Overview
Deep Carbon 2019: Launching the Next Decade of Deep Carbon Science is an international science conference sponsored by the Deep Carbon Observatory (DCO), with support from the Alfred P. Sloan Foundation, the Carnegie Institution for Science, and other organizations. Deep Carbon 2019 will take place 24-26 October, 2019 in Washington, DC. The conference will highlight DCO’s many scientific advances, representing the culmination of ten years of deep carbon research, exploration, and discovery. Deep Carbon 2019 will also serve to launch the future endeavors of this dynamic, interdisciplinary community.
Over the course of three days, we will share DCO’s key successes and showcase novel and forward-looking achievements in science, modeling, and instrumentation through presentations, posters, exhibits, books, films, and more.
The meeting will explore the significant progress and remaining questions in a variety of deep carbon science topics, such as:
- the nature and extent of carbon in Earth’s core and the effects of extreme temperatures and pressures on carbon’s interactions with other elements
- the physical and thermodynamic pathways in the crust and mantle that control the movements of organic molecules and how organic molecules such as methane form in deep Earth
- the nature of the whole Earth carbon cycle and how has it changed over Earth’s history
- the mechanisms that govern microbial evolution and dispersal in the deep biosphere and the ecological principles that explain deep microbial community structure
All attendees are welcome to share their experience at the meeting on Twitter using the hashtag, #DeepCarb19.
DC2019 Science Program Committee
- Isabelle Daniel, Chair, Université Claude Bernard Lyon 1
- James Badro, Institut de Physique du Globe de Paris
- Peter Barry, Woods Hole Oceanographic Institution
- Mark Lever, ETH Zürich
- Catherine McCammon, University of Bayreuth
- Brendan McCormick Kilbride, University of Manchester
- Graham Pearson, University of Alberta
- Craig Schiffries, Carnegie Institution for Science
- Fengping Wang, Shanghai Jiao Tong University
Draft Plenary Program
Thursday, 24 October 2019
Download the program (.pdf, 823 KB)
Download the abstracts (.pdf, 1.1 MB)
8:00 AM | Check-in, Continental breakfast | National Academy of Sciences, 2101 Constitution Ave NW, Washington, DC 20418 |
9:00 AM | Opening Remarks | Chair, Robert Hazen, Carnegie Institution for Science |
Eric Isaacs, Carnegie Institution for Science | ||
Adam Falk, Alfred P. Sloan Foundation | ||
9:35 AM | Lightning Talks I | Chair, Graham Pearson, University of Alberta |
Hot springs reveal deep Earth processes | Peter Barry, Woods Hole Oceanographic Institution | |
Abiotic organic compounds form in rocks below hydrothermal vents | Muriel Andreani, Université Claude Bernard Lyon 1 | |
Carbon’s transformative journey to the deep mantle | Susannah Dorfman, Michigan State University | |
Large gem-quality super-deep diamonds provide snapshots of deep Earth processes | Evan Smith, Gemological Institute of America | |
10:00 AM | Coffee break | |
10:30 AM | Session I: A Decade of Discovery | Chair, Craig Schiffries, Carnegie Institution for Science |
Extreme Physics and Chemistry | Craig Manning, University of California, Los Angeles | |
Reservoirs and Fluxes | Marie Edmonds, University of Cambridge | |
Deep Energy | Isabelle Daniel, Université Claude Bernard Lyon 1 | |
Deep Life | Mitchell Sogin, Marine Biological Laboratory | |
12:00 PM | DCO Emerging Leader Awards Presentation | |
12:15 PM | Group Photo | |
12:30 PM | Lunch | |
2:00 PM | Session II: New Programs Emerging from DCO | Chair, Catherine McCammon, University of Bayreuth |
Ocean Floor - Earth's Uncharted Interface | Kai-Uwe Hinrichs, University of Bremen | |
International Center for Deep Life Investigation: A global platform for the entire deep life community | Fengping Wang, Shanghai Jiao Tong University | |
The DFG Research Unit 2125 “Structures, properties and reactions of carbonates at high pressures and temperatures, CarboPaT" | Bjoern Winkler, Goethe University Frankfurt | |
SZ4D: Understanding the Processes that Underlie Subduction Zone Hazards in 4D | Terry Plank, Lamont-Doherty Earth Observatory / Columbia University | |
Science for Clean Energy | Alberto Striolo, University College London | |
