Introduction to Geomicrobiology
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Student Handbook
A Handbook for Geology Students 1 Contents Why study Geology? ............................................................................................. 3 Job Prospects and Salaries .................................................................................. 7 Why Appalachian Geology? ................................................................................ 10 Geology Faculty and Staff ................................................................................... 13 Financial Support in the Department ................................................................... 23 Geology Department Awards and Honors .......................................................... 26 Opportunities and Requirements ........................................................................ 28 Degree Programs in Geology ............................................................................. 35 Geology Courses ................................................................................................ 44 Field Camp ......................................................................................................... 51 2 Why study Geology? Geology is the multi-disciplinary science that studies the earth and its history. We live on a dynamic planet that is constantly changing. Our ability to survive as a civilization and as a species is intricately linked to the geologic processes that shape our earth, form its natural resources and allow it to recover from the abuse that our society heaps upon it. Geology is important because -
The Morphology and Histology of a Certain Structure Connected with the Pars Intermedia of the Pituitary Body Ofthe Ox1
THE MORPHOLOGY AND HISTOLOGY OF A CERTAIN STRUCTURE CONNECTED WITH THE PARS INTERMEDIA OF THE PITUITARY BODY OFTHE OX1 ROSALIND \VULZEX From the Hearst Anatomical Laboratory oj the University oj California SEVENTEEN FIGURES Certain physiological experiments are now being conducted in the Rudolph Spreckels Physiological Laboratory of this University which necessitate the separation of a great number of ox pituitaries into their two main divisions. As an interesting anatomical feature was in this way brought to our attention the material was used in addition for this anatomical study. This feature has not been mentioned by the following who have written more or less fully upon the pituitary body of the ox, Peremeschko ('67), Dostojewski ('86), Herring ('08)' and Traut- mann ('11). The pituitary body of the ox, like that of other vertebrates, is composed of two distinct portions. One, the pars nervosa, is derived from the brain as an outgrowth of the hypothalamus. The other originates as a hollow buccal evagination which in time is completely separated from the digestive tract. That portion of this evagination which comes into contact with the pars nervosa is called the pars intermedia. It is a comparatively thin sheet of epithelium which spreads as a coating over much Material amounting to thousands of pituitary bodies was most kindly sup- plied by the Oakland Meat and Packing Company through the courtesy of the Superintendent. It was derived from cows, bulls and steers. As the cone struc- ture was present indifferently in these three varieties, its appearance can have little to do with sex or castration. -
Geological Sciences 1
Geological Sciences 1 GEOLOGICAL SCIENCES Certificates • Geophysics - Graduate Certificate (catalog.colorado.edu/graduate/ With one of the most successful graduate programs in the nation, colleges-schools/arts-sciences/programs-study/geological-sciences/ the Department of Geological Sciences has enjoyed a reputation of geophysics-graduate-certificate/) excellence for more than 100 years. Our doctoral program is ranked • Hydrologic Sciences - Graduate Certificate (catalog.colorado.edu/ among the top 10 percent of U.S. geology programs by the National graduate/colleges-schools/arts-sciences/programs-study/geological- Research Council, and CU Boulder is ranked as one of the top two sciences/hydrologic-sciences-graduate-certificate/) universities in the world for geosciences by U.S. News and World Report. Graduate students have an opportunity to work with over 35 tenured Faculty and tenure-track faculty who support a wide range of interdisciplinary While many faculty teach both undergraduate and graduate students, research programs in such areas