Spatial Analyses of Ediacaran Communities at Mistaken Point
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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. -
Lessons from the Fossil Record: the Ediacaran Radiation, the Cambrian Radiation, and the End-Permian Mass Extinction
OUP CORRECTED PROOF – FINAL, 06/21/12, SPi CHAPTER 5 Lessons from the fossil record: the Ediacaran radiation, the Cambrian radiation, and the end-Permian mass extinction S tephen Q . D ornbos, M atthew E . C lapham, M argaret L . F raiser, and M arc L afl amme 5.1 Introduction and altering substrate consistency ( Thayer 1979 ; Seilacher and Pfl üger 1994 ). In addition, burrowing Ecologists studying modern communities and eco- organisms play a crucial role in modifying decom- systems are well aware of the relationship between position and enhancing nutrient cycling ( Solan et al. biodiversity and aspects of ecosystem functioning 2008 ). such as productivity (e.g. Tilman 1982 ; Rosenzweig Increased species richness often enhances ecosys- and Abramsky 1993 ; Mittelbach et al. 2001 ; Chase tem functioning, but a simple increase in diversity and Leibold 2002 ; Worm et al. 2002 ), but the pre- may not be the actual underlying driving mecha- dominant directionality of that relationship, nism; instead an increase in functional diversity, the whether biodiversity is a consequence of productiv- number of ecological roles present in a community, ity or vice versa, is a matter of debate ( Aarssen 1997 ; may be the proximal cause of enhanced functioning Tilman et al. 1997 ; Worm and Duffy 2003 ; van ( Tilman et al. 1997 ; Naeem 2002 ; Petchey and Gaston, Ruijven and Berendse 2005 ). Increased species rich- 2002 ). The relationship between species richness ness could result in increased productivity through (diversity) and functional diversity has important 1) interspecies facilitation and complementary implications for ecosystem functioning during resource use, 2) sampling effects such as a greater times of diversity loss, such as mass extinctions, chance of including a highly productive species in a because species with overlapping ecological roles diverse assemblage, or 3) a combination of biologi- can provide functional redundancy to maintain cal and stochastic factors ( Tilman et al. -
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. -
PERSATUAN GEOLOGI MALAYSIA WARTA GEOLOGI NEWSLETTER of the GEOLOGICAL SOCIETY of MALAYSIA
PERSATUAN GEOLOGI MALAYSIA WARTA GEOLOGI NEWSLETTER of the GEOLOGICAL SOCIETY OF MALAYSIA 50TH ANNIVERSARY SPECIAL ISSUE Jilid 43 OCTOBER – DECEMBER Volume 43 No. 4 2017 No. 4 ISSN 0126 - 5539 PP2509/07/2013(032786) Warta Geologi Newsletter of the Geological Society of Malaysia PERSATUAN GEOLOGI MALAYSIA Editor Geological Society of Malaysia Wan Hasiah Abdullah (University of Malaya) Council 2017/2018 Editorial Board President : Mr. Abd. Rasid Jaapar Chow Weng Sum Vice President : Dr. Che Aziz Ali Universiti Teknologi Petronas, Malaysia Secretary : Mr. Lim Choun Sian Azman A. Ghani Assistant Secretary : Mr. Askury Abd Kadir University of Malaya, Malaysia Treasurer : Mr. Ahmad Nizam Hasan Harry Doust Editor : Prof. Dr. Wan Hasiah Abdullah The Netherlands & Vrije Universiteit, Immediate Past President : Dr. Mazlan Madon Amsterdam Councillors : Ms. Marelyn Telun Daniel Robert Hall Dr. Meor Hakif Amir Hassan University of London, UK Mr. Muhammad Ashahadi Dzulkafli Dr. Norbet Simon Howard Johnson Imperial College London, UK Mr. Nicholas Jacob Dr. Nur Iskandar Taib Ibrahim Komoo Mr. Tan Boon Kong Universiti Kebangsaan Malaysia, Malaysia Dato’ Yunus Abdul Razak Alfredo Lagmay University of the Philippine, Philippine Lee Chai Peng University of Malaya, Malaysia The Geological Society of Malaysia was founded in Mohd Shafeea Leman 1967 with the aim of promoting the advancement of Universiti Kebangsaan Malaysia, Malaysia geoscience, particularly in Malaysia and Southeast Asia. The Society has a membership of about 600 Ian Metcalfe local and international geoscientists. University of New England, Australia Ng Tham Fatt Warta Geologi (Newsletter of the Geological University of Malaya, Malaysia Society of Malaysia) is published quarterly by the Society. Warta Geologi covers short geological Peter R. -
Ordination Methods and the Evaluation of Ediacaran Communities
Chapter 1 Ordination Methods and the Evaluation of Ediacaran Communities Matthew E. Clapham Contents 1.1 Introduction...................................................................................................................... 000 1.2 Dataset Summary............................................................................................................. 000 1.3 Data Standardization........................................................................................................ 000 1.4 Ordination Methods......................................................................................................... 000 1.4.1 Principal Components Analysis (PCA)................................................................ 000 1.4.2 Correspondence and Detrended Correspondence Analysis (CA/DCA)............................................................................................. 000 1.4.3 Non-Metric Multidimensional Scaling (NMDS)................................................. 000 1.5 Comparison and Interpretation of Results....................................................................... 000 1.6 Conclusion....................................................................................................................... 000 References................................................................................................................................. 000 Abstract Analysis of paleocommunity data poses a challenge because of its multivariate nature, containing counts of many species in many samples. -
