CRACKING the CAMBRIAN New Fossils and Sites Are Helping Make Sense of the Mysterious Flowering of Animal Life Half a Billion Years Ago

Total Page:16

File Type:pdf, Size:1020Kb

CRACKING the CAMBRIAN New Fossils and Sites Are Helping Make Sense of the Mysterious Flowering of Animal Life Half a Billion Years Ago NEWS FEATURES Downloaded from http://science.sciencemag.org/ on December 3, 2018 CRACKING THE CAMBRIAN New fossils and sites are helping make sense of the mysterious flowering of animal life half a billion years ago By Joshua Sokol, in Kootenay National Park in Canada; Photography by John Lehmann he drumming of the jackhammer Star Wars. “It’s a spaceship landing area During the Cambrian, which began about deepens. Then, a block of shale here,” says expedition leader Jean-Bernard 540 million years ago, nearly all modern butterflies open, exposing to crisp Caron, curator of invertebrate paleontology animal groups—as diverse as mollusks mountain air a surface that hasn’t at the Royal Ontario Museum (ROM) in To- and chordates—leapt into the fossil record. seen sunlight in half a billion ronto, Canada. Those early marine animals exhibited a years. “Woo!” says paleontologist Those “spaceships” are carapaces, molted dazzling array of body plans, as though evo- Cédric Aria of the Nanjing Insti- onto a long-vanished ocean floor by a lution needed to indulge a creative streak tute of Geology and Palaeontology species new to science. This field season before buckling down. For more than a in China, bracing the top slab of they’ve been spilling out of the rocks here, century, scientists have struggled to make rock upright. where Caron’s team has spent the past heads or tails—sometimes literally—of TIts underside bears charcoal-colored few years unearthing groundbreaking ani- those specimens, figure out how they relate smudges that look vaguely like horse- mal fossils from the Cambrian period, the to life today, and understand what fueled shoe crabs or the Millennium Falcon from coming-out party for animal life on Earth. the evolutionary explosion. MUSEUM ONTARIO ROYAL FOSSIL: 880 23 NOVEMBER 2018 • VOL 362 ISSUE 6417 sciencemag.org SCIENCE Published by AAAS Jean-Bernard Caron shows off the “mothership,” insured a Burgess Shale specimen for half or even into the present. So, for example, he an enigmatic Cambrian life form his team a million Canadian dollars when it went concluded almost all the creatures resem- found in the Canadian Rockies this summer. on loan, he says—and that was an animal bling today’s arthropods were crustaceans. known through multiple fossils. This is one But later paleontologists had other ideas. Gingerly, Aria and Caron place the top of a kind. Harvard University’s Stephen Jay Gould piece of their slab aside. Space is hard to “It’s going to be iconic,” Caron says. “It’s perhaps best captured the charisma of Cam- come by in the quarry, perched on a ledge the most extraordinary fossil I’ve ever found.” brian life in his 1989 book Wonderful Life: the size of a small bedroom at an altitude The Burgess Shale and the Nature of His- of 2500 meters, far above Tokumm Creek. FOR YEARS, CARON SUSPECTED Walcott’s site tory, in which he lavished attention on the For years, an equally forbidding site about might be rivaled elsewhere in the Rocky “weird wonders” excavated from Walcott’s 40 kilometers northwest of this valley of- Mountains. The breakthrough came in city block–size quarry. Gould argued that fered the clearest window on the Cam- 2012, near an area called Marble Canyon, oddballs such as the aptly named Halluci- brian. There, in 1909, U.S. paleontologist where a 2003 wildfire had burned off the genia, a worm with legs and hard spines, Charles Doolittle Walcott discovered the trees. While crossing an avalanche chute seem unrelated to later animals. He slotted Burgess Shale, a fossil formation that pre- filled with broken tiles of rock, his recon- the unusual forms into their own phyla and serves not only hard shells, but also soft naissance party found itself surrounded by argued that they were evolution’s forgotten features such as the legs, eyes, and guts of impressions of soft-bodied creatures, many experiments, later cast aside by contingen- Cambrian creepy-crawlies. with unfamiliar shapes. “It was clear that cies of fate. But in recent years, Caron has shown nobody had ever been walking over this Contemporary paleontologists have that the richest fossil-bearing rock extends pile of rocks before with this purpose in settled on yet another way to understand Downloaded from many kilometers beyond Walcott’s site. mind,” says Bob Gaines, a geochemist from them. Consider the arthropods, arguably This summer’s excavation marks his latest Pomona College in Claremont, California, Earth’s most successful animals. In a fam- visit to this long Cambrian tapestry. Each who has joined Caron’s expeditions since ily tree, the spray of recent branches that new stop has offered striking views of un- the beginning. end in living arthropods—spiders, insects, familiar animals, many already described They returned to excavate in 2014. At crustaceans—constitutes a “crown” group. in high-profile papers: the