The Importance of Neutral Over Niche Processes in Structuring Ediacaran Early Animal
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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. -
A Rich Ediacaran Assemblage from Eastern Avalonia: Evidence of Early
Publisher: GSA Journal: GEOL: Geology Article ID: G31890 1 A rich Ediacaran assemblage from eastern Avalonia: 2 Evidence of early widespread diversity in the deep ocean 3 [[SU: ok? need a noun]] 4 Philip R. Wilby, John N. Carney, and Michael P.A. Howe 5 British Geological Survey, Keyworth, Nottingham NG12 5GG, UK 6 ABSTRACT 7 The Avalon assemblage (Ediacaran, late Neoproterozoic) constitutes the oldest 8 evidence of diverse macroscopic life and underpins current understanding of the early 9 evolution of epibenthic communities. However, its overall diversity and provincial 10 variability are poorly constrained and are based largely on biotas preserved in 11 Newfoundland, Canada. We report coeval high-diversity biotas from Charnwood Forest, 12 UK, which share at least 60% of their genera in common with those in Newfoundland. 13 This indicates that substantial taxonomic exchange took place between different regions 14 of Avalonia, probably facilitated by ocean currents, and suggests that a diverse deepwater 15 biota that had a probable biogeochemical impact may already have been widespread at 16 the time. Contrasts in the relative abundance of prostrate versus erect taxa record 17 differential sensitivity to physical environmental parameters (hydrodynamic regime, 18 substrate) and highlight their significance in controlling community structure. 19 INTRODUCTION 20 The Ediacaran (late Neoproterozoic) Avalon assemblage (ca. 578.8–560 Ma) 21 preserves the oldest evidence of diverse macroorganisms and is key to elucidating the 22 early radiation of macroscopic life and the assembly of benthic marine communities Page 1 of 15 Publisher: GSA Journal: GEOL: Geology Article ID: G31890 23 (Clapham et al., 2003; Van Kranendonk et al., 2008). -
Retallack 2014 Newfoundland Ediacaran
Downloaded from gsabulletin.gsapubs.org on May 2, 2014 Geological Society of America Bulletin Volcanosedimentary paleoenvironments of Ediacaran fossils in Newfoundland Gregory J. Retallack Geological Society of America Bulletin 2014;126, no. 5-6;619-638 doi: 10.1130/B30892.1 Email alerting services click www.gsapubs.org/cgi/alerts to receive free e-mail alerts when new articles cite this article Subscribe click www.gsapubs.org/subscriptions/ to subscribe to Geological Society of America Bulletin Permission request click http://www.geosociety.org/pubs/copyrt.htm#gsa to contact GSA Copyright not claimed on content prepared wholly by U.S. government employees within scope of their employment. Individual scientists are hereby granted permission, without fees or further requests to GSA, to use a single figure, a single table, and/or a brief paragraph of text in subsequent works and to make unlimited copies of items in GSA's journals for noncommercial use in classrooms to further education and science. This file may not be posted to any Web site, but authors may post the abstracts only of their articles on their own or their organization's Web site providing the posting includes a reference to the article's full citation. GSA provides this and other forums for the presentation of diverse opinions and positions by scientists worldwide, regardless of their race, citizenship, gender, religion, or political viewpoint. Opinions presented in this publication do not reflect official positions of the Society. Notes © 2014 Geological Society of America Downloaded from gsabulletin.gsapubs.org on May 2, 2014 Volcanosedimentary paleoenvironments of Ediacaran fossils in Newfoundland Gregory J. -
Of Time and Taphonomy: Preservation in the Ediacaran
