Early Life, Science, and Wrestling

Total Page:16

File Type:pdf, Size:1020Kb

Early Life, Science, and Wrestling Palaeontologia Electronica http://palaeo-electronica.org EARLY LIFE, SCIENCE, AND WRESTLING Stefan Bengtson The road to wisdom? – Well, it’s plain fossilized signatures of life correctly. The and simple to express: fact that most natural entities, life not least, Err and err have fuzzy boundaries is commonly and err again ignored or denied, because words, the but less tools of our thoughts and communication, and less seem so crisp. Either a thing is a fossil and less organism or it isn’t, isn’t it? Either a thing Piet Hein was living or it wasn’t, wasn’t it? The sim- To someone who has been reading ple fact, however, is that right at the the recent media reports, the foundations boundaries of life, at its very beginning of palaeontology and astrobiology would here on Earth, the task to recognize it is seem to be crumbling. The up till now hardest of all and demands the utmost of widely accepted geochemical and palae- our skill and imagination – and humility. ontological evidences for the earliest life Let’s not worry for the moment about on Earth (Schopf 1993; Mojzsis et al. where the correct, or best, answers lie in 1996) have been thrown into serious this ongoing debate, but rather a little doubt (Brasier et al. 2002; Fedo and about how the scientific process is por- Whitehouse 2002; Zuilen et al. 2002). The trayed in the media, and how that influ- issue is of paramount importance for our ences us as scientists. The open-ended understanding of life on Earth and beyond: nature of the scientific inquiry is its most The apparent establishment of life on important characteristic. This is a much Earth as soon as environmental conditions more crucial piece of knowledge in a mod- allowed it some 3.85 Ga ago, and the ern society than any single scientific dis- appearance of microbial fossils soon covery. But it’s a difficult one to grasp, for thereafter (well, about 400 million years its message of "there is no absolute cer- later), have suggested to us that life is tainty" is confusingly similar to "there is no somehow built into the fabric of the uni- absolute truth". The latter is a recipe for verse and will start evolving as soon as "anything goes"; the former describes sci- conditions are right. If our basic presump- ence. tion is wrong, the possibility of finding life In retrospect, it’s often easy to see elsewhere in the universe suddenly which ideas were right and which were becomes bleaker. wrong. When matters are developing, it’s It would seem as though in this most not so easy. Furthermore, "wrong" ideas important of contexts paleontology has sometimes lead to good science. Just one failed its most basic task: to identify the example: The hypothesis of spontaneous Bengtson, Stefan, 2002. EARLY LIFE, SCIENCE, AND WRESTLING. Palaeontologia Electronica, vol. 5, issue 1, editorial 4: 3pp., 96KB; http://palaeo-electronica.org. BENGTSON, STEFAN: EARLY LIFE, SCIENCE, AND WRESTLING generation of life has many times been to the principle that science is an open- shown to be inadequate, but it has proba- ended search, that the value of a hypothe- bly inspired more good science than most sis lies in whether it can help to advance "correct" hypotheses – just think of knowledge rather than being in an abso- Francesco Redi, Louis Pasteur, and John lute sense true. Above all, we take pride in Tyndall. Today, the hypothesis isn’t dead, our ability to learn through error. At the but it has moved to the Archean stage, same time we know that scientists – like where it continues to generate good all creative people – have egos, often big research. Only the future will tell us ones. But unlike art (where the products whether in the end the hypothesis will be are, by definition, artificial), scientific prod- as inadequate to explain the origin of life ucts concern themselves with facts and on Earth as it was to account for the histories about which there is ultimately appearance of maggots in flesh or infuso- only one "right" answer. When a prominent rians in water. But even if that turns out to scientist’s prominent interpretation of an be the case, the hypothesis will have con- object is falsified, some personal damage tinued to stimulate good research. It’s thus is all but inevitable. So, science is a a good hypothesis. Had it been just a nutty human endeavor, run by humans for idea, few would have bothered to refute it. humans. No change there, then. The world is full of nutty ideas, most of Nevertheless, a healthy scientific cul- which are not even worth