Hydrogen Isotope Ratios of Individual Organic Compounds

Total Page:16

File Type:pdf, Size:1020Kb

Hydrogen Isotope Ratios of Individual Organic Compounds HYDROGEN ISOTOPE RATIOS OF INDIVIDUAL ORGANIC COMPOUNDS Alex L. Sessions Submitted to the faculty of the University Graduate School in partial fulfillment of the requirements for the degree Doctor of Philosophy in the Department of Geological Sciences Indiana University August, 2001 i Acknowledgements The completion of this thesis is due to the patient advice and kind help of many, many people. Foremost among them is Dr. John Hayes, who has worked tirelessly to teach me not only the fundamentals, but the art of conducting scientific research. The depth and breadth of my education under him has been remarkable, and I am deeply grateful. I can think of no better compliment than the fact that I am eagerly staying on as a post-doc under his direction. My advising committee, Drs. Simon Brassell, Tim Eglinton, Gary Hieftje, and Arndt Schimmelmann, also deserve a hearty thank-you. They have been encouraging and supportive as I progressed through the Ph.D. program, and each one has answered more than his share of ridicu- lous questions (Why does D2O kill bugs?) My parents – who also deserve a great deal of credit for encouraging an inquistive mind and love of science – sympathize with you all. Two people in particular are responsible for teaching me the nuts and bolts of isotope geochemistry. Dr. Tom Burgoyne, a post-doc at Bloomington, coached me in the fine points of using, fixing, and understanding mass spectrometers. Dr. Chris Reddy, a post-doc and later assistant scientist at WHOI, showed me how to work in an organic geochemistry laboratory. It is a rare day that I do not use some technique, trick, or rule of thumb that they taught me. Many other folks have helped me with this thesis in countless ways. Arndt Schimmelmann performed offline δD measurements of all our organic standards, and of the culture media and gases used in Chapter 5. Peter Sauer helped collect specimens for our first D/H analyses (Chapter 1), and Great Pond sediment for exchange experiments. Sean Sylva helped prepare, extract, and analyze the hydrogen exchange experiments (Chapter 4). Linda Jahnke grew Methylococcus capsulatus, and Kathleen Londry grew sulfate-reducing bacteria, which together comprise Chapter 5. Roger Summons provided numerous consultations over mass spectra. Other helpful folks include: Steve Studley, Julie Primack, Kristen Leckrone, Lisa Pratt, Jennifer Villinski, and Jon Fong at Indiana University; Daniel Montlucon, Jeff Seewald, Kai-Uwe Hinrichs, Paul Fucile, Carl Johnson, Leah Houghton, and the entire staff of NOSAMS at WHOI. Financial support during the past five years has been provided by a fellowship from the University Graduate School at Indiana University; by grants to John Hayes from NASA and the National Science Foundation; through John Hayes’ WHOI research funds; and by a generous grant from Royal Dutch Shell, arranged by Dr. Olaf Podlaha. Last and most importantly, I would not have made it this far without my wife, Karen. She has supported and encouraged me in every way possible. Many thanks to all of you. ii Preface When I first met John Hayes in February, 1996, he suggested that the development of continuous-flow hydrogen-isotopic analyses might be a good thesis project. While I scarcely understood what ‘continuous-flow’ meant at the time, the project sounded exciting and I ac- cepted. Thus began a five-year project involving myself, John Hayes, Tom Burgoyne, and Arndt Schimmelmann. By the spring of 1997 work was underway. Tom quickly developed high-tem- perature pyrolysis as an efficient means for converting organic hydrogen to H2, work that was later published in Analytical Chemistry (1998, 70:5136-5141). Meanwhile, Arndt and I struggled to perfect a Pd filter for separating H2 from He. That approach quickly fizzled, and I began to systematically study the problem of H3 correction in continuous flow hydrogen analyses. In preparation for improvements to come, I began to develop the Excel macros that Tom would eventually dub ‘AlexDAT’ after the Finnigan software of a similar name. By the spring of 1998, we were testing our second prototype of the ‘ED,’ an energy-dis- criminating lens that Tom designed and built to suppress low-energy He+. In June, I moved my family and the partially-developed hydrogen system to Woods Hole to continue work in John’s new labs. A discouraging summer of testing and rebuilding the ED followed, but by the fall the ED had evolved enough to allow us to make our first crude D/H measurements of real samples. We quickly discovered that many, if not all, organic geochemical laboratories are rife with the perdeuterated compounds used as internal standards for GC. To facilitate more rapid progress, John and I scoured the WHOI biology department in search of suitable phytoplankton cultures, and in February, 1999, Peter Sauer and I collected the plants from Woods Hole Harbor that eventually formed the basis for our 1999 Organic Geochemistry paper (Chapter 1). With an initial publication under our belt, in the summer of 1999 we turned back to refining analytical tech- niques, working both on perfecting H3 corrections and on eliminating the GC peak-tailing that had plagued us from the earliest days. Work on H3 corrections eventually culminated in the publication of back-to-back papers in Analytical Chemistry in December, 2000 (Chapters 2 and 3). But despite the helpful suggestions from many gurus of gas chromatography, we never solved the peak-tailing problems, though (much to our chagrin) Andreas Hilkert in Bremen did. By the fall of 1999 Tom had moved to Oklahoma State, the hydrogen system was largely functional, and our research