The 4D Initiative: Deep-time Data Driven Discovery in the Evolution of Planetary Systems | Shaunna Morrison, Carnegie Institution for Science | |
The Earth First Origins Project: A New Paradigm for Searching for Life’s Origins | Karyn Rogers, Rensselaer Polytechnic Institute | |
CLEVER Planets | Raj Dasgupta, Rice University | |
4:00 PM | Depart for Poster Session | Charter bus transportation provided |
4:30 - 7:00 PM | Poster Session I including DCO Cinema and Virtual Reality Demos | Carnegie Institution for Science, 1530 P St NW, Washington, DC 20005 |
8:00 PM | The Story Collider, Special DCO Edition (tickets required) | Busboys and Poets, 2021 14th St NW, Washington, DC 20009 |
Friday, 25 October 2019
8:00 AM | Check-in, Continental Breakfast | National Academy of Sciences, 2101 Constitution Ave NW, Washington, DC 20418 |
9:00 AM | Lightning Talks II | Chair, Maggie Lau, Institute of Deep-Sea Science and Engineering, Chinese Academy of Sciences |
What the frack? Creation of a 2500 meter deep ecosystem | Kelly Wrighton, Colorado State University | |
Using noble gases to investigate the carbon-rich, ancient fluids of the deep subsurface | Oliver Warr, University of Toronto | |
Inclusions in diamonds reveal differences in how continents are made | Karen Smit, Gemological Institute of America | |
Crossover to diamond-like carbonates in the lower mantle | Sergey Lobanov, GFZ German Research Center for Geosciences | |
9:25 AM | Session III: DCO Synthesis | Chair, Tamsin Mather, University of Oxford |
Tectonic drivers of the planetary carbon cycle on geological timescales | Sabin Zahirovic, University of Sydney | |
Biology Meets Subduction: Plate tectonics drive deep biosphere microbial community compositions | Donato Giovannelli, University of Naples Federico II | |
The Carbon Mineral Challenge: A Look Back on a Four-Year Experiment in Big Data Mineralogy | Daniel Hummer, Southern Illinois University | |
How Carbon Links Fluids, Melts, and Rocks in the Deep Earth | Dimitri Sverjensky, Johns Hopkins University | |
10:30 AM | Coffee break | |
11:00 AM | Session IV: DCO Field Studies | Chair, Doug LaRowe, University of Southern California |
Initial Results of the Oman Drilling Project | Peter Kelemen, Lamont-Doherty Earth Observatory, Columbia University | |
Missions to the upper mantle—toward the most challenging endeavor in geosciences | Fumio Inagaki, Japan Agency for Marine-Earth Science and Technology | |
Exploration into the Earth’s Deep Biosphere and Hydrogeosphere | Barbara Sherwood Lollar, University of Toronto | |
Potential of abiotic methane generation in hydrothermal settings | Shuhei Ono, Massachusetts Institute of Technology | |
Forecasting Volcanic Eruptions Using Gas Emissions | Maarten de Moor, National University of Costa Rica | |
Serpentinization, carbon and life: Insights through drilling the Atlantis Massif (IODP Expedition 357) | Gretchen Früh-Green, ETH Zürich | |
12:30 PM | Lunch | |
2:00 PM | Session V: Future of Deep Carbon Science | Chair, Ivan Selin |
DCO's Decadal Goals: Crafting a Roadmap for the First 10 Years | Robert Hazen, Carnegie Institution for Science | |
Deep Carbon: Past to Present...and Future | Beth Orcutt, Bigelow Laboratory for Ocean Sciences | |
Data Science Perspectives for the Next Decade of Deep Carbon Science: Origins, Forms, Quantities, and Movements in Biogeochemical Contexts. | Peter Fox, Rensselaer Polytechnic Institute | |
Future of Deep Carbon Science: Leveraging Knowledge from the DCO on Non-steady state C-cycle catastrophes and its role in future climate states | Celina Suarez, University of Arkansas | |
The most important research questions in deep carbon science for the coming decade | Karen Lloyd, University of Tennessee | |
3:00 PM | Discussion with Audience | |
4:00 PM | Depart for Poster Session | Charter bus transportation provided |
4:30 - 7:00 PM | Poster Session II including DCO Cinema and Virtual Reality Demos | Carnegie Institution for Science, 1530 P St NW, Washington, DC 20005 |
6:45 PM | Toast and remarks | |
7:00 PM | Depart for Reception | Charter bus transportation provided |
7:30 - 9:30 PM | Reception | Smithsonian National Museum of Natural History, 10th & Constitution Ave NW, Washington, DC 20560 |
Saturday, 26 October 2019
8:00 AM | Check-in, Continental breakfast | National Academy of Sciences, 2101 Constitution Ave NW, Washington, DC 20418 |
