The Fossil Record
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JVP 26(3) September 2006—ABSTRACTS
Neoceti Symposium, Saturday 8:45 acid-prepared osteolepiforms Medoevia and Gogonasus has offered strong support for BODY SIZE AND CRYPTIC TROPHIC SEPARATION OF GENERALIZED Jarvik’s interpretation, but Eusthenopteron itself has not been reexamined in detail. PIERCE-FEEDING CETACEANS: THE ROLE OF FEEDING DIVERSITY DUR- Uncertainty has persisted about the relationship between the large endoskeletal “fenestra ING THE RISE OF THE NEOCETI endochoanalis” and the apparently much smaller choana, and about the occlusion of upper ADAM, Peter, Univ. of California, Los Angeles, Los Angeles, CA; JETT, Kristin, Univ. of and lower jaw fangs relative to the choana. California, Davis, Davis, CA; OLSON, Joshua, Univ. of California, Los Angeles, Los A CT scan investigation of a large skull of Eusthenopteron, carried out in collaboration Angeles, CA with University of Texas and Parc de Miguasha, offers an opportunity to image and digital- Marine mammals with homodont dentition and relatively little specialization of the feeding ly “dissect” a complete three-dimensional snout region. We find that a choana is indeed apparatus are often categorized as generalist eaters of squid and fish. However, analyses of present, somewhat narrower but otherwise similar to that described by Jarvik. It does not many modern ecosystems reveal the importance of body size in determining trophic parti- receive the anterior coronoid fang, which bites mesial to the edge of the dermopalatine and tioning and diversity among predators. We established relationships between body sizes of is received by a pit in that bone. The fenestra endochoanalis is partly floored by the vomer extant cetaceans and their prey in order to infer prey size and potential trophic separation of and the dermopalatine, restricting the choana to the lateral part of the fenestra. -
Download Abstract Booklet Session 4
Abstract Volume 17th Swiss Geoscience Meeting Fribourg, 22nd + 23rd November 2019 4 Palaeontology 106 4. Palaeontology Torsten Scheyer, Christian Klug, Lionel Cavin Schweizerische Paläontologische Gesellschaft Kommission des Schweizerischen Paläontologischen Abhandlungen (KSPA) Symposium 4: Palaeontology TALKS: 4.1 Alleon J., Bernard S., Olivier N., Thomazo C., Marin-Carbonne J.: Molecular characteristics of organic microfossils in Paleoarchean cherts 4.2 Antcliffe J.B., Jessop W., Daley A.C.: Prey fractionation in the Archaeocyatha and its implication for the ecology of the first animal reef systems 4.3 Bastiaans D., Kroll J.F., Jagt J.W.M., Schulp A.S.: Cranial pathologies in a Late Cretaceous mosasaur from the Netherlands: behavioral and immunological implications. 4.4 Daley A.C., Antcliffe J.B., Lheritier M.: Understanding the fossil record of arthropod moulting using experimental taphonomic approaches 4.5 Dziomber L., Foth C., Joyce W.G.: A geometric morphometric study of turtle shells 4.6 Evers S.W.: A new hypothesis of turtle relationships provides insights into the evolution of marine adaptation, and turtle diversification 4.7 Fau M., Villier L., Ewin T.: Diversity of early Forcipulatacea (Asteroidea) 4.8 Ferrante C., Cavin L.: Weird coelacanths from the Triassic of Switzerland 4.9 Frey L., Coates M.I., Rücklin M., Klug C.: A new early symmoriid with an unusual jaw articulation from the Late Devonian of Morocco 4.10 Friesenbichler E., Hautmann M., Bucher H.: Palaeoecology of benthic macroinvertebrates from three Middle Triassic -
Caswell Et Al. 2019 Preprint Part1
© 2019. This manuscript version is made available under the CC-BY-NC-ND 4.0 license http:// creativecommons.org/licenses/by-nc-nd/4.0/ 1 An ecological status indicator for all time: Are AMBI and 2 M-AMBI effective indicators of change in deep time? 3 4 Bryony A. Caswell*1, 2, Chris L. J. Frid3, Angel Borja4 5 6 1Environmental Futures Research Institute, Griffith University, Gold Coast, 7 Queensland 4222, Australia. 8 2School of Environmental Science, University of Hull, Hull, HU6 7RX, UK 9 3School of Environment and Science, Griffith University, Gold Coast, QLD 4222, 10 Australia. 