refuting, but we ture shouldn’t encourage itself or the gen- shouldn’t be afraid of nut-flavored scien- eral public to focus on the egotistical tific hypotheses as long as they are in aspects of the process. Certainly, it should some way testable. Even if "wrong", they foster honest and careful work (there is no may teach us something. inherent value in making errors), but it Life isn’t fair. A palaeontologist who should also encourage retractions from misidentifies a clam for a coral may be earlier held positions when they lead into a temporarily embarrassed but isn’t likely to cul-de-sac. A cornerstone of such a cul- suffer any career damage only for that ture is prestige-less dialogue. Do we have blunder. Only his or her peers will know, such a culture? Maybe, but when one of and will likely shrug it off, knowing that the flagships of science suddenly looks they may goof someday too. One who more like a tabloid picked up at a super- mistakes an a biologically formed structure market checkout counter, it’s time to real- for the world’s oldest fossil is in deeper ize that such a culture has to be nurtured trouble, however much more difficult that in order to survive. task is, if only because the action takes So finally to the point. What prompts place in the limelight. Colleagues will turn this diatribe is Rex Dalton’s (2002) recent on him or her. The same media that have news feature in Nature on the arguments hyped the discovery in the first place will between Bill Schopf and Martin Brasier be quick to pooh-pooh it now. regarding the alleged earliest fossils on In a way, there’s a fair balance here: Earth. I don’t read wrestling magazines, The greater the rewards for success, the but I figure their readers would be comfort- greater the punishment for failure. A scien- able with this portrayal of a scientific dis- tist should enter that mined territory with pute as a heavy-weight match, where one eyes wide open. But fame and shame is of the combatants is painted as a righ- not what good science is made of, or teous if haughty knight, and the other as a should be made of. We all pay lip service scoundrel who has been able to fool the 2 BENGTSON, STEFAN: EARLY LIFE, SCIENCE, AND WRESTLING world for too long. No matter that the ness, but as scientists we should be much "scoundrel" has probably done more to more concerned with the science than with advance the science of Precambrian pale- the splatter entertainment. Besides, good obiology as a multidisciplinary endeavor science is much more fun – and much than anybody else – down with him! more honest – than media-manufactured It’s disheartening to read such a yarn wrestling matches. in a journal dedicated to the advancement of science. Yet we cannot just blame sci- ACKNOWLEDGEMENT ence journalists for the shortcomings of Thanks to Norm MacLeod for useful the scientific culture. It’s each and every- comments. one’s responsibility to help keep it sound. Indeed, we should blow the whistle at vil- REFERENCES lains who forge or steal results. But being Brasier, M.D., Green, O.R., Jephcoat, A.P., Kleppe, A.K., right or wrong in science is not a matter of Van Kranendonk, M.J., Lindsay, J.F., Steele, A. & heroes and villains, and shouldn’t be con- Grassineau, N.V. 2002. Questioning the evidence for Earth’s oldest fossils. Nature, 416:76–81. strued as such. Instead, we should foster Dalton, R. 2002. Squaring up over ancient life. Nature, an atmosphere where we can deal con- 417:782–784. structively with conflicting interpretations. Fedo, C.M. & Whitehouse, M.J. 2002. Metasomatic ori- In a good atmosphere there is an open gin of quartz-pyroxene rock, Akilia, Greenland, and implications for Earth’s earliest life. Science scientific discussion, where ideas are 296:1448–1452. tested against each other and against Mojzsis, S.J., Arrhenius, G., McKeegan, K.D., Harrison, observations in a spirit of mutual coopera- T.M., Nutman, A.P. & Friend, C.R.L. 1996. Evidence tion and collaborative search for the best for life on Earth before 3,800 million years ago. Nature, 384:55–59. available interpretation. In a foul atmo- Schopf, J.W. 1993. Microfossils of the Early Archean sphere, the proponents of the respective Apex Chert: New evidence of the antiquity of life. Sci- ideas punch each other to pulp in a wres- ence, 260:640–646. Zuilen, M.A. van, Lepland, A. & Arrhenius, G. 2002. tling ring before a cheering audience. If Reassessing the evidence for the earliest traces of they want to do it anyway, that’s their busi- life. Nature, 418:627–630. Copyright: Palaeontologia Electronica, 30 August 2002 http://palaeo-electronica.org 3.
