Understanding Earth's Deep Past: Lessons for Our Climate Future
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Cyclicity, Dune Migration, and Wind Velocity in Lower Permian Eolian Strata, Manitou Springs, CO
Cyclicity, Dune Migration, and Wind Velocity in Lower Permian Eolian Strata, Manitou Springs, CO by James Daniel Pike, B.S. A Thesis In Geology Submitted to the Graduate Faculty of Texas Tech University in Partial Fulfillment of the Requirements for the Degree of MASTER OF SCIENCES Approved Dustin E. Sweet Chair of Committee Tom M. Lehman Jeffery A. Lee Mark Sheridan Dean of the Graduate School August, 2017 Copyright 2017, James D. Pike Texas Tech University, James Daniel Pike, August 2017 ACKNOWLEDGMENTS I would like to extend my greatest thanks to my advisor Dr. Dustin Sweet, who was an excellent advisor during this research. Dr. Sweet was vital throughout the whole process, be it answering questions, giving feedback on figures, and imparting his extensive knowledge of the ancestral Rocky Mountains on me; for this I am extremely grateful. Dr. Sweet allowed me to conduct my own research without looking over my shoulder, but was always available when needed. When I needed a push, Dr. Sweet provided it. I would like to thank my committee memebers, Dr. Lee and Dr. Lehman for providing feedback and for their unique perspectives. I would like to thank Jenna Hessert, Trent Jackson, and Khaled Chowdhury for acting as my field assistants. Their help in taking measurements, collecting samples, recording GPS coordinates, and providing unique perspectives was invaluable. Thank you to Melanie Barnes for allowing me to use her lab, and putting up with the mess I made. This research was made possible by a grant provided by the Colorado Scientific Society, and a scholarship provided by East Texas Geological Society. -
Geologic Map and Upper Paleozoic Stratigraphy of the Marble Canyon Area, Cottonwood Canyon Quadrangle, Death Valley National Park, Inyo County, California
Geologic Map and Upper Paleozoic Stratigraphy of the Marble Canyon Area, Cottonwood Canyon Quadrangle, Death Valley National Park, Inyo County, California By Paul Stone, Calvin H. Stevens, Paul Belasky, Isabel P. Montañez, Lauren G. Martin, Bruce R. Wardlaw, Charles A. Sandberg, Elmira Wan, Holly A. Olson, and Susan S. Priest Pamphlet to accompany Scientific Investigations Map 3298 2014 U.S. Department of the Interior U.S. Geological Survey Cover View of Marble Canyon area, California, showing dark rocks of Mississippian Indian Springs Formation and Pennsylvanian Bird Spring Formation overlying light rocks of Mississippian Santa Rosa Hills Limestone in middle distance. View is southeast toward Emigrant Wash and Tucki Mountain in distance. U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2014 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit http://www.usgs.gov or call 1–888–ASK–USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Suggested citation: Stone, P., Stevens, C.H., Belasky, P., Montanez, I.P., Martin, L.G., Wardlaw, B.R., Sandberg, C.A., Wan, E., Olson, H.A., and Priest, S.S., 2014, Geologic map and upper Paleozoic stratigraphy of the Marble Canyon area, Cottonwood Canyon quadrangle, Death Valley National Park, Inyo County, California: U.S. Geological Survey Scientific Investigations Map 3298, scale 1:24,000, 59 p., http://dx.doi.org/10.3133/sim3298. -
North America Free Download
NORTH AMERICA FREE DOWNLOAD Libby Koponen | 48 pages | 01 Mar 2009 | Children's Press(CT) | 9780531218303 | English | New York, NY, United States North America Plymouth remains the de jure capital. With soldiers in tow, his goal was to find gold for the Spanish Crown. United States of America Bureau of the Census. Nearly North America million immigrants have a four-year college degree or better. Retrieved 3 October This North America a list of North American countries and dependent territories by population. New Spain, a territory that stretched from the southwestern modern-day U. He explained the rationale for the name in the accompanying book Cosmographiae Introductio : [6]. This section needs expansion. Oceans portal Book Category. About ten years later another trading company, the West India Company, settled groups of colonists on Manhattan Island and at Fort Orange. North America has been historically referred to by other names. The