9:00 AM | Session VI: Quantities and Movements of Deep Carbon | Chair, Mark Lever, ETH Zürich |
Carbon in the Convecting Mantle | Elizabeth Cottrell, National Museum of Natural History, Smithsonian Institution | |
Volatile cycling within the Aleutian Arc: Isotopic constraints from subducted sediment inputs and volcanic gas outputs | Taryn Lopez, University of Alaska Fairbanks | |
Metamorphic degassing of abiotic methane at convergent margins | Alberto Vitale Brovarone, Università degli Studi di Torino; IMPMC-CNRS | |
The biomass and biodiversity of the continental subsurface | Cara Magnabosco, ETH Zürich | |
Keynote: Release the Juice | Chris Ballentine, University of Oxford | |
10:30 AM | Coffee break | |
11:00 AM | Session VII: Forms of Deep Carbon | Chair, James Badro, Institut de Physique du Globe de Paris |
Earth’s carbon paradox | Jackie Li, University of Michigan | |
New perspectives on abiotic organic synthesis during hydrothermal alteration of the oceanic lithosphere | Bénédicte Menez, Institut de Physique du Globe de Paris | |
High pressure forms of aqueous carbon | Ding Pan, Hong Kong University of Science and Technology | |
C storage in reduced mantle | Marc Hirschmann, University of Minnesota | |
Keynote: Viewing carbon at extreme conditions | Wendy Mao, Stanford University | |
12:30 PM | Lunch | |
1:30 PM | Session VIII: Origins of Deep Carbon | Chair, Sami Mikhail, University of St Andrews |
Origins of Carbon in the Solar System and on Earth: An Update | Bernard Marty, University de Lorraine, CRPG/CNRS | |
CH4 isotopic bond ordering in two dimensions: summary and perspectives | Ed Young, University of California, Los Angeles | |
Carbon cycling and serpentinization: an update from Lost City and the Atlantis Massif | Susan Lang, University of South Carolina | |
Global patterns of subsurface microbial diversity and function | Rick Colwell, Oregon State University | |
Keynote: When and how does subsurface life make methane under extreme energy and carbon limitation | Alexis Templeton, University of Colorado | |
3:00 PM | Coffee break | |
3:30 PM | Future Opportunities and Closing Remarks | Chair, Marie Edmonds, University of Cambridge |
Long term evolution of whole earth carbon cycling | Cin-Ty Lee, Rice University | |
Alien oceans as an opportunity for the deep carbon community | Christopher Glein, Southwest Research Institute | |
Closing Remarks | Marie Edmonds, University of Cambridge | |
4:30 PM | Adjourn |
Poster Program
Thursday, 24 October 2019
Title | Presenter | |
T1 | CO2 output and origin from the Earth’s most actively degassing volcanoes (2005-2015): lessons learnt from the DECADE DCO project | Alessandro Aiuppa, DiSTeM - Università di Palermo |
T2 | Hydrochemical facies in ophiolitic systems | Calin Baciu, Babeș-Bolyai University |
T3 | High-temperature generation of methane in terrestrial geothermal systems: evidence from clumped isotopologues | Patrick Beaudry, Massachusetts Institute of Technology |
T4 | Predicting rates and distribution of carbonate melting in oceanic upper mantle: Implications for global carbon circulation | Mark Behn, Boston College |
T5 | Stability to dissociation and melting of carbon dioxide phase V | Roberto Bini, University of Florence - LENS |
T6 | Fate of carbon during the formation of Earth’s core | Ingrid Blanchard, Bayerisches Geoinstitut |
T7 | Natural kind clustering of presolar silicon carbides and its astrophysical implications | Asmaa Boujibar, Carnegie Institution for Science |
T8 | High-Pressure Transformations and Stability of Ferromagnesite in the Earth’s Mantle | Eglantine Boulard, CNRS-IMPMC-Sorbonne Université |
T9 | Quantifying the power of life in the deep marine biosphere | James Bradley, Queen Mary University of London |
T10 | Detection of primordial heavy noble gases in Yellowstone National Park | Michael Broadley, Centre de Recherches Pétrographiques et Géochimiques |
T11 | Using data science tools to unravel interactions between microbial communities and their geologic environment | Joy Buongiorno, Carnegie Institution for Science |
T12 | Replicate mantle diamonds | Hélène Bureau, IMPMC/CNRS |
T13 | Stability of iron-bearing carbonates in the deep Earth’s interior | Elena Bykova, Carnegie Institution for Science |
