Palaeontology
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A New Species of Yunnanozoan with Implications for Deuterostome
R EPORTS istry, K. S. Birdi, Ed. (CRC Press Inc., Boca Raton, FL, 23. L. H. Sperling, Polymeric Multicomponent Materials (grant EA/TU¨ BA-GEBI˙P/2001-1-1) and the Koc¸ Uni- 1997), chap. 9. (Wiley-Interscience, New York, 1997), chap. 6. versity Fiat Fund. 18. , G. McHale, M. I. Newton, Langmuir 18, 2636 24. J. Varga, in Polypropylene Structure, Blends and Com- Supporting Online Material (2002). posites, J. Karger-Kocsis, Ed. (Chapman and Hall, Lon- www.sciencemag.org/cgi/content/full/299/5611/1377/ 19. Materials and methods are available as supporting don, 1995), vol. 1, chap. 3. DC1 material on Science Online. 25. We thank A. Altay, M. A. Gu¨lgu¨n of Sabancı Univer- Materials and Methods 20. R. N. Wenzel, Ind. Eng. Chem. 28, 988 (1936). sity, and A. Alkan of Brisa for their help with SEM Figs. S1 and S2 21. A. B. D. Cassie, S. Baxter, Trans. Faraday Soc. 3, 16 (1944). measurements. A.L.D. acknowledges the financial References 22. R. A. Veselovsky, V. N. Kestelman, Adhesion of Poly- support of the Turkish Academy of Sciences in the mers (McGraw-Hill, New York, 2002), chap. 2. framework of the Young Scientist Award Program 11 September 2002; accepted 22 January 2003 and ventral units are rarely touching (Fig. 1, A New Species of Yunnanozoan G and H), suggesting that the entire anterior region could expand and contract in height. with Implications for The expansion would occur by an accommo- dation along the median zone and about an axis of rotation near the posterior of the units. -
Timeline of the Evolutionary History of Life
Timeline of the evolutionary history of life This timeline of the evolutionary history of life represents the current scientific theory Life timeline Ice Ages outlining the major events during the 0 — Primates Quater nary Flowers ←Earliest apes development of life on planet Earth. In P Birds h Mammals – Plants Dinosaurs biology, evolution is any change across Karo o a n ← Andean Tetrapoda successive generations in the heritable -50 0 — e Arthropods Molluscs r ←Cambrian explosion characteristics of biological populations. o ← Cryoge nian Ediacara biota – z ← Evolutionary processes give rise to diversity o Earliest animals ←Earliest plants at every level of biological organization, i Multicellular -1000 — c from kingdoms to species, and individual life ←Sexual reproduction organisms and molecules, such as DNA and – P proteins. The similarities between all present r -1500 — o day organisms indicate the presence of a t – e common ancestor from which all known r Eukaryotes o species, living and extinct, have diverged -2000 — z o through the process of evolution. More than i Huron ian – c 99 percent of all species, amounting to over ←Oxygen crisis [1] five billion species, that ever lived on -2500 — ←Atmospheric oxygen Earth are estimated to be extinct.[2][3] Estimates on the number of Earth's current – Photosynthesis Pong ola species range from 10 million to 14 -3000 — A million,[4] of which about 1.2 million have r c been documented and over 86 percent have – h [5] e not yet been described. However, a May a -3500 — n ←Earliest oxygen 2016 -
Constraints on the Timescale of Animal Evolutionary History
Palaeontologia Electronica palaeo-electronica.org Constraints on the timescale of animal evolutionary history Michael J. Benton, Philip C.J. Donoghue, Robert J. Asher, Matt Friedman, Thomas J. Near, and Jakob Vinther ABSTRACT Dating the tree of life is a core endeavor in evolutionary biology. Rates of evolution are fundamental to nearly every evolutionary model and process. Rates need dates. There is much debate on the most appropriate and reasonable ways in which to date the tree of life, and recent work has highlighted some confusions and complexities that can be avoided. Whether phylogenetic trees are dated after they have been estab- lished, or as part of the process of tree finding, practitioners need to know which cali- brations to use. We emphasize the importance of identifying crown (not stem) fossils, levels of confidence in their attribution to the crown, current chronostratigraphic preci- sion, the primacy of the host geological formation and asymmetric confidence intervals. Here we present calibrations for 88 key nodes across the phylogeny of animals, rang- ing from the root of Metazoa to the last common ancestor of Homo sapiens. Close attention to detail is constantly required: for example, the classic bird-mammal date (base of crown Amniota) has often been given as 310-315 Ma; the 2014 international time scale indicates a minimum age of 318 Ma. Michael J. Benton. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Philip C.J. Donoghue. School of Earth Sciences, University of Bristol, Bristol, BS8 1RJ, U.K. [email protected] Robert J. -
Chordates (Phylum Chordata)