first attempt by Europeans to colonize the New World occurred around A. Weishampel, David B. Demographics by North America. Other French-speaking locales include the Province of Ontario the official language is English, but there are an estimated North America, Franco-Ontariansthe Province of Manitoba co-official as de jure with Englishthe French West Indies and Saint-Pierre et Miquelonas well as North America US state of Louisiana, where French is also an official language. Canada shows significant growth in the sectors of services, mining and manufacturing. Inexplicably, Vineland was abandoned after only a few years. Between and Frobisher as well as John Davis explored along the Atlantic coast. Central Intelligence Agence. -
Carbon and Strontium Isotope Stratigraphy of the Permian from Nevada and China: Implications from an Icehouse to Greenhouse Transition
Carbon and strontium isotope stratigraphy of the Permian from Nevada and China: Implications from an icehouse to greenhouse transition Dissertation Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University By Kate E. Tierney, M.S. Graduate Program in the School of Earth Sciences The Ohio State University 2010 Dissertation Committee: Matthew R. Saltzman, Advisor William I. Ausich Loren Babcock Stig M. Bergström Ola Ahlqvist Copyright by Kate Elizabeth Tierney 2010 Abstract The Permian is one of the most important intervals of earth history to help us understand the way our climate system works. It is an analog to modern climate because during this interval climate transitioned from an icehouse state (when glaciers existed extending to middle latitudes), to a greenhouse state (when there were no glaciers). This climatic amelioration occurred under conditions very similar to those that exist in modern times, including atmospheric CO2 levels and the presence of plants thriving in the terrestrial system. This analog to the modern system allows us to investigate the mechanisms that cause global warming. Scientist have learned that the distribution of carbon between the oceans, atmosphere and lithosphere plays a large role in determining climate and changes in this distribution can be studied by chemical proxies preserved in the rock record. There are two main ways to change the distribution of carbon between these reservoirs. Organic carbon can be buried or silicate minerals in the terrestrial realm can be weathered. These two mechanisms account for the long term changes in carbon concentrations in the atmosphere, particularly important to climate. -
Curriculum Vitae
Carl Simpson 1 CU Museum of Natural History Phone (USA): +1 303-735-5323 University of Colorado, 265 UCB [email protected] Boulder, CO, 8039-0265 http://simpson-carl.github.io @simpson carl Position Assistant Professor, Department of Geological Sciences, University of Colorado, Boulder. Curator of Invertebrate Paleontology, CU Museum, University of Colorado, Boulder. Education Ph.D. Department of Geophysical Sciences, 2006 University of Chicago, Chicago, IL, USA B.A. College of Creative Studies (Biology), June 2000 University of California, Santa Barbara, CA, USA Professional Experience 2015 - 2016 Springer Fellow, Department of Paleobiology, National Museum of Natural History, Smithsonian Institution 2012-2015 Abbott Fellow, Department of Paleobiology, National Museum of Natural His- tory, Smithsonian Institution. 2012 Visiting Scholar, Cooperation and Evolution of Multicellularity program. Kavli In- stitute for Theoretical Physics. 2011 Visiting Scholar Fellowship, National Evolutionary Synthesis Center. 2008-2012 Postdoctoral Researcher, Museum f¨ur Naturkunde, Leibniz Institute for Evo- lution and Biodiversity at the Humbolt University, Berlin. 2006-2008 Research Associate, Department of Biology, Duke University. 2004 Research assistant for John Alroy, the Paleobiology Database, National Center for Ecological Analysis and Synthesis. 2001 Santa Fe Institute Complex Systems Summer School; Budapest, Hungary. 2001 Comparative Invertebrate Embryology. Friday Harbor Marine Laboratories. Fellowships & Grants • Springer Fellowship, \Quantifying the stochastic and deterministic aspects of macroevo- lution" Smithsonian Institution, National Museum of Natural History 2015-2016. • NSF ELT Collaborative Research: \Investigating the Biotic and Paleoclimatic Con- sequences of Dust in the Late Paleozoic." 2013-2017. with Gerilyn Soreghan, Linda Hinnov, Sarah Aciego, and Nicholas Heavens. • Abbott Postdoctoral Fellowship, \The Macroevolution of Bryozoan Polymorphism" Smithsonian Institution, National Museum of Natural History. -
