Volcanic and Magmatic Studies Group Annual Meeting 2013
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Deep Carbon Emissions from Volcanoes Michael R
Reviews in Mineralogy & Geochemistry Vol. 75 pp. 323-354, 2013 11 Copyright © Mineralogical Society of America Deep Carbon Emissions from Volcanoes Michael R. Burton Istituto Nazionale di Geofisica e Vulcanologia Via della Faggiola, 32 56123 Pisa, Italy [email protected] Georgina M. Sawyer Laboratoire Magmas et Volcans, Université Blaise Pascal 5 rue Kessler, 63038 Clermont Ferrand, France and Istituto Nazionale di Geofisica e Vulcanologia Via della Faggiola, 32 56123 Pisa, Italy Domenico Granieri Istituto Nazionale di Geofisica e Vulcanologia Via della Faggiola, 32 56123 Pisa, Italy INTRODUCTION: VOLCANIC CO2 EMISSIONS IN THE GEOLOGICAL CARBON CYCLE Over long periods of time (~Ma), we may consider the oceans, atmosphere and biosphere as a single exospheric reservoir for CO2. The geological carbon cycle describes the inputs to this exosphere from mantle degassing, metamorphism of subducted carbonates and outputs from weathering of aluminosilicate rocks (Walker et al. 1981). A feedback mechanism relates the weathering rate with the amount of CO2 in the atmosphere via the greenhouse effect (e.g., Wang et al. 1976). An increase in atmospheric CO2 concentrations induces higher temperatures, leading to higher rates of weathering, which draw down atmospheric CO2 concentrations (Ber- ner 1991). Atmospheric CO2 concentrations are therefore stabilized over long timescales by this feedback mechanism (Zeebe and Caldeira 2008). This process may have played a role (Feulner et al. 2012) in stabilizing temperatures on Earth while solar radiation steadily increased due to stellar evolution (Bahcall et al. 2001). In this context the role of CO2 degassing from the Earth is clearly fundamental to the stability of the climate, and therefore to life on Earth. -
Inside Science
SPRING 2009 NEWS FROM THE ROYAL SOCIETY INSIDE SCIENCE YOUNG EXPLORERS TOUCHDOWN IN NEW ZEALAND International Expedition Prize is a ‘once in a lifetime experience’ SCIENCE TAKES TO THE STAGE The Royal Shakespeare Company premiers a new play on the emergence of modern science UPDATE FROM THE ROYAL SOCIETY This third issue of Inside Science contains early information DID YOU KNOW? about exciting plans for the Royal Society’s 350th Anniversary in 2010. The Anniversary is a marvellous STEADY FOOTING, opportunity to increase the profile of science, explore its SHAKY BRIDGE benefits and address the challenges it presents for society On its opening day, crowds of but perhaps most important of all to inspire young minds pedestrians experienced unexpected with the excitement of scientific discovery. swaying as they walked across London’s Our policy work continues to address major scientific issues Millennium Bridge. Whilst pedestrians affecting the UK. In December we cautioned the Government on fondly nicknamed it the ‘wobbly bridge’, the levels of separated plutonium stockpiled in the UK – currently physicists were busy exploring the the highest in the world. With support from our Plutonium Working Group, the Society has reasons for the phenomenon. submitted detailed comment to the Nuclear Decommissioning Authority (NDA) for a report to The view was widely held that the Government on management options for the stockpile. ‘wobble’ was due to crowd loading and Late last year we ran an extremely successful MP-Scientist pairing scheme, helping to build pedestrians synchronising their footsteps bridges between parliamentarians and some of the best young scientists in the UK. -
My Main Research Interests Centre on the Science Behind Volcanoes and Volcanic Behaviour