11 4AZTI, Marine Research Division, Herrera Kaia Portualdea s/n, 20100 Pasaia, Spain 12 13 *Corresponding author: email; Phone: +44(0)1482466341 14 15 Abstract 16 17 Increasingly environmental management seeks to limit the impacts of human 18 activities on ecosystems relative to some ‘reference’ condition, which is often the 19 presumed pre-impacted state, however such information is limited. We explore how 20 marine ecosystems in deep time (Late Jurassic)are characterised by AZTI’s Marine 21 Biotic Index (AMBI), and how the indices responded to natural perturbations. AMBI 22 is widely used to detect the impacts of human disturbance and to establish 23 management targets, and this study is the first application of these indices to a fossil 24 fauna. Our results show AMBI detected changes in past seafloor communities (well- 25 preserved fossil deposits) that underwent regional deoxygenation in a manner 26 analogous to those experiencing two decades of organic pollution. These findings 27 highlight the potential for palaeoecological data to contribute to reconstructions of 28 pre-human marine ecosystems, and hence provide information to policy makers and 29 regulators with greater temporal context on the nature of ‘pristine’ marine 30 ecosystems. -
A Passion for Palaeontology September 22, 2012-March 17, 2013
BACK COVER PAGE COVER PAGE Bearing Witness Inside the ROM Governors A dark chapter in ROM NEWSLETTER OF THE Cambodia’s history ROM GOVERNORS The Institute for Contemporary FALL/WINTER 2 012 Summer at the ROM has been a whirlwind of activity. Culture (ICC) presents Observance Exciting new initiatives such as Friday Night Live and our and Memorial: Photographs from family weekend programming have been extremely popular S-21, Cambodia, featuring over 100 and we have seen many new visitors and partners come photographs developed from original through our doors. Also hugely successful has been our negatives abandoned by the Khmer Special thanks to Susan Crocker and INSIDER groundbreaking exhibition Ultimate Dinosaurs: Giants from Rouge in January 1979, at the S-21 secret John Hunkin, Ron Graham, the Gondwana, which pioneers the use of Augmented Reality prison in Phnom Penh, Cambodia. Honourable William C. Graham and and includes the largest dinosaur ever mounted in Canada. Curated by Photo Archive Group, and Cathy Graham, Deanna Horton, Dr. Carla Shapiro from the Munk School Richard W. Ivey, and Sarah and Tom This month, it is a great pleasure to welcome Robert Pierce of Global Affairs, University of Toronto, Milroy for their generous support of this as the new chairman of the Board of Governors. As a this exhibition calls attention to the exhibition. For information on how you long-time volunteer, Board member for more than 12 years, atrocities in Cambodia in the 1970s can support Observance and Memorial and supporter of the ROM, Rob has served in a leadership or to make a donation to the ICC, BIG and human rights issues. -
PROGRAMME ABSTRACTS AGM Papers
The Palaeontological Association 63rd Annual Meeting 15th–21st December 2019 University of Valencia, Spain PROGRAMME ABSTRACTS AGM papers Palaeontological Association 6 ANNUAL MEETING ANNUAL MEETING Palaeontological Association 1 The Palaeontological Association 63rd Annual Meeting 15th–21st December 2019 University of Valencia The programme and abstracts for the 63rd Annual Meeting of the Palaeontological Association are provided after the following information and summary of the meeting. An easy-to-navigate pocket guide to the Meeting is also available to delegates. Venue The Annual Meeting will take place in the faculties of Philosophy and Philology on the Blasco Ibañez Campus of the University of Valencia. The Symposium will take place in the Salon Actos Manuel Sanchis Guarner in the Faculty of Philology. The main meeting will take place in this and a nearby lecture theatre (Salon Actos, Faculty of Philosophy). There is a Metro stop just a few metres from the campus that connects with the centre of the city in 5-10 minutes (Line 3-Facultats). Alternatively, the campus is a 20-25 minute walk from the ‘old town’. Registration Registration will be possible before and during the Symposium at the entrance to the Salon Actos in the Faculty of Philosophy. During the main meeting the registration desk will continue to be available in the Faculty of Philosophy. Oral Presentations All speakers (apart from the symposium speakers) have been allocated 15 minutes. It is therefore expected that you prepare to speak for no more than 12 minutes to allow time for questions and switching between presenters. We have a number of parallel sessions in nearby lecture theatres so timing will be especially important. -