interests diverged. I began dabbling with hydrogen exchange experiments, and travelled to Moffett Field to learn how to grow Methylococcus capsulatus from the master, Linda Jahnke. The period from fall, 1999, to spring, 2001 was spent producing the data that appears in Chapters 4 and 5. The purposes of this rambling preface are twofold. The first is to provide a historical perspective for the D/H project. This thesis chronicles only the parts of the project for which I was primarily responsible. The chapters of the thesis are presented as they were written, in chronological order, rather than in some logical progression of topics. Chapters 1–3 have been reproduced in the form they appeared in publication, complete with abstract and references. For consistency, chapters 4 and 5 follow this format, though they have not yet been submitted for publication. The second purpose of this preface is to emphasize that this project has been a team effort in every sense, and while each of us was responsible for different aspects of it, none of the work reported here (or elsewhere) would have been possible without the individual contributions of all four scientists. iii Table of Contents Acknowledgements ........................................................................................................... ii Preface ............................................................................................................................... iii Chapter 1 — Fractionation of hydrogen isotopes in lipid biosynthesis ....................... 1 Abstract ..................................................................................................................................... 1 Introduction ............................................................................................................................... 2 Experimental ............................................................................................................................. 3 Isotopic Measurements ....................................................................................................... 3 Sample Collection and Preparation .................................................................................... 5 Results and Discussion ............................................................................................................. 5 Variations of δD Within Organisms ................................................................................... 8 Isotopic Fractionation ....................................................................................................... 10 Variations of δD Between Organisms .............................................................................. 11 Conclusions ............................................................................................................................. 12 References ............................................................................................................................... 13 + Chapter 2 — Correction of H3 contributions in hydrogen isotope-ratio-monitoring mass spectrometry .................................................................................................... 15 Abstract ................................................................................................................................... 15 Introduction ............................................................................................................................. 16 Theory ..................................................................................................................................... 16 + H3 Correction Algorithms ................................................................................................ 18 Peakwise Corrections ....................................................................................................... 19 Pointwise Corrections .....................................................................................................
Recommended publications
  • Characterization of N-Alkanes, Pristane and Phytane in the Cretaceous/ Tertiary Boundary Sediments at Kawaruppu, Hokkaido, Japan
    Geochemical Journal, Vol. 33, pp. 285 to 294, 1999 Characterization of n-alkanes, pristane and phytane in the Cretaceous/ Tertiary boundary sediments at Kawaruppu, Hokkaido, Japan HAJIME MITA and AKIRA SHIMOYAMA Department of Chemistry, University of Tsukuba, Tsukuba 305-8571, Japan (Received December 24, 1998; Accepted April 22 , 1999) Normal alkanes from C12 to C36, pristane and phytane were identified in the Cretaceous/Tertiary (K/T) boundary sediments at Kawaruppu, Hokkaido, Japan. These compounds were found at the levels of sub to a few nmol g-1. Total concentrations of the n-alkanes within the boundary claystone were generally one third to one half of those in the sediments above and below the claystone. The smaller concentrations within the claystone were mainly due to smaller concentrations of longer chain n-alkanes (C25 to C31) than in the sediments above and below it. The longer chain n-alkanes were likely from terrestrial plants and reflected their small population at the end of Cretaceous. The concentration of longer chain n-alkanes decreased rapidly at the base of the boundary claystone, indicating the sudden cease of terrestrial n-alkane input, continued low to the horizon at the upper two thirds of the claystone and then, started increasing toward the top of the claystone. The n-alkane concentration change indicates the period of the small input of terrestrial n-alkanes to be ca. 7,000 years at most and the recovery period to be ca. 2,000 years. The depth distribution pattern of pristane plus phytane concentrations in the K/T sediments roughly resembles that of the n-alkanes.
