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Cryogenian Glaciation and the Onset of Carbon-Isotope Decoupling” by N
CORRECTED 21 MAY 2010; SEE LAST PAGE REPORTS 13. J. Helbert, A. Maturilli, N. Mueller, in Venus Eds. (U.S. Geological Society Open-File Report 2005- M. F. Coffin, Eds. (Monograph 100, American Geophysical Geochemistry: Progress, Prospects, and New Missions 1271, Abstracts of the Annual Meeting of Planetary Union, Washington, DC, 1997), pp. 1–28. (Lunar and Planetary Institute, Houston, TX, 2009), abstr. Geologic Mappers, Washington, DC, 2005), pp. 20–21. 44. M. A. Bullock, D. H. Grinspoon, Icarus 150, 19 (2001). 2010. 25. E. R. Stofan, S. E. Smrekar, J. Helbert, P. Martin, 45. R. G. Strom, G. G. Schaber, D. D. Dawson, J. Geophys. 14. J. Helbert, A. Maturilli, Earth Planet. Sci. Lett. 285, 347 N. Mueller, Lunar Planet. Sci. XXXIX, abstr. 1033 Res. 99, 10,899 (1994). (2009). (2009). 46. K. M. Roberts, J. E. Guest, J. W. Head, M. G. Lancaster, 15. Coronae are circular volcano-tectonic features that are 26. B. D. Campbell et al., J. Geophys. Res. 97, 16,249 J. Geophys. Res. 97, 15,991 (1992). unique to Venus and have an average diameter of (1992). 47. C. R. K. Kilburn, in Encyclopedia of Volcanoes, ~250 km (5). They are defined by their circular and often 27. R. J. Phillips, N. R. Izenberg, Geophys. Res. Lett. 22, 1617 H. Sigurdsson, Ed. (Academic Press, San Diego, CA, radial fractures and always produce some form of volcanism. (1995). 2000), pp. 291–306. 16. G. E. McGill, S. J. Steenstrup, C. Barton, P. G. Ford, 28. C. M. Pieters et al., Science 234, 1379 (1986). 48. -
Tectonic Imbrication and Foredeep Development in the Penokean
Tectonic Imbrication and Foredeep Development in the Penokean Orogen, East-Central Minnesota An Interpretation Based on Regional Geophysics and the Results of Test-Drilling The Penokean Orogeny in Minnesota and Upper Michigan A Comparison of Structural Geology U.S. GEOLOGICAL SURVEY BULLETIN 1904-C, D 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 cur rent-year issues of the monthly catalog "New Publications of the U.S. Geological Survey." Prices of available U.S. Geological Sur vey publications released prior to the current year are listed in the most recent annual "Price and Availability List." Publications that are listed in various U.S. Geological Survey catalogs (see back inside cover) but not listed in the most recent annual "Price and Availability List" are no longer available. Prices of reports released to the open files are given in the listing "U.S. Geological Survey Open-File Reports," updated month ly, which is for sale in microfiche from the U.S. Geological Survey, Books and Open-File Reports Section, Federal Center, Box 25425, Denver, CO 80225. Reports released through the NTIS may be obtained by writing to the National Technical Information Service, U.S. Department of Commerce, Springfield, VA 22161; please include NTIS report number with inquiry. Order U.S. Geological Survey publications by mail or over the counter from the offices given below. BY MAIL OVER THE COUNTER Books Books Professional Papers, Bulletins, Water-Supply Papers, Techniques of Water-Resources Investigations, Circulars, publications of general in Books of the U.S. -
The Geology of the Middle Precambrian Rove Formation in Northeastern Minnesota
MINNESOTA GEOLOGICAL SURVEY 5 P -7 Special Publication Series The Geology of the Middle Precambrian Rove Formation in northeastern Minnesota G. B. Morey UNIVERSITY OF MINNESOTA MINNEAPOLIS • 1969 I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I I THE GEOLOGY OF THE MIDDLE PRECAMBRIAN ROVE FORMATION IN NORTHEASTERN MINNESOTA by G. B. Morey CONTENTS Page Abstract ........................................... 1 Introduction. 3 Location and scope of study. 3 Acknowledgements .. 3 Regional geology . 5 Structural geology . 8 Rock nomenclature . 8 Stratigraphy . .. 11 Introduction . .. 11 Nomenclature and correlation. .. 11 Type section . .. 11 Thickness . .. .. 14 Lower argillite unit. .. 16 Definition, distribution, and thickness. .. 16 Lithologic character . .. 16 Limestones. .. 17 Concretions. .. 17 Transition unit . .. 