of international usage. -
Qt53v080hx.Pdf
UC Berkeley PaleoBios Title A new Early Pliocene record of the toothless walrus Valenictus (Carnivora, Odobenidae) from the Purisima Formation of Northern California Permalink https://escholarship.org/uc/item/53v080hx Journal PaleoBios, 34(0) ISSN 0031-0298 Author Boessenecker, Robert W. Publication Date 2017-06-15 DOI 10.5070/P9341035289 Peer reviewed eScholarship.org Powered by the California Digital Library University of California PaleoBios 34:1-6, June 15, 2017 PaleoBios OFFICIAL PUBLICATION OF THE UNIVERSITY OF CALIFORNIA MUSEUM OF PALEONTOLOGY Boessenecker, Robert W. (2017). A New Early Pliocene Record of the Toothless Walrus Valenictus (Carnivora, Odobenidae) from the Purisima Formation of Northern California. Cover photo: Life restoration of the extinct Pliocene walrus Valenictus and flightless auks (Mancalla) hauled out on the rocky shore of the uplifted Coast Ranges of California (top right); cliff exposures of the Purisima Formation near Santa Cruz, from where Valenictus was collected by Wayne Thompson (left); bivalves, chiefly Clinocardium meekianum, exposed in the Purisima Formation near the locality (bottom). Photo credit and original artwork: Robert W. Boessenecker. Citation: Boessenecker, Robert W. 2017. A New Early Pliocene Record of the Toothless Walrus Valenictus (Carnivora, Odobenidae) from the Puri- sima Formation of Northern California. PaleoBios, 34. ucmp_paleobios_35289 A New Early Pliocene Record of the Toothless Walrus Valenictus (Carnivora, Odobenidae) from the Purisima Formation of Northern California ROBERT W. BOESSENECKER1,2 1Department of Geology and Environmental Geosciences, College of Charleston, Charleston, SC 29424; [email protected] 2University of California Museum of Paleontology, University of California, Berkeley, CA 94720 The walrus (Odobenus rosmarus) is a large tusked molluskivore that inhabits the Arctic and is the sole living member of the family Odobenidae. -
Convergent Evolution in Aquatic Tetrapods: Insights from an Exceptional Fossil Mosasaur
Convergent Evolution in Aquatic Tetrapods: Insights from an Exceptional Fossil Mosasaur Johan Lindgren1*, Michael W. Caldwell2,3, Takuya Konishi2¤, Luis M. Chiappe4 1 Department of Earth and Ecosystem Sciences, Lund University, Lund, Sweden, 2 Department of Biological Sciences, University of Alberta, Edmonton, Alberta, Canada, 3 Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, Alberta, Canada, 4 The Dinosaur Institute, Natural History Museum of Los Angeles County, Los Angeles, California, United States of America Abstract Mosasaurs (family Mosasauridae) are a diverse group of secondarily aquatic lizards that radiated into marine environments during the Late Cretaceous (98–65 million years ago). For the most part, they have been considered to be simple anguilliform swimmers – i.e., their propulsive force was generated by means of lateral undulations incorporating the greater part of the body – with unremarkable, dorsoventrally narrow tails and long, lizard-like bodies. Convergence with the specialized fusiform body shape and inferred carangiform locomotory style (in which only a portion of the posterior body participates in the thrust-producing flexure) of ichthyosaurs and metriorhynchid crocodyliform reptiles, along with cetaceans, has so far only been recognized in Plotosaurus, the most highly derived member of the Mosasauridae. Here we report on an exceptionally complete specimen (LACM 128319) of the moderately derived genus Platecarpus that preserves soft tissues and anatomical details (e.g., large portions of integument, a partial body outline, putative skin color markings, a downturned tail, branching bronchial tubes, and probable visceral traces) to an extent that has never been seen previously in any mosasaur. Our study demonstrates that a streamlined body plan and crescent-shaped caudal fin were already well established in Platecarpus, a taxon that preceded Plotosaurus by 20 million years. -
Active Tectonics at Wheeler Ridge, Southern San Joaquin Valley, California
Active tectonics at Wheeler Ridge, southern San Joaquin Valley, California E. A. Keller* Environmental Studies Program and Department of Geological Sciences, University of California, Santa Barbara, California 93106 R. L. Zepeda 1342 Grove Street, Alameda, California 94501 T. K. Rockwell Department of Geological Sciences, San Diego State University, San Diego, California 91282 T. L. Ku Department of Earth Sciences, University of Southern California, Los Angeles, California 90089-0740 W. S. Dinklage Department of Geological Sciences, University of California, Santa Barbara, California 93106 ABSTRACT INTRODUCTION where geomorphic surfaces are folded over the anticlinal axis (Zepeda et al., 1986). In addition, Wheeler Ridge is an east-west–trending Buried reverse faults associated with actively the 1952 Kern County earthquake was centered anticline that is actively deforming on the up- deforming folds are known to produce large earth- below Wheeler Ridge, but not on the Wheeler per plate of the Pleito–Wheeler Ridge thrust- quakes. Several recent, large California earth- Ridge thrust fault; therefore the potential earth- fault system. Holocene and late Pleistocene de- quakes are examples: M = 6.7, Northridge, 1994; quake hazard in the area is clear. formation is demonstrated at the eastern end M = 6.1, Whittier Narrows, 1987; MS = 6.4, The primary goals of the research at Wheeler of the anticline where Salt Creek crosses the Coalinga, 1983, and MS = 7.7, Kern County, Ridge are (1) to characterize the tectonic geomor- anticlinal axis. Uplift, tilting, and faulting, as- 1952. Detailed investigations of folding associ- phology; (2) to develop the Pleistocene chronol- sociated with the eastward growth of the anti- ated with concealed reverse faults are therefore ogy; and (3) to test the hypothesis that climatic cline, are documented by geomorphic surfaces necessary in order to better understand earthquake perturbations are responsible for most Pleistocene that are higher and older to the west. -