    [Show full text]
  • Carbon Geochemistry of Serpentinites in the Lost City Hydrothermal System (30°N, MAR)
    Available online at www.sciencedirect.com Geochimica et Cosmochimica Acta 72 (2008) 3681–3702 www.elsevier.com/locate/gca Carbon geochemistry of serpentinites in the Lost City Hydrothermal System (30°N, MAR) Ade´lie Delacour a,*, Gretchen L. Fru¨h-Green a, Stefano M. Bernasconi b, Philippe Schaeffer c, Deborah S. Kelley d a Institute for Mineralogy and Petrology, ETH Zurich, CH-8092 Zurich, Switzerland b Geological Institute, ETH Zurich, CH-8092 Zurich, Switzerland c Laboratoire de Ge´ochimie Bioorganique, UMR 7177 du CNRS, Universite´ Louis Pasteur, Strasbourg, France d School of Oceanography, University of Washington, Seattle, WA 98195, USA Received 18 June 2007; accepted in revised form 30 April 2008; available online 24 May 2008 Abstract The carbon geochemistry of serpentinized peridotites and gabbroic rocks recovered at the Lost City Hydrothermal Field (LCHF) and drilled at IODP Hole 1309D at the central dome of the Atlantis Massif (Mid-Atlantic Ridge, 30°N) was exam- ined to characterize carbon sources and speciation in oceanic basement rocks affected by long-lived hydrothermal alteration. Our study presents new data on the geochemistry of organic carbon in the oceanic lithosphere and provides constraints on the fate of dissolved organic carbon in seawater during serpentinization. The basement rocks of the Atlantis Massif are charac- 13 terized by total carbon (TC) contents of 59 ppm to 1.6 wt% and d CTC values ranging from À28.7& to +2.3&. In contrast, 13 total organic carbon (TOC) concentrations and isotopic compositions are relatively constant (d CTOC: À28.9& to À21.5&) 13 and variations in d CTC reflect mixing of organic carbon with carbonates of marine origin.
    [Show full text]
  • The Effects of Detritus Input on Soil Organic Matter Content and Carbon Dioxide Emission in a Central European Deciduous Forest
    Acta Silv. Lign. Hung., Vol. 7 (2011) 87–96 The Effects of Detritus Input on Soil Organic Matter Content and Carbon Dioxide Emission in a Central European Deciduous Forest a* b c István FEKETE – Zsolt KOTROCZÓ – Csaba VARGA – b b Zsuzsa VERES – János Attila TÓTH a Institute of Environmental Science, College of Nyíregyháza, Nyíregyháza, Hungary b Department of Ecology, University of Debrecen, Debrecen, Hungary c Department of Land and Environmental Management, College of Nyíregyháza, Nyíregyháza, Hungary Abstract – A major objective of our research was to survey soil biological activity and organic matter content reduction in a Central European oak forest during treatments of various detritus inputs within the Síkf őkút DIRT ( Detritus Input and Removal Treatments ) Project. Beside the control, three detritus removal and two detritus duplication treatments were applied. Our examinations have proven that soil organic matter content declined relatively fast in detritus removal treatments. The reduction was especially remarkable in root detritus removal treatments, where – due to the lack of transpiration – soils were moister during the whole year than in the other treatments. The higher moisture content, despite of the reduction of detritus input, produced an intense soil respiration. This can be explained by the fact that decomposing organisms have increased the use of soil organic matter. Detritus input reduction had a significantly greater effect on soil respiration and organic matter content than detritus input duplication of the same extent. The latter did not cause any significant change compared to the control. litter manipulation / soil respiration / DIRT Project / humus content / climate change Kivonat – Az avarinput hatása a talaj szerves anyag tartalmára és szén-dioxid kibocsátására egy Közép-európai lombhullató erd őben.