17 Definition, distribution, and thickness. .. 17 Lithologic character . .. 19 Thin-bedded graywacke unit . .. 19 Definition, distribution, and thickness. .. 19 Lithologic character. .. 20 Concretions ... .. 20 Sedimentary structures. .. 22 Internal bedding structures. .. 22 Structureless bedding . .. 23 Laminated bedding . .. 23 Graded bedding. .. 23 Cross-bedding . .. 25 Convolute bedding. .. 26 Internal bedding sequences . .. 26 Post-deposition soft sediment deformation structures. .. 27 Bed pull-aparts . .. 27 Clastic dikes . .. 27 Load pockets .. .. 28 Flame structures . .. 28 Overfolds . .. 28 Microfaults. .. 28 Ripple marks .................................. 28 Sole marks . .. 28 Groove casts . .. 30 Flute casts . -
Cretaceous Paleoceanography
GEOLOGIC A CARPATH1CA, 46, 5, BRATISLAVA, OCTOBER 1995 257 - 266 CRETACEOUS PALEOCEANOGRAPHY A v Z XI06ER WILLIAM W. HAY BORE* CRETACEOUS GEOMAR, Wischhofstr. 1-3, D-24148 Kiel, Germany Department of Geological Sciences and Cooperative Institute for Research in Environmental Sciences, Campus Box 250, University of Colorado, Boulder, CO 80309, USA (Manuscript received January 17, 1995; accepted in revised form June 14, 1995) Abstract: The modem ocean is comprised of four units: an equatorial belt shared by the two hemispheres, tropical-subtropi cal anticyclonic gyres, mid-latitude belts of water with steep meridional temperature gradients, and polar oceans characterized by cyclonic gyres. These units are separated by lines of convergence, or fronts: subequatorial, subtropical, and polar. Con vergence and divergence of the ocean waters are forced beneath zonal (latitude-parallel) winds. The Early Cretaceous ocean closely resembled the modem ocean. The developing Atlantic was analogous to the modem Mediterranean and served as an Intermediate Water source for the Pacific. Because sea-ice formed seasonally in the Early Cretaceous polar seas, deep water formation probably took place largely in the polar region. In the Late Cretaceous, the high latitudes were warm and deep waters moved from the equatorial region toward the poles, enhancing the ocean’s capacity to transport heat poleward. The contrast between surface gyre waters and intermediate waters was less, making them easier to upwell, but be cause their residence time in the oxygen minimum was less and they contained less nutrients. By analogy to the modem ocean, ’’Tethyan” refers to the oceans between the subtropical convergences and ’’Boreal” refers to the ocean poleward of the subtropical convergences. -
SVP's Letter to Editors of Journals and Publishers on Burmese Amber And
Society of Vertebrate Paleontology 7918 Jones Branch Drive, Suite 300 McLean, VA 22102 USA Phone: (301) 634-7024 Email: [email protected] Web: www.vertpaleo.org FEIN: 06-0906643 April 21, 2020 Subject: Fossils from conflict zones and reproducibility of fossil-based scientific data Dear Editors, We are writing you today to promote the awareness of a couple of troubling matters in our scientific discipline, paleontology, because we value your professional academic publication as an important ‘gatekeeper’ to set high ethical standards in our scientific field. We represent the Society of Vertebrate Paleontology (SVP: http://vertpaleo.org/), a non-profit international scientific organization with over 2,000 researchers, educators, students, and enthusiasts, to advance the science of vertebrate palaeontology and to support and encourage the discovery, preservation, and protection of vertebrate fossils, fossil sites, and their geological and paleontological contexts. The first troubling matter concerns situations surrounding fossils in and from conflict zones. One particularly alarming example is with the so-called ‘Burmese amber’ that contains exquisitely well-preserved fossils trapped in 100-million-year-old (Cretaceous) tree sap from Myanmar. They include insects and plants, as well as various vertebrates such as lizards, snakes, birds, and dinosaurs, which have provided a wealth of biological information about the ‘dinosaur-era’ terrestrial ecosystem. Yet, the scientific value of these specimens comes at a cost (https://www.nytimes.com/2020/03/11/science/amber-myanmar-paleontologists.html). Where Burmese amber is mined in hazardous conditions, smuggled out of the country, and sold as gemstones, the most disheartening issue is that the recent surge of exciting scientific discoveries, particularly involving vertebrate fossils, has in part fueled the commercial trading of amber. -