Atmospheric Dust Stimulated Marine Primary Productivity During Earth's
https://doi.org/10.1130/G46977.1 Manuscript received 14 April 2019 Revised manuscript received 8 November 2019 Manuscript accepted 12 November 2019 © 2019 Geological Society of America. For permission to copy, contact [email protected]. Published online 17 December 2019 Atmospheric dust stimulated marine primary productivity during Earth’s penultimate icehouse Mehrdad Sardar Abadi1, Jeremy D. Owens2, Xiaolei Liu1, Theodore R. Them II2,3, Xingqian Cui4, Nicholas G. Heavens5,6 and Gerilyn S. Soreghan1 1 School of Geosciences, University of Oklahoma, Norman, Oklahoma 73019, USA 2 Department of Earth, Ocean, and Atmospheric Science, Florida State University, and National High Magnetic Field Laboratory, Tallahassee, Florida 32306, USA 3 Department of Geology and Environmental Geosciences, College of Charleston, Charleston, South Carolina 29424, USA 4 Department of Earth Atmospheric and Planetary Sciences, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, USA 5 Department of Atmospheric and Planetary Sciences, Hampton University, 21 E. Tyler Street, Hampton, Virginia 23668, USA 6 Space Science Institute, 4750 Walnut Street, Suite 205, Boulder, Colorado 80301, USA ABSTRACT BACKGROUND AND METHODS The importance of dust as a source of iron (Fe) for primary production in modern oceans Pennsylvanian–Permian carbonate strata is well studied but remains poorly explored for deep time. Vast dust deposits are well recog- of the study area were located at ∼30°S at the nized from the late Paleozoic and provisionally implicated in primary production through Fe time of deposition, adjacent to the northeastern fertilization. Here, we document dust impacts on marine primary productivity in Moscovian Arabian margin of Gondwana, in relative prox- (Pennsylvanian, ca. -
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Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Pangea B and the Late Paleozoic Ice Age ⁎ D.V. Kenta,b, ,G.Muttonic a Earth and Planetary Sciences, Rutgers University, Piscataway, NJ 08854, USA b Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964, USA c Dipartimento di Scienze della Terra 'Ardito Desio', Università degli Studi di Milano, via Mangiagalli 34, I-20133 Milan, Italy ARTICLE INFO ABSTRACT Editor: Thomas Algeo The Late Paleozoic Ice Age (LPIA) was the penultimate major glaciation of the Phanerozoic. Published compi- Keywords: lations indicate it occurred in two main phases, one centered in the Late Carboniferous (~315 Ma) and the other Late Paleozoic Ice Age in the Early Permian (~295 Ma), before waning over the rest of the Early Permian and into the Middle Permian Pangea A (~290 Ma to 275 Ma), and culminating with the final demise of Alpine-style ice sheets in eastern Australia in the Pangea B Late Permian (~260 to 255 Ma). Recent global climate modeling has drawn attention to silicate weathering CO2 Greater Variscan orogen consumption of an initially high Greater Variscan edifice residing within a static Pangea A configuration as the Equatorial humid belt leading cause of reduction of atmospheric CO2 concentrations below glaciation thresholds. Here we show that Silicate weathering CO2 consumption the best available and least-biased paleomagnetic reference poles place the collision between Laurasia and Organic carbon burial Gondwana that produced the Greater Variscan orogen in a more dynamic position within a Pangea B config- uration that had about 30% more continental area in the prime equatorial humid belt for weathering and which drifted northward into the tropical arid belt as it transformed to Pangea A by the Late Permian. -
2016-2017 Research & Scholarship Report
