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2018 | OriginalPaper | Buchkapitel

3. What Is the Ultimate Ancestor? Evidence from Fossils and Gene Analyses

verfasst von : Hiromoto Nakazawa

Erschienen in: Darwinian Evolution of Molecules

Verlag: Springer Singapore

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Abstract

The current results of science from two research fields approaching the origin of life are reviewed. We will see how close we are to identifying the origin of life by following the biological evolutionary phylogenetic tree provided by evidence from the fossil record and the research results that suggest an “ultimate ancestor” by the analysis of biomolecules, such as genes and proteins.

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Vorheriges Kapitel Why Did Life Generate? Why Does Life Evolve? Physical Perspective of the Origin of Life

Nächstes Kapitel “Miller–Urey Experiment” in the Recent Picture of the Early Earth

Near Edge X-ray Absorption Fine Structure (NEXAFS).

Minute Portion Infrared Raman Spectroscopy.

Secondary ion mass spectrometry is a technique used to analyze the composition of solid surfaces by sputtering the surface of the specimen with a focused primary ion beam and collecting and analyzing ejected secondary ions.

There are four stable isotopes in sulfur atoms, i.e., ³²S, ³³S, ³⁴S, and ³⁵S in the ratio 95.02, 0.75, 4.21, and 0.02%, respectively. Sulfur-reducing bacteria tend to ingest sulfate ions containing “light sulfur (³²S)” so that pyrite formed is enriched in the light sulfur isotopes. Because the isotope ratio of “heavy sulfur” (³⁴S) is less than 2/1000 ~ 46/1000, the pyrite is estimated to be formed after bacterial metabolism.

These are the chemoautotrophs of the chemosynthetic bacteria. They use abiotic hydrogen for their metabolism. Sulfur-reducing bacteria living presently in sludge are chemoheterotrophs since they use biotic hydrogen of bio-organic molecules. Thus, they are a different kind of “sulfur-reducing bacteria” than those described here.

Ernst Heinrich Philipp August Höckel (1834–1919).

Barghoorn ES, Tyler SA (1965) Microorganism from Gunflint chert. Science 147:563–575CrossRef

Brasier MD, Green OR, Jephcoat AP, Kleppe AK, Van Kranendonk MJ, Lindsay JF, Steel A, Grassineau NV (2002) Questioning the evidence for Earth’s oldest fossils. Nature 416:76–81CrossRef

Cloud R (1965) Significance of the Gunflint (Precambrian) microflora. Science 148:27–45CrossRef

Dalton R (2002) Microfossils: squaring up over ancient life. Nature 417:782–784CrossRef

Doolittle WF (1999) Phylogenetic classification and the universal tree. Science 284:2124–2128CrossRef

Environmental Ministry of Japan (2010) White paper on the environment: Chapter 3 crisis of biodiversity and our lives, p. 68, www.env.go.jp/policy/hakusho/h22/pdf.html

Erb TJ, Kiefer P, Hattendorf B, Günter D, Vorholt JA (2012) GFA-1 is an arsenate-resistant, phosphate-dependent organism. Science 337:467–470CrossRef

Fedo CM, Whitehouse MJ (2002) Metasomatic origin of quartz-pyroxene rock, Akilia, Greenland, and implications for Earth’s earliest life. Science 296:1448–1452CrossRef

Garcia-Ruiz JM, Hyde ST, Carnerup AM, Christy AG, Van Kranendonk MJ, Welham NJ (2003) Self-assembled silica-carbonate structure and detection of ancient microfossils. Science 302:1194–1197CrossRef

Höckel EH (1866) Generelle Morphologie der Organissmen, Allgemeine Entwickelungsgeschichte, Druck und Verlag von Georg Reimen. Berlin

House CH, Oehler DZ, Sugitani K, Miura K (2013) Carbon isotopic analyses of ca. 3.0 Ga microstructures imply planktonic autotrophs inhabited Earth’s early oceans. Geology 41:651–654CrossRef

Iwabe N, Kuma K, Hasegawa M, Osawa S, Miyata T (1989) Evolutionary relationship of archaebacteria, eubacteria, and eukaryotes inferred from phylogenetic trees of duplicated genes. Proc Natl Acad Sci USA 86:9355–9359CrossRef

JAMSTEC Close Up (2009) 2.7 billion years ago, direct evidence that oxygen began to increase in the atmosphere (in Japanese). Blue Earth 21(1)

Kuroiwa T (2000) Where came from the Mitochondria (in Japanese). NHK Books, Tokyo

Lepot K, Benzerara K, Brown GE, Philippot P (2008) Microbially influenced formation of 2,724-million-year-old stromatolite. Nature Geosci 1:118–121CrossRef

Lowe DR (1980) Stromatolites 3,400-Myr old from the archaean of Western Australia. Nature 284:441–443CrossRef

Lowe DR (1994) Abiological origin of described stromatolites older than 3.2 Ga. Geology 22:387–390CrossRef

Margulis L (1970) Origin of eukaryotic cells. Yale University Press, New Haven

Margulis L (1981) Symbiosis in cell evolution: life and its environment on the early earth. Freeman, San Francisco

Margulis L, Sagan D (1986) Microcosmos: for billion years of microbial evolution. Summit Books, New York

Miller SL, Lazcano A (1995) The origin of life—Did it occur at high temperatures? J Mol Evol 41:689–692CrossRef

Miyata T (ed) (1998) Molecular evolution—analytical techniques and its application (in Japanes). Kyoritsushuppan, Tokyo

Mojzsis SJ, Arrhenius G, McKeegan KD, Harison TM, Nutman AP, Friend CRL (1996) Evidence for life on Earth before 3,800 million years ago. Nature 384:55–59CrossRef