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. -
64Th Palaeontological Association Annual Meeting
64TH PALAEONTOLOGICAL ASSOCIATION ANNUAL MEETING 16 –18 DECEMBER 2020 OXFORD UNIVERSITY MUSEUM OF NATURAL HISTORY The Palaeontological Association 64th Annual Meeting Virtual meeting 16th–18th December 2020 Oxford University Museum of Natural History PROGRAMME ABSTRACTS AGM papers ANNUAL MEETING Palaeontological Association 1 The Palaeontological Association 64th Annual Meeting 16 –18 December 2020 Hosted online by Oxford University Museum of Natural History The programme and abstracts for the 64th Annual Meeting of the Palaeontological Association are provided after the following information and summary of the meeting. Platforms The Annual Meeting will take place online, hosted by the Oxford University Museum of Natural History, UK. All talks will be broadcast via the WebinarJam platform. We recommend using Google Chrome when attending WebinarJam events. The poster sessions will take place on the Discord platform, which you will be able to access via your web browser, or by downloading the Discord application. Delegates will be e-mailed a set of personal links to access all content, as well as guidance on how to access the conference sessions. Fringe events should be registered for separately. Presentation formats The Organizing Committee would like to emphasize that all presentation formats – standard talks, flash talks and posters – have equal importance. The three different presentation styles offer varied ways to present research and discuss it with colleagues. In all cases presenting authors will be able to deliver their research and debate the content with delegates at the Annual Meeting. Oral Presentations Presenters giving standard talks have been allocated 15 minutes; these talks should last for no more than 12 minutes to allow time for questions and switching between presenters. -
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). -
The Ediacaran Fossils of Charnwood Forest: Shining New Light on a Major Biological
*Manuscript Click here to view linked References 1 The Ediacaran fossils of Charnwood Forest: shining new light on a major biological 2 revolution 3 Charlotte G. Kenchingtona, Simon J. Harrisb, Philip B. Vixseboxsec, Chris Pickupd, Philip R. 4 Wilbyb 5 aDepartment of Earth Sciences, Memorial University of Newfoundland, Prince Philip Drive, 6 St John’s A1B 3X5, Canada. Present address: Department of Earth Sciences, University of 7 Cambridge, Downing Street, Cambridge CB2 3EQ, UK. [email protected] 8 bBritish Geological Survey, Environmental Science Centre, Nicker Hill, Keyworth, Nottingham 9 NG12 5GG, UK. [email protected] [email protected] 10 cSchool of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, 11 Bristol BS8 1RJ, UK. [email protected] 12 dSchool of Arts & Humanities, Nottingham Trent University, Mary Anne Evans Building, 13 Clifton Campus, Nottingham NG11 8NS, UK. [email protected] 14 Corresponding author: [email protected] 15 16 Keywords 17 Ediacaran; Charnwood Forest; Reflectance Transformation Imaging; Avalon Assemblage 18 19 Abstract 20 Charnwood Forest (UK) hosts some of the oldest and best-preserved macrofossils known 21 from the Ediacaran. It is the counterpoint to the more widely studied fossil sites of south- 22 eastern Newfoundland (Canada), which include the recently-designated UNESCO World 23 Heritage Site of Mistaken Point. Discoveries made in Charnwood Forest since 2008 have the 24 potential to revolutionise our understanding of the evolution of complex macroscopic life 25 and the subsequent development of ‘modern’ (i.e. Phanerozoic) ecosystems. The sites in 26 Charnwood include the holotypes for several iconic Ediacaran taxa, and both the oldest and 27 potentially youngest representatives of the deep-water Avalon Assemblage. -
Of Time and Taphonomy: Preservation in The
1 OF TIME AND TAPHONOMY: PRESERVATION IN THE 2 EDIACARAN 3 Charlotte G. Kenchington1,2 and Philip R. Wilby2 4 1. Department of Earth Sciences, University of Cambridge, Downing Street, 5 Cambridge, CB2 3EQ, UK. [email protected] 6 2. British Geological Survey, Keyworth, Nottingham, NG12 5GG, UK. 7 8 ABSTRACT.—The late Neoproterozoic witnessed a revolution in the history of life: the 9 transition from a microbial world to the one we know today. The enigmatic organisms of 10 the Ediacaran hold the key to understanding the early evolution of metazoans and their 11 ecology, and thus the basis of Phanerozoic life. Crucial to interpreting the information 12 they divulge is a thorough understanding of their taphonomy: of what is preserved and 13 how it is preserved, and also of what is not preserved. Fortunately, this Period is also 14 recognized for its abundance of soft-tissue preservation, which is viewed through a wide 15 variety of taphonomic windows. Some of these, such as pyritization and carbonaceous 16 compression, are also present throughout the Phanerozoic, but the abundance and variety 17 of moldic preservation of body fossils in siliclastic settings is unique to the Ediacaran. In 18 rare cases, one organism is preserved in several preservational styles which, in 19 conjunction with our increased understanding of the taphonomic processes involved in 20 each style, allow us to more confidently interpret aspects of the biology and ecology of 21 the organisms preserved. Several groundbreaking advances in this field have been made 22 since the 1990s, and have paved the way for increasingly thorough analyses and elegant 23 interpretations.