Recommended publications
  • 12.007 Geobiology Spring 2009
    MIT OpenCourseWare http://ocw.mit.edu 12.007 Geobiology Spring 2009 For information about citing these materials or our Terms of Use, visit: http://ocw.mit.edu/terms. Geobiology 2009 Lecture 10 The Antiquity of Life on Earth Homework #5 Topics (choose 1): Describe criteria for biogenicity in microscopic fossils. How do the oldest describes fossils compare? Use this to argue one side of the Brasier-Schopf debate OR What are stromatolites; where are they found and how are they formed? Articulate the two sides of the debate on antiquity and biogenicity. Up to 4 pages, including figures. Due 3/31/2009 Need to know • How C and S- isotopic data in rocks are informative about the advent and antiquity of biogeochemical cycles • Morphological remains and the antiquity of life; how do we weigh the evidence? • Indicators of changes in atmospheric pO2 • A general view of the course of oxygenation of the atm-ocean system Readings for this lecture Schopf J.W. et al., (2002) Laser Raman Imagery of Earth’s earliest fossils. Nature 416, 73. Brasier M.D. et al., (2002) Questioning the evidence for Earth’s oldest fossils. Nature 416, 76. Garcia-Ruiz J.M., Hyde S.T., Carnerup A. M. , Christy v, Van Kranendonk M. J. and Welham N. J. (2003) Self-Assembled Silica-Carbonate Structures and Detection of Ancient Microfossils Science 302, 1194-7. Hofmann, H.J., Grey, K., Hickman, A.H., and Thorpe, R. 1999. Origin of 3.45 Ga coniform stromatolites in Warrawoona Group, Western Australia. Geological Society of America, Bulletin, v. 111 (8), p.
    [Show full text]
  • Cause of Cambrian Explosion - Terrestrial Or Cosmic?
    Progress in Biophysics and Molecular Biology xxx (2018) 1e21 Contents lists available at ScienceDirect Progress in Biophysics and Molecular Biology journal homepage: www.elsevier.com/locate/pbiomolbio Cause of Cambrian Explosion - Terrestrial or Cosmic? * Edward J. Steele a, j, , Shirwan Al-Mufti b, Kenneth A. Augustyn c, Rohana Chandrajith d, John P. Coghlan e, S.G. Coulson b, Sudipto Ghosh f, Mark Gillman g, Reginald M. Gorczynski h, Brig Klyce b, Godfrey Louis i, Kithsiri Mahanama j, Keith R. Oliver k, Julio Padron l, Jiangwen Qu m, John A. Schuster n, W.E. Smith o, Duane P. Snyder b, Julian A. Steele p, Brent J. Stewart a, Robert Temple q, Gensuke Tokoro o, Christopher A. Tout r, Alexander Unzicker s, Milton Wainwright b, j, Jamie Wallis b, Daryl H. Wallis b, Max K. Wallis b, John Wetherall t, D.T. Wickramasinghe u, J.T. Wickramasinghe b, N. Chandra Wickramasinghe b, j, o, Yongsheng Liu v, w a CY O'Connor ERADE Village Foundation, Piara Waters, WA, Australia b Buckingham Centre for Astrobiology, University of Buckingham, UK c Center for the Physics of Living Organisms, Department of Physics, Michigan Technological University, Michigan, United States d Department of Geology, University of Peradeniya, Peradeniya, Sri Lanka e University of Melbourne, Office of the Dean, Faculty Medicine, Dentistry and Health Sciences, 3rd Level, Alan Gilbert Building, Australia f Metallurgical & Materials Engineering IIT, Kanpur, India g South African Brain Research Institute, 6 Campbell Street, Waverly, Johannesburg, South Africa h University Toronto
    [Show full text]
  • Paleontology1
    PALEONTOLOGY1 Thoreau’s firm grasp of paleontology laid the groundwork for the climax of WALDEN, which describes the emergence of complexity and beauty from the simple flow of muddy sand at the Deep Cut. It also was the taproot of his lifelong frustration with Christian supernaturalists, who insisted on a fairly brief history of life. Paraphrasing Lyell’s PRINCIPLES, he jested [in A WEEK ON THE C ONCORD AND M ERRIMACK R IVERS]: “It took 100 years to prove that fossils are organic, and 150 more, to prove that they are not to be referred to the Noachian deluge.” Not everyone believes this, even today. Modern “young Earth” creationists still insist that the Elizabethan-era Mosaic chronology of Archbishop Ussher is the correct one, and that we twenty-first century scientists are in error. — Professor Robert M. Thorson, WALDEN’S SHORE, pages 60-1 1. (“Paleology” would be the study of antiques, how much they might fetch at auction.) HDT WHAT? INDEX PALEONTOLOGY PALEONTOLOGY 23,000 BCE Full glacial world, cold and dry; Stage 2 (includes the latest “Glacial Maximum”). This period includes the two ‘coldest phases’ –Heinrich Events– at something like 21,000 BCE-19,000 BCE and at something like 15,000 BCE-12,500 BCE. Music was produced by humans in what is now France; archaeological evidence includes cave paintings, footprints in caves that seem to be those of dancers, and carved bones that seem to be wind and percussion instruments. People made artifacts with primitive geometrical designs. THE WISCONSONIAN GLACIATION “NARRATIVE HISTORY” AMOUNTS TO FABULATION, THE REAL STUFF BEING MERE CHRONOLOGY “Stack of the Artist of Kouroo” Project Paleontology HDT WHAT? INDEX PALEONTOLOGY PALEONTOLOGY 18,000 BCE On the basis of Carbon-14 measurements, this was the last Glacial Maximum, the coldest period of the most recent Ice Age.
