Convergence to Cometary Panspermia
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Cometary Panspermia a Radical Theory of Life’S Cosmic Origin and Evolution …And Over 450 Articles, ~ 60 in Nature
35 books: Cosmic origins of life 1976-2020 Physical Sciences︱ Chandra Wickramasinghe Cometary panspermia A radical theory of life’s cosmic origin and evolution …And over 450 articles, ~ 60 in Nature he combined efforts of generations supporting panspermia continues to Prof Wickramasinghe argues that the seeds of all life (bacteria and viruses) Panspermia has been around may have arrived on Earth from space, and may indeed still be raining down some 100 years since the term of experts in multiple fields, accumulate (Wickramasinghe et al., 2018, to affect life on Earth today, a concept known as cometary panspermia. ‘primordial soup’, referring to Tincluding evolutionary biology, 2019; Steele et al., 2018). the primitive ocean of organic paleontology and geology, have painted material not-yet-assembled a fairly good, if far-from-complete, picture COMETARY PANSPERMIA – cultural conceptions of life dating back galactic wanderers are normal features have argued that these could not into living organisms, was first of how the first life on Earth progressed A SOLUTION? to the ideas of Aristotle, and that this of the cosmos. Comets are known to have been lofted from the Earth to a coined. The question of how from simple organisms to what we can The word ‘panspermia’ comes from the may be the source of some of the have significant water content as well height of 400km by any known process. life’s molecular building blocks see today. However, there is a crucial ancient Greek roots ‘sperma’ meaning more hostile resistance the idea of as organics, and their cores, kept warm Bacteria have also been found high in spontaneously assembled gap in mainstream understanding - seed, and ‘pan’, meaning all. -
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. -
Oxygen Isotopic Signature of CO2 from Combustion Processes
Atmos. Chem. Phys., 11, 1473–1490, 2011 www.atmos-chem-phys.net/11/1473/2011/ Atmospheric doi:10.5194/acp-11-1473-2011 Chemistry © Author(s) 2011. CC Attribution 3.0 License. and Physics Oxygen isotopic signature of CO2 from combustion processes M. Schumacher1,2,3, R. A. Werner3, H. A. J. Meijer1, H. G. Jansen1, W. A. Brand2, H. Geilmann2, and R. E. M. Neubert1 1Centre for Isotope Research, University of Groningen, Nijenborgh 4, 9747 AG Groningen, The Netherlands 2Max-Planck-Institute for Biogeochemistry, Hans-Knoell-Straße 10, 07745, Jena, Germany 3Institute of Plant Sciences, Swiss Federal Institute of Technology Zurich,¨ Universitatsstraße¨ 2, 8092 Zurich,¨ Switzerland Received: 21 July 2008 – Published in Atmos. Chem. Phys. Discuss.: 5 November 2008 Revised: 2 February 2011 – Accepted: 5 February 2011 – Published: 16 February 2011 Abstract. For a comprehensive understanding of the global (diffusive) transport of oxygen to the reaction zone as the carbon cycle precise knowledge of all processes is neces- cause of the isotope fractionation. The original total 18O sig- sary. Stable isotope (13C and 18O) abundances provide in- nature of the material appeared to have little influence, how- formation for the qualification and the quantification of the ever, a contribution of specific bio-chemical compounds to diverse source and sink processes. This study focuses on the individual combustion products released from the involved 18 δ O signature of CO2 from combustion processes, which material became obvious. are widely present both naturally (wild fires), and human in- duced (fossil fuel combustion, biomass burning) in the car- bon cycle. All these combustion processes use atmospheric 1 Introduction oxygen, of which the isotopic signature is assumed to be con- stant with time throughout the whole atmosphere. -
