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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. -
UC Riverside UC Riverside Electronic Theses and Dissertations
UC Riverside UC Riverside Electronic Theses and Dissertations Title Exploring the Texture of Ocean-Atmosphere Redox Evolution on the Early Earth Permalink https://escholarship.org/uc/item/9v96g1j5 Author Reinhard, Christopher Thomas Publication Date 2012 Peer reviewed|Thesis/dissertation eScholarship.org Powered by the California Digital Library University of California UNIVERSITY OF CALIFORNIA RIVERSIDE Exploring the Texture of Ocean-Atmosphere Redox Evolution on the Early Earth A Dissertation submitted in partial satisfaction of the requirements for the degree of Doctor of Philosophy in Geological Sciences by Christopher Thomas Reinhard September 2012 Dissertation Committee: Dr. Timothy W. Lyons, Chairperson Dr. Gordon D. Love Dr. Nigel C. Hughes ! Copyright by Christopher Thomas Reinhard 2012 ! ! The Dissertation of Christopher Thomas Reinhard is approved: ________________________________________________ ________________________________________________ ________________________________________________ Committee Chairperson University of California, Riverside ! ! ACKNOWLEDGEMENTS It goes without saying (but I’ll say it anyway…) that things like this are never done in a vacuum. Not that I’ve invented cold fusion here, but it was quite a bit of work nonetheless and to say that my zest for the enterprise waned at times would be to put it euphemistically. As it happens, though, I’ve been fortunate enough to be surrounded these last years by an incredible group of people. To those that I consider scientific and professional mentors that have kept me interested, grounded, and challenged – most notably Tim Lyons, Rob Raiswell, Gordon Love, and Nigel Hughes – thank you for all that you do. I also owe Nigel and Mary Droser a particular debt of graditude for letting me flounder a bit my first year at UCR, being understanding and supportive, and encouraging me to start down the road to where I’ve ended up (for better or worse). -
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. -
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 -
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. -
Subglacial Meltwater Supported Aerobic Marine Habitats During Snowball Earth
Subglacial meltwater supported aerobic marine habitats during Snowball Earth Maxwell A. Lechtea,b,1, Malcolm W. Wallacea, Ashleigh van Smeerdijk Hooda, Weiqiang Lic, Ganqing Jiangd, Galen P. Halversonb, Dan Asaele, Stephanie L. McColla, and Noah J. Planavskye aSchool of Earth Sciences, University of Melbourne, Parkville, VIC 3010, Australia; bDepartment of Earth and Planetary Science, McGill University, Montréal, QC, Canada H3A 0E8; cState Key Laboratory for Mineral Deposits Research, School of Earth Sciences and Engineering, Nanjing University, 210093 Nanjing, China; dDepartment of Geoscience, University of Nevada, Las Vegas, NV 89154; and eDepartment of Geology and Geophysics, Yale University, New Haven, CT 06511 Edited by Paul F. Hoffman, University of Victoria, Victoria, BC, Canada, and approved November 3, 2019 (received for review May 28, 2019) The Earth’s most severe ice ages interrupted a crucial interval in Cryogenian ice age. These marine chemical sediments are unique eukaryotic evolution with widespread ice coverage during the geochemical archives of synglacial ocean chemistry. To develop Cryogenian Period (720 to 635 Ma). Aerobic eukaryotes must have sur- a global picture of seawater redox state during extreme glaci- vived the “Snowball Earth” glaciations, requiring the persistence of ation, we studied 9 IF-bearing Sturtian glacial successions across 3 oxygenated marine habitats, yet evidence for these environments paleocontinents (Fig. 1): Congo (Chuos Formation, Namibia), is lacking. We examine iron formations within globally distributed Australia (Yudnamutana Subgroup), and Laurentia (Kingston Cryogenian glacial successions to reconstruct the redox state of the Peak Formation, United States). These IFs were selected for synglacial oceans. Iron isotope ratios and cerium anomalies from a analysis because they are well-preserved, and their depositional range of glaciomarine environments reveal pervasive anoxia in the environment can be reliably constrained. -
Aerobic Iron and Manganese Cycling in a Redox-Stratified Mesoarchean Epicontinental Sea