Moreau JW, Sharp TG (2004) Atransmission electron microscopy study of silica and kerogen biosignatures in ~1.9 Ga Gunflint microfossils. Astrobiology 4:196–210CrossRef

Nutman AP, Bennett VC, Friend CRL, Kranendonk MJV, Chivas AR (2016) Rapid emergence of life shown by discovery of 3,700-million-year-old microbial structures. Nature 537:535–538CrossRef

Ohtomo Y, Kakegawa T, Ishida A, Nagase T, Rosing MT (2014) Evidence for biotic graphite in early Archean Isua metasedimentary rocks. Nature Geosci 7:25–28CrossRef

Okamoto N, Inoue I (2005) A secondary symbiosis in progress? Science 310:287CrossRef

Oshima T (1995) Life began in hhydrothermal water. Kagakudojin Ltd, Tokyo

Phillipot P, Van Zuilen M, Lepot K, Thomazo C, Farquhar J, Van Kranendonk MJ (2007) Early Archean microorganisms preferred elemental sulfur, not sulfate. Science 317:1534–1537CrossRef

Reaves ML, Sinha S, Rabinowitz JD, Kruglyak L, Redfield RJ (2012) Absence of detectable arsenate in DNA from arsenate-grown GFAJ-1 cells. Science 337:470–473CrossRef

Rivera MC, Lake JA (2004) The ring of life provides evidence for a genome fusion origin of eukaryotes. Nature 431:152–155CrossRef

Rosing MT (1999) ¹³C-depleted carbon microparticles in > 3,700-Ma sea-floor sedimentary rocks from West Greenland. Science 283:674–676CrossRef

Schopf JW (1993) Microfossils of the early Archean Apex chart: new evidence of the antiquity of life. Science 260:640–646CrossRef

Schopf JW, Packer BM (1987) Early Arcean (3.3-billion to 3.5-billion-year-old) microfossils from Warawoona Group, Australia. Science 237:70–73CrossRef

Shen Y, Buick R, Canfield DE (2001) Isotopic evidence for microbial sulphate reduction in the early Archean era. Nature 410:77–81CrossRef

Shen Y, Faquher J, Masterson A, Kaufman AJ, Buick R (2009) Evaluating the role of microbial sulfate reduction in the early Archean using quadruple isotope systematics. Earth Planet Sci Lett 279:383–391CrossRef

The Asahi Shimbun (in Japanese), 10 Dec 2010

The Nikkei (in Japanese), 3 Dec 2010

The Yomiuri (in Japanese), 4 Dec 2010

Ueno Y, Yurimoto H, Yoshioka H, Komiya T, Maruyama S (2002) Ion microprove analysis of graphite from c. 3.8 Ga metasediments, Isua supracrustal belt, West Greenland: relationship between metamorphism and carbon isotopic composition. Geochim Cosmochim Acta 66:1257–1268CrossRef

Ueno Y, Isozaki Y, McNamara KJ (2006) Coccoid-like microstructures in a 3.0 Ga chert from Western Australia. Inter. Geol Rev 48:78–88CrossRef

Ueno Y, Ono S, Rumble D, Maruyama S (2008) Quadruple sulfur isotope analysis of ca. 3.5 Ga dresser formation: new evidence for microbial sulfate reduction in the early Archean. Geochim Cosmochim Acta 72:5675–5691CrossRef

Wacey D, McLougin N, Whitehouse WJ, Kilbrn MR (2010) Two coexisting sulfur metabolisms in a ca. 3400 Ma sandstone. Geology 38:1115–1118CrossRef

Wacey D, Kilburn MR, Saunders M, Criff J, Brasier MD (2011) Microfossils of Sulphur-metabolizing cells in 3.4 billion-years-old rocks of Western Australia. Nat Geosci 4:698–702CrossRef

Walter MR, Buick R, Dunlop JSR (1980) Stromatolites 3400–3500 Myr old form the North Pole area Western Australia. Nature 284:443–445CrossRef

Woese CR (1987) Bacterial evolution. Microbiol Rev 51:221–271

Woese CR, Fox GE (1977) phylogenetic structure of the prokaryotic domain: The primary kingdoms. Proc Natl Acad Sci USA 74:5088–5090CrossRef

Woese CR, Kandler O, Wheelis ML (1990) Towards a natural system of organisms: proposal for the domains Archaea, Bacteria, and Eucarya. Proc Natl Acad Sci USA 87:4576–4579CrossRef

Wolfe-Simon F, Blum JS, Kulp TR, Gordon GW, Hoeft SE, Pett-Ridge J, Stolz JF., Webb SM, Weber PK, Dacies PCW, Anbar AD, Oremland RS (2010) A bacterium that can grow by using arsenic instead of phosphorus. Science 332: 1163–1166, Online publication 2 Dec 2010CrossRef

Yamagishi A (2005) Origin of cell and related problems. Biol Sci Space 19:268–275CrossRef

Yamagishi A, Kon T, Takahashi G, Oshima T (1998) From the common ancestor of all living organisms to protoeukaryotic cell. In: Wiegel J, Adams MWW (eds) Thermophilis: the key to molecular evolution and the origin of life? Taylor and Francis Ltd, London, pp 287–295

Titel: What Is the Ultimate Ancestor? Evidence from Fossils and Gene Analyses
verfasst von: Hiromoto Nakazawa
Verlag: Springer Singapore
Buch: Darwinian Evolution of Molecules
Print ISBN: 978-981-10-8723-3

Electronic ISBN: 978-981-10-8724-0

Copyright-Jahr: 2018
DOI: https://doi.org/10.1007/978-981-10-8724-0_3