The Bizarre Species That Are Rewriting Animal Evolution
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The Ediacaran Frondose Fossil Arborea from the Shibantan Limestone of South China
Journal of Paleontology, 94(6), 2020, p. 1034–1050 Copyright © 2020, The Paleontological Society. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/ licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. 0022-3360/20/1937-2337 doi: 10.1017/jpa.2020.43 The Ediacaran frondose fossil Arborea from the Shibantan limestone of South China Xiaopeng Wang,1,3 Ke Pang,1,4* Zhe Chen,1,4* Bin Wan,1,4 Shuhai Xiao,2 Chuanming Zhou,1,4 and Xunlai Yuan1,4,5 1State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology and Center for Excellence in Life and Palaeoenvironment, Chinese Academy of Sciences, Nanjing 210008, China <[email protected]><[email protected]> <[email protected]><[email protected]><[email protected]><[email protected]> 2Department of Geosciences, Virginia Tech, Blacksburg, Virginia 24061, USA <[email protected]> 3University of Science and Technology of China, Hefei 230026, China 4University of Chinese Academy of Sciences, Beijing 100049, China 5Center for Research and Education on Biological Evolution and Environment, Nanjing University, Nanjing 210023, China Abstract.—Bituminous limestone of the Ediacaran Shibantan Member of the Dengying Formation (551–539 Ma) in the Yangtze Gorges area contains a rare carbonate-hosted Ediacara-type macrofossil assemblage. This assemblage is domi- nated by the tubular fossil Wutubus Chen et al., 2014 and discoidal fossils, e.g., Hiemalora Fedonkin, 1982 and Aspidella Billings, 1872, but frondose organisms such as Charnia Ford, 1958, Rangea Gürich, 1929, and Arborea Glaessner and Wade, 1966 are also present. -
The Cambrian Explosion: a Big Bang in the Evolution of Animals
The Cambrian Explosion A Big Bang in the Evolution of Animals Very suddenly, and at about the same horizon the world over, life showed up in the rocks with a bang. For most of Earth’s early history, there simply was no fossil record. Only recently have we come to discover otherwise: Life is virtually as old as the planet itself, and even the most ancient sedimentary rocks have yielded fossilized remains of primitive forms of life. NILES ELDREDGE, LIFE PULSE, EPISODES FROM THE STORY OF THE FOSSIL RECORD The Cambrian Explosion: A Big Bang in the Evolution of Animals Our home planet coalesced into a sphere about four-and-a-half-billion years ago, acquired water and carbon about four billion years ago, and less than a billion years later, according to microscopic fossils, organic cells began to show up in that inert matter. Single-celled life had begun. Single cells dominated life on the planet for billions of years before multicellular animals appeared. Fossils from 635,000 million years ago reveal fats that today are only produced by sponges. These biomarkers may be the earliest evidence of multi-cellular animals. Soon after we can see the shadowy impressions of more complex fans and jellies and things with no names that show that animal life was in an experimental phase (called the Ediacran period). Then suddenly, in the relatively short span of about twenty million years (given the usual pace of geologic time), life exploded in a radiation of abundance and diversity that contained the body plans of almost all the animals we know today. -
Page - Paleo Lab 06 - the Cambrian Explosion of Life
page - Paleo Lab 06 - The Cambrian Explosion of Life An Introduction to Index Fossils CLASSIFICATION AND TAXONOMY Geologists follow the lead of biologists in the classification and naming of organisms (taxonomy after taxon = name). Since its introduction early in the 18th century, the system devised by Linnaeus has been used to categorize organisms and to affix a formal name to each species. Major classification categories or groupings are listed below on the left with an example using the species of the common house cat to show how the system may be used: KINGDOM Animalia PHYLUM Chordata CLASS Mammalia ORDER Carnivora FAMILY Felidae GENUS Felis SPECIES domestica The basic unit of the system is the species, and each category above it includes the divisions below. A two part (binomial) formal designation for each species, following the scheme of Linnaeus, is composed