as: cosmochemistry and planetary some instruct students at the undergraduate level only. For more geology; Earth science education; economic and energy resources; information, contact the faculty member's home department. geobiology and astrobiology; geochemistry; geochronology and Abbott, Lon D. (https://experts.colorado.edu/display/fisid_145044/) thermochronology; geodynamics, geophysics, and remote sensing; Senior Instructor; PhD, University of California, Santa Cruz geomorphology and cryosphere; global change; hydrology; natural hazards; paleoclimate and paleoceanography; paleontology and Anderson, Robert S. (https://experts.colorado.edu/display/fisid_130117/) paleobiology; petrology and mineralogy; sedimentology and stratigraphy; Distinguished Professor; PhD, University of Washington and structure and tectonics. Arthurs, Leilani A. (https://experts.colorado.edu/display/fisid_145087/) The graduate degrees offered include Master of Science (MS) and Doctor Assistant Professor; PhD, University of Notre Dame of Philosophy (PhD). -
Geomicrobiological Processes in Extreme Environments: a Review
202 Articles by Hailiang Dong1, 2 and Bingsong Yu1,3 Geomicrobiological processes in extreme environments: A review 1 Geomicrobiology Laboratory, China University of Geosciences, Beijing, 100083, China. 2 Department of Geology, Miami University, Oxford, OH, 45056, USA. Email: [email protected] 3 School of Earth Sciences, China University of Geosciences, Beijing, 100083, China. The last decade has seen an extraordinary growth of and Mancinelli, 2001). These unique conditions have selected Geomicrobiology. Microorganisms have been studied in unique microorganisms and novel metabolic functions. Readers are directed to recent review papers (Kieft and Phelps, 1997; Pedersen, numerous extreme environments on Earth, ranging from 1997; Krumholz, 2000; Pedersen, 2000; Rothschild and crystalline rocks from the deep subsurface, ancient Mancinelli, 2001; Amend and Teske, 2005; Fredrickson and Balk- sedimentary rocks and hypersaline lakes, to dry deserts will, 2006). A recent study suggests the importance of pressure in the origination of life and biomolecules (Sharma et al., 2002). In and deep-ocean hydrothermal vent systems. In light of this short review and in light of some most recent developments, this recent progress, we review several currently active we focus on two specific aspects: novel metabolic functions and research frontiers: deep continental subsurface micro- energy sources. biology, microbial ecology in saline lakes, microbial Some metabolic functions of continental subsurface formation of dolomite, geomicrobiology in dry deserts, microorganisms fossil DNA and its use in recovery of paleoenviron- Because of the unique geochemical, hydrological, and geological mental conditions, and geomicrobiology of oceans. conditions of the deep subsurface, microorganisms from these envi- Throughout this article we emphasize geomicrobiological ronments are different from surface organisms in their metabolic processes in these extreme environments. -
MICR 423: Geomicrobiology Fall 2018 3 Credit Hours
MICR 423: Geomicrobiology Fall 2018 3 Credit Hours Course description. This course will focus on the role that microorganisms play in fundamental geological processes. Topics will include an outline of the present understanding of microbial involvement of weathering of rocks, formation and transformation of soils and sediments, genesis and degradation of minerals. Elemental cycles will also be covered with emphasis on the interrelationships between the various geochemical cycles and the microbial trophic groups involved. Prerequisite: MICR 301 and Chemistry 210 and 21l. Recommended: GEOL 220, 221 or 222. Lecture. Life Science II, Room 430, 9:35 – 10:50 Tues and Thurs Course Goals. At the end of this course you will be able to: • Intelligently converse with microbiologists, geologists, environmental scientists and engineers about the role microorganisms play in the cycling of elements • Be familiar with a variety of techniques to identify and characterize microorganisms in any environment • Relate microbial physiology, genetics, cell structure, and metabolism to the effect, role, or signature that microbes imprint on their surroundings Instructor Office Office Hours Dr. Scott Hamilton-Brehm Life Science III, Rm 1009 M 10-12 pm or by 453-3818 appointment [email protected] Strongly suggested textbooks: • BROCK BIOLOGY OF MICROORGANISMS, 15th edition, 2017, Michael T. Madigan, Kelly S. Bender, Daniel H. Buckley, Matthew W. Sattley, and David A. Stahl (Benjamin Cummings/Pearson). • Hall BG. Phylogenetic trees made easy: a how-to manual. 2008. Final Course Grading scale Grade Points Percentage A 900 - 1000 90-100% B 800 - 899 80-89% C 700 - 799 70-79% D 600 - 699 60-69% F 0 - 599 0-59% Lecture Grades. -
