Modelling the Transport of Nutrients in Early Animals

Total Page:16

File Type:pdf, Size:1020Kb

Modelling the Transport of Nutrients in Early Animals Evol Biol (2009) 36:256–266 DOI 10.1007/s11692-008-9047-2 ESSAY Modelling the Transport of Nutrients in Early Animals N. J. Beaumont Received: 20 June 2008 / Accepted: 6 November 2008 / Published online: 10 January 2009 Ó Springer Science+Business Media, LLC 2008 Abstract The single-celled ancestors of multi-cellular Introduction animals (metazoans) did not need to transport nutrients between cells, but this ability is vital for modern animals. The origins of multi-cellularity are obscure. It is unclear How could intercellular nutrient transport have begun? how early multi-cellular animals evolved, and why it And how did this influence the early evolution of animals? happened at that particular time. Suggestions or hypotheses In this hypothesis, I suggest that nutrients could have about the origins can be tested using the main lines of passed directly between the cytoplasm of conjoined cells in available evidence about the earliest animals: the fossil early compacted cell-balls, along the plane of the closed record and the molecular and developmental data from epithelium. This would have limited early animals to the modern species. size and form of modern embryos. The mechanisms that The Precambrian fossil record provides evidence of the indirectly transport nutrients between discrete cells, via the earliest known multi-cellular forms. Multi-cellular organ- extracellular fluid within the body-space, are modelled to isms have been identified from rocks up to 600 million years have evolved sequentially; so comparison of nutrient old. A diverse group of large fossils, the Ediacaran Fauna, transport processes could provide evidence of any early have been found at sites around the World in rocks from divergences of phyla. When the last of the indirect inter- between approximately 580 million and 550 million years cellular transport processes for essential nutrients had been ago. It has been suggested that these frondose organisms developed, the extracellular fluid within the body-space were ancestral to some modern animals (Glaessner and would have contained all necessary nutrients. Then the Wade 1966). However, an alternative hypothesis has been epithelium could have greatly expanded, and cells lived suggested: that they were an independent ‘‘experiment’’ in and divided within the body-space. This development of multi-cellularity (Seilacher 1984). At this stage, it is unclear nutrient transport processes would have enabled animals to whether these organisms were ancestral to modern phyla. greatly increase in size and complexity. Microfossils have been found in southern China from approximately 580 million years ago (Xiao et al. 1998; Keywords Metazoan Evolution Cambrian Chen et al. 2000). These minute fossils are less than a Proterozoic Á Á Á millimetre across but are exquisitely preserved. They have been interpreted as embryonic forms; but the adult forms do not seem to be present—so it is unclear how they should be incorporated into an account of early multi-cellularity. A putative bilaterian from this area has also been reported. Vernanimalcula (Chen et al. 2004a) has been interpreted as N. J. Beaumont (&) having a mouth, gut and anus in a hollow form of less than Department of Medicine, Royal Free & University College a millimetre; however this interpretation is controversial Medical School, Royal Free Campus, Rowland Hill Street, (Bengtson and Budd 2004; Chen et al. 2004b). London NW3 2PF, UK e-mail: [email protected]; Animals from extant phyla definitely start to appear in [email protected] the fossil record from around 530 million years ago. The 123 Evol Biol (2009) 36:256–266 257 apparently sudden appearance of a broad range of complex in the fossil record. Nevertheless, it is clear that multi- animals from virtually all recognised phyla has been called cellular creatures arose from simpler organisms, as surely the Cambrian ‘‘explosion’’. Taking the fossil record on its as the adult develops from the fertilized egg by way of the own, it suggests that animals with bodyplans similar to embryo, so it is intriguing to consider the reasons and modern animals appeared suddenly, with no obviously requirements for such changes. simpler precursors. There is continuing debate over whe- The aim here is to understand the advent of multi-cel- ther this is an artefact of the fossil record or an accurate, if lularity by considering how nutrients move between the rather puzzling, record of events. cells of modern animals, and then considering how this The comparison of homologous molecular sequences distribution could have begun. I argue that these processes from different modern phyla, calibrated with reference to would not have developed in unicellular organisms, but the fossil record, has been used to create ‘‘molecular that they are necessary for triploblastic metazoans. I pres- clocks’’. These data have been used to extrapolate back to ent a model of early nutrient transport