Sedimentation of the Lower Cretaceous Xiagou Formation and Its Response to Regional Tectonics in the Qingxi Sag, Jiuquan Basin, NW China
Cretaceous Research 47 (2014) 72e86 Contents lists available at ScienceDirect Cretaceous Research journal homepage: www.elsevier.com/locate/CretRes Sedimentation of the Lower Cretaceous Xiagou Formation and its response to regional tectonics in the Qingxi Sag, Jiuquan Basin, NW China Si Chen a,b, Hua Wang a,*, Jun Wei c, Zhenyu Lv d, Huajun Gan a, Siding Jin a a Key Laboratory of Tectonics and Petroleum Resources, MOE, China University of Geosciences, Wuhan 430074, China b Jackson School of Geosciences, The University of Texas at Austin, 78712, USA c PetroChina Yumen Oilfield Company, Yumen 735200, China d Tianjin Branch of CNOOC Ltd., Tianjin 300452, China article info abstract Article history: Under the constraint of an isochronous sequence stratigraphic framework, sediment infill of the Xiagou Received 24 May 2013 Formation reflects the overall control of dynamic tectonic movements and episodic sedimentations in Accepted in revised form 11 November 2013 the Qingxi Sag. Structure reactivity during post-depositional processes could cause stratigraphic varia- Available online 11 December 2013 tions in longitudinal time and lateral space. This study documents sediment infill features and their response to the tectonic evolutions of the Qingxi Sag. The data sets include comparison of cores, well Keywords: drilling, 3D seismic, inter-well correlation, wave impedance inversion profiles, original strata recovery Jiuquan Basin data, sedimentary facies spatial evolution and their superimposition with paleogeomorphology. Qingxi Sag Xiagou Formation The Jiuquan Basin is a Mesozoic-Cenozoic superposition basin comprising an early rifting graben phase Sediment infill and a later compression phase. Since the Early Cretaceous, the basin has undergone four major tectonic Tectonic evolution episodes: 1) extension during the Early Cretaceous, 2) tectonic inversion caused by northwest-southeast contraction from the Late Cretaceous to the Paleocene, 3) weak extension from the Eocene to the Miocene and 4) contraction from the Miocene to the present. -
The Cambrian Explosion: a Big Bang in the Evolution of Animals
The Cambrian Explosion A Big Bang in the Evolution of Animals Very suddenly, and at about the same horizon the world over, life showed up in the rocks with a bang. For most of Earth’s early history, there simply was no fossil record. Only recently have we come to discover otherwise: Life is virtually as old as the planet itself, and even the most ancient sedimentary rocks have yielded fossilized remains of primitive forms of life. NILES ELDREDGE, LIFE PULSE, EPISODES FROM THE STORY OF THE FOSSIL RECORD The Cambrian Explosion: A Big Bang in the Evolution of Animals Our home planet coalesced into a sphere about four-and-a-half-billion years ago, acquired water and carbon about four billion years ago, and less than a billion years later, according to microscopic fossils, organic cells began to show up in that inert matter. Single-celled life had begun. Single cells dominated life on the planet for billions of years before multicellular animals appeared. Fossils from 635,000 million years ago reveal fats that today are only produced by sponges. These biomarkers may be the earliest evidence of multi-cellular animals. Soon after we can see the shadowy impressions of more complex fans and jellies and things with no names that show that animal life was in an experimental phase (called the Ediacran period). Then suddenly, in the relatively short span of about twenty million years (given the usual pace of geologic time), life exploded in a radiation of abundance and diversity that contained the body plans of almost all the animals we know today. -
Late Carboniferous Tropical Dryland Ecosystem, Joggins, Nova Scotia1