Investigations of Nuclear Forensic Signatures in Uranium Bearing Materials a Dissertation Submitted to the Graduate School of the University of Cincinnati
Investigations of Nuclear Forensic Signatures in Uranium Bearing Materials A dissertation submitted to the Graduate School of the University of Cincinnati in partial fulfillment of the requirements for the degree of Doctor of Philosophy (Ph.D) In the Department of Chemistry Of the McMicken College of Arts and Sciences By Lisa Ann Meyers B.S. Ohio Northern University 2009 August 2013 Committee Chairs: Thomas Beck, Ph.D. Apryll Stalcup, Ph.D. i Abstract Nuclear forensics is a multidisciplinary science that uses a variety of analytical methods and tools to investigate the physical, chemical, elemental, and isotopic characteristics of nuclear and radiological material. A collection of these characteristics is called signatures that aids in determining how, where and when the material was manufactured. Radiological chronometry (i.e., age dating) is an important tool in nuclear forensics that uses several methods to determine the length of time that has elapsed since a material was last purified. For example, the “age” of a uranium-bearing material is determined by measuring the ingrowth of 230Th from its parent, 234U. A piece of scrap uranium metal bar buried in the dirt floor of an old, abandoned metal rolling mill was analyzed using multi-collector inductively coupled plasma mass spectroscopy (MC-ICP- MS). The mill rolled uranium rods in the 1940s and 1950s. The age of the metal bar was determined to be 61 years at the time of analysis using the 230Th/234U chronometer, which corresponds to a purification date of July 1950 ± 1.5 years. Radiochronometry was determined for three different types of uranium metal samples. -
First Life in Primordial-Planet Oceans: the Biological Big Bang Gibson/Wickramasinghe/Schild First Life in Primordial-Planet Oceans: the Biological Big Bang
Journal of Cosmology First life in primordial-planet oceans: the biological big bang Gibson/Wickramasinghe/Schild First life in primordial-planet oceans: the biological big bang Carl H. Gibson 1,2 1 University of California San Diego, La Jolla, CA 92093-0411, USA [email protected], http://sdcc3.ucsd.edu/~ir118 N. Chandra Wickramasinghe3,4 3Cardiff Centre for Astrobiology, 24 Llwynypia Road, Lisvane, Cardiff CF14 0SY [email protected] Rudolph E. Schild5,6 5 Center for Astrophysics, 60 Garden Street, Cambridge, MA 02138, USA 6 [email protected] Abstract: A scenario is presented for the formation of first life in the universe based on hydro- gravitational-dynamics (HGD) cosmology. From HGD, the dark matter of galaxies is H-He gas dominated planets (primordial-fog-particle PFPs) in million solar mass clumps (protoglobularstar- cluster PGCs), which formed at the plasma to gas transition temperature 3000 K. Stars result from mergers of these hot-gas-planets. Over-accretion causes stars to explode as supernovae that scatter life-chemicals (C, N, O, P, S, Ca, Fe etc.) to other planets in PGC clumps and beyond. These chemicals were first collected gravitationally by merging PFPs to form H-saturated, high-pressure, dense oceans of critical-temperature 647 K water over iron-nickel cores at ~ 2 Myr. Stardust fertil- izes the formation of first life in a cosmic hot-ocean soup kitchen comprised of all planets and their moons in meteoric communication, > 10100 kg in total. Ocean freezing at 273 K slows this biologi- cal big bang at ~ 8 Myr. HGD cosmology confirms that the evolving seeds of life are scattered on intergalactic scales by Hoyle-Wickramasinghe cometary panspermia. -
Can Algal Photosynthetic Inorganic Carbon Isotope Fractionation Be Predicted in Lakes Using Existing Models?