in animals, suggest the metazoan radiation, to estimate the time when the stem how this may have evolved into modern forms and con- groups that led to modern phyla diverged. In contrast to the sider some of the implications this had for evolution. impression formed from the fossil record, many of the studies based upon molecular data have suggested that The Transport of Nutrients in Animals modern phyla diverged a long time before the Cambrian period (Wray et al. 1996; Pisani et al. 2004). These studies The cells of multi-cellular organisms must obtain sufficient suggest that the ancestral stem groups of modern phyla had nutrients from either the environment or from within the diverged for a considerable length of Precambrian time organism. Nutrients pass between cells in triploblastic without leaving traces in the fossil record. This is surpris- animals by a variety of methods. These processes can be ing because the stem groups of modern phyla were divided into direct and indirect transport, depending upon probably multi-cellular. However, there may have been a whether the molecules that are being transported pass number of gene, and even genome, duplications around the across cell membranes and through another compartment time of the metazoan radiation, and rates of genetic change when moving between cells. In direct transport, nutrients could have varied between phyla. These factors may have pass between cells via cytoplasmic bridges (such as gap jeopardized the assumption of uniform rates of variation junctions). These link the cytoplasm of conjoined cells and upon which this approach is based (Peterson et al. 2004). allow small molecules to non-specifically equilibrate It is difficult to understand the beginning of multi-cel- between them without having to cross extracellular space lular animals because it is unclear how the metazoan or the plasma membrane (Fig. 1a). This can happen in cell- radiation, when the variety of modern phyla first arose— types such as epithelia or syncitia. which has been investigated by analyzing molecular However, there are some cell types, such as muscle, sequences, was related to the Cambrian ‘‘explosion’’ seen bone and blood cells, which are not conjoined with other AB Fig. 1 Nutrients can pass between cells by direct or indirect Nutrients are released into the enclosed body-space by the cells that nutrient transport. Simplified representation in which only two take them up from the gut. They are then available for other cells nutrients (blue and red) are depicted in cross-sections of hypothetical (such as the token isolated internal cell depicted). Note that a separate gastrula-like forms. a Direct nutrient transport: Both nutrients are indirect nutrient transport process is required for each nutrient. taken up into the organism and pass from cell to cell by cytoplasmic Nutrients are only depicted in the top half of the figure links across the closed epithelium. b Indirect nutrient transport: 123 258 Evol Biol (2009) 36:256–266 cells and take up all the nutrients they require from the Therefore, metazoan nutrient uptake processes could have extracellular fluid. This requires that they have all the derived from those used by unicellular organisms. necessary transport mechanisms to take up each nutrient as needed across the plasma membrane, and also that all Nutrients Could have Moved Between Cells Within essential nutrients are present in the extracellular fluid. Early Animals by Direct Transport This in turn requires that the cells that take up the nutrients from food (for example, the enterocytes that line the Some cells in early multi-cellular organisms would have mammalian gut) also release these nutrients into the needed to receive nutrients from other cells when their extracellular space within the organism so that they may be ability to take up nutrients from the environment became taken up by other cells. This mode of intercellular nutrient limited because their access to food was hampered by their transport is here designated indirect, to denote that the position in the organism. This movement of nutrients could nutrients pass between cells by crossing the plasma mem- have happened by direct transport. Cytoplasmic bridges brane, moving across the extracellular space within the would have established a physical link between cells, organism and then crossing the membrane of another cell which would have coupled the pools of solutes in them (Fig. 1b). without requiring the development of specialized transport The two processes that move nutrients between the cells processes for each nutrient. This ability
Recommended publications
  • Integrative and Comparative Biology Integrative and Comparative Biology, Volume 58, Number 4, Pp
