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Geology.Gsapubs.Org on 19 September 2009
Downloaded from geology.gsapubs.org on 19 September 2009 Geology History of Laurentide meltwater flow to the Gulf of Mexico during the last deglaciation, as revealed by reworked calcareous nannofossils Thomas M. Marchitto and Kuo-Yen Wei Geology 1995;23;779-782 doi: 10.1130/0091-7613(1995)023<0779:HOLMFT>2.3.CO;2 Email alerting services click www.gsapubs.org/cgi/alerts to receive free e-mail alerts when new articles cite this article Subscribe click www.gsapubs.org/subscriptions/ to subscribe to Geology Permission request click http://www.geosociety.org/pubs/copyrt.htm#gsa to contact GSA Copyright not claimed on content prepared wholly by U.S. government employees within scope of their employment. Individual scientists are hereby granted permission, without fees or further requests to GSA, to use a single figure, a single table, and/or a brief paragraph of text in subsequent works and to make unlimited copies of items in GSA's journals for noncommercial use in classrooms to further education and science. This file may not be posted to any Web site, but authors may post the abstracts only of their articles on their own or their organization's Web site providing the posting includes a reference to the article's full citation. GSA provides this and other forums for the presentation of diverse opinions and positions by scientists worldwide, regardless of their race, citizenship, gender, religion, or political viewpoint. Opinions presented in this publication do not reflect official positions of the Society. Notes Geological Society of America Downloaded from geology.gsapubs.org on 19 September 2009 History of Laurentide meltwater flow to the Gulf of Mexico during the last deglaciation, as revealed by reworked calcareous nannofossils Thomas M. -
Oxygen Isotope Geochemistry of Laurentide Ice-Sheet Meltwater Across Termination I
UC Davis UC Davis Previously Published Works Title Oxygen isotope geochemistry of Laurentide ice-sheet meltwater across Termination I Permalink https://escholarship.org/uc/item/292234zr Authors Vetter, L Spero, HJ Eggins, SM et al. Publication Date 2017-12-15 DOI 10.1016/j.quascirev.2017.10.007 Peer reviewed eScholarship.org Powered by the California Digital Library University of California Quaternary Science Reviews 178 (2017) 102e117 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Oxygen isotope geochemistry of Laurentide ice-sheet meltwater across Termination I * Lael Vetter a, , Howard J. Spero a, Stephen M. Eggins b, Carlie Williams c, Benjamin P. Flower c a Department of Earth and Planetary Sciences, University of California Davis, Davis, CA 95616, USA b Research School of Earth Sciences, The Australian National University, Canberra 0200, ACT, Australia c College of Marine Sciences, University of South Florida, St. Petersburg, FL 33701, USA article info abstract Article history: We present a new method that quantifies the oxygen isotope geochemistry of Laurentide ice-sheet (LIS) Received 3 April 2017 meltwater across the last deglaciation, and reconstruct decadal-scale variations in the d18O of LIS Received in revised form meltwater entering the Gulf of Mexico between ~18 and 11 ka. We employ a technique that combines 1 October 2017 laser ablation ICP-MS (LA-ICP-MS) and oxygen isotope analyses on individual shells of the planktic Accepted 4 October 2017 18 foraminifer Orbulina universa to quantify the instantaneous d Owater value of Mississippi River outflow, which was dominated by meltwater from the LIS. -
Ocean Storage
277 6 Ocean storage Coordinating Lead Authors Ken Caldeira (United States), Makoto Akai (Japan) Lead Authors Peter Brewer (United States), Baixin Chen (China), Peter Haugan (Norway), Toru Iwama (Japan), Paul Johnston (United Kingdom), Haroon Kheshgi (United States), Qingquan Li (China), Takashi Ohsumi (Japan), Hans Pörtner (Germany), Chris Sabine (United States), Yoshihisa Shirayama (Japan), Jolyon Thomson (United Kingdom) Contributing Authors Jim Barry (United States), Lara Hansen (United States) Review Editors Brad De Young (Canada), Fortunat Joos (Switzerland) 278 IPCC Special Report on Carbon dioxide Capture and Storage Contents EXECUTIVE SUMMARY 279 6.7 Environmental impacts, risks, and