What Doomed the Stromatolites? SCIENTISTS FIND KEY CLUE to Ancient ENIGMA by Cherie Winner
Microbes What Doomed the Stromatolites? SCIENTISTS FIND KEY CLUE TO ANCIENT ENIGMA by Cherie Winner Virginia Edgcomb/WHOI Rocky formations like these, called stromatolites, dominated coastal areas billions of years ago. Now they exist in only a few locations. bout a billion years before the dinosaurs became extinct, Forams are abundant in present-day ocean sediments, where stromatolites roamed the Earth until they mysteriously they use fingerlike extensions called pseudopods to engulf prey disappeared. Well, not roamed exactly. and to explore their surroundings. In the process, their pseudo- Stromatolites (“layered rocks”) are rocky structures pods churn the sediments on a microscopic scale. made by photosynthetic cyanobacteria. The microbes Living stromatolites can still be found today, in limited and secrete sticky compounds that bind together sediment widely scattered locales, as if a few velociraptors still roamed in grains,A creating a mineral “microfabric” that accumulates in fine remote valleys. Bernhard, Edgcomb, and colleagues looked for layers. Massive formations of stromatolites showed up along foraminifera in living stromatolite and thrombolite formations shorelines all over the world about 3.5 billion years ago. They from Highborne Cay in the Bahamas. Using microscope and were the earliest visible manifestation of life on Earth and domi- RNA sequencing techniques, they found forams in both—and nated the scene for more than two billion years. thrombolites were especially rich in the kinds of forams that “They were one of the earliest examples of the intimate were probably the first foraminifera to evolve on Earth. connection between biology—living things—and geology— “The timing of their appearance corresponds with the the structure of the Earth itself,” said Joan decline of layered stromatolites and the Bernhard, a geobiologist at Woods Hole appearance of thrombolites in the fossil re- Oceanographic Institution (WHOI). -
2011 Fall Paper Session Program And
Rochester Academy of Science Fall 2011 Scientific Papers Day Saturday, October 29, 2011 Hosted by: Monroe County Community College and the Departments of Biology, Chemistry and Geosciences, and Engineering Science and Physics Table of Contents Page Schedule of the Day 3 Session Schedules Session I: Agriculture, Anthropology & New Approaches 5 Session II: Phylogeny, Ecology & Paleontology 6 Session III: Ecology 7 Session IV: Meteorology, Physics & Astronomy 8 Session V: Chemistry I 9 Session VI: Chemistry II 10 List of Posters 11 All Abstracts 21 Acknowledgements 91 2 Rochester Academy of Science Fall 2011 Scientific Papers Day Saturday, October 29, 2011 Hosted by: Monroe County Community College and the Departments of Biology, Chemistry and Geosciences, and Engineering Science and Physics 8:00 am Registration Gilman Lounge, Flynn Campus Center 8:00 – 9:00 am Coffee & Refreshments Gilman Lounge, Flynn Campus Center 9:00 – 11:00 am Oral Presentations Session I: Agriculture, Anthropology & New Approaches 12-209 Session II: Phylogeny, Ecology & Paleontology 12-203 Session III: Ecology 12-207 Session IV: Meteorology, Physics & Astronomy 12-215 Session V: Chemistry I 12-211 Session VI: Chemistry II 12-213 11:00 am – 12:00 pm Poster Session Forum (3-130) 12:00 pm Luncheon Monroe A and B, Flynn Campus Center 1:00 pm Key Note Speaker Monroe A and B, Flynn Campus Center Disappearing Ice! Mass Loss and Dynamics of the Greenland Ice Sheet Dr. Beata Csatho Department of Geology, University of Buffalo 3 4 Oral Presentations Session I: Agriculture, -
Need for Seismic Hydrology Research with a Geomicrobiological Focus