    [Show full text]
  • Lipid Analysis of CO2-Rich Subsurface Aquifers Suggests an Autotrophy-Based Deep Biosphere with Lysolipids Enriched in CPR Bacteria
    The ISME Journal (2020) 14:1547–1560 https://doi.org/10.1038/s41396-020-0624-4 ARTICLE Lipid analysis of CO2-rich subsurface aquifers suggests an autotrophy-based deep biosphere with lysolipids enriched in CPR bacteria 1,2 3,4 1,3 3 3 Alexander J. Probst ● Felix J. Elling ● Cindy J. Castelle ● Qingzeng Zhu ● Marcus Elvert ● 5,6 6 1 7,9 7 Giovanni Birarda ● Hoi-Ying N. Holman ● Katherine R. Lane ● Bethany Ladd ● M. Cathryn Ryan ● 8 3 1 Tanja Woyke ● Kai-Uwe Hinrichs ● Jillian F. Banfield Received: 20 November 2018 / Revised: 5 February 2020 / Accepted: 25 February 2020 / Published online: 13 March 2020 © The Author(s) 2020. This article is published with open access Abstract Sediment-hosted CO2-rich aquifers deep below the Colorado Plateau (USA) contain a remarkable diversity of uncultivated microorganisms, including Candidate Phyla Radiation (CPR) bacteria that are putative symbionts unable to synthesize membrane lipids. The origin of organic carbon in these ecosystems is unknown and the source of CPR membrane lipids remains elusive. We collected cells from deep groundwater brought to the surface by eruptions of Crystal Geyser, sequenced 1234567890();,: 1234567890();,: the community, and analyzed the whole community lipidome over time. Characteristic stable carbon isotopic compositions of microbial lipids suggest that bacterial and archaeal CO2 fixation ongoing in the deep subsurface provides organic carbon for the complex communities that reside there. Coupled lipidomic-metagenomic analysis indicates that CPR bacteria lack complete lipid biosynthesis pathways but still possess regular lipid membranes. These lipids may therefore originate from other community members, which also adapt to high in situ pressure by increasing fatty acid unsaturation.
    [Show full text]
  • APPENDIX M SUMMARY of MAJOR TYPES of Carfg2 REFINERY
    APPENDIX M SUMMARY OF MAJOR TYPES OF CaRFG2 REFINERY MODIFICATIONS Appendix M: Summan/ of Major Types of CaRFG2 Refinery Modifications: Alkylation Units A process unit that combines small-molecule hydrocarbon gases produced in the FCCU with a branched chain hydrocarbon called isobutane, producing a material called alkylate, which is blended into gasoline to raise the octane rating. Alkylate is a high octane, low vapor pressure gasoline blending component that essentially contains no olefins, aromatics, or sulfur. This plant improves the ultimate gasoline-making ability of the FCC plant. Therefore, many California refineries built new or modified existing units to increase alkylate production to blend and to produce greater amounts of CaRFG2. Alkylate is produced by combining C3, C4, and C5 components with isobutane (nC4). The process of alkylation is the reverse of cracking. Olefins (such as butenes and propenes) and isobutane are used as feedstocks and combined to produce alkylate. This process enables refiners to utilize lighter components that otherwise could not be blended into gasoline due to their high vapor pressures. Feed to alkylation unit can include pentanes from light cracked gasoline treaters, isobutanes from butane isomerization unit, and C3/C4 streams from delayed coking units. Isomerization Units - C4/C5/C6 A refinery that has an alkylation plant is not likely to have exactly enough is-butane to match the proplylene and butylene (olefin) feeds. The refiner usually has two choices - buy iso-butane or make it in a butane isomerization (Bl) plant. Isomerization is the rearrangement of straight chain hydrocarbon molecules to form branched chain products or to convert normal paraffins to their isomer.