of the capitalized name of the genus (plural = genera) followed by the uncapitalized name of the species (plural = species). Note that the binomial is printed in a special way (italics) to distinguish it. After at least 5000 years of domestication, man has drawn out of that species such a variety of traits through selection and cross-breeding that it may be more difficult to realize that all such cats belong to the same species than it is to recognize that they share the same genus with the lion (Felis leo), leopard (Felis pardus), jaguar (Felis onca), tiger (Felis tigris), and the cougar or puma (Felis concolor). All wildcats belong to the same genus but are classified in three separate species found in Europe, Africa, and the Americas (the ocelot), Felis sylvestris, F. -
Frondose and Turf-Dominated Marine Habitats Support Distinct Trophic Pathways: Evidence from 15N and 13C Stable Isotope Analyses
Arquipelago - Life and Marine Sciences ISSN: 0873-4704 Frondose and turf-dominated marine habitats support distinct trophic pathways: evidence from 15N and 13C stable isotope analyses CLÁUDIA HIPÓLITO, RAUL M.A. NETO, TARSO M.M. COSTA, MARIA A. DIONÍSIO, AFONSO C.L. PRESTES, JOSÉ M.N. AZEVEDO, GUSTAVO M. MARTINS AND ANA I. NETO Hipólito, C., R.M.A. Neto, T.M.M. Costa, M.A. Dionísio, A.C.L. Prestes, J.M.N. Azevedo, G.M. Martins and A.I. Neto 2020. Frondose and turf-dominated marine habitats support distinct trophic pathways: evidence from 15N and 13C stable isotope analyses. Arquipelago. Life and Marine Sciences 37: 37 – 44. https://doi.org/10.25752/arq.23546 Marine vegetation plays an important structuring role, delivering key functions and services to coastal systems the extent of which depends on the foundation species and their architecture. In increasingly urbanised coastlines, turf-forming macroalgae are replacing frondose morphotypes. Trophic relationships within these systems can be studied through stable isotope analysis of the different food web compartments. In the present study, we investigated trophic pathways in two distinct macroalgal assemblages: one dominated by small brown frondose algae, and one dominated by low-lying turf-forming species. 15N and 13C isotopic signatures were determined for selected macroalgae and sedentary animals from distinct trophic levels, collected from two habitats on São Miguel Island (Azores, Portugal). In frondose habitats macroalgae appeared to make up the primary carbon source for the entire food web, whilst in turf-dominated habitats there was a decouple between macroalgae and higher trophic levels. -
The Ediacaran Frondose Fossil Arborea from the Shibantan Limestone of South China
Journal of Paleontology, 94(6), 2020, p. 1034–1050 Copyright © 2020, The Paleontological Society. This is an Open Access article, distributed under the terms of the Creative Commons Attribution licence (http://creativecommons.org/ licenses/by/4.0/), which permits unrestricted re-use, distribution, and reproduction in any medium, provided the original work is properly cited. 0022-3360/20/1937-2337 doi: 10.1017/jpa.2020.43 The Ediacaran frondose fossil Arborea from the Shibantan limestone of South China Xiaopeng Wang,1,3 Ke Pang,1,4* Zhe Chen,1,4* Bin Wan,1,4 Shuhai Xiao,2 Chuanming Zhou,1,4 and Xunlai Yuan1,4,5 1State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology and Center for Excellence in Life and Palaeoenvironment, Chinese Academy of Sciences, Nanjing 210008, China <[email protected]><[email protected]> <[email protected]><[email protected]><[email protected]><[email protected]> 2Department of Geosciences, Virginia Tech, Blacksburg, Virginia 24061, USA <[email protected]> 3University of Science and Technology of China, Hefei 230026, China 4University of Chinese Academy of Sciences, Beijing 100049, China 5Center for Research and Education on Biological Evolution and Environment, Nanjing University, Nanjing 210023, China Abstract.—Bituminous limestone of the Ediacaran Shibantan Member of the Dengying Formation (551–539 Ma) in the Yangtze Gorges area contains a rare carbonate-hosted Ediacara-type macrofossil assemblage. This assemblage is domi- nated by the tubular fossil Wutubus Chen et al., 2014 and discoidal fossils, e.g., Hiemalora Fedonkin, 1982 and Aspidella Billings, 1872, but frondose organisms such as Charnia Ford, 1958, Rangea Gürich, 1929, and Arborea Glaessner and Wade, 1966 are also present. -