PROF. TAMSIN A. MATHER Department of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, UK. Tel.: +44 (0)1865 282125 [email protected] My main research interests centre on the science behind volcanoes and volcanic behaviour. My motivation is to understand volcanoes as (a) natural hazards, (b) a key planetary scale process throughout geological time, playing a key role in change but vital for maintaining habitability and (c) natural resources (e.g., geothermal power and the development of ore deposits). I use techniques including satellite Earth Observation, remote and direct measurements of volcanic gas/aerosol, field mapping and petrological and geochemical analysis. I have also studied the emissions from an oil depot fire (Buncefield 2005) and am generally interested in the global mercury cycle as well as other biogeochemical cycles. Post-doctoral employment (Maternity leave: June-December 2007 and January-July 2010) 2014–present: Professor of Earth Sciences, University of Oxford. 2006–2014: Lecturer/Academic Fellow in Physics & Chemistry of the Earth and Environment, Dept of Earth Sciences, University of Oxford & Fellow, University College. 2005–2009: Royal Society Dorothy Hodgkin research fellow, awarded at Cambridge and moved to Oxford (Volcanic volatile emissions: from lithosphere to atmosphere) 2005: NERC fellow Parliamentary Office of Science and Technology (Report title: Carbon capture and storage) Education and Qualifications 2001–2004: Ph.D., Dept of Earth Sciences, University of Cambridge, ‘Near-source chemistry of tropospheric volcanic plumes’. NERC funded. Awarded December 2004. 1999–2000: M.Phil. (History and Philosophy of Science), University of Cambridge. Distinction. 1995–1999: M.Sci. -
2017/18 Trinity Hall Review 2017/18 Trinity Hall CAMBRIDGE
TRINITY HALL CAMBRIDGE Trinity Hall Review 2017/18 Academic Year 2017/18 Academic Year Trinity Hall Trinity A year in the Hall life community of the Trinity 2017/18 2017/18 2 Trinity Hall Reports from our Officers Welcome to the fifth edition of the Trinity Hall Review. We hope you enjoy reading about the year in College. A highlight for us was the Alumni Summer Party in July. We were delighted to welcome over 190 alumni and guests to a sunny Wychfield for a fun-filled day of activities and socialising. We hope everyone had as much fun as our cover star! During the year, we also launched the improved College website, received planning permission for a new music practice and performance space in Avery Court, and welcomed back several alumni for their weddings in College. Your generous donations continue to have a positive impact on the lives of students and the fabric of College; thank you for your continued support. Kathryn Greaves Alumni Communications Officer Stay in touch with the College network: 32 Alumni @TrinityHallCamb News inside Reports from our Officers 2 The Master 2 The Bursar 4 The Senior Tutor 6 The Graduate Tutor 8 The Admissions Tutor 10 The Dean 11 The Development Director 12 The Junior Bursar 14 The Head of Conference and Catering Services 15 The Librarian 16 The Director of Music 17 College News 18 The JCR President’s Report 20 The MCR President’s Report 21 Student Reports 22 News of Fellows and Staff 26 Seminars and Lectures 28 Fundraising 30 18 Alumni News 32 THA Secretary’s Report 34 College News Alumni News 36 In Memoriam 38 2017/18 Information 40 List of Fellows 42 College Statistics 46 List of Donors 50 Get involved 59 Thank you to all who have contributed to this edition of the Trinity Hall Review. -
The Role of Melt Composition on Aqueous Fluid Vs. Silicate Melt
The role of melt composition on aqueous fluid vs. silicate melt partitioning of bromine in magmas Anita Cadoux, Giada Iacono-Marziano, Bruno Scaillet, Alessandro Aiuppa, Tamsin Mather, David Pyle, Étienne Deloule, Emanuela Gennaro, Antonio Paonita To cite this version: Anita Cadoux, Giada Iacono-Marziano, Bruno Scaillet, Alessandro Aiuppa, Tamsin Mather, et al.. The role of melt composition on aqueous fluid vs. silicate melt partitioning of bromine in magmas. Earth and Planetary Science Letters, Elsevier, 2018, 498, pp.450-463. 10.1016/j.epsl.2018.06.038. insu-01856882 HAL Id: insu-01856882 https://hal-insu.archives-ouvertes.fr/insu-01856882 Submitted on 13 Aug 2018 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. Distributed under a Creative Commons Attribution - NonCommercial - NoDerivatives| 4.0 International License *Manuscript Click here to view linked References 1 2 The role of melt composition on aqueous fluid vs. silicate melt 3 partitioning of bromine in magmas 4 5 Anita Cadouxa,b,c,d, Giada Iacono-Marzianoa,b,c, Bruno Scailleta,b,c, Alessandro Aiuppae,f, 6 Tamsin A. Matherg, David M. Pyleg, Etienne Delouleh, Emanuela Gennaroa,b,c,f, Antonio 7 Paonitae 8 9 10 a Université d’Orléans, ISTO, UMR 7327, 45071, Orléans, France 11 b CNRS, ISTO, UMR 7327, 45071 Orléans, France 12 c BRGM, ISTO, UMR 7327, BP 36009, 45060 Orléans, France 13 d GEOPS, Univ. -