T14 | Characterising diffuse CO2 degassing in tectonically active areas by using groundwater | Carlo Cardellini, Università di Perugia |
T15 | Phase relations and elastic properties of Fe-C-H alloys at high pressures: Implications to deep carbon and hydrogen cycles | Bin Chen, University of Hawaii at Manoa |
T16 | Quantifying 4He Degassing from Crystalline Basement with 1D Vertical Transport Models | Anran Cheng, University of Oxford |
T17 | Modeling the transport of melt and volatiles by integrating thermodynamic models in geodynamic simulations using the community code ASPECT | Juliane Dannberg, University of Florida |
T18 | Decreasing temperature and increasing XCO2 boost silica dissolution in the system MgO-SiO2-H2O-CO2 | Daniel Fineman, University of California, Los Angeles |
T19 | Crustal diamonds from organic carbon compounds | Maria Luce Frezzotti, Università Milano Bicocca |
T20 | The DEW-MELTS connection: Integration of thermodynamic models for magmatic systems and aqueous fluids at elevated temperatures and pressures | Mark Ghiorso, OFM Research |
T21 | The speciation of carbon, nitrogen, hydrogen, and oxygen in magma oceans and the resulting compositions of proto-atmospheres | Damanveer Grewal, Rice University |
T22 | In vivo visualization of methyl coenzyme M reductase transcriptional activity in deep biosphere anaerobic methanotrophs (ANMEs) | Rachel Harris, Princeton University |
T23 | Global diversity of subseafloor sedimentary microbiome | Tatsuhiko Hoshino, JAMSTEC |
T24 | Injection of volatile-rich magma triggered intense paroxysmal eruption (23 Nov 2013) at Etna | Ery Hughes, California Institute of Technology |
T25 | Exploring chemolithotrophic and chemoorganotrophic microorganisms from deep granitic Archaean basement underneath the Deccan Traps, India | Sufia Kazy, National Institute of Technology Durgapur |
T26 | Origin and flux of methane within the Fennoscandian Shield, Finland | Riikka Kietäväinen, Geological Survey of Finland |
T27 | Deep Hydrocarbon Cycle | Vladimir Kutcherov, Gubkin University, KTH Royal Institute of Technology |
T28 | Magma degassing and CO2 emission at Merapi volcano, Indonesia, during a rare post-paroxysmal rest phase: continuous survey and implications | Patrick Allard, IPGP, CNRS, Université de Paris |
T29 | Microbial processing of organic carbon on a global scale | Doug LaRowe, University of Southern California |
T30 | Multiple sulfur and oxygen isotopic constraints on the origin of dissolved sulfate powering the deep subsurface biosphere in the Witwatersrand Basin, South Africa | Long Li, University of Alberta |
T31 | Preliminary results of CO2 degassing in the tectonically active areas of Balkan Peninsula. | Artur Ionescu, University of Perugia |
T32 | Deep Time Knowledge Base: Facilitate Data Integration through Machine-Readable Geologic Time Concepts | Marshall X Ma, University of Idaho |
T33 | Carbon recycling at subduction zones | Alberto Malinverno, Lamont-Doherty Earth Observatory |
T34 | Aerosol chemistry of the 2018 Kīlauea Lower East Rift Zone eruption – from source to exposed communities | Emily Mason, University of Cambridge |
T35 | Challenges to quantifying and understanding magmatic carbon fluxes today and over geological history: examples from the East African Rift | Tamsin Mather, University of Oxford |
T36 | Iron/carbon interplay in subsurface serpentinites of the Atlantis Massif (IODP Exp. 357) | Lisa Mayhew, University of Colorado Boulder |
T37 | How Earth’s early magma ocean captured mantle carbon | Catherine McCammon, University of Bayreuth |
T38 | The Evolving Picture of Abiotic Organic Synthesis in Serpentinite-hosted Deep-sea Hydrothermal Systems | Tom McCollom, University of Colorado |
T39 | Linking Enzyme Evolution to the Rock Record with Stable Isotope Enabled Enzymology | Shawn McGlynn, Earth-Life Science Institute |
T40 | Carbonate, serpentinite and water storage and supply in subducted upper oceanic lithosphere for the past 320 Ma | Andrew Merdith, Université Lyon 1 |
T41 | Structure and thermal equation of state of Ca3KNa(CO3)4 carbonate and their role in REE partitioning | Marco Merlini, Università degli Studi di Milano |
T42 | The history of deep carbon science: the 400 years of discovery prior to DCO | Simon Mitton, University of Cambridge |