The Cambrian Explosion: Biology's Big Bang
© 2001 by Stephen C. Meyer, P. A. Nelson, and Paul Chien. All Rights Reserved. The Cambrian Explosion: Biology’s Big Bang by Stephen C. Meyer, P. A. Nelson, and Paul Chien I. INTRODUCTION: DESIGN WITHOUT A DESIGNER? Both Darwin himself, and contemporary neo-Darwinists such as Francisco Ayala, Richard Dawkins and Richard Lewontin, acknowledge that biological organisms appear to have been designed by an intelligence. Yet classical Darwinists and contemporary Darwinists alike have argued that what Francisco Ayala calls the “obvious design” of living things is only apparent. As Ayala, 1994 president of the American Association for the Advancement of Science, has explained: The functional design of organisms and their features would therefore seem to argue for the existence of a designer. It was Darwin’s greatest accomplishment to show that the directive organization of living beings can be explained as the result of a natural process, natural selection, without any need to resort to a Creator or other external agent. ....[Darwin’s] mechanism, natural selection, excluded God as the explanation accounting for the obvious design of organisms.1 According to Darwin, and his contemporary followers, the mechanism of natural selection acting on random variation suffices to explain the origin of those features of life that once seemed to require explanation by reference to an intelligent designer. Thus, according to Darwinists, the design hypothesis now represents an unnecessary and unparsimonious explanation for the complexity and apparent design of living organisms. On these as well as methodological grounds contemporary biologists have generally excluded the design hypothesis from consideration as an explanation for the origin of biological structure. -
Assessment of Coral Reefs Using Herbivory
FAU Institutional Repository http://purl.fcla.edu/fau/fauir This paper was submitted by the faculty of FAU’s Harbor Branch Oceanographic Institute. Notice: ©2006 John Wiley & Sons, Ltd. This manuscript is an author version with the final publication available at http://www.interscience.wiley.com and may be cited as: Littler, M. M., & Littler, D. S. (2007). Assessment of coral reefs using herbivory/nutrient assays and indicator groups of benthic primary producers: a critical synthesis, proposed protocols, and critique of management strategies. Aquatic Conservation: Marine and Freshwater Ecosystems. 17(2), 195‐215. doi:10.1002/aqc.790 AQUATIC CONSERVATION: MARINE AND FRESHWATER ECOSYSTEMS Aquatic Conserv: Mar. Freshw. Ecosyst. 17: 195–215 (2007) Published online 8 August 2006 in Wiley InterScience (www.interscience.wiley.com) DOI: 10.1002/aqc.790 REVIEW Assessment of coral reefs using herbivory/nutrient assays and indicator groups of benthic primary producers: a critical synthesis, proposed protocols, and critique of management strategiesy MARK M. LITTLER* and DIANE S. LITTLER Smithsonian Institution, National Museum of Natural History, Department of Botany, Washington, DC, USA ABSTRACT 1. Rapid assessment protocols for determining and monitoring the status of any given coral reef are provided and include measuring: (a) standing stocks of functional indicator groups, (b) herbivore populations, (c) water-column nutrient levels, (d) tissue C:N:P ratios, (e) algal physiological-response assays, and (f) herbivory assays. These measurements can reveal quantitative tipping-point levels beyond which resilience to undesirable phase shifts begins to become critically reduced. Universal tipping-point approximations are reviewed for inorganic nutrients, and posited for the first time for herbivory. -
The Cambrian Explosion and the Origins of Diversity