little fish rela- least one in five of the animals they found But some animals in the Burgess Shale http://science.sciencemag.org/ tive Metaspriggina, a vertebrate ances- at Marble Canyon belongs to species new to probably come from earlier “stems” that tor that Caron now speculates clustered science, the team concluded. Now, they’ve branched off before the crown arthropods. in schools; the pincered Tokummia; and moved on to other sites along the valley. These branches of the tree don’t have sur- the ice cream cone–shaped fossils called How Cambrian species are related to to- viving descendants, like a childless great- hyoliths, which Caron’s Ph.D. student day’s animals has been debated since the uncle grinning out from a family photo. In Joseph Moysiuk last year linked to shelled fossils first came to light. Walcott classified that view, many of Gould’s weird wonders animals called brachiopods, some of which his oddities within known groups, noting are stem group organisms, related to the persist today. that some Burgess Shale fossils, such as the ancestors of current creatures although Other sites around the world are also brachiopods, persisted after the Cambrian not ancestors themselves. Newer fossils opening new vistas of the Cambrian. Scien- tists can now explore the animal explosion on December 3, 2018 with a highlight reel of specimens, along All in the family A partial schematic of a proposed family tree of arthropods shows the complex with results from new imaging technolo- relations among living and extinct groups. Some extinct Cambrian creatures (red) may belong to “stem” groups gies and genetic and developmental stud- that branched off the arthropod tree before the common ancestor of living groups like arachnids and insects. ies of living organisms. “There have been a host of new discoveries,” says paleonto- logist Doug Erwin of the Smithsonian In- stitution’s National Museum of Natural History in Washington, D.C. Researchers may be closer than ever to fitting these strange creatures into their proper places Arachnids Crustaceans Velvet worms Insects in the tree of life—and understanding the 0 Horseshoe Centipedes, “explosion” that birthed them. crabs millipedes Each new find brings the simple joy of unearthing and imagining a seemingly alien creature. On a break, Caron cau- tiously shows off this year’s crown jewel, found about a week earlier. It’s an intact, DATA) JO WOLFE, MIT JO WOLFE, DATA) hand-size carapace with a center spine, like a Prussian spiked helmet frozen in an- Radiodontans Trilobites and relatives cient rock. Another undescribed species, SCIENCE; ( SCIENCE; it seems to be related to the spaceships. Caron’s team calls it the mothership. He’s nervous just holding it. Burgess Hallucigenia Shale fossils are so valuable that Parks Canada keeps the exact locations of Caron’s 541 million sites secret, monitors them with cameras, years CREDITS: (GRAPHIC) N. DESAI/ N. (GRAPHIC) CREDITS: and prosecutes fossil poachers. ROM once ago SCIENCE sciencemag.org 23 NOVEMBER 2018 • VOL 362 ISSUE 6417 881 Published by AAAS NEWS | FEATURES Downloaded from http://science.sciencemag.org/ from the Canadian Rockies help support ing nervous tissue in exceptionally preserved Critics argue that paleontologists such that view. Caron argued in 2015, for ex- Chinese fossils. Those nervous system archi- as Ma and Ortega-Hernández overinterpret ample, that his specimens of Hallucigenia tectures offer a parallel way to sort animals some fossils, spotting nervous tissues that have features suggesting the animal be- into evolutionary groups, beyond the usual aren’t there. Many of those structures, the longs on a stem group of the velvet worms, anatomical structures, and other teams have critics say, might just be “halos,” biofilms creatures that still crawl around in tropical presented their own compelling specimens. formed when microbes broke down inter- forests spitting slime. In fossils of the shrimplike Chengjiangoca- nal parts like muscles or guts after death. Similar analysis awaits the spaceships. At ris kunmingensis from southwest China, for But other researchers are convinced. “If you first glance, Caron’s team thinks they are a example, “we have this structure that looks look at the best-preserved nervous systems, new species or group of radiodontans, stem almost like a pearl necklace,” running almost there’s no doubt” that the features are real, arthropods that also include Anomalocaris, head to tail, says Javier Ortega-Hernández, says Graham Budd, a paleontologist at Up- on December 3, 2018 the Cambrian’s charismatic apex predator—a an incoming professor at Harvard. His team, psala University in Sweden and an architect clawed, fearsome-jawed swimmer half a me- led by Jie Yang at Yunnan University in Kun- of the current stem-and-crown concept. ter long. Filling out the branches of that stem ming, China, argued in 2016 that the neck- Bold claims that use anatomy to revise group gives a “step-by-step view of how an lace is a nerve cord studded with smaller family trees engender similar controversy arthropod built its body” through evolution- clusters of neurons, themselves sprout- throughout the field.