A short story Leathem Mehaffey, III, Fall 201993 The First Chordates (Phylum Chordata) • Chordates (our phylum) first appeared in the Cambrian, 525MYA. 94 Invertebrates, Chordates and Vertebrates • Invertebrates are all animals not chordates • Generally invertebrates, if they have hearts, have dorsal hearts; if they have a nervous system it is usually ventral. • All vertebrates are chordates, but not all chordates are vertebrates. • Chordates: • Dorsal notochord • Dorsal nerve chord • Ventral heart • Post-anal tail • Vertebrates: Amphioxus: archetypal chordate • Dorsal spinal column (articulated) and skeleton 95 Origin of the Chordates 96 Haikouichthys Myllokunmingia Note the rounded extension to Possibly the oldest the head bearing sensory vertebrate: showed gill organs bars and primitive vertebral elements Early and primitive agnathan vertebrates of the Early Cambrian (530MYA) Pikaia Note: these organisms were less Primitive chordate, than an inch long. similar to Amphioxus 97 The Cambrian/Ordovician Extinction • Somewhere around 488 million years ago something happened to cause a change in the fauna of the earth, heralding the beginning of the Ordovician Period. • Rather than one catastrophe, the late-Cambrian extinction seems to be a series of smaller extinction events. • Historically the change in fauna (mostly trilobites as the index species) was thought to be due to excessive warmth and low oxygen. • But some current findings point to an oxygen spike due perhaps to continental drift into the tropics, driving rapid speciation and consequent replacement of old with new organisms. 98 Welcome to the Ordovician YOU ARE HERE 99 The Ordovician Sea, 488 million years 100 ago The Ordovician Period lasted almost 45 million years, from 489 to 444 MYA. -
Fish and Amphibians
Fish and Amphibians Geology 331 Paleontology Phylum Chordata: Subphyla Urochordata, Cephalochordata, and: Subphylum Vertebrata Class Agnatha: jawless fish, includes the hagfish, conodonts, lampreys, and ostracoderms (armored jawless fish) Gnathostomates: jawed fish Class Chondrichthyes: cartilaginous fish Class Placoderms: armored fish Class Osteichthyes: bony fish Subclass Actinopterygians: ray-finned fish Subclass Sarcopterygians: lobe-finned fish Order Dipnoans: lung fish Order Crossopterygians: coelocanths and rhipidistians Class Amphibia Urochordates: Sea Squirts. Adults have a pharynx with gill slits. Larval forms are free-swimming and have a notochord. Chordates are thought to have evolved from the larval form by precocious sexual maturation. Chordate evolution Cephalochordate: Branchiostoma, the lancelet Pikaia, a cephalochordate from the Burgess Shale Yunnanozoon, a cephalochordate from the Lower Cambrian of China Haikouichthys, agnathan, Lower Cambrian of China - Chengjiang fauna, scale is 5 mm A living jawless fish, the lamprey, Class Agnatha Jawless fish do have teeth! A fossil jawless fish, Class Agnatha, Ostracoderm, Hemicyclaspis, Silurian Agnathan, Ostracoderm, Athenaegis, Silurian of Canada Agnathan, Ostracoderm, Pteraspis, Devonian of the U.K. Agnathan, Ostracoderm, Liliaspis, Devonian of Russia Jaws evolved by modification of the gill arch bones. The placoderms were the armored fish of the Paleozoic Placoderm, Dunkleosteus, Devonian of Ohio Asterolepis, Placoderms, Devonian of Latvia Placoderm, Devonian of Australia Chondrichthyes: A freshwater shark of the Carboniferous Fossil tooth of a Great White shark Chondrichthyes, Great White Shark Chondrichthyes, Carcharhinus Sphyrna - hammerhead shark Himantura - a ray Manta Ray Fish Anatomy: Ray-finned fish Osteichthyes: ray-finned fish: clownfish Osteichthyes: ray-finned fish, deep water species Lophius, an Eocene fish showing the ray fins. This is an anglerfish. -
New Evolutionary and Ecological Advances in Deciphering the Cambrian Explosion of Animal Life
Journal of Paleontology, 92(1), 2018, p. 1–2 Copyright © 2018, The Paleontological Society 0022-3360/18/0088-0906 doi: 10.1017/jpa.2017.140 New evolutionary and ecological advances in deciphering the Cambrian explosion of animal life Zhifei Zhang1 and Glenn A. Brock2 1Shaanxi Key Laboratory of Early Life and Environments, State Key Laboratory of Continental Dynamics and Department of Geology, Northwest University, Xi’an, 710069, China 〈[email protected]〉 2Department of Biological Sciences and Marine Research Centre, Macquarie University, Sydney, NSW, 2109, Australia 〈[email protected]〉 The Cambrian explosion represents the most profound animal the body fossil record of ecdysozoans and deuterostomes is very diversification event in Earth history. This astonishing evolu- poorly known during this time, potentially the result of a distinct tionary milieu produced arthropods with complex compound lack of exceptionally preserved faunas in the Terreneuvian eyes (Paterson et al., 2011), burrowing worms (Mángano and (Fortunian and the unnamed Stage 2). However, this taxonomic Buatois, 2017), and a variety of swift predators that could cap- ‘gap’ has been partially filled with the discovery of exceptionally ture and crush prey with tooth-rimmed jaws (Bicknell and well-preserved stem group organisms in the Kuanchuanpu Paterson, 2017). The origin and evolutionary diversification of Formation (Fortunian Stage, ca. 535 Ma) from Ningqiang County, novel animal body plans led directly to increased ecological southern Shaanxi Province of central China. High diversity and complexity, and the roots of present-day biodiversity can be disparity of soft-bodied cnidarians (see Han et al., 2017b) and traced back to this half-billion-year-old evolutionary crucible. -