    Integrative and Comparative Biology Integrative and Comparative Biology, volume 58, number 4, pp. 605–622 doi:10.1093/icb/icy088 Society for Integrative and Comparative Biology SYMPOSIUM INTRODUCTION The Temporal and Environmental Context of Early Animal Evolution: Considering All the Ingredients of an “Explosion” Downloaded from https://academic.oup.com/icb/article-abstract/58/4/605/5056706 by Stanford Medical Center user on 15 October 2018 Erik A. Sperling1 and Richard G. Stockey Department of Geological Sciences, Stanford University, 450 Serra Mall, Building 320, Stanford, CA 94305, USA From the symposium “From Small and Squishy to Big and Armored: Genomic, Ecological and Paleontological Insights into the Early Evolution of Animals” presented at the annual meeting of the Society for Integrative and Comparative Biology, January 3–7, 2018 at San Francisco, California. 1E-mail: [email protected] Synopsis Animals originated and evolved during a unique time in Earth history—the Neoproterozoic Era. This paper aims to discuss (1) when landmark events in early animal evolution occurred, and (2) the environmental context of these evolutionary milestones, and how such factors may have affected ecosystems and body plans. With respect to timing, molecular clock studies—utilizing a diversity of methodologies—agree that animal multicellularity had arisen by 800 million years ago (Ma) (Tonian period), the bilaterian body plan by 650 Ma (Cryogenian), and divergences between sister phyla occurred 560–540 Ma (late Ediacaran). Most purported Tonian and Cryogenian animal body fossils are unlikely to be correctly identified, but independent support for the presence of pre-Ediacaran animals is recorded by organic geochemical biomarkers produced by demosponges.
    [Show full text]
  • Cambrian Small Bilaterian Fossils from 40 to 55 Million Years Before
    Supporting Online Material Systematic Paleontology Genus Vernanimalcula gen. et sp. nov. Etymology: Generic name denotes (from Latin) small spring animal (i.e., after Snowball Earth winter). Diagnosis: Small triploblastic bilaterian animal (about 120-180 microns in length), with an oval-shaped dorsal view. The alimentary canal is differentiated into a pharynx, which is muscular and multi-layered (three, possibly four single cell layers), running anterior- posterior with a collared mouth situating ventrally near anterior margin of the body. The pharynx opens into an expanded stomach/intestine, which terminates at the posterior end with an anus. Alimentary canal is flanked by paired coeloms, which are bounded with single-cell mesodermal layers. Externally the mesodermal layers are covered with ectoderm layers and internally they abut the endodermal wall of the alimentary tract. The body is convex dorsally and there are at least three pits on each side of the outer surface. These pits are floored with small cells. The ventral surface is interpreted to be flat. Type species: Vernanimalcula guizhouena gen. et sp. nov. (Fig. 1 A; Table 1). Etymology: Specific name refers to Guizhou Province, where the fossils came from. Holotype: The holotype represents a complete animal preserved; the section runs nearly parallel to the ventral surface of the animal. Material: Five specimens, all of which are nearly complete. Specimen numbers are given in Table 1. Diagnosis: Same as the generic diagnosis. This and the other specimens described are housed at the Early Life Research Center in Chengjiang, Yunnan, China. Locality and Stratigraphy: Badoushan, Weng'an County, Central Guizhou; from ~2-m- thick basal black bituminous phosphorite layer of the Precambrian lower Weng'an Phosphate Member, Doushantuo Formation.
    [Show full text]
  • Radial Symmetry Or Bilateral Symmetry Or "Spherical Symmetry"
    Symmetry in biology is the balanced distribution of duplicate body parts or shapes. The body plans of most multicellular organisms exhibit some form of symmetry, either radial symmetry or bilateral symmetry or "spherical symmetry". A small minority exhibit no symmetry (are asymmetric). In nature and biology, symmetry is approximate. For example, plant leaves, while considered symmetric, will rarely match up exactly when folded in half. Radial symmetry These organisms resemble a pie where several cutting planes produce roughly identical pieces. An organism with radial symmetry exhibits no left or right sides. They have a top and a bottom (dorsal and ventral surface) only. Animals Symmetry is important in the taxonomy of animals; animals with bilateral symmetry are classified in the taxon Bilateria, which is generally accepted to be a clade of the kingdom Animalia. Bilateral symmetry means capable of being split into two equal parts so that one part is a mirror image of the other. The line of symmetry lies dorso-ventrally and anterior-posteriorly. Most radially symmetric animals are symmetrical about an axis extending from the center of the oral surface, which contains the mouth, to the center of the opposite, or aboral, end. This type of symmetry is especially suitable for sessile animals such as the sea anemone, floating animals such as jellyfish, and slow moving organisms such as sea stars (see special forms of radial symmetry). Animals in the phyla cnidaria and echinodermata exhibit radial symmetry (although many sea anemones and some corals exhibit bilateral symmetry defined by a single structure, the siphonoglyph) (see Willmer, 1990).