Recommended publications
  • Decoupled Evolution of Soft and Hard Substrate Communities During the Cambrian Explosion and Great Ordovician Biodiversification Event
    Decoupled evolution of soft and hard substrate communities during the Cambrian Explosion and Great Ordovician Biodiversification Event Luis A. Buatoisa,1, Maria G. Mánganoa, Ricardo A. Oleab, and Mark A. Wilsonc aDepartment of Geological Sciences, University of Saskatchewan, Saskatoon, SK, Canada S7N 5E2; bEastern Energy Resources Science Center, US Geological Survey, Reston, VA 20192; and cDepartment of Geology, The College of Wooster, Wooster, OH 44691 Edited by Steven M. Holland, University of Georgia, Athens, GA, and accepted by Editorial Board Member David Jablonski May 6, 2016 (received for review November 21, 2015) Contrasts between the Cambrian Explosion (CE) and the Great shed light on the natures of both radiations. Because there is still Ordovician Biodiversification Event (GOBE) have long been recog- controversy regarding Sepkoski’s nonstandardized curves of nized. Whereas the vast majority of body plans were established Phanerozoic taxonomic diversity (13–15), a rarefaction analysis as a result of the CE, taxonomic increases during the GOBE were was performed in an attempt to standardize diversity data. The manifested at lower taxonomic levels. Assessing changes of ichno- aims of this paper are to document the contrasting ichnodiversity diversity and ichnodisparity as a result of these two evolutionary and ichnodisparity trajectories in soft and hard substrate com- events may shed light on the dynamics of both radiations. The early munities during these two evolutionary events and to discuss the Cambrian (series 1 and 2) displayed a dramatic increase in ichnodi- possible underlying causes of this decoupled evolution. versity and ichnodisparity in softground communities. In contrast to this evolutionary explosion in bioturbation structures, only a few Results Cambrian bioerosion structures are known.
    [Show full text]
  • The Geologic Time Scale Is the Eon
    Exploring Geologic Time Poster Illustrated Teacher's Guide #35-1145 Paper #35-1146 Laminated Background Geologic Time Scale Basics The history of the Earth covers a vast expanse of time, so scientists divide it into smaller sections that are associ- ated with particular events that have occurred in the past.The approximate time range of each time span is shown on the poster.The largest time span of the geologic time scale is the eon. It is an indefinitely long period of time that contains at least two eras. Geologic time is divided into two eons.The more ancient eon is called the Precambrian, and the more recent is the Phanerozoic. Each eon is subdivided into smaller spans called eras.The Precambrian eon is divided from most ancient into the Hadean era, Archean era, and Proterozoic era. See Figure 1. Precambrian Eon Proterozoic Era 2500 - 550 million years ago Archaean Era 3800 - 2500 million years ago Hadean Era 4600 - 3800 million years ago Figure 1. Eras of the Precambrian Eon Single-celled and simple multicelled organisms first developed during the Precambrian eon. There are many fos- sils from this time because the sea-dwelling creatures were trapped in sediments and preserved. The Phanerozoic eon is subdivided into three eras – the Paleozoic era, Mesozoic era, and Cenozoic era. An era is often divided into several smaller time spans called periods. For example, the Paleozoic era is divided into the Cambrian, Ordovician, Silurian, Devonian, Carboniferous,and Permian periods. Paleozoic Era Permian Period 300 - 250 million years ago Carboniferous Period 350 - 300 million years ago Devonian Period 400 - 350 million years ago Silurian Period 450 - 400 million years ago Ordovician Period 500 - 450 million years ago Cambrian Period 550 - 500 million years ago Figure 2.
    [Show full text]
  • 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.