risk management 298 6.1 Introduction and background 279 6.7.1 Introduction to biological impacts and risk 298 6.1.1 Intentional storage of CO2 in the ocean 279 6.7.2 Physiological effects of CO2 301 6.1.2 Relevant background in physical and chemical 6.7.3 From physiological mechanisms to ecosystems 305 oceanography 281 6.7.4 Biological consequences for water column release scenarios 306 6.2 Approaches to release CO2 into the ocean 282 6.7.5 Biological consequences associated with CO2 6.2.1 Approaches to releasing CO2 that has been captured, lakes 307 compressed, and transported into the ocean 282 6.7.6 Contaminants in CO2 streams 307 6.2.2 CO2 storage by dissolution of carbonate minerals 290 6.7.7 Risk management 307 6.2.3 Other ocean storage approaches 291 6.7.8 Social aspects; public and stakeholder perception 307 6.3 Capacity and fractions retained -
Oxygen Isotope Geochemistry of Laurentide Ice-Sheet Meltwater Across Termination I
Quaternary Science Reviews 178 (2017) 102e117 Contents lists available at ScienceDirect Quaternary Science Reviews journal homepage: www.elsevier.com/locate/quascirev Oxygen isotope geochemistry of Laurentide ice-sheet meltwater across Termination I * Lael Vetter a, , Howard J. Spero a, Stephen M. Eggins b, Carlie Williams c, Benjamin P. Flower c a Department of Earth and Planetary Sciences, University of California Davis, Davis, CA 95616, USA b Research School of Earth Sciences, The Australian National University, Canberra 0200, ACT, Australia c College of Marine Sciences, University of South Florida, St. Petersburg, FL 33701, USA article info abstract Article history: We present a new method that quantifies the oxygen isotope geochemistry of Laurentide ice-sheet (LIS) Received 3 April 2017 meltwater across the last deglaciation, and reconstruct decadal-scale variations in the d18O of LIS Received in revised form meltwater entering the Gulf of Mexico between ~18 and 11 ka. We employ a technique that combines 1 October 2017 laser ablation ICP-MS (LA-ICP-MS) and oxygen isotope analyses on individual shells of the planktic Accepted 4 October 2017 18 foraminifer Orbulina universa to quantify the instantaneous d Owater value of Mississippi River outflow, which was dominated by meltwater from the LIS. For each individual O. universa shell, we measure Mg/ Ca (a proxy for temperature) and Ba/Ca (a proxy for salinity) with LA-ICP-MS, and then analyze the same 18 18 O. universa for d O using the remaining material from the shell. From these proxies, we obtain d Owater and salinity estimates for each individual foraminifer. Regressions through data obtained from discrete 18 18 core intervals yield d Ow vs. -
Routing of Meltwater from the Laurentide Ice Sheet During The
LETTERS TO NATURE very high sulphate concentrations (Fig. 1). Thus, differences in P release has yet to prove the mechanism behind this relation P cycling between fresh waters and salt waters may also influence ship. If sediment P release were controlled largely by sulphur, the switch in nutrient limitation. our view of the lakes that are being affected by atmospheric A further implication of our findings is a possible effect of S pollution could be altered. It is believed generally that anthropogenic S pollution on P cycling in lakes. Our data lakes with well-buffered watersheds are insensitive to the effects indicate that aquatic systems with low sulphate concentrations of atmospheric S pollution. However, because changing have low RPR under either oxic or anoxic conditions; systems atmospheric S inputs can alter the sulfate concentration in with only slightly elevated sulphate concentrations have sig surface waters22 independent of acid neutralization in the water nificantly elevated RPR, particularly under anoxic conditions shed, the P cycle of even so-called 'insensitive' lakes may be (Fig. 1). Work on the relationship between sulphate loading and affected. D Received 22 February; accepted 15 August 1987. 17. Nurnberg. G. Can. 1 Fish. aquat. Sci. 43, 574-560 (1985). 18. Curtis, P. J. Nature 337, 156-156 (1989). 1. Bostrom, B .. Jansson. M. & Forsberg, G. Arch. Hydrobiol. Beih. Ergebn. Limno/. 18, 5-59 (1982). 19. Carignan, R. & Tessier, A. Geochim. cosmochim. Acta 52, 1179-1188 (1988). 2. Mortimer. C. H. 1 Ecol. 29, 280-329 (1941). 20. Howarth, R. W. & Cole, J. J. Science 229, 653-655 (1985). -