Aquat. Sci. 68 (2006) 142–153 1015-1621/06/020142-12 DOI 10.1007/s00027-006-0818-5 Aquatic Sciences © Eawag, Dübendorf, 2006 Research Article Can algal photosynthetic inorganic carbon isotope fractionation be predicted in lakes using existing models? Darren L. Bade1,3,*, Michael L. Pace2, Jonathan J. Cole2 and Stephen R. Carpenter1 1 Center for Limnology, University of Wisconsin-Madison, USA 2 Institute of Ecosystem Studies, Millbrook, NY, USA 3 Present address: Institute of Ecosystem Studies, PO Box AB (65 Sharon Turnpike), Millbrook, NY 12545, USA Received: 30 June 2005; revised manuscript accepted: 7 December 2005 Abstract. Differential fractionation of inorganic carbon stable isotopes for studies ranging from food webs to stable isotopes during photosynthesis is an important paleolimnology. In our largest comparative study, values cause of variability in algal carbon isotope signatures. of δ13C-POC ranged from –35.1 ‰ to –21.3 ‰. Using Several physiological models have been proposed to ex- several methods to obtain an algal isotopic signature, we ε plain algal photosynthetic fractionation factors ( p). These found high variability in fractionation among lakes. There ε models generally consider CO2 concentration, growth was no relationship between p and one of the most im- rate, or cell morphometry and have been supported by portant predictors in existing models, pCO2. A whole-lake empirical evidence from laboratory cultures. Here, we inorganic 13C addition was used to create distinct algal ε explore the applicability of these models to a broad range isotope signatures to aid in examining p. Measurements of lakes with mixed phytoplankton communities. Under- and a statistical model from the isotope addition revealed standing this fractionation is necessary for using carbon that algal fractionation was often low (0 – 15 ‰). -
Sources of Variation in the Stable Isotopic Composition of Plants*
CHAPTER 2 Sources of variation in the stable isotopic composition of plants* JOHN D. MARSHALL, J. RENÉE BROOKS, AND KATE LAJTHA Introduction The use of stable isotopes of carbon, nitrogen, oxygen, and hydrogen to study physiological processes has increased exponentially in the past three decades. When Harmon Craig (1953, 1954), a geochemist and early pioneer of natural abundance stable isotopes, fi rst measured isotopic values of plant materials, he found that plants tended to have a fairly narrow δ13C range of −25 to −35‰. In these initial surveys, he was unable to fi nd large taxonomic or environmental effects on these values. Since that time ecologists have identi- fi ed clear isotopic signatures based not only on different photosynthetic pathways, but also on ecophysiological differences, such as photosynthetic water-use effi ciency (WUE) and sources of water and nitrogen used. As large empirical databases have accumulated and our theoretical understanding of isotopic composition has improved, scientists have continued to discover mismatches between theoretical and observed values, as well as confounding effects from sources and factors not previously considered. In the best tradi- tion of science, these discoveries have led to important new insights into physiological or ecological processes, as well as new uses of stable isotopes in plant ecophysiology. This chapter reviews the most common applications of stable isotope analysis in plant ecophysiology. Carbon isotopes Photosynthetic pathways 13 Plants contain less C than the atmospheric CO2 on which they rely for photosynthesis. They are therefore “depleted” of 13C relative to the atmo- sphere. This depletion is caused by enzymatic and physical processes that discriminate against 13C in favor of 12C. -
Evidence to Clinch the Theory of Extraterrestrial Life