    [Show full text]
  • Geobiological Events in the Ediacaran Period
    Geobiological Events in the Ediacaran Period Shuhai Xiao Department of Geosciences, Virginia Tech, Blacksburg, VA 24061, USA NSF; NASA; PRF; NSFC; Virginia Tech Geobiology Group; CAS; UNLV; UCR; ASU; UMD; Amherst; Subcommission of Neoproterozoic Stratigraphy; 1 Goals To review biological (e.g., acanthomorphic acritarchs; animals; rangeomorphs; biomineralizing animals), chemical (e.g., carbon and sulfur isotopes, oxygenation of deep oceans), and climatic (e.g., glaciations) events in the Ediacaran Period; To discuss integration and future directions in Ediacaran geobiology; 2 Knoll and Walter, 1992 • Acanthomorphic acritarchs in early and Ediacara fauna in late Ediacaran Period; • Strong carbon isotope variations; • Varanger-Laplandian glaciation; • What has happened since 1992? 3 Age Constraints: South China (538.2±1.5 Ma) 541 Ma Cambrian Dengying Ediacaran Sinian 551.1±0.7 Ma Doushantuo 632.5±0.5 Ma 635 Ma 635.2±0.6 Ma Nantuo (Tillite) 636 ± 5Ma Cryogenian Nanhuan 654 ± 4Ma Datangpo 663±4 Ma Neoproterozoic Neoproterozoic Jiangkou Group Banxi Group 725±10 Ma Tonian Qingbaikouan 1000 Ma • South China radiometric ages: Condon et al., 2005; Hoffmann et al., 2004; Zhou et al., 2004; Bowring et al., 2007; S. Zhang et al., 2008; Q. Zhang et al., 2008; • Additional ages from Nama Group (Namibia), Conception Group (Newfoundland), and Vendian (White Sea); 4 The Ediacaran Period Ediacara fossils Cambrian 545 Ma Nama assemblage 555 Ma White Sea assemblage 565 Ma Avalon assemblage 575 Ma 585 Ma Doushantuo biota 595 Ma 605 Ma Ediacaran Period 615 Ma
    [Show full text]
  • Trace Fossils and Substrates of the Terminal Proterozoic–Cambrian Transition: Implications for the Record of Early Bilaterians and Sediment Mixing
    Trace fossils and substrates of the terminal Proterozoic–Cambrian transition: Implications for the record of early bilaterians and sediment mixing Mary L. Droser*†,So¨ ren Jensen*, and James G. Gehling‡ *Department of Earth Sciences, University of California, Riverside, CA 92521; and ‡South Australian Museum, Division of Natural Sciences, North Terrace, Adelaide 5000, South Australia, Australia Edited by James W. Valentine, University of California, Berkeley, CA, and approved August 16, 2002 (received for review May 29, 2002) The trace fossil record is important in determining the timing of the appearance of bilaterian animals. A conservative estimate puts this time at Ϸ555 million years ago. The preservational potential of traces made close to the sediment–water interface is crucial to detecting early benthic activity. Our studies on earliest Cambrian sediments suggest that shallow tiers were preserved to a greater extent than typical for most of the Phanerozoic, which can be attributed both directly and indirectly to the low levels of sediment mixing. The low levels of sediment mixing meant that thin event beds were preserved. The shallow depth of sediment mixing also meant that muddy sediments were firm close to the sediment–water interface, increasing the likelihood of recording shallow-tier trace fossils in muddy sed- iments. Overall, trace fossils can provide a sound record of the onset of bilaterian benthic activity. he appearance and subsequent diversification of bilaterian Tanimals is a topic of current controversy (refs. 1–7; Fig. 1). Three principal sources of evidence exist: body fossils, trace fossils (trails, tracks, and burrows of animal activity recorded in the sedimentary record), and divergence times calculated by means of a molecular ‘‘clock.’’ The body fossil record indicates a geologically rapid diversification of bilaterian animals not much earlier than the Precambrian–Cambrian boundary, the so-called Cambrian explosion.