    [Show full text]
  • Geobiology 2007 Lecture 4 the Antiquity of Life on Earth Homework #2
    Geobiology 2007 Lecture 4 The Antiquity of Life on Earth Homework #2 Topics (choose 1): Describe criteria for biogenicity in microscopic fossils. How do the oldest described fossils compare? How has the Brasier-Schopf debate shifted in five years? OR What are stromatolites; where are they found and how are they formed? Articulate the two sides of the debate on antiquity and biogenicity. Up to 4 pages, including figures. Due 3/01/2006 Required readings for this lecture Nisbet E. G. & Sleep N. H. (2001) The habitat and nature of early life, Nature 409, 1083. Schopf J.W. et al., (2002) Laser Raman Imagery of Earth’s earliest fossils. Nature 416, 73. Brasier M.D. et al., (2002) Questioning the evidence for Earth’s oldest fossils. Nature 416, 76. Garcia-Ruiz J.M., Hyde S.T., Carnerup A. M. , Christy v, Van Kranendonk M. J. and Welham N. J. (2003) Self-Assembled Silica-Carbonate Structures and Detection of Ancient Microfossils Science 302, 1194-7. Hofmann, H.J., Grey, K., Hickman, A.H., and Thorpe, R. 1999. Origin of 3.45 Ga coniform stromatolites in Warrawoona Group, Western Australia. Geological Society of America, Bulletin, v. 111 (8), p. 1256-1262. Allwood et al., (2006) Stromatolite reef from the Early Archaean era of Australia. Nature 441|, 714 J. William Schopf, Fossil evidence of Archaean life (2006) Phil. Trans. R. Soc. B 361, 869–885. Martin Brasier, Nicola McLoughlin, Owen Green and David Wacey (2006) A fresh look at the fossil evidence for early Archaean cellular life. Phil. Trans. R. Soc. B 361, 887–902 What is Life? “Life can be recognized by its deeds — life is disequilibrium, leaving behind the signatures of disequilibrium such as fractionated isotopes or complex molecules.
    [Show full text]
  • The Earliest Bioturbators As Ecosystem Engineers
    Downloaded from http://sp.lyellcollection.org/ at University of Hull on February 4, 2017 Engineering the Cambrian explosion: the earliest bioturbators as ecosystem engineers LIAM G. HERRINGSHAW1,2*, RICHARD H. T. CALLOW1,3 & DUNCAN MCILROY1 1Department of Earth Sciences, Memorial University of Newfoundland, Prince Philip Drive, St John’s, NL, A1B 3X5, Canada 2Geology, School of Environmental Sciences, University of Hull, Cottingham Road, Hull HU6 7RX, UK 3Statoil ASA, Stavanger 4035, Norway *Correspondence: [email protected] Abstract: By applying modern biological criteria to trace fossil types and assessing burrow mor- phology, complexity, depth, potential burrow function and the likelihood of bioirrigation, we assign ecosystem engineering impact (EEI) values to the key ichnotaxa in the lowermost Cambrian (Fortunian). Surface traces such as Monomorphichnus have minimal impact on sediment properties and have very low EEI values; quasi-infaunal traces of organisms that were surficial modifiers or biodiffusors, such as Planolites, have moderate EEI values; and deeper infaunal, gallery biodiffu- sive or upward-conveying/downward-conveying traces, such as Teichichnus and Gyrolithes, have the highest EEI values. The key Cambrian ichnotaxon Treptichnus pedum has a moderate to high EEI value, depending on its functional interpretation. Most of the major functional groups of mod- ern bioturbators are found to have evolved during the earliest Cambrian, including burrow types that are highly likely to have been bioirrigated. In fine-grained (or microbially bound) sedimentary environments, trace-makers of bioirrigated burrows would have had a particularly significant impact, generating advective fluid flow within the sediment for the first time, in marked contrast with the otherwise diffusive porewater systems of the Proterozoic.