sustainability Communication Need for Seismic Hydrology Research with a Geomicrobiological Focus Heejung Kim Department of Geology, Kangwon National University, Chuncheon 24341, Korea; [email protected] Abstract: Earthquakes cause deformation in previously stable groundwater environments, resulting in changes to the hydrogeological characteristics. The changes to hydrological processes follow- ing large-scale earthquakes have been investigated through many physicochemical studies, but understanding of the associated geomicrobiological responses remains limited. To complement the understanding of earthquakes gathered using hydrogeochemical approaches, studies on the effects of the Earth’s deep crustal fluids on microbial community structures can be applied. These studies could help establish the degree of resilience and sustainability of the underground ecosystem following an earthquake. Furthermore, investigations on changes in the microbial community structure of the Earth’s deep crustal fluids before and after an earthquake can be used to predict an earthquake. The results derived from studies that merge hydrogeochemical and geomicrobiological changes in the deep crustal fluids due to the effect of stress on rock characteristics within a fault zone can be used to correlate these factors with earthquake occurrences. In addition, an earthquake risk evaluation method may be developed based on the observable characteristics of fault-zone aquifers. Keywords: earthquake; seismic hydrology; groundwater; hydrogeochemistry; geomicrobiology Citation: Kim, H. Need for Seismic Many studies on the reaction of the Earth’s deep crustal fluids before and after earth- Hydrology Research with a quakes have been conducted worldwide, including in countries with a high frequency Geomicrobiological Focus. of earthquakes. Seismic hydrology is the study of earthquake prediction by analyzing Sustainability 2021, 13, 8704. -
Area of Study
DEPARTMENT OF EARTHDEPARTMENT SCIENCES OF THE GRADUATE SCHOOL | MONTANA STATE UNIVERSITY AreaEarth ofSciences Study DEGREES OFFERED • M.S. in Earth Sciences FirstThe Departmentgraph of Earth Sciences at Montana State University has a faculty of 13 earth • Ph.D. in Earth Sciences scientists, geologists and geographers. The Master of Science and Doctor of Philosophy in Earth • Ph.D. in Ecology and TextSciences programs have around 45 active graduate students and stress independent thesis Environmental Science research with some supporting course work. Faculty expertise and research in the department spans a large majority of the subfields of Earth Sciences. Our geography faculty includes specialties from settlement geography to bioclimatology, from international urban geography to GIS to snow science. The interests of our geology faculty range from petrogenesis to paleobiology to structural geology, and from dinosaur taphonomy and stratigraphy to geomorphology. Our geobiology faculty have research interests in vertebrate paleontology, paleoecology, biogeography, paleoclimatology and geomicrobiology. Program strengths are in basin analysis and energy resources, dinosaur paleontology, geography of the northern Rocky Mountains, architecture and composition of the lithosphere, snow science and cryospheric processes, and climate change. ADMISSION Applicants should a GPA of 3.0 or higher, GRE scores better than the 50th percentile and a strong academic background in Earth Sciences (geography, geology or geobiology). Foreign students must have a TOEFL score better than 550 for the paper test and 231 for the computer test. The department does not accept general applicants to our graduate program. An applicant should identify a major advisor from the list of faculty, contact that individual, and Department Address: determine whether there is space available in that advisor’s program. -
Geomicrobiology: Interactions Between Microbes and Minerals, Comes at a Very Opportune Time
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by Hemeroteca Cientifica Catalana INTERNATL MICROBIOL (1998) 1:241–242 241 © Springer-Verlag Ibérica 1998 BOOK REVIEWS a few chapters are devoid of typographical mistakes which Geomicrobiology: Interactions between in some case have resulted in factual errors. Nealson and Microbes and Minerals Stahl state that freshwater environments typically contain JILLIAN F. BANFIELD, KENNETH H. NEALSON (eds) 100 to 250 mM of sulfate while marine systems contain 1997. Mineralogical Society of America, Washington, DC. micromolar amounts (just the opposite is true). Bazylinski (Series: Reviews in Mineralogy, vol. 35) and Moskowitz have inadvertently created a new subgroup 448 pp. Paperback, $32. of Proteobacteria. The volume I received also included an ISBN 0-93995045-6 insert correcting a figure in chapter 11, earlier versions did not. Suffice it to say reediting would greatly enhance the The recent controversy over