    [Show full text]
  • A Fundamental Precambrian–Phanerozoic Shift in Earth's Glacial
    Tectonophysics 375 (2003) 353–385 www.elsevier.com/locate/tecto A fundamental Precambrian–Phanerozoic shift in earth’s glacial style? D.A.D. Evans* Department of Geology and Geophysics, Yale University, P.O. Box 208109, 210 Whitney Avenue, New Haven, CT 06520-8109, USA Received 24 May 2002; received in revised form 25 March 2003; accepted 5 June 2003 Abstract It has recently been found that Neoproterozoic glaciogenic sediments were deposited mainly at low paleolatitudes, in marked qualitative contrast to their Pleistocene counterparts. Several competing models vie for explanation of this unusual paleoclimatic record, most notably the high-obliquity hypothesis and varying degrees of the snowball Earth scenario. The present study quantitatively compiles the global distributions of Miocene–Pleistocene glaciogenic deposits and paleomagnetically derived paleolatitudes for Late Devonian–Permian, Ordovician–Silurian, Neoproterozoic, and Paleoproterozoic glaciogenic rocks. Whereas high depositional latitudes dominate all Phanerozoic ice ages, exclusively low paleolatitudes characterize both of the major Precambrian glacial epochs. Transition between these modes occurred within a 100-My interval, precisely coeval with the Neoproterozoic–Cambrian ‘‘explosion’’ of metazoan diversity. Glaciation is much more common since 750 Ma than in the preceding sedimentary record, an observation that cannot be ascribed merely to preservation. These patterns suggest an overall cooling of Earth’s longterm climate, superimposed by developing regulatory feedbacks
    [Show full text]
  • The Weeks Formation Konservat-Lagerstätte and the Evolutionary Transition of Cambrian Marine Life
    Downloaded from http://jgs.lyellcollection.org/ by guest on October 1, 2021 Review focus Journal of the Geological Society Published Online First https://doi.org/10.1144/jgs2018-042 The Weeks Formation Konservat-Lagerstätte and the evolutionary transition of Cambrian marine life Rudy Lerosey-Aubril1*, Robert R. Gaines2, Thomas A. Hegna3, Javier Ortega-Hernández4,5, Peter Van Roy6, Carlo Kier7 & Enrico Bonino7 1 Palaeoscience Research Centre, School of Environmental and Rural Science, University of New England, Armidale, NSW 2351, Australia 2 Geology Department, Pomona College, Claremont, CA 91711, USA 3 Department of Geology, Western Illinois University, 113 Tillman Hall, 1 University Circle, Macomb, IL 61455, USA 4 Department of Zoology, University of Cambridge, Downing Street, Cambridge CB2 3EJ, UK 5 Museum of Comparative Zoology and Department of Organismic and Evolutionary Biology, Harvard University, 26 Oxford Street, Cambridge, MA 02138, USA 6 Department of Geology, Ghent University, Krijgslaan 281/S8, B-9000 Ghent, Belgium 7 Back to the Past Museum, Carretera Cancún, Puerto Morelos, Quintana Roo 77580, Mexico R.L.-A., 0000-0003-2256-1872; R.R.G., 0000-0002-3713-5764; T.A.H., 0000-0001-9067-8787; J.O.-H., 0000-0002- 6801-7373 * Correspondence: [email protected] Abstract: The Weeks Formation in Utah is the youngest (c. 499 Ma) and least studied Cambrian Lagerstätte of the western USA. It preserves a diverse, exceptionally preserved fauna that inhabited a relatively deep water environment at the offshore margin of a carbonate platform, resembling the setting of the underlying Wheeler and Marjum formations. However, the Weeks fauna differs significantly in composition from the other remarkable biotas of the Cambrian Series 3 of Utah, suggesting a significant Guzhangian faunal restructuring.
    [Show full text]
  • 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.
    [Show full text]
  • 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.
    [Show full text]
  • Can Molecular Clocks and the Fossil Record Be Reconciled?
    Prospects & Overviews Review essays The origin of animals: Can molecular clocks and the fossil record be reconciled? John A. Cunningham1)2)Ã, Alexander G. Liu1)†, Stefan Bengtson2) and Philip C. J. Donoghue1) The evolutionary emergence of animals is one of the most Introduction significant episodes in the history of life, but its timing remains poorly constrained. Molecular clocks estimate that The apparent absence of a fossil record prior to the appearance of trilobites in the Cambrian famously troubled Darwin. He animals originated and began diversifying over 100 million wrote in On the origin of species that if his theory of evolution years before the first definitive metazoan fossil evidence in were true “it is indisputable that before the lowest [Cambrian] the Cambrian. However, closer inspection reveals that clock stratum was deposited ... the world swarmed with living estimates and the fossil record are less divergent than is creatures.” Furthermore, he could give “no satisfactory answer” often claimed. Modern clock analyses do not predict the as to why older fossiliferous deposits had not been found [1]. In the intervening century and a half, a record of Precambrian presence of the crown-representatives of most animal phyla fossils has been discovered extending back over three billion in the Neoproterozoic. Furthermore, despite challenges years (popularly summarized in [2]). Nevertheless, “Darwin’s provided by incomplete preservation, a paucity of phylo- dilemma” regarding the origin and early evolution of Metazoa genetically informative characters, and uncertain expecta- arguably persists, because incontrovertible fossil evidence for tions of the anatomy of early animals, a number of animals remains largely, or some might say completely, absent Neoproterozoic fossils can reasonably be interpreted as from Neoproterozoic rocks [3].