The U-Series Toolbox for Paleoceanography
The U-series toolbox for paleoceanography Gideon M. Henderson Department of Earth Sciences, Oxford University, South Parks Road, Oxford, OX1 3PR, ENGLAND. e-mail: [email protected] Robert F. Anderson Lamont-Doherty Earth Observatory of Columbia University, Route 9W, Palisades, NY 10964, USA. e-mail: [email protected] Reviews in Mineralogy and Geochemistry "Uranium Series Geochemistry" Revised Version 1 1. Introduction The geochemistry of marine sediments is a major source of information about the past environment. Of the many measurements that provide such information, those of the U-series nuclides are unusual in that they inform us about the rate and timescales of processes. Oceanic processes such as sedimentation, productivity, and circulation, typically occur on timescales too short to be assessed using parent-daughter isotope systems such as Rb-Sr or Sm-Nd. So the only radioactive clocks that we can turn to are those provided by cosmogenic nuclides (principally 14C) or the U-series nuclides. This makes the U-series nuclides powerful allies in the quest to understand the past ocean-climate system and has led to their widespread application over the last decade. As in other applications of the U-series, those in paleoceanography rely on fractionation of the nuclides away from secular equilibrium. In the oceanic setting, this fractionation is generally due to differences in the solubility of the various nuclides. The general behavior of the U-series nuclides in the oceans was widely researched in the middle decades of the twentieth century. This work established knowledge of the concentrations of the nuclides in the various compartments of the ocean system, and of their fluxes between these compartments. -
Cyanobacterial Evolution During the Precambrian
International Journal of Astrobiology 15 (3): 187–204 (2016) doi:10.1017/S1473550415000579 © Cambridge University Press 2016 This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. Cyanobacterial evolution during the Precambrian Bettina E. Schirrmeister1, Patricia Sanchez-Baracaldo2 and David Wacey1,3 1School of Earth Sciences, University of Bristol, Wills Memorial Building, Queen’s Road, Bristol BS8 1RJ, UK e-mail: [email protected] 2School of Geographical Sciences, University of Bristol, University Road, Bristol BS8 1SS, UK 3Centre for Microscopy, Characterisation and Analysis, and ARC Centre of Excellence for Core to Crust Fluid Systems, The University of Western Australia, 35 Stirling Highway, Crawley, WA 6009, Australia Abstract: Life on Earth has existed for at least 3.5 billion years. Yet, relatively little is known of its evolution during the first two billion years, due to the scarceness and generally poor preservation of fossilized biological material. Cyanobacteria, formerly known as blue green algae were among the first crown Eubacteria to evolve and for more than 2.5 billion years they have strongly influenced Earth’s biosphere. Being the only organism where oxygenic photosynthesis has originated, they have oxygenated Earth’s atmosphere and hydrosphere, triggered the evolution of plants –being ancestral to chloroplasts– and enabled the evolution of complex life based on aerobic respiration. Having such a strong impact on early life, one might expect that the evolutionary success of this group may also have triggered further biosphere changes during early Earth history. -
A Fundamental Precambrian–Phanerozoic Shift in Earth's Glacial