LETTER Doi:10.1038/Nature13414
LETTER doi:10.1038/nature13414 A primitive fish from the Cambrian of North America Simon Conway Morris1 & Jean-Bernard Caron2,3 Knowledge of the early evolution of fish largely depends on soft- (Extended Data Fig. 4f). Incompleteness precludes a precise estimate of bodied material from the Lower (Series 2) Cambrian period of South size range, but themostcomplete specimens (Fig.1a,b) areabout 60 mm China1,2. Owing to the rarity of some of these forms and a general in length and 8–13 mm in height. Laterally the body is fusiform, widest lack of comparative material from other deposits, interpretations of near the middle, tapering to a fine point posteriorly (Fig. 1a, b and Ex- various features remain controversial3,4, as do their wider relation- tended Data Fig. 4a), whereas in dorsal view the anterior termination is ships amongst post-Cambrian early un-skeletonized jawless verte- rounded (Fig. 1d and Extended Data Fig. 4c–e). The animal was com- brates. Here we redescribe Metaspriggina5 on the basis of new material pressed laterally, as is evident from occasional folding of the body as well from the Burgess Shale and exceptionally preserved material collected as specimensindorso-ventral orientation being conspicuously narrower near Marble Canyon, British Columbia6, and three other Cambrian (Fig. 1a and Extended Data Fig. 5a). Along the anterior ventral margin Burgess Shale-type deposits from Laurentia. This primitive fish dis- there was a keel-like structure (Fig. 1b, g, i, k, l), but no fins have been plays unambiguous vertebrate features: a notochord, a pair of prom- recognized. In the much more abundant specimens of Haikouichthys1,3,4 inent camera-type eyes, paired nasal sacs, possible cranium and arcualia, fins are seldom obvious, suggesting that their absence in Metaspriggina W-shaped myomeres, and a post-anal tail. -
29 | Vertebrates 791 29 | VERTEBRATES
Chapter 29 | Vertebrates 791 29 | VERTEBRATES Figure 29.1 Examples of critically endangered vertebrate species include (a) the Siberian tiger (Panthera tigris), (b) the mountain gorilla (Gorilla beringei), and (c) the Philippine eagle (Pithecophega jefferyi). (credit a: modification of work by Dave Pape; credit b: modification of work by Dave Proffer; credit c: modification of work by "cuatrok77"/Flickr) Chapter Outline 29.1: Chordates 29.2: Fishes 29.3: AmphiBians 29.4: Reptiles 29.5: Birds 29.6: Mammals 29.7: The Evolution of Primates Introduction Vertebrates are among the most recognizable organisms of the animal kingdom. More than 62,000 vertebrate species have been identified. The vertebrate species now living represent only a small portion of the vertebrates that have existed. The best-known extinct vertebrates are the dinosaurs, a unique group of reptiles, which reached sizes not seen before or after in terrestrial animals. They were the dominant terrestrial animals for 150 million years, until they died out in a mass extinction near the end of the Cretaceous period. Although it is not known with certainty what caused their extinction, a great deal is known about the anatomy of the dinosaurs, given the preservation of skeletal elements in the fossil record. Currently, a number of vertebrate species face extinction primarily due to habitat loss and pollution. According to the International Union for the Conservation of Nature, more than 6,000 vertebrate species are classified as threatened. Amphibians and mammals are the classes with the greatest percentage of threatened species, with 29 percent of all amphibians and 21 percent of all mammals classified as threatened. -
J32 the Importance of the Burgess Shale < Soft Bodied Fauna >
580 Chapter j PALEOCONTINENTS The Present is the Key to the Past: HUGH RANCE j32 The importance of the Burgess shale < soft bodied fauna > Only about 33 animal body plans are presently [sic] being used on this planet (Margulis and Schwartz, 1988). —Scott F. Gilbert, Developmental Biology, 1991.1 Almost all animal phyla known today were already present by 505 million years ago— the age of the Burgess shale, Middle Cambrian marine sediments, discovered at the Kicking Horse rim, British Columbia, in 1909 by Charles Doolittle Walcott, that provide a unique window on life without hard parts that had continued to exist shortly after the time of the Cambrian explosion (see Topic j34).2 Legend has it that Walcott, then secretary of the Smithsonian Institution, vacationing near Field, British Columbia, was thrown from a horse carrying