obiolog str y & f A O u o l t a r e n a Chandra Wickramasinghe, Astrobiol Outreach 2015, 3:2 r c u h o J Journal of Astrobiology & Outreach DOI: 10.4172/2332-2519.1000e107 ISSN: 2332-2519 EditorialResearch Article OpenOpen Access Access Evidence to Clinch the Theory of Extraterrestrial Life Chandra Wickramasinghe N1,2,3 1Buckingham Centre for Astrobiology (BCAB), Buckingham University, UK 2Institute for the Study of Panspermia and Astroeconomics, Gifu, Japan 3University of Peradeniya, Peradeniya, Sri Lanka New data may serve to bring about the long overdue paradigm probe) appears to have been finally vindicated, both by the discovery of shift from theories of Earth-centred life to life being a truly cosmic organic molecules on the surface, and more dramatically by the recent phenomenon. The theory that bacteria and viruses similar to those discovery of time-variable spikes in methane observed by the Curiosity on Earth exist in comets, other planets and generally throughout the galaxy was developed as a serious scientific discipline from the early 1980’s [1-4]. Throughout the past three decades this idea has often been Relectivity Spectrum the subject of criticism, denial or even ridicule. Even though many discoveries in astronomy, geology and biology continued to provide supportive evidence for the theory of cosmic life, the rival theory of Earth-centered biology has remained deeply rooted in scientific culture. However, several recent developments are beginning to strain the credibility of the standard point of view. The great abundance of highly complex organic molecules in interstellar clouds [5], the plentiful existence of habitable planets in the galaxy numbering over 100 billion and separated one from another just by a few light years [6], the extreme space-survival properties of bacteria and viruses -make it exceedingly difficult to avoid the conclusion that the entire galaxy is a single connected biosphere. -
Lead Isotope Determinations by Inductively-Coupled Plasma Mass Spectrometry (ICP-MS): Potential of Sector Field Instruments
NGU-BULL 436, 2000 - PAGE 203 Lead isotope determinations by inductively-coupled plasma mass spectrometry (ICP-MS): potential of sector field instruments BELINDA FLEM, ANDREAS GRIMSTVEDT & NIGEL COOK Flem, B., Grimstvedt, A. & Cook, N.J. 2000: Lead isotope determinations by inductively-coupled plasma mass spectrometry (ICP-MS): potential of sector field instruments. Norges geologiske undersøkelse Bulletin 436, 203-207. Lead isotope measurements have been carried out using a high-resolution inductively-coupled plasma mass spectrometer (Finnigan MAT ELEMENT, configured with CD-1 option). The method can be applied to all types of geological samples brought into solution form. Three common lead standards are used for documentation of the method. Detection limits for 204Pb, 206Pb, 207Pb and 208Pb lie between 0.124 and 2.86 pg ml-1. Optimisation of scanning conditions at a count rate of approximately 200,000 cps for 206Pb and 207Pb, led to a relative standard deviation of 0.05% for the mean 207Pb/206Pb isotope ratio, based on 15 consecutive measurements. The method can be routinely applied to gain geochronological and petrological data for genetic studies of mineral deposits, including deposits of industrial minerals. Because of space charge effects in the skimmer cone region and mass-dependent sensitivity of the mass spectrometer, the measured intensity ratio of samples must generally be calibrated using external or internal standards of known isotope ratios to correct for mass biases and mass fractionation. Belinda Flem, Andreas Grimstvedt & Nigel Cook, Geological Survey of Norway, N-7491 Trondheim, Norway. which the Pb isotope systematics have been reset. The appli- Introduction cation of Pb isotopes for geochronology has declined in pop- Geochronological, isotopic and petrological data are impor- ularity in recent years. -
Lead Isotopes, Metal Sources, Smelters, Precipitation, Toxic Release Inventory
Coupling Meteorology, Metal Concentrations, and Pb Isotopes for Source Attribution in Archived Precipitation Samples Joseph R. Graneya*, Matthew S. Landisb aGeological Sciences and Environmental Studies, Binghamton University, Binghamton, NY USA 13902 bU.S. EPA Office of Research and Development, Research Triangle Park, NC USA 27709 *Corresponding author: Telephone: 607 777 6347 Fax: 607 777 2288 Postal Address: Department of Geological Sciences and Environmental Studies P.O. Box 6000 Binghamton University Binghamton, NY 13902-6000 E-mail address: [email protected] 1 Abstract A technique that couples lead (Pb) isotopes and multi-element concentrations with meteorological analysis was used to assess source contributions to precipitation samples at the Bondville, Illinois USA National Trends Network (NTN) site. Precipitation samples collected over a 16 month period (July 1994 - October 1995) at Bondville were parsed into six unique meteorological flow regimes using a minimum variance