    [Show full text]
  • Late Ediacaran Organic Microfossils from Finland
    Geological Magazine Late Ediacaran organic microfossils from www.cambridge.org/geo Finland Sebastian Willman and Ben J. Slater Original Article Department of Earth Sciences, Palaeobiology, Uppsala University, Villavägen 16, SE-75236, Uppsala, Sweden Cite this article: Willman S and Slater BJ. Late Abstract Ediacaran organic microfossils from Finland. Geological Magazine https://doi.org/10.1017/ Here we present a detailed accounting of organic microfossils from late Ediacaran sediments S0016756821000753 of Finland, from the island of Hailuoto (northwest Finnish coast), and the Saarijärvi meteorite impact structure (~170 km northeast of Hailuoto, mainland Finland). Fossils were Received: 16 March 2021 recovered from fine-grained thermally immature mudstones and siltstones and are preserved Revised: 10 June 2021 Accepted: 24 June 2021 in exquisite detail. The majority of recovered forms are sourced from filamentous prokaryotic and protistan-grade organisms forming interwoven microbial mats. Flattened Nostoc-ball-like Keywords: masses of bundled Siphonophycus filaments are abundant, alongside Rugosoopsis and Ediacaran; Bilateria; microbial mats; acritarchs; Palaeolyngbya of probable cyanobacterial origin. Acritarchs include Chuaria, Leiosphaeridia, impact crater; organic-walled microfossils; Symplassosphaeridium and Synsphaeridium. Significantly, rare spine-shaped sclerites of Baltica bilaterian origin were recovered, providing new evidence for a nascent bilaterian fauna in Author for correspondence: the terminal Ediacaran. These findings offer a direct body-fossil insight into Ediacaran Sebastian Willman, mat-forming microbial communities, and demonstrate that alongside trace fossils, detection Email: [email protected]; of a bilaterian fauna prior to the Cambrian might also be sought among the emerging record Ben Slater, Email: [email protected] of small carbonaceous fossils (SCFs).
    [Show full text]
  • The Paleoproterozoic Fossil Record: Implications for the Evolution of the Biosphere During Earth’S Middle-Age Emmanuelle J
    The Paleoproterozoic fossil record: Implications for the evolution of the biosphere during Earth’s middle-age Emmanuelle J. Javaux, Kevin Lepot To cite this version: Emmanuelle J. Javaux, Kevin Lepot. The Paleoproterozoic fossil record: Implications for the evolution of the biosphere during Earth’s middle-age. Earth-Science Reviews, Elsevier, 2018, 176, pp.68-86. 10.1016/j.earscirev.2017.10.001. insu-03190875 HAL Id: insu-03190875 https://hal-insu.archives-ouvertes.fr/insu-03190875 Submitted on 6 Apr 2021 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. Distributed under a Creative Commons Attribution - NonCommercial| 4.0 International License Earth-Science Reviews 176 (2018) 68–86 Contents lists available at ScienceDirect Earth-Science Reviews journal homepage: www.elsevier.com/locate/earscirev Invited review The Paleoproterozoic fossil record: Implications for the evolution of the biosphere during Earth's middle-age T ⁎ Emmanuelle J. Javauxa, , Kevin Lepotb a University of Liège, Department of Geology, Palaeobiogeology-Palaeobotany-Palaeopalynology, 14, allée du 6 Août B18, quartier AGORA, 4000 Liège, (Sart-Tilman), Belgium b Université de Lille, CNRS, Université Littoral Côte d'Opale, Laboratoire d'Océanologie et de Géosciences UMR8187, Cité Scientifique, SN5, 59655 Villeneuve d'Ascq, France ARTICLE INFO ABSTRACT Keywords: The Paleoproterozoic (2.5–1.6 Ga) Era is a decisive time in Earth and life history.