2016-2017 RESEARCH & SCHOLARSHIP REPORT StFX l 2016-2017 Research and Scholarship Report 3 About the University 1 Message From The Academic Vice-President & Provost and the Associate Vice-President, Research & Graduate Studies 2 Researcher Profiles 3 FACULTY OF ARTS Anthropology 9 Economics 11 English 13 History 14 Modern Languages (French, German, Spanish) 15 Philosophy 15 Political Science 19 Psychology 22 Religious Studies 27 Sociology 27 FACULTY OF BUSINESS Accounting and Finance 28 Management 29 Marketing and Enterprise Systems 29 FACULTY OF EDUCATION Adult Education 30 Education 32 TABLE OF CONTENTS FACULTY OF SCIENCE Biology 35 Chemistry 39 Earth Sciences 41 Human Kinetics 51 Human Nutrition 55 Mathematics, Statistics and Computer Science 56 Nursing 57 Physics 61 OTHER ACADEMIC PROGRAMS Climate & Environment Program 63 Development Studies 63 Public Policy & Governance Program 64 Women’s and Gender Studies 66 Coady International Institute 67 Extension Department 68 National Collaborating Centre for Determinants of Health 69 ACADEMIC ADMINISTRATIVE UNITS Vice-President’s Office 69 Research Services Group 70 StFX RESEARCH STATISTICS 72 ACKNOWLEDGEMENTS 75 StFX l 2016-2017 Research and Scholarship Report 5 ABOUT THE UNIVERSITY Founded in 1853, St. Francis Xavier University (StFX) in Antigonish, Nova Scotia, began as a small school of higher studies established by the Catholic Church. Today, StFX is widely recognized as one of Canada’s leading undergraduate universities with a longstanding tradition of academic excellence, innovation in teaching, research and service to society. It brings together over 4,500 students for studies in arts, sciences, business, education and applied professional programs. The University is known for its strong traditions of social engagement and service to humanity, as well as for the numerous communities with which it engages. -
Demystifying Climate Change Session 6
Demystifying Climate Change Session 6 CO2 and Other Greenhouse Gases: Where do they come from? Where do they go? How are they regulated? Burp… OLLI at Illinois Spring 2021 D. H. Tracy [email protected] 418.53 ppm Mar 6, 2021 3/9/21 Climate Change 6 2 Course Outline 1. Building Blocks: Some important concepts 2. Our Goldilocks Earth: a Radiative Balancing Act 3. The Role of the Atmosphere: Greenhouse Gases & Clouds 4. Global Circulation and Dynamics of the Earth System: Oceans, Atmosphere, Biosphere, Cryosphere, People, Lithosphere 5. Natural Variability of the Climate, short and long term. Ice Ages 6. Carbon Dioxide and other Greenhouse Gases: Where do they come from, where do they go, how are they regulated? 7. Impacts and Future Projections for Global Warming -- Uncertainties 8. Amelioration Strategies. The Climate Debate. Policy Options. 3/9/21 Climate Change 6 3 Remember CO2 Saturation? 400ppm CO2 T260K P0.5 L6.4m 100%100% Lesson: Blue: 800 ppm 80% Greenhouse Gases 4 ppm are much more Red: potent, per ppm, 400 ppm 60% when at low 1 ppm concentrations: 40% Not saturated. Absorption of Full Atmosphere Full of Absorption 20% Absorption of Full Atmosphere ofFull Absorption 0% 8.5 9 10 11 12 13 14 15 16 17 18 19 20 Wavelength (mm) Wavelength (m) 3/9/21 Climate Change 6 4 Actual Surface Temperature vs. GH Gas Concentration Doublings Behavior Expected for Linear Increase Minor/Trace Gases ∆T2X TSURF 2x Log Increase Saturation TSKIN setting in 254 K (-2F) Doublings T 0 1 1 1 1 1 /128 x /64 x /32 x /16 x /8 x ¼ x ½x 1x 2x 4x 8x 3/9/21 -
Fjord Network in Namibia: a Snapshot Into the Dynamics of the Late Paleozoic Glaciation Pierre Dietrich1,2, Neil P
https://doi.org/10.1130/G49067.1 Manuscript received 20 October 2020 Revised manuscript received 19 March 2021 Manuscript accepted 21 June 2021 © 2021 The Authors. Gold Open Access: This paper is published under the terms of the CC-BY license. Fjord network in Namibia: A snapshot into the dynamics of the late Paleozoic glaciation Pierre Dietrich1,2, Neil P. Griffis3,4, Daniel P. Le Heron5, Isabel P. Montañez3, Christoph Kettler5, Cécile Robin1 and François Guillocheau1 1 Géosciences Rennes, Université de Rennes, CNRS, UMR 6118, 35000 Rennes, France 2 Department of Geology, University of Johannesburg, Johannesburg 2006, South Africa 3 Department of Earth and Planetary Sciences, University of California, Davis, California 95616, USA 4 Berkeley Geochronology Center, Berkeley, California 94709, USA 5 Department für Geologie, Universität Wien, Althanstraße 14, 1190 Wien, Austria ABSTRACT infer the pace of ice-margin fluctuations and Fjords are glacially carved estuaries that profoundly influence ice-sheet stability by the paleo-ice thickness that once occupied draining and ablating ice. Although abundant on modern high-latitude continental shelves, these fjords. Furthermore, we