    [Show full text]
  • Fractionation and Characterization of Natural Organic Matter from Certain Rivers and Soils by Free-Flow Electrophoresis
    Fractionation and Characterization of Natural Organic Matter from Certain Rivers and Soils by Free-Flow Electrophoresis GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1817-E Fractionation and Characterzation of Natural Organic Matter from Certain Rivers and Soils by Free-Flow Electrophoresis By J. A. LEENHEER and R. L. MALCOLM ORGANIC SUBSTANCES IN WATER GEOLOGICAL SURVEY WATER-SUPPLY PAPER 1817-E UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1973 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY V. E. McKelvey, Director Library of Congress catalog-card No. 73-600209 For sale by the Superintendent of Documents, U. S. Government Printing Office Washington, D. C. 20402 - Price 35 cents (paper cov«?r) Stock No. 2401-02400 CONTENTS Page Abstract ___________________________________________ El Introduction __________________________________ __ 1 Methods and materials __________________________________ 3 Sample preparation ______ _______ _ __ 3 Sample description _________________________________ 3 Separation procedure _______ ___________ __ 4 Assay of fractions ___________________________________ 4 Results and discussion _ _______________ 5 Conclusions ________________________________________ 12 References _____________________________________ __ 14 ILLUSTRATIONS Page FIGURES 1-3. Graphs showing: 1. Organic-carbon and optical-density electrophoretic fraction- ation curves for organic materials from soil and from river water ___________________________ E6 2. Organic-carbon and polysaccharide electrophoretic
    [Show full text]
  • Stable Carbon and Hydrogen Isotopic Fractionation of Individual N-Alkanes Accompanying Biodegradation: Evidence from a Group of Progressively Biodegraded Oils
    中国科技论文在线 http://www.paper.edu.cn Organic Geochemistry 36 (2005) 225–238 Stable carbon and hydrogen isotopic fractionation of individual n-alkanes accompanying biodegradation: evidence from a group of progressively biodegraded oils Yongge Sun a,*, Zhenyan Chen b, Shiping Xu a, Pingxia Cai a a SKLOG, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Wushan, Guangzhou 510640, PR China b Exploration and Development Research Institute of Liaohe Oil Field Branch Company, PetroChina, Panjing, Liaoning 124010, PR China Received 10 March 2004; accepted 16 August 2004 (returned to author for revision 16 April 2004) Available online 11 November 2004 Abstract Seven crude oils of known source and maturity, representing a natural sequence of increasing degree of biodegrada- tion, were collected from reservoirs in the Liaohe Basin, NE China, in an effort to determine the magnitude and direction of isotopic shift of carbon and hydrogen in individual n-alkanes during microbial degradation. The results show that bio- degradation has little effect on the carbon isotopic composition of the whole oil. However, a sequential loss of n-alkanes leads to 13C depletion of the bulk residual saturate fraction. The stable carbon isotopic compositions of aromatics and macromolecular organic matter (resins and asphaltenes) follow a pattern, with an overall trend towards 13C enrichment of 0.8–1.7& in the residues. The stable carbon and hydrogen isotope values of individual n-alkanes demonstrate that they follow different trends during biodegradation. No significant carbon isotopic fractionation occurs for n-alkanes during slight to moderate biodegradation. However, there is a general increase of up to 4& in the d13C values of low molecular weight n-alkanes (C15–C18) during heavy biodegradation.
    [Show full text]
  • Determining the Fraction of Organic Carbon RISC Nondefault Option
    Indiana Department of Environmental Management Office of Land Quality 100 N. Senate Indianapolis, IN 46204-2251 GUIDANCE OLQ PH: (317) 232-8941 Indiana Department of Environmental Management Office of Land Quality Determining the Fraction of Organic Carbon RISC Nondefault Option Background Soil can be a complex mixture of mineral-derived compounds and organic matter. The ratios of each component can vary widely depending on the type of soil being investigated. Soil organic matter is a term used by agronomists for the total organic portion of the soil and is derived from decomposed plant matter, microorganisms, and animal residues. The decomposition process can create complex high molecular weight biopolymers (e.g., humic acid) as well as simpler organic compounds (decomposed lignin or cellulose). Only the simpler organic compounds contribute to the fraction of organic carbon. There is not a rigorous definition of the fraction of organic carbon (Foc). However, it can be thought of as the portion of the organic matter that is available to adsorb the organic contaminants of concern. The higher the organic carbon content, the more organic chemicals may be adsorbed to the soil and the less of those chemicals will be available to leach to the ground water. A nondefault option in the Risk Integrated System of Closure (RISC) is to use Foc in the Soil to Ground Water Partitioning Model to calculate a site specific migration to ground water closure level. In the Soil to Ground Water Partition Model, the coefficient, Kd, for organic compounds is the Foc multiplied by the chemical-specific soil organic carbon water partition coefficient, Koc.