    [Show full text]
  • Caterpillars Evolved from Onychophorans by Hybridogenesis
    Caterpillars evolved from onychophorans by hybridogenesis Donald I. Williamson1 Marine Biology, University of Liverpool, Liverpool L69 7ZB, United Kingdom Communicated by Lynn Margulis, University of Massachusetts Amherst, Amherst, MA, July 24, 2009 (received for review May 19, 2009) I reject the Darwinian assumption that larvae and their adults adults and ontogeny is a short, rapid recapitulation of phylogeny. evolved from a single common ancestor. Rather I posit that, in Garstang (6) proposed that modern larvae represent ancestral animals that metamorphose, the basic types of larvae originated as larvae rather than adults. He posited that adults in one taxon that adults of different lineages, i.e., larvae were transferred when, resemble larvae in another are ‘‘persistent larvae,’’ i.e., forms through hybridization, their genomes were acquired by distantly that were originally larvae but now mature without metamor- related animals. ‘‘Caterpillars,’’ the name for eruciforms with phosis. I regard his persistent larvae as relatives of adult animals thoracic and abdominal legs, are larvae of lepidopterans, hym- that were sources of larvae in distant lineages. enopterans, and mecopterans (scorpionflies). Grubs and maggots, ‘‘Even the illustrious Cuvier did not perceive that a barnacle including the larvae of beetles, bees, and flies, evolved from was, as it certainly is, a crustacean; but a glance at the larva shows caterpillars by loss of legs. Caterpillar larval organs are dismantled this to be the case in an unmistakable manner’’ wrote Darwin and reconstructed in the pupal phase. Such indirect developmental (ref. 1, p. 420), and barnacles provide a clear example of the patterns (metamorphoses) did not originate solely by accumula- differences between Darwin’s attitude to larvae and mine.
    [Show full text]
  • Feast Clue to Smell of Ancient Earth Fossils Show Earliest Animal
    Feast Clue to Smell of Ancient Earth Apr. 29, 2013 — Tiny 1,900 million-year-old fossils from rocks around Lake Superior, Canada, give the first ever snapshot of organisms eating each other and suggest what the ancient Earth would have smelled like. The fossils, preserved in Gunflint chert, capture ancient microbes in the act of feasting on a cyanobacterium-like fossil called Gunflintia -- with the perforated sheaths of Gunflintia being the discarded leftovers of this early meal. A team, led by Dr David Wacey of the University of Western Australia and Bergen University, Norway, and Professor Martin Brasier of Oxford University, reports in this week's Proceedings of the National Academy of Sciences the fossil evidence for how this type of feeding on organic matter -- called 'heterotrophy' -- was taking place. They also show that the ancient microbes appeared to prefer to snack on Gunflintia as a 'tasty morsel' in preference to another bacterium (Huroniospora). 'What we call 'heterotrophy' is the same thing we do after dinner as the bacteria in our gut break down organic matter,' said Professor Martin Brasier of Oxford University's Department of Earth Sciences, an author of the paper. 'Whilst there is chemical evidence suggesting that this mode of feeding dates back 3,500 million years, in this study for the first time we identify how it was happening and 'who was eating who'. In fact we've all experienced modern bacteria feeding in this way as that's where that 'rotten egg' whiff of hydrogen sulfide comes from in a blocked drain. So, rather surprisingly, we can say that life on earth 1,900 million years ago would have smelled a lot like rotten eggs.' The team analysed the microscopic fossils, ranging from about 3-15 microns in diameter, using a battery of new techniques and found that one species -- a tubular form thought to be the outer sheath of Gunflintia -- was more perforated after death than other kinds, consistent with them having been eaten by bacteria.