    [Show full text]
  • Hallucigenia
    www.palaeontologyonline.com |Page 1 Title: Fossil Focus - Hallucigenia and the evolution of animal body plans Author(s): Martin Smith *1 Volume: 7 Article: 5 Page(s): 1-9 Published Date: 01/05/2017 PermaLink: http://www.palaeontologyonline.com/articles/2017/fossil_focus_hallucigenia/ IMPORTANT Your use of the P alaeontology [online] ar chive ind icates y our accep tance of P alaeontology [online]'s T erms and Conditions of Use, a vailable a t http://www.palaeontologyonline.com/site-information/terms-and-conditions/. COPYRIGHT Palaeontology [online] (w ww.palaeontologyonline.com) publishes all w ork, unless other wise s tated, under the Creative Commons A ttribution 3.0 Unport ed (CC BY 3.0) license. This license le ts other s dis tribute, r emix, tw eak, and build upon the published w ork, e ven commercially, as long as the y cr edit P alaeontology[online] f or the original cr eation. This is the mo st accommodating of licenses of fered b y Cr eative Commons and is r ecommended f or ma ximum dissemina tion of published ma terial. Further de tails ar e a vailable a t h ttp://www.palaeontologyonline.com/site-information/copyright/. CITATION OF ARTICLE Please cit e the f ollowing published w ork as: Smith, Martin. 2017. F ossil F ocus - Hallucigenia and the e volution of animal body plans. P alaeontology Online, Volume 5, Article 5, 1-9. Published by: Palaeontology [online] www.palaeontologyonline.com |Page 2 Fossil Focus: Hallucigenia and the evolution of animal body plans by Martin Smith *1 Introduction: Five hundred and fifty million years ago, few (if any) organisms on Earth were much more complex than seaweed.
    [Show full text]
  • Hallucigenia's Onychophoran-Like Claws
    LETTER doi:10.1038/nature13576 Hallucigenia’s onychophoran-like claws and the case for Tactopoda Martin R. Smith1 & Javier Ortega-Herna´ndez1 The Palaeozoic form-taxon Lobopodia encompasses a diverse range of Onychophorans lack armature sclerites, but possess two types of ap- soft-bodied‘leggedworms’ known from exceptionalfossil deposits1–9. pendicular sclerite: paired terminal claws in the walking legs, and den- Although lobopodians occupy a deep phylogenetic position within ticulate jaws within the mouth cavity9,23.AsinH. sparsa, claws in E. Panarthropoda, a shortage of derived characters obscures their evo- kanangrensis exhibit a broad base that narrows to a smooth conical point lutionary relationships with extant phyla (Onychophora, Tardigrada (Fig. 1e–h). Each terminal clawsubtends anangle of130u and comprises and Euarthropoda)2,3,5,10–15. Here we describe a complex feature in two to three constituent elements (Fig. 1e–h). Each smaller element pre- the terminal claws of the mid-Cambrian lobopodian Hallucigenia cisely fills the basal fossa of its container, from which it can be extracted sparsa—their construction from a stack of constituent elements— with careful manipulation (Fig. 1e, g, h and Extended Data Fig. 3a–g). and demonstrate that equivalent elements make up the jaws and claws Each constituent element has a similar morphology and surface orna- of extant Onychophora. A cladistic analysis, informed by develop- ment (Extended Data Fig. 3a–d), even in an abnormal claw where mental data on panarthropod head segmentation, indicates that the element tips are flat instead of pointed (Extended Data Fig. 3h). The stacked sclerite components in these two taxa are homologous— proximal bases of the innermost constituent elements are associated with resolving hallucigeniid lobopodians as stem-group onychophorans.
    [Show full text]