This is a repository copy of Aerobic iron and manganese cycling in a redox-stratified Mesoarchean epicontinental sea. White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/134011/ Version: Accepted Version Article: Ossa Ossa, F, Hofmann, A, Wille, M et al. (5 more authors) (2018) Aerobic iron and manganese cycling in a redox-stratified Mesoarchean epicontinental sea. Earth and Planetary Science Letters, 500. pp. 28-40. ISSN 0012-821X https://doi.org/10.1016/j.epsl.2018.07.044 © 2018 Elsevier B.V. This manuscript version is made available under the CC-BY-NC-ND 4.0 license http://creativecommons.org/licenses/by-nc-nd/4.0/. Reuse This article is distributed under the terms of the Creative Commons Attribution-NonCommercial-NoDerivs (CC BY-NC-ND) licence. This licence only allows you to download this work and share it with others as long as you credit the authors, but you can’t change the article in any way or use it commercially. More information and the full terms of the licence here: https://creativecommons.org/licenses/ Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ *Manuscript Click here to view linked References Aerobic iron and manganese cycling in a redox-stratified Mesoarchean epicontinental sea Frantz Ossa Ossaa,b*, Axel Hofmanna, Martin Willeb,c, Jorge E. Spangenbergd, Andrey Bekkere,a, Simon W. -
041-2011-Abstracts-BOE-III-Crete.Pdf
Boreskov Institute of Catalysis of the Siberian Branch of Russian Academy of Sciences, Novosibirsk, Russia Institute of Cytology and Genetics of the Siberian Branch of Russian Academy of Sciences, Novosibirsk, Russia Borissiak Paleontological Institute of Russian Academy of Sciences, Moscow, Russia III International Conference “Biosphere Origin and Evolution” RETHYMNO, CRETE, GREECE OCTOBER 16-20, 2011 ABSTRACTS Novosibirsk, 2011 © Boreskov Institute of Catalysis, 2011 INTERNATIONAL SCIENTIFIC COMMITTEE Alexei Rozanov, Borissiak Paleontological Institute RAS, Moscow, Russia Co‐Chairman Georgii Zavarzin, Institute of Microbiology RAS, Moscow, Russia Co‐Chairman Vadim Agol Moscow State University, Russia Yury Chernov Severtsov Institute of Ecology and Evolution, Moscow, Russia Institute of Protein Research RAS, Pushchino, Moscow region, Alexander Chetverin Russia David Deamer Biomolecular Engineering, School of Engineering, Santa Cruz, USA V.S. Sobolev Institute of Geology and Mineralogy SB RAS, Nikolay Dobretsov Novosibirsk, Russia Mikhail Fedonkin Geological Institute RAS, Moscow, Russia Siegfried Franck Potsdam Institute for Climate Impact Research, Germany V.I. Vernadskii Institute of Geochemistry and Analytical Chemistry Eric Galimov RAS, Moscow, Russia Mikhail Grachev Limnological Institute SB RAS, Irkutsk, Russia Richard Hoover Nasa Marshall Space Flight Ctr., Huntsville, USA North‐Western Scientific Center RAS, St. Petersburg State Sergey Inge‐Vechtomov University, Russia Trofimuk Institute of Petroleum‐Gas Geology and Geophysics Alexander Kanygin SB RAS, Novosibirsk, Russia Astrospace Centre of Lebedev Physical Institute RAS, Moscow, Nikolay Kardashev Russia Józef Kaźmierczak Institute of Paleobiology PAN, Warsaw, Poland Nikolay Kolchanov Institute of Cytology and Genetics SB RAS, Novosibirsk, Russia Trofimuk Institute of Petroleum‐Gas Geology and Geophysics Alexei Kontorovich SB RAS, Novosibirsk, Russia National Center for Biotechnology Information, National Library Eugene V. -
Biology Curricula at Universities
Biology curricula at universities European Communities Biologists Association ECBA publication No 1 Biology curricula at universities Report of a Workshop organized by the European Communities Biologists Association Index 1. INTRODUCTION ......................................................................................................................................... 4 2. OBJECTIVES OF THE WORKSHOP......................................................................................................... 5 3. GENERAL CONSIDERATIONS ................................................................................................................. 6 4. THE BASIC TRAINING BIOLOGISTS PRIOR TO SPECIALIZATION .................................................. 8 4.1. INTRODUCTION...................................................................................................................................... 8 4.2. TOPICS TO BE INCLUDED IN THE CENTRAL CORE-PROGRAM................................................................... 8 4.3. SKILLS AND ATTITUDES....................................................................................................................... 10 5. THE PHASE OF SPECIALIZATION (INTO PROFESSION)................................................................... 12 5.1. INTRODUCTION.................................................................................................................................... 12 5.2. FURTHER TRAINING IN RESEARCH ......................................................................................................