Tectonophysics 375 (2003) 353–385 www.elsevier.com/locate/tecto A fundamental Precambrian–Phanerozoic shift in earth’s glacial style? D.A.D. Evans* Department of Geology and Geophysics, Yale University, P.O. Box 208109, 210 Whitney Avenue, New Haven, CT 06520-8109, USA Received 24 May 2002; received in revised form 25 March 2003; accepted 5 June 2003 Abstract It has recently been found that Neoproterozoic glaciogenic sediments were deposited mainly at low paleolatitudes, in marked qualitative contrast to their Pleistocene counterparts. Several competing models vie for explanation of this unusual paleoclimatic record, most notably the high-obliquity hypothesis and varying degrees of the snowball Earth scenario. The present study quantitatively compiles the global distributions of Miocene–Pleistocene glaciogenic deposits and paleomagnetically derived paleolatitudes for Late Devonian–Permian, Ordovician–Silurian, Neoproterozoic, and Paleoproterozoic glaciogenic rocks. Whereas high depositional latitudes dominate all Phanerozoic ice ages, exclusively low paleolatitudes characterize both of the major Precambrian glacial epochs. Transition between these modes occurred within a 100-My interval, precisely coeval with the Neoproterozoic–Cambrian ‘‘explosion’’ of metazoan diversity. Glaciation is much more common since 750 Ma than in the preceding sedimentary record, an observation that cannot be ascribed merely to preservation. These patterns suggest an overall cooling of Earth’s longterm climate, superimposed by developing regulatory feedbacks -
The Penokean Orogeny in the Lake Superior Region Klaus J
Precambrian Research 157 (2007) 4–25 The Penokean orogeny in the Lake Superior region Klaus J. Schulz ∗, William F. Cannon U.S. Geological Survey, 954 National Center, Reston, VA 20192, USA Received 16 March 2006; received in revised form 1 September 2006; accepted 5 February 2007 Abstract The Penokean orogeny began at about 1880 Ma when an oceanic arc, now the Pembine–Wausau terrane, collided with the southern margin of the Archean Superior craton marking the end of a period of south-directed subduction. The docking of the buoyant craton to the arc resulted in a subduction jump to the south and development of back-arc extension both in the initial arc and adjacent craton margin to the north. A belt of volcanogenic massive sulfide deposits formed in the extending back-arc rift within the arc. Synchronous extension and subsidence of the Superior craton resulted in a broad shallow sea characterized by volcanic grabens (Menominee Group in northern Michigan). The classic Lake Superior banded iron-formations, including those in the Marquette, Gogebic, Mesabi and Gunflint Iron Ranges, formed in that sea. The newly established subduction zone caused continued arc volcanism until about 1850 Ma when a fragment of Archean crust, now the basement of the Marshfield terrane, arrived at the subduction zone. The convergence of Archean blocks of the Superior and Marshfield cratons resulted in the major contractional phase of the Penokean orogeny. Rocks of the Pembine–Wausau arc were thrust northward onto the Superior craton causing subsidence of a foreland basin in which sedimentation began at about 1850 Ma in the south (Baraga Group rocks) and 1835 Ma in the north (Rove and Virginia Formations). -
Isotopic and Chemical Characterization of Water from Mine Pits and Wells on the Mesabi Iron Range, Northeastern Minnesota, As a Tool for Drinking Water Protection
Isotopic and Chemical Characterization of Water From Mine Pits and Wells on the Mesabi Iron Range, Northeastern Minnesota, as a Tool for Drinking Water Protection James F. Walsh, Minnesota Department of Health Abstract The Biwabik Iron Formation is both a world-class source of iron ore and an important aquifer for the residents of the Mesabi Iron Range in northeastern Minnesota. Numerous public water supply wells draw from this aquifer, and several communities pump directly from abandoned mine pits for their water supply. It is important that the groundwater flow characteristics of this aquifer be determined so that drinking water supplies can be protected in a technically defensible manner. The iron formation is early Proterozoic in age and consists primarily of fine-grained silica and iron minerals that were deposited as chemical sediments in a marine environment. The unit has little primary porosity. Groundwater flow through the aquifer is controlled predominantly by secondary features such as folds, high- angle faults, joints, and man-made mining structures. Efforts