A Guide to Using Compound-Specific Stable Isotope Analysis to Study the Fates of Molecules in Organisms and Ecosystems
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Stable Isotope Methods in Biological and Ecological Studies of Arthropods
eea_572.fm Page 3 Tuesday, June 12, 2007 4:17 PM DOI: 10.1111/j.1570-7458.2007.00572.x Blackwell Publishing Ltd MINI REVIEW Stable isotope methods in biological and ecological studies of arthropods CORE Rebecca Hood-Nowotny1* & Bart G. J. Knols1,2 Metadata, citation and similar papers at core.ac.uk Provided by Wageningen University & Research Publications 1International Atomic Energy Agency (IAEA), Agency’s Laboratories Seibersdorf, A-2444 Seibersdorf, Austria, 2Laboratory of Entomology, Wageningen University and Research Centre, P.O. Box 8031, 6700 EH Wageningen, The Netherlands Accepted: 13 February 2007 Key words: marking, labelling, enrichment, natural abundance, resource turnover, 13-carbon, 15-nitrogen, 18-oxygen, deuterium, mass spectrometry Abstract This is an eclectic review and analysis of contemporary and promising stable isotope methodologies to study the biology and ecology of arthropods. It is augmented with literature from other disciplines, indicative of the potential for knowledge transfer. It is demonstrated that stable isotopes can be used to understand fundamental processes in the biology and ecology of arthropods, which range from nutrition and resource allocation to dispersal, food-web structure, predation, etc. It is concluded that falling costs and reduced complexity of isotope analysis, besides the emergence of new analytical methods, are likely to improve access to isotope technology for arthropod studies still further. Stable isotopes pose no environmental threat and do not change the chemistry or biology of the target organism or system. These therefore represent ideal tracers for field and ecophysiological studies, thereby avoiding reductionist experimentation and encouraging more holistic approaches. Con- sidering (i) the ease with which insects and other arthropods can be marked, (ii) minimal impact of the label on their behaviour, physiology, and ecology, and (iii) environmental safety, we advocate more widespread application of stable isotope technology in arthropod studies and present a variety of potential uses. -
Stable Isotope Fingerprinting: a Novel Method for Identifying Plant, Fungal
Ecology, 00(0), 0000, pp. 000–000 Ó 0000 by the Ecological Society of America Stable isotope fingerprinting: a novel method for identifying plant, fungal, or bacterial origins of amino acids 1 THOMAS LARSEN,D.LEE TAYLOR,MARY BETH LEIGH, AND DIANE M. O’BRIEN Institute of Arctic Biology and Department of Biology and Wildlife, University of Alaska, Fairbanks, Alaska 99775-7000 USA Abstract. Amino acids play an important role in ecology as essential nutrients for animals and as currencies in symbiotic associations. Here we present a new approach to tracing the origins of amino acids by identifying unique patterns of carbon isotope signatures generated by amino acid synthesis in plants, fungi, and bacteria (‘‘13C fingerprints’’). We measured 13 amino acid d C from 10 C3 plants, 13 fungi, and 10 bacteria collected and isolated from a boreal forest in interior Alaska, USA, using gas chromatography-combustion-isotope ratio mass spectrometry (GC-C-IRMS). Microorganisms were cultured under amino-acid-free conditions and identified based on DNA sequences. Bacteria, fungi, and plants generated consistent, unique 13C fingerprints based on the more complex amino acids (five or more biosynthetic steps) that are classified as essential for animals. Linear discriminant analysis classified all samples correctly with .99% certainty and correctly classified nearly all insect samples from a previous study by diet. Our results suggest that 13C fingerprints of amino acids could provide a powerful in situ assay of the biosynthetic sources of amino acids and a potential new tool for understanding nutritional linkages in food webs. Key words: Alaska, USA; compound-specific stable isotope analysis; d13C; essential amino acids; eukaryotes; gas chromatography-combustion-isotope ratio mass spectrometry (GC-C-IRMS); prokaryotes. -
CV Seth Newsome.Pdf