The Generation of Mega Glacial Meltwater Floods and Their Geologic
urren : C t R gy e o s l e o r a r LaViolette, Hydrol Current Res 2017, 8:1 d c y h H Hydrology DOI: 10.4172/2157-7587.1000269 Current Research ISSN: 2157-7587 Research Article Open Access The Generation of Mega Glacial Meltwater Floods and Their Geologic Impact Paul A LaViolette* The Starburst Foundation, 1176 Hedgewood Lane, Niskayuna, New York 12309, United States Abstract A mechanism is presented explaining how mega meltwater avalanches could be generated on the surface of a continental ice sheet. It is shown that during periods of excessive climatic warmth when the continental ice sheet surface was melting at an accelerated rate, self-amplifying, translating waves of glacial meltwater emerge as a distinct mechanism of meltwater transport. It is shown that such glacier waves would have been capable of attaining kinetic energies per kilometer of wave front equivalent to 12 million tons of TNT, to have achieved heights of 100 to 300 meters, and forward velocities as great as 900 km/hr. Glacier waves would not have been restricted to a particular locale, but could have been produced wherever continental ice sheets were present. Catastrophic floods produced by waves of such size and kinetic energy would be able to account for the character of the permafrost deposits found in Alaska and Siberia, flood features and numerous drumlin field formations seen in North America, and many of the lignite deposits found in Europe, Siberia, and North America. They also could account for how continental debris was transported thousands of kilometers into the mid North Atlantic to form Heinrich layers. -
Divergence of Cryptic Species of Doryteuthis Plei Blainville
Aberystwyth University Divergence of cryptic species of Doryteuthis plei Blainville, 1823 (Loliginidae, Cephalopoda) in the Western Atlantic Ocean is associated with the formation of the Caribbean Sea Sales, João Bráullio de L.; Rodrigues-Filho, Luis F. Da S.; Ferreira, Yrlene do S.; Carneiro, Jeferson; Asp, Nils E.; Shaw, Paul; Haimovici, Manuel; Markaida, Unai; Ready, Jonathan; Schneider, Horacio; Sampaio, Iracilda Published in: Molecular Phylogenetics and Evolution DOI: 10.1016/j.ympev.2016.09.014 Publication date: 2017 Citation for published version (APA): Sales, J. B. D. L., Rodrigues-Filho, L. F. D. S., Ferreira, Y. D. S., Carneiro, J., Asp, N. E., Shaw, P., Haimovici, M., Markaida, U., Ready, J., Schneider, H., & Sampaio, I. (2017). Divergence of cryptic species of Doryteuthis plei Blainville, 1823 (Loliginidae, Cephalopoda) in the Western Atlantic Ocean is associated with the formation of the Caribbean Sea. Molecular Phylogenetics and Evolution, 106(N/A), 44-54. https://doi.org/10.1016/j.ympev.2016.09.014 General rights Copyright and moral rights for the publications made accessible in the Aberystwyth Research Portal (the Institutional Repository) are retained by the authors and/or other copyright owners and it is a condition of accessing publications that users recognise and abide by the legal requirements associated with these rights. • Users may download and print one copy of any publication from the Aberystwyth Research Portal for the purpose of private study or research. • You may not further distribute the material or use it for any profit-making activity or commercial gain • You may freely distribute the URL identifying the publication in the Aberystwyth Research Portal Take down policy If you believe that this document breaches copyright please contact us providing details, and we will remove access to the work immediately and investigate your claim. -
Gulf Facts: Also Occur Here