T43 | Global evolution of CO2 in oceanic lithosphere over the last 230 million years | Dietmar Muller, The University of Sydney |
T44 | The Atlantic Ring of Fire: When, How, Why on Earth? | Matthieu Galvez, Swiss Federal Institute of Technology |
T45 | Recently produced microbial methane mixes with abiotic methane released during low-temperature alteration in the Samail ophiolite, Oman | Daniel Nothaft, University of Colorado |
T46 | The Potential Double-Edge Reactivity of Asbestos Fibers in Biological Systems | Ileana Pérez-Rodríguez, University of Pennsylvania |
T47 | Data to Science. Science to Data. Data Science! - EarthChem's Collaboration with the DCO | Lucia Profeta, Lamont Doherty Earth Observatory |
T48 | The Carbon Mineral Challenge: A Look Back on a Four-Year Experiment in Big Data Mineralogy | Daniel Hummer, Southern Illinois University |
T49 | Crystallographic investigations of diamonds and their inclusions: a powerful tool to unravel geological processes | Matteo Alvaro, University of Pavia |
T50 | Global Monitoring of Carbon and Sulfur Emissions from Volcanoes: Insights from Five Contributions to the DCO-DECADE initiative | Santiago Arellano, Chalmers University of Technology |
T51 | Wehrlitisation as a proxy for passage and degassing of carbonated melts | Sonja Aulbach, Goethe University |
T52 | How much methane is there in the oceans? | Max Coleman, California Institute of Technology |
T53 | The carbon content of Earth's core from metal-silicate partitioning experiments | Rebecca Fischer, Harvard University |
T54 | Volcanic and Tectonic Degassing: Progress and Challenges | Tobias Fischer, University of New Mexico |
T55 | Dihedral angle of CO2-rich melts in the deep mantle | Sujoy Ghosh, IIT Kharagpur |
T56 | Aqueous Glycine Condensation Under Extreme Conditions | Nir Goldman, Lawrence Livermore National Laboratory |
T57 | Cycling Phosphorus on the Early Earth | Jihua Hao, Rutgers University & University of Lyon 1 |
T58 | Coupled serpentinization and carbon trapping in the Oman Ophiolite | Isabelle Martinez, Institut de Physique du Globe de Paris |
T59 | Materials of the Universe - from Cosmology to Mineralogy to Materials Science | Sergey Ushakov, University of California, Davis |
T60 | Experimental Thermodynamics of Oxides above 2000 °C | Sergey Ushakov, University of California, Davis |
T61 | The Census of Deep Life and its Metadata Journey | Karyn Rogers, Rensselaer Polytechnic Institute |
T62 | The Earth First Origins Project: A New Paradigm for Searching for Life’s Origins | Karyn Rogers, Rensselaer Polytechnic Institute |
Friday, 25 October 2019
Title | Presenter | |
F1 | Oxidized carbon forms in the Earth mantle: A journey to the core mantle boundary | Valerio Cerantola, European XFEL |
F2 | Experimental constraints on the fate of MgCO3 and CaCO3 subducted into Earth’s lower mantle | Susannah Dorfman, Michigan State University |
F3 | Crystal scavenging from mush piles produces spurious melt inclusion CO2 systematics | Marie Edmonds, University of Cambridge |
F4 | An evolutionary system of mineralogy: data-driven classification of carbon minerals | Robert Hazen, Carnegie Institution for Science |
F5 | How the bacterial lipids became isotopically so “light”? | Maggie Lau, Institute of Deep-Sea Science and Engineering, Chinese Academy of Sciences |
F6 | The view from ABOVE: Aerial-based Observations of Volcanic Emissions at Manam, Papua New Guinea | Emma Liu, University College London |
F7 | Melt inclusion constraints on mantle carbon heterogeneity within an individual mantle plume | Simon Matthews, Johns Hopkins University |
F8 | Volcanic gas chemistry and flux from Bagana, a major “known unknown” deep carbon source | Brendan McCormick Kilbride, University of Manchester |
F9 | Diamonds illuminate the nature of Earth’s deep and dynamic carbon cycle | Sami Mikhail, University of St Andrews |
F10 | Macroscopic fossils of microbial communities in Eoarchean jasper from the Nuvvuagittuq Supracrustal Belt | Dominic Papineau, University College London |
F11 | Carbonic fluids trap gas in magmas and increase eruption magnitude | Mattia Pistone, University of Georgia |
F12 | DCO Engagement: Seven years of sharing deep carbon science | Robert Pockalny, University of Rhode Island, Graduate School of Oceanography |
F13 | Modelling the liquidus surface of carbonatitic magmas | Stefano Poli, Università di Milano |