Report of Activities 2002 181 Late Carboniferous Tropical Dryland Ecosystem, 1 Joggins, Nova Scotia H. J. Falcon-Lang and J. H. Calder Museum dioramas usually depict the Late Carboniferous tropical zone as being covered by humid rainforests composed of densely spaced tree-sized lycopsids. However, new evidence from the Langsettian fossil cliffs of Joggins, Nova Scotia suggests that this may only be half the story. At this classic site, grey coal-bearing units deposited in humid wetland coastal plain environments and containing 'normal' lycopsid-dominated rainforest vegetation are interbedded with red bed units. The red bed units, which are the focus of this paper, were deposited in seasonal dryland alluvial environment and contain an unusual floral and faunal assemblage. Depauperate floral remains in the deposits of anastomosing river channels, crevasse splays, and overbank muds are dominated by cordaite gymnosperms (Cordaites leaves, Artisia pith casts, and woody Dadoxylon trunks and branches; >80% of specimens). Present in subordinate numbers are pteridosperms (Eusphenopteris), sphenopsids (Calamites) and lycopsids (Sigillaria). A high proportion of this plant material has been charred in wildfires. Faunal remains associated with waterhole deposits in seasonally dry channels include land snails (Dendropupa), giant freshwater clams (Asterodonta) and the pelvic girdle and jaw of loxomatid reptiles. These data indicate that Late Carboniferous dryland tropical environments supported low diversity, fire-prone gymnospermous vegetation consisting mostly of shrubs or small trees inhabited by a unique fauna. At Joggins, gymnospermous dryland ecosystems repeatedly alternated with lycopsid wetland ecosystems, perhaps in response to glacial-interglacial climate rhythms. 16th European Palaeobotany and Palynology Conference, Athens, Greece; in Abstracts with Programs, p. -
Appendix A. Supplementary Material
Appendix A. Supplementary material Comprehensive taxon sampling and vetted fossils help clarify the time tree of shorebirds (Aves, Charadriiformes) David Cernˇ y´ 1,* & Rossy Natale2 1Department of the Geophysical Sciences, University of Chicago, Chicago 60637, USA 2Department of Organismal Biology & Anatomy, University of Chicago, Chicago 60637, USA *Corresponding Author. Email: [email protected] Contents 1 Fossil Calibrations 2 1.1 Calibrations used . .2 1.2 Rejected calibrations . 22 2 Outgroup sequences 30 2.1 Neornithine outgroups . 33 2.2 Non-neornithine outgroups . 39 3 Supplementary Methods 72 4 Supplementary Figures and Tables 74 5 Image Credits 91 References 99 1 1 Fossil Calibrations 1.1 Calibrations used Calibration 1 Node calibrated. MRCA of Uria aalge and Uria lomvia. Fossil taxon. Uria lomvia (Linnaeus, 1758). Specimen. CASG 71892 (referred specimen; Olson, 2013), California Academy of Sciences, San Francisco, CA, USA. Lower bound. 2.58 Ma. Phylogenetic justification. As in Smith (2015). Age justification. The status of CASG 71892 as the oldest known record of either of the two spp. of Uria was recently confirmed by the review of Watanabe et al. (2016). The younger of the two marine transgressions at the Tolstoi Point corresponds to the Bigbendian transgression (Olson, 2013), which contains the Gauss-Matuyama magnetostratigraphic boundary (Kaufman and Brigham-Grette, 1993). Attempts to date this reversal have been recently reviewed by Ohno et al. (2012); Singer (2014), and Head (2019). In particular, Deino et al. (2006) were able to tightly bracket the age of the reversal using high-precision 40Ar/39Ar dating of two tuffs in normally and reversely magnetized lacustrine sediments from Kenya, obtaining a value of 2.589 ± 0.003 Ma. -
Evidence for Gill Slits and a Pharynx in Cambrian Vetulicolians: Implications for the Early Evolution of Deuterostomes Ou Et Al
Evidence for gill slits and a pharynx in Cambrian vetulicolians: implications for the early evolution of deuterostomes Ou et al. Ou et al. BMC Biology 2012, 10:81 http://www.biomedcentral.com/1741-7007/10/81 (2 October 2012) Ou et al. BMC Biology 2012, 10:81 http://www.biomedcentral.com/1741-7007/10/81 RESEARCHARTICLE Open Access Evidence for gill slits and a pharynx in Cambrian vetulicolians: implications for the early evolution of deuterostomes Qiang Ou1, Simon Conway Morris2*, Jian Han3, Zhifei Zhang3, Jianni Liu3, Ailin Chen4, Xingliang Zhang3 and Degan Shu1,3* Abstract Background: Vetulicolians are a group of Cambrian metazoans whose distinctive bodyplan continues to present a major phylogenetic challenge. Thus, we see vetulicolians assigned to groups as disparate as deuterostomes and ecdysozoans. This divergence of