    [Show full text]
  • The Early History of the Metazoa—A Paleontologist's Viewpoint
    ISSN 20790864, Biology Bulletin Reviews, 2015, Vol. 5, No. 5, pp. 415–461. © Pleiades Publishing, Ltd., 2015. Original Russian Text © A.Yu. Zhuravlev, 2014, published in Zhurnal Obshchei Biologii, 2014, Vol. 75, No. 6, pp. 411–465. The Early History of the Metazoa—a Paleontologist’s Viewpoint A. Yu. Zhuravlev Geological Institute, Russian Academy of Sciences, per. Pyzhevsky 7, Moscow, 7119017 Russia email: [email protected] Received January 21, 2014 Abstract—Successful molecular biology, which led to the revision of fundamental views on the relationships and evolutionary pathways of major groups (“phyla”) of multicellular animals, has been much more appre ciated by paleontologists than by zoologists. This is not surprising, because it is the fossil record that provides evidence for the hypotheses of molecular biology. The fossil record suggests that the different “phyla” now united in the Ecdysozoa, which comprises arthropods, onychophorans, tardigrades, priapulids, and nemato morphs, include a number of transitional forms that became extinct in the early Palaeozoic. The morphology of these organisms agrees entirely with that of the hypothetical ancestral forms reconstructed based on onto genetic studies. No intermediates, even tentative ones, between arthropods and annelids are found in the fos sil record. The study of the earliest Deuterostomia, the only branch of the Bilateria agreed on by all biological disciplines, gives insight into their early evolutionary history, suggesting the existence of motile bilaterally symmetrical forms at the dawn of chordates, hemichordates, and echinoderms. Interpretation of the early history of the Lophotrochozoa is even more difficult because, in contrast to other bilaterians, their oldest fos sils are preserved only as mineralized skeletons.
    [Show full text]
  • 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. Lecture 13 Chitin (C8H13O5N)n (pronounced /kaɪtən/) is a long‐chain polymer of a N‐acetylglucosamine, a derivative of glucose, and it is found in many places throughout the natural world. It is the main component of the cell walls of fungi, the exoskeletons of arthropods, such as crustaceans (like the crab, lobster and shrimp) and the insects, including ants, beetles and butterflies, the radula of mollusks and the beaks of the cephalopods, including squid and octopuses. Chitin has also proven useful for several medical and industrial purposes. Chitin is a biological substance which may be compared to the polysaccharide cellulose and to the protein keratin. Although keratin is a protein, and not a carbohydrate, both keratin and chitin have similar structural functions. Keratin Keratins are a family of fibrous structural proteins; tough and insoluble, they form the hard but nonmineralized structures found in reptiles, birds, amphibians and mammals. They are rivaled as biological materials in toughness only by chitin. There are various types of keratins within a single animal. Keratins are the main constituent of structures that grow from the skin: • the α-keratins in the hair (including wool), horns, nails, claws and hooves of mammals[verification needed] • the harder β-keratins in the scales and claws of reptiles, their shells (chelonians, such as tortoise, turtle, terrapin), and in the feathers, beaks, and claws of birds.[verification needed] (These keratins are formed primarily in beta sheets.