    [Show full text]
  • Fortunian GSSP.Pdf
    bY, M arlin B rasier, John C ow ie and M ichael Tavlor D ecisio n o n th e P reca m b rian - C a m b ria n boundary stratotype The G lobal Stratotype Se(,tion and Pointjbr the P ro- dom inate elsew here. It w its for this reas(川that B D aily (unpub- terozoiC- C anibrian botindarv has been agreed upon. lished) em phasised the potential of' [race fossil stratigraphy as a subsidiary gVuide. The botindarY is defi ned in a coastal section near the T his w a s l 'o llow cd in 1974 by a m eeting in Paris. at w hich the loviln Of' Fortune in sotitheaste,二 N etyfl)undland, follow ing Points W ere 1.111aniniously agreed (C ow ie, 1992). C a n ad a . T he prim ary task of the W orking G ro up w as the choice o f a stra- Lotype boundary point-, a secondary task w as the consideration ot associated stratigraphic divisions above and below the bound- a ry . In tro d u c tio n A ny s uccession selected for the boundary point m ust be as con- fi nUOUS as possible, m arine. and as m ono facial as possib le} the m ain m ethod of guidance in selection should be biostratig- T he problem of the Precambrian-Cambrian boundary is part of one raphy although all possible m ethods of correlation should be ol'ihe Lreatcst enigm as of the fossil record; i.e. the relatively abrupt e nliste d .
    [Show full text]
  • COMMENTARY on HOMAGE to DARWIN DEBATE by James D
    A COMMENTARY ON HOMAGE TO DARWIN DEBATE By James D. MacAllister With an Afterword by Professor Denis Noble PART 1 An unrehearsed program chaired by Oxford University Professor of Physiology, Denis Noble (author of Music of Life; Biology Beyond Genes [2008]) was open to students and the public. It was organized at Balliol College, Oxford University UK (May 8, 2009) on the 200th anniversary year of Darwin’s birth. A lively discussion by faculty, students and others ensued. Four short presentations by Oxford Professors constitute Part 1 (43 minutes): new Oxford Professor of Microbiology, Stephen Bell described the archaebacterial legacy of eukaryotes; Professor of Paleobiology, geologist Martin Brasier showed complexification in forams, the “fruitflies of geology”, their appearances and extinctions in the fossil record; Prof. Richard Dawkins presented his “gene’s-eye view of evolution”; and Prof. Denis Noble commented on cooperating genes. A review of the previous presentations by Eastman Professor Lynn Margulis, University of Massachusetts-Amherst, an introduction to her film “Eukaryosis, origin of nucleated cell” and the presentation of the 14-minute film with her live narration constitute Part 2 (51 minutes). Part 3, a less formal continuation of the discussion took place later in the evening at the same venue and was documented with digital audio but not videotaped. I have included sequentially numbered “markers.” These are for navigation when the DVD or web streaming video is viewed and correspond to the transcript and this commentary. Scenes can be randomly accessed using the “chapter” function found on most DVD players and computers. There are also running times given in brackets [e.g., 23:16] that closely match the running time to match the transcription to video or the mp3 audio CD.
    [Show full text]
  • Darwin's Lost World
    DARWIN’S LOST WORLD .......................t ....................... The Hidden History of Animal Life Martin Brasier 1 Brasier / Darwin's 9780199548972_000i-0xiv_Brasier_Darwin_Prelims Final Proof page i 14.12.2009 9:26pm DARWIN’SLOSTWORLD Martin Brasier is Professor of Palaeobiology at Oxford University, and Adjunct Professor at the Memorial University of Newfoundland. He has worked closely with NASA concerning fieldwork on Mars and the earliest signs of life on Earth, on which his research is focussed. Professor Brasier chaired the international commission that established the Precambrian-Cambrian boundary. He is the author of over 200 research papers; the founding author of Microfossils, the standard text on the subject; and co-editor of The Precambrian-Cambrian Boundary. Brasier / Darwin's 9780199548972_000i-0xiv_Brasier_Darwin_Prelims Final Proof page vi 14.12.2009 9:26pm ................................................. PREFACE ................................................. ome 150 years ago, in 1859, Charles Darwin was greatly S puzzled by a seeming absence of animal fossils in rocks older than the Cambrian period. He drew attention to a veritable Lost World that was later found to have spanned more than eighty per cent of Earth history. This book tells the story of his lost world, and of the quest to rescue its hidden history from the fossil record. Intriguingly, such a quest did not really begin until 1958, some hundred years after Darwin. Why did an understanding take so long? Arguably it was because it was, and still remains, a very big and very difficult problem. Its study now involves the whole of the natural sciences. Progress has been a matter of slow attrition. For most of this time, for example, there has been no concept of the vast duration of Precambrian time, nor any evidence for a distinct biota.
    [Show full text]