F14 | Genome replication and effective CRISPR defense indicate a highly active microbiome in the continental subsurface | Alexander Probst, University of Duisburg-Essen |
F15 | Geochemical and thermodynamic constraints on the origin, composition, and stability of organic carbon in deep crustal rocks | Laurent Richard, Nazarbayev University |
F16 | Carbonate melt mobility in the upper mantle | Xenia Ritter, University of Münster, Institute for Mineralogy |
F17 | Changing the paradigm in observational volcano science: The GloVO and AVERT initiatives | Diana Roman, Carnegie Institution for Science |
F18 | Extreme Biophysics: The molecular limits of life | Catherine Royer, Rensselaer Polytechnic Institute |
F19 | Global patterns of subsurface microbial diversity and function | S. Emil Ruff, Marine Biological Laboratory |
F20 | Some unusual properties of carbonate melts in the upper and lower mantle | Chrystele Sanloup, Sorbonne Université |
F21 | Diversity and distribution of deep life within the Archaean granitic crust at Koyna, India | Pinaki Sar, Indian Institute of Technology Kharagpur |
F22 | "No vestige of a beginning…”: True or False? | John Saul |
F23 | The Deep Carbon Observatory: An Interdisciplinary Quest to Study Carbon in Earth | Craig Schiffries, Carnegie Institution for Science |
F24 | Microbial Community Responses to Drilling Induced Perturbations in a Serpentinization-Influenced Aquifer | Matt Schrenk, Michigan State University |
F25 | Insights to microbial carbon cycling in an Archean banded iron formation | Cody Sheik, University of Minnesota Duluth |
F26 | Evaluating the roles of melt-rock interaction and partial degassing on the CO2/Ba ratios of MORB: Implications for the CO2 budget in the Earth’s depleted upper mantle | Kei Shimizu, Carnegie Institution for Science |
F27 | Foundations for Geomimicry and Geobiochemistry Based on Earth as Organic Chemist | Everett Shock, Arizona State University |
F28 | Carbon solubility in the subducting slab and mantle wedge | Joyce Shi Sim, Carnegie Institution for Science |
F29 | New Observational Constraints on Decarbonation During Subduction | Emily Stewart, Yale University |
F30 | Large presence of carbonic acid in CO2-rich aqueous fluids under Earth’s mantle conditions | Nore Stolte, The Hong Kong University of Science and Technology |
F31 | C-cycle perturbation of the Late Triassic to Early Jurassic: the continental record of Western Pangea | Celina Suarez, University of Arkansas |
F32 | Deep microbial proliferation in Fe, Mg smectite-filled basalt fissures in aged oceanic crust: Implications for heterotrophic rock-hosted life | Yohey Suzuki, The University of Tokyo |
F33 | Water content of silicate mineral inclusions in superdeep diamonds from Juina, Brazil | Andrew Thomson, University College London |
F34 | Carbon Reservoirs and Fluxes in Earth from DECCIMOL: Deep Carbon Cycle Integration Model | Jonathan Tucker, Carnegie Institution for Science |
F35 | Absence of Amorphous Forms When Ice is Compressed at Low Temperature | Chris Tulk, Oak Ridge National Laboratory |
F36 | Patterns of high-P serpentinization at blueschist-to-eclogite-facies conditions and related genesis of H2 and abiotic hydrocarbons | Alberto Vitale Brovarone, Torino University/IMPMC-CNRS |
F37 | Estimating CO2 emissions at São Miguel Island (Azores archipelago) – an ongoing task | Fátima Viveiros, IVAR - University of the Azores |
F38 | Demonstration of a highly miniaturized 13CO2/12CO2 analyser for real-time, in situ, field analysis | Damien Weidmann, Rutherford Appleton Laboratory |
F39 | Carbon Dioxide Emissions from Subaerial Volcanic Regions | Cynthia Werner, Contractor (USGS, VIC) |
F40 | Earth’s Carbon Transportation System | Josh Wood, University of Rhode Island |
F41 | A deconvolution-based sensor response correction for volcanic gas measurements | Kieran Wood, University of Bristol |
F42 | Fluid driven carbonation of serpentinite in the forearc mantle wedge – a high pressure experimental investigation using serpentinite cores | Greg Yaxley, Australian National University |
F43 | Understanding modes of pyrite formation using natural clustering | Shuang Zhang, Carnegie Institution for Science |
F44 | The Influence of Nanoporosity on the Behaviour of Carbon-Bearing Fluids | Alberto Striolo, University College London |