Seth D. Newsome University of New Mexico Associate Professor, Department of Biology Associate Director, Center for Stable Isotopes 190 Castetter Hall Albuquerque, NM 87131 USA [email protected] http://sethnewsome.org Research Interests Animal Ecology, Animal Eco-Physiology, Historical Ecology, Conservation Biology Education 2000–2005 Ph.D., University of California Santa Cruz (Santa Cruz, CA) Earth & Planetary Sciences Department 1995–1999 B.A., Dartmouth College (Hanover, NH) Earth Sciences Department Positions & Professional Development 2018– Associate Professor, Biology Department, University of New Mexico (Albuquerque, NM) 2014– Associate Director, University of New Mexico Center for Stable Isotopes 2013–2018 Assistant Professor, Biology Department, University of New Mexico (Albuquerque, NM) 2009–2012 Post-Doctoral Research Scientist, University of Wyoming (Laramie, WY) Research focused on (1) using compound specific stable isotope analysis to quantify protein routing in mammals, birds and fish; (2) characterizing the ecology of an adaptive radiation in a group of South American songbirds via biochemical, physiological, and genetic tools. Advisors: Drs. Carlos Martinez del Rio and David G. Williams 2006–2009 Post-Doctoral Research Scientist, Carnegie Institution of Washington (Washington, DC) Research focused on (1) development of stable isotope methods to assess ecological niche and eco-physiological variation, foraging specialization, and dispersal characteristics of mammals and birds; (2) human impacts on ecosystem change in Australia and southern California. Advisor: Dr. Marilyn L. Fogel 2000–2005 Ph.D. Candidate, UC-Santa Cruz (Santa Cruz, CA) Research focused on historic and prehistoric ecology of marine mammals, with emphasis on the northern fur seal in the northeast Pacific Ocean. Advisor: Dr. Paul L. Koch 2000 Senior Lab Technician, Lawrence Berkeley National Laboratory (Berkeley, CA) Managed stable isotope facility and conducted research using isotopic tracers to track fluid and contaminant migration through sediments and groundwater. -
Measurement of the Isotopic Composition of Dissolved Iron in the Open Ocean F
Measurement of the isotopic composition of dissolved iron in the open ocean F. Lacan, Amandine Radic, Catherine Jeandel, Franck Poitrasson, Géraldine Sarthou, Catherine Pradoux, Remi Freydier To cite this version: F. Lacan, Amandine Radic, Catherine Jeandel, Franck Poitrasson, Géraldine Sarthou, et al.. Measure- ment of the isotopic composition of dissolved iron in the open ocean. Geophysical Research Letters, American Geophysical Union, 2008, pp.L24610. 10.1029/2008GL035841. hal-00399111 HAL Id: hal-00399111 https://hal.archives-ouvertes.fr/hal-00399111 Submitted on 15 Jul 2009 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. 1 Measurement of the Isotopic Composition of dissolved Iron in the Open Ocean 2 3 Lacan1 F., Radic1 A., Jeandel1 C., Poitrasson2 F., Sarthou3 G., Pradoux1 C., Freydier2 R. 4 5 1: CNRS, LEGOS, UMR5566, CNRS-CNES-IRD-UPS, Observatoire Midi-Pyrénées, 18, Av. 6 E. Belin, 31400 Toulouse, France. 7 2: LMTG, CNRS-UPS-IRD, 14-16, avenue Edouard Belin, 31400 Toulouse, France. 8 3: LEMAR, UMR CNRS 6539, IUEM, Technopole Brest Iroise, Place Nicolas Copernic, 9 29280 Plouzané, France. 10 11 Paper published in Geophysical Research Letters (2008) L24610. 12 We acknowledge Geophysical Research Letters and the American Geophysical Union copyright 13 14 This work demonstrates for the first time the feasibility of the measurement of the isotopic 15 composition of dissolved iron in seawater for a typical open ocean Fe concentration range 16 (0.1-1nM). -
Effect of Cover Crop on Carbon Distribution in Size and Density
Article Effect of Cover Crop on Carbon Distribution in Size and Density Separated Soil Aggregates Michael V. Schaefer 1,2 , Nathaniel A. Bogie 3,4 , Daniel Rath 5, Alison R. Marklein 1,6, Abdi Garniwan 1, Thomas Haensel 1, Ying Lin 7, Claudia C. Avila 1 , Peter S. Nico 6, Kate M. Scow 5,8, Eoin L. Brodie 6,9, William J. Riley 6 , Marilyn L. Fogel 7,10, Asmeret Asefaw Berhe 3 , Teamrat A. Ghezzehei 3, Sanjai Parikh 5 , Marco Keiluweit 11 and Samantha C. Ying 1,12,* 1 Department of Environmental Sciences, University of California, Riverside, CA 92521; USA; [email protected] (M.V.S.); [email protected] (A.R.M.); [email protected] (A.G.); [email protected] (T.H.); [email protected] (C.C.A.) 2 Pacific Basin Research Center, Soka University of America, Laguna Hills, CA 92656, USA 3 Environmental System, University of California, Merced, CA 95343, USA; [email protected] (N.A.B.); [email protected] (A.A.B.); [email protected] (T.A.G.) 4 Geology Department, San Jose State University, San Jose, CA 95192, USA 5 Department of Land, Air, and Water Resource, University of California, Davis, CA 95616, USA; [email protected] (D.R.); [email protected] (K.M.S.); [email protected] (S.P.) 6 Earth and Environmental Sciences, Lawrence Berkeley National Laboratory, Berkeley, CA 94720, USA; [email protected] (P.S.N.); [email protected] (E.L.B.); [email protected] (W.J.R.) 7 Environmental Dynamics and GeoEcology Institute, University of California, Riverside, CA 92521, USA; [email protected] (Y.L.); [email protected] (M.L.F.) 8 Agricultural -