estimate glacio- fjord-network morphologies have never been identified in Earth’s pre-Cenozoic glacial epochs, isostatic adjustment following deglaciation. hindering our ability to constrain ancient ice-sheet dynamics. We show that U-shaped valleys This work highlights the dynamic nature of in northwestern Namibia cut during the late Paleozoic ice age (LPIA, ca. 300 Ma), Earth’s the LPIA in southwestern Gondwana and the penultimate icehouse, represent intact fjord-network morphologies. This preserved glacial potential for an under-appreciated deep-time morphology and its sedimentary fill permit a reconstruction of paleo-ice thicknesses, glacial carbon and sediment sink that, if valid, would dynamics, and resulting glacio-isostatic adjustment. -
Illawarra Reversal: the fingerprint of a Superplume That Triggered Pangean Breakup and the End-Guadalupian (Permian) Mass Extinction
Gondwana Research 15 (2009) 421–432 Contents lists available at ScienceDirect Gondwana Research journal homepage: www.elsevier.com/locate/gr Illawarra Reversal: The fingerprint of a superplume that triggered Pangean breakup and the end-Guadalupian (Permian) mass extinction Yukio Isozaki Department of Earth Science and Astronomy, The University of Tokyo, Komaba, Meguro, Tokyo 153-8902, Japan article info abstract Article history: The Permian magnetostratigraphic record demonstrates that a remarkable change in geomagnetism occurred in Received 22 July 2008 the Late Guadalupian (Middle Permian; ca. 265 Ma) from the long-term stable Kiaman Reverse Superchron Received in revised form 10 December 2008 (throughout the Late Carboniferous and Early-Middle Permian) to the Permian–Triassic Mixed Superchron with Accepted 11 December 2008 frequent polarity changes (in the Late Permian and Triassic). This unique episode called the Illawarra Reversal Available online 24 December 2008 probably reflects a significant change in the geodynamo in the outer core of the planet after a 50 million years of Keywords: stable geomagnetism. The Illawarra Reversal was likely led by the appearance of a thermal instability at the – Illawarra Reversal 2900 km-deep core mantle boundary in connection with mantle superplume activity. The Illawarra Reversal Permian and the Guadalupian–Lopingian boundary event record the significant transition processes from the Paleozoic Superplume to Mesozoic–Modern world. One of the major global environmental changes in the Phanerozoic occurred Geodynamo almost simultaneously in the latest Guadalupian, as recorded in 1) mass extinction, 2) ocean redox change, 3) Mass extinction sharp isotopic excursions (C and Sr), 4) sea-level drop, and 5) plume-related volcanism. -
Read Book Continent Ebook Free Download
CONTINENT PDF, EPUB, EBOOK Jim Crace | 176 pages | 04 Jan 2008 | Pan MacMillan | 9780330453318 | English | London, United Kingdom Continent - Wikipedia Geologists theorize that continents move. This theory is called plate tectonics , which holds that the lithosphere , the outermost layer of Earth where continents are , lies on top of a semifluid layer of partially molten magma called the asthenosphere. Convection from the decay of radioactive elements in the mantle causes continental and oceanic plates to move. Pangea is a landmass of the Early Permian to Early Jurassic Periods that incorporated almost all modern landmasses and is thus considered a supercontinent. There is great variation in the sizes of continents; Asia is more than five times as large as Australia. The largest island in the world, Greenland , is only about one-fourth the size of Australia. The continents differ sharply in their degree of compactness. Africa has the most regular coastline and, consequently, the lowest ratio of coastline to total area. Europe is the most irregular and indented and has by far the highest ratio of coastline to total area. The continents are not distributed evenly over the surface of the globe. The distribution of the continental platforms and ocean basins on the surface of the globe and the distribution of the major landform features have long been among the most intriguing problems for scientific investigation and theorizing. Each continent has one of the so-called shield areas that formed 2 billion to 4 billion years ago and is the core of the continent to which the remainder most of the continent has been added.