See discussions, stats, and author profiles for this publication at: http://www.researchgate.net/publication/273127997 Of time and taphonomy: preservation in the Ediacaran CHAPTER · JANUARY 2014 READS 36 2 AUTHORS, INCLUDING: Charlotte Kenchington University of Cambridge 5 PUBLICATIONS 2 CITATIONS SEE PROFILE Available from: Charlotte Kenchington Retrieved on: 02 October 2015 ! OF TIME AND TAPHONOMY: PRESERVATION IN THE EDIACARAN CHARLOTTE G. KENCHINGTON! 1,2 AND PHILIP R. WILBY2 1Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge, CB2 3EQ, UK <[email protected]! > 2British Geological Survey, Keyworth, Nottingham, NG12 5GG, UK ABSTRACT.—The late Neoproterozoic witnessed a revolution in the history of life: the transition from a microbial world to the one known today. The enigmatic organisms of the Ediacaran hold the key to understanding the early evolution of metazoans and their ecology, and thus the basis of Phanerozoic life. Crucial to interpreting the information they divulge is a thorough understanding of their taphonomy: what is preserved, how it is preserved, and also what is not preserved. Fortunately, this Period is also recognized for its abundance of soft-tissue preservation, which is viewed through a wide variety of taphonomic windows. Some of these, such as pyritization and carbonaceous compression, are also present throughout the Phanerozoic, but the abundance and variety of moldic preservation of body fossils in siliciclastic settings is unique to the Ediacaran. In rare cases, one organism is preserved in several preservational styles which, in conjunction with an increased understanding of the taphonomic processes involved in each style, allow confident interpretations of aspects of the biology and ecology of the organisms preserved. -
Annual Meeting 2011
The Palaeontological Association 55th Annual Meeting 17th–20th December 2011 Plymouth University PROGRAMME and ABSTRACTS Palaeontological Association 2 ANNUAL MEETING ANNUAL MEETING Palaeontological Association 1 The Palaeontological Association 55th Annual Meeting 17th–20th December 2011 School of Geography, Earth and Environmental Sciences, Plymouth University The programme and abstracts for the 55th Annual Meeting of the Palaeontological Association are outlined after the following summary of the meeting. Venue The meeting will take place on the campus of Plymouth University. Directions to the University and a campus map can be found at <http://www.plymouth.ac.uk/location>. The opening symposium and the main oral sessions will be held in the Sherwell Centre, located on North Hill, on the east side of campus. Accommodation Delegates need to make their own arrangements for accommodation. Plymouth has a large number of hotels, guesthouses and hostels at a variety of prices, most of which are within ~1km of the University campus (hotels with PL1 or PL4 postcodes are closest). More information on these can be found through the usual channels, and a useful starting point is the website <http://www.visitplymouth.co.uk/site/where-to-stay>. In addition, we have organised discount rates at the Jury’s Inn, Exeter Street, which is located ~500m from the conference venue. A maximum of 100 rooms have been reserved, and will be allocated on a first-come-first-served basis. Further information can be found on the Association’s website. Travel Transport into Plymouth can be achieved via a variety of means. Travel by train from London Paddington to Plymouth takes between three and four hours depending on the time of day and the number of stops. -
Experimental Fluid Mechanics of an Ediacaran Frond