TRAINING REVAMPED John Underhill on the Role of Doctoral Training in Addressing 21St Century Challenges
SCIENTISTVOLUME 29 No. 08 ◆ SEPTEMBER 2019 ◆ WWW.GEOLSOC.ORG.UK/GEOSCIENTIST GEOThe Fellowship Magazine of the Geological Society of London @geoscientistmag A fresh look at geoscience education TRAINING REVAMPED John Underhill on the role of doctoral training in addressing 21st Century challenges GEOSCIENTISTS WANTED! FUTURE RESOURCES STATE OF PLAY To steward the transition Building a The worrying decline of UK to clean energy multidisciplinary community geoscience education WWW.GEOLSOC.ORG.UK/GEOSCIENTIST | SEPTEMBER 2019 | 1 WHERE IS YOUR The Geological Society FUTURE IN MINING? Career and Industry Days 2019/20 Wednesday 6 November 2019 JOIN DIGBEE AND FIND OUT... Venue: BGS, Keyworth, Nottingham, UK Wednesday 4 December 2019 Venue: Our Dynamic Earth, Edinburgh, UK Wednesday 19 February 2020 World's first expert network for mining professionals Venue: The Geological Society of London, Burlington House, London, UK www.geolsoc.org.uk/Education-and-Careers/ Free access to data from thousands of mining projects Careers-Information/Careers-Days Earn recurring income by writing geological summaries The Geological Society Career & Industry Day is an essential meeting place for geoscience students and the geoscience industry, and is the most recognised geoscience from technical feasibility studies (coming Q4 2019) careers focused forum in the country. The day will include short career and industry presentations covering different areas Free to join of geology and academia, and there will be an exhibition consisting of industry and professional bodies, and higher education institutions promoting MSc and PhD programmes. There will also be a CV and careers workshop running alongside the talks. For more info: Registration thedigbee.com/geologist This event is free to attend but there are limited numbers so pre-booking is recommended. -
A View from the City
UNIVERSITY COLLEGE OXFORD ISSUE 3 SUMMER 2015 A VIEW FROM THE CITY LEIGH INNES (1994) AND LIFE IN THE MARKETPLACE ALSO IN THIS ISSUE GEORGE CAWKWELL CELEBRATES 65 YEARS AT UNIV LOUISE TAYLOR (2011) ON THE PURSUIT OF PERFECTION ELECTION NIGHT SPECIAL WITH SIR IVOR CREWE THE MAGNA CARTA AT UNIV JOHN RADCLIFFE’S MEDICAL LEGACY FROM THE EDITOR University College Oxford OX1 4BH elcome to the Summer 2015 issue of The Martlet, the magazine for www.univ.ox.ac.uk Members and Friends of University College Oxford. I would like to Wexpress my sincere thanks to those Old Members, students, Fellows, staff www.facebook.com/univalumni and Friends of the College who contributed to this issue. [email protected] I would also like to take this opportunity to thank our extended Univ team – © University College, Oxford, 2015 Charles New and Andrew Boyle at B&M Design & Advertising Limited, who produce the magazine; Clare Holt and the team at Nice Tree Films who worked tirelessly on Produced by B&M Design & Advertising our recent videos – in particular the Election Night Special, for which they stayed www.bm-group.co.uk up well past their bedtimes! Michelle Enoch and the team at h2o creative for their splendid design concepts for the 1249 Society, and our unofficial ‘in-house’ designer Rob Moss and photographer Rachel Harrison for all their hard work on our event If you would like to share your thoughts or programmes and College photography. comments about The Martlet, please e-mail: [email protected] Enormous thanks also to Dr Robin Darwall-Smith and Frances Lawrence for their invaluable help with the In Memoriam section of the magazine. -
Glaciovolcanism at Volcán Sollipulli, Southern Chile: Lithofacies Analysis and Interpretation