clustering technique on back trajectory endpoints. Pb isotope ratios and multi-element concentrations were measured using high resolution inductively coupled plasma – sector field mass spectrometry (ICP-SFMS) on the archived precipitation samples. Bondville is located in central Illinois, ~ 250 km downwind from Pb smelters in southeast Missouri. The Mississippi Valley Type ore deposits in Missouri provided a unique multi-element and Pb isotope fingerprint for smelter emissions which could be contrasted to industrial emissions from the Chicago and Indianapolis urban areas (~ 125 km north and east, of Bondville respectively); and regional emissions from electric utility facilities. Significant differences in Pb isotopes and element concentrations in precipitation varied according to the meteorological clusters. Industrial sources from urban areas, and thorogenic Pb from coal use, could be differentiated from smelter emissions from Missouri by coupling Pb isotope ratios with multi-element concentrations in precipitation. -
Comment on Liquid Water and Life on Mars
obiolog str y & f A O u o l t a r e n Chandra Wickramasinghe, Astrobiol Outreach 2015, 3:5 a r c u h o J Journal of Astrobiology & Outreach DOI: 10.4172/2332-2519.1000e111 ISSN: 2332-2519 Editorial Open Access Comment on Liquid Water and Life on Mars Chandra Wickramasinghe N*,1,2,3 1Buckingham Centre for Astrobiology (BCAB), Buckingham University, UK 2Institute for the Study of Panspermia and Astroeconomics, Gifu, Japan 3University of Peradeniya, Peradeniya, Sri Lanka *Corresponding author: Wickramasinghe NC, Buckingham Centre for Astrobiology (BCAB), Buckingham University, UK, Tel: +44-777-838-9243; E-mail: [email protected] Rec date: October 01, 2015; Acc date: October 05, 2015; Pub date: October 07, 2015 Copyright: © 2015 Chandra Wickramasinghe N, et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited. Editorial but it was quickly rejected on grounds of alleged uncertainties of interpretation, as well as the lack of organic molecules detectable at the The announcement this week of the detection of liquid water on landing site. A year later, in1977, a major dust storm enveloped the Mars has come close on 4 decades after the arrival of the first Viking planet and H. Abadi and the present writer reported evidence of landers at the red planet in 1976 [1]. The temperatures at the two absorption properties of the Martian dust that was consistent with the original landing sites of the Viking spacecraft in 1976 ranged between a presence of aromatic hydrocarbons [3]. -
5 Books by Chandra Wickramasinghe
World Scientific proudly presents books by Chandra Wickramasinghe THE SEARCH FOR OUR COSMIC ANCESTRY by Chandra Wickramasinghe (Buckingham Centre for Astrobiology, UK) “The author is today’s foremost expert on panspermia, having inherited that mantle from the iconic astronomer of the 20th century Sir Fred Hoyle who, with Wickramasinghe as his pupil, strongly re- introduced the subject in the early 1970’s. He makes a compelling case for panspermia conveying a cosmic imperative for biology.” Gilbert V Levin Principal Investigator of NASA’s Mars Viking Mission of 1976 Discoverer of evdience for Microbial Life on Mars Arizona State University “The book is accessible to those interested in an appreciation of a central question that spans VINDICATION OF COSMIC all ages, and scientists and science students, who are seeking coverage of this pioneering BIOLOGY subject matter. The historical approach to the subject will be appreciated by readers. The book will take you on an intellectual trek and can transform how you think about humans and the Tribute to Sir Fred Hoyle (1915 – 2001) universe. Hopefully it will encourage the next generation of scholars to continue seeking an edited by Nalin Chandra Wickramasinghe understanding of the origin of life, one of the most profound challenges for humanity.” (University of Buckingham, UK) Professor J T Trevors In the year 2015, 100 years after Fred Hoyle was University of Guelph, Canada born, the ideas relating to the cosmic origins of life 216pp Dec 2014 are slowly gaining credence in scientific circles. 978-981-4616-96-6 US$64 £42 Once regarded as outrageous heresy, evidence 978-981-4616-97-3(pbk) US$38 £25 from a variety of disciplines — astronomy, geology, biology — is converging to support these once heretical ideas.