opinions revolves around a strikingly arthropod-like body, but one that also bears complex lateral structures on its anterior section interpreted as pharyngeal openings. Establishing the homology of these structures is central to resolving where vetulicolians sit in metazoan phylogeny. Results: New material from the Chengjiang Lagerstätte helps to resolve this issue. Here, we demonstrate that these controversial structures comprise grooves with a series of openings. The latter are oval in shape and associated with a complex anatomy consistent with control of their opening and closure. Remains of what we interpret to be a musculature, combined with the capacity for the grooves to contract, indicate vetulicolians possessed a pumping mechanism that could process considerable volumes of seawater. Our observations suggest that food captured in the anterior cavity was transported to dorsal and ventral gutters, which then channeled material to the intestine. -
Interpretive Programs in Yoho National Park
Interpretive Programs Yoho National Park July 1 - August 31, 2015 Guided Activities Evening Hikes Programs SUNDAY MONDAY TUESDAY WEDNESDAY THURSDAY FRIDAY SATURDAY Burgess Shale: Burgess Shale: Burgess Shale: Burgess Shale: Burgess Shale: Walcott Quarry Walcott Quarry Walcott Quarry Walcott Quarry Walcott Quarry Reservation Required Reservation Required Reservation Required Reservation Required Reservation Required 7 am 7 am 7 am 7 am 7 am Burgess Shale: Burgess Shale: Emerald Lake Activities with Burgess Shale: Mt. Stephen Mt. Stephen Guided Walk Interpreters Mt. Stephen Reservation Required Reservation Required Emerald Lake Bridge Emerald Lake Reservation Required 7 am 7 am 1-4 pm 1-4 pm 7 am Burgess Shale Learn to ESI: EcoSystem Rock Stars Geocache Investigator Kicking Horse Kicking Horse Kicking Horse Campground Theatre Campground Theatre Campground Theatre 7:30 pm 7:30 pm 7:30 pm Canada Day, July 1st: Watch for fun, hands-on activities at the Canada Day celebration in Yoho. For more information contact the Yoho Visitor Centre (250-343-6783). Parks Day, July 18th: Emerald Lake Guided Walk, See description for details, 1-4 pm. en français nt offert PLEASE NOTE: Events subject to change without notice. Participants require a valid park pass. All pro- Ces présentations sont en anglais seulement. Pour obtenir des renseignements en grams free unless otherwise noted. français sur les présentations, téléphonez au 250-343-6783. Égaleme Burgess Shale Evening Activities $ Interpretive Programs Guided Hikes Programs Yoho National Park Join a Parks Canada interpreter on a full- July 1 - August 31, 2015 Activities with Interpreters day hike to the Walcott Quarry, Mt. Stephen Kicking Horse Watch for interpreters at park hot-spots. -
The Canadian Experience by Rebecca Kennedy
World Heritage nominations – the Canadian experience February 2020 Killarney, Ireland 1 • The World Heritage Convention in Canada • Canadian Tentative List process • Heart’s Content Cable Station, Newfoundland • Lessons learned in development of Canadian nominations • Transboundary and serial nominations • Looking ahead 2 Rebecca Kennedy, “focal point” for World Heritage programme in Canada Who is this person?! 3 Why is Parks Canada Our national involved in Canada’s World office Heritage? Parks Canada has many responsibilities that extend beyond management of National Historic Sites and National Parks 4 Why is Parks Canada involved in Canada’s World Heritage? Given its expertise in cultural and natural heritage, Parks Canada was designated as the lead for World Heritage on behalf of the Government of Canada in 1976 • In 1978, Nahanni National Park and L’Anse aux Meadows National Historic Site were in the first group of 11 sites put on the World Heritage List 5 Canada and World Heritage • Canada is well respected for its expertise and credibility in our work on World Heritage • Elected member of the World Heritage Committee from 1976 to 1978, from 1985 to 1991, from 1995 to 2001 and from 2005 to 2009 • Committee meeting host in 1990 (Banff) and 2008 (Québec City) 6 Canada and World Heritage As the Government of Canada’s representative for the Convention, Parks Canada… • leads the Canadian delegation at Committee meetings • manages Canada’s official participation in relevant international workshops and provides policy input as requested