at delineating source water protection areas on the Mesabi Range have been complicated by the extremely heterogeneous and anisotropic nature of porosity in the Biwabik Iron Formation aquifer. In the absence of reliable groundwater flow models for this type of setting, isotopic and chemical studies have been emphasized, in addition to hydrogeologic mapping. Conservative environmental tracers such as chloride and the stable isotopes of oxygen and hydrogen have proved useful for 1) identifying wells that are receiving recharge from mine pits, 2) characterizing the tracer signature of those mine pits that may represent recharge areas for nearby public supply wells, and 3) quantifying the significance of these recharge areas for the purpose of targeting source water protection efforts. -
UNIVERSITY of CALIFORNIA RIVERSIDE Investigation of The
UNIVERSITY OF CALIFORNIA RIVERSIDE Investigation of the Composition and Preservation Potential of Precambrian Sedimentary Organic Matter and Lipid Biosignatures A Dissertation submitted in partial satisfaction of the requirements for the degree of Doctor of Philosophy in Geological Sciences by Kelden Pehr June 2020 Dissertation Committee: Dr. Gordon D. Love, Chairperson Dr. Andrey Bekker Dr. Marilyn Fogel Copyright by Kelden Pehr 2020 The Dissertation of Kelden Pehr is approved: Committee Chairperson University of California, Riverside ACKNOWLEDGMENTS This research was made possible through funding and support from the NASA Earth and Space Science Fellowship (17-PLANET17R-0019), the Earle C Anthony Award and the UCR Dissertation Year Fellowship. I am very grateful to my advisor Gordon Love, whose support and guidance has been invaluable over these past years. I would like to thank my qualifying exams and defense committee members as follows: Andrey Bekker for the many opportunities and great conversations; Marilyn Fogel for the encouragement and excellent discussions on all things biogeochemical; Mary Dorser for welcoming me as an honorary member of the Droser lab; and Francesca Hopkins for asking the big questions. Rose Bisquera, Carina Lee, Alex Zumberge, JP Duda, Adam Hoffman, Nathan Marshall, and Adriana Rizzo were all wonderful lab mentors and mates. Steven Bates and Laurie Graham provided much needed support in the dark hours of instrument failure. Aaron Martinez deserves a special shout out for the awesome adventures, fantastic food, and long hours of laughter. I have had the pleasure to work with an amazing cast of collaborators, without whom, this research presented here would not have been possible. -
Cenozoic Paleoceanography 1986: an Introduction
University of New Hampshire University of New Hampshire Scholars' Repository Affiliate Scholarship Center for Coastal and Ocean Mapping 12-1987 Cenozoic paleoceanography 1986: An introduction W. H. Berger University of California - Davis Larry A. Mayer University of New Hampshire, [email protected] Follow this and additional works at: https://scholars.unh.edu/ccom_affil Part of the Oceanography and Atmospheric Sciences and Meteorology Commons, and the Paleontology Commons Recommended Citation Berger, W.H., and Mayer, L.A., 1987, Cenozoic paleoceanography 1986: An introduction, in Berger, W.H. and Mayer, L.A., eds. Paleoceanography, vol. 2, no. 6, pp. 613-623 This Article is brought to you for free and open access by the Center for Coastal and Ocean Mapping at University of New Hampshire Scholars' Repository. It has been accepted for inclusion in Affiliate Scholarship by an authorized administrator of University of New Hampshire Scholars' Repository. For more information, please contact [email protected]. PALEOCEANOGRAPHY,VOL. 2, NO. 6, PAGES 613-623, DECEMBER 1987 CENOZOIC PALEOCEANOGRAPHY 1986: AN INTRODUCTION W. H. Berger Scripps Institution of Oceanography University of California, San Diego La Jolla L. A. Mayer Department of Oceanography Dalhousie University Halifax, Nova Scotia, Canada Absgracg. New developments in Cenozoic Toronto, 1980: Berger and Crowell [1982]; paleoceanography include the application Zfirich, 1983: Hs•i and Weissert [1985]), we of climate models and atmospheric general note several new developments.