Summary of North American Blancan Nonmarine Mollusks1
MALACOLOGIA , 1966, 4(1): 1-172 SUMMARY OF NORTH AMERICAN BLANCAN NONMARINE MOLLUSKS1 D. W. Taylor U. S. Geological Survey, and Research Associate, University of Michigan Museum of Zoology, Ann Arbor, Michigan, U. S. A. ABSTRACT All known North American nonmarine mollusks of Blancan (late Pliocene and early Pleistocene) age have been here fitted into the available framework of associated fossils, physical stratigraphy and radiogenic potassium-argon dates. Many of the independently dated molluscan assemblages are so similar to other faunas that most of the fossils summarized can be assigned confidently to the Blancan age. These assignments permitted compilation of lists of last appear- ances of genera and families that are unknown during or after Blancan times. About 50-55 Blancan assemblages are known, and together with about 10-15 older or younger faunas included for convenience of discussion they are summarized under 57 local geographic headings (map, Fig. 1). For each local assemblage the following data have been given so far as possi- ble: location, previous references to mollusks, stratigraphic unit and most recent geologic maps, number of species of mollusks, mention of other fossils from the same locality or formation, age, institution where fossils are preserved, and most recent topographic maps. The detail of treatment varies widely, according to available information, progress of knowledge since previous liter- ature and the usefulness of new information. Lists of species are included usually only if the fauna is revised or first recorded in this paper, but the references to previous work are intended to be complete. The Blancan faunas from the Great Plains region (Nebraska, Kansas, Okla- homa, Texas), and from Arizona, are generally similar and include mainly widespread living species. -
Pdf/15/4/1164/4799287/1164.Pdf 1164 by California Inst of Technology User on 06 August 2019 Research Paper
Research Paper GEOSPHERE Late Cenozoic structure and tectonics of the southern Sierra Nevada–San Joaquin Basin transition, California GEOSPHERE, v. 15, no. 4 Jason Saleeby and Zorka Saleeby Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California 91125, USA https://doi.org/10.1130/GES02052.1 ■ ABSTRACT the San Joaquin Basin is widely known for its Neogene deep-marine condi- 17 figures; 3 tables; 1 set of supplemental files tions that produced prolific hydrocarbon reserves (Hoots et al., 1954). Rarely This paper presents a new synthesis for the late Cenozoic tectonic, paleogeo- in the literature are the late Cenozoic geologic features of these two adjacent CORRESPONDENCE: [email protected] graphic, and geomorphologic evolution of the southern Sierra Nevada and adja- regions discussed in any depth together. The late Cenozoic features of these cent eastern San Joaquin Basin. The southern Sierra Nevada and San Joaquin Ba- two regions speak to a number of significant issues in tectonics and geomor- CITATION: Saleeby, J., and Saleeby, Z., 2019, Late Cenozoic structure and tectonics of the southern Si- sin contrast sharply, with the former constituting high-relief basement exposures phology. These include: (1) the Earth’s surface responses to geologically rapid erra Nevada–San Joaquin Basin transition, Califor- and the latter constituting a Neogene marine basin with superposed low-relief changes in the distribution of mantle lithosphere loads; (2) the stability of nia: Geosphere, v. 15, no. 4, p. 1164–1205, https:// uplifts actively forming along its margins. Nevertheless, we show that Neogene cover strata–basement transition zones and the time scales over which pro- doi .org /10.1130 /GES02052.1. -
Revision of the Genus Styxosaurus and Relationships of the Late Cretaceous Elasmosaurids (Sauropterygia: Plesiosauria) of the Western Interior Seaway
Marshall University Marshall Digital Scholar Theses, Dissertations and Capstones 2020 Revision of the Genus Styxosaurus and Relationships of the Late Cretaceous Elasmosaurids (Sauropterygia: Plesiosauria) of the Western Interior Seaway Elliott Armour Smith Follow this and additional works at: https://mds.marshall.edu/etd Part of the Biology Commons, Paleobiology Commons, and the Paleontology Commons REVISION OF THE GENUS STYXOSAURUS AND RELATIONSHIPS OF THE LATE CRETACEOUS ELASMOSAURIDS (SAUROPTERYGIA: PLESIOSAURIA) OF THE WESTERN INTERIOR SEAWAY A thesis submitted to the Graduate College of Marshall University In partial fulfillment of the requirements for the degree of Master of Science In Biological Sciences by Elliott Armour Smith Approved by Dr. F. Robin O’Keefe, Committee Chairperson Dr. Habiba Chirchir, Committee Member Dr. Herman Mays, Committee Member Marshall University May 2020 ii © 2020 Elliott Armour Smith ALL RIGHTS RESERVED iii DEDICATION Dedicated to my loving parents for supporting me on my journey as a scientist. iv ACKNOWLEDGEMENTS I would like to thank Dr. Robin O’Keefe for serving as my advisor, and for his constant mentorship and invaluable contributions to this manuscript. I would like to thank Dr. Herman Mays and Dr. Habiba Chirchir for serving on my committee and providing immensely valuable feedback on this manuscript and the ideas within. Thanks to the Marshall University Department of Biological Sciences for travel support. I would like to thank curators Ross Secord (University of Nebraska), Chris Beard (University of Kansas), Tylor Lyson (Denver Museum of Nature and Science), and Darrin Paginac (South Dakota School of Mines and Technology) for granting access to fossil specimens. Thanks to Joel Nielsen (University of Nebraska State Museum), Megan Sims (University of Kansas), Kristen MacKenzie (Denver Museum of Nature and Science) for facilitating access to fossil specimens.