NASA Astrobiology Institute 2018 Annual Science Report
A National Aeronautics and Space Administration 2018 Annual Science Report Table of Contents 2018 at the NAI 1 NAI 2018 Teams 2 2018 Team Reports The Evolution of Prebiotic Chemical Complexity and the Organic Inventory 6 of Protoplanetary Disk and Primordial Planets Lead Institution: NASA Ames Research Center Reliving the Past: Experimental Evolution of Major Transitions 18 Lead Institution: Georgia Institute of Technology Origin and Evolution of Organics and Water in Planetary Systems 34 Lead Institution: NASA Goddard Space Flight Center Icy Worlds: Astrobiology at the Water-Rock Interface and Beyond 46 Lead Institution: NASA Jet Propulsion Laboratory Habitability of Hydrocarbon Worlds: Titan and Beyond 60 Lead Institution: NASA Jet Propulsion Laboratory The Origins of Molecules in Diverse Space and Planetary Environments 72 and Their Intramolecular Isotope Signatures Lead Institution: Pennsylvania State University ENIGMA: Evolution of Nanomachines in Geospheres and Microbial Ancestors 80 Lead Institution: Rutgers University Changing Planetary Environments and the Fingerprints of Life 88 Lead Institution: SETI Institute Alternative Earths 100 Lead Institution: University of California, Riverside Rock Powered Life 120 Lead Institution: University of Colorado Boulder NASA Astrobiology Institute iii Annual Report 2018 2018 at the NAI In 2018, the NASA Astrobiology Program announced a plan to transition to a new structure of Research Coordination Networks, RCNs, and simultaneously planned the termination of the NASA Astrobiology Institute -
Stable Isotope Analyses Differentiate Between Different Trophic Pathways Supporting Rocky-Reef Fishes
MARINE ECOLOGY PROGRESS SERIES Vol. 95: 19-24, 1993 Published May 19 Mar. Ecol. Prog. Ser. Stable isotope analyses differentiate between different trophic pathways supporting rocky-reef fishes Carrie J. Thomas, Lawrence B. Cahoon Biological Sciences, University of North Carolina at Wilmington, Wilmington, North Carolina 28403, USA ABSTRACT: Stable isotope analyses of 5 reef-associated fishes, Decapterus punctatus. Diplodus holbrooki, Rhornboplites aurorubens. Pagrus pagrus, and Haernulon aurolineatum, were conducted to determine the ability of stable isotope analysis to distinguish among the species and the trophic pathways that support them. Analyses of F13C, 615~,and 634~from white swimming muscle yielded significant differences between species. Multiple stable isotope signatures of these 5 species indicated that at least 2 trophic pathways, one planktonic and one benthic, supported these reef-associated species. Variability of isotopic signatures within species was largely a result of collection site differ- ences. 8l3C and 615N values inchcated that all fishes were feeding at similar trophic levels. P4S values proved to be useful supplements to carbon and nitrogen isotope values in separating species by signature. INTRODUCTION sandy areas (Hales 1987, Donaldson 1991). Other fishes, such as Diplodus holbrooki (spottail pinfish), Total primary production on the continental shelf off feed upon benthic macroalgae and associated inverte- North Carolina, USA, is supported by 3 sources: phyto- brates (Hay & Sutherland 1988, Pike 1991). Finally, plankton, benthic macroalgae, and benthic micro- demersal zooplankton feed on benthic microalgae algae. Cahoon et al. (1990) found benthic microalgal (Tronzo 1989).Demersal zooplankton are in turn a food biomass frequently equalled or exceeded integrated item for fishes such as Haemulon aurolineatum phytoplankton biomass across the shelf. -
Ocean Ecogeochemistry a Review