Note to Teachers Chemistry in the Gulf of Mexico is a teacher’s instructional guide to accompany the poster of the same title. In this guide, you will find information that relates principles from a basic chemistry class to actual processes occurring in the ocean. This guide will focus on four of these processes. The information and activities are intended for use at the 11-12 grade levels. Additional topics and resources are included at the end of the guide. The Minerals Management Service (MMS) has funded numerous scientific studies to understand better the oceanographic processes in the Gulf of Mexico. This Teacher’s Companion contains information that was gathered during these studies. The MMS is the Federal agency that regulates oil and gas activities on the U.S. Outer Continental Shelf. To learn more about the MMS, please visit our website at www.mms.gov. Author: Mary C. Boatman Graphics: Allan Linker Editors: Michael Dorner Deborah Miller Acknowledgments: We wish to thank Ranell Troxler, a sixth grade teacher in St. Charles Parish, for her review of this document. Where to get the Poster and Teacher’s Companion Copies of the poster and Teacher’s Companion may be obtained from the Public Information Office (MS 5034) at the following address: U.S. Department of the Interior Minerals Management Service Gulf of Mexico OCS Region Public Information Office (MS 5034) 1201 Elmwood Park Boulevard New Orleans, Louisiana 70123-2394 Telephone Number: (504) 736-2519 or 1-800-200-GULF 1 Table of Contents Page Number About This Lesson 3 Where It Fits into the Curriculum 3 Objectives for Students 4 Materials for Students 4 What is Chemical Oceanography? 5 Chemical Oceanography in the Gulf of Mexico 5 Temperature and Salinity Plots 6 Thermocline 6 Suspended Sediments 6 Nutrients 6 Phytoplankton 7 Detrital Rain 7 Hypoxia 7 Currents, Eddies, and Upwelling - The Eddy Graveyard 8 Naturally Occurring Oil Seeps 8 Barite Chimneys 8 Gas Hydrates and Chemosynthetic Communities 9 Naturally Occurring Brine Pools 9 Vocabulary 10 Suggested Topics for Term Papers 11 Activities 1. -
Geographic Drivers of Diversification in Loliginid Squids with an Emphasis on the Western Atlantic Species
bioRxiv preprint doi: https://doi.org/10.1101/2020.07.20.211896; this version posted July 21, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 1 Original Article Geographic drivers of diversification in loliginid squids with an emphasis on the western Atlantic species Gabrielle Genty1*, Carlos J Pardo-De la Hoz1,2*, Paola Montoya1,3, Elena A. Ritschard1,4* 1Departamento de Ciencias Biológicas, Universidad de los Andes, Bogotá D.C, Colombia. 2Department of Biology, Duke University, Durham, North Carolina, 27708, United States of America 3Instituto de Investigación de Recursos Biológicos Alexander von Humboldt, Bogotá, D.C., Colombia 4Department of Neuroscience and Developmental Biology, University of Vienna, Austria * These authors contributed equally to this work. Correspondence author: Gabrielle Genty, [email protected] Acknowledgements We would like to thank Daniel Cadena and Andrew J. Crawford for their suggestions and guidance during the early stages of this investigation. bioRxiv preprint doi: https://doi.org/10.1101/2020.07.20.211896; this version posted July 21, 2020. The copyright holder for this preprint (which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made available under aCC-BY-NC-ND 4.0 International license. 2 ABSTRACT Aim: Identifying the mechanisms driving divergence in marine organisms is challenging as opportunities for allopatric isolation are less conspicuous than in terrestrial ecosystems. -
Redalyc.Biomagnificación De Mercurio En La Cadena Trófica Del
Revista de Biología Marina y Oceanografía ISSN: 0717-3326 [email protected] Universidad de Valparaíso Chile Kehrig, Helena A.; Baptista, Gilberto; Di Beneditto, Ana Paula M.; Almeida, Marcelo G.; Rezende, Carlos E.; Siciliano, Salvatore; de Moura, Jailson F.; Moreira, Isabel Biomagnificación de mercurio en la cadena trófica del Delfín Moteado del Atlántico (Stenella frontalis), usando el isótopo estable de nitrógeno como marcador ecológico Revista de Biología Marina y Oceanografía, vol. 52, núm. 2, agosto, 2017, pp. 233-244 Universidad de Valparaíso Viña del Mar, Chile Disponible en: http://www.redalyc.org/articulo.oa?id=47952503004 Cómo citar el artículo Número completo Sistema de Información Científica Más información del artículo Red de Revistas Científicas de América Latina, el Caribe, España y Portugal Página de la revista en redalyc.org Proyecto académico sin fines de lucro, desarrollado bajo la iniciativa de acceso abierto Revista de Biología Marina y Oceanografía Vol. 52, N°2: 233-244, agosto 2017 ARTÍCULO Biomagnificación de mercurio en la cadena trófica del Delfín Moteado del Atlántico (Stenella frontalis), usando el isótopo estable de nitrógeno como marcador ecológico Mercury biomagnification in the Atlantic spotted dolphin (Stenella frontalis) food chain, using nitrogen stable isotope as an ecological tracer Helena A. Kehrig1*, Gilberto Baptista2, Ana Paula M. Di Beneditto1, Marcelo G. Almeida1, Carlos E. Rezende1, Salvatore Siciliano3, Jailson F. de Moura4 y Isabel Moreira2 1Laboratório de Ciências Ambientais, Universidade -