Journal of Volcanology and Geothermal Research 303 (2015) 59–78 Contents lists available at ScienceDirect Journal of Volcanology and Geothermal Research journal homepage: www.elsevier.com/locate/jvolgeores Glaciovolcanism at Volcán Sollipulli, southern Chile: Lithofacies analysis and interpretation Stefan M. Lachowycz a,⁎, David M. Pyle a, Jennie S. Gilbert b, Tamsin A. Mather a,KatyMeec, José A. Naranjo d, Laura K. Hobbs b a Department of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, United Kingdom b Lancaster Environment Centre, Lancaster University, Lancaster LA1 4YQ, United Kingdom c British Geological Survey, Environmental Science Centre, Keyworth, Nottingham NG12 5GG, United Kingdom d Servicio Nacional de Geología y Minería, Avenida Santa María 0104, Santiago, Chile article info abstract Article history: Magma–ice–meltwater interactions produce diverse landforms and lithofacies, reflecting the multitude of factors Received 18 December 2014 that influence glaciovolcanism, including both magmatic (e.g., composition, eruption rate) and glacial (e.g., ice Accepted 20 June 2015 thickness, thermal regime) conditions. This is exemplified by the walls of the partly ice-filled summit caldera Available online 3 July 2015 of Volcán Sollipulli, a stratovolcano in southern Chile, which include lithofacies from eruptions of a wide range of magma compositions beneath or in contact with ice. Here we analyse these lithofacies and hence propose Keywords: new interpretations of the eruptive and glacial history of Sollipulli. The facies include a thick, laterally extensive Volcano–ice interaction fi Glaciovolcanic lithofacies sequence of fragmental glaciovolcanic deposits, comprising massive, ma c lava pillow-bearing hyaloclastite Hyaloclastite overlain by sills and then hyaloclastic debris flow deposits (similar to Dalsheidi-type sequences). -
Je-S Combined
NERC Polaris House, North Star Avenue, Swindon, Wiltshire, United Kingdom SN2 1EU Telephone +44 (0) 1793 411500 Web http://www.nerc.ac.uk/ COMPLIANCE WITH THE DATA PROTECTION ACT 1998 In accordance with the Data Protection Act 1998, the personal data provided on this form will be processed by NERC, and may be held on computerised database and/or manual files. Further details may be found in the guidance notes Large Grant Document Status: With Council PROPOSAL NERC Reference: NE/L013932/1 Large Grant NOV13 Organisation where the Grant would be held Research Organisation Organisation University of Edinburgh RiftVolc Reference: Division or Department Sch of Geosciences Project Title [up to 150 chars] Rift volcanism: past, present and future Start Date and Duration a. Proposed start b. Duration of the grant 01 September 2014 60 date (months) Applicants Role Name Organisation Division or Department How many hours a week will the investigator work on the project? Professor Kathryn Principal Investigator University of Edinburgh Sch of Geosciences 7.5 Whaler Professor Ian Graham Co-Investigator University of Edinburgh Sch of Geosciences 1.13 Main Co-Investigator Dr Eliza Calder University of Edinburgh Sch of Geosciences 1.8 Co-Investigator Dr Andrew Bell University of Edinburgh Sch of Geosciences 1.8 Technology Is this project technology-led? No Describe the type of technology being developed and its application to NERC science; an indicator of the level of maturity of the technology should be included (up to 500 characters). Collaborative Centres Please check the the appropriate button if this proposal is being submitted under the auspices of either NCAS or NCEO, and has been explicitly agreed with the centre administrator. -
Vmsg Abstract Book
V-VMSG Annual General Meeting 6-8 January 2021 Abstract book CODE OF CONDUCT FOR MEETINGS AND EVENTS The Volcanic & Magmatic Studies Group is a Special Interest Group joint between the Geological Society of London and Mineralogical Society. These learned societies are signatories to the Science Council Declaration on Diversity, Equality and Inclusion. Through their members, the Geological Society of London and Mineralogical Society have a duty in the public interest to provide a safe, productive and welcoming environment for all participants and attendees of meetings, workshops, and events regardless of gender, sexual orientation, gender identity, race, ethnicity, religion, disability, physical appearance, or career level. The Volcanic & Magmatic Studies Group has worked with the Geological Society of London and Mineralogical Society on Code of Conduct policies. These are available from https://www.geolsoc.org.uk/codeofconduct and https://www.minersoc.org/code-of- conduct.html. The Code of Conduct outlined below specifically applies to all participants in Volcanic & Magmatic Studies Group activities, including ancillary events and social gatherings. The Volcanic & Magmatic Studies Group expects all participants -- including, but is not limited to, attendees, speakers, volunteers, exhibitors, staff, service providers and representatives to outside bodies -- to uphold the principles of this Code of Conduct. 1. Behaviour The Volcanic & Magmatic Studies Group aims to provide a constructive, supportive and professionally stimulating environment for all its members. Participants of VMSG meetings and events are expected to behave in a professional manner at all times. 2. Unacceptable Behaviour Harassment and/or sexist, racist, or exclusionary comments or jokes are not appropriate and will not be tolerated. -