Oceanography and Marine Biology: An Annual Review, 2013, 51, 327-374 © Roger N. Hughes, David Hughes, and I. Philip Smith, Editors Taylor & Francis OcEaN EcOgeochemistry: a review KElton w. mcmahon1,2,3, Li Ling HamaDy1 & SImon R. ThorrolD1 1Biology Department, Woods Hole Oceanographic Institution, MS50, Woods Hole, MA 02543, USA E- mail: [email protected] (corresponding author), [email protected] 2Red Sea Research Center, King Abdullah University of Science and Technology, Thuwal, Kingdom of Saudi Arabia E- mail: [email protected] 3Ocean Sciences Department, University of California-Santa Cruz, SantaCruz, CA 95064, USA animal movements and the acquisition and allocation of resources provide mechanisms for indi- vidual behavioural traits to propagate through population, community and ecosystem levels of biological organization. Recent developments in analytical geochemistry have provided ecolo- gists with new opportunities to examine movements and trophic dynamics and their subsequent influence on the structure and functioning of animal communities. we refer to this approach as ecogeochemistry—the application of geochemical techniques to fundamental questions in popula- tion and community ecology. we used meta- analyses of published data to construct δ2H, δ13c, δ15N, δ18O and Δ14c isoscapes throughout the world’s oceans. These maps reveal substantial spatial vari- ability in stable isotope values on regional and ocean- basin scales. we summarize distributions of dissolved metals commonly assayed in the calcified tissues of marine animals. Finally, we review stable isotope analysis (SIa) of amino acids and fatty acids. These analyses overcome many of the problems that prevent bulk SIa from providing sufficient geographic or trophic resolution in marine applications. we expect that ecologists will increasingly use ecogeochemistry approaches to estimate animal movements and trace nutrient pathways in ocean food webs. -
Ocean Primary Production
Learning Ocean Science through Ocean Exploration Section 6 Ocean Primary Production Photosynthesis very ecosystem requires an input of energy. The Esource varies with the system. In the majority of ocean ecosystems the source of energy is sunlight that drives photosynthesis done by micro- (phytoplankton) or macro- (seaweeds) algae, green plants, or photosynthetic blue-green or purple bacteria. These organisms produce ecosystem food that supports the food chain, hence they are referred to as primary producers. The balanced equation for photosynthesis that is correct, but seldom used, is 6CO2 + 12H2O = C6H12O6 + 6H2O + 6O2. Water appears on both sides of the equation because the water molecule is split, and new water molecules are made in the process. When the correct equation for photosynthe- sis is used, it is easier to see the similarities with chemo- synthesis in which water is also a product. Systems Lacking There are some ecosystems that depend on primary Primary Producers production from other ecosystems. Many streams have few primary producers and are dependent on the leaves from surrounding forests as a source of food that supports the stream food chain. Snow fields in the high mountains and sand dunes in the desert depend on food blown in from areas that support primary production. The oceans below the photic zone are a vast space, largely dependent on food from photosynthetic primary producers living in the sunlit waters above. Food sinks to the bottom in the form of dead organisms and bacteria. It is as small as marine snow—tiny clumps of bacteria and decomposing microalgae—and as large as an occasional bonanza—a dead whale. -
Late Archean Rise of Aerobic Microbial Ecosystems
Late Archean rise of aerobic microbial ecosystems Jennifer L. Eigenbrode*†‡ and Katherine H. Freeman* *Department of Geosciences and Penn State Astrobiology Research Center, Pennsylvania State University, University Park, PA 16802; and †Geophysical Laboratory, Carnegie Institution of Washington, Washington, DC 20015 Communicated by John M. Hayes, Woods Hole Oceanographic Institution, Woods Hole, MA, August 30, 2006 (received for review January 18, 2006) We report the 13C content of preserved organic carbon for a 150 zone. Thus, we focus this work on relative water-column depth, million-year section of late Archean shallow and deepwater sedi- and we present kerogen ␦13C data for a well preserved, 150 ments of the Hamersley Province in Western Australia. We find a million-year stratigraphic section from the late Archean, in 13C enrichment of Ϸ10‰ in organic carbon of post-2.7-billion-year- which we distinguish isotopic signatures of shallow versus deep- old shallow-water carbonate rocks relative to deepwater sedi- water sedimentary environments. We