    [Show full text]
  • Lecture 23 the Cambrian Explosion Life on Earth - Timescale
    Lecture 23 The Cambrian explosion Life on Earth - Timescale Precambrian (4,600 to 543 MYA) (MYA = million years ago) - life on earth evolved about 3,800 MYA. - prokaryotes evolved about 3,500 MYA - eukaryotes evolved about 2,100 MYA - multicellular eukaryotes appeared about 1,500 MYA. Life on Earth - Timescale Differences between Prokaryotes and Eukaryotes 1. much larger cell sizes. 2. a nucleus and organelles. 3. aerobic. 4. cilia and flagella with tubulin rather than flagellin protein. 5. linear DNA molecules complexed with histones 6. commonly being multicellular. 7. both mitosis and meiosis 8. Presence of a cytoskeleton Emergence of Eukaryotes - there is a general trend towards increasing size of fossils 1.9 to 1.3 bya - average sizes of fossils increased from 10 microns to 60 to 80 microns. This is consistent with the increased size of eukaryotic cells and the increasing levels of O2 during this period (by 1.9 bya it was 15% of its current level). - the earliest possible eukaryote has been dated to about 1.8 bya in the Canadian shield region. Serial Endosymbiotic Hypothesis - all mitochondria are monophyletic – they all trace to a proteobacterial ancestor. - unlike mitochondria, chloroplasts have evolved several (4?) times – they are polyphyletic! - Margulis also argues that cilia/flagella were similarly acquired. Endosymbioses 1. The ciliate Paramecium bursaria and green algae (Chlorella) - the ciliate readily uptakes the algae which supplies carbon compounds from photosynthesis. - similar to early chloroplast evolution? 2. The anaerobic amoeba, Pelomyxa palustris (lacks mitochondria) - the amoeba readily uptakes aerobic bacteria and then switches to requiring oxygen. - similar to early mitochondrial evolution? 3.
    [Show full text]
  • The Weng'an Biota (Doushantuo Formation): an Ediacaran Window on Soft-Bodied and Multicellular Microorganisms
    Cunningham, J. A., Vargas, K., Yin, Z., Bengtson, S., & Donoghue, P. C. J. (2017). The Weng’an Biota (Doushantuo Formation): an Ediacaran window on soft bodied and multicellular microorganisms. Journal of the Geological Society, 174(5), 793-802. https://doi.org/10.1144/jgs2016-142 Publisher's PDF, also known as Version of record License (if available): CC BY Link to published version (if available): 10.1144/jgs2016-142 Link to publication record in Explore Bristol Research PDF-document This is the final published version of the article (version of record). It first appeared online via The Geological Society at http://jgs.geoscienceworld.org/content/early/2017/04/27/jgs2016-142. Please refer to any applicable terms of use of the publisher. University of Bristol - Explore Bristol Research General rights This document is made available in accordance with publisher policies. Please cite only the published version using the reference above. Full terms of use are available: http://www.bristol.ac.uk/red/research-policy/pure/user-guides/ebr-terms/ Review Focus Journal of the Geological Society Published Online First https://doi.org/10.1144/jgs2016-142 The Weng’an Biota (Doushantuo Formation): an Ediacaran window on soft-bodied and multicellular microorganisms John A. Cunningham1,2*, Kelly Vargas1, Zongjun Yin3, Stefan Bengtson2 & Philip C. J. Donoghue1 1 School of Earth Sciences, University of Bristol, Life Sciences Building, 24 Tyndall Avenue, Bristol BS8 1TQ, UK 2 Department of Palaeobiology and Nordic Center for Earth Evolution, Swedish Museum of Natural History, 10405 Stockholm, Sweden 3 State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China K.V., 0000-0003-1320-4195; S.B., 0000-0003-0206-5791; P.C.J.D., 0000-0003-3116-7463 * Correspondence: [email protected] Abstract: The Weng’an Biota is a fossil Konservat-Lagerstätte in South China that is c.