Palaeontologia Electronica palaeo-electronica.org Experimental fluid mechanics of an Ediacaran frond Amy Singer, Roy Plotnick, and Marc Laflamme ABSTRACT Ediacaran fronds are iconic members of the soft-bodied Ediacara biota, character- ized by disparate morphologies and wide stratigraphic and environmental ranges. As is the case with nearly all Ediacaran forms, views of their phylogenetic position and ecol- ogy are equally diverse, with most frond species considered as sharing a similar eco- logical guild rather than life history. Experimental biomechanics can potentially constrain these interpretations and suggest new approaches to understanding frond life habits. We examined the behavior in flow of two well-know species of Charniodiscus from the Mistaken Point Formation of Newfoundland, Canada (Avalon assemblage): Charniodiscus spinosus and C. procerus. Models reflecting alternative interpretations of surface morphology and structural rigidity were subjected to qualitative and quantita- tive studies of flow behavior in a recirculating flow tank. At the same velocities and orientations, model C. procerus and C. spinosus expe- rienced similar drag forces; the drag coefficient of C. procerus was smaller, but it is taller and thus experiences higher ambient flow velocities. Reorientation to become parallel to flow dramatically reduces drag in both forms. Models further demonstrated that C. procerus (and to a lesser extent C. spinosus) behaved as self exciting oscilla- tors, which would have increased gas exchange rates at the surface of the fronds and is consistent with an osmotrophic life habit. Amy Singer. Geosciences Department, The University of Montana, 32 Campus Drive #1296, Missoula, MT 59812-1296; [email protected] Roy Plotnick (correspondence author). -
Rangeomorphs, Thectardis (Porifera?) and Dissolved Organic Carbon in the Ediacaran Oceans E
Geobiology (2011), 9, 24–33 DOI: 10.1111/j.1472-4669.2010.00259.x Rangeomorphs, Thectardis (Porifera?) and dissolved organic carbon in the Ediacaran oceans E. A. SPERLING,1,2 K. J. PETERSON3 AND M. LAFLAMME1 1Department of Geology and Geophysics, Yale University, New Haven, CT, USA 2Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA, USA 3Department of Biological Sciences, Dartmouth College, Hanover, NH, USA ABSTRACT The mid-Ediacaran Mistaken Point biota of Newfoundland represents the first morphologically complex organ- isms in the fossil record. At the classic Mistaken Point localities the biota is dominated by the enigmatic group of ‘‘fractally’’ branching organisms called rangeomorphs. One of the few exceptions to the rangeomorph body plan is the fossil Thectardis avalonensis, which has been reconstructed as an upright, open cone with its apex in the sediment. No biological affinity has been suggested for this fossil, but here we show that its body plan is consis- tent with the hydrodynamics of the sponge water-canal system. Further, given the habitat of Thectardis beneath the photic zone, and the apparent absence of an archenteron, movement, or a fractally designed body plan, we suggest that it is a sponge. The recognition of sponges in the Mistaken Point biota provides some of the earliest body fossil evidence for this group, which must have ranged through the Ediacaran based on biomarkers, molec- ular clocks, and their position on the metazoan tree of life, in spite of their sparse macroscopic fossil record. Should our interpretation be correct, it would imply that the paleoecology of the Mistaken Point biota was domi- nated by sponges and rangeomorphs, organisms that are either known or hypothesized to feed in large part on dissolved organic carbon (DOC). -
Mistaken Point, with Insets Showing Some of the Diverse Ediacaran Macrofossils Present at Mistake Point (Photo: A
Open File NFLD/3320 GEOLOGICAL ASSOCIATION OF CANADA Newfoundland and Labrador Section 2015 FALL FIELD TRIP The Ediacaran fossils of the Avalon Peninsula Alex G. Liu and James Conliffe with contributions from Liam Herringshaw, Jack Matthews, and Duncan McIlroy September 18–20th, 2015 Cover photo: Overview of the fossil bearing bedding planes at Mistaken Point, with insets showing some of the diverse Ediacaran macrofossils present at Mistake Point (photo: A. Liu) GAC Newfoundland and Labrador Section – 2015 Fall Field Trip Ediacaran macrofossils from the Mistaken Point ‘E’ Surface. 