Focus: Illuminating Science credit: http://rst.gsfc.nasa.gov/Sect20/A12c.html The Cambrian Explosion and the Origins of Diversity here is a grandeur in this view environmental change or fundamental By Anirudh Penumaka Tof life.” Darwin famously wrote PRGLÀFDWLRQWRWKHRUJDQLVPVWKHP- these words about his theory of evo- selves which suddenly open the door lution, and indeed there is something for many new forms of life to arise. astounding about the idea that change $VSHFLÀFSHULRGRI LQFUHDVHGHYROX- “During the Cambrian is the only constant of life, mirroring tion, commonly called the Cambrian yet also transcending the change we “explosion,” occurred approximately ‘explosion,’ life on Earth FDQVHHLQWKHÁHHWLQJOHQJWKRIKXPDQ 560 million years ago (2). Life on Earth underwent a massive lifetimes (1). Over billions of years, underwent a massive surge that created and as the result of a calculus we are all of the major phyla of organisms that surge that created all of only beginning to untangle, life evolved exist even today. Life, which had been from simple, single celled forms into primarily unicellular, quickly became the major phyla of or- complex organisms, some of which multicellular, and organisms evolved ganisms that exist even are capable of emotion, thought, and much more complex morphologies than strikingly, consciousness. But this slow had previously existed (2). today” march of gradual change by means of The Cambrian explosion witnessed natural selection may not be that-a the appearance of diverse phyla includ- slow march-after all. Evolution may ing those characterized by mineralized instead proceed through periods of long skeletons such as Arthropoda, Echino- stagnation, interspersed with periods dermata, Mollusca, and Brachiopoda, RILQFUHGLEOHDQGUDSLGGLYHUVLÀFDWLRQ in addition to phyla made up of soft to generate the vastly different organ- bodied species such as Annelida, isms that inhabit the Earth today. -
The Cambrian ''Explosion'
Perspective The Cambrian ‘‘explosion’’: Slow-fuse or megatonnage? Simon Conway Morris* Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, United Kingdom Clearly, the fossil record from the Cambrian period is an invaluable tool for deciphering animal evolution. Less clear, however, is how to integrate the paleontological information with molecular phylogeny and developmental biology data. Equally challenging is answering why the Cambrian period provided such a rich interval for the redeployment of genes that led to more complex bodyplans. illiam Buckland knew about it, The First Metazoans. Ediacaran assem- 1). The overall framework of early meta- WCharles Darwin characteristically blages (2, 5) are presumably integral to zoan evolution comes from molecular agonized over it, and still we do not fully understanding the roots of the Cambrian data, but they cannot provide insights into understand it. ‘‘It,’’ of course, is the seem- ‘‘explosion,’’ and this approach assumes the anatomical changes and associated ingly abrupt appearance of animals in the that the fossil record is historically valid. It changes in ecology that accompanied the Cambrian ‘‘explosion.’’ The crux of this is markedly at odds, however, with an emergence of bodyplans during the Cam- evolutionary problem can be posed as a alternative view, based on molecular data. brian explosion. The fossil record series of interrelated questions. Is it a real These posit metazoan divergences hun- provides, therefore, a unique historical event or simply an artifact of changing dreds of millions of years earlier (6, 7). As perspective. fossilization potential? If the former, how such, the origination of animals would be Only those aspects of the Ediacaran rapidly did it happen and what are its more or less coincident with the postu- record relevant to the Cambrian diversi- consequences for understanding evolu- lated ‘‘Big Bang’’ of eukaryote diversifi- fication are noted here. -
The Nature of Macroalgae and Their Interactions on Reefs Mark M
The Nature of Macroalgae and Their Interactions on Reefs Mark M. Littler and Diane S. Littler ABSTRACT. What was known about tropical reef algae prior to the use of scuba came largely from dredging studies or drift collections, which usually resulted in highly mutilated specimens and questionable habitat data. Scuba allows a precise determination of ecological conditions and permits in situ photography, two techniques our group has relied on during the past three decades for quan- titative studies and field guide production. A goal of this review is to familiarize the scientific diving community with the kinds and roles of algae on tropical reefs, with the hope that seaweeds will be utilized more fully as tools for addressing important ecological questions. ecause of the rapid degradation of tropical reefs worldwide, it is