    [Show full text]
  • Darwin's Doubt
    Advancing the Scientific Debate In Paperback Now with a New Epilogue Purchase today at www.DarwinsDoubt.com Darwin’s Doubt: A Discussion Guide Introduction This discussion guide is designed to facilitate the use of Stephen Meyer’s book Darwin’s Doubt: The Explosive Origin of Animal Life and the Case for Intelligent Design in small groups, adult education classes, and book discussion clubs. The guide contains brief summaries of each chapter grouped into eight total discussion sessions. Each discussion session also contains discussion questions for the chapters covered by that session. Permission is hereby granted to distribute and reproduce this guide in whole or in part for non- commercial educational use, provided that: (1) the original source is credited; (2) any copies display the web addresses for Discovery Institute’s Center for Science and Culture (www.discovery.org/csc), IntelligentDesign.org (www.intelligentdesign.org), and the official Darwin’s Doubt website (www.darwinsdoubt.com); and (3) the copies are distributed free of charge. Contents Session 1 (p. 4) Prologue; Chapter 1: Darwin’s Nemesis; Chapter 2: The Burgess Bestiary Session 2 (p. 7) Chapter 3: Soft Bodies and Hard Facts; Chapter 4: The Not Missing Fossils? Session 3 (p. 10) Chapter 5: The Genes Tell the Story?; Chapter 6: The Animal Tree of Life; Chapter 7: Punk Eek! Session 4 (p. 14) Chapter 8: The Cambrian Information Explosion; Chapter 9: Combinatorial Inflation; Chapter 10: The Origin of Genes and Proteins Session 5 (p. 18) Chapter 11: Assume a Gene; Chapter 12: Complex Adaptations and the Neo- Darwinian Math Session 6 (p.
    [Show full text]
  • Two Schools of Evolutionary Thought
    Evolution of centralized nervous systems: Two schools of evolutionary thought R. Glenn Northcutt1 Laboratory of Comparative Neurobiology, Scripps Institution of Oceanography and Department of Neurosciences, University of California at San Diego, La Jolla, CA 92093 Edited by John C. Avise, University of California, Irvine, CA, and approved May 1, 2012 (received for review February 27, 2012) Understanding the evolution of centralized nervous systems Fossil Record requires an understanding of metazoan phylogenetic interrela- The fossil record is notoriously incomplete. Fossils essentially exist tionships, their fossil record, the variation in their cephalic neural as snapshots in time, and these snapshots are of varying quality. characters, and the development of these characters. Each of these Some are grainy, providing only a glimpse of organisms and their topics involves comparative approaches, and both cladistic and ecology; others are fine-grained photographs of individual taxa phenetic methodologies have been applied. Our understanding of and their ecology (Lagerstätten). Regardless, each snapshot metazoan phylogeny has increased greatly with the cladistic provides unique and critical insights into the minimal age of a analysis of molecular data, and relaxed molecular clocks gener- radiation. Each snapshot helps calibrate molecular clocks, establish ally date the origin of bilaterians at 600–700 Mya (during the ecological settings of evolutionary events, and reveal unsuspected Ediacaran). Although the taxonomic affinities of the Ediacaran bi- morphological characters that challenge current conclusions re- ota remain uncertain, a conservative interpretation suggests that garding character transformation (2). a number of these taxa form clades that are closely related, if not stem clades of bilaterian crown clades. Analysis of brain–body Ediacaran Biota.
    [Show full text]
  • Was the Eumetazoan Ancestor a Holopelagic, Planktotrophic Gastraea? Claus Nielsen
    Nielsen BMC Evolutionary Biology 2013, 13:171 http://www.biomedcentral.com/1471-2148/13/171 REVIEW Open Access Life cycle evolution: was the eumetazoan ancestor a holopelagic, planktotrophic gastraea? Claus Nielsen Abstract Background: Two theories for the origin of animal life cycles with planktotrophic larvae are now discussed seriously: The terminal addition theory proposes a holopelagic, planktotrophic gastraea as the ancestor of the eumetazoans with addition of benthic adult stages and retention of the planktotrophic stages as larvae, i.e. the ancestral life cycles were indirect. The intercalation theory now proposes a benthic, deposit-feeding gastraea as the bilaterian ancestor with a direct development, and with planktotrophic larvae evolving independently in numerous lineages through specializations of juveniles. Results: Information from the fossil record, from mapping of developmental types onto known phylogenies, from occurrence of apical organs, and from genetics gives no direct information about the ancestral eumetazoan life cycle; however, there are plenty of examples of evolution from an indirect development to direct development, and no unequivocal example of evolution in the opposite direction. Analyses of scenarios for the two types of evolution are highly informative. The evolution of the indirect spiralian life cycle with a trochophora larva from a planktotrophic gastraea is explained by the trochophora theory as a continuous series of ancestors, where each evolutionary step had an adaptational advantage. The loss of ciliated larvae in the ecdysozoans is associated with the loss of outer ciliated epithelia. A scenario for the intercalation theory shows the origin of the planktotrophic larvae of the spiralians through a series of specializations of the general ciliation of the juvenile.