F45 | Modelling oceanic sediment thickness and deep-sea carbonates through time | Dietmar Müller, The University of Sydney |
F46 | Coevolution of Life and Planet: role of trace metal availability in the evolution of biogeochemically relevant redox metalloenzymes | Donato Giovannelli, University of Naples Federico II |
F47 | Bridging the Gap - Implementing unusual sampling techniques at Ol Doinyo Lengai volcano, Tanzania. | Kate Laxton, University College London |
F48 | Variable carbon sources potentially lead to ecological niche adaptation and microbial diversification in serpentinizing systems. | Aurélien Lecoeuvre, Université de Paris, Institut de Physique du Globe de Paris |
F49 | Microbially mediated basalt alteration and increased CO2 retention in inoculated basalts | Rachael Moore, Institut de Physique du Globe de Paris |
F50 | Catalytic role of serpentinite paragenesis for the in situ abiotic synthesis of amino acids: a way towards metalloenzymes? | Celine Pisapia, Institut de Physique du Globe de Paris |
F51 | Fennoscandian Shield deep biosphere studies in Finland | Lotta Purkamo, Geological Survey of Finland |
F52 | Origin and rheology of CO2-rich magmas controlled by changes in the mantle oxidation state through time | Vincenzo Stagno, Sapienza University of Rome |
F53 | Transformation of carbon during high-pressure serpentinization: implications for deep carbon flux and deep energy | Renbiao Tao, Université Lyon 1, ENS de Lyon, CNRS |
F54 | Basalt-hosted crustal fluid microbial communities use diverse mechanisms to fix inorganic carbon | Elizabeth Trembath-Reichert, Arizona State University |
F55 | First-principles calculation of the stability of iron bearing carbonates at high pressure conditions. | Jun Tsuchiya, Ehime University |
F56 | A seawater throttle on H2 production in Precambrian serpentinizing systems | Benjamin Tutolo, University of Calgary |
F57 | Microbial Diversity of Rock-Hosted Serpentinite Subsurface Environment | Katrina Twing, Tennessee Tech University |
F58 | Diamonds and the Mantle Geodynamics of Carbon (DMGC): Deep Mantle Evolution from the Diamond Record | Steve Shirey, Carnegie Institution for Science |
F59 | The Deep-Sea Osmolyte TMAO and Macromolecular Crowding Facilitate Conformational Stability of DNA Hairpins and G-Quadruplex Structures Against Extreme Environmental Stresses | Roland Winter, TU Dortmund University |
F60 | Microbial and viral diversity of a deep, basalt-hosted geothermal aquifer near Mauna Kea, Hawaii | Olivia Nigro, Hawaii Pacific University |
ePosters
ePosters will be on display both Thursday and Friday.
Data Science
Title | Presenter | |
E1 | Global Earth Mineral Inventory (GEMI) : A DCO Data Legacy Global Earth Mineral Inventory (GEMI) | Anirudh Prabhu, Rensselaer Polytechnic Institute |
E1 | Analysis Toolkit for Deep-time Atmospheric Carbon Flux due to Subduction Zone Interactions Global Map of Carbon Lithology | Ahmed Eleish, Rensselaer Polytechnic Institute |
E1 | Deep Carbon Data Portal: Origins and Insights | Kathy Fontaine, Rensselaer Polytechnic Institute |
E1 | Comprehensive dataset for Hydrocarbons and H2 Formation during Serpentinization Experiments | Fang Huang, Rensselaer Polytechnic Institute |
Maps, Visualizations, and Portals
Title | Presenter | |
E2 | Mapping the Deep Subsurface Biosphere on a Sphere | Rob Pockalny, University of Rhode Island |
E2 | DCO Field Studies Map | Brenda Thompson, Rensselaer Polytechnic Institute |
E2 | Eruptions, Earthquakes & Emissions | Global Volcanism Program, Smithsonian Institution |
E2 | ENKI Portal | Mark Ghiorso, OFM Research |
E2 | The DECADE Portal | Global Volcanism Program, Smithsonian Institution, MaGa Database, EarthChem Geochemical Portal |
Poster Details
Poster boards are 6 feet wide, landscape orientation, and will have space for two posters side by side. Please ensure that your poster will fit into these maximum dimensions: 3 feet wide x 4 feet tall (91.5 cm wide x 122 cm tall).
If you submitted a poster abstract, you have been assigned to present at either the Thursday or Friday poster session. See the online program above for your assigned day and poster number. Bring your poster with you to the National Academy of Sciences on the morning of your presentation and staff will deliver it to the poster session venue and hang it in the assigned spot.