nanofossils in a Martian utility of this text. Despite its shortcomings, it is a good meteorite and reports of bacteria growing in basalt have once primer for the novice and an important volume for the again brought the study of geomicrobiology into the seasoned veteran. headlines. Thus, Geomicrobiology: Interactions Between Microbes and Minerals, comes at a very opportune time. The book, a byproduct of a short course of the same title hosted John F. Stolz by the Mineralogical Society of America last fall, provides Duquesne University, Pittsburgh, Pennsylvania an in depth look at a fascinating subject. Containing 13 chapters it begins with a review for non-specialists on microorganisms and biogeochemical cycles and concludes with the evolution of the carbon cycle. -
Lake Clifton
Advice to the Minister for the Environment, Heritage and the Arts from the Threatened Species Scientific Committee (the Committee) on an Amendment to the List of Threatened Ecological Communities under the Environment Protection and Biodiversity Conservation Act 1999 (EPBC Act) 1. Name of the ecological community Thrombolite (microbialite) Community of a Coastal Brackish Lake (Lake Clifton) This advice follows the assessment of information provided by a public nomination to include the “Thrombolite (microbial) Community of a Coastal Brackish Lake (Lake Clifton)” in the critically endangered category of the list of threatened ecological communities under the Environment Protection and Biodiversity Conservation Act 1999 (EPBC Act). This name is consistent with the name used for this ecological community in Western Australia, although a reference to stromatolites which appears in the Western Australian title has been omitted for the sake of clarity. 2. Public Consultation The nomination was made available for public exhibition and comment for a minimum 30 business days. In addition, detailed consultation with experts on the ecological community was undertaken. The Committee also had regard to all public and expert comment that was relevant to the consideration of the ecological community. 3. Summary of conservation assessment by the Committee The Committee provides the following assessment of the appropriateness of the ecological community’s inclusion in the EPBC Act list of threatened ecological communities. The Committee judges that the ecological community has been demonstrated to have met sufficient elements of Criterion 2 to make it eligible for listing as critically endangered. The Committee judges that the ecological community has been demonstrated to have met sufficient elements of Criterion 3 to make it eligible for listing as critically endangered. -
Light and Electron Microscopic Observations on the Anterior Pituitary of the Mouse Injected with Dl-Thyroxine By
Okajimas Fol. anat. jap., 43: 21-51, 1967 Light and Electron Microscopic Observations on the Anterior Pituitary of the Mouse injected with dl-Thyroxine By Tomiji Uchida Department of Anatomy, Nagoya University School of Medicine, Nagoya, Japan (Director : Prof. Dr. Ka z u m a r o Y a m ad a) Introduction Probably, the first suggestion of the existence of a functional relationship between the thyroid and hypophysis was given by Niepce (1851) who described pituitary enlargement in a series of goitrous cretins. Since then numerous studies have provided detailed evidence of this relationship. The reciprocal interrelationship be- tween thyroid stimulating hormone (TSH) secretion in the anterior hypophysis and the circulating levels of thyroid hormone has been well established, and in general, procedures which reduce effective plasma concentrations of thyroid hormone increase thyrotrophic hormone release in the anterior pituitary, whereas increased circulat- ing levels of thyroxine inhibit thyrotophic hormone secretion. This negative feedback mechanism resides both in the level of the pituitary and of a hypothalamic " TSH releasing center " (S o 1 o m on and Dowling, '60). Earlier views (Ma rin e, Rosen and Spar k, '35; Morris, '52) favored pituitary acidophile cell as the source of thyrotrophic hormone, but results of many recent studies implicate the basophile cell (Zeckwer, '38a and '38b; Griesbach and Purves, '45 Pur v es and Griesbac h, '46a, '46b, '51a, '51b, '51c, '57a and '57b; Goldberg and Chaikoff, '50; Salter, '50, Halmi, '50, '51, '52a , '52b, and 52c ; R ennel s, '53; Halm i and G u d e, '54 D'Angelo, '53 and '55; Knigge, '55; Elf tman, '58; Mura - s h i m a, '60 and others).