Glaciovolcanism at Volcán Sollipulli, Southern Chile: Lithofacies Analysis and Interpretation
Journal of Volcanology and Geothermal Research 303 (2015) 59–78 Contents lists available at ScienceDirect Journal of Volcanology and Geothermal Research journal homepage: www.elsevier.com/locate/jvolgeores Glaciovolcanism at Volcán Sollipulli, southern Chile: Lithofacies analysis and interpretation Stefan M. Lachowycz a,⁎, David M. Pyle a, Jennie S. Gilbert b, Tamsin A. Mather a,KatyMeec, José A. Naranjo d, Laura K. Hobbs b a Department of Earth Sciences, University of Oxford, South Parks Road, Oxford OX1 3AN, United Kingdom b Lancaster Environment Centre, Lancaster University, Lancaster LA1 4YQ, United Kingdom c British Geological Survey, Environmental Science Centre, Keyworth, Nottingham NG12 5GG, United Kingdom d Servicio Nacional de Geología y Minería, Avenida Santa María 0104, Santiago, Chile article info abstract Article history: Magma–ice–meltwater interactions produce diverse landforms and lithofacies, reflecting the multitude of factors Received 18 December 2014 that influence glaciovolcanism, including both magmatic (e.g., composition, eruption rate) and glacial (e.g., ice Accepted 20 June 2015 thickness, thermal regime) conditions. This is exemplified by the walls of the partly ice-filled summit caldera Available online 3 July 2015 of Volcán Sollipulli, a stratovolcano in southern Chile, which include lithofacies from eruptions of a wide range of magma compositions beneath or in contact with ice. Here we analyse these lithofacies and hence propose Keywords: new interpretations of the eruptive and glacial history of Sollipulli. The facies include a thick, laterally extensive Volcano–ice interaction fi Glaciovolcanic lithofacies sequence of fragmental glaciovolcanic deposits, comprising massive, ma c lava pillow-bearing hyaloclastite Hyaloclastite overlain by sills and then hyaloclastic debris flow deposits (similar to Dalsheidi-type sequences). -
7.9 Contents5 Auth UK US.Indd
Vol 443 | Issue no. 7107 | 7 September 2006 AUTHORS inclusions, the pockets of melt trapped by crys- Abstractions MAKING THE PAPER tals deep below Earth’s surface. By examining FIRST AUTHOR Kathy Cashman various inclusions trapped at different times Studies of the visual during the magma’s ascent, they attempted to system have revealed a piece together how magma changes as it works lot about how we process Volcano monitoring heats up with its way to the surface. simple features of an new magma knowledge The work relied on 25 years’ worth of sam- object such as its shape, ples from Mount St Helens in Washington and colour and movement. Volcanologists still aren’t particularly adept at additional samples collected over a period of Much less is known about working out exactly when volcanic eruptions five years from the Kamchatka Peninsula, a vol- how the brain encodes the meaning, or will occur, how they happen or how long they canic hotbed in eastern Russia. Cashman and category, of visual stimuli. On page 85 of this are likely to last. Now, Kathy Cashman at the Blundy analysed selected inclusions with an issue, David Freedman, from Harvard Medical University of Oregon in Eugene and her col- instrument known as an ion microprobe. This School, reports the identification of monkey leagues have found a geological clue about the measures the water content and the concentra- brain cells that they believe allot meaning to heating of magma (see page 76). This could tion of different elements by blasting away part objects. These cells are located in the lateral help modellers better describe the several- of the sample and running it through a mass intraparietal (LIP) area, a brain region that uses visual information to help monkeys kilometre journey this molten rock makes to spectrometer.