Geophysical and Geochemical Signatures of Gulf of Mexico Seafloor Brines
Biogeosciences, 2, 295–309, 2005 www.biogeosciences.net/bg/2/295/ Biogeosciences SRef-ID: 1726-4189/bg/2005-2-295 European Geosciences Union Geophysical and geochemical signatures of Gulf of Mexico seafloor brines S. B. Joye1, I. R. MacDonald2, J. P. Montoya3, and M. Peccini2 1Department of Marine Sciences, University of Georgia, Athens, Georgia 30602, USA 2School of Physical and Life Sciences, Texas A&M University, Corpus Christi, Texas, USA 3School of Biology, Georgia Institute of Technology, Atlanta, Georgia 30332, USA Received: 21 April 2005 – Published in Biogeosciences Discussions: 31 May 2005 Revised: 30 August 2005 – Accepted: 23 September 2005 – Published: 28 October 2005 Abstract. Geophysical, temperature, and discrete depth- 1 Introduction stratified geochemical data illustrate differences between an actively venting mud volcano and a relatively quiescent brine Submarine mud volcanoes are conspicuous examples of fo- pool in the Gulf of Mexico along the continental slope. Geo- cused flow regimes in sedimentary settings (Carson and Scre- physical data, including laser-line scan mosaics and sub- aton, 1998) and have been associated with high thermal gra- bottom profiles, document the dynamic nature of both envi- dients (Henry et al., 1996), shallow gas hydrates (Ginsburg ronments. Temperature profiles, obtained by lowering a CTD et al., 1999), and an abundance of high-molecular weight hy- into the brine fluid, show that the venting brine was at least drocarbons (Roberts and Carney, 1997). Mud volcanoes are 10◦C warmer than the bottom water. At the brine pool, ther- common seafloor features along continental shelves, conti- mal stratification was observed and only small differences in nental slopes, and in the deeper portions of inland seas (e.g., stratification were documented between three sampling times the Caspian Sea, Milkov, 2000) along both active and pas- (1991, 1997 and 1998). -
UCLA Electronic Theses and Dissertations
UCLA UCLA Electronic Theses and Dissertations Title Evolution and Population Genomics of Loliginid Squids Permalink https://escholarship.org/uc/item/0zw3h4ps Author Cheng, Samantha Hue Tone Publication Date 2015 Peer reviewed|Thesis/dissertation eScholarship.org Powered by the California Digital Library University of California UNIVERSITY OF CALIFORNIA Los Angeles Evolution and Population Genomics of Loliginid Squids A dissertation submitted in partial satisfaction of the requirements for the degree of Doctor of Philosophy in Biology by Samantha Hue Tone Cheng 2015 ABSTRACT OF THE DISSERTATION Evolution and Population Genomics of Loliginid Squids by Samantha Hue Tone Cheng Doctor of Philosophy in Biology University of California, Los Angeles, 2015 Professor Paul Henry Barber, Chair Globally, rampant harvesting practices have left vital marine resources in sharp decline precipitating a dramatic loss of the biodiversity and threatening the health and viability of natural populations. To protect these crucial resources and ecosystems, a comprehensive assessment of biodiversity, as well as a rigorous understanding of the mechanisms underlying it, is urgently needed. As global finfish fisheries decline, harvest of cephalopod fisheries, squid, in particular, has exponentially increased. However, while much is known about the evolution and population dynamics of teleost fishes, much less is understood about squids. This dissertation provides a robust, in-depth examination of these mechanisms in commercially important squids using a novel approach combining genetics and genomics methods. In the first chapter, a suite of genetic markers is used to thoroughly examine the distribution and evolution of a species complex of bigfin reef squid (Sepioteuthis cf. lessoniana) throughout the global center of marine biodiversity, the Coral Triangle, and adjacent areas.