    [Show full text]
  • Progress and Challenges in Using Stable Isotopes to Trace Plant Carbon and Water Relations Across Scales
    Biogeosciences, 9, 3083–3111, 2012 www.biogeosciences.net/9/3083/2012/ Biogeosciences doi:10.5194/bg-9-3083-2012 © Author(s) 2012. CC Attribution 3.0 License. Progress and challenges in using stable isotopes to trace plant carbon and water relations across scales C. Werner1,19, H. Schnyder2, M. Cuntz3, C. Keitel4, M. J. Zeeman5, T. E. Dawson6, F.-W. Badeck7, E. Brugnoli8, J. Ghashghaie9, T. E. E. Grams10, Z. E. Kayler11, M. Lakatos12, X. Lee13, C. Maguas´ 14, J. Ogee´ 15, K. G. Rascher1, R. T. W. Siegwolf16, S. Unger1, J. Welker17, L. Wingate18, and A. Gessler11 1Experimental and Systems Ecology, University Bielefeld, 33615 Bielefeld, Germany 2Lehrstuhl fur¨ Grunlandlehre,¨ Technische Universitat¨ Munchen,¨ 85350 Freising-Weihenstephan, Germany 3UFZ – Helmholtz Centre for Environmental Research, Permoserstr. 15, 04318 Leipzig, Germany 4University of Sydney, Faculty of Agriculture, Food and Natural Resources, 1 Central Avenue, Eveleigh, NSW 2015, Australia 5College of Oceanic and Atmospheric Sciences, Oregon State University, 104 COAS Admin Bldg, Corvallis (OR), USA 6Center for Isotope Biogeochemistry, Department of Integrative Biology, University of California, Berkeley, CA 94720, USA 7Potsdam Institute for Climate Impact Research (PIK) PF 60 12 03, 14412 Potsdam, Germany 8CNR – National Research Council of Italy – Institute of Agro-environmental and Forest Biology, via Marconi 2, 05010 Porano (TR), Italy 9Laboratoire d’Ecologie, Systematique´ et Evolution (ESE), CNRS AgroParisTech – UMR8079, Batimentˆ 362, Universite´ de Paris-Sud (XI), 91405 Orsay Cedex, France 10Ecophysiology of Plants, Department of Ecology and Ecosystem Management, Technische Universitat¨ Munchen,¨ Von-Carlowitz-Platz 2, 85354 Freising, Germany 11Institute for Landscape Biogeochemistry Leibniz-Zentrum fur¨ Agrarlandschaftsforschung (ZALF) e.V., Eberswalderstr.
    [Show full text]
  • Is Extraterrestrial Organic Matter Relevant to the Origin of Life on Earth?
    IS EXTRATERRESTRIAL ORGANIC MATTER RELEVANT TO THE ORIGIN OF LIFE ON EARTH? D. C. B. WHITTET Department of Physics, Applied Physics and Astronomy, Rensselaer Polytechnic Institute, Troy, NY 12180, U.S.A. (Received 19 August 1996) Abstract. I review the relative importance of internal and external sources of prebiotic molecules on Earth at the time of life's origin 3.7 Gyr ago. The ef®ciency of synthesis in the Earth's atmosphere was critically dependent on its oxidation state. If the early atmosphere was non-reducing and CO2- dominated, external delivery might have been the dominant source. Interplanetary dust grains and micrometeorites currently deliver carbonaceous matter to the Earth's surface at a rate of 3 5 7 10 kg/yr (equivalent to a biomass in 2 Gyr), but this may have been as high as 5 10 kg/yr (a biomass in only 10 Myr) during the epoch of late bombardment. Much of the incoming material is in the form of chemically inactive kerogens and amorphous carbon; but if the Earth once had a dense (10-bar) atmosphere, small comets rich in a variety of prebiotic molecules may have been suf®ciently air-braked to land non-destructively. Lingering uncertainties regarding the impact history of the Earth and the density and composition of its early atmosphere limit our ability to draw ®rm conclusions. 1. Introduction In at least one sense, a connection between the Universe at large and life in our small corner of it is inevitable. The hydrogen, carbon, nitrogen, oxygen, and other elements that make up our bodies and other living things were created billions of years ago in the interiors of stars and, in the case of hydrogen, in the the Big Bang itself (see Trimble, 1997, in this volume for an eloquent review).