    [Show full text]
  • Chen Et Al., Science 2004
    Small Bilaterian Fossils from 40 to 55 Million Years Before the Cambrian Jun-Yuan Chen, et al. Science 305, 218 (2004); DOI: 10.1126/science.1099213 The following resources related to this article are available online at www.sciencemag.org (this information is current as of October 14, 2008 ): Updated information and services, including high-resolution figures, can be found in the online version of this article at: http://www.sciencemag.org/cgi/content/full/305/5681/218 Supporting Online Material can be found at: http://www.sciencemag.org/cgi/content/full/1099213/DC1 A list of selected additional articles on the Science Web sites related to this article can be found at: http://www.sciencemag.org/cgi/content/full/305/5681/218#related-content This article cites 16 articles, 9 of which can be accessed for free: http://www.sciencemag.org/cgi/content/full/305/5681/218#otherarticles on October 14, 2008 This article has been cited by 39 article(s) on the ISI Web of Science. This article has been cited by 15 articles hosted by HighWire Press; see: http://www.sciencemag.org/cgi/content/full/305/5681/218#otherarticles This article appears in the following subject collections: Paleontology http://www.sciencemag.org/cgi/collection/paleo www.sciencemag.org Information about obtaining reprints of this article or about obtaining permission to reproduce this article in whole or in part can be found at: http://www.sciencemag.org/about/permissions.dtl Downloaded from Science (print ISSN 0036-8075; online ISSN 1095-9203) is published weekly, except the last week in December, by the American Association for the Advancement of Science, 1200 New York Avenue NW, Washington, DC 20005.
    [Show full text]
  • Distinguishing Biology from Geology in Soft-Tissue Preservation
    DISTINGUISHING BIOLOGY FROM GEOLOGY! IN SOFT-TISSUE PRESERVATION 1,2 1 2 ! JOHN A. CUNNINGHAM, PHILIP C. J. DONOGHUE, AND STEFAN BENGTSON 1School of Earth Sciences, University of Bristol, Bristol BS8 1RJ UK <[email protected]! > 2Department of Palaeobiology and Nordic Centre for Earth Evolution, Swedish Museum of Natural History, 10405 Stockholm, Sweden ABSTRACT.—Knowledge of evolutionary history is based extensively on relatively rare fossils that preserve soft tissues. These fossils record a much greater proportion of anatomy than would be known solely from mineralized remains and provide key data for testing evolutionary hypotheses in deep time. Ironically, however, exceptionally preserved fossils are often among the most contentious because they are difficult to interpret. This is because their morphology has invariably been affected by the processes of decay and diagenesis, meaning that it is often difficult to distinguish preserved biology from artifacts introduced by these processes. Here we describe how a range of analytical techniques can be used to tease apart mineralization that preserves biological structures from unrelated geological mineralization phases. This approach involves using a series of X-ray, ion, electron and laser beam techniques to characterize the texture and chemistry of the different phases so that they can be differentiated in material that is difficult to interpret. This approach is demonstrated using a case study of its application to the study of fossils from the Ediacaran Doushantuo Biota. INTRODUCTION another. This would be a mistake: these organisms ! have invariably undergone microbial decay, which The bulk of the animal fossil record consists of often plays a key role in the authigenic biomineralized remains such as bones, teeth, or mineralization of soft tissues (Briggs, 2003; shells.
    [Show full text]