2 GAC Newfoundland and Labrador Section – 2015 Fall Field Trip TABLE OF CONTENTS INTRODUCTION AND OVERVIEW 4 ACKNOWLEDGEMENTS 4 SAFETY INFORMATION 5 MISTAKEN POINT ECOLOGICAL RESERVE (MPER) 7 PART 1: BACKGROUND MATERIAL 9 INTRODUCTION 9 Introduction to the Neoproterozoic‒Phanerozoic Transition 9 Stratigraphy, Structural Geology, and Depositional Environment of the Avalon Peninsula 13 EDICARAN PALEONTOLOGY OF THE AVALON PENINSULA 16 Preservation of Ediacaran macrofossils 16 The Avalon Assemblage 18 Current research into the Mistaken Point Ediacaran Fossils 21 PART 2: FIELD TRIP ITINERARY 24 Day One – Harbour Main and Spaniard’s Bay 25 Day Two – Mistaken Point Ecological Reserve 31 Day Three – Mistaken Point Ecological Reserve and Ferryland 46 INVENTORY OF TAXA IN MISTAKEN POINT ECOLOGICAL RESERVE 53 REFERENCES 54 3 GAC Newfoundland and Labrador Section – 2015 Fall Field Trip INTRODUCTION AND OVERVIEW The Mistaken Point Ecological Reserve (Fig. 1) is home to the some of the world’s most impressive Ediacaran fossil assemblages. Large bedding planes covered in thousands of exceptionally preserved specimens can be found in situ throughout a continuous ~2 km succession of sedimentary strata. -
Curriculum Vitae August 2012 Guy M
Curriculum Vitae August 2012 Guy M. Narbonne, FRSC Professor and Queen's Research Chair Office: Home: Geological Sciences and Geological Engineering #1 - 249 Macdonnell St. Queen's University Kingston, ON Kingston, ON, K7L 3N6 K7L 4C4 Ph. (613) 533-6168 / Fax (613) 533-6592 Ph. (613) 541-0842 email: [email protected] Birthdate and place: January 19, 1954; Montreal, QC, Canada Professional Affiliations and Memberships: Geological Association of Canada Palaeontological Association Paleontological Society Royal Society of Canada NASA Astrobiology Program Employment: Queen's Research Chair Queen's University 2005-15 Professorial Fellow University of New South Wales 2011-pres. Honourary Associate Monash University 2008-pres. Associate Researcher Royal Ontario Museum 2002-pres. Adjunct Professor Macquarie University 1997-pres. Professor Queen's University 1994-pres. Associate Professor Queen's University 1987-1994 Assistant Professor Queen's University 1982-87 N.S.E.R.C. Post-doctoral Fellow Université de Montréal 1981-82 Education: University of Ottawa Ph.D. 1975-1981 Brock University B.Sc. 1971-1975 Research Interests: Early evolution of animals and their ecosystems (Neoproterozoic - Cambrian) Ediacaran and Paleozoic trace fossils (systematics, paleoecology, evolution) Proterozoic and Paleozoic reefs (paleoecology, sedimentology) Proterozoic carbonate and siliciclastic sedimentation Proterozoic chemical oceanography 1 HONOURS: Research Awards: 2010 – Elected Fellow of the Royal Society of Canada and Canadian Academy of Science 2009 -
Ediacaran Biozones Identified with Network Analysis Provide Evidence for Pulsed Extinctions of Early Complex Life
ARTICLE https://doi.org/10.1038/s41467-019-08837-3 OPEN Ediacaran biozones identified with network analysis provide evidence for pulsed extinctions of early complex life A.D. Muscente1,11, Natalia Bykova 2, Thomas H. Boag3, Luis A. Buatois4, M. Gabriela Mángano4, Ahmed Eleish5, Anirudh Prabhu5, Feifei Pan5, Michael B. Meyer6, James D. Schiffbauer 7,8, Peter Fox5, Robert M. Hazen9 & Andrew H. Knoll1,10 1234567890():,; Rocks of Ediacaran age (~635–541 Ma) contain the oldest fossils of large, complex organisms and their behaviors. These fossils document developmental and ecological innovations, and suggest that extinctions helped to shape the trajectory of early animal evolution. Conventional methods divide Ediacaran macrofossil localities into taxonomically distinct clusters, which may represent evolutionary, environmental, or preservational variation. Here, we investigate these possibilities with network analysis of body and trace fossil occurrences. By partitioning multipartite networks of taxa, paleoenvironments, and geologic formations into community units, we distinguish between biostratigraphic zones and paleoenvir- onmentally restricted biotopes, and provide empirically robust and statistically significant evidence for a global, cosmopolitan assemblage unique to terminal Ediacaran strata. The assemblage is taxonomically depauperate but includes fossils of recognizable eumetazoans, which lived between two episodes of biotic turnover. These turnover events were the first major extinctions of complex life and paved the way for the Cambrian radiation of animals. 