him, when it tripped on, and split open a stray fallen slab of shale. Walcott, with his face literally rubbed in it, saw strange, but not hallucinational, forms crisply etched in black against the blue-black bedding surface of the shale: a bonanza of fossils of sea creatures without mineralized shells or backbones. Many are preserved whole; including those with articulated organic (biodegradable) exoskeletons. Details of even their soft body parts can be seen (best using PTM)3 as silvery films (formed of phyllosilicates on a coating of kerogenized carbon) that commonly outline even the most delicate structures on the fossilized animal.4 The Burgess shale is part of the Stephen Formation of greenish shales and thin-bedded limestones, which is a marine-offlap deposit between the thick, massive, carbonates of the overlying Eldon formation, and the underlying Cathedral formation.6 As referenced in the Geological Atlas of the Western Canada Sedimentary Basin - Chapter 8, the Stephen Formation has been “informally divided into a normal, ‘thin Stephen’ on the platform areas and a ‘thick Stephen’ west of the Cathedral Escarpment. -
The Fossil Record of the Cambrian “Explosion”: Resolving the Tree of Life Critics As Posing Challenges to Evolution
Article The Fossil Record of the Cambrian “Explosion”: 1 Resolving the Tree of Life Keith B. Miller Keith B. Miller The Cambrian “explosion” has been the focus of extensive scientifi c study, discussion, and debate for decades. It has also received considerable attention by evolution critics as posing challenges to evolution. In the last number of years, fossil discoveries from around the world, and particularly in China, have enabled the reconstruction of many of the deep branches within the invertebrate animal tree of life. Fossils representing “sister groups” and “stem groups” for living phyla have been recognized within the latest Precambrian (Neoproterozoic) and Cambrian. Important transitional steps between living phyla and their common ancestors are preserved. These include the rise of mollusks from their common ancestor with the annelids, the evolution of arthropods from lobopods and priapulid worms, the likely evolution of brachiopods from tommotiids, and the rise of chordates and echinoderms from early deuterostomes. With continued new discoveries, the early evolutionary record of the animal phyla is becoming ever better resolved. The tree of life as a model for the diversifi cation of life over time remains robust, and strongly supported by the Neoproterozoic and Cambrian fossil record. he most fundamental claim of bio- (such as snails, crabs, or sea urchins) as it logical evolution is that all living does to the fi rst appearance and diversi- T organisms represent the outer tips fi cation of dinosaurs, birds, or mammals. of a diversifying, upward- branching tree This early diversifi cation of invertebrates of life. The “Tree of Life” is an extreme- apparently occurred around the time of ly powerful metaphor that captures the the Precambrian/Cambrian boundary over essence of evolution. -
A Paleontological Perspective of Vertebrate Origin
http://www.paper.edu.cn Chinese Science Bulletin 2003 Vol. 48 No. 8 725-735 Cover: The earliest-known and most primitive vertebrates on the A paleontological perspective Earth---Myllokunmingia fengjiaoa , (upper) Zhongjianichthys rostratus of vertebrate origin ( middle ), Haikouichthys ercaicunensis (lower left and lower right). They were SHU Degan Early Life Institute & Department of Geology, Northwest products of the early Cambrian Explosion, University, Xi’an, 710069, China; School of Earth excavated from the famous Chengjiang Sciences and Resources, China University of Geosciences, Beijing, 100083, China Lagersttat, which was formed in the (e-mail:[email protected]) eastern Yunnan about 530 millions of years ago. These ancestral vertebrates not only Abstract The Early Cambrian Haikouichthys and Haikouella have been claimed to be related to contribute in an important developed primitive separate vertebral way to our understanding of vertebrate origin, but there have elements, but also possessed principal been heated debates about how exactly they are to be interpreted. New discoveries of numerous specimens of sensory organs, including a pair of large Haikouichthys not only confirm the identity of previously lateral eyes, nostril with nasal sacs, then described structures such as the dorsal and the ventral fins, and chevron-shaped myomeres, but also reveal many new had led to the transition from acraniates to important characteristics, including sensory organs of the head craniates (true vertebrates). The (e.g. large eyes), and a prominent notochord with differentiated vertebral elements. This “first fish” appears, discoveries of these “naked” agnathans however, to retain primitive reproductive features of have pushed the earliest record of acraniates, suggesting that it is a stem-group craniates. -
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.