specifically evaluate this ments. The shallow-water organic-carbon 13C content has a 29‰ isotopic record after the pronounced depletion in organic 13C range in values (؊57 to ؊28‰), and it contrasts with the less signatures at 2.72 Ga, and we compare it with published isotopic variable but strongly 13C-depleted (؊40 to ؊45‰) organic carbon records from other regions to assess global changes in microbial in deepwater sediments. The 13C enrichment likely represents ecosystems during this important time. microbial habitats not as strongly influenced by assimilation of methane or other 13C-depleted substrates. We propose that con- Results tinued oxidation of shallow settings favored the expansion of Kerogen ␦13C values for 175 samples from a 2.72- to 2.57-Ga aerobic ecosystems and respiring organisms, and, as a result, section in the Hamersley Province, Western Australia, vary isotopic signatures of preserved organic carbon in shallow settings between Ϫ57‰ and Ϫ28‰ (Fig. -
Online Resources for Stable Isotope Laboratory Education and Training and Ecological Applications
Online Resources for Stable Isotope Laboratory Education and Training and Ecological Applications Lisandra Trine, J. Renée Brooks, and William Rugh Ecological Effects Branch Pacific Ecological Systems Division Corvallis, OR, 97330 Introduction EPA’s Integrated Stable Isotope Research Facility developed a table of online educational and training resources for stable isotope analysis methods and ecological applications. This table was compiled from broad input from the stable isotope geochemistry community on the ISOGEOCHEM list serve. This resource material provides continued training of EPA and other staff in the greater stable isotope research group during situations when they may not have access to the laboratories. For any comments or recommendations to incorporate into this general listing, email [email protected]. Notice/Disclaimer Statement The views expressed in this document are those of the author(s) and do not necessarily represent the views or policies of the U.S. Environmental Protection Agency. Any mention of trade names, products, or services does not imply an endorsement by the U.S. Government or the U.S. Environmental Protection Agency. The EPA does not endorse any commercial products, services, or enterprises. This document provides links to non-EPA web sites that provide additional information about this topic. EPA cannot attest to the accuracy of information on that non-EPA page. Copywrite laws must be considered for all material in these links. Providing links to a non- EPA Web site is not an endorsement of the other site or the information it contains by EPA or any of its employees. Also, be aware that the privacy protection provided on the EPA.gov domain (see Privacy and Security Notice) may not be available at the external link. -
Stable Isotope Diagrams of Freshwater Food Webs
NOTES AND COMMENTS 2293 i.e., m, = d,ls,, where d, is the number of deaths during mortality rates, which have been described above, are the time interval i, and s, is the number of survivors approaches that can enable very short periods of time at the midpoint of the time interval i. to be identified when mortality risks differ substantially Gehan ( 1969) has derived an equation which enables between sets of plants. Although for the field ecologist the variance of the midpoint age-specific mortality to inferences about the causes of plant death will always be determined: be easier than proof, the ability to compare mortality rates over very short time intervals will allow more accurate interpretation of the causes of mortality and Var[m,] = (:/ {1 - ( ~')l promote a sharper understanding of the tolerance lim its of species in the field. d, . where q, = -, I.e., s, Acknowledgments: This work was undertaken while K. D. Booth was in receipt of a Science and Engineering 2 , (m,)' 2 {. ( m,' ) } Research Council studentship. We gratefully acknowl Var[m,] = T 1 - . 2 edge the helpful comments of four referees, including David Pyke and Dolph Schluter. This formula may be used to calculate 95% confidence intervals around m, values (Fig. 1), aiding the com Literature Cited parison of survivorship patterns in the cohorts (Lee Gehan, E. A. 1969. Estimating survival functions from the 1980). When this procedure is applied to the data of life table. Journal of Chronic Diseases 21:629-644. Pyke and Thompson ( 1986), the analysis shows that Lee, E. T.