1 Department of Earth and Planetary Sciences, Harvard University, Cambridge, MA 02138, USA. 2 Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch Russian Academy of Sciences, Novosibirsk 630090, Russia. 3 Department of Geological Sciences, Stanford University, Stanford, CA 94305, USA. 4 Department of Geological Sciences, University of Saskatchewan, Saskatoon, SK S7n 5E2, Canada. -
The Relative Influence of Niche Versus Neutral Processes on Ediacaran Communities
bioRxiv preprint doi: https://doi.org/10.1101/443275; this version posted December 10, 2018. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. 1 The relative influence of niche versus neutral processes on Ediacaran communities 2 3 *Emily G .Mitchell1, Simon Harris2, Charlotte G. Kenchington1, Philip Vixseboxse3, Lucy 4 Roberts4, Catherine Clark1, Alexandra Dennis1, Alexander G. Liu1, Philip R. Wilby2. 5 6 1Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 7 3EQ, UK. 8 2British Geological Survey, Nicker Hill, Keyworth, Nottingham NG12 5GG, United 9 Kingdom. 10 3School of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, 11 Bristol, BS8 1RJ, United Kingdom. 12 4Department of Zoology, University of Cambridge… 13 14 *Correspondence: [email protected]. 15 16 Keywords: Ediacaran, neutral theory, spatial point process analysis, paleoecology, ecology, 17 paleontology, rangeomorph 18 19 1 bioRxiv preprint doi: https://doi.org/10.1101/443275; this version posted December 10, 2018. The copyright holder for this preprint (which was not certified by peer review) is the author/funder. All rights reserved. No reuse allowed without permission. 20 Abstract 21 A fundamental question in community ecology is the relative influence of niche versus 22 neutral processes in determining ecosystem dynamics. The extent to which these processes 23 structured early animal communities is yet to be explored. Here we use spatial point process 24 analyses (SPPA) to determine the influence of niche versus neutral processes on early total- 25 group metazoan paleocommunities from the Ediacaran Period ~565 million years in age. -
Recognizing the Reproductive Mode of Fractofusus Through Spatial
Mitchell, E., Kenchington, C., Liu, A. G. S. C., Matthews, J., & Butterfield, N. (2015). Reconstructing the reproductive mode of an Ediacaran macro-organism. Nature, 524(7565), 343-346. https://doi.org/10.1038/nature14646 Peer reviewed version License (if available): Unspecified Link to published version (if available): 10.1038/nature14646 Link to publication record in Explore Bristol Research PDF-document 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/ 1 Reconstructing the reproductive mode of an Ediacaran macro-organism 2 Mitchell, Emily G.1, Kenchington, Charlotte G.1, Liu, Alexander G.2, Matthews, Jack J.,3 and 3 Butterfield, Nicholas J.1 4 1Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge, CB2 5 3EQ, U.K. Email: [email protected] Telephone: +44 (0)1223 322772 6 2School of Earth Sciences, University of Bristol, Life Sciences Building, 24 Tyndall Avenue, 7 Bristol, BS8 1TQ, U.K. 8 3Department of Earth Sciences, University of Oxford, South Parks Road, Oxford, OX1 3AN, 9 U.K. 10 11 Enigmatic macrofossils of late Ediacaran age (580–541 million years ago [Ma]) provide the 12 oldest known record of diverse complex organisms on Earth, lying between the microbially- 13 dominated ecosystems of the Proterozoic and the Cambrian emergence of the modern 14 biosphere.1