    [Show full text]
  • Development of Compound-Specific Hydrogen Isotope Ratio Analysis Of
    Development of Compound-Specific Hydrogen Isotope Ratio Analysis of Biomarkers and their Application as New Proxy for Reconstruction of Palaeoenvironment and Palaeoclimate Entwicklung komponentenspezifischer Wasserstoffisotopen- Analyse von Biomarkern und deren Anwendung als neuartiger Proxy zur Rekonstruktion von Paläoumwelt und Paläoklima Dissertation zur Erlangung des akademischen Grades doctor rerum naturalium (Dr. rer. nat.) vorgelegt dem Rat der Chemisch-Geowissenschaftlichen Fakultät der Friedrich-Schiller-Universität Jena von Diplom Geologe Jens Radke geboren am 20.2.1967 in Bremerhaven Gutachter: 1. Prof.Dr.R.Gaupp 2. PD.Dr.G.Gleixner Tag der öffentlichen Verteidigung: 18.1.2006 Printed on 100% recycled paper (after ISO9706, 133 CIE, DIN 6738 LDK 24-85) Content Content ABSTRACT KURZFASSUNG ABBREVIATIONS 1 INTRODUCTION ......................................................................................................... 1 2 FRACTIONATION OF WATER ISOTOPES IN THE ENVIRONMENT ........................................ 2 2.1 Fractionation of water isotopes in the climate system......................................... 2 2.2 Fractionation of hydrogen in the biosynthesis of plant biomass.......................... 3 3 SEDIMENTS AND METHODS........................................................................................ 6 3.1 Sediment samples and stratigraphic framework ................................................. 6 3.2 Sample preparation for bulk and compound specific analysis ............................ 8 3.2.1 Sample
    [Show full text]
  • The Nature and Dynamics of Soil Organic Matter: Plant Inputs, Microbial Transformations, and Organic Matter Stabilization
    Soil Biology & Biochemistry 98 (2016) 109e126 Contents lists available at ScienceDirect Soil Biology & Biochemistry journal homepage: www.elsevier.com/locate/soilbio Review paper The nature and dynamics of soil organic matter: Plant inputs, microbial transformations, and organic matter stabilization Eldor A. Paul Natural Resource Ecology Laboratory and Department of Soil and Crop Sciences, Colorado State University, Fort Collins, CO 80523-1499, USA article info abstract Article history: This review covers historical perspectives, the role of plant inputs, and the nature and dynamics of soil Received 19 November 2015 organic matter (SOM), often known as humus. Information on turnover of organic matter components, Received in revised form the role of microbial products, and modeling of SOM, and tracer research should help us to anticipate 31 March 2016 what future research may answer today's challenges. Our globe's most important natural resource is best Accepted 1 April 2016 studied relative to its chemistry, dynamics, matrix interactions, and microbial transformations. Humus has similar, worldwide characteristics, but varies with abiotic controls, soil type, vegetation inputs and composition, and the soil biota. It contains carbohydrates, proteins, lipids, phenol-aromatics, protein- Keywords: Soil organic matter derived and cyclic nitrogenous compounds, and some still unknown compounds. Protection of trans- 13C formed plant residues and microbial products occurs through spatial inaccessibility-resource availability, 14C aggregation of mineral and organic constituents, and interactions with sesquioxides, cations, silts, and Plant residue decomposition clays. Tracers that became available in the mid-20th century made the study of SOM dynamics possible. Soil carbon dynamics Carbon dating identified resistant, often mineral-associated, materials to be thousands of years old, 13 Humus especially at depth in the profile.
    [Show full text]