Local print shops:
Minuteman Press, 1020 19th St NW LL 50, Washington, DC 20036
Monday - Friday 9:00 a.m. - 5:30 p.m. (202) 466-7575
Sir Speedy, 2001 L Street NW Washington, DC 20036
Monday - Friday 9:00 a.m. - 5:00 p.m. (202) 857-0033
Venues & Logistics
National Academy of Sciences 2101 Constitution Ave NW, Washington, DC 20418
The main DC2019 conference venue is the National Academy of Sciences (NAS) building on Constitution Ave. Please use the Constitution Avenue building entrance on the South side of the building facing the Mall. Doors will open for check-in at 8:00 AM each day. The conference begins at 9:00 AM. We'll provide continental breakfast, AM coffee break, and lunch each day.
A government-issued photo ID will be needed each day for building security.
Directions Visitor's Guide Albert Einstein Memorial
Carnegie Institution for Science 1530 P St NW, Washington, DC 20005
Posters sessions will be held at Carnegie Science HQ on P St on Thursday (24 Oct.) and Friday (25 Oct.) from 4:30 - 7:00 PM. There will be deep carbon science posters, virtual reality demonstrations, a DCO cinema, along with drinks and hors d'oeuvres. We will provide charter bus transportation from NAS. If you arrive on foot, you can use the P St. or 16th street entrances.
Carnegie Science will host a special Capital Science Evening Lecture "Slow, Energy-efficient, and Mysterious Life Deep Within Earth’s Crust" with Karen Lloyd on Wednesday (23 Oct.) from 6:30 - 7:45 PM. This lecture is free and open to the public, but registration is required. See the event website for more information.
Smithsonian National Museum of Natural History 10th St & Constitution Ave NW, Washington, DC 20560
Deep Carbon 2019 will hold the conference reception at the Smithsonian National Museum of Natural History on Friday (25 Oct.) from 7:30 - 9:30 PM. We will provide charter bus transportation from the poster session. But if you arrive on foot, please use the the 10th and Constitution Ave entrance. There will be a coat check available. We'll have drinks and hors d'oeuvres for guests to enjoy while they explore the Hall of Geology, Gems, and Minerals.
Busboys and Poets 2021 14th St NW, Washington, DC 20009
The Story Collider is hosting a special edition of their live show with five DCO scientists at Busboys and Poets 14th St. on Thursday (24 Oct.) at 8:00 PM. Conference participants can purchase tickets at a discounted rate. Contact Katie Pratt of the DCO Engagement Team for more for details.
Download DC2019 logistics memo
Map of all DC2019 and associated event venues
Transportation
If you arrive into Dulles Airport, there are multiple options to get into downtown DC. This is a good overview that includes prices. The Silverline Express bus is a good option if you want to use public transportation. If you fly into National (DCA) Airport, there are lots of easy options to get downtown.
Once in downtown DC, most venues are within walking distance or a short Metro or cab ride away. We will provide charter bus transportation between meeting venues. But you will need to plan your way to NAS in the morning and back to your hotel after evening events.
Please note that the Marine Corps Marathon will take place on Sunday, 27 October. There will be extensive road closures from 3:30 a.m. – 5:00 p.m. to accommodate the 30K+ runners. If you are departing DC on Sunday, please allow for extra time to travel to the airport.
Accommodations
Participants are responsible for arranging their own travel and hotel reservations. We strongly advise you to make your hotel reservations as soon as possible. Our meeting dates overlap with other city-wide events and as our meeting dates approach, we anticipate that many hotels will be sold out and/or their rates may rise above the per diem reimbursement limit.
AirBNB is another recommended option, especially for participants who might want to share common space. Please contact us if you need specific questions regarding accommodations. Below are several hotels within a 1-2 miles from the conference venues:
Near National Academy of Sciences:
The Courtyard by Marriott Washington DC / Foggy Bottom 515 20th St NW, Washington, DC 20006
State Plaza Hotel 2117 E Street NW, Washington D.C. 20037
Near Dupont Circle / Carnegie Science:
Tabard Inn 1739 N St NW, Washington, DC 20036
The Fairfax at Embassy Row 2100 Massachusetts Avenue NW, Washington, DC 20008
Kimpton Hotel Palomar 2121 P St NW, Washington, DC 20037
Holiday Inn Washington DC - Central 1501 Rhode Island Ave NW, Washington, DC 20005
Other hotels downtown:
The Westin DC City Center 1400 M St NW, Washington, DC 20005
Contact
Please direct questions to DeepCarbon2019@carnegiescience.edu
or Jennifer Mays - jmays@ciw.edu or 202-505-0544 (cell)