imperative that the role and diversity of macroalgae be studied in a timely, efficient, and scientifi- Bcally verifiable manner. It is of paramount importance to characterize the world’s coral reef environments and to understand the responses of foundation species. The fleshy macroalgal forms are the food of herbivores, and only become abundant when their pro- duction rate exceeds the capacity of herbivores to consume them. On healthy oligotrophic coral reefs, even very low nutrient increases may shift relative dominance from corals (Cnidaria) to macroalgae by both stimulating macroalgal production and inhibiting cor- als. As a result, frondose macroalgae are generally recognized as harmful to the longevity of coral reefs due to the link between excessive blooms and coastal eutrophication. Reef plant complexity has evolved along very different evolutionary lines. -
Cambrian Explosion of Life: the Big Bang in Metazoan Evolution
GENERAL I ARTICLE Cambrian Explosion of Life: the Big Bang in Metazoan Evolution P V Sukumaran Despite the protracted history of life on earth spanning well over 3.8 Ga, fossil record of the Precambrian (>543 Ma) largely documents only microscopic life. The mostly simple Precambrian life forms were followed by a sudden explosive radiation of multicellular animals at the tum of the Cam brian period (543-490 Ma) between 530 and 520 Ma ago, when almost two-thirds of the animal phyla make their dramatic appearance in the fossil record. This unusual and amazing burst of macroevolutionary change is called the P V Sukumaran has been Cambrian explosion. working with the Geologi cal Survey of India since In all probability life originated on earth ~ 4 Ga ago (Giga 1974. His interests include, 9 among others, origin and annum = 10 years; see Sukumaran, Resonance: October and early evolution of life. November 2001). Despite this long history, multicellular life (the terms metazoans, multicellular animals and animals are syn onymous) appears first in the fossil record (see Box 1) only between 530 and 520 Ma (Mega an~um= 106 years), after a gap of nearly 3.5 Ga since the origin of life. Amazingly, when they arrived, they arrived in profusion and geologically very abruptly. The sudden and explosive diversification of life forms at the early Cambrian period as documented in the fossil record is called the Cambrian explosion. Palaeontologists, evolutionary biologists and geneticists hotly debate the causes of this extraor dinary event in the evolutionary history of life. Recent advances in genetics and molecular biology have shed new light on genetic controls of body plan development (see Box 2) in metazoan phyla. -
Ediacaran Life Close to Land: Coastal and Shoreface Habitats of the Ediacaran Macrobiota, the Central Flinders Ranges, South Australia
Journal of Sedimentary Research, 2020, v. 90, 1463–1499 Research Article DOI: 10.2110/jsr.2020.029 EDIACARAN LIFE CLOSE TO LAND: COASTAL AND SHOREFACE HABITATS OF THE EDIACARAN MACROBIOTA, THE CENTRAL FLINDERS RANGES, SOUTH AUSTRALIA 1 2 2 1 WILLIAM J. MCMAHON,* ALEXANDER G. LIU, BENJAMIN H. TINDAL, AND MAARTEN G. KLEINHANS 1Faculty of Geosciences, Utrecht University, Princetonlaan 8a, 3584 CB, Utrecht, The Netherlands 2Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, U.K. [email protected] ABSTRACT: The Rawnsley Quartzite of South Australia hosts some of the world’s most diverse Ediacaran macrofossil assemblages, with many of the constituent taxa interpreted as early representatives of metazoan clades. Globally, a link has been recognized between the taxonomic composition of individual Ediacaran bedding-plane assemblages and specific sedimentary facies. Thorough characterization of fossil-bearing facies is thus of fundamental importance for reconstructing the precise environments and ecosystems in which early animals thrived and radiated, and distinguishing between environmental and evolutionary controls on taxon distribution. This study refines the paleoenvironmental interpretations of the Rawnsley Quartzite (Ediacara Member and upper Rawnsley Quartzite). Our analysis suggests that previously inferred water depths for fossil-bearing facies are overestimations. In the central regions of the outcrop belt, rather than shelf and submarine canyon environments below maximum (storm-weather) wave base,